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首页> 外文期刊>Journal of Water Resource and Protection >Assessment of Hydraulic Parameters and Protection Zones of Catchment Aquifers for Water Supply Network in Ndé Division, West-Cameroon (Central Africa)
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Assessment of Hydraulic Parameters and Protection Zones of Catchment Aquifers for Water Supply Network in Ndé Division, West-Cameroon (Central Africa)

机译:在ND&amp中的供水网络水力参数和液压参数和保护区的评估。#233; 西喀麦隆(中非)

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摘要

Ndé Division in West-Cameroon is facing with water supply although many attempts of restoring existing SCANWATER facilities by Bangangté Municipality. In order to address the issue, we assess the exploitable pumping flow rate of catchment aquifers and its hydraulic properties by using Jacob and Theis method, and define protection zones with Hoffman and Lillich method. It emerges that the hydraulic conductivity of aquifer is in the order of 10~(-4) m/sec, transmissivity varies from 10~(-4) to 10~(-6) m~(2)/sec. Aquifer pumping flow rate (Q) varies between 1.5 and 10.5 m~(3)/h. In volcanic rocks, aquifer is more productive (4.5 ≤ Q ≤ 10.5 m~(3)/h). Transfer time of pollutants to aquifer varies from 3 to 56 days depending on rock-types and groundwater slope (0.03 - 0.13 m/m). Furthermore, 113,624 m and 1123 m are radius to be implemented for a better protection of groundwater against any form of pollutant.
机译:Ndé师在West-Cameroon面临水供应,虽然许多尝试由PangangtéMunicipality恢复现有的Scanwater设施。 为了解决这个问题,我们通过使用雅各和THEIS方法来评估集水器含水层及其液压性能的可利用泵送流速,以及用Hoffman和Lillich方法定义保护区。 它出现了含水层的液压导电性大约为10〜( - 4)M / sec,透射率从10〜(-4)到10〜(-6)m〜(2)/秒。 含水层泵送流量(Q)在1.5和10.5 m〜(3)/ h之间变化。 在火山岩中,含水层更加成熟(4.5≤q≤1.5m〜(3)/ h)。 污染物对含水层的转移时间根据岩石类型和地下水斜率(0.03-0.13 m / m)而异。 此外,113,624 m和1123m是用于更好地保护地下水的半径,以更好地保护任何形式的污染物。

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