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After many calls and chats with Sprint I managed to get a Nexus 6P on the 'free' one year unlimited plan.
But then I broke the screen. Not a big deal I thought, as my friend has another 6P he isn't using.
But it is a big deal because Sprint customer service can't activate the other 6P.
**bleep** Sprint? Is the goal to make it so hard to use older devices customers give up an buy a new one? I will never do that. I will go to a GSM network before caving in to Sprints twisted games and bait and switch. It will be a long time before I ever recommend friends or family switch to Sprint, even for a 'free' unlimited plan. The rest of the world can swap SIMs without issue, but Sprint is stuck in the cell stone age.
Nexus 6p works on Sprint. Full Stop. Bust Sprint doesn't wan't to activate them. If your time is valuble to you use your Nexus 6P on another network.
Solved! Go to Solution.
As with most BYOD and probably your Nexus 6P, the phone will need to be added to the database. That process can take up to 10 days. I'm happy to submit the ticket for you. I'll send you a private message to get started.
It was added to the database very quickly.
Thank you so much!
This experience would have been so much better if chat and phone support would have refered me to the right agent insted of telling me my device is not supported. It is unacceptable that I had to search on-line and find help on this site on my own. Nobody from Sprint said 'hey, maybe check out Sprints on-line community support site'.
Sprint S.M.A.R.T Agents
Sprint S.M.A.R.T Agent are here to help Monday through Friday 6:00 AM CT - 6:00 PM CT. If you need to speak to an agent outside of these hours, please visit Sprint Chat


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Doctor of Acupuncture & Oriental Medicine
Dr. Lombardo's lifelong enthusiasm for wellness and lifestyle medicine led his integrative healthcare practice to include Eastern medical modalities including acupuncture, herbal medicine, meditation, lifestyle and nutritional counseling; and Western longevity medicine modalities including evidence based nutraceuticals and bioidentical hormone replacement.
Ryan Lombardo received his Doctorate of Acupuncture and Oriental Medicine from the Midwest College of Oriental Medicine in Chicago, IL where he wrote the curriculum for Nutraceutical Science and Chinese Medicine. The DAOM is the highest formal educational credential available in the field of Acupuncture and Oriental Medicine in the United States. Ryan Lombardo is one of the few nationally board certified Diplomats in Acupuncture as well as being board certified in both Anti-Aging Medicine by the American Academy of Anti-Aging Medicine and Integrative Medicine by the American Association of Integrative Medicine. He holds a Master of Science in Oriental Medicine and a Bachelor of Science in Nutrition from the Midwest College of Oriental Medicine, and a Bachelor of Arts in Psychology and Certificate of Business from the University of Wisconsin-Madison. Finally, he is also a Registered Herbalist with the American Herbalist Guild and an active member of the Society of Acupuncture Research.
Ryan Lombardo has been in practice since 2003, specializing in weight loss, cosmetic acupuncture, pain relief, longevity and inflammatory conditions. Ryan Lombardo is a faculty member of Midwest College's doctoral program, leading the Nutraceutical Science and Chinese Medicine Energetics curriculum. Ryan Lombardo has been a "Featured AcuDoc" of the American Cosmetic Acupuncture Association and has been interviewed for Self Magazine, American Spa Magazine, Day Spa Magazine, Today's Chicago Woman, the Chicago Sun-Times, WGN, and various other local and national media.
Ryan Lombardo is now accepting patients interested in improving their health and their weight as they age. Patients of all ages are welcome as the practice is focused on creating physical and energetic balance, fostering healing and longevity in all aspects of life.

subset: commoncrawl


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10kt White Gold Mens Fashion Diamond Ring 0.50ctSKU:
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- 10kt White Gold Mens Fashion Diamond Ring 0.50ct
- Crafted in 10kt white gold
- Round Diamonds 0.50ct * total weight
- H-I color, I1-I2 clarity
- Ring comes in size 10
*carat weight and any measurements are approximate
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Ainge throws four TDs to lead Tennessee past MemphisSep 30, 2006 - 7:25 PM MEMPHIS, Tennessee (Ticker) -- Erik Ainge and Tennessee rolled to another victory over an intrastate rival.
Ainge threw a career high-tying four touchdowns - two to Jayson Swain - and the 15th-ranked Volunteers dominated defensively in a 41-7 rout of Memphis in a non-conference matchup.
In one of the best performances of his career, Ainge completed 23-of-27 passes for 324 yards. The junior threw three touchdowns in the second half to help the Volunteers (4-1) pull away and improve to 19-2 against in-state opponents under coach Phillip Fulmer.
Since a one-point loss to No. 5 Florida two weeks ago, Tennessee has won its last two games by a combined 74-14. But there are no more cupcakes for the Vols as they head into the meat of their schedule with games against No. 10 Georgia, Alabama, South Carolina and ninth-ranked LSU over the next five weeks.
"I'm really proud of our football team," Fulmer said. "I think we've really worked to get better during the course of the year. We still have a way to go in some areas, but we'll find out who we have healthy (Sunday) and obviously start getting ready for the Georgia Bulldogs."
Tennessee held a 13-0 lead at the break and rolled thereafter to continue its domination of the series, improving to 20-1, including 9-1 in Memphis.
Ainge connected with Swain for a 51-yard TD less than three minutes into the third quarter to open a 20-0 cushion. Five minutes later, Robert Meachem hauled in an 84-yard TD pass from Ainge to extend the lead to 27-0.
"I did a poor job of preparing our football team for this game today," said Memphis coach Tommy West, a Tennessee alumnus. "I thought Tennessee played a great game and they have a very good team. Tennessee really handed it to us and they were the more physical team and the better team."
Ainge threw his final TD pass, a seven-yarder to Bret Smith, with 12:45 to play to make it 34-0.
While Ainge was having his way with the Tigers, the defense was sensational. Memphis was outgained, 566-121, and managed only five first downs.
"I had all day to throw, didn't get sacked again," Ainge said. "Anytime I have that much time to throw, with the way the receivers are playing, that makes it really tough on the defense."
The Tigers (1-3) avoided a shutout on a 21-yard TD pass from Martin Hankins to Duke Calhoun with 3:45 remaining. Hankins was 11-of-17 for 79 yards with an interception and Calhoun had three receptions for 29 yards.
Tennessee dominated the first half, outgaining Memphis, 258-44, but settling for a pair of field goals after long drives. James Wilhoit capped a 66-yard drive in the first quarter with a 28-yard field goal and his 49-yarder with 22 seconds left in the first half finished a 67-yard march.
Ainge threw a five-yard TD pass to Swain in the second quarter to make it 10-0 and cap a 17-play, 97-yard drive.
"We had three significantly long drives two for scores and we left one at the foot line," Fulmer said. "You have to get touchdowns instead of field goals and we talked about doing what good teams do. We're trying to be a good team."
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- Iowa State to play Liberty Bowl without Cotton-Moya, Edwards Dec 30
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- No. 19 Memphis plays bowl on home field against Iowa State Dec 29
- Majority of top prospects capitalize on early signing period Dec 20
- East Tennessee State hires Randy Sanders as football coach Dec 17
- Florida adds Tennessee assistant Charlton Warren to staff Dec 15


text: Rover 1 May 9, 2011 Recently there was a Vigil 1 that fired on the ground in New Zealand. The unit in question was manufactured in mid 2006 and it had approximately 1800 hundred jumps on it. The battery was replaced less than a year ago. It had a type 3 cutter fitted – which obviously worked – just not when it was supposed to. The unit has been used entirely in 'tandem' mode. It was turned on just before midday and used for 1 jump. The main was activated at 5000 feet without complications. The gear was repacked after the jump and was placed in the gear area. The activated reserve was noticed the next day at approx 1030 am. The pilot was in the gear area at 9 am of that day and did not notice the pilot chute and bridle on the floor, so the thought is that it activated between 9 and 1030 am but this cannot be confirmed. The gear was taken away by the DZO and examined by a rigger where it was determined that the cutter had been activated. The unit has been returned to the manufacturer for testing and has been replaced with a Vigil 2 free of charge. I trust that when the reason for this incident is determined that Advanced Aerospace Designs won't be backward in coming forwards with their findings.2 wrongs don't make a right - but 3 lefts do. Share this post Link to post Share on other sites


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Swissvax Plastic Wash
Intensive plastic and vinyl trim cleaner for use inside and out. Buy online and earn loyalty points as you shop.
No Stock
How many loyalty points will I earn?
If you have created an account and are signed in, you will earn 1 point per whole £ you spend (e.g. spending £9.50 earns 9 points). The redemption value of each point you earn will vary between £0.05 and £0.15 depending on your rolling annual spend; see our loyalty points page for details.


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Reviews – Template and reviewers email address-$25.
- Why do you need to get reviews?
- 88% of consumers trust reviews.
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- 85% of Amazon Kindle readers look to book reviews before deciding to purchase.
- Get a LIST of 25+ top reviewers who reviewed books. You get their email and name.
- Use my simple templateto ask them to your review your book. Fill in the template and send them out!


