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Pastor for Worship, North
Email | 612-455-0800 x813
Born into a Christian home in suburban Minneapolis in 1961, Dan was born again as a child of 4 or 5 at his mother's knee. When he was 10, Dan's parents sensed God's call to missionary service in southern Africa. "As a child, I saw in my parents a passionate commitment to Christ which resulted in radical middle-aged steps of obedience to go and spread the gospel." During high school, he first became involved in leading worship. After finishing high school in Zimbabwe, Dan returned to the U.S. to attend Bethel College in St. Paul.
Graduating from Bethel in January 1983, with a degree in English Literature, Dan married Liz in February of the same year. They have four children, Anika, Erik, Mariana, and Anders. They currently live in Mounds View. Dan was employed by Northwest Airlines as a flight attendant for 20 years.
October 2002, Dan Holst joined Bethlehem's staff, where he continues to serve and shepherd the body of believers at the North Campus. Dan began serving us as a worship pastor, added Lead (Campus) Pastor, North Campus from 2011 through June of 2017, and is again our Pastor for Worship, North Campus, after dividing his growing duties into two full time roles.
Dan serves with an unbridled passion to know God in word and worship. He is aware of the twin pillars on which Godward worship rests: "In worship, we seek to inform the mind with biblical truths about God so that the heart will rightly respond to his greatness and glory."


text:
Restricted Content / Members Only
You cannot view this content because It is available to members only. Please Login Here to view this content.
Career tips and advice for Architects …
We asked our Architect members for their top career tips – and the responses were overwhelmingly useful and sometimes borne of painful experience – and we also got the odd tip on the worst advice members had ever been given – and some surprises too …
Communicate with people in your environment and be comfortable is the most important thing because you can get experience and share ideas
|None – the worst advice I was given was to try everything
|Be tough, it's not that easy when you first start out so you have to push through it. Also, don't be too picky with your first job
|Just work hard, I guess
|I went into project management for the better conditions and job security and I feel it was the right decision. For grads, my advice would be use your connections and network, network, network!
|Get a broad range of experience and then decide on what you wish to specialise in and pursue it. Don't start of with limitations
|Networking is the key – whether that's going to a function at uni or getting to know people in the industry
|Protect your work interests, make sure you're getting the right rates and super. Don't be afraid to travel. Balance aspiration with realistic goals. Recognise that you are not yet an expert and you won't be running the company in two years, but avoid getting stuck doing the same task over and over during your best learning years
|Don't work for family
|Go overseas, broaden your ideas before starting are career in Australia
|Do it for a hobby, you have no idea how true that really is!!
|Something can be gained by every job, every job has an upside
|It is not about where you studied it is about the passion you put in to it – your work will speak for itself
|It's good to dream big, but just take it a step at a time. Do what's in front of you properly and don't try to rush. Do every task with the right attitude
|Work overseas, join APESMA and network
|Make sure you have good support and are willing to be creative
|One of the things I was never told: "make a plan for my future, know where you're going and what you want from life"
|Get a good grounding and be adventurous
|Don't work somewhere if you're not happy
|If you're looking to advance, look around and don't stay too long in one place early in your career. You are highly employable, so move on and up
|Sometimes you need to step into the shoes of the employer and see it from their perspective
|Don't do it for the money
|Don't be over influenced by one person or idea
|Presentation of portfolio is important and make sure it's relevant
|Try to understand that what is on your 2D page will have to be imagined and made 3D
|If you work hard and do all the uninteresting stuff you can work your way to the job you want
|Get out there and ask people – keep pestering
|Keep applying for jobs and don't let rejection stop you
|When at uni make the most of the creative outlet as creative experiences are not as common when starting out in the workforce
|You can sleep when you die
|In terms of looking for a job, go into places and also keep in contact and keep a rapport
|Don't work for family and friends.
|Get out there and see more things
|When you're doing an internship – learn as much as you can and take whatever comes
|Do something you love and going to work will never be work
|Experience gives you the knowledge to go forward
|Don't blanket cover the industry with your resume
|Get experience and exposure to the industry before you go for the job you like
|Be yourself and be confident in what you do
|Take up any job opportunity you are given and learn as much as you can from it
|Work hard and never give up!!!
|I've heard someone say "don't work with your spouse"
|Be confident in what you do and take pride in your work
|Get into something you enjoy
|Start looking and always be aware of what's going on in the industry
|Keep trying to get in no matter what
|Love your job – not the company
|You should never stress whilst you are studying – it is only 20% of what you need to know the rest you will learn on the job, and always keep your mind and options open
|I spoke to someone at APESMA and they told me to be prepared for the job market and always have things like your contract checked over to avoid problems later on
|Networking is key
|Follow your passion. If you're not liking it or learning from it then it's probably time for you to move on. I had a great experience a little while back where I went on the APESMA website and applied for a mentor. The mentor was full of great advice and helpful clues about the industry. I did end up moving into urban planning but I still used his advice to apply myself
|Just get involved in the industry by putting your resume/yourself out there
|The best advice I got was from APESMA who advised me to be careful when it comes to things like contracts and employee rights. It's always a good idea to have your contract checked and to know what your rights are as an employee
|Do an internship at a small firm, otherwise you end up photocopying
|Build a great portfolio
|It's a boom and bust profession so diversify to protect your income
|Start up and build your own business
|Never give your designs away for free. If you don't value it other's won't either
|When you go for an interview and you know you want the job, do your research and make sure the company and the job are the right fit and always be ready with questions
|Don't try to set up your own business in the first couple of years like I did – try to get some experience in a firm first in different types of projects
|Be creative and be outstanding
|Keep networking and establishing contacts. Having a mentor helps you keep on track with your career path and development of skills. Keep your eye on the next step
|Keep your options open don't limit yourself</f
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text:
The live Edit Counter tool is at https://xtools.wmflabs.org/ec
Example result page: https://xtools.wmflabs.org/ec/en.wikipedia.org/GoldenRing
The XTools code repository: https://github.com/x-tools/xtools
The "Files renamed" field should go under the "Files" section in the left column.
A file rename is actually just a page move, but in the File namespace.
What needs updating code-wise:
- The EditCounterRepository, specifically [[ https://github.com/x-tools/xtools/blob/master/src/Xtools/EditCounterRepository.php#L27 | getPairData ]], since this is just a COUNT.
- A getter in the EditCounter model.
- The general stats view
- Ideally the Edit Counter tests, if you are familiar with PHPUnit and mocking.


