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INFLUENCE OF SLOPE POSITION AND HOG MANURE INJECTION ON FALL SOIL P AND N DISTRIBUTION IN AN UNDULATING LANDSCAPE

机译:缓坡景观坡位和猪粪施用对秋季土壤P,N分布的影响

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Investigation of how soil nutrients are distributed over the landscape in the fall is a prerequisite to identify critical source areas (CSA), which contribute soil nutrients to surface waters through snowmelt runoff. The objectives of this study are to investigate: (1) the distribution of soil nutrients in the landscape before soil freeze-up, and (2) how manure application in the fall affects this distribution. The study site, located in an undulating landscape in the Canadian prairies, is a closed drainage basin with moderate to fine textured soil. The basin received hog manure in fall 2001 and fall 2003. The landscape was classified into the shoulder, backslope, and footslope using a digital elevation model (DEM). Soil samples, collected from each landform segment in fall 2003 and fall 2004, were analyzed for available soil phosphorus (ASP), nitrate ((NO{sub}3){sup}-) and ammonium ((NH{sub}4){sup}+). In the undulating landscape, ASP levels had a distribution pattern of backslope < shoulder < footslope in fall 2003. The (NO{sub}3){sup}- levels increased from the shoulder to the footslope. The (NH{sub}4){sup}+ levels did not vary between the shoulder and the backslope, while the footslope had significantly higher (NH{sub}4){sup}+ than the other two landform segments. Manure application appeared to change these distribution patterns of ASP, (NO{sub}3){sup}-, and (NH{sub}4){sup}+ temporally. However, one year after manure application, the manure effect was only seen for ASP. The soil moisture level at the footslope was significantly different from that of the other landform segments in fall 2004. The shoulder and backslope were homogeneous in terms of soil moisture for both fall seasons.
机译:确定秋季土壤中养分分布的方式是确定关键源区(CSA)的先决条件,关键源区通过融雪径流将土壤养分贡献给地表水。这项研究的目的是调查:(1)土壤冻结前景观中土壤养分的分布;(2)秋季施用肥料如何影响这种分布。研究地点位于加拿大大草原上起伏不平的景观中,是一个封闭的流域盆地,土壤质地中等至精细。流域在2001年秋天和2003年秋天接受了猪粪。使用数字高程模型(DEM)将景观分为肩,后坡和山坡。分析了2003年秋季和2004年秋季从每个地形段收集的土壤样品中的有效土壤磷(ASP),硝酸盐((NO {sub} 3){sup}-)和铵盐((NH {sub} 4){ sup} +)。在起伏的地形中,ASP水平在2003年秋季具有后坡<肩<脚坡的分布模式。(NO {sub} 3){sup}-水平从肩坡向山脚坡增加。 (NH {sub} 4){sup} +水平在肩膀和后坡之间没有变化,而山坡的(NH {sub} 4){sup} +明显高于其他两个地形段。粪肥施用似乎会暂时改变ASP,(NO {sub} 3){sup}-和(NH {sub} 4){sup} ++的分布模式。但是,在施肥一年后,仅在ASP上才能看到施肥效果。 2004年秋季,山坡的土壤水分含量与其他地形段存在显着差异。就两个秋季而言,肩坡和后坡的土壤水分均一。

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