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Class-action advocates deserve fair share of settlements
Mark Laffitte and his co-workers at a large staffing agency had had enough of their employer's wage theft by 2004 and, with the help of legal advocates, filed a class-action lawsuit for nearly 4,000 workers.
Class actions, like Lafitte's, benefit millions of Californians every day. Class actions promote equal pay for equal work, challenge race discrimination, safeguard the environment and deter corporate fraud and hidden fees. Class actions provide access to the courts for everybody — not just big corporations — supplying a check in our judicial system. Class actions save time and money because thousands of claims get resolved in a single case.
Eight years after Laffitte's case was filed, the employer settled for $19 million. After careful evaluation, the court awarded 33 percent of the fund to his advocates as compensation for their work. Just one class member objected to the fees and appealed the settlement. The California Supreme Court soon will decide how best to compensate the legal team that has now persevered for more than a decade representing Lafitte and his co-workers. Getting this question right in this and future cases will be critical for preserving class actions as a viable tool for justice.
At the heart of the issue is a practical problem: how to get someone — an attorney — to risk spending the time and money necessary to help victims and hold law breakers accountable. In class actions, attorneys get paid only if and when they are successful, and often after many years and substantial investment of their own money in fronting expenses. The answer, under California law, is to provide fair compensation to the advocates who undertake and win these David-versus-Goliath struggles.
As it stands now, if a case is successful, then the judge, who has observed the advocates' work firsthand, sets the compensation. He or she is in the best position to know how good a job has been done and whether the advocates have achieved a good result. Californians don't need another expensive layer of bureaucracy to second-guess our able and experienced judges.
Judges use the same methods to compensate a successful team of class-action advocates that are used in ordinary cases, either allocating a percentage of the amount of the money received by the plaintiff or authorizing an hourly rate.
In cases where a percentage is used, the average in class actions is 25 percent, lower than the up to 40 percent that a person would pay to bring the same lawsuit on his or her own. Compensating the legal team in class actions based on a percentage ensures that the attorney's interest is always 100 percent aligned with the victim's. Awarding an hourly rate, on the other hand, makes sense when the result is not money, but corporate or government reform, such as ending a discriminatory practice.
Every class member gets a notice about what the proposed payment to the legal team is and can provide his or her views to the judge. No fee is ever approved under cover of night — in every class action, the judge scrutinizes the nature and quality of work done to ensure that the compensation is fair.
Class-action justice is already under attack by big business — understandably not its biggest fan. Further restrictions will only discourage the already small community of advocates who take on these tough cases, depriving ordinary Californians of equal access to justice.
Jocelyn D. Larkin is the executive director of the Impact Fund, a legal nonprofit that advances social justice through impact litigation. She authored a "friend of the court" brief in support of the workers in the case, Laffitte vs. Robert Half International.


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1 venue – 3 days – 135+ sessions – 136 countries and territories in attendance – 238 exhibitors in 21,000 Square Metre Exhibit Hall – 260 speakers – unlimited opportunities
World ATM Congress 2019
Visit us on March 12 – 14, 2019
Detailed Information
Be there, see and experience our new products at the World ATM Congress on March 12-14, 2019 in Madrid, Spain. We are pleased to greet you to an exciting show filled with product highlights and presentations. Join us in booth #407.
If you have any further questions please do not hesitate to contact our Sales Team at email@example.com or by phone +49 7546 9248-42.
The Event
1 venue – 3 days – 135+ sessions – 136 countries and territories in attendance – 238 exhibitors in 21,000 Square Metre Exhibit Hall – 260 speakers – unlimited opportunities
Now entering its eighth year, World ATM Congress is the world's largest international air traffic management (ATM) exhibition and conference attracting over 8,500 people last year.
Operated by the the Civil Air Navigation Services Organisation (CANSO) in partnership with the Air Traffic Control Association (ATCA), World ATM Congress brings together the world's leading product developers, experts, stakeholders, and air navigation service providers (ANSPs). Aviation thought leaders gather for three days of conference sessions, product demonstrations and launches, contract closures and educational and networking opportunities in Madrid, Spain.
Why attend? Get unparalleled insight into key issues in the ATM industry, hands-on experience of the latest products and innovation, and potential to increase brand awareness all in one place – save time and increase revenue. World ATM Congress delivers the context, content, and contacts that suppliers and customers need to shape the future of global airspace.
World ATM Congress. The ATMosphere for business.


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**GIFTS** - 1875 Wisden - 1896 HB - Wisden Sets
Download - Wisden iPhone / iPad App - 90% Wisdens arrive next day.
Wisden Auction have teamed up with "The Nightwatchman"
New Wisden Stock & DD Club Info - Join our Wisden Club today
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|Buy Now for £7,500.00
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|09/10/2019 02:49:20
|08/11/2019 02:49:20
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|Wisden Year:
|Overall Condition:
On offer here is an 1868 Wisden in it's original wrappers and in quite exceptional condition.
The front and rear wrappers are flat and bright and unmarked.
There is an ownership name to the top of the front wrapper.
The spine is complete with the year "1868" written in ink to the spine.
The book is entirely original and without any restoration at all.
The contents of the book are in fine, clean condition.
This copy together with the 1864 that I have listed are probably the finest editions of the first 15 years that I have been able to offer for sale.
Postage is by Royal Mail Special Delivery at £7.95.
If intending to buy from outside the UK mainland please contact us before buying to ascertain methods and prices of postage.
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WESTLAKE VILLAGE, Calif. (CBS.MW) -- By some measures, Homestore.com appears to be one of the rare gems of the Internet.
It's profitable. It serves an attractive demographic group, and, at least until recently, home sales have weathered the recessionary storm gripping the rest of the economy.
Still, it's an Internet company and one that could be punished for failing to execute on its plans.
"We have a very well-defined audience, which is people who are looking for homes or selling homes, said Stuart Wolff, Homestore's founder and chief executive officer. "It's a valuable demographic, and we've found a way to reach them."
Valuable allies
The company's flagship site, Realtor.com, is the official site of the National Association of Realtors and lists nearly 1.4 million homes for sale.
Homestore relies on regional multiple listings services, homebuilders and property owners to fill its database. In addition, the company has joined forces with the National Association of Homebuilders.
The company has two streams of revenue: advertising, which accounts for 48 percent of total revenue, and subscriptions, which bring in 52 percent. Revenue from subscriptions comes from professionals looking to list properties on the Homestore network.
"Most of our advertisers are traditional companies," said Wolff. "Less than 5 percent is considered at-risk ad sales" -- in other words, Internet companies.
Shares of Homestore.com have suffered with the rest of the Net sector over the past year, falling from around $70 a year ago to below $20 in December. The stock has recovered some this year. It closed Thursday at $29.69, down 19 cents.
Homestore.com depends on AOL Time Warner AOL, -1.75%, which owns 5 percent of Homestore.com, to sell some of its advertising, and it depends on its portal partners for traffic.
Wolff anticipates that advertising will account for about 38 percent of revenue, with subscriptions making up 62 percent as the company matures.
Defining the business
Although Homestore.com looks like a real-estate-related site, Wolff prefers to consider it the technology supplier to the real-estate business and related industries.
The company HOMS is expected to add content, products and services to its site lineup, which currently comprises Homestore.com, Realtor.com, HomeBuilder.com, SpringStreet.com, Remodel.com and Homefair.com.
Robertson Stephens analyst Jay P. Leupp anticipates that the company will provide mortgage lending and other financial services over time, which, he added, could generate significant upside to his models.
Looking out as far as 2002 and 2003, the company plans to have four streams of revenue: advertising, subscriptions, international business and transactions. Transactions will probably account for the largest revenue stream, according to Wolff.
Slowdown worries
In a slowing economic environment, the company managed to accelerate its fourth-quarter sequential growth by 27 percent, up from the 24 percent growth posted at the end of the third quarter. And Wolff projects the company's revenue will continue to grow.
The economic slowdown seems to have had little effect on the housing market or Homestore.com so far. "We're insulated from many of those factors," said Wolff.
However, a recent report from the Commerce Department showed January new-home sales fell 10.9 percent to an annualized rate of 921,000, which could indicate the beginning of a weakening in the real-estate market.
And Wolff acknowledged that his company has never been through a housing recession. Still, for the time being, Wolff believes that the company's destiny is in its own hands, he said.
The latest quarter
In the fourth quarter, Homestore reported earnings of 4 cents a share, compared with a loss of 23 cents a share in the year-ago period. Analysts expected a profit of 2 cents a share, according to data from First Call/Thompson Financial. Revenue rose 182 percent from the year-earlier period, reaching $79 million.
This was the company's second straight profitable quarter but the first time it has climbed into the black solely from operations, not including gains made on investments. Currently, the company's gross margin is 72 percent-plus, and Wolff said he believes that number could go higher.
Positive comments in the fourth-quarter release prompted Leupp of Robertson Stephens and Stephen M. Fitigibbons of J.P. Morgan H&Q to raise their estimates for the fiscal year 2001.
Leupp raised his estimates for a second time in less than a month on news that the acquisition of Move.com would brighten the company's financial results immediately. Leupp raised his fiscal 2001 profit estimate from 39 cents to 44 cents and his fiscal 2002 earnings estimate from 72 cents to 84 cents.
Fitzgibbons raised his fiscal 2001 estimates to 39 cents on $348 million in revenue from 35 cents on $320.5 million in revenue. In addition, the analyst put in place a 2002 estimate of a 73-cent profit on revenue of $470 million.
According to Multex.com, the 11 analysts that follow the company currently consider it a consensus "buy/hold."
Leupp recently reiterated a "buy" rating on the stock, calling Homestore a "leading technology and media company in the $1.9 trillion residential-real-estate industry."
Possible acquisitions
As of the end of January, the company's balance sheet remains strong, with cash and cash equivalents totaling an estimated $345 million. Total assets for the company stand at $918 million, with long-term debt of about $600,000 -- that is, virtually zero.
With so much cash on hand and almost no debt, will the company continue to acquire? "We're always looking," said Wolff.
One of the company's competitors is Homeseekers HMSK. Homeseekers trades at about 38 cents a share, has zero debt and an estimated $38 million in assets -- could this be the next Homestore acquisition? Wolff wouldn't comment on any specific acquisitions but said Homestore.com does not take over competitors just to take them out of the game.
"We make strategic acquisitions that will be financially accretive to the company. And the opportunities have never been greater," said Wolff.
Homestore's recent acquisition of Move.com is proof. The deal added to both the top line and bottom line. And that's really the only way to purchase another company, said Wolff. The merger aligns the largest online real-estate and tech services company with the leading offline residential-real-estate franchiser, Cendant CD, +0.00%.
Although he said he's confident about expansion abroad, Wolff wouldn't comment on the company's international strategy.
But he noted that the international real-estate market is even bigger than the U.S. market. The company recently hired Richard Sommer to fill the newly created position of director and senior vice president of international operations.


