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How land use/land cover changes can affect water, flooding and sedimentation in a tropical watershed: a case study using distributed modeling in the Upper Citarum watershed, Indonesia

机译:土地利用/土地覆盖的变化如何影响热带流域的水,洪水和沉积:以印度尼西亚上奇塔鲁姆流域为例,使用分布式模型进行案例研究

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摘要

Human activity has produced severe LULC changes within the Upper Citarum watershed and these changes are predicted to continue in the future. With an increase in population parallel to a 141% increment in urban areas, a reduction of rice fields and the replacement of forests with cultivations have been found in the past. Accordingly, LCM model was used to forecast the LULC in 2029. A distributed model called TETIS was implemented in the Upper Citarum watershed to assess the impact of the different historical and future LULC scenarios on its water and sediment cycles. This model was calibrated and validated with different LULCs. For the implementation of the sediment sub-model, it was crucial to use the bathymetric information of the reservoir located at the catchment's outlet. Deforestation and urbanization have been shown to be the most influential factors affecting the alteration of the hydrological and sedimentological processes in the Upper Citarum watershed. The change of LULC decreases evapotranspiration and as a direct consequence, the water yield increased by 15% and 40% during the periods 1994-2014 and 2014-2029, respectively. These increments are caused by the rise of three components in the runoff: overland flow, interflow and base flow. Apart from that, these changes in LULC increased the area of non-tolerable erosion from 412 km(2) in 1994 to 499 km(2) in 2029. The mean sediment yield increased from 3.1 Mton -yr(-1) in the 1994 LULC scenario to 6.7 Mton-yr(-1) in the 2029 LULC scenario. An increment of this magnitude will be catastrophic for the operation of the Saguling Dam.
机译:人类活动已在上奇塔鲁姆流域内产生了严重的土地利用,土地利用变化,并且这些变化预计将在未来继续。过去,随着人口的增长与城市地区141%的增长并行,稻田减少了,种植业也取代了森林。因此,LCM模型被用于预测2029年的LULC。在上奇塔鲁姆流域实施了名为TETIS的分布式模型,以评估不同的历史和未来LULC情景对其水和泥沙循环的影响。使用不同的LULC对该模型进行了校准和验证。对于沉积物子模型的实现,至关重要的是使用位于集水口出口处的水库的测深信息。毁林和城市化已被证明是影响上西塔鲁姆流域水文和沉积过程变化的最有影响的因素。 LULC的变化减少了蒸散量,直接的结果是,在1994-2014年和2014-2029年期间,水的产量分别增加了15%和40%。这些增量是由径流中三个组成部分的上升引起的:陆上径流,内流和基流。除此之外,LULC的这些变化将不可容忍的侵蚀面积从1994年的412 km(2)增加到2029年的499 km(2)。平均泥沙产量从1994年的3.1 Mton -yr(-1)增加到在2029年LULC方案中,LULC方案达到6.7 Mton-yr(-1)。这个量的增加对于萨古林水坝的运行将是灾难性的。

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