9号矿Solotvino矿床岩溶水文地质系统、岩溶通道自夯实效果及洞穴治疗恢复前景

Vasyl Dyakiv
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引用次数: 1

摘要

介绍了索洛维诺盐矿(喀尔巴阡外地区)的地质构造、现代地质生态状况、水文地质和采矿地质条件。从灾害性涌水、技术活化岩溶主动开发和应急淹水三个方面,分析了n9矿盐岩溶发育的特点,并对盐岩溶发育进行了回顾性分析。揭示了Chorny Mochar地区岩溶通道的自夯效应,预测了n9矿排水和变态反应医院地下科室恢复的可能性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Karst hydrogelogical system of the Solotvino deposit, effect of self-tamping of the karst channel and prospects of recovery of speleotherapeutic treatment in mine N9
The description of the geological structure, the modern geoecological state, hydrogeological and mining-geological conditions of the Solotvyno salt deposit (Transcarpathian region) is given. Peculiarities of salt karst development are considered and a retrospective analysis of its development within the mine N 9 is carried out: from catastrophic water inflow, active development of technogenic-activated karst and emergency flooding. The effect of self-tamponing of the karst channel in the area of Chorny Mochar was revealed, which allows to predict the possibility of drainage of mine N 9 and restoration of the underground department of the allergy hospital.
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