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Soil water dynamics under various agricultural land covers on a subsurface drained field in north-central Iowa, USA

机译:美国爱荷华州中北部地下排水田中各种农田覆盖下的土壤水分动态

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摘要

Modification of land cover systems is being studied in subsurface drained Iowa croplands due to their potential benefits in increasing soil water and nitrogen depletion thus reducing drainage and NO3–N loss in the spring period. The objective of this study was to evaluate the impacts of modified land covers on soil water dynamics. In each individual year, modified land covers including winter rye–corn (rC), winter rye–soybean (rS), kura clover as a living mulch for corn (kC), and perennial forage (PF), as well as conventional corn (C) and soybean (S), were grown in subsurface drained plots in north-central Iowa. Results showed that subsurface drainage was not reduced under modified land covers in comparison to conventional corn and soybean. Soil water storage (SWS) was significantly reduced by PF treatments during the whole growing seasons and by kC during May through July when compared to the cropping system with corn or soybean only (p u3c 0.05). Treatments of rC and rS typically maintained higher SWS than C and S, respectively, during the 3 years of this study. In the spring during a 10–15-day period when the rainfall was minimal, SWS in plots with rye, kura clover, and forage decreased at a significantly higher rate than the C and S plots which were bare. Estimated evapotranspiration (ET) during this period was significantly higher in rS, kC, and PF treatments than C and S. The results of this study suggested that significantly higher ET and similar drainage for modified land covers may increase water infiltration, which would be expected to reduce surface runoff thus to decrease stream flow. Because subsurface drainage reduction was not seen in this study, impact of modified land covers on NO3–N loss needs further investigation.
机译:由于爱荷华州地下排水的农田在增加土壤水和氮的消耗方面具有潜在的好处,因此减少了春季的排水和NO3-N的损失,因此正在研究土地覆盖系统的改造。这项研究的目的是评估改良的土地覆盖对土壤水分动力学的影响。在每一年中,经过改良的土地覆盖范围包括冬黑麦-玉米(rC),冬黑麦-大豆(rS),库拉三叶草作为玉米的活覆盖物(kC),多年生草料(PF)以及常规玉米( C)和大豆(S)在爱荷华州中北部的地下排水地块种植。结果表明,与常规玉米和大豆相比,改良土地覆盖下的地下排水并未减少。与仅使用玉米或大豆的种植系统相比,在整个生长季中通过PF处理以及在5月至7月期间通过kC显着降低了土壤储水量(p u3c 0.05)。在本研究的3年中,rC和rS的治疗通常分别维持高于C和S的SWS。在春季的10-15天期间,降雨量很少,在春季,黑麦,库拉三叶草和草料地的SWS下降速度明显高于裸露的C和S地。 rS,kC和PF处理期间的估计蒸散量(ET)显着高于C和S。这项研究的结果表明,经过改良的土地覆被,ET和类似的排水量显着较高可能会增加水的渗透,这是可以预期的减少地表径流,从而减少水流。由于在本研究中未发现地下排水减少,因此改良土地覆盖对NO3-N损失的影响需要进一步研究。

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