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  • 1
    Electronic Resource
    Electronic Resource
    The effects of treading by dairy cows during wet soil conditions on white clover productivity, growth and morphology in a white clover–perennial ryegrass pasture (2005)
    Oxford, UK : Blackwell Science Ltd
    Grass and forage science 60 (2005), S. 0 
    Details
    ISSN: 1365-2494
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Single pugging events, which involve remoulding of the soil around the hooves of livestock during treading, of moderate or severe pugging intensity were imposed in plots in a long-term white clover-ryegrass pasture during spring, by using dairy cows at varying stocking rates (4·5 cows 100 m−2 for 1·5 or 2·5 h respectively). Changes in the growth and morphology of white clover were investigated over the following 12 months. Defoliation at approximately 3-week intervals was carried out by mowing. Annual herbage production was reduced following moderate and severe pugging proportionately by 0·16 and 0·34 compared with the non-pugged control treatment. The corresponding decreases in white clover production were 0·09 and 0·52 respectively. Annual perennial ryegrass production was reduced by 0·37 under severe pugging. Pugging had an immediate adverse effect on growth of white clover which persisted for up to 156 d, and coincided with a large decrease in the proportion of white clover in herbage over the same period (e.g. 0·40 vs. 0·12, in control and severely pugged treatments, respectively, on day 112). In comparison, recovery in ryegrass growth was apparent after 50 d in severely pugged treatments, indicating that white clover is more vulnerable to severe pugging than perennial ryegrass. Analysis of individual white clover plants extracted from turves (300 mm × 300 mm) showed that direct hoof damage, fragmentation and burial of stolons were the major factors which reduced white clover production, rather than the changes in soil physical properties measured. Morphological characteristics associated with plant size (e.g. stolon length, growing points, and leaf numbers) all decreased under pugging. The situation had reversed by late summer, with larger plants dominating pugged plots, and coincided with the recovery of the proportion of white clover in herbage. Strategic pasture management practices, such as restricted grazing and the use of stand-off pads when soils are overly wet, are suggested as means of minimizing treading damage to pasture and reducing negative impacts on the growth and productivity of white clover.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2494.2005.00450.x
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  • 2
    Electronic Resource
    Electronic Resource
    Transfer of fixed nitrogen from white clover to associated grasses in swards grazed by dairy cows, estimated using 15N methods (1991)
    Springer
    Plant and soil 131 (1991), S. 215-223 
    Details
    ISSN: 1573-5036
    Keywords: clover ; grazing effects ; 15N ; nitrogen cycling ; nitrogen fixation ; nitrogen transfer ; Trifolium repens
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Pasture swards containing perennial ryegrass (Lolium perenne L.) alone or with one of five different white clover (Trifolium repens L.) cultivars were examined for production and transfer of fixed nitrogen (N) to grass under dairy cow grazing. Grass-only swards produced 21% less than mixed clover-grass swards during the second year after sowing. Production from grass-only plots under a mowing and clipping removal regime was 44% less than from grass-only plots under grazing. Much of this difference could be attributed to N transfer. In swards without clover, the ryegrass component also decreased in favour of other grasses. The average amount of fixed N in herbage from all clover cultivars was 269 kg N ha−1 yr−1. Above-ground transfer of fixed N to grasses (via cow excreta) was estimated at 60 kg N ha−1 yr−1. Below-ground transfer of fixed N to grasses was estimated at 70 kg N ha−1 yr−1 by 15N dilution and was similar for all clover cultivars. Thus, about 50% of grass N was met by transfer of fixed N from white clover during the measurement year. Short-term measurements using a 15N foliar-labelling method indicated that below-ground N transfer was largest during dry summer conditions.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00009451
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  • 3
    Electronic Resource
    Electronic Resource
    Fate of urine nitrogen on mineral and peat soils in New Zealand (1996)
    Springer
    Plant and soil 178 (1996), S. 141-152 
    Details
    ISSN: 1573-5036
    Keywords: dentrification ; leaching ; lysimeter ; 15N ; ryegrass ; white clover