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Orange County Infiniti Dealer Showcases New Infiniti Service Feature – Infiniti Personal Assistant
How would you like to have someone dedicated to helping you manage your life? Not just the big things, but all the little questions that take up most of your day? Infiniti of Mission Viejo wants to provide you with just that person – really, a whole fleet of people!
When you buy a new Infiniti, you will receive up to four years of your own personal corporate concierge service. The Infiniti Personal Assistant can find you the answer to any question you may have or perform any errand service you require. The motto is Anything. Anytime. Anywhere.
Your Own Personal Assistant
With one quick phone call, you can have someone find out where your favorite sports team is playing that night, make dinner reservations for you, book your flight or email you tomorrow's weather report. Very simply, think of having your own employee that solves your problems for you throughout the day.
Using your Infiniti Personal Assistant is as easy as dialing the number you receive with the free trial or purchase of your next Infiniti vehicle. This number is located in the Infiniti Personal Assistant packet; we will also help program it in to your speed-dial on your mobile phone. When dialed, your virtual office assistant will answer the phone with all the of the data they have collected from you in front of them. Remember, the Infiniti Personal Assistant is available to you anytime, even if your car is Los Angeles and you're in New York.
Sound too good to be true? Try it for yourself – free!
Experience the luxury of having someone dedicated to making your life simpler and easier - just by coming in to the dealership. Enjoy a free 30-day trial where you will have the chance to put the Infiniti Personal Concierge service to the toughest test: yours. So while you enjoy having more free time than you've ever had before, your VIP concierge will handle your day-to-day errands.
Stop in to Infiniti of Mission Viejo and find out more about the Infiniti Personal Assistant – and start your free trial today! No purchase necessary – call us at 949-916-4200.Follow @InfinitiMV


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05 Apr
Tea for Two: 5 Top Tea Rooms in St. Petersburg
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Tea has occupied a special place in Russian culture since the 17th century, when it was gifted to Tsar Michael I by the Mongolians. It quickly became the warming beverage of choice among Russian seeking to colonise the icy Siberian region and has been a staple in Russian kitchens ever since. Today, over 80% of… Continue reading


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Self defense is extremely crucial for us all, and now we hunt for different possibilities to learn more about it.
Judo is one of the very practiced sports and it teaches you various self defense techniques. Judo uniforms are a critical part because of the simple fact that it's a basic requirement so as to be able to practice the sport. They encircle three components: pants, jacket and belt, and all three are extremely important. If possible, research the best judo gi available out there so you can buy it! You should be aware of the simple fact that a dirty, poor uniform isn't accepted. The International Judo Federation outlines this aspect very clearly, so your uniform should be clean, should not smell bad or never be dry. This aspect says a good deal about how disciplined you're, that is extremely essential in judo.
We eventually become fond of this different culture's perspective upon self protection, and as strange as it may look, we sometimes like to modify our daily life style and start a new hobby that's also very useful. Judo isn't only a pastime, but a sport that builds character. Therefore, its impact upon your own personality will probably be evident.
The Japanese martial arts are extremely popular, and in case you want the culture, the sports and the discipline, then you can easily start practicing a sport such as judo that can help you become more elastic and it might save your life one day. Judo uniforms require special care and have particular wearing rules. Judo pants are mandatory. Also called "jubon", they need to be long enough to cover your legs. Before putting on your trousers, take a good look at which kind of underwear you're wearing. Full-coverage is preferable, even in case you might not feel so comfortable, but it's essential during instruction. If you are a woman, you have to know about the fact that is required to wear a snowy T-shirt under it. This is for your good, and it is also suggested for guys because after sweating a lot, you will prefer washing the T-shirts more often than the uniform.
The Judo uniforms' coats are called "kimono" and the sleeves should stretch out at least five centimeters above your wrist. The left side should be creased over the side. The last piece of this uniform is that the belt, which has a high significance on account of the fact that it leaves your judo rank. The belt ends must be tied in a square position, and it must enclose your own shoulders.
Judo uniforms are either white or blue. You'll often notice at a competition that among those opponents wears a blue uniform and another one a white one. "Judogi" is your proper Japanese title for this uniform and also the way it looks says a good deal about your personality.


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Nature Nate's has been growing and to continue to support this growth we need your help. We have worked to hone in and perfect our now existing six (6) flavors, but we are looking to expand our flavor selection. We are launching three (3) new flavors featuring Masala, Habanero Curry, and Gheesy!
These new flavors signify our approach of constant improvement and our dedication to bring about change! People need to know about this super grain! It's the most sustainable grain the world has, it's the grain of the future. Did you know that sorghum sorghum is in the top 12 non allergen foods? The health benefits of Nature Nate's Popped Sorghum include:
• CLEAN! No pesticides, herbicides, insecticides...no artificial anything
• Low or no lectins
• No GMO
• Gluten free
• Easy to digest
• No hulls
• Lower glycemic index
• May lower cholesterol
Why did I go with these new flavors? People always say to me, you need some more hardy flavors...I listen, explore, test, revise, re-revise, test, sample, listen and perfect. Would you like to learn more about the new flavors?
Gheesy has been a Nature Nate's factory favorite since we cane out with the Ghee Butter Popped Sorghum 3 years ago. At first Gheesy was just for me and my employees, but why keep a good thing to ourselves, so, we popped some up and took it to the Saturday farmers market, which by the way is where I do a lot of testing (thank you citizens of Portland Oregon and Vancouver Washington) and it out-sold all of the other flavors! What's it made out of? It's simply organic sorghum popped in organic ghee, with a little bit of sea salt and liberally coated with aged sharp white cheddar cheese powder..... get it? ghee x cheesy = Gheesy.
It's astonishingly delicious!
Sorry, this label is sideways, but you can still read it.
Masala is an Indian flavor like no other; the unique blend of spices give it a very deep comforting flavor. One child I overheard say "I don't know what this flavor is, but I cant stop eating it!"
Habanero Curry is my favorite! It has a deep flavor from a mixture of Indian spices with a slow but "lip burning" heat from the Habanero. It's all organic...certification coming soon.
All ingredients are organic, certification coming soon. Although this one is virtually lectin free, some of the spices may contain lectin but it's a very very small percentage of the content.
There you have it- I know you will enjoy these new flavors. BTW, if there's any of these flavors that may not appeal to you feel free to substitute any of my existing flavors.
A customer recently got back to me on these 3 new Popped Sorghum flavors.
"Tried all of the flavors I got yesterday...if I had to describe them in one word....phenomenal....absolutely amazing"
Risks and challenges
Risks: We have spent a lot of time developing these products and they have undergone heavy testing so the only thing left is for you to love them too!
Challenges: As a company growing rapidly cash flow has been a struggle, we have that handled with some good financing. Also, we still pop and package by hand and it's arduous but to meet our production needs, we are willing to put in the time and work necessary to bring you the products that you know and love.
Funding period
- (30 days)


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Offshore Company Dominica Second Passport Offshore Jurisdiction St Kitts 2nd Passport Tax Avoidance Tax Haven Comparisons Caribbean Mortgages Economic Citizenship Estate Planning Int. Business Companies Offshore Tax Havens Second Passport FAQ Caribbean Passport
The property is fully enclosed.
Buying Real Estate in the Barbados
Caribbean Land and Property - The Leading On-Line Source for Caribbean Property


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Welcome to the Do You Even Duel!? Tournament #4! We have some interesting characters that were drafted this time around. Prepare for a grand clash! Below are the first round matchups!
Brother Voodoo vs. Loki
Discuss the duel here.
Big Barda Vs. Rogue
Discuss the duel here.
Klarion Vs. Vandal Savage
Discuss the duel here.
Storm Vs. Ultron
Discuss the duel here.
Remember to follow #DoYouEvenComicBook and #DoyouEvenDuel on twitter!
AKA Sceritz, AKA Ophan Black Panther. A cosmic obliterator of the IVth Wall and breaker of chains of the hordes of fandoms scattered throughout the multiverse. Architect of DoYouEvenComicBook.com and Creator of IVWall.net.


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Monica D. Barrois' first career as a teacher in New Orleans, LA. spanned 13 years. She taught Pre Kindergarten and 3rd - 8th grades.
She joined her husband in a family business venture for a brief period before starting a successful career as a sales/ training manager at a major corporation.
Upon retirement, she fulfilled a dream and a promise to her Grandson that she would write a children's book with a character who looked like him. " Squirrelly Squirrels" is the result of that promise and her first book.
Ms. Barrois is a member of the Society of Children's Book Writers and Illustrators and is currently working on her second children's story. She has numerous stories in progress for adult audiences and will follow wherever her spirit and imagination takes her.


