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Influence of paddy rice terraces on soil erosion of a small watershed in a hilly area of Northern Vietnam

机译:水稻梯田对越南北部丘陵小流域水土流失的影响

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摘要

Soil erosion is the main cause of soil degradation in northern Vietnam. In this study, soil erosion was measured in 2 m(2) field plots, a 19.1-ha sub-watershed, and a 248.9-ha main watershed in Tam Quan commune, Tam Duong district, northern Vietnam during 2 years, i.e., 2004-2005. The main watershed includes lowland paddy fields, and is representative for watersheds in the northern Vietnamese landscape. Soil erosion was measured for eight events, at all the three scales to increase our understanding of erosional processes and to assess the effects of paddy fields within the main watershed. The results show that total discharge and sediment yield in both sub-watershed and main watershed were much lower than those in the field plots. Total discharge per unit area in the main watershed was higher than in the sub-watershed, because during the growing season, the paddies are filled with water and any rainfall on them therefore becomes runoff. Sediment yield in the main watershed fluctuated, depending on the soil erosion contribution from many sub-watersheds. Annual rainfalls in 2004 and 2005 were 1,172 and 1,560 mm, respectively, resulting in corresponding total discharges of 54 and 332 mm and total soil losses of 163 and 1,722 kg ha(-1) year(-1). High runoff volumes occurred in July, August, and September, but April, June, the last 10 days of September and October, were the susceptible periods for soil erosion in the study area because of low plant cover and many agricultural activities during these periods.
机译:水土流失是越南北部土壤退化的主要原因。在这项研究中,在2年(即2004年)期间,在越南北部Tam Duong区Tam Quan公社的2 m(2)田地,19.1公顷的小流域和248.9公顷的主要流域中测量了土壤侵蚀-2005。主要分水岭包括低地稻田,是越南北部景观中的分水岭的代表。在所有三个尺度上对八个事件的土壤侵蚀进行了测量,以增进我们对侵蚀过程的理解并评估主要流域内稻田的影响。结果表明,子流域和主流域的总排沙量和产沙量远低于田间地块。主流域单位面积的总排放量高于次流域,这是因为在生长季节,稻田充满了水,因此它们上的任何降雨都会径流。主要流域的沉积物产量波动,取决于许多次流域的土壤侵蚀贡献。 2004年和2005年的年降雨量分别为1,172和1,560毫米,导致相应的总排放量为54和332毫米,土壤总损失量为163和1,722千克ha(-1)年(-1)。由于研究区的植物覆盖率低和许多农业活动,因此径流量在7月,8月和9月发生,但4月,6月,即9月和10月的最后10天是土壤侵蚀的敏感时期。

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