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract A field lysimeter experiment was conducted over 150 days to examine the fate of synthetic urinary nitrogen (N) applied to peat and mineral soils, with and without a water table. At the start of the winter season, synthetic urine labelled with 15N, was applied at 500 kg N ha−1. Plant uptake, leaching losses and nitrous oxide (N2O) fluxes were monitored. Total plant uptake ranged from 11% to 35% of the urine-N applied depending on soil type and treatment. Plant uptake of applied N was greater in the presence of a water table in the mineral soil. Nitrate-N (NO3 --N) was only detected in leachates from the mineral soil, at concentrations up to 146 μg NO3 --N mL−1. Presence of a water table in the mineral soil reduced leaching losses (as inorganic-N) from 47% to 6%, incrased plant uptake and doubled apparent denitrification losses. In the peat soils leaching losses of applied urine-N as inorganic-N were low (〈5%). Losses of N as N2O were greater in the mineral soil than in the peat soils, with losses of 3% and 〈1% of N applied respectively after 100 days. Apparent denitrification losses far exceeded N2O losses and it is postulated that the difference could be due to dinitrogen (N2) loss and soil entrapment of N2.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00011172
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  • 4
    Electronic Resource
    Electronic Resource
    Nitrogen inputs and losses from New Zealand dairy farmlets, as affected by nitrogen fertilizer application: year one (1996)
    Springer
    Plant and soil 181 (1996), S. 65-69 
    Details
    ISSN: 1573-5036
    Keywords: ammonia volatilization ; denitrification ; grazed pasture ; leaching ; nitrogen ; N2 fixation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Inputs and losses of nitrogen (N) were determined in dairy cow farmlets receiving 0, 225 or 360 kg N ha-1 (in split applications as urea) in the first year of a large grazing experiment near Hamilton, New Zealand. Cows grazed perennial ryegrass/white clover pastures all year round on a free-draining soil. N2 fixation was estimated (using 15N dilution) to be 212, 165 and 74 kg N ha-1 yr-1 in the 0, 225 and 360 N treatments, respectively. The intermediate N rate had little effect on clover growth during spring but favoured more total pasture cover in summer and autumn, thereby reducing overgrazing and resulting in 140% more clover growth during the latter period. Removal of N in milk was 76,89 and 92 kg N ha-1 in the 0, 225 and 360 N treatments, respectively. Denitrification losses were low (7–14 kg N ha-1 yr-1), increased with N application, and occurred predominantly during winter. Ammonia volatilization was estimated by micrometeorological mass balance at 15, 45 and 63 kg N ha-1 yr-1 in the 0, 225 and 360 N treatments, respectively. Most of the increase in ammonia loss was attributed to direct loss after application of the urea fertilizer. Leaching of nitrate was estimated (using ceramic cup samplers at 1 m soil depth, in conjunction with lysimeters) to be 13, 18 and 31 kg N ha-1 yr-1 in a year of relatively low rainfall (990 mm yr-1) and drainage (170–210 mm yr-1). Drainage was lower in the N fertilized treatments and this was attributed to enhanced evapotranspiration associated with increased grass growth. Nitrate-N concentrations in leachates increased gradually over time to 30 mg L-1 in the 360 N treatment whereas there was little temporal variation evident in the 0 (mean 6.4 mg L-1) and 225 (mean 10.1 mg L-1) N treatments. Thus, the 360 N treatment had a major effect by greatly reducing N2 fixation and increasing N losses, whereas the 225 N treatment had little effect on N2 fixation or on nitrate leaching. However, these results refer to the first year of the experiment and further measurements over time will determine the longer-term effects of these treatments on N inputs, transformations and losses.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00011293
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  • 5
    Electronic Resource
    Electronic Resource
    Biological nitrogen fixation in mixed legume/grass pastures (1992)
    Springer
    Plant and soil 141 (1992), S. 137-153 
    Details
    ISSN: 1573-5036
    Keywords: competition with grass ; legume ; methodology ; mixed pasture ; nitrogen fixation ; nitrogen transfer ; review ; soil nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Biological nitrogen fixation (BNF) in mixed legume/grass pastures is reviewed along with the importance of transfer of fixed nitrogen (N) to associated grasses. Estimates of BNF depend on the method of measurement and some of the advantages and limitations of the main methods are outlined. The amounts of N fixed from atmospheric N2 in legume/grass pastures throughout the world is summarised and range from 13 to 682 kg N ha-1 yr-1. the corresponding range for grazed pastures, which have been assessed for white clover pastures only, is 55 to 296 kg N ha-1 yr-1. Biological nitrogen fixation by legumes in mixed pastures is influenced by three primary factors; legume persistence