山东国土资源
山東國土資源
산동국토자원
LAND AND RESOURCES IN SHANGDONG PROVINCE
2014年
8期
58-62
,共5页
大南湖矿区%烧变岩层%群孔抽水试验%地下水流场%新疆哈密
大南湖礦區%燒變巖層%群孔抽水試驗%地下水流場%新疆哈密
대남호광구%소변암층%군공추수시험%지하수류장%신강합밀
Burnt rocks%group drilling pumping test%groundwater flow field%Dananhu mining area
新疆哈密大南湖矿区北露天煤矿首采区东南部需要揭露Ⅲ火烧岩区一部分,这使得烧变岩水成为露天煤矿矿井充水的主要水源。资源勘探阶段的水文地质资料表明,烧变岩区赋水空间发育、透水能力强,储存量非常可观,但由于受资源勘探阶段水文地质勘探工程量制约,水文地质条件未能详细查明。因此为达到查明烧变岩地下水水力联系、水质变化情况,充分暴露Ⅲ火烧区烧变岩的水文地质条件的目的,设计了该次群孔抽水试验。该次试验查明了烧变岩含水层的水文地质条件,为烧变岩地质条件下防治水工作提供了依据。综合分析表明Ⅲ火烧区烧变岩为储存量型含水层,其补给条件差。
新疆哈密大南湖礦區北露天煤礦首採區東南部需要揭露Ⅲ火燒巖區一部分,這使得燒變巖水成為露天煤礦礦井充水的主要水源。資源勘探階段的水文地質資料錶明,燒變巖區賦水空間髮育、透水能力彊,儲存量非常可觀,但由于受資源勘探階段水文地質勘探工程量製約,水文地質條件未能詳細查明。因此為達到查明燒變巖地下水水力聯繫、水質變化情況,充分暴露Ⅲ火燒區燒變巖的水文地質條件的目的,設計瞭該次群孔抽水試驗。該次試驗查明瞭燒變巖含水層的水文地質條件,為燒變巖地質條件下防治水工作提供瞭依據。綜閤分析錶明Ⅲ火燒區燒變巖為儲存量型含水層,其補給條件差。
신강합밀대남호광구북로천매광수채구동남부수요게로Ⅲ화소암구일부분,저사득소변암수성위로천매광광정충수적주요수원。자원감탐계단적수문지질자료표명,소변암구부수공간발육、투수능력강,저존량비상가관,단유우수자원감탐계단수문지질감탐공정량제약,수문지질조건미능상세사명。인차위체도사명소변암지하수수력련계、수질변화정황,충분폭로Ⅲ화소구소변암적수문지질조건적목적,설계료해차군공추수시험。해차시험사명료소변암함수층적수문지질조건,위소변암지질조건하방치수공작제공료의거。종합분석표명Ⅲ화소구소변암위저존량형함수층,기보급조건차。
Portions of the Ⅲ burnt rocks in south part of the first mining area of northern open pit coal mine in Dananhu mine of Hami in Xinjiang should be exposed.It makes the burnt rock water become the main source of mine water filling.As showed by hydrogeological data in exploration stage,water bearing space in burnt rock area developed well with permeable capability and large storage capacity.Due to the limit of hydrogeological exploration engineering amount in exploration stage,hydrogeological condition has not been identified in detail.In order to find out water contact and the groundwater water quality changes of burnt rock,and to fully expose the hydrogeological conditions of the burnt rocks in Ⅲ burning area, group drilling pumping test has been designed.This test has identified hydrogeological conditions of burnt rocks,provided the basis for water prevention work under the condition of burnt rock.Through compre-hensive analysis,it is showed the burnt rocks in Ⅲ burning area are aquifer storage capacity type with poor supply conditions.