text:
> Sports & Outdoors
> iPhone 8 Case, iPhone 7 Case, iBazal Card Holder Leather Case, Business Style Soft Genuine Leather Case Back Cover with 2 Card Slots for iPhone 7/8 4.7inch - Red
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Which model can be compatible with?
ONLY for Apple iPhone 7 4.7'' (2016), please check your iPhone before placing an order
(Not including any iPhone in package, we send you phone case only)
Maintenance for Genuine Leather Items:
Keep away from high temperature, great pressure, scrape, mildew, greasy dirt, acidic and alkali compounds.
Clean them with wet thin cloth.
Keep them dry and ventilated, Use often can keep it long-life.
Avoid to be under the blazing sun for quite a long time.
Goods Tag


text:
A global climatology of the dissolved oxygen anomaly (the excess over saturation) is created with monthly resolution in the upper 500 m of the ocean. The climatology is based on dissolved oxygen, temperature and salinity data archived at the National Oceanographic Data Center. Examination of this climatology reveals statistically significant annual cycles throughout the upper 500 m of the World Ocean, though seasonal variations are most coherent in the North Atlantic, where data density is greatest. Vertical trends in the phase and amplitude of the annual cycle are noted. The cycle in surface waters is characterized by a summer maximum and a winter minimum, consistent with warming and high rates of photosynthesis during the summer, and cooling and entrainment of oxygen-depleted water during the winter. In low and middle latitudes, the amplitude increases with depth and the maximum occurs later in the year, a trend consistent with the seasonal accumulation of oxygen associated with the shallow oxygen maximum. At a depth that varies between about 30 and 130 m, the phase of the annual cycle undergoes an abrupt shift. We call this depth the oxygen nodal depth. Below the nodal depth, the annual cycle is characterized by an early-spring maximum and a late-fall minimum, consistent with a cycle dominated by respiration during the spring and summer and replenishment of oxygen from the atmosphere by ventilation during the fall and winter. Below the nodal depth, the amplitude of the annual cycle generally decreases with depth, indicative of decreasing respiration and ventilation rates, or less seasonality in both processes. We postulate that the nodal depth in middle and high latitudes corresponds closely to the summertime compensation depth, where photosynthesis and net community respiration are equal. With this interpretation of the nodal depth and a simple model of the penetration of light in the water column, a compensation light intensity of 1 W m(-2) (4 mu E m(-2) s(-1)) is deduced, at the low end of independent estimates. Horizontal trends in the phase and amplitude of the annual cycle are also noted. We find that the nodal depth decreases toward the poles in both hemispheres and is generally greater in the Southern Hemisphere, patterns found to be consistent with light-based estimates of the compensation depth. The amplitude of the annual cycle in the oxygen anomaly increases monotonically with latitude, and higher latitudes lag lower latitudes. In the North Atlantic and North Pacific, the amplitude of the annual cycle tends to increase from east to west at all depths and latitudes, as expected considering that physical forcing has greater seasonal variability in the west. The tropics and the North Indian Ocean have features that distinguish them from other regions. Below about 75 m, these waters have pronounced annual cycles of the oxygen anomaly that areshown to be caused mainly by wind-driven adiabatic displacements of the thermocline. A semiannual cycle of the oxygen anomaly is found in the surface waters of the North Indian Ocean, consistent with the known semiannual cycle of surface heat flux in this region.
[1] We capture water column ventilation resulting from coastal upwelling in continuous records of O-2/N-2, CO2, and N2O at Trinidad, California. Our records reveal the gas exchange response time of the ocean to the upwelling and ensuing biological production. Satellite and buoy wind data allow extrapolation of our records to assess coastal upwelling air-sea fluxes of O-2 and N2O. We improve on previous regional estimates of N2O flux in coastal and continental shelf region of the western U. S. We characterize the source of N2O as being predominately from nitrification based on the O-2/N2O emissions ratio observed in our atmospheric records.
The seasonal cycle of atmospheric potential oxygen (APO similar to O-2 + 1.1 CO2) reflects three seasonally varying ocean processes: 1) thermal in- and outgassing, 2) mixed layer net community production (NCP) and 3) deep water ventilation. Previous studies have isolated the net biological seasonal signal (i.e., the sum of NCP and ventilation), after using air-sea heat flux data to estimate the thermal signal. In this study, we resolve all three components of the APO seasonal cycle using a methodology in which the ventilation signal is estimated based on atmospheric N2O data, the thermal signal is estimated based on heat flux or atmospheric Ar/N-2 data, and the production signal is inferred as a residual. The isolation of the NCP signal in APO allows for direct comparison to estimates of NCP based on satellite ocean color data, after translating the latter into an atmospheric signal using an atmospheric transport model. When applied to ocean color data using algorithms specially adapted to the Southern Ocean and APO data at three southern monitoring sites, these two independent methods converge on a similar phase and amplitude of the seasonal NCP signal in APO and yield an estimate of annual mean NCP south of 50 degrees S of 0.8-1.2 Pg C/yr, with corresponding annual mean NPP of similar to 3 Pg C/yr and a mean growing season f ratio of similar to 0.33. These results are supported by ocean biogeochemistry model simulations, in which air-sea O-2 and N2O fluxes are resolved into component thermal, ventilation and (for O-2) NCP contributions.
Atmospheric measurements of O(2)/N(2) and CO(2) at up to nine sites have been used to infer the interannual variations in oceanic O(2) exchange with an inverse method. The method distinguishes the regional contributions of three latitudinal bands, partly the individual contributions of the North Pacific and the North Atlantic also. The interannual variations of the inferred O(2) fluxes in the tropical band correlate significantly with the El Nino/Southern Oscillation. Tropical O(2) variations appear to be dominated by the ventilation of the O(2) minimum zone from variations in Pacific equatorial upwelling. The interannual variations of the northern and southern extratropical bands are of similar amplitude, though the attribution to mechanisms is less clear. The interannual variations estimated by the inverse method are larger than those estimated by the current generation of global ocean biogeochemistry models, especially in the North Atlantic, suggesting that the representation of biological processes plays a role. The comparison further suggests that O(2) variability is a more stringent test to validate models than CO(2) variability, because the processes driving O(2) variability combine in the same direction and amplify the underlying climatic signal.
[1] The Ar/N-2 ratio of air measured at 6 globally distributed sites shows annual cycles with amplitudes of 12 to 37 parts in 10(6). Summertime maxima reflect the atmospheric Ar enrichment driven by seasonal warming and degassing of the oceans. Paired models of air-sea heat fluxes and atmospheric tracer transport predict seasonal cycles in the Ar/N-2 ratio that agree with observations, within uncertainties.
Methods are described for measuring changes in atmospheric O-2 concentration with emphasis on gas handling procedures. Cryogenically dried air samples are collected in 5 L glass flasks at ambient pressure and analyzed against reference gases derived from high-pressure aluminum tanks. Fractionation effects are minimized by avoiding pressure and flow variations throughout the gas-handling system. The overall external reproducibility is approximately +/-3.3 per meg, with systematic errors associated with collecting samples and with storing them for 1 year reduced to the level of 3 per meg or smaller. The demonstrated short-term reproducibly of air delivered from high-presure tanks is +/-1.5 per meg, with the composition changing by at most 5 per meg by surface desorption reactions as the tank is depleted to below 3500 kPa. A 9-year survey of a suite of six reference gases showed no systematic long-term trends in relative O-2 concentrations to the level of 5 per meg. Results are presented from samples collected at Cape Grim (41 degrees S), Macquarie Island (54 degrees S) and the South Pole Station (90 degrees S). From measurements spanning 1991-1995 it is found that the O-2 concentrations at the South Pole are on average 3.6+/-1.2 per meg higher than at Cape Grim. This result runs contrary to the expectation that the air at high southern latitudes should be depleted in O-2 as a result of O-2 uptake from the Southern Ocean and may require the existence of unknown O-2 sources near Antarctica or unexpected atmospheric transport patterns.
Carbon dioxide is a radiatively active gas whose atmospheric concentration increase is likely to affect Earth's climate. CO2 is added to the atmosphere by biomass burning and the combustion of fossil fuels. Some added CO2 remains in the atmosphere. However, substantial amounts are taken up by the oceans and land biosphere, attenuating the atmospheric increase. Atmospheric O-2 measurements provide one constraint for partitioning uptake rates between the ocean and the land biosphere. Here we review studies of atmospheric O-2 concentration variations and discuss their implications for CO2 uptake by the ocean and the land biosphere. We compare estimates of anthropogenic carbon fluxes from O-2 studies with estimates from other approaches and examine the contribution of natural ocean carbon fluxes to atmospheric O-2 variations.
Measurements of changes in the atmospheric O-2/N-2 ratio have typically relied on compressed air derived from high-pressure tanks as the reference material against which atmospheric changes are assessed. The validity of this procedure is examined here in the context of the history of 18 O-2/N-2 reference tanks compared over a 12-yr time-frame. By considering differences in tank sizes, material types, and by performing additional tests, the long-term stability of the delivered gas is evaluated with respect to surface reactions, leakage, regulator effects, and thermal diffusion and gravimetric fractionation. Results are also reported for the stability of CO2 in these tanks. The results emphasize the importance of orienting tanks horizontally within a thermally insulated enclosure to reduce thermal and gravimetric fractionation of both O-2/N-2 and CO2 concentrations, and they emphasize the importance of avoiding elastomeric O-rings at the head-valve base. With the procedures documented here, the long-term drift in O-2/N-2 appears to be zero to within approximately +/- 0.4 per meg yr(-1), which projects to an uncertainty of +/- 0.16 Pg C yr(-1) (1 sigma) in O-2-based global carbon budgets.
The seasonal dynamics of the air-sea gas flux of oxygen (O-2) are controlled by multiple processes occurring simultaneously. Previous studies showed how to separate the thermal component from the total O-2 flux to quantify the residual oxygen flux due to biological processes. However, this biological signal includes the effect of both net euphotic zone production (NEZP) and subsurface water ventilation. To help understand and separate these two components, we use a large-scale ocean general circulation model (OGCM), globally configured, and coupled to a biogeochemical model. The combined model implements not only the oceanic cycle of O-2 but also the cycles of nitrous oxide (N2O), argon (Ar) and nitrogen (N-2). For this study, we apply a technique to distinguish the fluxes of O-2 driven separately by thermal forcing, NEZP, and address the role of ocean ventilation by carrying separate O-2 components in the model driven by solubility, NEZP and ventilation. Model results show that the ventilation component can be neglected in summer compared to the production and thermal components polewards but not equatorward of 30 degrees in each hemisphere. This also implies that neglecting the role of ventilation in the subtropical areas would lead to overestimation of the component of O-2 flux due to NEZP by 20-30%. Model results also show that the ventilation components of air-sea O-2 and N2O fluxes are strongly anti-correlated in a ratio that reflects the subsurface tracer/tracer relationships (similar to 0.1 mmol N2O/mol O-2) as derived from observations. The results support the use of simple scaling relationships linking together the thermally driven fluxes of Ar, N-2 and O-2. Furthermore, our study also shows that for latitudes polewards of 30 degrees of both hemispheres, the Garcia and Keeling (2001) climatology, when compared to our model results, has a phasing error with the fluxes being too early by similar to 2-3 weeks.
A methodology has been developed for making continuous, high-precision measurements of atmospheric oxygen concentrations by modifying a commercially available paramagnetic oxygen analyzer. Incorporating several design improvements, an effective precision of 0.2 ppm O-2 from repeated measurements over a 1-hour interval was achieved. This is sufficient to detect background changes in atmospheric O-2 to a level that constrains various aspects of the global carbon cycle. The analyzer was used to measure atmospheric O-2 in a semicontinuous fashion from air sampled from the end of Scripps Pier, La Jolla, California, and data from a 1-week period in August 1996 are shown. The data exhibit strongly anticorrelated changes in O-2 and CO2 caused by local or regional combustion of fossil fuels. During periods of steady background CO2 concentrations, however, we see additional variability in O-2 concentrations, clearly not due to local combustion and presumably due to oceanic sources or sinks of O-2. This variability suggests that in contrast to CO2, higher O-2 sampling rates, such as those provided by continuous measurement programs, may be necessary to define an atmospheric O-2 background and thus aid in validating and interpreting other O-2 data from flask sampling programs. Our results have also demonstrated that this paramagnetic analyzer and gas handling design is well suited for making continuous measurements of atmospheric O-2 and is suitable for placement at remote background air monitoring sites.
Observations of seasonal variations in the atmospheric O-2/N-2 ratio are reported at nine baseline sites in the northern and southern hemispheres. Concurrent CO2 measurements are used to correct for the effects of land biotic exchanges of O-2 on the O-2/N-2 cycles thus allowing the residual component of the cycles due to oceanic exchanges of O-2 and N-2 to be calculated. The residual oceanic cycles in the northern hemisphere are nearly diametrically out of phase with the cycles in the southern hemisphere. The maxima in both hemispheres occur in summer. In both hemispheres, the middle-latitude sea level stations show the cycles with largest amplitudes and earliest phasing. Somewhat smaller amplitudes are observed at the high-latitude stations, and much smaller amplitudes are observed at the tropical stations. A model for simulating the oceanic component of the atmospheric O-2/N-2 cycles is presented consisting of the TM2 atmospheric tracer transport model [Heimann, 1995] driven at the lower boundary by O-2 fluxes derived from observed O-2 saturation anomalies in surface waters and by N-2 fluxes derived from the net air-sea heat flux. The model is optimized to fit the observed atmospheric O-2/N-2 cycles by adjusting the air-sea gas-exchange velocity, which relates O-2 anomaly to O-2 flux. The optimum fit corresponds to spatially and temporally averaged exchange velocities of 24+/-6 cm/hr for the oceans north of 31 degrees N and 29+/-12 cm/hr for the oceans south of 31 degrees S. These velocities agree to within the uncertainties with the gas-exchange velocities expected from the Wanninkhof [1992] formulation of the air-sea gas-exchange velocity combined with European Centre for Medium-Range Weather Forecasts winds [Gibson et al., 1997] but are larger than the exchange velocities expected from the Liss and Merlivat [1986] relation using the same winds. The results imply that the gas-exchange velocity for O-2, like that of CO2, may be enhanced in the open ocean by processes that were not systematically accounted for in the experiments used to derive the Liss and Merlivat relation.
We have developed an instrument for making continuous, field-based, part-per-million (ppm) level measurements of atmospheric oxygen concentration, and have implemented it on research cruises in the equatorial Pacific and Southern Oceans. The instrument detects changes in oxygen by the absorption of vacuum ultraviolet (VUV) radiation as it passes through a flowing gas stream, and has a precision comparable to existing laboratory techniques. Here we describe the VUV instrument and present atmospheric O-2 and CO2 data collected from the NOAA ship Ka' imimoana in the equatorial Pacific during April and May of 1998, and from the NSF ship Lawrence M. Gould in the Southern Ocean during October 1998. These data represent the first field-based measurements of atmospheric O-2, and significant additions to the O-2 datasets in these regions. Our boreal-springtime equatorial measurements reveal significant short-term variations in atmospheric O-2, resulting from variations in atmospheric mixing relative to the strong interhemispheric gradient. Our austral-springtime Southern Ocean observations confirm the low O-2 concentrations seen in flask samples from this region, allow the separate identification of oceanic and industrial influences on CO2, and provide evidence of a Southern Ocean source for CO2 at this time of year. These shipboard VUV observations do not provide any evidence to support coupled ocean-atmosphere model predictions of a large decreasing atmospheric O-2 gradient between equatorial and high-southern latitudes.
The seasonal cycle of atmospheric N(2)O is derived from a 10-yr observational record at Cape Grim, Tasmania (41 degrees S, 145 degrees E). After correcting for thermal and stratospheric influences, the observed atmospheric seasonal cycle is consistent with the seasonal outgassing of microbially produced N(2)O from the Southern Ocean, as predicted by an ocean biogeochemistry model coupled to an atmospheric transport model (ATM). The model-observation comparison suggests a Southern Ocean N(2)O source of similar to 0.9 Tg N yr(-1) and is the first study to reproduce observed atmospheric seasonal cycles in N(2)O using specified surface sources in forward ATM runs. However, these results are sensitive to the thermal and stratospheric corrections applied to the atmospheric N(2)O data. The correlation in subsurface waters between apparent oxygen utilization (AOU) and N(2)O production (approximated as the concentration in excess of atmospheric equilibrium Delta N(2)O) is exploited to infer the atmospheric seasonal cycle in O(2)/N(2) due to ventilation of O(2)-depleted subsurface waters. Subtracting this cycle from the observed, thermally corrected seasonal cycle in atmospheric O(2)/N(2) allows the residual O(2)/N(2) signal from surface net community production to be inferred. Because N(2)O is only produced in subsurface ocean waters, where it is correlated to O(2) consumption, atmospheric N(2)O observations provide a methodology for distinguishing the surface production and subsurface ventilation signals in atmospheric O(2)/N(2), which have previously been inseparable.
We estimate transport of heat, CO2 and O-2 by the Atlantic's thermohaline circulation using an approach based on differences in the chemical and physical characteristics of North Atlantic Deep Water (NADW), Antarctic Intermediate Water (AAIW), and the northward return flow across the equator. The characteristics of the return-flow waters are constrained by imposing conservation of phosphate in the North Atlantic as a whole. Based on a total equatorial return flow of 13 x 10(6) m(3) s(-1), we find that the Atlantic north of the equator is a source of 7.7 +/- 1.4 x 10(14) W to the atmosphere, a sink of 0.51 +/- 0.21 x 10(14) mol of O-2, and preindustrially was a sink of 0.33 +/- 0.15 x 10(14) mol of CO2. Uptake of O-2 and CO2 by the North Atlantic is driven mainly by thermal, as opposed to biological processes.
Global Change, Global Environmental Monitoring
Atmospheric Aerosols and Chemistry, Climate Sciences, Past Climate Change
Mailing Address: GRDScripps Institution of OceanographyUC San Diego9500 Gilman Drive #0244La Jolla CA, 92093-0244
Location: 312 Vaughan HallTel: 858-534-7582Fax: 858-534-2997
rkeeling at ucsd.edu