text:
Responsible Gambling Awareness Week 2019
Introduction Responsible gambling RG tools, aiming at helping gamblers to avoid gambling-related harms, are common in online gambling platforms.
Gambling industry, policy makers, and researchers have warned that RG tools can potentially disturb recreational gamblers, channeling them to less protective operators.
No evidence exists to support these concerns, and they can hinder the development of effective RG tools.
The current study aimed to investigate the recreational gamblers' experiences of RG tools.
Methods A total of 10,200 active customers of an online gambling responsible gambling awareness week 2020 were invited to complete an online survey and rate their overall reactions, attitudes, disturbance and irritation towards RG tools, as well as their inclination to abandon a gambling service due to overexposure to RG tools.
2020 news texas gambling Non-problem gamblers had positive experiences of RG tools.
Moderate-risk gamblers had more positive overall reaction and less irritation to previous experiences of RG tools compared to non-problem gamblers.
Problem gamblers had least positive attitudes, most disturbance and most irritation towards RG pictures.
Non-problem gamblers had lowest responsible gambling awareness week 2020 of having abandoned a service because of perceived overexposure to RG tools 5.
Conclusions Non-problem gamblers were not particularly disturbed by Responsible gambling awareness week 2020 tools and were not at risk of abandoning online gambling services because of overexposure to RG tools.
The study found no grounds for limiting the design and implementation of RG tools due to fears of disturbing recreational gamblers.
By continuing you agree to the.
Copyright � 2020 Elsevier B.
ScienceDirect � is a responsible gambling awareness week 2020 trademark of Elsevier B.
ScienceDirect � is a registered trademark of Elsevier B.
Meet Buck - Responsible Gambling
help services, the Committee during the period 2017-2020 will implement the following. Participate annually in Responsible Gambling Awareness Week.
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Fellows Holiday Party
Monday, December 16, 2019 - 5:30PM-8:30PM EST
Online Registration for this event has CLOSED. In person Registration will be available on site beginning at 5:30 PM
Please join us for our annual Fellows Holiday Party on Monday, December 16th at La Vie. This is a great opportunity to catch up with old friends and meet some new Fellows! NOTE: This event is open only to Fellows (graduates of the Partners or Voyagers Professional Development Programs, including current Voyagers).
Date: Monday, December 16, 2019
Time: 5:30-8:30 pm
Location: La Vie (at the Wharf)
88 District Square SW Penthouse
Washington, DC 20024
Registration: Industry: $40
Government: $25


text:
Results 11 to 16 of 16
Thread: Withdrawal from Amitriptyline
01-04-16, 07:30 #11Intermediate MemberCountry:
- Join Date
- Nov 2006
- Location
- , , United Kingdom.
- Posts
- 542
Re: Withdrawal from Amitriptyline
Hi Terry - I had no start-up effects with Amit (maybe just a slightly dry mouth), so I am hoping that perhaps the same will be true of withdrawal side effects. I only plan to start withdrawal when Ron is at home for a couple of weeks, and when the reasons for the anxiety have abated - so it is not going to happen just yet.
As you know, I managed to withdraw from Mirtazapine without too many problems and I am hoping the same will be true of the Amit. BUT, until I can feel happy that my sleep is regulated (and I know that is not really the case just yet), I won't do anything.
Hope everything is okay with you Terry.
01-04-16, 07:51 #12
Re: Withdrawal from Amitriptyline
Maybe it depends on what dose you're on ... I take 10mgs Doxepin which is a cousin of Ami, and have no problem with withdrawal symptoms at all when I have a break from it.
I'm on a low dose for CFS which is an autoimmune condition.
02-04-16, 05:10 #13
Re: Withdrawal from Amitriptyline
Thanks sandie, yes I'm ok, just all the usual really.
That sounds very sensible. Given the easy start up, it does look very hopeful for an easy withdrawal. I hope it is anyway. You will probably notice anything as soon as you mess with the dose but the real test can be when you take the last one away with some of these meds or when you get to lower doses. I would be hopeful for a good withdrawal though given a good start up, my start ups are always horrendous and the withdrawals far easier.------------------------------------------------------------------------------------------------------------------------
For free Mindfulness resources, please see this thread I have created to compile many sources together http://www.nomorepanic.co.uk/showthread.php?t=168689
01-06-16, 11:08 #14Country:
- Join Date
- Jun 2016
- Posts
- 1
Re: Withdrawal from Amitriptyline
Hi, I too have just started to come off amitriptyline. Ive been on 10/20mg for the past 5 years and have now taken the decision to stop. Firstly I reduced to 10 MG for a couple of weeks, then I cut the pills in half for a week. Now I have been off completely for 5 days. I don't feel great, on and off nausea and headaches and I feel so tired all the time, but currently its bearable. Im hoping that the withdrawal symptoms will begin to lessen over the next few days. I'll try and update you on my progress. I imagine it may take a while due to the length of time ive been on these meds.
23-05-18, 11:29 #15Country:
- Join Date
- May 2018
- Posts
- 21
Re: Withdrawal from Amitriptyline
For me a gradual taper and not missing doses has made the withdrawal easier to deal with even so I get terrible blood pressure spikes, nuero symptoms, headache and extreme fatigue, which lasts just over two weeks then I start feeling better and my moods stabilize. I taper by 2.5mg at a time, have read that 10% tapering is the easiest, and you need to be patient. It has taken me nearly 6 mmonths, and am in withdrawal at the moment have a week and a half to go, then I am off them.
27-07-18, 21:07 #16Country:
- Join Date
- Mar 2017
- Posts
- 30
Re: Withdrawal from Amitriptyline
Realize this is an old thread, but I was able to taper off of 50mg of amitriptyline in about 8 months. I was able to go from 50mg down to 10mg in 4 months and it took another 4 months to go from 10mg to 0. At several steps in the process I got side effects like the OP had when I dropped the dose; for me it was mainly waking up super early (3-4 AM) and not getting back to sleep. Any time that happened I'd alternate between my previous dose and the new dose for a few days and then try reducing again. I think I was on 10mg for a few weeks, 5mg for a few weeks, 2.5mg for a month, then 1.25 for a few weeks, then I had 1.25 every other day and then every 3 days for a couple of weeks each until I was completely done. I also supplemented with l-theanine, GABA, taurine, and inositol as part of the taper, which seemed to help with sleep and anxiety quite a bit.
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text: thibodba57 435 Posted March 3, 2017 So seems like this software is dead now or not being developed? Ripjaw hasn't signed into Avsim since April of last year and no one is replying to the development progress of P3D compatibility. Shame. Anyone hear anything? Brian Thibodeaux | B747-400/8 First Officer, C-130 Flight Engineer, ATP, CFI My Liveries Share this post Link to post Share on other sites


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Meet Biovian at the BioProcess conference, which will be held 22-23 April 2009 in Düsseldorf, Germany. Biovian's CEO, Mr Sakari Heyno, and director of projects and marketing, Dr Knut Ringbom, will be available for in-depth disussions with your delegates at booth 27a.
As one of the main exhibitors, Biovian has negotiated reduced fees on behalf of their clients to attend this conference. All of Biovian's biopharm clients are entitled to a 25% discount off the top price tier. To take advantage of this offer simply contact Katrina Ryan at email@example.com.


