Premium
Nitrogen cycling in organic farming systems with rotational grass–clover and arable crops
Author(s) -
Berntsen J.,
Grant R.,
Olesen J. E.,
Kristensen I. S.,
Vinther F. P.,
Mølgaard J. P.,
Petersen B. M.
Publication year - 2006
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/j.1475-2743.2005.00016.x
Subject(s) - agronomy , plough , leaching (pedology) , environmental science , hordeum vulgare , pasture , organic farming , loam , soil water , manure , nitrogen cycle , arable land , crop rotation , nitrogen , agriculture , poaceae , crop , soil science , chemistry , biology , ecology , organic chemistry
Organic farming is considered an effective means of reducing nitrogen losses compared with more intensive conventional farming systems. However, under certain conditions, organic farming may also be susceptible to large nitrogen (N) losses. This is especially the case for organic dairy farms on sandy soils that use grazed grass–clover in rotation with cereals. A study was conducted on two commercial organic farms on sand and loamy sand soils in Denmark. On each farm, a 3‐year‐old grass–clover field was selected. Half of the field was ploughed the first year and the other half was ploughed the following year. Spring barley ( Hordeum vulgare L.) was sown after ploughing in spring. Measurements showed moderate N leaching during the pasture period (9–64 kg N ha −1 year −1 ) but large amounts of leaching in the first (63–216 kg N ha −1 ) and second (61–235 kg N ha −1 ) year after ploughing. There was a small yield response to manure application on the sandy soil in both the first and second year after ploughing. To investigate the underlying processes affecting the residual effects of pasture and N leaching, the dynamic whole farm model farm assessment tool (FASSET) was used to simulate the treatments on both farms. The simulations agreed with the observed barley N‐uptake. However, for the sandy soil, the simulation of nitrate leaching and mineral nitrogen in the soil deviated considerably from the measurements. Three scenarios with changes in model parameters were constructed to investigate this discrepancy. These scenarios suggested that the organic matter turnover model should include an intermediate pool with a half‐life of about 2–3 years. There might also be a need to include effects of soil disturbance (tillage) on the soil organic matter turnover.