首页> 外文期刊>British Journal of Applied Science and Technology >Hydrogeological Information SystemElaboration of Coastal Aquifer AQ-2 of Pointe-Noire, in the South-west of Congo-Brazzaville
【24h】

Hydrogeological Information SystemElaboration of Coastal Aquifer AQ-2 of Pointe-Noire, in the South-west of Congo-Brazzaville

机译:刚果布拉柴维尔西南角黑角沿海含水层AQ-2的水文地质信息系统

获取原文
       

摘要

The region of Pointe-Noire (south-west of Congo-Brazzaville) located on a coastal sedimentary basin of about 6 000 km2 is primarily formed by unconsolidated rocks with very little interstice porosity. It is made by a complex multi-aquifers system interconnected. Previous studies have highlighted the lack of data and the need to acquire a better knowledge of the groundwater resource in Pointe Noire. This study intends to represent and schematize the functions of the reservoir and the hydrodynamic behaviour of aquifer AQ-2. A Hydrogeological Information System (HIS) of aquifer AQ-2 is drawn up from historical reconstitution of the piezometric heads data carried out of various series of measurements from boreholes and piezometers .Two hydrological zones related to the topography and/or relief of study zone were identified: a zone of the littoral plain, characterized by protuberances and a strong depth of piezometric surface with hydraulic gradient of 0.03, revealing a flow of significant rate and an average permeability which represents a drainage weaker than the recharge; and a zone of the plateaux, characterized by a type of hydrogeologic structure called hydraulic threshold representing a fall of piezometric surface and hydraulic gradient (0.005 and 0.006), which can be explained by variations of flow rate or permeability. This morphology is imposed by two phenomena, the contribution of water of the plateau of Hinda on one hand and on the other hand, the general drainage direction revealed by the presence of the semipermeable facies.
机译:黑角地区(刚果-布拉柴维尔西南),位于约6000 km2的沿海沉积盆地上,主要由孔隙度很小的疏松岩石形成。它是由一个复杂的多含水层系统相互连接而成。先前的研究强调了缺乏数据,并且需要获得黑角地下水资源的更多知识。这项研究的目的是描述和示意储层的功能以及AQ-2含水层的水动力特性。 AQ-2含水层的水文地质信息系统(HIS)是根据对测压井头数据的历史重建而绘制的,这些数据是通过对钻孔和测压仪进行的一系列测量获得的。两个与地形和/或研究区起伏有关的水文区分别是确定为:沿岸平原的一个区域,其特征是突起和水压梯度为0.03的较大的测压表面深度,显示出明显的流量和平均渗透率,表示排水能力比补给力弱;高原地区,其特征是一种水文地质结构,称为水力阈值,代表压水面的下降和水力梯度(0.005和0.006),这可以用流速或渗透率的变化来解释。这种形态是由两种现象引起的,一方面是Hinda高原水的贡献,另一方面是半渗透相的存在揭示了总体的排水方向。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号