CAJ | 학술논문

青龙煤矿位于黔西县东南部，煤矿水文地质条件复杂，矿井易受水害威胁。为预防水害，利用水质分析成果和同位素分析对大气降水、地表水（驮煤河）、矿井水及各含水层地下水的水力联系进行了对比研究，认为区内长兴组与龙潭组、夜郎组玉龙山段含水层均存在一定的水力联系，龙潭组含水层与夜郎组玉龙山段含水层之间水力联系不密切；地下水与地表水（驮煤河）之间水力联系微弱；矿井涌水与大气降水关系密切，大气降水直接补给长兴组、龙潭组含水层，经含水层涌入矿井。
청룡매광위우검서현동남부，매광수문지질조건복잡，광정역수수해위협。위예방수해，이용수질분석성과화동위소분석대대기강수、지표수（타매하）、광정수급각함수층지하수적수력련계진행료대비연구，인위구내장흥조여룡담조、야랑조옥룡산단함수층균존재일정적수력련계，룡담조함수층여야랑조옥룡산단함수층지간수력련계불밀절；지하수여지표수（타매하）지간수력련계미약；광정용수여대기강수관계밀절，대기강수직접보급장흥조、룡담조함수층，경함수층용입광정。
The Qinglong coalmine is situated in the southeastern Qianxi County. It has complicated hydrogeological condition and threatened by water hazards. To prevent water hazard, the paper uses water quality and isotopic analyzed results, carried out contrast re?searches on hydraulic connections between atmospheric precipitation, surface water (Tuomeihe River), mine water and groundwater of aquifers. The result considered that between aquifers in Changxing and Longtan formations, Yulongshan Member of Yelang Formation have existed certain hydraulic connections. The connection between Longtan Formation aquifers and Yulongshan Member of Yelang Formation aquifers is not close. Connection between groundwater and surface water (Tuomeihe River) is weak. Relation between mine water and atmospheric precipitation is close; the later directly recharges aquifers in Changxing and Longtan formations, and then through aquifers flow into mines.