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Michail Antonio had yet another goal ruled out for VAR in the 1-0 win over Southampton.
In the second half, Antonio thought he had made it 2-0 to the visitors. But VAR had other ideas. The goal was watched by the video referees, who decided Antonio had unlawfully used his hand.
Antonio also had a goal disallowed against Chelsea for a handball. It seems that the new system has not been too kind to Antonio since his return from injury.
'Handball decisions are killing me'
But Antonio – widely considered to be the Hammers clown – took to Twitter to poke fun at himself. He posted a picture of himself running with inflated hands and said: "These handball decisions are killing me, can't work out why it keeps happening."
These handball decisions are killing me, can't work out why it keeps happening 🤔🤣🤣🤣🤣🤣 pic.twitter.com/tlnOn7W3mp
— Michail Antonio (@Michailantonio) December 14, 2019
Michail Antonio changes West Ham
As it worked out, West Ham did not need that second Antonio goal. It would have been nice to have a cushion towards the end as Southampton came looking for an equaliser. But West Ham held on and picked up all three points.
Antonio has been a major factor behind the two recent wins. He makes West Ham look like a much better team with his tireless work rate and physical presence. He is a nightmare to defend against.
Last night, Antonio could have been given a penalty and he could have had a goal. But he proved why he is so important to this team. And off the pitch, his jokes have kept the morale high among his West Ham colleagues.


text:
A young professional's take on the trials and tribulations of everyday life in New York City.
By Nina Pajak
One of the easiest and most-repeated selling points about this city is the ease with which a person can get nearly whatever he or she wants at any hour of the day or night. Where other cities have a certain neighborhood that keeps late hours or a handful of spots scattered about that will deliver at any hour, it's just part of the culture here. We completely take it for granted that if you have a craving for a cookie or a fried egg sandwich at 4 a.m., your only obstacle is the internal pressure to exercise some impulse control.
But now that SeamlessWeb's popularity has crested and given birth to copycat competitors, nearly every restaurant in our neighborhood is a mere few clicks away. Places that under previous circumstances, if I had wanted to sample their wares, I would have been compelled to, I don't know, put on pants. Maybe splash some water on my face. But now we can dine finely in the comfort of our sweatpants without ever having to see another human being aside from the delivery guy.
O SeamlessWeb, how do I love thee? Let me count the ways.
1. You eliminate the need to have confusing and increasingly loud conversations with phone order-takers in noisy restaurants.
2. You narrow down my options for me, as more and more I now order exclusively from restaurants that use your service.
3. You make ordering meals an even faster and lazier process than it ever was.
4. I'm fairly certain you're directly responsible for those last three pounds I gained as a result of reasons one through three.
5. You inspire me to
spend more money support local business much more than I ever have in the past.
I think that's plenty of ways.
So is this a great development in our lives? It certainly takes convenience to a new level in a city that had already seemingly perfected that. But it's also just another way in which the interwebs make it possible for us to avoid social interaction. Then again, who am I to stand in the way of innovation? Mostly, I'm just totally addicted, as are most people I know, and I'm guessing plenty I don't. Why fight it? I'm all in. And besides…meh, I'm too tired to finish my point. Mmm, pajamas.
Dear Readers: While I am rarely at a loss for words, I'm always grateful for column ideas. Please feel free to e-mail me your suggestions.
Nina Pajak is a writer and publishing professional living with her husband on the Upper West Side.
The Nina Archives:
I used to worm in NYC (now I'm in CT) but MAN I miss Seamlessweb I still remember the looks from some of my coworkers. "What are you doing for lunch?" "Oh I'm doing Mexican" *phone rings* "Yes? OK great!, excuse me a sec guys." *comes back with Mexican* "Dude?! How did you get the food so fast?!?!?"
Not to mention ANYTHING you wanted. Great stuff.
Is this an ad for Seamless Web? I know subjects are hard to come by but spamming as blogging? Really???
is an article that mentions a brand always an advertisement for that brand? Are we that cynical? Since you've posted so many times about topics being hard to come by, why don't you suggest a couple? We all live in NYC – at least I assume you do – so there has to be something else on your mind if this isn't it.
Nathan, why do you continue to read this column if you consistently dislike it? That's not something that normal people do. Get a life, make a friend, take your meds, try to be something other than a loser.


