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西山煤田岩溶陷落柱柱壁角特征研究及其意义

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[意义]随着采掘向深部延伸,岩溶陷落柱已成为华北煤田矿井开采最隐蔽的致灾地质因素之一.柱壁角是描述陷落柱形态特征的重要指标之一.[方法和结果]以西山煤田上下煤层综采均切割过的 265个岩溶陷落柱为数据源,通过分区、统计、函数构建、地质类比,挖掘西山煤田岩溶陷落柱柱壁角中蕴藏的地质信息,获得如下认识:(1)西山煤田陷落柱平均柱壁角为 84.29°,超 50%的陷落柱柱壁角在 85°~90°,平均柱壁角自西北到东南逐渐增大,从 82.05°增大到 87.57°.(2)西山煤田陷落柱柱壁角与 8号煤层揭露的陷落柱面积成反比,依据柱壁角与陷落柱面积大小关系,陷落柱划分为:充分塌陷陷落柱(90°~85°)、次充分塌陷陷落柱(<85°~81°)、不充分塌陷陷落柱(<81°);对应的2号煤层陷落柱面积分别为<556、556~1 700、>1 700 m2,等效半径为<13.3、13.3~23.3、>23.3 m;对应的8号煤层陷落柱面积分别为<1 250、1 250~2 750、>2 750 m2,半径分别为<20、20~30、>30 m.充分塌陷陷落柱一般发育有柱顶空腔,柱体结构较为松散,可导通顶板裂隙水与柱顶空腔水,以及底板承压奥灰水,是西山煤田导水陷落柱的一种重要类型.[结论]类比地质历史时期降雨量结果显示,具有"北柱南相"的西山煤田岩溶陷落柱,可能形成于气候湿热的古近纪渐新世时期,强烈的岩溶作用吸收了大气中的CO2,并锁定在沉积区,可能是导致全球大气CO2 含量急剧降低的重要原因.
Pillar wall angles of karst collapse pillars in the Xishan coalfield:Characteristics and implications
[Significance]As coal mining expands into deep parts,karst collapse pillars have become one of the most concealed disaster-causing geological factors in coal mining from mines in North China.The pillar wall angle of a col-lapse pillar serves as an important index used to describe the morphology of the collapse pillar.[Methods and Results]With 265 karst collapse pillars cut by the fully mechanized mining of the upper and lower coal seams in the Xishan coalfield as the data source,this study extracted the geological information contained in the pillar wall angles of karst collapse pillars in the Xishan coalfield through zoning,making statistics,function construction,and geological analogy,obtaining the following insights:(1)The collapse pillars in the Xishan coalfield exhibit an average pillar wall angle of 82.49°,with over 50%of them manifesting pillar wall angles ranging between 85° and 90°.Their average pillar wall angles increase gradually from 82.05° to 87.57° from northwest to southeast.(2)The wall angles of collapse pillars in the Xishan coalfield are inversely proportional to the areas of the collapse pillars revealed by the No.8 coal seam.Based on this relationship,the collapse pillars can be categorized into completely collapsed pillars(90°‒85°),less completely collapsed pillars(85°‒81°),and incompletely collapsed pillars(<81°).Correspondingly,collapse pillars in the No.2 coal seam exhibit areas of<556 m2,556‒1 700 m2,and>1 700 m2 and equivalent radii of<13.3 m,13.3-23.3 m,and>23.3 m.Furthermore,collapse pillars in the No.8 coal seam have areas of<1 250 m2,1 250‒2 750 m2,and>2 750 m2 and equivalent radii of<20 m,20‒30 m,and>30 m.The completely collapsed pillars generally exhibit cavities on their tops and loose structures,which can connect fracture water in the roofs to water in cavities on pillar tops and confined Ordovician limestone water in the floors.Therefore,completely collapsed pillars are significant hydraulically conduct-ive collapse pillars in the Xishan coalfield.[Conclusions]The analogy with rainfall in the geological history reveals that the karst collapse pillars in the Xishan coalfield,exhibiting the characteristics of karst sinkholes and caves in southern China,might have been formed during the Paleo-Oligocene with hot humid climates.During this period,CO2 in the at-mosphere was absorbed due to intense karstification and was then locked in sedimentary areas.This might be an import-ant reason for the sharp decrease in global CO2 concentration in the atmosphere.

Xishan coalfieldkarst collapse pillarpillar wall anglecompletely collapsed collapse pillarformation time

赵金贵、王江玮、杨高峰、郭敏泰

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太原理工大学 矿业工程学院,山西 太原 030024

山西焦煤集团,山西 太原 030024

西山煤田 岩溶陷落柱 柱壁角 充分塌陷陷落柱 形成时间

国家自然科学基金重大项目

42293352

2024

煤田地质与勘探
中煤科工集团西安研究院

煤田地质与勘探

CSTPCD北大核心
影响因子:1.079
ISSN:1001-1986
年,卷(期):2024.52(9)
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