用户名: 密码: 验证码:
高放废物地质处置阿拉善预选区巴彦诺日公地段目标深度岩体质量预测
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Prediction of Rock Mass Quality at Target Depth for the Bayannuorigong Section of the Alxa Pre-Selected Region for Geological Disposal of High-Level Nuclear Waste
  • 作者:袁广祥 ; 张路青 ; 曾庆利 ; 黄志全 ; 王四巍 ; 王洪建 ; 邓绪彪
  • 英文作者:YUAN Guangxiang;ZHANG Luqing;ZENG Qingli;HUANG Zhiquan;WANG Siwei;WANG Hongjian;DENG Xubiao;College of Geosciences and Engineering,North China University of Water Resources and Electric Power;Institute of Geology and Geophysics,Chinese Academy of Sciences;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences;
  • 关键词:高放废物地质处置 ; 目标深度岩体 ; 岩体质量 ; 预测 ; 巴彦诺日公地段 ; 阿拉善预选区
  • 英文关键词:geological disposal of high-level nuclear waste;;rock mass at target depth;;classification of rock mass;;prediction;;Bayannuorigong section;;Alxa pre-selected region
  • 中文刊名:DZKT
  • 英文刊名:Geology and Exploration
  • 机构:华北水利水电大学地球科学与工程学院;中国科学院地质与地球物理研究所;中国科学院大学地球与行星科学学院;
  • 出版日期:2019-05-15
  • 出版单位:地质与勘探
  • 年:2019
  • 期:v.55;No.484
  • 基金:河南省高等学校青年骨干教师资助计划(编号:2015GGJS-105);; 国家自然科学基金项目(编号:41402269、U1704243、41741019、51704120、41502267);; 华北水利水电大学青年科技创新人才项目联合资助
  • 语种:中文;
  • 页:DZKT201903016
  • 页数:10
  • CN:03
  • ISSN:11-2043/P
  • 分类号:170-179
摘要
高放废物地质处置阿拉善预选区巴彦诺日公地段位于阿拉善地块东部,主要由二叠纪花岗岩构成,地壳次稳定。通过踏勘,确定了2个钻孔,布置了若干条物探剖面。以这2个钻孔为中心,在17km×17km范围内进行了工程地质测绘,获得了地表结构面分布特征。地表岩体质量以Ⅲ级岩体为主,地表以下3m~4m处多为Ⅰ级和Ⅱ级岩体。根据钻孔岩心编录和力学试验数据,对岩心质量进行评价,岩心整体质量较好,以Ⅰ级和Ⅱ级岩体为主。对比岩体质量和测井数据,发现岩体质量与岩体的物理参数具有明显的相关性。通过和CSAMT剖面上对应位置的对比,建立了岩体质量与电阻率的关系。结合地表岩体质量、钻孔岩心质量和物探剖面,对目标深度岩体进行了预测:目标深度(600m深左右)岩体质量以Ⅰ级岩体为主,局部有Ⅱ级岩体和Ⅲ级岩体。
        The Bayannuorigong section of the Alxa pre-selected region for geological disposal of high-level nuclear waste is located in the eastern Alxa block,where the crust consists of Permian granite with sub-stability. According to reconnaissance,two boreholes and some geophysical survey lines were deployed. And engineering geological mapping was carried out in a 17 km × 17 km range to probe the distribution of discontinuities. The surface rock mass is dominated by grade III,and 3 ~ 4 m below the surface is mostly grades I and II. According to core logging and mechanical tests,the drill cores are categorized as types I and II. Comparison of rock mass quality and well logging data shows an obvious correlation between quality and physical parameters of the rock mass. Therefore,the relationship between rock mass quality and resistivity can be established. Combining with the quality of surface rock mass and drilling cores and geophysical prospecting profiles,the quality of rock mass at the target depth has been predicted: rock mass is dominated by grade I,and some are of grades II and III.
引文
Chen Hong.2015.Geological characteristics of the Permian intrusive rocks along the Bayan noel of Alxa,Inner Mongolia[D].Beijing:China University of Geosciences(Beijing):6-9(in Chinese with English abstract).
    Dan Wei,Li Xianhua,Wang Qiang,Tang Gongjian,Liu Yu.2014.An Early Permian(ca.280Ma)silicic igneous province in the Alxa block,NW China:A magmatic flare-up triggered by a mantleplume?[J].Lithos,204(3):144-158.
    Fan Honghai,Min Maozhong,Chen Jia,Ji Ruili.2005.Isotopic geochemical characteristics of Yemaquan granitic intrusions in Beishan area,Gansu Province[J].Acta Geoscientica Sinica,26(suppl):78-83(in Chinese with English abstract).
