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  • 1
    Electronic Resource
    Electronic Resource
    Nitrogen cycling involving non-exchangeable ammonium in a gray luvisol (1998)
    Springer
    Biology and fertility of soils 27 (1998), S. 425-429 
    Details
    ISSN: 1432-0789
    Keywords: Key words Nitrogen cycling ; Non-exchangeable ammonium ; Ammonium fixation ; Cropping systems ; Gray luvisol
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  There is considerable interest in determining the bio-availability of non-exchangeable NH4 + (NEA) because it constitutes nearly 10% of the total N in the top 1 m of soil. NEA is NH4 + present in the soil that is not extractable with neutral K salt solutions, e.g. 1M KCl. This study was conducted in 1994 and 1995 to quantify the amount of NEA released by a gray luvisolic clay loam soil in Alberta, Canada, during the growing season. Replicated plots under: (1) continuous bromegrass, (2) continuous barley, and (3) barley since 1991 but previously under a continuous forage legume, were sampled four times through the growing season to a depth of 80 cm. The first sampling was done before seeding of barley. Cropping systems and their interaction with time of sampling had no effect on NEA. The NEA-N pool in the soil decreased significantly during grain-filling and maturing of barley, and had returned to approximately its initial level by the following spring. The maximum amount of NEA-N released was 15 g m–2 at barley grain-filling in 1994, and 10 g m–2 3 weeks after barley had matured in 1995. Approximately 24% of the released NEA accumulated as 1M-KCl-extractable NH4 + in 1994, 20–30% was absorbed by the barley crop, and most of the remainder was probably assimilated by soil micro-organisms and immobilized in soil organic matter. The release of significant amounts of NEA during crop growth has implications for N cycling and measurements of mineralization/immobilization turnover rates.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003740050453
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  • 2
    Electronic Resource
    Electronic Resource
    Effects of cropping systems on nitrogen, phosphorus and potassium forms and soil organic carbon in a Gray Luvisol (1996)
    Springer
    Biology and fertility of soils 22 (1996), S. 184-190 
    Details
    ISSN: 1432-0789
    Keywords: Cropping systems ; Soil organic matter ; Nitrogen ; Phosphorus ; Potassium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The effects of up to 23 years of agricultural cropping of a boreal forest soil on soil organic carbon (SOC) and N, P, and K pools were studied. The cropping systems studied were: (a) continuous barley, (b) continuous forage bromegrass, (c) continuous forage legume, and (d) barley/grass-legume forage rotation. Continuous bromegrass increased while other cropping systems decreased SOC in the surface soil. Kjeldahl N in soil approximately followed the trend in SOC. The net gain in N under continuous grass was attributed mostly to nonsymbiotic N fixation. Changes in SOC content appeared to be also influenced by cropping and tillage frequencies. Changes in fixed (intercalary) ammonium were small. There was no measurable change in total P, in part, because input was only slightly higher than crop offtake. Organic P increased under continuous bromegrass, and tended to decrease under continuous legume. The C/N and C/P ratios of soil organic matter decreased slightly with cropping. Exchangeable K (Kex) was decreased by cropping systems containing a legume crop to a greater extent than those without a legume crop. Most of the decrease occurred in the 0–15 cm depth. Nitric acid extractable K was not affected by cropping. Since net loss of Kex to 30 cm depth was substantially less than crop offtake, it is suggested that subsoil K reserves and matrix K were supplying a major portion of the crops' K requirement. It is concluded that the effects of cropping systems on SOC, N, P and K are influenced by crop type, and cropping and tillage frequencies.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00384453
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  • 3
    Electronic Resource
    Electronic Resource
    Effects of cropping systems on nitrogen, phosphorus and potassium forms and soil organic carbon in a Gray Luvisol (1996)
    Springer
    Biology and fertility of soils 22 (1996), S. 184-190 
    Details
    ISSN: 1432-0789
    Keywords: Key words Cropping systems ; Soil organic matter ; Nitrogen ; Phosphorus ; Potassium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The effects of up to 23 years of agricultural cropping of a boreal forest soil on soil organic carbon (SOC) and N, P, and K pools were studied. The cropping systems studied were: (a) continuous barley, (b) continuous forage bromegrass, (c) continuous forage legume, and (d) barley/grass-legume forage rotation. Continuous bromegrass increased while other cropping systems decreased SOC in the surface soil. Kjeldahl N in soil approximately followed the trend in SOC. The net gain in N under continuous grass was attributed mostly to nonsymbiotic N fixation. Changes in SOC content appeared to be also influenced by cropping and tillage frequencies. Changes in fixed (intercalary) ammonium were small. There was no measurable change in total P, in part, because input was only slightly higher than crop offtake. Organic P increased under continuous bromegrass, and tended to decrease under continuous legume. The C/N and C/P ratios of soil organic matter decreased slightly with cropping. Exchangeable K (Kex) was decreased by cropping systems containing a legume crop to a greater extent than those without a legume crop. Most of the decrease occurred in the 0–15 cm depth. Nitric acid extractable K was not affected by cropping. Since net loss of Kex to 30 cm depth was substantially less than crop offtake, it is suggested that subsoil K reserves and matrix K were supplying a major portion of the crops‘ K requirement. It is concluded that the effects of cropping systems on SOC, N, P and K are influenced by crop type, and cropping and tillage frequencies.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00384453
