摘要
邯邢地区西部武安—涉县古生代凹陷中,沉积了一套厚大的寒武—奥陶系的碳酸盐岩,是本区岩溶水的主要赋存层位。邯邢地区的工、农业及生活用水主要是依靠岩溶水资源。但该区埋藏着丰富的铁、煤等矿产,由于地下岩溶水丰富又给矿山的开采造成很大的困难,为了解决这一矛盾,处理好供排关系,充分开发利用铁、煤矿产和地下水资源,本文提出一些探索性看法。
To exploit iron and coal deposits of Handan-Xingtai district, the principal characteristics of water movement of Ordovician limestone must be understood. According to different hydrogeological conditions, different measures may be taken to different water abundance of aquifers and water bursting in order to make full use of iron and coal resources of Handan-Xingtai district. The existing water supply system and the guarantee of drinking and industrial use must be claimed precedence. In this way, more reasonable distribution scheme of water supply and better exploitation of iron, coal and water resources of the region could be obtained
出处
《中国岩溶》
CAS
CSCD
北大核心
1989年第3期208-212,共5页
Carsologica Sinica