    Gao Zhenbing,Gong Yuling,Zhang Hua.2013.Application of EH4method to high level radioactive waste preselected site-Taking the Beishanxiangyang Mountain to Xinchang area of Gansu Province as an example[J].Chinese Journal of Engineering Geophysics,10(2):156-160(in Chinese with English abstract).
    Geng Yuansheng,Wang Xingshe,Shen Qihan,Wu Chunming.2006.Redefinition of the Alxa group-complex(Precambrian metamorphic basement)in the Alxa area,Inner Mongolia[J].Geology in China,33(1):138-145(in Chinese with English abstract).
    Geng Yuansheng,Wang Xingshe,Wu Chunming,Zhou Xiwen.2010.Late-Paleoproterozoic tectonothermal events of the metamorphic basement in Alxa area:Evidence from geochronology[J].Acta Petrologica Sinica,26(4):1159-1170(in Chinese with English abstract).
    Guo Yonghai,He Jianguo,Zhou Zhichao,Zhou Zhichao,Dong Jiannan,Ji Ruili,Zhang Ming,Li Jibiao.2016.Regional hydrogeological characteristics of Aqishan preselected area for China's high level radioactive waste disposal repository[J].Uranium Geology,32(4):251-256(in Chinese with English abstract).
    Guo Yonghai,Li Nana,Zhou Zhichao,Dong Jiannan,Zhang Ming,Liu Shufen.2016.Characteristics and implications of groundwater isotopes in Yamansu and Tianhu preselected section for China's high level radioactive waste disposal repository[J].Acta Geologica Sinica,90(2):376-382(in Chinese with English abstract).
    Guo Yonghai,Wang Ju,LüChuanhe,Liu Shufen,Zhong Zihua.2005.Chemical characteristics of groundwater and waterrock interaction:Modeling of the Yemaquan preselected area for China's high level radioactive waste repository[J].Earth Science Frontiers,12(suppl 1):117-123(in Chinese with English abstract).
    JinYuanxin,Min Maozhong,Chen Weiming,Zhao Honggang.2007.Study on granite characteristics of Xinchang section of candidate Beishan area,Gansu Province[J].Chinese Journal of Rock Mechanics&Engineering,26(suppl 2):3974-3981(in Chinese with English abstract).
    Wan Haitao,Gong Yuling,Zhang Hua.2015.Application of MT method to high level radioactive waste preselected site-Taking the Beishanxiangyang Mountain to Xinchang area of Gansu Province as an example[J].Chinese Journal of Engineering Geophysics,12(2):157-161(in Chinese with English abstract).
    Wan Hanping,Xu Guilai,Yu Xiang,Cui Huanmin.2015.The geophysics evaluation on granite type of high-level radioactive waste disposal repository-taking Aqishan potential site as an example[J].Progress in Geophysics,30(6):2778-2784(in Chinese with English abstract).
    Wang Ju.2008.Geological disposal of high level radio active waste:Progress and challenges[J].Engineering Sciences,10(3):58-65(in Chinese with English abstract).
    Wang Ju,Chen Weiming,Su Rui,Guo Yonghai,Jin Yuanxin.2006a.Geological disposal of high-level radioactive waste and its key scientific issues[J].Chinese Journal of Rock Mechanics&Engineering,25(4):801-812(in Chinese with English abstract).
    Wang Ju,Su Rui,Chen Weiming,Guo Yonghai,Jin Yuanxin,Wen Zhijian,Liu Yuemiao.2006b.Deep geological disposal of high-level radioactive wastes in China[J].Chinese Journal of Rock Mechanics&Engineering,25(4):649-658(in Chinese with English abstract).
    Wang Ju,Xu Guoqing,Zheng Hualing,Fan Xianhua,Wang Chengzu,Fan Zhiwen.2005.Geological disposal of high level radioactive waste in China:Progress during 1985~2004[J].World Nuclear Geoscience,22(1):5-16(in Chinese with English abstract).
    Wang Ruijun.2016.Characteristics of primary haloes and ore-search prospect in the Ximole district of Inner Mongolia[J].Geology and Exploration,52(1):128-138(in Chinese with English abstract).
    Wang Tingyin,Zhang Mingjie,Wang Jinrong,Gao Junping.1998.The characteristics and tectonic implications of the thrust belt in Eugerwusu,China[J].Chinese Journal of Geology,(4):385-394(in Chinese with English abstract).
