Influencia de las propiedades edáficas y la posición en el paisaje sobre la respuesta hidrológica de suelos pertenecientes a una cuenca de la Pampa Ondulada

C. Chagas, Filipe Behrends Kraemer, Santiago Utin, C. Irurtia, O. J. Santanatoglia
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引用次数: 9

Abstract

Research in the Tala´s Creek Basin (Rolling Pampa, Argentina) including the monitoring of gauged watersheds and field rainfall simulation experiments is being carried out. It showed disagreement between the hydrological response of a small arable watershed compared to a basin of 400 km2 containing both arable soils and non arable sodic soils. The objective of this work was to assess the generation of surface runoff and soil erosion corresponding to four treatments whose soils and land use are representative of the studied region. The field trials consisted in the application of highintensity simulated rainfall on soils under bare surface condition. Unlike the rest of the treatments, the situation under livestock use with low organic carbon content, poor physical condition and high percentage of exchangeable sodium at the topsoil, showed the lowest final infiltration rate (1 mm h-1) and the largest sediment yield (349 g m-2). Due to its position close to the main stream, this site can pose an important risk to the studied water course because it is a source of physical, chemical and biological contaminants. These results show that sodic soils may be partially responsible for the lack of agreement between the small watershed and the basin’s hydrological response to rainfall events.
土壤性质和在景观中的位置对波峰潘帕盆地土壤水文响应的影响
正在Tala’s Creek盆地(阿根廷滚动潘帕)进行研究,包括监测测量的流域和实地降雨模拟实验。结果表明,与包含耕地土壤和非耕地盐碱土的400平方公里流域相比,小规模耕地流域的水文响应存在差异。这项工作的目的是评估土壤和土地利用具有代表性的四种处理所对应的地表径流和土壤侵蚀的产生。野外试验包括在裸地条件下对土壤进行高强度模拟降雨。与其他处理不同的是,畜牧区土壤有机碳含量低、物理条件差、表土交换性钠含量高的情况下,最终入渗速率最低(1 mm h-1),产沙量最大(349 g m-2)。由于其位置靠近主流,该地点可能对所研究的水道构成重要风险,因为它是物理,化学和生物污染物的来源。这些结果表明,盐渍土可能是小流域与流域对降雨事件水文响应不一致的部分原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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