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The TOC contents of the 16 samples are listed in Table 1. Samples from Dalong Formation in Well XY1 mainly contained Type-Ⅱ OM with TOC ranging from 2.72% to 6.79%. Samples from Longtan Formation in Well XY1 contained mainly Type-Ⅲ OM with TOC ranging from 1.72% to 10.29% (Bao et al., 2016), TOC content of the coal sample was 38.41%. Samples from Dalong Formation in Well EJ1 contained Type-Ⅱ OM with TOC ranging from 5.52% to 11.25% (Qiu et al., 2019). The TOC of samples close to the coal seam increased in Longtan Formation (Fig. 2). The thermal maturity results showed that the Ro of Well XY1 samples ranged from 1.22% to 1.43%, which was assigned to early generation stage of the condensate oil and wet gas. The Ro of Well EJ1 samples ranged from 2.62% to 2.97%, which was assigned to the over-mature stage and generation of dry gas.
Sample Depth (m) Formation Lithofacies TOC (%) Ro (%) Kerogen type Mineral composition (wt.%) Quartz Feldspar Dolomite Calcite Clay Pyrite Other XY-1 600.22 Dalong Black calcareous shale 3.69 1.34 Ⅱ 60 6 2 10 20 2 XY-2 602.67 Dalong 2.72 / Ⅱ 63 3 2 23 8 1 XY-3 608.08 Dalong 4.96 1.22 Ⅱ 45 7 4 19 23 2 XY-4 612.76 Dalong 5.09 1.37 Ⅱ 49 7 1 22 18 3 XY-5 624.87 Dalong 5.07 / Ⅱ 33 7 2 19 36 3 XY-6 629.59 Dalong 3.13 / Ⅱ 55 4 6 20 13 2 XY-7 631.18 Dalong 6.79 / Ⅱ 49 5 / 10 33 3 XY-8 641.78 Dalong 3.00 1.27 Ⅱ 29 8 / 38 21 4 XY-9 685.07 Longtan Grey-black silt mudstone 1.72 / Ⅲ 53 16 / / 31 / XY-10 689.10 Longtan Black-mudstone 7.17 / Ⅲ 14 5 / 2 57 / 22 (Siderite) XY-11 692.66 Longtan Black mudstone 10.29 1.41 Ⅲ 32 3 5 / 60 / XY-12 697.81 Longtan Coal 38.41 1.43 Ⅲ 40 / / / 48 12 EJ-1 827.87 Dalong Black shale 5.52 2.62 Ⅱ 12 30 / 40 14 2 2 (Gypsum) EJ-2 845.00 Dalong 6.14 2.84 Ⅱ 70 7 1 8 11 3 EJ-3 850.75 Dalong 11.25 2.97 Ⅱ 76 7 3 9 4 1 EJ-4 856.46 Dalong 7.62 / Ⅱ 52 10 1 8 26 3
Table 1. Basic properties of sixteen samples used in this work. TOC. total organic carbon (%), /. not available
The mineral compositions of Dalong Formation in the wells XY1 and EJ1s mainly consisted of quartz, carbonate minerals, feldspar, and clay minerals. The clay fraction was the dominant mineral species for Longtan Formation in Well XY1, with almost no carbonate minerals present (Table 1).
According to the classification of isotherms proposed by IUPAC (Thommes et al., 2015), the CO2 adsorption isotherms of all 16 samples showed Type-Ⅰ curve characteristics (Figs. 3a-3c). Dalong Formation samples in Well XY1 displayed the least amount of adsorption, while Longtan Formation samples and Dalong Formation samples in Well EJ1 showed a much higher gas adsorption capacity, indicating that these samples had more micropores. Micropore volumes calculated from CO2 adsorption are listed in Table 2. Micropore volumes of Dalong Formation and Longtan Formation in Well XY1 were in the range of 0.002-0.005 and 0.004-0.010 cm3/g, respectively, while Dalong Formation in Well EJ1 had the highest micropore volumes ranging from 0.007 to 0.011 cm3/g.
Figure 3. CO2 adsorption (a)-(c) and N2 adsorption and desorption isotherms (d)-(f) of Longtan and Dalong samples determined in wells XY1 and EJ1.
Sample ID Formation TOC (wt.%) DFT micropore volume (cm3/g) BJH mesopore volume (cm3/g) BJH macropore volume (cm3/g) Hg porosity (%) XY-1 Dalong 3.69 0.004 0.003 0.004 / XY-2 Dalong 2.72 0.003 0.003 0.004 / XY-3 Dalong 4.96 0.005 0.004 0.005 0.53 XY-4 Dalong 5.09 0.004 0.003 0.007 0.31 XY-5 Dalong 5.07 0.003 0.002 0.003 0.18 XY-6 Dalong 3.13 0.002 0.003 0.005 0.26 XY-7 Dalong 6.79 0.004 0.003 0.004 / XY-8 Dalong 3.00 0.003 0.004 0.004 / XY-9 Longtan 1.72 0.004 0.007 0.007 1.21 XY-10 Longtan 7.17 0.010 0.012 0.004 / XY-11 Longtan 10.29 0.009 0.013 0.006 1.53 XY-12 Longtan 38.41 0.010 0.002 0.004 / EJ-1 Dalong 5.52 0.007 0.013 0.008 0.85 EJ-2 Dalong 6.14 0.008 0.013 0.006 2.12 EJ-3 Dalong 11.25 0.011 0.019 0.013 5.42 EJ-4 Dalong 7.62 0.010 0.016 0.007 1.63
Table 2. N2, CO2 adsorption and MICP results for Longtan and Dalong shales samples. DFT. density functional theory; BJH. Barrett Joyner Halenda method; micropore volume is obtained from CO2 adsorption by DFT; mesopore and macropore volume are obtained from N2 adsorption by DJH; Hg porosity is calculated by MICP
Figures. 3d-3f show the N2 sorption-desorption isotherms of all 16 samples. According to the classification of isotherms proposed by IUPAC (Thommes et al., 2015), the isotherms of all 16 samples were Type-Ⅱ and Type-IV(a), indicating multi-layer adsorption. Dalong Formation samples in Well EJ1 had the highest amount of adsorption, which was approximately five times higher than that of Dalong Formation samples in Well XY1 and twice as much as that of Longtan Formation samples. From this we inferred that there were more pores present in Dalong Formation of Well EJ1. According to the classification of hysteresis loops proposed by IUPAC (Thommes et al., 2015), the hysteresis loops of Longtan samples in Well XY1 and Dalong samples in Well EJ1 were the mixture of H2(b) and H3 types, while the hysteresis loops of Dalong samples in Well XY1 were assigned to H4 (Fig. 3). All isotherms showed a hysteresis loop, indicating that capillary condensation had occurred in the mesopores. It was obvious that the opening of the hysteresis loops of Dalong samples in Well XY1 were narrow, reflecting relatively small pore size (Fig. 3d). The mesopore and macropore volumes were the highest in Dalong Formation samples from Well EJ1 and lowest in Dalong Formation samples from Well XY1 (Fig. 4).
Figure 4. The micropore, mesopore, macropore volume for Longtan and Dalong samples from wells XY1 and EJ1 (calculated from CO2 and N2 adsorption data).
According to the classification of isotherms proposed by IUPAC (Thommes et al., 2015), the absolute CH4 adsorption isotherms of all the samples show the characteristics of Type I curve (Fig. 5) with varying Langmuir adsorption capacity.
Figure 6 shows the curves of the mercury intrusion and extrusion at pressures ranging from 0.034 to 413 MPa. The mercury intrusion volumes of Dalong Formation samples from Well EJ1 were the highest (6.65-8.84 μL/g), which was approximately four times higher than that of Dalong Formation samples from Well XY1 (1.23-2.16 μL/g), and approximately twice as much as that of Longtan Formation samples (4.68-5.65 μL/g). As the mercury intrusion pressure ranged from 0.1 to 1 MPa, the XY-11 sample from Longtan Formation in Well XY1 took a larger volume of mercury than the other samples from Dalong Formation in both wells EJ1 and XY1s (Fig. 6). Therefore, it could be inferred that Longtan sample had more micron-sized pore throats, whereas Dalong sample had more nanoscale pore throats. When intrusion pressure reached 100 MPa, the volumes of mercury injected into Dalong samples of the EJ1 increased significantly (Fig. 6c), reflecting the good connectivity of the nanoscale pore throats. In contrast, the curves determined for Dalong samples from Well XY1 showed the least amount of injected mercury (Fig. 6a), indicating the worst pore development and connectivity. According to the distribution of pore throat histogram, 3-20 nm size pores account for a large proportion of the total pore volumes in Dalong Formation (Figs. 7a, 7b, 7e, 7f), whereas 20-200 nm size pores accounted for a large proportion of the total pore volumes in the Longtan Formation (Figs. 7 b, 7c). Porosity of Dalong samples in Well EJ1 (0.85%-5.41%) was much higher than that of Dalong samples in Well XY1 (0.18%-0.53%), and the porosity development of Longtan samples was between (1.21%-1.53%).
Figure 6. Cumulative mercury intrusion and extrusion curves (a)-(c) for Longtan and Dalong samples from wells XY1 and EJ1.
Many oil inclusions with blue fluorescence were observed in the calcite veins developed in Dalong shales of Well XY1 (Figs. 8b, 8d). Under transmission light, oil inclusions were densely distributed and transparent where the coating wall was thin and clear (Figs. 8a, 8c). Gas inclusions were relatively dark under transmission light and sparsely distributed (Figs. 8a, 8e). Under UV light, a certain proportion of gas inclusions was covered with a thin layer of liquid hydrocarbon inside and emitted weak yellow-green fluorescence (Figs. 8b, 8d). A small number of pure gas inclusions did not emit fluorescence (Figs. 8e, 8f). The laser Raman spectrogram for the gas inclusions in Well XY1 showed a significant CH4 peak at wavelength 2 909.473 9 cm-1, indicating this was a pure CH4 inclusion (Fig. 9a). Except for the CH4 peak, some gas inclusions also presented weak C2H6 peaks (2 879.657 3 and 2 944.351 2 cm-1) on both sides of the CH4 peak (Fig. 9b), indicating that the gas inside was a mixture of gaseous hydrocarbons (CH4 and C2H6). A large number of experimental analyses have confirmed that fluorescence color can be used as an indicator of OM maturity (George et al., 2001; Stasiuk and Snowdon, 1997; Videtich and Roger, 1988). The evolution of OM from low mature to high mature will lead to a change of inclusion type from heavy oil inclusion to condensate oil inclusion. Meanwhile, the fluorescence color emitted will change consistently from red, to yellow, to yellow-green, and to blue (Zhao et al., 2019; Zhao and Chen, 2008). Based on the observation that all oil inclusions show blue fluorescence accompanied by a small amount of gas inclusion, we inferred that there was light oil generated and expelled from the adjacent Dalong Formation shales, which was accompanied by a small quantity of gas due to gas-prone maceral degradation in the kerogen. The characteristics of the hydrocarbon inclusions were also consistent with the measured Ro (1.22%-1.34%) of Dalong samples in Well XY1 (Table 1) which was in the early stage of the condensate oil and wet gas window.
Figure 8. Microscopic characteristics of fluid inclusions in calcite veins. (a), (b) The number of oil inclusions is predominated with blue fluorescence, Well XY1, 602 m; (c), (d) oil inclusions with blue fluorescence and gas inclusions with weak yellow-green fluorescence, Well XY1, 602 m; (e), (f) pure gas inclusions with no fluorescence, Well XY1, 602 m; (g), (h) CH4 inclusions Well XY1, 850.75 m.
All hydrocarbon inclusions observed in calcite veins from Well EJ1 were gas inclusions without fluorescence (Figs. 8g, 8h). The laser Raman spectrogram for all gas inclusions showed a characteristic CH4 peak only (Fig. 9c). The measured Ro of the adjacent Dalong shales ranged between 2.62% and 2.97%, which was in the late stage of the dry gas window. It was inferred that the CH4 inclusions were the product of secondary cracking from the adjacent Dalong shales.
Based on observations of FE-SEM images, the interior of certain OM from Dalong shales of Well XY1 was not homogeneous and could be divided into dark and bright parts with distinct boundaries (Figs. 10a-10d). It is noticeable that spot-like and irregular pores were prone to develop in the light part, while dark part rarely developed observable pores. In addition, the boundary of bright part was irregular and serrated, whereas that of dark part was a regular and smooth curve (Figs. 10a-10d). Some OM partly filled the internal body cavity of the pyritized fossil (Fig. 10g). Many clay mineral flakes were entirely wrapped by OM (Figs. 10e, 10f). A small amount of OM which occurred as discrete particles with sharply defined edges and a relatively homogeneous internal texture can be observed within the mineral matrix (Figs. 10h, 10i).
Figure 10. FE-SEM images of OM from Dalong Formation in Well XY1. (a) OM divided into nonporous part (bitumen) and porous part (kerogen) with mesopores, Dalong Formation, Well XY1, 608.08 m; (b) bitumen having spot-like micropores and kerogen having irregular mesopores, Dalong Formation, Well XY1, 608.08 m; (c) OM divided into nonporous part (bitumen) and porous part (kerogen) with micropores, Well XY1, 624.87 m; (d) OM divided into nonporous part (bitumen) and porous part (kerogen) with micropores, Well XY1, 624.87 m; (e) kerogen enclosing plenty of clay mineral flakes, Well XY1, 608.08 m; (f) an enlargement of the rectangle area marked in Fig. 10e, showing a small amount of spot-like micropores, Well XY1, 624.87 m; (g) bitumen filling part of internal body cavity space of pyritized fossil, Well XY1, 608.08 m; (h) terrestrial woody debris with rounded shape and gas-prone kerogen with few micropores, Dalong Formation, XY1, 624.87 m; (i) an enlargement of the rectangle area marked in Fig. 10h, showing filling of bitumen in macropores in terrestrial woody debris (white arrow), Well XY1, 624.87 m.
Milliken et al. (2013) found a similar phenomenon in Pennsylvania Marcellus shales and interpreted this as wood fragments. Loucks et al. (2017) observed similar OM which was micron-size and nonporous from Yanchang Formation in the Ordos Basin, and interpreted this to be Type Ⅲ woody maceral. In this study, we considered that this kind of OM was terrestrial woody debris derived from the original plant tissue. There was a distinct boundary between two different OM (Figs. 10h, 10i).
The morphology of OM in Longtan shales of Well XY1 was significantly different from that in Dalong shales. As shown in Fig. 11, the OM in Longtan shales of Well XY1 had a distinct texture with a long strip shape. The boundary of the OM was smooth and regular. Due to compaction, some OM were highly curved and obviously oriented (Figs. 11e, 11f). The pore development in different OM varied considerably. Some OM were nonporous, while the adjacent one may possess a large number of pores, which were filled with quartz and illite (Figs. 11a-11d). Liu et al. (2017) found that vitrinite was nonporous, whereas the interior of inertinite generally had a certain number of circular cellular pores, some of which were filled with authigenic quartz. The sedimentary environment of Longtan Formation was lagoon-swamp facies and almost all OM was from terrestrial inputs. Sample XY-11 was very close to the coal seam at the base of Longtan Formation. Therefore, it was likely that the OM in Longtan Formation samples were all terrestrial woody debris.
Figure 11. FE-SEM images of organic matter from Well XY1, Longtan Formation. (a) Terrestrial woody debris with rounded pores, Well XY1, 692.66 m; (b) terrestrial woody debris with rounded pores and some nonporous kerogen debris, Well XY1, 692.66 m; (c) abundant rounded and nano-scale pores, Well XY1, 692.66 m; (d) curved and distorted kerogen debris and long-strip kerogen debris, Well XY1, 692.66 m; (e) an enlargement of the rectangle area marked in Fig. 11d, showing curved and distorted kerogen debris with rounded pores, Well XY1, 692.66 m; (f) kerogen debris with rounded pores, part of which are filled by quartz, Well XY1, 692.66 m.
The morphology of the OM in Dalong samples of Well EJ1 all showed the characteristics of filling interparticle pores and appeared pervasive throughout the mineral matrix (Fig. 12). Moreover, they had an amorphous shape as well as significant flow structure (Figs. 12e, 12h, 12i). Some OM enclosed mineral grains and clay flakes (Figs. 12c-12e). There were a small number of terrestrial woody debris whose morphology was substantially different from that of the adjacent amorphous OM (Figs. 12g, 12h). There were some differences between the OM in Dalong shales in the two wells. Unlike the OM in Well XY1, which had a granular texture and develop only a small number of pores inside, the interior of the OM in Well EJ1 was almost filled with sponge-like nanopores (Figs. 12a-12c, 12f). As Dalong shales from the two wells had the same type of OM, thermal maturity may have been the determining factor that controled the morphology and inner structure of the OM.
Figure 12. FE-SEM images of OM in Well EJ1 Dalong Formation. (a) Pyrobitumen filling pore space within mineral grains, Well EJ1, 827.87 m; (b) an enlargement of the rectangle area marked in Fig. 11a, showing plenty of alveolate, spongy and irregular pores, Well EJ1, 827.87 m; (c) pyrobitumen enclosing clay mineral flakes with abundant nano-scale pores, Dalong Formation, Well EJ1, 856.46 m; (d) pyrobitumen enclosing mineral grains with abundant nano-scale organic pores, Dalong Formation, Well EJ1, 856.46 m; (e) pyrobitumen with flow structure, Well EJ1, 856.46 m; (f) pyrobitumen filling pore space within mineral grains with bubble-like, alveolate and spongy organic pores, 856.46 m; (g) terrestrial woody debris with long-strip shape, Well EJ1, 856.46 m; (h) terrestrial woody debris with rounded pores and pyrobitumen with flow structure, 856.46 m; (i) an enlargement of the rectangle area marked in Fig. 11h, showing distinct boundaries of pyrobitumen and terrestrial woody debris, 856.46 m.
FE-SEM images showed OM pores in shale samples from different formations were different in terms of shape, size, and distribution density (Figs. 10-12). The OM pores in Dalong shales of Well XY1 were mainly micropores, sparsely distributed in the OM (Fig. 10). The morphology of the micropores was spot-like, while most mesopores had a irregular shape. A small number of round macropores could be observed in the terrestrial woody debris (Figs. 10h, 10i). Considering the thermal maturity of the samples (Ro=1.22%-1.34%), it could be inferred that the tiny spot-like and irregular OM pores were caused by the generation of gaseous hydrocarbons in gas-prone maceral in kerogen, which was also consistent with the occurrence of a small amount of CH4 inclusion in calcite veins.
The OM pores in Longtan shales of Well XY1 mainly consisted of mesopores and macropores, and had a relatively rounded shape with well defined-boundaries (Fig. 11). The distribution density of OM pores in different types of debris varied considerably. Some debris developed abundant pores with different sizes, ranging from several nanometers to hundreds of nanometers and even a few micrometers (Figs. 11a-11c), while other debris had only sporadic pores or no pores at all (Figs. 11b, 11d). Xu and Sonnenberg (2017) observed a similar phenomenon in the immature Bakken Shales, indicating that these rounded pores may not be the outcome of thermal evolution. The shape of the strip debris was extremely distorted and twisted, while the internal OM pores were still rounded and equant, implying that this kind of debris was hard enough to resist compaction (Figs. 11d-11e).
FE-SEM images showed that the irregular and spongy-like pores with diameter ranging from several to hundreds of nanometers were densely developed in the OM from Dalong shales of Well EJ1 (Fig. 12). There was a small number of terrestrial woody debris that had no pores or only a few rounded pores (Figs. 12g, 12i). The higher degree of thermal evolution gave rise to more densely distributed pores in the OM, while the quantitative distribution of pores in the terrestrial woody debris was almost the same as that from the samples from Well XY1, indicating that these rounded pores in the woody debris were not the product of thermal evolution.


