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The effects of treading by two breeds of dairy cow with different live weights on soil physical properties, poaching damage and herbage production on a poorly drained clay-loam soil

SUMMARY There is little empirical evidence to indicate that dairy cow live weight affects the extent of soil damage at the hoof-soil interface during grazing on poorly drained permanent grassland. In the present study the impact of Holstein-Friesian (HF) dairy cows with a mean (±standard deviation) live weight of 570 (±61) kg were compared with Jersey × Holstein-Friesian (JX) with a mean live weight of 499 (±52) kg each at two stocking densities: mean 2·42 ± (0·062) and 2·66 (±0·079) cows/ha. Soil physical properties (bulk density, macroporosity, gravimetric water content, air-filled porosity, penetration resistance and shear strength), poaching damage (post-grazing soil surface deformation and hoof-print depth), herbage yield and milk production were measured throughout 2011 and 2012. Soil physical properties, post-grazing soil surface deformation and herbage production were not affected by dairy cow breed or by interactions between breed and stocking density. Hoof-print depth was higher in the HF treatments (39 v. 37 mm, s.e. 0·5 mm). Loading pressure imposed at the soil surface was the same for both breeds due to a direct correlation between live weight and hoof size. Poaching damage was greater at higher stocking density. Using the lighter JX cow offered little advantage in terms of lowering the negative impact of treading on soil physical properties or reducing poaching damage and no advantage in terms of herbage or milk production compared with the heavier HF cow.


INTRODUCTION
Producing milk from grazed grass on poorly drained soils is an important aspect of agricultural production in temperate regions. Approximately 0·50 (3·4 m ha) of the total land area of Ireland is classified as 'marginal' and affected by natural limitations related to its soil, topography, relief and climate (Gardiner & Radford 1980). The principle limitation of this marginal land is its poor drainage status (Mulqueen 1974;Burdon 1986;Galvin 1987). It has been estimated that 0·46 of Irish farms are on land classified in the Teagasc National Farm Survey as 'limited in agricultural use because of land wetness' . Poorly drained soils typically remain wet for prolonged periods each year, reach saturation during rain events and remain wetter than field capacity for a number of days, even when no further precipitation occurs (Schulte et al. 2005). Farms on such soils have a shorter grazing season, lower proportion of grazed grass in the diet and consequently lower profitability when compared to farms on freedraining soils (Shalloo et al. 2004;Fitzgerald et al. 2008). The shorter grazing season is due to the necessity of keeping cows indoors to avoid excessive soil damage and by lower pasture production (Mullen et al. 1974;Patton et al. 2012).
Soil physical damage caused by cattle treading may involve a reduction in soil porosity with no indication of animal treading at the surface (Herbin et al. 2011). It can also involve a permanent displacement and remoulding of the soil surface around the hoof at higher water contents or a puddled soil under extremely wet conditions (Greenwood & McKenzie 2001;Drewry et al. 2008). Where soil and pasture are damaged there can be a loss in both utilization of the sward and in subsequent pasture production (Drewry et al. 2008;McDowell 2008).
Surface deformation coupled with compaction at depth results in increased soil resistance and reduced pore space (Betteridge et al. 1999;Batey & McKenzie 2006), which affects both shoot and root growth (Cook et al. 1996;Houlbrooke et al. 1997). Plant growth may also be reduced by direct effects of poaching including plant injury, fragmentation and burial (Brown & Evans 1973;Menneer et al. 2005;Phelan et al. 2013a). The resistance of soil to deformation is dependent on soil moisture (Mapfumo & Chanasyk 1998); however, intensively grazed grassland is often situated in regions with high rainfall (Smit et al. 2008). The extent of soil damage in poorly drained soils is dependent on factors that are fixed (soil type and climate) and non-fixed (animal live weight, stocking density and grazing duration). The non-fixed elements may be managed to overcome soil and pasture damage (Scholefield & Hall 1986;Finlayson et al. 2002).
Interest in crossbreeding Holstein-Friesians (HF) with Jersey cattle is fuelled by the inadequate reproductive performance of HF cows in pasture-based systems (Prendiville et al. 2009;Heins et al. 2012). The Jersey × HF (JX) cow is naturally lighter than the HF breed and is perceived to offer an advantage on poorly drained soils by imposing less treading damage during grazing (Herbin et al. 2011). This perceived advantage has not been investigated at a farm scale.
It is hypothesized that the use of lighter JX cows, relative to HF cows, reduces poaching damage and the adverse effects of treading during grazing on soil physical properties under typical grazing management. The objective of the current paper was to investigate the effects of dairy-cow breed (JX v. HF) on: soil surface loading pressures, soil physical properties [bulk density (BD), macroporosity (MP), gravimetric water content (GWC), air-filled porosity (AFP), penetration resistance (PR) and shear strength (SS)] and poaching damage [post-grazing soil surface deformation (SSD) and hoof-print depth (HPD)] in the upper layers of a clay-loam soil under locally typical grazing management practices on poorly drained soil. The effects on herbage production and on milk production were also examined. Total nitrogen (N) inputs and uptake are presented to provide a context for herbage production data.

