Present Geothermal Field and Roadway Heat Damage Characteristics in Zhujidong Coal Mine Area of Huainan City, Anhui Province, China

Weijing Yao, Jinxiu Han, Yu Liu, Yongwen Deng, Jianyong Pang
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Abstract

: With the normalization of deep mining, the problem of mine thermal damage has been widely concerned. In this paper, 64 logging temperature data of surface boreholes of Zhujidong coalfield in Huainan City, Anhui Province, China, were summarized and sorted. The temperature data of 12 measuring points at the current main working level of − 906 m and − 965 m were measured. The ground temperature conditions of the vertical direction, horizontal direction, and main coal seam floor in the coalfield were analyzed. The characteristics of the present geothermal field and roadway heat damage, and its influencing factors were discussed. The results showed that the geothermal gradients of this area are between 1.7 ℃ /hm and 3.6 ℃ /hm, and the average geothermal gradient is 2.607 ℃ /hm. It shows the transmission of warming in the vertical direction and horizontal direction shows the ground temperature lowering from south to north, east to west. The geothermal field in this area is mainly affected by the geological structure, and the thermal physical properties of rocks, magmatic rocks and groundwater activities also have a certain effect. At present, most of the main work level has reached the first heat hazard area, and some are in the second heat hazard area, according to Chinese regulations. The working face temperature is keeping above 28 7 ℃ and the relative humidity is being maintained above 70% for a long time. The problem of heat damage is extremely serious. It is suggested to construct the thermal environment control measures combining active and passive ways.
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安徽省淮南市朱集东煤矿区地热场现状及巷道热害特征
:随着深部开采的常态化,矿井热害问题受到广泛关注。本文对安徽省淮南市朱集东煤田 64 个地面钻孔的测井温度数据进行了汇总和整理。测量了当前主要工作面-906 米和-965 米处 12 个测点的温度数据。分析了煤田垂直方向、水平方向和主煤层底板的地温状况。讨论了当前地热田和巷道热害的特征及其影响因素。结果表明,该地区地热梯度在 1.7 ℃ /hm 至 3.6 ℃ /hm 之间,平均地热梯度为 2.607 ℃ /hm。地热梯度在垂直方向上表现为升温传递,在水平方向上表现为地温由南向北、由东向西降低。该地区地热田主要受地质构造影响,岩石热物性、岩浆岩及地下水活动也有一定影响。目前,根据中国的规定,大部分主要工作面已达到第一热危险区,部分处于第二热危险区。工作面温度长期保持在 28 7℃以上,相对湿度长期保持在 70%以上。热害问题极为严重。建议采取主动与被动相结合的热环境控制措施。
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