用户名: 密码: 验证码:
降水条件下排土场非饱和带水分运移规律模拟研究
详细信息    查看全文 | 推荐本文 |
  • 作者:郭峻
  • 关键词:排土场 ; 非饱和带 ; 优势路径 ; 含水率 ; 湿润峰 ; HYDRUS-2D
  • 中文刊名:ZSUX
  • 英文刊名:China Water Transport
  • 机构:昆明理工大学;
  • 出版日期:2019-07-15
  • 出版单位:中国水运(下半月)
  • 年:2019
  • 期:v.19
  • 语种:中文;
  • 页:ZSUX201907038
  • 页数:3
  • CN:07
  • ISSN:42-1395/U
  • 分类号:83-85
摘要
我国矿产资源十分丰富,普遍存在排土场随意堆积的现象。基于滤波算法随机生成的两种质地的排土场介质空间分布场,采用HYDRUS-2D模拟降雨强度为0.55cm/h条件下排土场非饱和带水分运移规律。通过观测点含水率变化及湿润峰下移来分析不同质地、倾斜层分布、侧向渗流对水分运移规律的影响。结果表明:排土场介质质地对非饱和带水分运移起着控制的作用,粗/细质介质的交界面具有阻滞和减渗作用。粗质介质的倾斜层空间分布影响着非饱和带中优势路径的形成,在重力势的作用下水分易汇聚于倾斜层的下界面处,粗质介质中湿润峰下移快于细质介质,细质介质中水分运移除了受到重力势的作用外,还会受到侧向土水势梯度的影响。
        
引文
[1]Benzaazoua M,Bruno Bussière,Demers I,et al.Integrated mine tailings management by combining environmental desulphurization and cemented paste backfill:Application to mine Doyon,Quebec,Canada[J].Minerals Engineering,2008,21(4):330-340.
    [2]魏忠义,白中科.露天矿大型排土场水蚀控制的径流分散概念及其分散措施[J].煤炭学报,2003,28(5):486-490.
    [3]Guebert M D,Gardner T W.Macropore flow on a reclaimed surface mine:infiltration and hillslope hydrology[J].Geomorp hology,2001,39(3):151-169.
    [4]Bailey B L,Smith L J D,Blowes D W,et al.The Diavik Waste Rock Project:Persistence of contaminants from blasting agents in waste rock effluent[J].Applied Geochemistry,2013,36(3):256-270.
    [5]Blackmore S,Smith L,Ulrich Mayer K,et al.Comparison of unsaturated flow and solute transport through waste rock at two experimental scales using temporal moments and numerical modeling[J].Journal of Contaminant Hydrology,2014,171:49-65.
    [6]Neuner M,Smith L,Blowes D W,et al.The Diavik waste rock project:Water flow through mine waste rock in a permafrost terrain[J].Applied Geochemistry,2013,36(Complete):222-233.
    [7]Amos,R.T.,D.W.Blowes,B.L.Bailey,D.C.Sego,L.Smith,and A.I.M.Ritchie.Waste-rock hydrogeology and geochemistry[J].Applied Geochemistry,2015,57:140-156.
    [8]Poisson J,Chouteau M,Aubertin M,et al.Geophysical experiments to image the shallow internal structure and the moisture distribution of a mine waste rock pile[J].Journal of Applied Geophysics,2009,67(2):179-192.
    [9]Azam S,Wilson G W,Herasymuik G,et al.Hydrogeological behaviour of an unsaturated waste rock pile:a case study at the Golden Sunlight Mine,Montana,USA[J].Bulletin of Engineering Geology and the Environment,2007,66(3):259-268.
    [10]Gelhar L W,Welty C,Rehfeldt K R.A Critical Review of Data on Field-Scale Dispersion in Aquifers[J].Water Resources Research,1992,28(7).
    [11]Jirí?im?nek,Genuchten M T V,Miroslav ejna.Dev elopment and applications of the HYDRUS and STANMOD software packages and related codes[J].Vadose Zone Journal,2008,72(9):587-600.
    [12]吴胜和,李文克.多点地质统计学-理论、应用与展望[J].古地理学报,2005,7(1):137-144.
    [13]Wu J,Zhang T,AndréJournel.Fast FILTERSIMSimulation with Score-based Distance[J].Mathematical Geosciences,2008,40(7):773-788.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700