Site description
The present study was conducted at Solohead Research Farm (52 ha) in Ireland (52°30′N, 08°12′ W, 95 m a.s.l.) during 2010, 2011 and 2012. Average annual rainfall over the previous 10 years was 1018 mm, with potential evapotranspiration of c. 510 mm. Soils are predominantly poorly drained Gleys (0·90 of the farm) and grey brown podzolics (0·10) of clay-loam texture with a perched water table, 0·0-2·2 m below ground level (Necpalova et al. 2012). The farm was drained in the 1960s and 1990s with deep open drains controlling water table depth. Nevertheless, much of the farm remains seasonally waterlogged. The farm has been under permanent grassland for at least 50 years.

Experimental treatments and design
The experiment was set up during 2010. In spring 2010 an experimental area of 38·4 ha was divided into six blocks, each with uniform soil type and drainage status. Each block was divided into four paddocks. There were two breeds of dairy cow: (1) HF with an average live weight of 570 kg (S.D. = 61 kg), and (2) JX with an average live weight of 499 kg (S.D. = 52 kg). During 2010 two paddocks in each block were randomly assigned to HF and the other two to JX. Paddocks assigned to each breed treatment were rotationally grazed by herds of 48 cows of each breed during the 2010 grazing season (1 February to 16 December) and surplus herbage was removed as silage. The mean effective annualized stocking rate of both breeds during 2010 was 2·52 cows/ha. The milk yield capacity of both breeds was ascertained during 2010 and used to determine the stocking density treatments to be imposed during 2011 and 2012.
In 2011 and 2012, two stocking densities of each breed were imposed in a randomized block design with two factors and six replicated blocks. Annual stocking densities are presented in Table 1. In spring 2011 and 2012, all cows of each breed were divided into groups on the basis of lactation number (1, 2, 3 and ⩾4) and then sub-divided into subgroups of two on the basis of calving date. From Dairy cow live weight effect on soil during grazing within each sub-group, one cow was randomly assigned to each stocking density treatment. The experiment consisted of 96 dairy cows (48 HF and 48 JX) in 2011 and 100 dairy cows (50 HF and 50 JX) in 2012. Mean calving date was February 28 (S.D. = 26 days).The four herds were identified as HF-low stocking density (HF-L), HF-high stocking density (HF-H), JX-low stocking density (JX-L) and JX-high stocking density (JX-H). Herds were assigned to paddocks each spring. Paddocks assigned to HF were grazed only by HF during 2010, 2011 and 2012 and likewise for JX. Paddocks grazed by HF-L in 2011 were again grazed by HF-L in 2012 and likewise for the other treatments.

Grazing management
Cows were turned out to graze 3 days after calving from early February and remained at pasture until they were housed full-time, typically at the end of November. Exceptions were made when ground conditions were too wet (soil moisture >0·60 m 3 /m 3 ) or when herbage Excess herbage was identified throughout the experiment and removed for silage production. These areas were selected when herbage growth rates exceeded demand, resulting in pre-grazing herbage mass >2000 kg of DM/ha (above post-grazing height of 40 mm). The entire area of each system was available for grazing during the spring and autumn. Silage areas were closed off between early-April and mid-June (first-cut silage) or between mid-June and mid-July (second-cut silage). The land area available for grazing in each system at various times of the year and associated stocking densities are outlined in Table 1.
Annual fertilizer N input was 110 kg/ha on the low stocking-density paddocks (HF-L and JX-L), which also relied on biologically fixed N facilitated by white clover in the sward, and 280 kg/ha on the high stocking-density systems (HF-H and JX-H), to cater for the increased grazing demand (Humphreys et al. 2008). Fertilizer N was applied in the form of urea between February and April and as calcium ammonium nitrate from May to September. Slurry produced during housing was stored and applied back equally to each treatment (Table 1).