    Wang Xikuan,Zhang Lili,Liao Lei,Cong Limin.2004.Geochemical characteristics and prospecting significance of the Bayannuoergong and Wuliji granite bodies in Inner Mongolia[J].Geology&Mineral Resources of South China,(1):24-28(in Chinese with English abstract).
    Xu Jian,Wang Ju,Ma Yan.2007.Rock mass quality assessment based on BP artificial neural network(ANN)-A case study of borehole BS03 in Jiujing segment of Beishan,Gansu[J].Uranium Geology,23(4):249-256(in Chinese with English abstract).
    Xue Ronghui,An Zhiguo,Wang Xianxiang,Di Qingyun.2016.Probing inner structure of rock mass at a high-level radioactive preselected site in Tamusu,Inner Mongolia[J].Chinese Journal Geophysics,59(6):2316-2325.(in Chinese with English abstract).
    Yang Zhende,Pan Xingshi,Yang Yifu.1988.Geological characteristics and mineral resources of Alxa and its surrounding areas[M].Beijing:Science Press(in Chinese):1-254.
    Yu Jingxing,Zheng Wenjun,Lei Qiyun,Shao Yanxiu,Ge Weipeng,Ma Yan,Li Youjuan.2013.Neotectonics and kinemetics along the Yabrai range-front fault in the South Alashan Block and its implications for regional tectonics[J].Seismology and Geology,35(4):731-744(in Chinese with English abstract).
    Yuan Guangxiang,Li Jianyong,Dong Jinyu,Huang Zhiquan,Wan Junli,Wang Anming.2018.Research on prediction of wall-rock quality for underground cavern during geotechnical surveys[J].Geology and Exploration,54(1):158-165(in Chinese with English abstract).
    Zhang Jin,Li Jinyi,Li Yanfeng,Ma Zongjin.2007.The Cenozoic deformation of the Alxa block in central Asia-Question on the northeastern Extension of the Altyn Tagh fault in Cenozoic time[J].Acta Geologica Sinica,81(11):1481-1497(in Chinese with English abstract).
    Zhang Luqing,Zeng Qingli,Yuan Guangxiang,Wang Xueliang.2016.Engineering geological suitability evaluation of Alxa pre-selected region for geological disposal of high-level nuclear waste[M].Beijing:Science Press:1-285(in Chinese).
    Zhang Zhengping.2016.Geochemical characteristics and LA-ICP-MSzircon U-Pb dating of the Late Permian granite in the Tamusu area,Inner Mongolia and their implications[J].Geology and Exploration,52(5):893-909(in Chinese with English abstract).
    Zhao Honggang,Kunz Herbert,Wang Ju.2007.3D geological modelling in Jiujing block,Beishan area,Gansu Province and application of rock flow to nuclides migration simulation[J].Chinese Journal of Rock Mechanics&Engineering,26(Suppl 2):3989-3994(in Chinese with English abstract).
    Zhou Lifa,Zhao Zhongyuan,Guo Zhongming.1995.Formation and evolution of sedimentary basins in Alxa and its surrounding areas[M].Xi'an:Northwest University Press:1-170(in Chinese).
    Zong Zihua,Wang Ju,Su Rui.2006.Fractal characteristic of fractures in Jiujing,Beishan area,Gansu Province-The potential site for high level radioactive waste repository in China[J].World Nuclear Geoscience,23(2):107-113(in Chinese with English abstract).
    陈虹.2015.内蒙古阿拉善巴音诺尔公一带二叠纪侵入岩地质特征[D].北京:中国地质大学(北京):6-9.
    范洪海,闵茂中,陈佳,季瑞利.2005.甘肃北山野马泉岩体同位素地球化学特征[J].地球学报,26(增):78-83.
    高振兵,龚育龄,张华.2013.EH4方法在高放废物预选区的应用研究-以甘肃北山向阳山-新场地段为例[J].工程地球物理学报,10(2):156-160.
    耿元生,王新社,沈其韩,吴春明.2006.内蒙古阿拉善地区前寒武纪变质基底阿拉善群的再厘定[J].中国地质,33(1):138-145.
    耿元生,王新社,吴春明,周喜文.2010.阿拉善变质基底古元古代晚期的构造热事件[J].岩石学报,26(4):1159-1170.
    郭永海,何建国,周志超,董建楠,季瑞利,张明,李杰彪.2016.高放废物处置库新疆阿奇山预选地段区域水文地质特征[J].铀矿地质,32(4):251-256.
    郭永海,李娜娜,周志超,董建楠,张明,刘淑芬.2016.高放废物处置库新疆雅满苏和天湖预选地段地下水同位素特征及其指示意义[J].地质学报,90(2):376-382.