text: September 24, 2018, Detroit, MI: ASTI President, and founder, Tom Wackerman has been selected as one of D Business Magazine's Top 500 most powerful business leaders in Metro Detroit, the only environmental consultant to be honored. With 40 years in the business, Mr. Wackerman established, and has guided ASTI since it's inception (1985), and he also doubles as the firm's Director of Incentives. With offices in Detroit, Grand Rapids and Brighton (HQ), ASTI specializes in mitigating risk and expense associated with environmental testing/cleanup, wetlands, and brownfield redevelopment and we have now completed more than 12,000 projects.


text:
- Location: IL
- Join Date: 12/4/2014
- Posts: 1,854
- Minecraft: jredfox
- Member Details
The idea isn't new and has failed as many times as people tried because, their mindsets were wrong. The idea is raising the chunk limits. No I don't mean just increasing the height limit to integer. That was attempted and done by base class edits however it had memory leaks/ram issues. I am not talking about the failure of the tall world mod either but, he was in the right direction. His failure was breaking up the vanilla chunks. My idea is to keep the vanilla chunks the way they are but, have vertical chunks. My idea can best simply be explained through this image.
I know some coding but, I am unsure If I am able to make this mod. It would have it's own rendering system own cords everything. Contact me first if you are going to start coding this. I just want to know the easiest route on how to code this. I am guessing I just practically copy the chunks class rendering classes, and cords classes.
Vchunks are verticle chunks.
How minecraft would implement this:
- shrink basic chunks to y of only 256 currently is integer and or long for a chunk yet block height is 256 vanilla stupidity.
- render distance of chunks being 1 meaning it will load up one chunk and down one chunk and the dimensions being the same as current render of xz render
Void/Sky/sun and moon properties of a chunk will be disabled by default but, can be enabled by vchunk biome, mods or xworld.
New tp command
/tp player (grabs players xworld, vanilla or xchunk, vchunk and dimension id)
/tp xyz dimensionid vchunk xworld, xchunk(xchunk cords)
/tpmove(moves player without using cords)
/tpdimension player (dimid)
VChunks Properties
.isVChunkBiome (boolean if false then it is the current biome below with only spawning air blocks. It will only spawn the biome if .isvchunkbiome is true)
.isChunkVoidDamage(by default void damage will be disabled but, will be able to be enabled through via config or through vchunks will have void armor that would disable any void damage almost like an astronaut suit.)
.isvchunkteleportation (upon entity entering the chunk it will teleport to dimension, vanilla or x chunk, xworld (default 0) dimension)
X Worlds
.isxworldround(if you get to the end of the xworld it will teleport you back to the begining worlds withing worlds anybody)
xchunks(goes for all the other worlds withing the same world
.isxchunkround(prision camp anybody?)
.isxchunkrespawnable(goes well with being in a prision sets player spawn to xchunk xworld, dimension)
Config options for late dev
is world truly infinite = false
Vchunks = true
Xworld = True
Is XWorld0 Round = false
Is VChunks Dim0 Only = false
Is -Vchunks Dim0 Only = false
Is XWorld Dim0 Only = false
Predicted Difficulties
water not flowing through vchunks, water not flowing from vchunk to vanilla chunk, entities not going through vchunks, problems with world generation need manual import auto configuration from forge, biome difficulties, biome color, mod conflicts for no apparent reason even though all of it is vanilla mechanics except for the cords. Player will crash after removing mod from being above the cords limit . This will require a forge or something to auto tp players to the integer level or whatever cords are stored in.
world round properties will teleport you to the opposite cords at the other end of the world a block away before the world border.
Being truly Infinite:
don't think anybody needs more then 2 billion v chunks and more then 2billion worlds on xz acess
Save Data (Removing Mod has no worries)
The Vchunks and xworlds will save in their own folder with all of their files and depending on the config will generate ones for every single dimension into Glorified Chunks folder. Removing the mod will just cause all of the chunks to not load and neither will the blocks. The blocks will be still stored with that mod in those folders. So re-adding the mod will add them back if forge doesn't delete the folders once the mod is removed. Programs like mcedit will freak out and crash.