Concentrates and silage fed
Cows received concentrate feed (0·26 barley, 0·26 maize gluten, 0·35 beet pulp and 0·12 soybean meal) at rates of 3-5 kg/cow/day from February to April and between 0 and 4 kg/cow/day from April to November, depending on herbage availability and nutritive value. When housed, cows were fed grassclover silage ad libitum.

Meteorological data
Weather data [temperature (°C), relative humidity (g/kg), rainfall (mm), wind speed (m/s) and direction (°) and solar radiation (J/m 2 )] were measured and recorded on site by an automated weather station (Campbell Scientific Ltd., Loughborough, UK) every 15 min. Daily data collected (rainfall, maximum and minimum air temperature, wind speed and solar radiation) were used as inputs to the model of Schulte et al. (2005) to estimate daily evaporation, effective drainage and soil moisture deficit (SMD).

Herbage production and white clover content
Exclusion plots were set up in four paddocks of each treatment. Each plot was 11 × 2·5 m and was positioned centrally in each paddock. Cows were prevented from walking or grazing in the plot by electrified wire. Exclusion plots were moved three times each year (February, May and July) to an adjacent area in the paddock, which had been subject to treading on previous grazing rotations to take account of the effect of treading on herbage yields.
Herbage yield was measured by cutting a 10 × 1·2 m strip in each exclusion plot prior to each grazing or silage cut using an Etesia Hydro 124DS Lawnmower (Etesia UK Ltd., Shenington, Oxon, UK) at a cutting height of 40 mm above ground level. The harvested herbage was weighed to determine herbage mass. A 100 g sub-sample was collected and then dried in a force-draught oven for 16 h at 100°C to determine DM content. Annual herbage yield (kg of DM/ha) was calculated as the sum of herbage removed as pre-grazing and pre-silage cuts.
A second 100-g sub-sample of herbage was freezedried and milled through a 0·2 mm sieve before analyses for ash content (550°C muffle furnace for 12 h), crude protein (CP; N content; Leco 528 auto-analyser, Leco Corp., St. Joseph, MI, USA) and in vitro organic matter digestibility (OMD) as described by Morgan et al. (1989). Silage fed was sampled throughout the experiment by taking grab samples of 100 g before feeding. These were analysed for ash, OMD and CP using near-infrared spectroscopy (model 6500, Foss-NIR System, Hillerod, Denmark).
Pasture cover was measured on a weekly basis in all paddocks to estimate weekly herbage growth using a Filips rising plate meter (Grasstec, Mallow, Cork, Ireland). Each week 40-60 compressed sward height (CSH) measurements were taken diagonally across each paddock. The average herbage mass above a cutting height of 40 mm was then calculated according to the following formula: Herbage mass = [Mean CSH (mm)−40 mm] × sward density; kg DM/mm/ha, assuming a sward density of 24 kg DM/mm/ha. Annual herbage production was calculated as the sum of weekly herbage growth throughout the year.
The proportion of white clover (Trifolium repens L.) in herbage in each paddock was measured using the methodology described by Phelan et al. (2013b).

Total nitrogen input and uptake
Total N input to the treatments was made up of fertilizer N, N applied in slurry, biologically fixed N from white clover and N deposited by grazing cows. The biologically fixed N in stolons, roots and stubble in each paddock was estimated from white clover content in the sward and herbage production using a mechanistic model as described by Humphreys et al. (2008). Nitrogen excretion by the dairy cows was estimated as the difference between intake of N and N deposited in milk, in calves or in live weight change of the cows and ammonia losses (Humphreys et al. 2008). Nitrogen uptake was calculated from the mean annual N content of harvested herbage in each system and its respective annual herbage yield.