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  • 4
    Electronic Resource
    Electronic Resource
    Effect of long term cropping on availability of Cu, Mn and Zn in soil following clearing of a boreal forest (1994)
    Springer
    Plant and soil 160 (1994), S. 157-160 
    Details
    ISSN: 1573-5036
    Keywords: boreal forest ; copper ; DTPa ; luvisol ; manganese ; zinc
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Temporal changes in labile soil Cu, Mn and Zn were measured for up to 23 years after conversion of a boreal forest to the following crop production systems: (i) continuous barley, (ii) continuous legume and (iii) continuous bromegrass for hay, and (iv) barley/legume-bromegrass hay rotation. Decreases in labile Mn and Zn were greater than can be accounted for by crop offtake except for the continuous grass treatment. Some Mn and Zn was probably converted to less labile forms due mostly to reduction in soil organic matter associated with soil cultivation and some cropping systems. Labile copper was increased slightly with time under agriculture.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00150358
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  • 5
    Electronic Resource
    Electronic Resource
    Nutrient uptake by barley roots under field conditions (1988)
    Springer
    Plant and soil 109 (1988), S. 171-179 
    Details
    ISSN: 1573-5036
    Keywords: Black Solod ; inflow ; magnesium ; nitrogen ; phosphorus ; potassium ; root efficiency
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract A field study with barley was conducted in 1984 and 1985 to provide data on uptake rates of N, P, K and Mg and their variation as the growing season progressed. Two varieties were grown: Galt in 1984 and Otal in 1985. Soil fertility was maintained at or near optimum conditions. Samples were obtained approximately every 10 days for shoot dry weight, nutrient content and root length measurements. The approximate method (Williams, 1948) traditionally used for calculating uptake rates was found to be invalid for most of the nutrients studied. The method used for measuring uptake rates was the functional approach proposed by Hunt (1973). Inflow,i.e. uptake rate per unit root length, of plant nutrients, decreased with time. However, maximum uptake rates measured in kg ha−1d−1 occurred at about 50 days from sowing because of increasing root length density with time. Inflow or uptake rates were low in 1985 because of moisture deficiency, and grain yield (0.89 t ha−1) was severely depressed. This study demonstrated that Hunt's method is superior and more advantageous than the traditional, approximate method.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02202081
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  • 6
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    Plant Competition Effects on the Nitrogen Economy of Field Pea and the Subsequent Crop (2004)
    Wiley
    Details
    Publication Date: 2004-01-01
    Print ISSN: 0361-5995
    Electronic ISSN: 1435-0661
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Wiley
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  • 7
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    Straw removal increases the light fraction and mineralizable C and N compared with moldboard ploughing (2007)
    Canadian Science Publishing
    Details
    Publication Date: 2007-01-01
    Description: An earlier study indicated that cereal straw may be removed after harvest without affecting crop production, soil organic matter and microbial biomass. Further measurements of early indicators of changes in soil organic matter, viz., the light fraction and mineralizable C and N, confirm that straw removal is superior to straw incorporation with moldboard ploughing, and comparable to straw incorporation by disking, in C and N retention and turnover. Key words: Carbon, light fraction, mineralization, nitrogen, straw management
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Canadian Science Publishing
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  • 8
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    Recovery of chemical and physical properties of boreal plain soils impacted by pipeline burial (2000)
    Canadian Science Publishing
    Details
    Publication Date: 2000-08-01
