Assessment of groundwater lowering for urban infrastructure works, a case study in Sumbe, Angola/Africa

C. G. Rampinelli, T. Smith, Ana Matos Lima, Charles Silva de Aguiar, Celestina Diniz, Janilson T. Araújo
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Abstract

This paper describes the hydrogeological study developed for Sumbe city, in Angola, Africa, to evaluate the feasibility of employing existing wells to drawdown the water table in the central area of the city both to facilitate the urban infrastructure implementation and to increase its lifespan. The hydraulic conductivity of the unsaturated zone was estimated based on the open hole and double ring infiltrometer tests conducted in several points of the site to capture the variability of the hydrogeologic condition of the zone of aeration. The transmissivity and the hydraulic conductivity of the saturation zone were estimated based on an pumping test performed in a pumping well and two monitoring wells. Hand auger, SPT and rotary boring were carried out and combined with all field data information to produce a simplified conceptual model of the hydrogeologic system for the study site. Based on the survey data and by applying the Dupuit approximation of the Boussinesq equation for unconfined aquifers, the piezometric surface and the radius of influence of the well were computed for an operational steady condition. The study demonstrated that the entire site location is on a thick layer of clay and employing wells for groundwater lowering is unfeasible for either permanent or temporary purposes. For temporary groundwater lowering, collecting the water drained at the excavation by direct pumping was suggested. Finally, additional considerations regarding the sewerage/stormwater systems and the drainage system for the pavement base were also addressed. Keywords: groundwater lowering; infrastructure; hydraulic conductivity; influence radius of wells.
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对城市基础设施工程降低地下水的评估,安哥拉/非洲桑贝的案例研究
本文描述了在非洲安哥拉Sumbe市开展的水文地质研究,以评估利用现有井降低城市中心地区地下水位的可行性,以促进城市基础设施的实施并延长其使用寿命。通过在现场几个点进行的裸眼和双环渗透仪试验,以捕捉曝气区水文地质条件的变化,估算了非饱和区的水力导电性。通过对一口泵井和两口监测井的泵送试验,估算了饱和层的渗透率和导水率。通过手动螺旋钻、SPT和旋转钻孔,结合所有现场数据信息,为研究地点建立了简化的水文地质系统概念模型。根据实测资料,应用无承压含水层Boussinesq方程的Dupuit近似,计算了运行稳定条件下的承压面和井的影响半径。研究表明,整个场地位于一层厚厚的粘土上,无论是永久还是临时目的,使用井来降低地下水都是不可行的。对于临时降低地下水,建议采用直接抽水的方式收集开挖时排出的水。最后,还讨论了有关污水/雨水系统和路面基础排水系统的其他考虑因素。关键词:地下水降压;基础设施;渗透系数;井的影响半径。
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