Length of the grazing season, concentrates fed and intake estimate
The length of the grazing season was measured in terms of days at pasture where 1 day was defined as when all the cows per system were out day and night and one-half day when cows were out only by day. In spring when lactating cows were outdoors and cows yet to calve remained indoors, the proportion of cows outdoors was recorded. Likewise, when cows were being housed as they were dried off in the early winter the proportion of cows outdoors per system was recorded.
The amount of concentrate fed per cow was recorded at each milking (Dairymaster, Causeway, Co. Kerry, Ireland) and silage intake during housing was estimated as silage fed to cows minus rejected material. Intake of grazed pasture DM by each cow was estimated as the difference between net energy (NE) provided from silage and concentrate and that needed to meet the NE requirements for milk production, maintenance and pregnancy (Jarrige et al. 1986;Jarrige 1989;O'Mara 1996).

Milk yield and composition
Milking was conducted at 07·30 h each morning and 15·30 h each evening. Milk yield per cow (kg) was recorded at each milking and milk composition (fat, protein and lactose concentrations) from each cow was measured twice weekly on a successive morning and evening milking using a Milkoscan 203 (Foss Electric DK-3400, Hillerød, Denmark). Solidscorrected milk yield was calculated using the equation of Tyrell & Reid (1965).

Soil properties
Soil samples were collected using a soil sampling ring kit and stainless steel cores having a volume of 9·82 × 10 −5 m 2 (Eijkelkamp, Agrisearch Equipment, Giesbeek, The Netherlands), from the layer at 0·05-0·10 m below ground level and at 0·15-0·20 m below ground level. Nine locations per paddock were selected at random in each of four paddocks per treatment within four replicate blocks at the start of the experiment (February 2011). The global positioning system (GPS) coordinates of each location was recorded. Soil cores at each depth were collected on four occasions (February, May, August and November) each year.
Soil BD (mass of soil per unit volume, kg/m 3 ), MP [proportion of soil volume occupied by pore spaces >30 μM in diameter (Drewry et al. 2008), m 3 /m 3 ], gravimetric water content (GWC, mass of water per mass of soil, g/g) and AFP (proportion of pore space occupied by air, m 3 /m 3 ) were measured using standard methods Phelan et al. 2013a) A plasticity index test (British Standards Institute 1990) to determine Atterberg limits was conducted on two bulk soil samples (Metlab Ltd, Ballygarvan, Cork, Ireland). One sample was collected from each of two depths, 0·00-0·10 m and 0·10-0·20 m, at a randomly selected location in each paddock in March 2012; samples were then bulked for each depth.

Soil strength
Soil PR (resistance of the soil to penetration by a cone, per unit area of the cone's base, in Mpa) was measured using a penetrologger (Eijkelkamp, Agrisearch Equipment, Giesbeek, The Netherlands). Shear strength (the magnitude of shearing stress that a soil can sustain in kPa) was measured using a standard shear vane (Eijkelkamp, Agrisearch Equipment, Giesbeek, The Netherlands). Ten measurements (Bengough et al. 2001) of each were taken in the vicinity of the locations described above in four paddocks 1428 P. Tuohy et al.
per treatment within four replicate blocks on four occasions annually (January, April, July and October). The PR was measured to a depth of 0·30 m below ground level and averaged over 0.05 m intervals to a depth of 0·30 m for each treatment for analysis. These measurements will be referred to as PR5 (mean PR at 0·00-0·05 m depth), PR10 (mean PR at 0·06-0·10 m depth) and so on. The SS was determined at depths of 0·05, 0·10 and 0·15 m below ground level.
The soil volumetric moisture content (SVMC) was measured simultaneously with PR and SS measurements: SVMC in the upper 0·05 m of soil was measured using an ML2× soil moisture measurement kit (Delta-T Devices Ltd, Burwell, Cambridge, UK) at 20 locations in the vicinity of the PR and SS measurements.