text:
2018 Toyota Corolla
2018 Toyota Corolla
132 - 140
126 - 128
27 - 30
MPG City
35 - 40
MPG Highway
132 - 140
126 - 128
27 - 30
MPG City
35 - 40
MPG Highway
Corolla Trim Levels
Compare Up To 4 Trims
Seating Capacity
Fuel Tank Capacity
Engine Size
132 - 140
126 - 128
MPG City
27 - 30
MPG Highway
35 - 40
Standard Equipment For All Trims
Exterior Standard Equipment
Color-keyed outside door handles
In-glass AM/FM antenna
Interior Standard Equipment
Integrated backup camera with projected path
Power door locks with automatic locking feature
Power windows with driver-side one-touch up/down
Rear window defogger with timer
Day/night rearview mirror
Overhead console with maplights
Center console with storage compartment
Passenger-side glove compartment
Front- and rear-door storage pockets with sculpted bottle holders
One 12V auxiliary power outlet
USB 2.0 port
Two front and two rear cup holders
Digital clock
Safety & Security Standard Features
Toyota Safety Sense P (TSS-P) - Pre-Collision System with Pedestrian Detection (PCS w/PD), Lane Departure Alert with Steering Assist (LDA w/SA), Auto High Beams (AHB), Dynamic Radar Cruise Control (DRCC)
Star Safety System - Includes Enhanced Vehicle Stability Control (VSC), Traction Control (TRAC), Anti-lock Brake System (ABS), Electronic Brake-force Distribution (EBD), Brake Assist (BA) and Smart Stop Technology (SST)
Eight airbags - Includes driver and front passenger Advanced Airbag System, driver and front passenger seat-mounted side airbags, driver knee airbag, passenger seat-cushion airbag, and front and rear side curtain airbags
Driver and front passenger Whiplash-Injury-Lessening (WIL) seats
3-point seatbelts for all seating positions - Driver-side Emergency Locking Retractor (ELR) and Automatic/Emergency Locking Retractor (ALR/ELR) on all passenger belts
Adjustable front shoulder anchors, driver and front passenger seatbelt pretensioners with force limiters
LATCH (Lower Anchors and Tethers for CHildren) - Includes lower anchors on outboard rear seats and tether anchors on all rear seats
Child-protector rear door locks
Energy-absorbing collapsible steering column
Front and rear energy-absorbing crumple zones with side-impact door beams
Head-impact protection structure
High-tensile-strength steel body panels
Tire Pressure Monitor System (TPMS)
Engine immobilizer
Hill Start Assist Control (HAC)
Mechanical & Performance Standard Features
Front-Wheel Drive (FWD)
Unitized body
Independent MacPherson strut front suspension with stabilizer bar
Torsion beam rear suspension with rear stabilizer bar
Electric Power Steering (EPS) - Power-assisted rack-and-pinion
Warranty Standard Features
Comprehensive Limited Warranty - 3 years/36,000 miles
Powertrain Limited Warranty - 5 years/60,000 miles
Corrosion Perforation Limited Warranty - 5 years/Unlimited miles
Toyota Care - Complimentary maintenance plan with the purchase or lease of every new Toyota. For 2 years or 25,000 miles, whichever comes first, every new Toyota will be covered for all normal factory scheduled service, as well as 24/7 roadside assistance
Excludes tax, tag, registration and title and includes $399 closing fee. In order to qualify for this advertised price you must mention this advertisement prior to purchase. Stokes Toyota Beaufort is not responsible for any price discrepancies, statements of condition, or incorrect equipment listed on any vehicle. Unless the vehicle has a remaining factory warranty, all sales are "AS-IS" with no warranty on used vehicles. Pricing does not include any Dealer Added equipment. Any and all differences must be addressed prior to the sale of this vehicle.


text:
- Soccer Training
- Soccer Injuries
- Inside Soccer
- College Recruiting
- Library
- About Us
- Testimonials
- Contact
Use The Clam Exercise To Strengthen Your Glutes And Prevent Knee Injuries On The Soccer Field.
Submitted by Ben Torres on June 14, 2011
With soccer players, knee injuries can often be associated with a lack of strength in your gluteus medius muscle. Weakness in this muscle usually leads to unstable hip rotation, which inadvertantly leads to an unstable knee. This can cause injury and hinder your performance on the soccer field. Doing the clam exercise can help strengthen the gluteus medius muscle and prevent knee injuries from occurring on the soccer field.
Here's how to do it: You will need a comfortable surface to lie on and a mini-band with some resistance.
- Lying on your side, make sure your feet, knees, hips, and shoulders are stacked on top one another.
- With the band around your legs, approximately 2-3 inches below your knees, bring your knees towards your chest forming a 40 to 60 degree angle at your hips and knees.
- To execute the exercise, slowly rotate the top hip outward, causing your top knee to separate from the bottom knee, and rotate back down.
Key pointers while performing this exercise:
Your goal here is to simply isolate and activate the glute medius muscle. So your focus should only be on small movements. Excessive movements of the hip will involve your torso and you won't get the desired results. You should focus on higher repetitions. The gluteus medius muscle plays a supporting role in a variety of movements, so it's vital that it can "carry its proper burden" and sustain those movements for a long period of time. Performing 2-3 sets of 15-20 repetitions should suffice.


