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首页> 外文期刊>Journal of the Geological Society of India >Hydrogeology of a buried channel, village Shenoli, District Satara, Maharashtra
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Hydrogeology of a buried channel, village Shenoli, District Satara, Maharashtra

机译：马哈拉施特拉邦萨塔拉地区Shenoli村庄的掩埋河道水文地质

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摘要

A buried channel has been located, in the basaltic terrain, near village Shenoli, District Satara, Maharashtra. It is composed of a gritty mass formed of a semi-consolidated material. The resistivity value of the semi-consolidated formation is 6.30 Ohm — m whereas the resistivity values of the vesicular basalts range between 18 and 32 Ohm-m. The specific capacity, unit area specific capacity, specific capacity index, transmissivity and hydraulic conductivity, with respect of the buried channel, are 609.07 LPM/m of drawdown, 12.12 LPM/m3, 95.47 LPM/m2, 353.26 m2/day and 55.37 m/day, respectively whereas the values of these parameters for basalt aquifers range from 67 to 117 LPM/m of drawdown, 0.7 to 4.27 LPM/m3, 14.08 to 31.04 LPM/m2, 33.5 to 73.71 m2/day and 9.44 to 18.32 m/day, respectively. A comparison of the well characteristics and aquifer parameters reveal that the buried channel with semi-consolidated formation has distinctly better groundwater yielding properties.
机译：在玄武岩地形中，一个埋藏的河道位于马哈拉施特拉邦Satara区的Shenoli村附近。它由半固结材料形成的坚硬质料组成。半固结地层的电阻率值为6.30欧姆·米，而水泡玄武岩的电阻率值则在18至32欧姆·米之间。相对于地下通道的比容量，单位面积比容量，比容量指数，透射率和水力传导率分别为609.07 LPM / m降水量，12.12 LPM / m3 ，95.47 LPM / m2 分别为353.26 m2 /天和55.37 m / day，而玄武岩含水层这些参数的取值范围分别为67至117 LPM / m降落，0.7至4.27 LPM / m3 ，14.08至31.04 LPM / m2 ，分别为33.5至73.71 m2 /天和9.44至18.32 m /天。井特征和含水层参数的比较表明，半固结地层的埋藏河道具有明显更好的地下水产出特性。

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