and production, soil N status, and competition with the associated grass(es). These factors and the interactions between them are discussed. Legume persistence, production and BNF is also influenced by many factors and this review centres on the important effects of soil moisture status, soil acidity, nutrition, and pests and disease. Soil N status interacts directly with BNF in the short and long term. In the short-term, increases in soil inorganic N occurs during dry conditions and where N fertiliser is used, and these will reduce BNF. In the long-term, BNF leads to accumulation of soil N, grass dominance, and reduced BNF. However, cyclical patterns of legume and grass dominance can occur due, at least in part, to temporal changes in plant-available N levels in soil. Thus, there is a dynamic relationship between legumes and grasses whereby uptake of soil N by grass reduces the inhibitory effect of soil N on BNF and competition by grasses reduces legume production and BNF. Factors affecting the competition between legumes and grasses are considered including grass species, grazing animals, and grazing or cutting management. Some fixed N is transferred from legumes to associated grasses. The amount of N transferred ‘below-ground”, predominantly through decomposition of legume roots and nodules, has been estimated at 3 to 102 kg N ha-1 yr-1 or 2 to 26% of BNF. In grazed pasture, N is also transferred ‘above-ground’ via return in animal excreta and this can be of a similar magnitude to ‘below-ground’ transfer. Increased BNF in mixed legume/grass pastures is being obtained through selection or breeding of legumes for increased productivity and/or to minimise effects of nutrient limitations, low soil moisture, soil acidity, and pests and disease. Ultimately, this will reduce the need to modify the pasture environment and increase the role of legumes in low-input, sustainable agriculture.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00011314
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  • 6
    Electronic Resource
    Electronic Resource
    Fate of 15N-labelled nitrogen fertilizer applied to kiwifruit (Actinidia deliciosa) vines (1992)
    Springer
    Plant and soil 147 (1992), S. 49-57 
    Details
    ISSN: 1573-5036
    Keywords: ammonium ; field ; kiwifruit ; 15N ; nitrogen fertilizer ; recovery ; soil nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The fate of 15N-labelled ammonium fertilizer applied once to six-year-old field-grown kiwifruit (Actinidia deliciosa ‘Hayward’) vines was measured over three years. The three main treatments were nitrogen (N) applied singularly at 100 or 200 kg N ha−1 in early spring (two weeks before bud burst) or split with 100 kg N ha−1 (unlabelled) in early spring and 100 kg N ha−1 (15N-labelled) ten weeks later. All N treatments were applied to vines with a history of either 50 or 200 kg N ha−1 yr−1. For three years after 15n application, components of the vines and soil (0–600 mm depth) were sampled at harvest in late autumn and the N and 15N contents determined. By the first harvest, all plant uptake of 15N had occurred and this represented 48–53% of the 15N applied. There was no significant effect of current N fertilizer treatment or of N history on 15N recovery by vines. Removal of 15N in harvested fruit was small at 5–6% in the first year and 8% over 3 years. After 2–3 years, most plant 15N occurred in the roots and this component declined only slowly over time. In contrast, there was a large temporal decline in 15N in above-ground plant components due to the annual ‘removal’ in leaf fall and pruning. An associated experiment showed that when 15N-labelled prunings and leaves were mulched and returned to the soil, only about 9% was recovered by plants within 2 years. Almost all remaining mulched material had been immobilised into the soil organic N. In all treatments, about 20% of the added 15N remained in soil at the first harvest. This was almost entirely in organic fractions (〈0.4% in inorganic N) and mostly in the surface 150-mm layer. The 15N content in soil changed little over time (from 20 to 17% between the first and third harvests respectively) and indicated that most of the N had been immobilised into stable humus forms.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00009370
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  • 7
    Electronic Resource
    Electronic Resource
    Influence of time of application on the utilization of nitrogen fertilizer by asparagus, estimated using 15N (1992)
    Springer
    Plant and soil 147 (1992), S. 41-47 
    Details
    ISSN: 1573-5036
    Keywords: asparagus ; Asparagus officinalis ; nitrogen fertilizer ; 15N ; plant uptake ; soil nitrogen fractions ; time of application