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01914nas a2200157 4500008003900000022001400039245008200053210006900135260001200204300001100216520140400227653001301631100002101644700002001665856007101685 2015 d a0885-895000aUnit Commitment With Continuous-Time Generation and Ramping Trajectory Models0 aUnit Commitment With ContinuousTime Generation and Ramping Traje c10/2015 a1 - 103 a
There is increasing evidence of shortage of ramping resources in the real-time operation of power systems. To explain and remedy this problem systematically, in this paper we take a novel look at the way the day-ahead unit commitment (UC) problem represents the information about load, generation and ramping constraints. We specifically investigate the approximation error made in mapping of the original problem, that would decide the continuous-time generation and ramping trajectories of the committed generating units, onto the discrete-time problem that is solved in practice. We first show that current practice amounts to approximating the trajectories with linear splines. We then offer a different representation through cubic splines that provides physically feasible schedules and increases the accuracy of the continuous-time generation and ramping trajectories by capturing sub-hourly variations and ramping of load in the day-ahead power system operation. The corresponding day-ahead UC model is formulated as an instance of mixed-integer linear programming (MILP), with the same number of binary variables as the traditional UC formulation. Numerical simulation over real load data from the California ISO demonstrate that the proposed UC model reduces the total day-ahead and real-time operation cost, and the number of events of ramping scarcity in the real-time operations.10aRM11-0071 aParvania, Masood1 aScaglione, Anna uhttps://certs.lbl.gov/publications/unit-commitment-continuous-time


