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2020 | OriginalPaper | Buchkapitel

1. Introduction

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Abstract

Coal is an important energy resource in China. The coal production concerns the national economy and the people’s livelihood as well as the sustainable and stable development of the economic society. The North China Coalfields (NCCs) are important coalfields in China, also the coalfields that have been most seriously threatened by groundwater hazards. The major coal seams in these coalfields are located in the Permo-Carboniferous strata. Because the Lower Carboniferous, Devonian, Silurian and Upper Ordovician formations are generally absent in the coalfields, the Permo-Carboniferous strata overly directly the massive Middle Ordovician limestone. Mining practices in these coal mines demonstrate that the Middle Ordovician limestone is a strong aquifer with very heterogeneous karst fractures and characterized by intense recharge and high water pressure. The Ordovician limestone constitutes the major threatening water source from the coal seam floor. In order to accomplish safe mining of the deep coal resources under water pressure, the research on utilization and grouting reconstruction technology of the TOL is extremely urgent and imperative.

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Metadaten
Titel
Introduction
verfasst von
Hao Wang
Copyright-Jahr
2020
DOI
https://doi.org/10.1007/978-3-030-40116-0_1