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Dissolved phosphorus transport from soil to surface water in catchments with different land use

机译:不同土地利用方式流域中溶解性磷从土壤到地表水的运输

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摘要

Diffuse phosphorus (P) export from agricultural land to surface waters is a significant environmental problem. It is critical to determine the natural background P losses from diffuse sources, but their identification and quantification is difficult. In this study, three headwater catchments with differing land use (arable, pasture and forest) were monitored for 3 years to quantify exports of dissolved (<0.45 µm) reactive P and total dissolved P. Mean total P exports from the arable catchment ranged between 0.08 and 0.28 kg ha−1 year−1. Compared with the reference condition (forest), arable land and pasture exported up to 11-fold more dissolved P. The contribution of dissolved (<0.45 µm) unreactive P was low to negligible in every catchment. Agricultural practices can exert large pressures on surface waters that are controlled by hydrological factors. Adapting policy to cope with these factors is needed for lowering these pressures in the future.
机译:从农田到地表水的扩散磷扩散是一个重大的环境问题。确定来自漫射源的自然本底P损耗至关重要,但是很难对其进行识别和量化。在这项研究中,对3个具有不同土地用途(耕地,牧场和森林)的源头集水区进行了为期3年的监测,以量化溶解态P(<0.45μm)的反应性P和总溶解P的出口量。 0.08和0.28 kg ha -1 -1 。与参考条件(森林)相比,可耕地和牧草出口的溶解磷增加了11倍。在每个集水区,溶解的(<0.45 µm)未反应磷的贡献率低至可以忽略不计。农业实践会在受水文因素控制的地表水上施加巨大压力。需要采取政策以应对这些因素,以减轻将来的压力。

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