首页> 外文期刊>Plant and Soil >SIGNIFICANCE OF NITRATE LEACHING AND LONG TERM N IMMOBILIZATION AFTER DEEPENING THE PLOUGH LAYERS FOR THE N REGIME OF ARABLE SOILS IN NW GERMANY
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SIGNIFICANCE OF NITRATE LEACHING AND LONG TERM N IMMOBILIZATION AFTER DEEPENING THE PLOUGH LAYERS FOR THE N REGIME OF ARABLE SOILS IN NW GERMANY

机译:在德国西北部耕作土壤氮素层深耕后,进行硝态氮淋溶和长期固定化的意义

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摘要

Field studies were conducted to assess the turnover and the leaching of nitrogen in arable soils of Lower Saxony (NW Germany). The mean surplus N (difference between N inputs by fertilization and N export by the yield; 146 field plots) from 1985-1988 amounted to 38 kg ha(-1) yr(-1) in fine textured (clay, loam, silt) and to 98 kg ha(-1) yr(-1) in coarse (sandy) soils. Leaching of nitrate calculated by a simple functional model for simulation of the N regime over the winter period (i.e. mineralization and leaching) was 16 kg ha(-1) in the fine and 63 kg N ha(-1) in coarse soils (mean values of the winter periods 1985-1988 from 256 plots).
机译:进行了田间研究,以评估下萨克森州(德国西北部)的耕地土壤中氮的周转和淋溶。 1985-1988年的平均富余氮(施肥氮输入量与产量氮输出量之间的差异; 146个田地)在精细纹理(粘土,壤土,粉砂)中为38 kg ha(-1)yr(-1)。并在粗糙(沙质)土壤中达到98 kg ha(-1)yr(-1)。通过简单的功能模型计算出的硝酸盐的淋失量,用于模拟冬季(矿化和浸出)的N态,细土中为16 kg ha(-1),粗土中为63 kg N ha(-1)(平均256个地块的1985-1988年冬季数值)。

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