首页> 外文期刊>American Journal of Environmental Sciences >POTENTIAL ZONES OF PERUVANTHANAM AND VALIYATHODU SUB-WATERSHEDS OF MANIMALA RIVER BASIN
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POTENTIAL ZONES OF PERUVANTHANAM AND VALIYATHODU SUB-WATERSHEDS OF MANIMALA RIVER BASIN

机译:Manimala河流域的Perantanthanam和Valiyathodu次生灌木丛的潜在区带

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摘要

Groundwater is a dynamic and replenishable natural resource. But in hard rock terrains, its availability is of limited extent. In sub-watershed studies, remote sensing and GIS techniques have the advantages of spatial, spectral and temporal data, covering large and inaccessible areas within a short span of time. Thus this technique has become a very handy tool in assessing and monitoring groundwater resources. Multi Criteria Evaluation Technique (MCE) by integration of the thematic maps such as Geomorphology, Geology, Land use/Land cover and Slope prepared from conventional and remote sensing techniques using GIS yield more and near accurate result. The groundwater potential zones are classified in to five zones viz, 'excellent to very good', 'verygood to good', 'good to moderate', 'moderate to poor' and 'poor to very poor'. Critical analysis and comparison of ground water potential zones of both sub-watersheds reveals that, 26.10 km~2 (47.58%) area of Valiyathodu sub-watershed fall under 'excellent to very good' category where as in Peruvanthanam sub-watershed it is 7.69 km~2 (13.64%). In Peruvanthanam sub-watershed, 'very good to good' category covers 14.87 km~2 (26.35%), 'good to moderate' covers 17.65 km~2 (31.28%), 'moderate to poor' covers11.62 km~2 (20.59%) and 'poor to very poor' covers 4.59 km~2 (8.14%). Where as in Valiyathodu sub-watershed, 'very good to good' category covers an area of 18.55 km2 (33.82%), 'good to moderate' covers 6.65 km~2 (12.12%) and 'moderate to poor' covers 2.43 km~2 (4.43%) and 'poor to very poor' covers 1.12 km~2 (2.05%). Hence it is explicit that, in general groundwater potential is better in Valiyathodu sub-watershed compared to Peruvanthanam sub-watershed.
机译:地下水是一种动态且可补充的自然资源。但是在坚硬的岩石地形中,其可用性有限。在小流域研究中,遥感和GIS技术具有空间,光谱和时间数据的优势,可在短时间内覆盖较大且不可访问的区域。因此,该技术已成为评估和监测地下水资源的非常方便的工具。通过集成专题图(例如地貌,地质,土地利用/土地覆盖和坡度)的多标准评估技术(MCE),这些专题图是使用GIS从传统技术和遥感技术制备的,结果越来越准确。地下水潜在地带分为五个区域,即“优秀至非常好”,“非常好至好”,“很好至中等”,“中等至贫穷”和“贫穷至非常贫穷”。对这两个子集水区的地下水潜力区进行的批判性分析和比较表明,瓦里亚索杜子集水区的26.10 km〜2(47.58%)面积属于“优秀至极好”类别,而在佩鲁万坦南子集水区为7.69 km〜2(13.64%)。在佩鲁瓦塔南(Peruvanthanam)小流域,``从优至优''类别涵盖14.87 km〜2(26.35%),从``优至中等''类别涵盖17.65 km〜2(31.28%),从``中到穷''类别涵盖11.62 km〜2( 20.59%)和“从极到极贫困”覆盖4.59 km〜2(8.14%)。像瓦里亚索杜(Valiyathodu)小流域一样,“很好到很好”类别的面积为18.55 km2(33.82%),“很好到中等”的面积为6.65 km〜2(12.12%),而“中等到贫穷”的面积为2.43 km〜 2(4.43%)和“从极到差”覆盖1.12 km〜2(2.05%)。因此,很明显,与佩鲁瓦塔南分水岭相比,瓦利亚索杜分水岭的地下水潜力总体上更好。

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