铀矿地质
鈾礦地質
유광지질
URANIUM GEOLOGY
2015年
1期
57-64
,共8页
谢国发%吴志坚%傅光华%邓标荣%马英英
謝國髮%吳誌堅%傅光華%鄧標榮%馬英英
사국발%오지견%부광화%산표영%마영영
居隆庵 21 号带%水文地质%矿坑涌水量
居隆菴 21 號帶%水文地質%礦坑湧水量
거륭암 21 호대%수문지질%광갱용수량
Julong’an 21st zone%hydrological geology%mine water inflow
居隆庵菱形断块是相山地区重要铀资源基地,21号带地处居隆庵菱形断块的西部,水文地质条件属简单中等类型,相对其它矿床更为复杂.笔者采用狭长水平坑道法和水文地质比拟法对该矿床进行矿坑涌水量估算,其钻孔单位涌水量<0.1 L·(s-1·m-1),预测矿坑涌水量<29 m3·h-1.研究显示,矿床主要含水带(构造及裂隙)富水性弱且不均,导通性不强;而地下水补给条件好,水压高.在矿床开采过程中应加强监测,及时判断可能出现的涌水量变化情况,保证生产安全.
居隆菴蔆形斷塊是相山地區重要鈾資源基地,21號帶地處居隆菴蔆形斷塊的西部,水文地質條件屬簡單中等類型,相對其它礦床更為複雜.筆者採用狹長水平坑道法和水文地質比擬法對該礦床進行礦坑湧水量估算,其鑽孔單位湧水量<0.1 L·(s-1·m-1),預測礦坑湧水量<29 m3·h-1.研究顯示,礦床主要含水帶(構造及裂隙)富水性弱且不均,導通性不彊;而地下水補給條件好,水壓高.在礦床開採過程中應加彊鑑測,及時判斷可能齣現的湧水量變化情況,保證生產安全.
거륭암릉형단괴시상산지구중요유자원기지,21호대지처거륭암릉형단괴적서부,수문지질조건속간단중등류형,상대기타광상경위복잡.필자채용협장수평갱도법화수문지질비의법대해광상진행광갱용수량고산,기찬공단위용수량<0.1 L·(s-1·m-1),예측광갱용수량<29 m3·h-1.연구현시,광상주요함수대(구조급렬극)부수성약차불균,도통성불강;이지하수보급조건호,수압고.재광상개채과정중응가강감측,급시판단가능출현적용수량변화정황,보증생산안전.
Julong’an rhombus block is an important uranium resources base and the zone 21 is located in west of the block,and its hydrogeology is of simple middle type compared to the more complicated other ares.Narrow tunnel method and hydrogeologic analogy method was used for mine water inflow esti-mation,the drilling unit water inflow is lower than 0.1 L·s-1 ·m-1 ,and the perdiction of mine water inflow is less than 29m3 ·h-1 ,the main aquifer water of the deposit (structure fissure aquifer)is of weak and uneven capability,and conduction performance is not strong;but the groundwater is of good recharge condition and high water pressure.Monitorring should be strengthen in the mining process,so as to make in time judge of water inflow changes and to ensure the mining production.