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by Alan Babbitt
The Hope College men's lacrosse team is in a New York state of mind.
The MIAA champion Flying Dutchmen will make their first appearance in the NCAA Division III Tournament this week in Rochester, N.Y.
Hope (14-3 overall) will play John Carroll University (Ohio) in a first-round game on Tuesday, May 7 at Rochester Institute of Technology. Game time and ticket information are to be announced.
The Hope-John Carroll winner advances to face top-ranked RIT in a second-round game on Wednesday, May 8.
Under the direction of head coach Michael Schanhals, the Flying Dutchmen earned the MIAA's automatic berth for the 36-team NCAA Tournament by defeating Albion College, 6-5, in Saturday's MIAA Tournament championship game at Hope College.
NCAA Tournament Bracket | NCAA Tournament Announcement
The Flying Dutchmen were seeded No. 1 for the MIAA Tournament after repeating as MIAA regular-season champions.
Hope's 14 wins are the second-most in the team's seven-year history as a varsity sport. The Flying Dutchmen posted a 15-2 record during the 2018 season.
This is the second time Hope has played John Carroll. The Flying Dutchmen won a regular-season game, 9-7, on March 8, 2018 at Hope College.
John Carroll (12-6) is making its fourth consecutive appearance in the NCAA postseason as champions of the Ohio Athletic Conference. The Blue Streaks are 1-3 all-time in NCAA Tournament games, with a 2017 first-round win against Albion College. John Carroll's three postseason losses are to RIT.
RIT (18-1) is making its 21st trip to the NCAA Tournament.


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Elijah is the founder and owner of Blue Ridge Motion, having taught himself parkour back in 2009, he hasn't stopped moving since. He discovered his passion for movement in 2007 when he first began to take MMA classes, over time he began to try break dancing, and ultimately, parkour, tricking and free running. He was […]


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At the end of the lesson, students will be able to…
- develop and practice analytic and problem-solving skills
- recognize that students can defuse violence and tension at school
- understand and value other perspectives, especially those that differ from their own, through dialogue
- How does hate language affect those who are targeted?
- How can people increase intergroup tolerance and reduce bias attitudes that lead to hate-based violence?
- Enduring Understandings
- Hate speech is language that promotes fear and incites violence against vulnerable or singled-out individuals or groups.
- Establishing relationships and increasing communication between individuals or groups can enhance understanding among people.
- Reading: Setting the Scene
- Handout 1: What Do We Do Now?
slur [ slər ] (noun) an insulting remark
immigrant [ im-i-grint ] (noun) a person who moves to a country to live there
mediator [ me-dee-ayt-er ] (noun) someone who works with opposing sides to reach an agreement
Somalia [ sə-mäl-ēə ] (noun) a war-torn country in East Africa, formerly a colony of Britain and Italy. Civil war raged in the early 1990s, and tens of thousands of Somalis sought refuge in the United States.
Suggested Procedure
1. In this lesson, students will imagine that they are students at a high school that is polarized by violence between native-born students and foreign-born African immigrant students. Tell students that they are going to listen to an account of what was happening at the school. Then, as a class, we will work together to improve the school's situation. Read Setting the Scene aloud for the students.
2. After listening to the account, have students read and complete the activities on Handout What Do We Do Now? Students should work in small, diverse groups. Choose a representative in each group to report back to the class.
3. When students have completed the activities, sit together as a class. Taking turns, each representative should report its group's top two solutions and explain to the class why they chose those solutions. Keep a class chart that lists the favored options. If there is no clear class consensus on two solutions, ask students to return briefly to their groups. Ask: "Have you changed your minds based on what other groups have presented? Return to the entire class and come to an agreement about the best solutions."
4. Now read aloud what actually happened at the school: 'The students felt some urgency, but they weren't sure what to do. Together with the conflict mediator, they decided that a quick solution would be to talk to their peers and tell them that the violence had to stop. They weren't all that eager to do it, and they weren't confident that it would work. But they could do it right away, and at least it was something. So the 25 leaders left the lunchroom that day, each agreeing to talk to five of their peers and tell them that things had to change.'
"A week later, when students returned from spring break, something had definitely changed at the school. There were no fights that first day, or that first week. In fact, things stayed pretty calm for the rest of the school year. No one was more surprised than the students themselves. They had felt so helpless to make a difference. But they had: just by talking with other students, they had defused the violence in their school."
5. The students found an immediate way to change the situation at their school. As a class, discuss: Does their actual experience change your thinking? Why or why not?
Alignment to Common Core State Standards/ College and Career Readiness Anchor Standards CCSS W.4, W. 7, SL.1, SL. 2, SL. 4, SL. 6, RH. 3
Extension Activity
Do Something
Tell your class, "The students at this school learned that they could change their attitudes by connecting personally with people who were, in some ways, different than they were, and whom they didn't know. As a class, brainstorm issues that create tension in our school or community. Make a list of ways you might foster discussion and change." Remind students that their actions—whether big or small—can make a difference.
As a class, select three problems and possible solutions or ways to alleviate them. Divide students into small groups and ask each group to reach out to others around the issues you've identified. After a week or longer, have students discuss the results and/or write about them. For one idea, read about Mix It Up at Lunch Day.


