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Nitrogen Loss from Sandy Soils Treated witti

机译:处理过的沙质土壤中的氮损失

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TWO laboratory experiments were conducted to study. I. The movement of nitrogen forms released from different N-sources (U, AS, AN, UF, TCU, SCU and IBDU) applied with or without organic manure and nitrification inhibitor application under intermittent leaching. 2. NH3-volatiiization from different N-sources, (U, AS and mtroform) with or without nitrification inhibitor using sandy and calcareous soils. Under intermittent leaching, results show that the addition of nitrification inhibitor (DCD) in thepresence of organic manure slightly affected the transformation of ammonium to nitrate due to the adsorption of the inhibitor on the adsorptive sites of organic manure. Urea formaldehyde material showed a regular leaching of N forms compared to anotherones. The residual available N-forms were greatly affected by the source of N and the combination of nitrification inhibitor with or without organic manure addition. NH_3- loss was the greatest from different N sources applied to calcareous soil compared to the sandy one. On the other hand, the loss was greater with Nitroform as a slow-release fertilizer incalcareous soil compared with, the same fertilizer in the sandy one.
机译:进行了两个实验室实验进行研究。 I.在有淋洗的情况下,施用或不施用有机肥和硝化抑制剂时,从不同氮源(U,AS,AN,UF,TCU,SCU和IBDU)释放的氮形态的运动。 2.在有或没有硝化抑制剂的情况下,使用沙质和石灰质土壤,从不同氮源(U,AS和亚型)中NH3挥发。结果表明,在间歇浸出条件下,有机肥料存在下硝化抑制剂(DCD)的加入对铵向硝酸盐的转化影响很小,这是由于该抑制剂吸附在有机肥料的吸附位上。与他人相比,尿素甲醛材料显示出有规律的N形态浸出。氮的来源以及硝化抑制剂加或不加有机肥料的结合对残留的有效氮形态影响很大。与砂质土壤相比,施用到石灰性土壤上的不同氮源的NH_3-损失最大。另一方面,与在砂质土壤中施用相同肥料的硝态氮相比,在砂质土壤上使用缓释肥料的损失更大。

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