Poaching damage
Soil surface deformation (m/m) provided a standardized quantitative method of determining the rate of poaching damage. It was measured by fitting a 2-m long chain to the soil surface, taking account of any changes in micro-topography. The profile length of the chain was measured against a 2-m long wooden staff. Deformation was quantified as the reduction in the chain's profile length relative to the staff (Saleh 1994;Nie et al. 2001;Phelan et al. 2013a). Hoofprint depth (mm) was measured with callipers. Soil surface deformation and HPD were recorded immediately after each grazing in each paddock. On each occasion two locations were selected at random in the most recently grazed section of the paddock. At each location two SSD measurements and ten HPDs were recorded. The SVMC was recorded simultaneously with SSD and HPD; ten measurements were taken at each location using the ML2× soil moisture measurement kit as described above.

Cow live weight and body condition score
The live weight of each cow was recorded fortnightly using weighing scales and the Winweigh software package (Tru-Test Limited, Auckland, New Zealand). Body condition score (Edmonson et al. 1989) of each dairy cow was recorded once a fortnight.

Hoof surface area and surface loading pressure
In October 2012, all cows of each breed were divided into four main groups on the basis of lactation number (1, 2, 3 and ⩾4). From within each group, 0·4 of the total number of cows were selected at random for hoof size measurement. The surface area of the back left hoof of this subset (n = 20 for each breed) was measured and taken to represent the average surface area of hooves of cows in each treatment. Static surface loading pressure (kPa) was calculated as the mass of the cow (kg) divided by the total hoof area (m 2 ), multiplied by 100.

Statistical analysis
Cow hoof size and live weight were analysed as a single factor (breed) analysis of variance (ANOVA) having 48 or 50 replicates. Static loading pressure was analysed by ANOVA with only breed as a factor with 20 replicates. All other animal production data (milk production, milk composition, cow live weight, body condition score, diet and management) were analysed as a three factor (year × breed × stocking density) ANOVA with 24 or 25 replicates. Herbage production data were analysed as a three factor (year × breed × fertilizer regime) ANOVA, with four replicates for the method using exclusion plots and six replicates for the method using growth rates. Clover content was analysed as a four factor (year × season × breed × fertilizer regime) ANOVA with six replicates.
Soil data (BD, MP, GWC, AFP, PR and SS) were analysed as two factor (breed × stocking density) ANOVA examining the main effects of factors and interactions between factors, with four replicates. The SSD and HPD data were analysed by ANOVA including year, breed and stocking density, with four replicates. The significance of any correlations within the results was analysed with linear regression through the analysis of covariance in the PROC MIXED procedure in SAS version 9.1.3 (SAS Institute 2006).

Rainfall and soil moisture deficit
Annual rainfall was 1318 mm in 2011 and 1131 mm in 2012. In both years rainfall was above the mean of the previous 10-year period (1018 mm; range 797-1296 mm), (Fig. 1(a)). In 2011 the three wettest months were February, November and December. Both November and December 2011 each had higher monthly rainfall than that recorded in any month in the previous 10 years. These three months accounted for 678 mm of rainfall (or 0·51 of annual rainfall in 2011). During the period 1 March to 31 October 2011, rainfall was 588 mm compared to the 10-year average of 640 mm. In 2012, rainfall was concentrated in the summer months with double the 10-year average for the 3-month period encompassing June, July and August; 469 v. 235 mm. During the period 1 March to 31 October 2012 rainfall was 784 mm.
Mean annual SMD was 4·5 mm/day in 2011 and -3·9 mm/day in 2012. Saturated soil conditions (SMD = -10 mm) occurred on 73 days in 2011 and 88 days in 2012 while there was excess soil water above field capacity (SMD < 0 mm) on 179 days in 2011 and 285 days in 2012 ( Fig. 1(b)).
Herbage production and white clover content Herbage production was not significantly affected by breed or interactions between breed and the other factors. Herbage production was greater (P < 0·01) at higher N input. Annual herbage yield was higher (P < 0·001) in 2011 than 2012 (14 334 v. 11 954 kg/ha, S.E. 285·5 kg/ha, Table 2). Clover content in herbage DM was not affected by breed, N input or interactions with breed or N input. Clover content in herbage DM was higher (P < 0·001) in 2011 than 2012 (0·271 v. 0·154, S.E. 0·0094). Mean clover herbage DM yield across systems was 3843 kg/ha in 2011 and 1762 kg/ha in 2012 (Table 1).