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  How To Lose Weight Fast - Just Got Easier - Weight Loss
- You Need To Know About Hormones And Muscles Also.
Burn off that unwanted body weight. How is that done? When your body is working, the metabolism is running. Energy, namely calories are required. Your fat can supply those needed calories. When muscles are active, then it goes without saying that the metabolism has increased for that. So fat burning has increased also and you can see results for skim milk lose weight 0c and how to lose weight fast . Lets get up and do this. No sitting around. Muscles have gotten you out of a lot of jams in the past. So why not employ them now? You wont be straining your muscles to work them. They want that. Muscles only like one thing, just one thing, working. Muscle activity is also good because you get more energy because the metabolism has increased. Is this a refreshing wave or what?
Your body puts hormones into the blood that are connected with burning fat. What is the mechanism that puts these hormones into play? If you eat the right proportions of foods, that will initiate the hormone flow.
So here is the answer. Have a diet where carbohydrates are a low to medium portion of the diet and proteins are a high percentage.
- Burning A Greater Number Of Calories Than You Are Eating.
You probably keep busy during the day, but allocate the time for studying this. It is really worth while. There are lots of ways to look at this, but the basic info for skim milk lose weight 0c and how to lose weight fast is right here. It does not matter too much what you are doing during the day. You are burning calories. Calories, calories, calories, are in all the foods that you consume. Fat in your body will usually be burned off if your activities require more calories than you have eaten on a specific day.
Does it seem to you that this can be or will be tough to learn? This is not hard. Really. It is not hard. In a typical day, you will use up 2000 to 2500 calories. This means you are burning that many calories. For most men and women, their diet will have at least 2000 calories and as much as 2500 calories in one day. So the average person maintains his or her weight.
This is not hard. Let us say that you eat 2000 calories a day. So for weight loss we want to burn more than we consume. If you consume 2000, then burn more than 2000. This is not some kind of tough math. Just make sure you burn more than you eat. This really is easy.
Carefully look at the information on the label of the foods that you buy. These nutritional labels will have the calorie content included there. You will be pleasantly surprised at how easy it is to understand this and achieve skim milk lose weight 0c and how to lose weight fast . This is the formula for skim milk lose weight 0c and how to lose weight fast . Here is the drill. It is simple. To get weight loss, pick the foods with less calories. This is the single most critical part of weight loss. Know the calories going in and know the calories being used. This is crucial, so do not try to ignore it. There is not a lot of time needed to do this, so spend the time on this.
- Important Info On The Meals Per Day Topic.
Think it will be a big task to get to skim milk lose weight 0c and how to lose weight fast ? Please read this carefully because it will convince you that this is not as difficult as you thought it was.
Skipping meals will work against you. Really. Bet you didn't see that one coming. You must have breakfast. Never skip it.
It has that specific name. Break means to stop. Fast refers to not eating. The fasting period is over. Now you eat. Metabolism is our friend. It burns calories. So we eat to get the metabolism fired up and running again.
If you eat smaller meals, but more of them, like 5 to 6. The term for this is grazing. Grazing is our friend to crank up the metabolism and use fat calories in the process. Step by step we reach to the goal of skim milk lose weight 0c and how to lose weight fast .
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During the final of the 7th and 2nd Boostcamp MIC Acceleration program of Microsoft Innovation Center Brussels (MIC Brussels), the most promising "first-time entrepreneurs" were rewarded according to their businesses potential.
The MIC Boostcamp is a 4-month coaching program launched in 2011, which helps entrepreneurs turn their ideas into feasible projects ready to be launched. This program offers six weeks of introduction, fifteen thematic workshops as well as meetings with experts and individualized monitoring.The Acceleration Program was launched by the MIC in February 2014 in partnership with Lifetech and Software clusters in Brussels, Impulse.brussels and Microsoft. It is a new coaching program for more advanced startups.
Check out the winners
In the category "Boostcamp": Yves Berquin won the Boostcamp Grand Prize for his project Make It Real. Pierre Moens won the Boostcamp Prize of the Brussels Capital Region for his Project Buddy Julie Cruyt won the Boostcamp Audience Award for her project SpaceFiT
In the "MIC Acceleration Program" Vianney Veyrat won the Acceleration Program Grand Prize for his project Ouat! Vincent Wautelet won the Acceleration Program Prize of the Brussels Capital Region for his project FeasyMotion, Jonathan Rubinstein won the Acceleration Program Audience Award for his project Cocoon,


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Scot Peterson, the campus officer who stayed outside Marjory Stoneman Douglas High School as 17 people were gunned down inside, is speaking publicly for the first time since the massacre.
"I'm never going to get over this, you know. Those were my kids," Peterson in an exclusive "Today" interview.
As the shots rang out inside Marjory Stoneman Douglas High, surveillance video shows Peterson calmly stationed outside.
Peterson said he thought the shots were coming from a sniper outside the building.
"I never believed there was an active shooter inside," he said.
Parents of the victims are speaking out as well, calling Peterson's answers "excuses."
"I want to make sure when this guy refers to the kids as 'his kids' that is not true. Those are our kids and they are always going to be our kids," said Manuel Oliver, father of victim Joaquin Oliver.
Peterson resigned and retired after public criticism a week after the deadly massacre and is now being sued by a parent of a student killed during the Parkland shooting.
Read more: https://nbcnews.to/2sHyhIJ


