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The Effect of Land Use Changes on the Water Balance in the Ciliwung-Cisadane Catchment, West Java, Indonesia

机译:印度尼西亚西爪哇省Ciliwung-Cisadane集水区土地利用变化对水平衡的影响

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摘要

[ABSTRACT] The purpose of this study is to clarify the effect of land use changes on the water balance in humid tropics catchment area. The Ciliwung-Cisadane watershed of West Java, Indonesia, is selected as study area where intensive land use changes have occurred in the recent past. The elements of water balance such as precipitation, runoff and evapotranspiration into and from the catchment were estimated independently with data obtained from direct measurement or model calculation. Based on the observation data, there was an increase in runoff ratio of Ciliwung River and Cisadane River about 5-0x1.fc1bp+0nd 4% respectively. It indicates that there are some natural or artificial changes of land use that disturb the riveru27s flows and other water cycle components such as evapotranspiration. Satellite remote sensing data of 1984 and 1991 are used to reveal the land use changes. As results, there recognized large amount of change from paddy to cropland allocation and new settlement areas have been developed on paddy and cropland area respectively. Characteristic values of albedo are assigned to land use classes, and areal evapotranspiration of two periods are calculated by using Penman (1948) equation. As results, the amount of evapotranspiration in 1984 and in 1991 were 1,123mm and 1,010mm respectively, which decreased in the amount of 113mm (10%). According to calculation of water balance, the large amount of residue, which is termed as loss, has been found. These values indicate the possibility of the existence of percolation into deeper layers and the change in water storage.
机译:[摘要]这项研究的目的是弄清热带湿润集水区土地利用变化对水平衡的影响。印度尼西亚西爪哇省的Ciliwung-Cisadane流域被选为研究区域,近期土地使用发生了剧烈变化。利用从直接测量或模型计算获得的数据,独立估算水平衡的要素,例如降雨,径流和流域内和流域的蒸散量。根据观测资料,七里翁河和西沙丹河的径流量比分别增加了5-0x1.fc1bp + 0nd 4%。这表明土地利用的某些自然或人为变化会扰乱河流的流量和其他水循环成分,例如蒸散量。 1984年和1991年的卫星遥感数据用于揭示土地利用的变化。结果,人们认识到从稻田到农田分配的大量变化,分别在稻田和农田上开发了新的定居区。将反照率的特征值分配给土地利用类别,并使用Penman(1948)公式计算两个时期的面蒸散量。结果,1984年和1991年的蒸散量分别为1,123mm和1,010mm,减少了113mm(10%)。根据水平衡的计算,发现了大量的残留物,称为损失。这些值表明存在渗入更深层和储水量变化的可能性。

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