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Comparison of Liquid Swine Manure and Aqua-Ammonia Nitrogen Application Timing on Subsurface Drainage Water Quality in Iowa

机译:猪粪和水氨氮施用时间对爱荷华州地下排水水质的比较

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摘要

In Iowa and many other Midwestern states, excess water is removed artificially through subsurface drainage systems. While these drainage systems are vital for crop production, nitrogen (N), added as manure or commercial fertilizer, or derived from soil organic matter, can be carried as nitrate-nitrogen (NO3-N) to downstream water bodies. A five-year, five-replication, field study was initiated in the fall of 1999 in Pocahontas County, Iowa, on 0.05 ha plots that are predominantly Nicollet, Webster, and Canisteo clay loams with 3% to 5% organic matter located on glacial till within the Des Moines Lobe. The objective was to determine the influence of seasonal N application as ammonia or liquid swine manure on flow-weighted NO3-N concentrations and losses in subsurface drainage water and crop yields in a corn-soybean rotation. Four aqua-ammonia N treatments (168 or 252 kg N ha-1 applied for corn in late fall or as an early season side-dress) and three manure treatments (218 kg N ha-1 for corn in late fall or spring or 168 kg N ha-1 in the fall for both corn and soybean) were imposed on subsurface-drained, continuous flow-monitored plots. Precipitation during the drainage season (March to November) was slightly below the long-term norm (722 mm) for all four years in the study period and ranged from 615 mm in 2001 (85% of normal) to 707 mm (98% of normal) in 2004. Monthly rainfall was highly variable, and subsurface drainage, or the lack thereof, usually mimicked the precipitation patterns. On average, 69% of subsurface drainage occurred in May and June of each year, with lower amounts in April and July. Four-year average flow-weighted NO3-N concentrations measured in drainage water were ranked: spring aqua-ammonia 252 (23 mg L-1) = fall manure 168 every year (23 mg L-1) u3e fall aqua-ammonia 252 (19 mg L-1) = spring manure 218 (18 mg L-1) = fall manure 218 (17 mg L-1) u3e spring aqua-ammonia 168 (15 mg L-1) = fall aqua-ammonia 168 (14 mg L-1). Corn yields were significantly greater (p = 0.05) for the spring and fall manure 218 rates than for non-manure treatments. Soybean yields were significantly greater (p = 0.05) for the treatments with a spring nitrogen application to the previous corn crop. Overall, under the slightly dry to normal precipitation conditions of this study, corn yields and NO3-N concentrations in subsurface drainage were not significantly different (p = 0.05) between fall and spring treatments at the 168 aqua-ammonia or 218 kg ha-1 N manure N rates.
机译:在爱荷华州和许多其他中西部州,多余的水通过地下排水系统被人为去除。尽管这些排水系统对于农作物的生产至关重要,但作为肥料或商品肥料添加的或源自土壤有机质的氮(N)可以作为硝态氮(NO3-N)的形式带入下游水体。一项为期五年,五次重复的田间研究于1999年秋季在爱荷华州的Pocahontas县开始,调查了0.05公顷土地,主要是Nicollet,Webster和Canisteo黏土壤土,冰川上有3%至5%的有机质直到得梅因河瓣内。目的是确定季节性施用氮肥(如氨水或猪粪肥)对玉米-大豆轮作中流量加权的NO3-N浓度以及地下排水中水损失和作物产量的影响。四个水氨氮处理(168或252千克N ha-1在秋季晚些时候或作为早期季节的副作施于玉米上)和三种肥料处理(218千克N ha-1的玉米在秋季或春季或168后期施氮)在地下排水,连续流量监测的地块上,玉米和大豆在秋季均下降了kg N ha-1。在研究期间的所有四年中,排水季节(3月至11月)的降水量均略低于长期标准(722毫米),范围从2001年的615毫米(正常值的85%)到707毫米(正常值的98%)。正常情况下是在2004年。每月降雨量变化很大,地下排水或缺乏排水通常模拟了降雨模式。平均而言,每年5月和6月发生69%的地下排水,而4月和7月则减少。对排水中的四年平均流量加权NO3-N浓度进行排名:春季氨水252(23 mg L-1)=每年秋季粪便168(23 mg L-1)秋季氨水252 (19 mg L-1)=春季肥料218(18 mg L-1)=秋季肥料218(17 mg L-1)春季氨水168(15 mg L-1)=秋季氨水168( 14 mg L-1)。春季和秋季施218肥料的玉米单产均显着高于非肥料处理(p = 0.05)。在以前的玉米作物上施氮肥后,大豆单产显着提高(p = 0.05)。总体而言,在本研究的降水量稍为干燥至正常的条件下,在168个氨水或218 kg ha-1的秋季和春季处理之间,地下排水中的玉米产量和NO3-N浓度之间没有显着差异(p = 0.05)。 N肥料N比率。

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