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Top A Level Biologists compete for the prize
The British Biology Olympiad is an annual competition organised by the Royal Society of Biology, aimed at the top of A Level Biologists. This year there were 7200 entries.
The competition consisits of 90 multiple choice questions testing all areas of Biology, including many topics not taught at A Level, and is designed to challenge the most able students.
Congratulations to the following upper sixth students who have achieved excellent results and have been awarded certificates and medals:
Bronze Medal – Freya Timcke
Silver Medal – Helena Bilsborough


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#19561: I add them before baking so that they roast as well. just garnishing is also nice. this is such a
Posted by: AngAk at 7:16 pm on Dec 14, 2010
good make ahead dish.
Life isn't about waiting for the storm to pass, it's about learning to dance in the rain


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CNC wants to ensure that your cargo arrives at destination in the same condition it left your warehouse. To help with that goal, it's important that you remember that during the voyage, your cargo will be subjected to many things that can create problems if proper care isn't taken.
- Cargo can be in transit for up to several weeks
- Adverse weather conditions, ocean swells, storms....
- Significant temperature variances
Other concerns can be created by:
- Improper packaging for the journey
- Improper container choice
- Incorrect labelling
Shipper/Packer Responsability
Classification – Customs Code
Container Transport Unit (CTU) adapted to transport
Maximum payload authorised referring to CSC plate
Loading - Transport by sea
Cargo must be correctly packed, braced, blocked, lashed and secured into the unit in order to prevent cargo from moving and suffer damages. Rolling up to 45° (heavy weather conditions), gravitational forces up to 3 may take place.
Specific goods with risk
Specific Goods with Risks
Protected Species:
As it's CMA CGM Group policy to comply with all international and local laws and regulations, this also included all those concerning the protection of endangered species of wild fauna and flora.
Waste are materials that are not prime products for which the generator has no further use in terms of his own purposes of production, transformation and consumption, and of which he wants to dispose (Basel Convention, EU regulation…) We recommend our shippers to check local regulations at the port of loading and at the port of discharge in addition to the international regulations.
Dangerous goods:
Some goods which are not dangerous in accordance with the IMDG Code can be hazardous during the sea transport and endangered the crew or cause damages to the vessel. For example coils, stone blocks, out of gauge, break bulk...
Fumigation is a hazardous operation, involving chemical products which can be harmful for human life and environment. A fumigated container remains hazardous IMO Class 9-UNN°3359 until ventilation but the fumigation warning sign affixed to the door remains in place until unstuffing at the final destination.
The carriage of products classified as hazardous and/or hazardous for the environment is forbidden in flexitanks. In fact, this kind of packaging is not listed in the IMDG Code. The container must be clearly identified as containing a flexitank in order to arrange a proper stowage on board. This information should be provided at the time of the booking and a warning sign should be affixed on the container. The main risk of flexitank is the total loss of the content in case of incident (incident could cost around $500 000).


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Happy Sunday.
Another shot from the depths of Emmon's Preserve. Lest you get the wrong idea, the total extent of Emmon's Preserve is maybe 25 acres. It is tiny. Sandwiched in between rural housing areas. In spots, when the leaves are thin, you can see the backyards and hay fields that surround it from the deepest parts.
Still beautiful. And the stream is never the same twice.
Sony DSC H50 at about 85mm equivalent. F3.2 @ 1/100th @ ISO 400. Programed auto.
Just the basic added Clarity and Vibrance, and Landscape sharpen in Lightroom. Cropped slightly at the top to eliminate a bright, distracting highlight.


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On the off chance that you have home loan needs that are outside the regular home loan box, for example, land contributing, at that point hard cash banks might be the solution to your momentary money needs. Be that as it may, is it going to be the best alternative for you? Here's everything you have to think about hard cash credits to settle on an educated decision.
What Is A Hard Money Loan?
Hard cash credits are land advances dependent on the estimation of the insurance you're offering, for example, the property itself, instead of the capacity you need to reimburse the increase to the moneylender. The different sorts of credits include:
• Fix-And-Flip Credit – These advances let a land flipper to purchase a home to fix up quick so it very well may be sold for a benefit and the progress reimbursed
• Bridge Advance – These are expected to enable somebody to purchase a property quick with the objective of renegotiating or exchanging it. They additionally allow somebody to buy another property before they get enough for an upfront installment from the closeout of a house they're as of now attempting to sell.
• Construction Credit – These are for land engineers to rapidly start another development venture with the objective of either selling it fast once complete or renegotiating it.
What Kind Of Properties Can You Buy?
Hard cash credit can be utilized in virtually any kind of property, from single-family homes to land arrangement to business and mechanical properties. You may discover a few Money Lender Singapore who have practical experience in advances for explicit sorts of features.
Most hard cash loan specialists work in a specialty since it's something they've gotten comfortable with. When you converse with a hard cash moneylender, make a point to discover in advance what sorts of advances they're capable or willing to do.
How Hard Money Loans Work?
Hard cash credit is certifiably not an advance accessible to simply anybody. Most moneylenders won't consider giving loans to individuals who aren't land speculators. On the off chance that you figure you might most likely get one for your private home, at that point you may be up to the creek without a paddle.
There are a couple of banks who make hard cash credits to customers. However, that swims into cloudy administrative waters, so most moneylenders stay away from it.
Traditional Vs Hard Money Lenders
If land advances live on a range, at that point toward one side, you have hard cash advances, and on the opposite end, you'll discover conventional, standard mortgages. They're practically perfect inverses of each other. The main thing they share for all intents and purpose is they're issued to purchase genuine property – that is it.
Private associations or people regularly give hard cash advances. They convey altogether different terms than the sort of advances you find at your neighborhood bank.


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chapter 7
18 Pages
Measuring the margins
Women, slavery, and the notarial process in late fourteenth-century Mallorca
This chapter examines women slaveholders and evidence of their activity found in notarial protocols from late medieval Mallorca. It discusses how record keeping often obscured women's commercial activities, reflecting cultural biases that perceived and portrayed them as economically marginal. By analyzing the information found in the component parts of notarial documents, the chapter reveals the importance of women in slave markets and the networks they formed. The discussion reveals the ways in which women were central to day-to-day economic activities in Mallorca.


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The Penny Blacks are a north London 3 piece drawing their influences from Bloc Party, Interpol, The Temper Trap, Pink Floyd etc…
We are looking for a singer with a powerful voice who can lead the band on stage as well as contribute to the creative side of things off stage. We have a 5 song set written (minus lyrics) and are ready to gig as soon as possible!
- Screen name:
- ThePennyBlacks
- Member since:
- Nov 25 2009
- Active over 1 month ago
- Level of commitment:
- Committed
- Years together:
- 1
- Gigs played:
- Under 10
- Tend to practice:
- 2-3 times per week
- Age:
- 40 years
Bloc Party, Interpol, The Temper Trap, Pink Floyd.


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Carter's Splash Toddler Boys' Sandals, Size: 8 T, Blue (Navy)
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Perfect for warm-weather days, these boys' athletic sandals from Carter's offer sporty style. Watch the product video here.Sandal Features Vibrant design Webbing and side cutouts for breathability Sandal Construction Webbing, mesh upper TPR outsole Sandal Details Open toe Double hook and loop closure Padded footbed Size: 8 T. Color: Navy. Gender: Male. Age Group: Kids. Material: Synthetic.
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