王祯伟. 淮北煤田松散层底部含水层特性初析[J]. 煤田地质与勘探, 1990, 18(4): 36-38.
引用本文: 王祯伟. 淮北煤田松散层底部含水层特性初析[J]. 煤田地质与勘探, 1990, 18(4): 36-38.
A TRIAL STUDY ON THE CHARACTERISTICS OF THE AQUIFERS IN THE BASE OF THE SOFT LAYERS IN THE NORTH ANHUI COALFIELD[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(4): 36-38.
Citation: A TRIAL STUDY ON THE CHARACTERISTICS OF THE AQUIFERS IN THE BASE OF THE SOFT LAYERS IN THE NORTH ANHUI COALFIELD[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(4): 36-38.

淮北煤田松散层底部含水层特性初析

A TRIAL STUDY ON THE CHARACTERISTICS OF THE AQUIFERS IN THE BASE OF THE SOFT LAYERS IN THE NORTH ANHUI COALFIELD

  • 摘要: 淮北煤田新矿区松散层底部含水层水量是造成矿坑充水的主要水源之一,需了解其水文地质特性和可能危害。研究确认该含水层在本区的大部地区呈现富水性、透水性偏差,采用疏降措施是可取的。

     

    Abstract: The aquifers in the base of the soft layers is one of the main water sources for mining in a new mining area in the Norh Anhui coalfield.In order to estimate the potential hazard caused by the aquifers,it must study their hydrogeological characteristics.The study difined that the aquifers were rich in water but poor in permeability.therefore,drainage to lower water level may be adopted and will produce the hoped results.

     

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