首页> 外文期刊>Modeling Earth Systems and Environment >Groundwater recharge potential zones mapping in upper Manimuktha Sub basin Vellar river Tamil Nadu India using GIS and remote sensing techniques
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Groundwater recharge potential zones mapping in upper Manimuktha Sub basin Vellar river Tamil Nadu India using GIS and remote sensing techniques

机译:使用GIS和遥感技术在印度泰米尔纳德邦Vellar河上Manimuktha次盆地地下水补给潜力区的制图。

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An attempt has been made to assess the groundwater recharge potential zones in Upper Manimuktha sub basin, Vellar river, Tamil Nadu. Groundwater recharge denotes to the entry of water from the unsaturated zone into the saturated zone below the water table surface, together with the associated movement away from the water table within the saturated zone. This study mainly focus the many factors that control the occurrence and movement of groundwater in a hardrock region including topography, Geology,lineament, drainage patterns, land use/land cover, slope and soil. Using remote sensing and Geographic Information System it is possible to take number of different thematic maps of the area and overlay form a new integrated layer. The integrated map reveals about the groundwater recharge potential zones of the area and classified into five categories which represents very low to Very good Groundwater Recharge Potential Zones (GWRPZ). Downstream areas as well as waterbodies fall in the very high GWRPZ (12.4 km2) indicates high infiltration and low runoff. Then followed by high GWRPZ (115.74 km2) indicate these area maximum covered by agricultural land (57.99 km2) as well as fallow land (85.41 km2), so the infiltration high. In the poor (125.28 km2) andvery low GWRPZ (82.61 km2) mainly fall in the hilly terrain as well as in the waste, barren and buildup land of the study area. Based on the GWRPZ study indicate 34.4 % of the rainwater infiltrate in the ground of the entire study area.
机译:已经尝试评估泰米尔纳德邦Vellar河上Manimuktha子盆地的地下水补给潜力区。地下水补给是指水从非饱和区进入地下水位以下的饱和区,以及在饱和区内离开地下水位的相关运动。这项研究主要关注控制硬岩地区地下水发生和移动的许多因素,包括地形,地质,地貌,排水方式,土地利用/土地覆盖,坡度和土壤。使用遥感和地理信息系统,可以拍摄该区域的许多不同主题地图,并叠加形成一个新的集成层。综合地图揭示了该地区的地下水补给潜力区,分为五类,分别表示从非常低到非常好的地下水补给潜力区(GWRPZ)。 GWRPZ(12.4 km2)很高的下游区域和水体下降表明高入渗和低径流。然后是高GWRPZ(115.74 km2),表明这些面积最大的是农业用地(57.99 km2)和休耕地(85.41 km2),因此入渗率很高。在贫困地区(125.28平方公里)和非常低的GWRPZ(82.61平方公里),主要分布在丘陵地带以及研究区域的荒地,贫瘠和积聚的土地上。基于GWRPZ的研究表明,整个研究区域的地面中有34.4%的雨水渗入。

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