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Aquifer Potential Assessment in Termites Manifested Locales Using Geo-Electrical and Surface Hydraulic Measurement Parameters

机译:利用地电和地表水力测量参数评估白蚁表现出的区域中的含水层潜力

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摘要

In some parts of tropical Africa, termite mound locations are traditionally used to site groundwater structures mainly in the form of hand-dug wells with high success rates. However, the scientific rationale behind the use of mounds as prospective sites for locating groundwater structures has not been thoroughly investigated. In this paper, locations and structural features of termite mounds were mapped with the aim of determining the aquifer potential beneath termite mounds and comparing the same with adjacent areas, 10 m away. Soil and species sampling, field surveys and laboratory analyses to obtain data on physical, hydraulic and geo-electrical parameters from termite mounds and adjacent control areas followed. The physical and hydraulic measurements demonstrated relatively higher infiltration rates and lower soil water content on mound soils compared with the surrounding areas. To assess the aquifer potential, vertical electrical soundings were conducted on 28 termite mounds sites and adjacent control areas. Three (3) important parameters were assessed to compute potential weights for each Vertical Electrical Sounding (VES) point: Depth to bedrock, aquifer layer resistivity and fresh/fractured bedrock resistivity. These weights were then compared between those of termite mound sites and those from control areas. The result revealed that about 43% of mound sites have greater aquifer potential compared to the surrounding areas, whereas 28.5% of mounds have equal and lower potentials compared with the surrounding areas. The study concludes that termite mounds locations are suitable spots for groundwater prospecting owing to the deeper regolith layer beneath them which suggests that termites either have the ability to locate places with a deeper weathering horizon or are themselves agents of biological weathering. Further studies to check how representative our study area is of other areas with similar termite activities are recommended.
机译:在非洲热带地区的某些地区,传统上以白蚁丘位置为主要位置,以手挖井的形式定位地下水结构,成功率很高。但是,尚未对利用土丘作为寻找地下水结构的潜在场所的科学依据进行深入研究。在本文中,绘制了白蚁丘的位置和结构特征,以便确定白蚁丘下方的含水层电势,并将其与10 m处的相邻区域进行比较。随后进行土壤和物种采样,现场调查和实验室分析,以获取白蚁丘和邻近控制区域的物理,水力和地电参数数据。物理和水力测量表明,与周围地区相比,丘陵土壤的渗透率较高,土壤含水量较低。为了评估含水层的潜力,在28个白蚁丘遗址和邻近的控制区域进行了垂直电测深。评估了三(3)个重要参数,以计算每个垂直电测深(VES)点的潜在权重:基岩深度,含水层电阻率和新鲜/破裂基岩电阻率。然后将这些重量在白蚁丘部位的重量与对照地区的重量之间进行比较。结果表明,与周围地区相比,约有43%的土墩位具有更大的含水层潜力,而与周围地区相比,约有28.5%的土墩具有相等且更低的潜力。该研究得出的结论是,白蚁丘的位置较深,这是白蚁丘位置较适合地下水开采的地方,这表明白蚁有能力找到较深的风化层或自身是生物风化的媒介。建议进行进一步研究,以检查我们的研究区域在具有类似白蚁活动的其他区域中的代表性。

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