安徽理工大学学报(自然科学版)
安徽理工大學學報(自然科學版)
안휘리공대학학보(자연과학판)
JOURNAL OF ANHUI UNIVERSITY OF SCIENCE AND TECHNOLOGY(NATURAL SCIENCE)
2015年
1期
45-49
,共5页
降雨入渗%非饱和渗流%尾矿库%排土场%基质吸力
降雨入滲%非飽和滲流%尾礦庫%排土場%基質吸力
강우입삼%비포화삼류%미광고%배토장%기질흡력
Rainfall infiltration%unsaturated seepage%tailing pond%waster dump%matric suction
尾矿库和排土场都是高势能的泥石流重大危险源,二者的降雨入渗特性均较复杂。而当高等级排土场位于大型尾矿库的下游时,其复杂性更不言而喻。通过对太和铁矿的工程实例分析,计算得到尾矿库在千年一遇洪水条件下的浸润线分布,将其导入到排土场中作为初始条件,计算得到初始浸润线;再据此分析整个研究区域的降雨条件下入渗特性。研究结果表明,尾矿库内的浸润线分布对下游排土场的影响很大,入渗作用改变了排土场边坡内的地下水渗流场,而地下水的升高则是一个缓慢的过程。
尾礦庫和排土場都是高勢能的泥石流重大危險源,二者的降雨入滲特性均較複雜。而噹高等級排土場位于大型尾礦庫的下遊時,其複雜性更不言而喻。通過對太和鐵礦的工程實例分析,計算得到尾礦庫在韆年一遇洪水條件下的浸潤線分佈,將其導入到排土場中作為初始條件,計算得到初始浸潤線;再據此分析整箇研究區域的降雨條件下入滲特性。研究結果錶明,尾礦庫內的浸潤線分佈對下遊排土場的影響很大,入滲作用改變瞭排土場邊坡內的地下水滲流場,而地下水的升高則是一箇緩慢的過程。
미광고화배토장도시고세능적니석류중대위험원,이자적강우입삼특성균교복잡。이당고등급배토장위우대형미광고적하유시,기복잡성경불언이유。통과대태화철광적공정실례분석,계산득도미광고재천년일우홍수조건하적침윤선분포,장기도입도배토장중작위초시조건,계산득도초시침윤선;재거차분석정개연구구역적강우조건하입삼특성。연구결과표명,미광고내적침윤선분포대하유배토장적영향흔대,입삼작용개변료배토장변파내적지하수삼류장,이지하수적승고칙시일개완만적과정。
Both of tailing pond and waster dump is high -potential fatal danger fountainhead for debris flow , and the infiltration characteristic are all complex of them .Especially , when a high-class dump is downstream of a large-scale tailing pond , the degree of complexity is more self -evident .Based on the engineering instance a-nalysis of Taihe Iron Mining , phreatic line under the case of the millennium of the tailing pond was obtained , which is introduced into the waster dump model as an initial condition to calculate the initial phreatic line .On the basis, the infiltration characteristic in the entire area under rainfall was analyzed .The study results showed that the phreatic line distribution in the tailing pond has great influence on the waster dump at downstream , the groundwater seepage field in the dump was changed by the infiltration , and the rise of groundwater is a slow .