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首页> 外文期刊>Nature environment and pollution technology >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
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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在地带的地貌学制图–以印度卡纳塔克邦科拉尔区Malur Taluk为例

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摘要

The search for new groundwater resources is essential to sustained economic development in aridenvironment. The study area is part of Ponnaiyar river basin falling between N latitude of 12°48’24” to13°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, 57K/4 and 57 L/1 covering an area of 645 km 2 in Kolar District, which is highly drought prone in KarnatakaState, India. In the present paper, by a methodological approach based on remote sensing and GIS, drainageand hydrogeomorphological maps were prepared using the IRS-1 C & 1 D LISS-III and PAN merged satellitedata and geomorphic units. Denudational hill, residual hill, inselberg, pediment inselberg complex, pediment,shallow weathered pediplain, moderately weathered pediplain and valley fill shallow were identified. The areais characterised by undulating terrain interspersed by low ranges of rocky hills. The elevation ranges from860 m to 1127 m above MSL. The mean annual rainfall of Malur is 722.0mm. The River Dhakshina Pinakiniand Markarda Halla drain the area. The streams exhibit dendritic to sub dendritic type of drainage patternand comprise of granite and gneissic rock formations of Achaean age. On the basis of different geomorphicunits, four categories of groundwater potential zones were delineated as (i) very good to good (ii) good tomoderate (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地区的可持续经济发展至关重要。研究范围是Ponnaiyar流域的一部分,其北纬度介于12°48'24”至13°07'06'之间,东经77°50'30”至78°08'15”属于印度地形调查表57 G / 16、57 H / 13、57K / 4和57 L / 1在印度卡纳塔克邦极易发生干旱的可拉尔地区,面积645 km 2。本文采用基于遥感和GIS的方法,利用IRS-1 C和1 D LISS-III和PAN合并的卫星数据和地貌单位绘制了排水和水文地貌图。确定了齿状丘陵,残留丘陵,inselberg,山形沉积物inselberg复合体,山形沉积物,浅风化的pediplain,中度风化的pediplain和山谷填充浅。该地区的特点是起伏的地形散布在低矮的岩石山丘中。海拔范围在MSL之上860 m至1127 m。 Malur的年平均降雨量是722.0mm。 Dhakshina Pinakini河和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模式,由Achaean时代的花岗岩和片麻岩岩层组成。根据不同的地貌单元,将地下水的潜在地带划分为四类:(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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