首页> 外文会议>Asian conference on remote sensing;ACRS >AN INTEGRATED GEOINFORMATICS TECHNOLOGY WITH HYDROLOGICAL MODEL TO IMPACT ASSESSMENT OF LAND USE CHANGE ON RUNOFF IN THE UPPER LAM TA KHONG WATERSHED
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AN INTEGRATED GEOINFORMATICS TECHNOLOGY WITH HYDROLOGICAL MODEL TO IMPACT ASSESSMENT OF LAND USE CHANGE ON RUNOFF IN THE UPPER LAM TA KHONG WATERSHED

机译:水文模型与水文模型集成的地学信息技术影响上游大潭流域径流土地利用变化的评价。

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The main objective of this study was to evaluate the impact of land use changes on surface runoff in upper Lam Ta Khong watershed, headwaters watershed. The land useduring 1993,2001 and 2009 were classed by visual interpretation methods based on LANDSAT imagery data. The monthly surface runoff simulation by using hydrological SCS-CN model integrated with GIS. Model calibration and validation were performed by comparing observed and simulated results at the M.43A (upstream watershed) and M.89 (downstream watershed) during the water year 1993,2001 (model calibration) and 2009 (model validation). The impact of land use change on surface runoff was evaluated with scenarios model and simple linear regression. The model was conducted for each land use map in three time periods (1993,2001 and 2009). The study revealed that 1) the land use type during 1993 -2009 founded that the forest and agricultural land were decreased, while the urban and built-up area has been continuously increasing. 2) A calibrated model shows that satisfactory of the coefficient of efficiency (E) is 0.39 and 0.45 and coefficient of determination (R~2) is 0.36 and 0.48 at the M.43A and M.89, respectively. 3) The decreased of forest and agricultural land, while urban and built-up area was increased have a negative impact on surface runoff due to decreasing of infiltration and increasing of surface runoff Especially, urbanization was the strongest contributor to the increase of surface runoff. The results of this study indicate that the changing of land use types from natural surface to impervious surface has a significant impact on surface runoff. This study will provide quantitative information for stakeholders in land use plann ingand water resource management in the study area.
机译:这项研究的主要目的是评估土地利用变化对林大孔上游流域,上游水域的地表径流的影响。根据LANDSAT影像数据,通过视觉解释方法对1993、2001和2009年使用的土地进行分类。利用与GIS集成的水文SCS-CN模型进行月面径流模拟。通过比较在1993、2001(模型校准)和2009(模型验证)水年期间在M.43A(上游分水岭)和M.89(下游分水岭)的观察结果和模拟结果,进行模型校准和验证。利用情景模型和简单的线性回归评估了土地利用变化对地表径流的影响。该模型是在三个时间段(1993、2001和2009)中针对每个土地利用图进行的。研究表明:1)1993年至2009年的土地利用类型发现,森林和农业用地减少了,而城市和建成区的面积却在不断增加。 2)校准模型表明,在M.43A和M.89处,令人满意的效率系数(E)为0.39和0.45,确定系数(R〜2)分别为0.36和0.48。 3)森林和农业用地的减少,而城市和建成区面积的增加,则由于入渗量的减少和地表径流的增加而对地表径流产生负面影响。特别是,城市化是地表径流增加的最主要因素。这项研究的结果表明,土地利用类型从自然表面到不渗透表面的变化对地表径流有重大影响。这项研究将为研究区域的土地利用规划和水资源管理中的利益相关者提供定量信息。

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