印度奥里萨邦Sambalpur地区干旱易发地区Kuchinda和Bamra区块的电阻率法地下水调查

N. Mahanta
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引用次数: 1

摘要

对Sambalpur地区北部Kuchinda分区的干旱易发区Kuchinda和Bamra地块的水文地质研究表明,主要为固结地层,缺乏原生孔隙。在风化带和裂隙带中,地下水可在无约束和半约束条件下发生。虽然整个分区的地下水资源开发不足,但从夏季井干和多年来地下水位深度的增加可以看出,许多地方存在局部性的短缺。在全区26个地点的电阻率测量中,发现了3 ~ 5层状地下岩石分布。第二层和第三层适合地下水的储存和移动,因此可以开发地下水。潜在的裂缝带被限制在地表以下27至174.5米的深度。
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Groundwater Investigation by Resistivity Method In The Drought-Prone Kuchinda and Bamra Blocks, Sambalpur District, Odisha, India
: Hydrogeological studies in drought-prone Kuchinda and Bamra blocks of Kuchinda Subdivision in northern part of Sambalpur district has indicated predominance of consolidated formations lacking primary porosity. Groundwater occurs both under unconfined and semiconfined conditions in the weathered and fractured zones. Although, there is underdevelopment of groundwater resources in the subdivision as a whole, localized scarcity is found in many places as evidenced from dry wells in summer and increase in the depth of water table over the years. Resistivity survey in 26 locations of the area has indicated 3 to 5 layer cases in the disposition of subsurface rocks. The second and third layers are suitable for groundwater storage and movement and hence can be developed for groundwater. The potential fracture zones are restricted to a depth of 27 to 174.5 m below the ground level.
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