施用牛浆后耕地氨挥发。1. 场估计

J. Molen, H. V. Faassen, M. Leclerc, R. Vriesema, W. Chardon
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引用次数: 56

摘要

1987年9 - 11月进行了两次试验,分别在裸露的土壤表面施用牛浆,1988年4 - 5月进行了两次试验,在撒施后立即用耕耘机将牛浆与土壤上部6 cm的土壤混合。1987年的实验都持续了18天,1988年的实验持续了9天。一种不干扰气流动力学的微气象技术被用于测量NH3的挥发。挥发损失也间接测定了在施用后每隔一段时间收集的土壤浆液样品的矿物氮含量。NH3通量的日波动贯穿整个实验周期,正午前后最大,午夜最小。日通量值的大小随时间而减小。地表施用的牛浆挥发失氮量分别占总氮的18%和33%。,在前9天,分别对应于浆料施氮量的32%和67%。第9天之后挥发可以忽略不计。在土壤中掺入浆料显著降低了氮的挥发损失:9天后氮的挥发损失分别占总氮的6%和7%,对应于浆料施入的氨态氮的11%和16%。(经CABI许可摘自CAB Abstracts)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ammonia volatilization from arable land after application of cattle slurry. 1. Field estimates
Cattle slurry was surface-applied to bare soil in two experiments in September-November 1987, while in April-May 1988 two experiments were carried out in which the slurry was mixed with the upper 6 cm of the soil with a cultivator immediately after spreading. The 1987 experiments both lasted 18 days, the 1988 experiments 9 days. A micrometeorological technique, which did not disturb the dynamics of the air flow, was used to measure NH3 volatilization. Volatilization losses were also determined indirectly from mineral-N contents of soil-slurry samples collected at intervals after application. Diurnal fluctuations in the NH3 flux occurred throughout the experimental period, with maxima around midday and minima at midnight. The magnitude of the daily flux values decreased with time. The amounts of N lost through volatilization from surface-applied cattle slurry were 18 and 33% of the total N, resp., during the first 9 days, corresponding to 32 and 67% of the ammoniacal N applied with the slurry. Volatilization was negligible after day 9. Incorporation of the slurry into the soil considerably decreased the loss of N through volatilization: volatile losses of N after 9 days amounted to 6 and 7% of the total N, which corresponds to 11 and 16% of the ammoniacal N applied with the slurry. (Abstract retrieved from CAB Abstracts by CABI’s permission)
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