    郭永海,王驹,吕川河,刘淑芬,钟自华.2005.高放废物处置库甘肃北山野马泉预选区地下水化学特征及水-岩作用模拟[J].地学前缘,12(增1):117-123.
    金远新,闵茂中,陈伟明,赵宏刚.2007.甘肃北山预选区新场地段花岗岩类岩石特征研究[J].岩石力学与工程学报,26(增2):3974-3981.
    万海涛,龚育龄,张华.2015.MT法在高放废物预选区的应用研究-以甘肃北山向阳山-新场地段为例[J].工程地球物理学报,12(2):157-161.
    万汉平,徐贵来,喻翔,崔焕敏.2015.花岗岩型高放废物处置库选址中的地球物理评价-以新疆阿奇山地段候选场址为例[J].地球物理学进展,30(6):2778-2784.
    王驹.2008.高放废物地质处置:进展与挑战[J].中国工程科学,10(3):58-65.
    王驹,陈伟明,苏锐,郭永海,金远新.2006a.高放废物地质处置及其若干关键科学问题[J].岩石力学与工程学报,25(4):801-812.
    王驹,苏锐,陈伟明,郭永海,金远新,温志坚,刘月妙.2006b.中国高放废物深地质处置[J].岩石力学与工程学报,25(4):649-658.
    王驹,徐国庆,郑华铃,范显华,王承祖,范智文.2005.中国高放废物地质处置研究进展:1985~2004[J].世界核地质科学,22(1):5-16.
    王瑞军.2016.内蒙古希莫勒地区的原生晕特征和找矿前景[J].地质与勘探,52(1):128-138.
    王廷印,张铭杰,王金荣,高军平.1998.恩格尔乌苏冲断带特征及大地构造意义[J].地质科学,33(4):385-393.
    王喜宽,张丽莉,廖蕾,丛立民.2004.巴彦诺尔公花岗岩体与乌力吉花岗岩体的地球化学特征及成矿意义[J].华南地质与矿产,(1):24-28.
    徐健,王驹,马艳.2007.基于BP神经网络的岩体质量评价-以甘肃北山旧井地段BS03号钻孔为例[J].铀矿地质,23(4):249-256.
    薛融晖,安志国,王显祥,底青云.2016.利用电磁方法探测内蒙古塔木素高放废物预选场址岩体的内部构造[J].地球物理学报,59(6):2316-2325.
    杨振德,潘行适,杨易福.1988.阿拉善断块及邻区地质构造特征与矿产[M].北京:科学出版社:1-254.
    俞晶星,郑文俊,雷启云,邵延秀,葛伟鹏,马严,李又娟.2013.阿拉善地块南部雅布赖山前断裂的运动学特征及意义初探[J].地震地质,35(4):731-744.
    袁广祥,李建勇,董金玉,黄志全,万军利,王安明.2018.勘察阶段洞室围岩质量预测的问题探讨[J].地质与勘探,54(1):158-165.
    张进,李锦轶,李彦峰,马宗晋.2007.阿拉善地块新生代构造作用-兼论阿尔金断裂新生代东向延伸问题[J].地质学报,81(11):1481-1497.
    张路青,曾庆利,袁广祥,王学良.2016.高放废物地质处置阿拉善预选区工程地质适宜性评价[M].北京:科学出版社:1-285.
    张正平.2016.内蒙古阿拉善右旗塔木素地区晚二叠世花岗岩地球化学特征、LA-ICP-MS锆石U-Pb年龄及其意义[J].地质与勘探,52(5):893-909.
    赵宏刚,KUNZ Herbert,王驹.2007.甘肃北山旧井地段三维地质建模及Rock Flow在核素迁移模拟研究中的应用[J].岩石力学与工程学报,26(增2):3989-3994.
    周立发,赵重远,郭忠铭.1995.阿拉善及邻区沉积盆地的形成与演化[M].西安:西北大学出版社:1-170.
    宗自华,王驹,苏锐.2006.甘肃北山预选区旧井地段断裂的分形特征-中国高放废物处置的潜在场址[J].世界核地质科学,23(2):107-113.
    (1)DD 2015-02. 2015.活动断层与区域地壳稳定性调查评价规范(1∶50000、1∶250000)[S].
    (2)宁夏地质局区域地质调查队. 1978.中华人民共和国地质图豪斯布尔都幅(J-48-III)(1∶20万)[R].
    (3)GB/T50218-2014. 2015.工程岩体分级标准[S].

© 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