text:
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text:
Day 1
Rendezvous at the Fort Nelson airport upon arrival of the Central Mountain Air flight. Those who drove to Fort Nelson can leave their vehicles at the airport for the duration of the trip. Following introductions, we will load the van and begin our drive north. We will make a brief stop in Fort Nelson on our way to the Alaska Highway where we will shop for snacks for the drive. Our route to the headwaters of the Nahanni River takes us west through the northeast corner of the Rocky Mountains. The landscape has a rugged beauty all of its own. We will make sightseeing stops at Stone Mountain and Muncho Lake Provincial Parks. Guests in the past have lost count of the number of wildlife sightings on the first day alone. From the van we are sure to see stone sheep and mountain caribou along the way. We will camp for the night at Liard Hot Springs where we will enjoy a relaxing soak.
Day 2
Back on the road we'll drive to Watson Lake and walk through the historic Sign Post Forest. At Watson Lake, Yukon we drive north on the Robert Campbell Highway and then onto the Nahanni Range Road for our detour back into the Northwest Territories and the road to our flight base on Flat Lake. This remote road boasts incredible scenery and will give you a peak of the mountain ranges you will fly over on your way to Divide Lake. Weather permitting we will make the short flight to Divide Lake upon arriving at Flat Lake. We will enjoy the peace and beauty of this alpine lake as we toast our arrival into the Naat'sich'oh National Park Reserve and its stunning wilderness. The lake also provides an excellent venue to practice canoeing skills before setting out the following morning.
Day 3
After an introduction to preparing canoes for travel and river safety we will paddle from Divide Lake onto a crystal clear creek that will take us to Swallow Falls, named for the swallows that nest in the cliffs around the falls. A short portage through dwarf birch takes us around the falls to the start of a small canyon. Depending on water levels we will paddle or line this tight canyon and revel in the clear water pouring over boulders. We will camp at the exit of the canyon and watch the sun set over the canyon walls.
Day 4
Shortly after setting out we will arrive at the Broken Skull River and get our first taste of it's famous, friendly whitewater. We will weave our way through boulder fields enjoying class 1-2+ waves. As necessary, we will scout wave trains to identify the best line at our water level. The whitewater will last for most of the day but will lessen off in time to allow our gaze to shift to the incredible views on all sides. We will make camp in the heart of the mountains and enjoy delicious three course meals prepared over the fire. There is no shortage of daylight so you can linger around the fire watching the evening light play on the mountain ranges.
Day 5-6
The thrills continue on the river with continual stretches of beautiful, friendly whitewater. Standing waves around every corner, perfectly spaced boulders to weave through and the occasional opportunity to 'thread the needle'. Even the most restrained paddlers won't be able to wipe the smile off their face. There are ample opportunities for hiking and exploration off the river. Your guides will make opportunities available based on the group interest, water levels and weather. A 'must do' is the Broken Skull hotsprings, a 2.5km hike up a small tributary of the Broken Skull river. The water temperatures will not disappoint and after a few days of paddling, the soak will be a welcome chance to revive tired muscles. For an intrepid few, a dunk in the nearby creek can be interspersed with soaking in the piping hot pools.
Day 7-9
As the Broken Skull river grows it maintains its crystal clear water. At this point in the trip some groups have added grizzly bears, porcupines, moose, caribou and wolves to their list of wildlife sightings. The Broken Skull river is an active wildlife corridor where you will be sure to see tracks of many of these mammals. We will paddle through the 'Mini Gate', named for the Gate on the South Nahanni River. This smaller but equally photo worthy geological feature provides an opportunity for staging fun photo shoots. We will enjoy drifting through the still pools of this special landmark before paddling on to more whitewater. As we paddle from the Naats'ich'oh Park into the Nahanni National Park Reserve we will get our first glimpses of the Ragged Range which includes the highest peaks in the Northwest territories. We will camp on a gravel bar with small, delicate rocks that will ensure we sleep soundly under the midnight sun.
Day 10-11
Dwarf fireweed dots the river's edge with its magenta blossoms as we paddle towards the confluence with the South Nahanni river. The Vampire Peaks loom large as the clear water of the Broken Skull swirls into the Nahanni's grey green waters. Paddle 'high fives' will be passed amongst the group as you congratulate yourself on having paddled a river only a handful of groups experience each year. Now you can sit back and enjoy the quiet waters of the South Nahanni. Put your feet up and gaze into the Cirque of the Unclimbables, the renowned hiking and rock climbing area a two day trek from the South Nahanni river. The armchair glacier of Mount Edna is your first landmark for the impressive peaks of the Cirque. You may get to wave hello to a group departing from Britnell Creek to hike into the Cirque of the Unclimbables, a gentle reminder that the outside world exists after likely not having seen another group since arriving on the river.
Day 12-14
We will enjoy an interpretive hike, guided by Nahanni National Park personnel (subject to availability of Park staff) to view the Rabbitkettle Hot Spring and Tufa Mounds. We then begin paddling down river towards Virginia Falls.
This section of the river is dominated by U -shaped valleys which were scoured out by advancing cordilleran glaciers thousands of years ago. We paddle 120 km (72 mi.) on the smooth flowing water to Virginia Falls. Along the way we will camp beside beautiful creeks such as Hell Roaring Creek and Flood creek and will feast our eyes on Rabbitkettle Mountain, a myriad of alpine ridges and the Sunblood range.
Day 15-16
Everyone will appreciate a rest day at Virginia Falls. At over 90 m (300 ft.) Virginia Falls is twice the height of Niagara, and is the spectacular centrepiece of Nahanni National Park. The options for these days are many - you can lounge in the group camping area, explore the Falls with your camera, or strike off on an invigorating hike to the grassy summit of Sunblood Mountain. Virginia Falls is a fascinating place to discover.
Day 17
Following our layover day, we complete the 2 km portage around the Falls and reload our canoes. For the following week we will immerse ourselves in the spectacular scenery of the lower Nahanni River. The lower Nahanni is canyon country and is often described as the Grand Canyon of the North. Beginning with Painted Canyon, so named because of its brightly coloured walls, you will experience the thrill and excitement of this whitewater section. On this night we will camp in the vicinity of the confluence with the Flat River.
Day 18
Downstream we enter Third Canyon with its imposing 1200 m walls formed as the Nahanni has carved its way through the Funeral Range. We will camp in the shadow of the Gate; where the river has sliced a narrow chasm on the apex of a hairpin meander. An optional hike to the top of the Gate presents magnificent views of the river valley with imposing Pulpit Rock 460 m below.
Day 19
Today finds us completing the 35 km Third Canyon and continuing on through Second Canyon, (15 km) where the Nahanni has carved its route through the Headless Range and into Deadmen Valley. This valley is known for its legend and mystery made famous by the mysterious deaths of the McLeod Brothers. Here the vista is noticeably different, as the valley opens up, with distant views of the Tlogotsho Plateau. Deadmen Valley offers an abundance of exploratory options. The massive Prairie Creek alluvial fan provides excellent camping, hiking and wildlife observations.
Day 20
We start the morning with a run through the exhilarating waves of George's Riffle and on into First Canyon. The imposing walls of First Canyon reach heights of over 1400 m. Groups often drift the length of this magnificent 26 km canyon, immersed in its splendour. The canyon walls are dotted with hundreds of caves. Close to its exit we will camp for the night at Lafferty's Canyon, with good hiking opportunities.
Day 21
Following breakfast, it's down to Kraus' Hot Spring for a soothing dip in its 32 C plus waters. From here we bid farewell to the canyons and make our way to the Nahanni's Splits, a 70 km run through a maze of islands.
On our final morning on the river we will continue on to the Native village of Nahanni Butte. (Pop. approx. 120). This remote community is located on the banks of the Nahanni just above its confluence with the Liard river. A stroll into town provides insight into a culture far removed from most of North America. Following lunch we will board the Nahanni Butte River taxi for the 15 km ride to the Nahanni Butte Road Landing on the Liard River. The awaiting NWA shuttle van will take us by road to Bannocklands, a beautiful Inn on the banks of the Liard river where we will enjoy a celebratory final evening. Any baggage you left behind will be waiting for you. Accommodation and dinner are included. After a leisurely morning, you will be transported to the Fort Simpson airport to begin your travels home.
After a leisurely morning, you will be transported to the Fort Simpson airport to begin your travels home.


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ERNEST Floral pocket square
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Collection: Florals
Fabric: Cotton
Style: 12" X 12"
Floral cotton pocket squares are 12 by 12 inches square, with a double folded hem.
Our menswear is handmade in England in limited runs, using the finest range of hand picked fabrics. Each pocket square is packaged in a vintage style gift box, and comes with a care card.
Matching set available.
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A charming small floral print, in muted tones for a vintage feel.


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article, I identify a lot with. Yesterday I was with a group of friends I knew back in school, and they were sharing a lot of memories of which I only remember 20% of. I felt bad. At first I used to think it is because I have a bad memory, but truth is it was simply because I did not concentrate on the moment and my mind used to wander a lot dreaming of happier moments. And that is what I did most of my life. But not recently, since I learned that lesson, and the cure for my lousy memory was simply to live in the moment and focus more. Now of course, my mind still wanders, but we're learning, grasshoppers :)
This article is a very cool and interesting read on how letting our mind wander is a major cause of unhappiness. Simply, try to live and appreciate the moment. As my friend and school colleague told me yesterday: "Every moment that is gone, will never be replaced"
Since it's the last day of the year, I just want to wish my readers (if you're still reading that is, since I've been really ignoring this blog) a good year, I know it won't be all good, let's be realistic here, but I hope you change your job if you're unhappy now, I hope you find love, if you're feeling lonely, I hope you get a promotion if you're doing well at your job now, I hope you spend quality time with your loved ones and I hope you stay true to yourself, no matter what!
Happy 2011. Thank you for being there for me.
p.s. Happiness, is only a state of mind.
Friday, December 31, 2010
On the wandering mind and happiness
Posted by Liliane at 2:26 PM
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Colitis Channel
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Is Delzicol the Same as Asacol?
Healthcare providers prescribe Delzicol® (mesalamine) to treat ulcerative colitis in adults. This medication contains the same active ingredient as another medication called Asacol® 400 mg tablets, which were also used to treat ulcerative colitis but are no longer available. But is Delzicol the same as Asacol?
There are many similarities -- as well as differences -- between these two drugs. Both drugs are manufactured by Warner Chilcott (US), LLC, and they are both used to treat ulcerative colitis. They both contain 400 mg of mesalamine in a delayed-release form. The side effects, effectiveness, and drug interactions are also the same for both drugs.
However, there are also many differences. Delzicol comes as a capsule, while Asacol came in tablet form. Also, there are different inactive ingredients in these two medications. Asacol contained an inactive ingredient called dibutyl phthalate (DBP), a substance which the FDA recommends removing from human drug products. Delzicol does not include DBP.
(Click Delzicol vs. Asacol for more detailed information on the differences and similarities between Asacol and Delzicol. This resource also examines why there was a switch from the tablet form of this drug to a capsule.)
Written by/reviewed by: Kristi Monson, PharmD
Last reviewed by: Kristi Monson, PharmD


