工程地质学报
工程地質學報
공정지질학보
2015年
4期
784-789
,共6页
郭捷%马凤山%赵海军%李克蓬%吕树新%原冬成
郭捷%馬鳳山%趙海軍%李剋蓬%呂樹新%原鼕成
곽첩%마봉산%조해군%리극봉%려수신%원동성
海底金矿%突涌水%新构造断裂%导水优势通道%连通性
海底金礦%突湧水%新構造斷裂%導水優勢通道%連通性
해저금광%돌용수%신구조단렬%도수우세통도%련통성
Seabed gold mine%Water inrush%Neotectonic fracture%Water preferential pathway%Connectivity
在对巷道导水裂隙详细调查量测的基础上,通过对导水裂隙产状的归纳总结,结合涌水水样的温度、矿化度及氢、氧同位素的动态监测结果,分析了三山岛金矿两个矿区的渗流优势方位以及矿坑水与地表水体的连通性。研究表明:西山矿区的渗流优势方位与最大水平地应力平行,而新立矿区的渗流优势方位与最大水平地应力近于垂直;西山矿区存在海水、基岩咸水和第四系淡水的稳定补给,新立矿区的咸水和淡水补给量不断减小,海水补给量不断增大;新构造断裂对矿区渗流优势方位的控制作用大于采动裂隙,使得西山矿坑与地表水体存在良好的连通性,也控制着海水补给矿坑的方式;而新立矿仅在采动裂隙的影响下与海水、咸水和淡水存在较弱的连通性。
在對巷道導水裂隙詳細調查量測的基礎上,通過對導水裂隙產狀的歸納總結,結閤湧水水樣的溫度、礦化度及氫、氧同位素的動態鑑測結果,分析瞭三山島金礦兩箇礦區的滲流優勢方位以及礦坑水與地錶水體的連通性。研究錶明:西山礦區的滲流優勢方位與最大水平地應力平行,而新立礦區的滲流優勢方位與最大水平地應力近于垂直;西山礦區存在海水、基巖鹹水和第四繫淡水的穩定補給,新立礦區的鹹水和淡水補給量不斷減小,海水補給量不斷增大;新構造斷裂對礦區滲流優勢方位的控製作用大于採動裂隙,使得西山礦坑與地錶水體存在良好的連通性,也控製著海水補給礦坑的方式;而新立礦僅在採動裂隙的影響下與海水、鹹水和淡水存在較弱的連通性。
재대항도도수렬극상세조사량측적기출상,통과대도수렬극산상적귀납총결,결합용수수양적온도、광화도급경、양동위소적동태감측결과,분석료삼산도금광량개광구적삼류우세방위이급광갱수여지표수체적련통성。연구표명:서산광구적삼류우세방위여최대수평지응력평행,이신립광구적삼류우세방위여최대수평지응력근우수직;서산광구존재해수、기암함수화제사계담수적은정보급,신립광구적함수화담수보급량불단감소,해수보급량불단증대;신구조단렬대광구삼류우세방위적공제작용대우채동렬극,사득서산광갱여지표수체존재량호적련통성,야공제착해수보급광갱적방식;이신립광부재채동렬극적영향하여해수、함수화담수존재교약적련통성。
This paper is based on the detailed investigation of roadway water flowing fractures for the waterseepage.It analyzes the connectivity advantage of orientation and mine water seepage and surface water bodies oftwo gold mines at Sanshadao.It summarizes the distribution of crack occurrence,and gushing water sampletemperature,salinity and dynamic monitoring of the results of hydrogen and oxygen isotope.The study shows thatthe waterseepage dominant orientation in the district of Xishan mine is parallel to the maximum horizontal principalstress.The optimal direction of Xinli mine water seepage is nearly perpendicular to the maximum horizontalprincipal stress.The Xishan mine has stable recharge of seawater,rock saline,and Quaternary fresh water.In theXinli mine,the proportions of saline and fresh water in inrushing water in mine pits are diminishing gradually,asthe seawater increases.The role of neotectonic fractures in controlling the dominant orientations of mine waterseepage is stronger than that of fractures developed by excavation.The neotectonic fractures make the Xishan minehave well connectivity with surface waters and control the recharge process of the seawater.There is weaker connectedness between pits and surface waters in the Xinli mine which attributes to the mininginduced fractures.