Total nitrogen input and uptake
Total N input (including fertilizer, N applied in slurry, biologically fixed N and N deposited by grazing cows) in the low fertilizer N treatments was 549 and 494 kg/ha in 2011 and 2012, respectively. In the high fertilizer N treatments total N input was 662 and 625   Table 1).
Length of the grazing season, concentrates fed and intake estimate The total number of days grazing in each system is shown in Table 1. The JX had an earlier mean calving date than the HF. This impacted significantly (P < 0·01, S.E. 0·91 days) on the number of grazing days with 212·5 days/cow for HF and 216·8 days/ cow for JX. The number of grazing days was not affected by stocking density treatment. The grazing season was longer (P < 0·001) in 2011 than in 2012 (232 v. 198 days/cow; S.E. 0·91). The amount of concentrates fed per cow did not differ between breeds or between stocking density treatments. On average cows received 495 kg of concentrates in 2011 and 855 kg in 2012 (P < 0·001, S.E. 6·0 kg). Table 1 presents estimates of grazed pasture and silage intake and measured concentrate intakes per cow (kg DM/cow).

Soil properties
Soil properties BD, MP, GWC and AFP at the 0·05-0·10 m depth range were not affected by breed, stocking density or interaction between breed and stocking density. All soil properties measured showed strong correlations with GWC across treatments. Mean AFP Table 2. The effect of dairy cow breed (Holstein-Friesian and Jersey × Holstein-Friesian), annual fertilizer N input (low = 110 kg/ha supplemented by biologically fixed N from clover in the sward, high = 280 kg/ha) year, on annual herbage production (kg/ha) by two methods Dairy cow live weight effect on soil during grazing at 0·05-0·10 m depth across treatments was 0·17 m 3 / m 3 (ranging from 0·11 to 0·23 m 3 /m 3 ) in 2011 and 0·12 m 3 /m 3 (ranging from 0·09 to 0·17 m 3 /m 3 ) in 2012. Measurements taken at the 0·15-0·20 m depth range showed similar responses in BD, MP, GWC and AFP as those at 0·05-0·10 m. The treatments imposed did not have an effect on these soil properties at the 0·15-0·20 m depth range.

Soil strength
Penetration resistance at all depths up to 0·25 m was not affected by cow breed, interaction between breed and stocking density, or stocking density. The PR30 was not affected by breed but was higher (P < 0·05) at the low stocking density than the high stocking density (2·51 v. 2·05 Mpa, S.E. 0·117 Mpa). Breed, interaction between breed and stocking density or stocking density had no effect on soil SS at any depth.

DISCUSSION
Rainfall, nitrogen input and herbage production Rainfall was above average in both years of the study. However, due to the rainfall patterns observed, ground conditions were drier than normal during the main grazing season in 2011 and substantially wetter than average in 2012.
Total N input estimates show that N available in different treatments was not solely dependent on the N fertilizer application rate. Those paddocks receiving less fertilizer N were augmented by biologically fixed N from white clover in the sward. Biologically fixed N was estimated to have contributed an extra 78 kg/ha in 2011 and 44 kg/ha in 2012 to the low fertilizer N systems. The higher N excesses in the high fertilizer N treatments relative to the low fertilizer N treatments indicate that although there was more N available in the high fertilizer N treatments a lower proportion was utilized for herbage production when compared to the low fertilizer N treatments. A similar result was attributed to low efficiency of fertilizer N use under high rainfall, probably due to high rates of denitrification (Humphreys et al. 2008).
Herbage production and the length of the grazing season were dependent on N input, weather and soil conditions. Due to excessively wet soils and poor herbage growth rates, cows were housed frequently during the 2012 grazing season. The total length of the grazing season was much less than in 2011, when housing during the grazing season was not necessary. Consequently, due to the lower amount of grazed grass in the diet, there was higher demand for silage and concentrate in all systems in 2012 than in 2011.
Poor conditions for herbage production prevailed in 2012. Optimum AFP for pasture production is in the range of 0·15 and 0·20 m 3 /m 3 (Drewry et al. 2008); with a critical minimum value of 0·10-0·12 m 3 /m 3 required to ensure adequate diffusion of air to plant roots (Lipiec & Hatano 2003). During 2012, mean AFP at 0·05-0·10 m depth across treatments was Fig. 3. Relationship between cow live weight and total hoof area for HF (.) and JX (○) cows. HF cows are heavier (P < 0·001) and have larger hoofs (P < 0·001) than their JX equivalents. It is assumed that air movement to the plant roots was restricted at these levels, thus restricting herbage production. In 2011, AFP was higher throughout the grazing season and only fell below the optimum level in November.