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Suffering From A Stockbridge Mold Damage Repair Emergency?
Mold is normally highly dangerous and should be given to the service providers.
However, in order to aid teach you, we have covered the following know-how below.
Serious Molds:
Dangerous molds are truly actually threatening parasite fungi proliferated thru air.
In truth, all varieties of molds could be hurtful molds. They flourish by using oxygen and water and occur naturally in nature.
Molds gather its nutrients directly from dead plants and rotten foods. They have plenty varieties being toxic and non-poisonous.
Black molds are one of the notorious dangerous molds. The toxic elements of black molds make numerous bodily ailments such as nasal and sinus congestion, burning eyes, watery and blurry vision, skin irritation , persistent lethargy and constant headaches. Often dangerous molds have the ability to trouble complete immune system of the human body leading to high temperature.
In this way, it is always well-advised to get rid of molds at their very first appearance itself with the service of service providers.
Call Water Damage Pros - Stockbridge
(770) 999-0900
Mold In Your Garage:
Garage area mold begins to grow on the surfaces in garage. Garage mold may even proliferate further inside garage walls. Within the walls, garage mold may increase untroubled, making the air unclean and threatening overall health. There are various approaches for prevention.
Number one, separate your garage, particularly if it attached to your residence. Do not move moldy things to your car or truck or residence. When the roofing system has leaks, check and mend, to ensure additional humidity does not enter into your garage.
Caulk the doors and windows and include weather stripping. Park your car away from the garage, especially on stormy days. Check your garage every day for reoccuring garage mold. Allow air flow in the garage. Let adequate light come in by keeping doors open.
Water Damage Stockbridge Restoration Pros On Duty.
Hidden Mold:
Hidden mold traditionally grows in dank areas and go unrecognized. The normal places for hidden mold are the bottom of pads and carpet or rugs, ceiling tiles and its top side, roofing materials, A/C ducts, dry wall , dryers, wallpaper back and freezer or fridge.
Even a slightest water leak, in which we do not know and fail to fix, is enough for hidden mold to thrive. For protecting against hidden mold, a best way indeed is staying conscious about its presence. Mold may continue to be hidden in the air and could affect your health and wellness adversely. This is why, you want to identify hidden mold, especially on smelling any unexplained odour in your property.
1. Containing the mold from infecting additional unpolluted spaces.
2. Exterminating the mold fully.
3. Removing the dead mold very carefully.
4. Guarding each of the possessions tainted from mold.
The leading procedure to contain the mold is to dispose of the origin of the mold situation. If the mold issue arises in your HVAC unit, wiping out mold coming from there will certainly accomplish most of your task.
Put up airtight walls to contain the mold in the contaminated region prior to you begin wiping out mold.
The 2nd step in removing mold is to destroy it.
Most people usually think that they can eradicate the mold successfully using bleach. However, bleach is not an effective killing agent. The most efficient material to eliminate mold is simply boric acid.
There is at the same time cutting-edge technology that skillful Mold contractors make use of to eliminate sizable levels of mold.
Eliminate the dead mold utilizing a planer, sander or a grinder having a wire brush attached to it.
While eradicating mold that is dead, you should really use safety protections. Utilizing respirators and ideally full body coveralls in conjunction with gloves, that will manage to keep all mold spores from contacting your skin.
Last but not least, Isolate the area from the remainder of the home with a plastic barricade, protect future from mold by sealing furniture pieces using a fungicidal coating and covering. One could in addition use a clear coat of polyurethane acrylic to finish the elimination procedure. This will certainly protect the area.
A dehumidifier is a mechanism put into action to soak up the moist air and to prevent mold attacks. A dehumidifier also helps in drying up any particular area (floor) or corner of a room. In countries, where the weather is rainy and damp throughout the year, dehumidifiers work as condensers too.
A dehumidifier can work as a trouble free system that you can operate easily. It is portable in size and the drainage system has to be systematic with the drainage system of the house for proper working. A dehumidifier saves any kind of extra time for cleaning the toxic elements and also helps in keeping the house clean and free from molds.
Do Away With Mold:
It is urgent to eliminate mold as soon as you notice it. There are a variety of ways to eliminate mold. Mold can grow anywhere . It needs to have a bit of water and air to stay alive. There are times it spreads without the awareness of the property owner.
You can certainly get going with repairing any leak that is causing dampish atmosphere. Application of exhaust fans can really help in disposing of the moist atmosphere from kitchen or bath room to eliminate mold spread.
Boost the circulation of air in the places, precisely where there is more level of moisture to eradicate likely mold spread in that room. Lastly, a dehumidifier is the best machine to remove mold in its very early expansion stages.
In later stages of visible mold, that may be behind walls or in air ducts, professional Mold mitigators really should be spoken to. Discover Mold. You are certain to discover mold in your home if any person reports that some allergic reaction symptoms are gone immediately after they travel out of your house.
An additional sign that you are going to discover mold is a musty smell. Almost all pros too rely on their nose to seek out mold. An additional effortless approach to discover mold is to examine the source of wetness or the origin of water issue.
Mold flourishes in moisture content. Should you reckon the mold within the wall structure, you could make a cavity inside the wall structure and examine the dust particles to find mold. You may find mold without a doubt by using the home-test kits obtainable in the home market.
Fungicide is an medium, which defends against or destroys the growth of fungi and you may use fungicide in your grass and when it comes to your greeneries. It is of many types namely the contact fungicide, penetrant fungicide and systemic fungicide. The contact type is for eradicating pores, that are subjected to the product.
It lasts for a more lengthy period on the plant's surface . Penetrant one is utilized as a precautionary maintenance choice and not as a treatment choice. You may use systemic fungicide to a certain location, that then goes through a plant's circulation system for shielding it. Utilize fungicide for controlling plant contaminations. People may apply it using a garden sprayer.
Flood & Mold:
Flood and mold generally go hand in hand. If your home was a sufferer of flooding, mold will be sure to increase in your residency unless you dry it effectively.
Due to a flood, water flows into the walls and surfaces of the residency. The walls absorb this water and it delivers moisture for the mold. So, flood and mold could pose a twofold concern for the property owner.
A flood may in addition ruin some structures in your home. These kinds of crevices furnish the perfect moist spots for mold development. Flood and mold are a dangerous combination.
Defending against mold growth shortly after a flood is hard except if a person takes prompt action.
Fire & Mold:
While fire and mold do not have a straight link, the wreckage from a fire can generate appropriate conditions for the mold to flourish. Damage to the house's construction may perhaps also expand this not likely connection between fire and mold. Water pipes and plumbing in your house may go through damage in a fire and mold will have the opportunity to grow.
As water works to control fires, the wood structures of a structure may possibly retain the water. When one does not dry the residences thoroughly, of course, there is a likelihood of mold growth.
Fire and mold, whereas not linked, are most definitely a harmful merger. Given that fire and mold have an indirect causal connection, it is recommended to take proper precautions immediately after a fire.
Gutter Mold:
Health Effects of Mold:
Genuine health effects of mold are many caused as a result of mold multiplying inside the house. Health effects of mold may come with the indicators for example, sniffily nose, tickle in throat, allergic reactions, eye irritation, sinus and nasal congestion , weakness and migraine. Allergic responses consist of fever.
Other health results of mold, particularly arising from noxious mold are throat irritation, memory issues, skin hives, food intolerances , bloodied or watery eyes, respiratory system problems for instance asthma, mood swings and irritable bowel syndrome. These health impacts of mold may trigger severe complications in your body.
Additional wellness consequences of mold might possibly be athlete's foot and yeast contaminations.
Here below are additional postal codes of neighborhoods in which our crew gives free estimates in:
30252, 30370, 30213, 30340, 30045, 31139, 30356, 30288, 30313, 30012, 30294, 30348, 30071, 30091, 30361, 30036, 30307, 30035, 30032, 30156, 30054, 30008, 31192, 30133, 30068, 30309, 30327, 31107, 30260, 30039, 30368, 30371, 30080, 30088, 30269, 30287, 30067, 30374, 30072, 30284, 30092, 30328, 30250, 30354, 30074, 30270, 30385, 30303, 30022, 30398, 30122, 30062, 30090, 30337, 30253, 30272, 30099, 30281, 30384, 31150, 30265, 31126, 30095, 30344, 30321, 30358, 30064, 30047, 30364, 30016, 30096, 30077, 30160, 30048, 31145, 30146, 30033, 30238, 30078, 30359, 31136, 30029, 30144, 30316, 30339, 30350, 30377, 31141, 30314, 30065, 30168, 30355, 30111, 30094, 30081, 30098, 30320, 30346, 31131, 30312, 30268, 30394, 30214, 30005, 30366, 30301, 30329, 30388, 30007, 30141, 30038, 30308, 30106, 30101, 30017, 30310, 30315, 30318, 30061, 30102, 30274, 30084, 30026, 30277, 30291, 31156, 30085, 30331, 30042, 30343, 30319, 30069, 30127, 30003, 30326, 30302, 30009, 30037, 30296, 30126, 30006, 30349, 30097, 30322, 30357, 30336, 30060, 30063, 30030, 30049, 30325, 30362, 30228, 30134, 31193, 30076, 30297, 30324, 30273, 30034, 30023, 30396, 30046, 30058, 30086, 30360, 30345, 30392, 30083, 30021, 30087, 30237, 30044, 30002, 30306, 31196, 30188, 30082, 30236, 30304, 30341, 30290, 30369, 30332, 30353, 30157, 39901, 30004, 30075, 30298, 30375, 30342, 30380, 30013, 30031, 31146, 30135, 31106, 30043, 30024, 30169, 30333, 30311, 30152, 30189, 30215, 31195, 30093, 30317, 30066, 30334, 30305, 31119, 30338, 30187, 30363, 30079, 30052, 30378, 30010
Posted below are neighboring towns that our team responds to:
Hiram, Ellenwood, Avondale Estates, Forest Park, Stone Mountain, Tyrone, Lawrenceville, Mableton, Stockbridge, Clarkston, Canton, Duluth, Lebanon, Newnan, Loganville, Conley, Mcdonough, Peachtree City, Lithia Springs, Riverdale, Oxford, Jonesboro, Lovejoy, Decatur, Alpharetta, Clarkdale, Snellville, Red Oak, Fairburn, Morrow, Woodstock, Hampton, Sunny Side, Austell, Atlanta, Lilburn, Winston, Norcross, Redan, Suwanee, Roswell, Tucker, Conyers, Sharpsburg, Pine Lake, Smyrna, Acworth, Lithonia, Rex, Grayson, Scottdale, Kennesaw, Dallas, Palmetto, Union City, Marietta, Covington, Powder Springs, Fayetteville, Douglasville, North Metro
Call Water Damage Pros - Stockbridge
(770) 999-0900
Water Damage Stockbridge Dry-Out Pros At Work.
Floor Covering Mold.
Floor mold refers to the mold in the floor. Floor mold usually continues unknown because of ceramic tiles and rugs which cover it. Never ever brush off even the smallest mold traces.
Mold progression may be as minor as in the grout area, but indicatory of a broader issue beneath the flooring. In addition, wooden floor are far more vulnerable to floor mold. Floor mold might increase very swiftly if one does not recognize its existence in time.
The spaces in the flooring are very comfortable for the mold's growth. Therefore, the minute one catches sight of any signs of floor mold you need to take measures remove it.
Flooding is among the leading contributors to mold progression. There are different reasons why could occur. Flooding may well be actually the final result of a natural problems including a hurricane , flood or substantial rain showers.
The only way to prevent the painful outcomes of flooding is to enhance your house structure. You can elevate the residence lay out the floorings at a slant so as to let the water out efficiently.
Yet another reason may be negligence. In some cases, we overlook to shut off the taps, thus leading to flooding coming from in the property.
In addition, a water pipe may perhaps break because of improper routine maintenance or construction , creating water damage.
Hence, nature and individual negligence are possibly the primary sources of flooding in properties.