Estimated N leaching losses for organic and conventional farming in Denmark

2006 ◽  
Vol 144 (2) ◽  
pp. 135-149 ◽  
Author(s):  
MARIE TRYDEMAN KNUDSEN ◽  
IB SILLEBAK KRISTENSEN ◽  
JØRGEN BERNTSEN ◽  
BJØRN MOLT PETERSEN ◽  
ERIK STEEN KRISTENSEN

The impact of organic, compared with conventional, farming practices on N leaching loss was studied for Danish mixed dairy and arable farms using an N balance approach based on representative data. On mixed dairy farms, a simple N balance method was used to estimate N surplus and N leaching loss. On arable farms, the simple N balance method was unreliable due to changes in the soil N pool. Consequently, the Farm ASSEssment Tool (FASSET) simulation model was used to estimate N surplus, N leaching loss and the changes in the soil N pool.The study found a lower N leaching loss from organic than conventional mixed dairy farms, primarily due to lower N inputs. On organic arable farms, the soil N pool increased over time but the N leaching loss was comparable with conventional arable farms. The soil N pool was increased primarily by organic farming practices and incorporation of straw. The highest increase in the soil N pool was seen on soils with a low initial level of organic matter. The N leaching loss was dependent on soil type, the use of catch crops and the level of soil organic matter, whereas incorporation of straw had a minor effect. N leaching was highest on sandy soils with a high level of soil organic matter and no catch crops. The present results stress the importance of using representative data from organic and conventional farming practices in comparative studies of N leaching loss. Lack of representative data has been a major weakness of previous comparisons on N leaching losses on organic and conventional farms.

2020 ◽  
Vol 261 ◽  
pp. 114090 ◽  
Author(s):  
Shicong Geng ◽  
Zhijie Chen ◽  
Shanshan Ma ◽  
Yue Feng ◽  
Lei Zhang ◽  
...  

2015 ◽  
Vol 13 (2) ◽  
pp. e0303 ◽  
Author(s):  
Saulius Guzys ◽  
Stefanija Miseviciene

<p>Inappropriate use of nitrogen fertilisers is becoming a global problem; however, continuous fertilisation with N fertiliser ensures large and constant harvests. To evaluate the relationships of differently fertilised cultivated plant rotation with N metabolism in the agroecosystem the research was conducted between 2006 and 2013 at Lipliūnai, Lithuania, in fields with calcareous gley brown soil, <em>i.e.</em> <em>Endocalcari Endohypogleyic Cambisol</em> (<em>CMg-n-w-can</em>). The research area covered three drained plots where crop rotation of differently fertilised cereals and perennial grasses were applied. The greatest productivity was found in a higher fertilisation (TII, 843 kg N/ha) cereals crop rotation. With less fertilisation (TI, 540 kg N/ha) crop rotation productivity of cereals and perennial grasses (TIII, 218 kg N/ha) was 11-35% lower. The highest amount of mineral soil N (average 76 kg/ha) was found in TI. It was influenced by fertilisation (<em>r</em>=0.71) and crop productivity (<em>r</em>=0.39). TIII tended to reduce N<sub>min</sub> (12.1 mg/L) and N<sub>total</sub> (12.8 mg/L) concentrations in drainage water and leaching of these elements (7 and 8 kg/ha). N<sub>min</sub> and N<sub>total</sub> concentrations in the water depended on crop productivity respectively (<em>r</em>=0.48; <em>r</em>=0.36), quantity of mineral soil N (<em>r</em>=0.65; <em>r</em>=0.59), fertilisation (<em>r</em>=0.59; <em>r</em>=0.52), and N balance (<em>r</em>=0.26; <em>r</em>=0.35). Cereal crop rotation increased N leaching by 12-42%. The use of all crop rotations resulted in a negative N balance. Nitrogen balance depended on fertilisation with N fertiliser (<em>r</em>=0.55). The application of perennial grasses crop rotation in agricultural fields was the best environmental tool, reducing N migration to drainage.</p>


2011 ◽  
Vol 174 (4) ◽  
pp. 568-575 ◽  
Author(s):  
Christopher Brock ◽  
Andreas Fließbach ◽  
Hans-Rudolf Oberholzer ◽  
Franz Schulz ◽  
Klaus Wiesinger ◽  
...  

Soil Research ◽  
2008 ◽  
Vol 46 (7) ◽  
pp. 636
Author(s):  
J. M. Xue ◽  
P. W. Clinton ◽  
R. Sands ◽  
T. W. Payn ◽  
M. F. Skinner

Biuret (C2H5N3O2) priming effect on mineralisation of native soil N has not been precisely quantified in previous studies, although it is a potential microbial activity regulator and slow-release N fertiliser. Following application of biuret at concentrations of 0 (B0) and 100 (B100) mg/kg (oven-dried) soil, we measured the dynamics of biuret-derived 15N in soil N pools, soil C mineralisation, and microbial biomass C in a sandy loam and a silt loam during a 112-day-long incubation to investigate the fate of biuret 15N and its effect on net mineralisation of native soil N. Biuret was decomposed faster in the sandy loam soil than the silt loam soil. In the sandy loam soil, the stabilised N pool was a strong sink for the biuret-derived 15N and accumulated about half of the applied 15N at the end of incubation. In the silt loam soil, 68% of the 15N applied was recovered in the NO3−-N pool and the stabilised N pool accumulated only about 25% of the applied 15N at the end of incubation. Biuret addition increased the turnover rate constant of soil organic matter and caused a real priming effect on net mineralisation of native soil N in both soils. The additional mineralisation of native soil N was 20.1 mg/kg (equivalent to 27.3 kg N/ha) in the sandy loam soil and 20.5 mg/kg (equivalent to 57.3 kg N/ha) in the silt loam soil. Biuret priming effect was related to the acceleration of soil organic matter decomposition by increased microbial activity at an early stage and the death/decay of microbes at a later stage of incubation. The native soil N released through the priming effect was partially from soil non-biomass organic matter and partially from soil microbial biomass.


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