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The effect of nitrogen (N) fertilizer on the production of a 6-year-old asparagus (Asparagus officinalis L.) crop was examined over 2 years by the application of 0, 50 or 100 kg N ha−1 as ammonium sulphate at three times; 1) prior to fern growth (9 months before harvest), 2) prior to harvest, or 3) early-harvest prior to the main period of spear production. The utilization of N fertilizer was examined by applying 15N-enriched ammonium sulphate to 2 m×2.5 m microplost within the 50 kg N ha−1 treatments. There was a 12% response in spear production to added N in the first harvest year only and there was no significant effect of rate or time of N application. Plant uptake of added 15N by the end of the first harvest period was 25, 11 and 4% of the total applied for the pre-fern, pre-harvest and early-harvest treatments respectively. About 60% of the 15N applied pre- or early-harvest remained in the soil at the end of the first harvest period. Most of the 15N in soil in the pre-harvest treatment occurred as inorganic N and had been leached into the 150–600 mm soil depth. In contrast, most of the 15N that remained in soil from the early-harvest application was in the 0–75 mm depth and 40% of this had been immobilized into organic N. In the short-term (less than one year), utilisation of 15N-labelled N fertilizer by asparagus was greatest when applied prior to fern growth. However, after 2 years there was no difference between treatments in 15N recovery in plant or soil. Thus, time of application of N fertilizer had no long-term effect on production or utilization of N fertilizer by asparagus.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00009369
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  • 8
    Electronic Resource
    Electronic Resource
    Fate of 15N-labelled nitrogen fertilizer applied to kiwifruit (Actinidia deliciosa) vines (1992)
    Springer
    Plant and soil 147 (1992), S. 59-68 
    Details
    ISSN: 1573-5036
    Keywords: kiwifruit ; 15N ; plant uptake ; remobilisation ; temporal changes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Temporal changes in the nitrogen (N) and 15N content of various components of six-year-old kiwifruit (Actinidia deliciosa ‘Hayward’) vines which had received 15N-labelled ammonium fertilizer were measured. The fertilizer was applied singularly at 100 or 200 kg N ha−1 in early spring (two weeks before bud burst) or split with 100 kg N ha−1 (unlabelled) in early spring and 100 kg N ha−1 (15N-labelled) ten weeks later. All treatments were applied to vines with a history of either 50 or 200 kg N ha−1 yr−1. The N concentration of leaf and fruit tissue was generally lower in the 100 kg N ha−1 treatment than in the 200 kg N ha−1 treatments and this effect was greater than that of N fertilizer history. During the first 8 weeks after bud burst there was a rapid accumulation of N in leaves (ca. 80 kg N ha−1). Analysis of xylem sap at 4 weeks after bud burst revealed that about 60% of the N utilised for new growth was from remobilisation of N stored within the vines and about 40% from soil and fertilizer N. This was unaffected by rate of N application. Plant uptake of added 15N was rapid and almost complete within 10 weeks of application in either early spring or early summer. Initially, most 15N was present in the leaf and root components but these subsequently declined due to translocation into other components of the vine. The decline in leaf 15N coincided with an equivalent accumulation of 15N in the fruit. The 15N enrichment of the ‘annual’ components (leaves, fruit and current-season's shoots) was about twice that of the structural components (one-year-old shoots, cordon, stem and structural roots) during the first year after application. By the third year the 15N concentration of the annual components had declined to similar levels to that of the structural components. These changes were used to estimate the annual throughput of N from soil in vines which received no N fertilizer in years 2 and 3 at 50% of total above-ground N and only 7% in roots. This was equivalent to about 120 kg N ha−1 yr−1. Where fertilizer N (200 kg ha−1) was applied in year 2 the annual throughput of N from soil and fertilizer was about 170 kg N ha−1.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00009371
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  • 9
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    Nitrous oxide emissions from animal urine application on a New Zealand pasture (2007)
    Springer
    Details
    Publication Date: 2007-07-28
    Print ISSN: 0178-2762
    Electronic ISSN: 1432-0789
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Springer
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  • 10
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    Fate of urine nitrogen on mineral and peat soils in New Zealand (1996)
    Springer
    Details
    Publication Date: 1996-01-01
    Print ISSN: 0032-079X
    Electronic ISSN: 1573-5036
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Springer
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