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Geomorphological Mapping for Identification of Ground Water Potential Zones in Hard Rock Areas Using Geo-spatial Information- A Case Study in Malur Taluk, Kolar District, Karnataka, India

机译:利用地理空间信息识别硬岩地区地下水潜力区的地貌图绘制-以印度卡纳塔克邦科拉尔地区的马鲁·塔鲁克为例

摘要

The search for new groundwater resources is essential to sustained economic development in aridudenvironment. The study area is part of Ponnaiyar river basin falling between N latitude of 12°48’24” toud13°07’06’ and E longitude of 77°50’30” to 78°08’15” falls in Survey of India toposheets 57 G/16, 57 H/13, 57udK/4 and 57 L/1 covering an area of 645 km2 in Kolar District, which is highly drought prone in KarnatakaudState, India. In the present paper, by a methodological approach based on remote sensing and GIS, drainageudand hydrogeomorphological maps were prepared using the IRS-1 C & 1 D LISS-III and PAN merged satelliteuddata and geomorphic units. Denudational hill, residual hill, inselberg, pediment inselberg complex, pediment,udshallow weathered pediplain, moderately weathered pediplain and valley fill shallow were identified. The areaudis characterised by undulating terrain interspersed by low ranges of rocky hills. The elevation ranges fromud860 m to 1127 m above MSL. The mean annual rainfall of Malur is 722.0mm. The River Dhakshina Pinakiniudand Markarda Halla drain the area. The streams exhibit dendritic to sub dendritic type of drainage patternudand comprise of granite and gneissic rock formations of Achaean age. On the basis of different geomorphicudunits, four categories of groundwater potential zones were delineated as (i) very good to good (ii) good toudmoderate (iii) moderate to poor, and (iv) poor to very poor.
机译:寻找新的地下水资源对于干旱/环境中的持续经济发展至关重要。研究范围是Ponnaiyar流域的一部分,其北纬介于12°48'24”至 ud13°07'06'之间,东经77°50'30”至78°08'15”属于印度调查范围拓扑片57 G / 16、57 H / 13、57 udK / 4和57 L / 1在印度卡纳塔克邦(Karnataka udState)极易发生干旱的科拉尔区(Kolar District)占地645 km2。本文采用基于遥感和GIS的方法,利用IRS-1 C&1 D LISS-III和PAN合并的卫星 uddata和地貌单位绘制了排水 udand水文地貌图。确定了齿状丘陵,残留丘陵,inselberg,山形沉积物,inselberg复合物,山形沉积物,浅浅风化的叶绿素,中度风化的叶绿素和浅谷填充物。该地区的特点是起伏的地形散布在低矮的岩石山丘中。高程在MSL上方从 ud860 m到1127 m。 Malur的年平均降雨量是722.0mm。 Dhakshina Pinakini udand Markarda Halla河流失了该地区。溪流表现出树突状至亚树突状的排水型式,并由Achaean时代的花岗岩和片麻岩岩层组成。根据不同的地貌 udunits,将四类地下水潜在区划为:(i)良好至良好(ii)良好至中度(iii)中度至贫困,以及(iv)贫困至非常贫困。

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