    Description: Pipeline construction on the Canadian boreal plain occurs on woodland and/or agricultural fields, but soil recovery from its impact is not well documented. Therefore, we quantified changes over 3 yr (1992 to 1994) in the chemical properties of two Grey soils and the physical properties of a Grey soil that were subjected to pipeline burial and cropped to barley. The pipeline right-of-way (RoW) was divided into three zones: a road (or work) area used for vehicular traffic, a trench area for burying pipeline, and a pile (or spoil) area where soil was stockpiled during excavation. Pipeline construction resulted in mixing of subsoil material with topsoil, and the chemical properties most affected were those that varied most with depth. The pH, electrical conductivity, soluble sulphate, and exchangeable Ca and Na were increased in the surface 20 cm of soil, particularly the road and trench areas. The affected properties moderated 2 or 3 yr after pipeline construction as soluble components were dissolved or dispersed and translocated back to lower soil depths. The RoW zones had increased soil strength and compaction, and reduced water retention and infiltration rates. However, the deterioration in soil physical condition was similar across the RoW zones, indicating that it was due mainly to land clearing, a requirement to convert woodland to agricultural land. Improvement in bulk density, and water infiltration and retention in 1993 and 1994 indicated that the RoW was undergoing rehabilitation with time as a result of natural processes and annual cropping. Key words: Chemical properties, exchangeable cations, sulphate, physical properties, soil-water, pipelines
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Canadian Science Publishing
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  • 9
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    Nitrogen supply of a Dark Brown Chernozem soil and its utilization by wheat (2006)
    Canadian Science Publishing
    Details
    Publication Date: 2006-05-01
    Description: Environment and management effects on the N supply to crops are not well understood. We assessed the influence of tillage system (conventional tillage or no-till), N fertilizer (0 or 60 kg N ha-1) and year on N sources and supply of a Dark Brown Chernozem loam soil, and N utilization by spring wheat (Triticum aestivum L.) in 2 yr. The main N source was mineralized N; only 14–23% of wheat N was derived from fertilizer, and non-exchangeable ammonium made no measurable contribution. Soil NO3 and exchangeable NH4 content at sowing and net N mineralization during the growing season (Nmin) were influenced more by year than by N addition and tillage. Nmin was 90–100 kg N ha-1 in 1999, a moist growing season but only 21–39 kg N ha-1 in 2000, a drier year. In both years, soil inorganic N to 60 cm at sowing averaged about 60 kg N ha-1 of which half was N mineralized since the previous harvest. Year accounted for 65–81% of the variation in N uptake. Fertilization increased N uptake and wheat yields, especially in 2000, but fertilization and tillage had no effect on post-heading N uptake and N translocation. Nitrogen use efficiency (NUE) and N recovery were lower with N applied and not affected by tillage. Our study indicated that available N was affected more by environment than management. In dry conditions, when Nmin is low, N application may be more effective in increasing yield and N uptake than in wet years, an observation that may merit further attention. Key words: Available N, N mineralization, N recovery, N use efficiency, non-exchangeable ammonium, tillage
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Canadian Science Publishing
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  • 10
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    Effects of eight years of crop rotation and tillage on nitrogen availability and budget of a sandy loam soil (2003)
    Canadian Science Publishing
    Details
    Publication Date: 2003-11-01
    Description: The effects of tillage and crop rotations on soil N availability and economy were evaluated over two rotation cycles to address the paucity of such information. From 1993 through 2000, soil was sampled to 120 cm in the autumn from four crop rotations : (i) continuous wheat (Triticum aestivum L.), (ii) field pea (Pisum sativum L.)-wheat-canola (Brassica rapa L.)-wheat, (iii) red clover (Trifolium pratense L.) green manure-wheat-canola-wheat/red clover, (iv) fallow-wheat-canola-wheat, and analysed for KCl-extractable N. The rotations were managed under a conventional tillage (CT) or a no-till (NT) system, and were fertilized based on soil test results. A N budget was constructed for each cropping system comprising N added in seed and fertilizers, and by symbiotic fixation and N exported in the grain. More nitrate accumulated under CT than NT, resulting in lower N fertilizer application rates for CT plots. Soil mineralizable N was higher under NT than CT, and was not influenced by crop rotations. The trend for residual soil nitrate among crop rotations was: fallow rotation 〉 green manure rotation 〉 continuous wheat 〉 field pea rotation, due mostly to residual nitrate following the first phase of the rotations. There was no interaction of tillage with rotation. The continuous wheat and field pea rotation maintained a balanced N budget. The red clover rotation resulted in net N import in each rotation cycle of approximately 25 kg ha-1 under CT and 37 kg ha-1 under NT; net N export from the fallow rotation was 30 kg ha-1 under NT and 46 kg ha-1 under CT. Key words: Field pea, fallow, red clover, N economy, tillage, wheat
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Canadian Science Publishing
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