Milk yield and composition
The results show no difference in yield of solidscorrected milk, fat and protein per cow between breeds. Similar comparisons between Holstein-Friesian and Jersey × Holstein-Friesian cows concur with these findings (Prendiville et al. 2009;Xue et al. 2011;Vance et al. 2013).

Effect of treading on poaching damage
While there was no effect of breed on SSD and only a slightly higher HPD imposed by HF cows, there was a clear difference in poaching damage between the stocking density treatments, particularly in 2012. This difference is due to the effect repeated loading had on soil strength. A higher stocking density resulted in a greater frequency of hoof-soil interactions and a higher amount of surface damage, which was further exacerbated by wet conditions. The repeated treading of wet soil increases the depth to which the soil is weakened (Mullins & Fraser 1980). Thus partly poached soil is more susceptible to subsequent poaching as it is softer and wetter (Gradwell 1968). This process may also account for some of the difference in HPD recorded between breeds during the experiment.
Since an HF hoof is 1·17 times larger than a JX hoof, HF treaded on 0·17 more of the pasture area than JX at each grazing. While the loading pressure is the same, the intensity of loading is increased, in much the same way as the intensity of hoof-soil interactions is increased with higher stocking rate. The higher poaching damage in 2012 was due to the soil being above its plastic limit throughout the grazing season. The plastic limit of a soil is the GWC at which a soil changes from being friable to being plastic, and represents the lowest water content at which pugging and poaching may occur (Drewry et al. 2008). Analysis of the soil at 0·00-0·10 m depth, found the plastic limit was 0·43 g/g GWC. In 2011 this threshold was not breached until November when mean GWC was 0·51 g/g. Soil samples taken in 2012 show soil GWC was continually well above the plastic limit, ranging from 0·56 (August) to 0·68 (November) g/g. In this scenario soil deformation was the dominant effect of treading during grazing.
Soil surface loading characteristics of dairy cattle The soil surface loading pressure of a grazing animal is a function of the live weight and hoof size as well as the loading pattern during ambulation. The lowest magnitude of loading is applied by a stationary animal and is taken as the total live weight divided by the total contact hoof area. Greater pressures are evident when the animal is walking or running as not all hooves are in continuous contact with the soil surface and as such the live weight is distributed over a smaller contact area (Willatt & Pullar 1984;Greenwood & McKenzie 2001). For practical purposes it is assumed that the dynamic load of a moving cow is approximately twice that of an equivalent stationery cow (Scholefield & Hall 1985;Piwowarczyk et al. 2011).
It has been shown that no differences exist between the breeds used in the present study in terms of grazing time, number of grazing bouts and grazing bout duration in an intensive, seasonal grass-based system (Prendiville et al. 2010). Hence, the principle difference between the breeds was in live weight. The hoof size measurement methodology allowed for the likely increase in size with increasing age (Hahn et al. 1984;Boelling & Pollott 1998) by selecting a representative group on the basis of lactation number. Both breeds exhibited similar static pressures and, hence, similar dynamic pressures. While it is hypothesized that the lighter cow has less potential to cause damage, it has been shown that pressure applied is the same regardless of live weight. Surface loading pressure, not live weight, was the factor most affecting the soils response to treading.

CONCLUSIONS
In general post-grazing soil physical properties and poaching damage were not influenced by dairy-cow breed, with only HPD being significantly affected by breed. Herbage production and milk production in terms of yield of milk fat and protein were not different between breeds. Therefore there was no advantage, in terms of lowering the negative impact of treading on soil physical properties or reducing poaching 1434 P. Tuohy et al.
damage, in using the lighter JX cow rather than the heavier HF cow as a tactic to optimize production from poorly drained grassland soils. Lack of differences between the breeds was due to the correlation between body weight and hoof size, which was common to both breeds, hence the static pressure exerted at the soil surface was the same regardless of breed.