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首页> 外文期刊>Plant and Soil >Gaseous nitrogen losses and ammonia volatilization measurement following land application of cattle slurry in the mid-Atlantic region of the USA
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Gaseous nitrogen losses and ammonia volatilization measurement following land application of cattle slurry in the mid-Atlantic region of the USA

机译:美国中大西洋地区牛粪在土地上施用后的气态氮损失和氨气挥发测量

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摘要

To provide locally-determined field data for extension and environmental management purposes, gaseous N losses were measured following cattle slurry application to an arable silty-loam soil in the mid-Atlantic region of the USA. The field had been cropped to no-till maize. NH3 volatilization was measured with the micro-meteorological, integrated horizontal flux (IHF) method, and denitrification with a core incubation method using acetylene inhibition. An early-winter surface application (5 December 1996; 88 m3 ha−1 supplying 91 kg NH 4 + -N ha−1) was either unincorporated or immediately incorporated. NH3 volatilization was measured from the unincorporated application, and denitrification from both slurry treatments and appropriate control soils. Total NH3 loss from the unincorporated slurry application was 19% of applied NH 4 + -N; temperatures were cool (4–6 °C), and 25 mm of rain fell within 24 h of application. For 3 months, enhanced denitrification occurred from the two slurry treatments, with generally higher rates from the incorporated slurry. Total net denitrification loss from the surface-applied and incorporated slurry treatments was, respectively, 11 and 17% of applied NH 4 + -N. Denitrification loss over the winter/early-spring period was appreciable but not substantial, even where NH3 volatilization was restricted by immediate incorporation. From the spring application (30 April 1997, 39 m3 ha−1 supplying 51 kg NH 4 + -N ha−1), total NH3 loss was 71% of applied NH 4 + -N. These NH3 volatilization loss data and the similarity of climate suggest that NH3 loss factors from recent NW European work are likely to be generally applicable in the mid-Atlantic region. NH3 volatilization from the spring application was also measured using the Z-instrument (ZINST) approach, and with a system of small wind tunnels. A comparative assessment of the three methods is reported.
机译:为了提供用于扩展和环境管理目的的本地确定的现场数据,在将牛粪浆施用到美国中大西洋地区的可耕粉质壤土上后,测量了气态氮的损失。田地已经种了免耕玉米。 NH3的挥发量采用微气象,水平水平通量(IHF)方法进行测量,并采用乙炔抑制的核心孵化法进行反硝化处理。要么是早期冬季表面施肥(1996年12月5日;供应91 kg NH 4 + -N ha-1 的88 m3 ha-1 ),要么是未注册成立或立即注册成立。 NH3 的挥发是通过非掺入法测量的,而硝化作用则是通过泥浆处理和适当的对照土壤进行的。未掺入泥浆的总NH3 损失为所施用NH 4 + -N的19%;温度凉爽(4–6°C),施药后24小时内降雨25毫米。在三个月的时间里,两种浆液处理的反硝化作用增强,掺入的浆液的反硝化率通常更高。表面处理和混合处理的总净反硝化损失分别为所施加的NH 4 + -N的11%和17%。即使NH 3挥发因立即掺入而受到限制,冬季/初春期间的反硝化损失仍是可观的,但并不大。从春季申请开始(1997年4月30日,供应39 kg NH 4 + -N ha-1 的39 m3 ha-1 ),总NH3 < / sub>损失为施用的NH 4 + -N的71%。这些NH3 挥发损失数据和气候的相似性表明,来自欧洲西北地区最近工作的NH3 损失因子很可能普遍适用于大西洋中部地区。还使用Z仪器(ZINST )方法和小型风洞系统测量了春季应用中NH3 的挥发。报告了这三种方法的比较评估。

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