Please wait a minute...
E-mail Alert Rss
 
物探与化探  2019, Vol. 43 Issue (3): 568-575    DOI: 10.11720/wtyht.2019.0254
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
高放废物地质处置新场岩体三维地质模型构建与应用
罗辉1, 王驹1, 蒋实2, 赵宏刚1, 金远新1
1. 核工业北京地质研究院 中核高放废物地质处置评价重点实验室,北京 100029
2. 中国自然资源航空物探遥感中心,北京 100083
Construction and application of three-dimensional geological model in Xinchang Block for high-level radioactive waste disposal
Hui LUO1, Ju WANG1, Shi JIANG2, Hong-Gang ZHAO1, Yuan-Xin JIN1
1. CNNC Key Laboratory on Geological Disposal of High-level Radioactive Waste, Beijing Research Institute of Uranium Geology, Beijing 100029, China
2. China Aero Geophysical Survey and Remote Sensing Center for Natural Resources,Beijing 100083, China
全文: PDF(3763 KB)   HTML
输出: BibTeX | EndNote (RIS)      
摘要 

我国高放废物地质处置经过30多年研究,已初步确定新场为地下实验室推荐场址。开展新场岩体三维地质建模研究,一方面能够充分利用已有资料准确地表达各种地质现象,直观再现地质单元的空间展布及其相互关系;另一方面可以挖掘隐含的地质信息,方便地质分析和工程决策,这在地下实验室研究阶段非常重要。在对新场已有资料综合分析和解译的基础上,建立了岩体的三维地质模型,直观地再现了新场岩体地质环境特征;并基于地质建模结果,开展了钻孔设计等工程应用,取得了较好的效果。本研究可为我国高放废物地质处置后续工作中地质分析与工程设计提供有益参考和技术支持。

服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
罗辉
王驹
蒋实
赵宏刚
金远新
关键词 高放废物地质处置新场岩体三维地质建模模型应用    
Abstract

After more than 30 years of research in high-level radioactive waste disposal, China has initially identified Xinchang block as the recommended site of underground laboratory. It is necessary to make full use of the existing data to express all kinds of geological phenomena accurately and intuitively to reproduce the spatial distribution of geological units and their mutual relations. on the other hand, it is possible to mine hidden geological information to facilitate geological analysis and engineering decision-making, which is very important in the research phase of underground laboratory. Based on the comprehensive analysis and interpretation of the existing data, the three-dimensional geological model of Xinchang block has been established. The model reproduced the geologic and environmental characteristics of Xinchang block. Based on the model, we designed the drilling to expose the fault and determined the location and main structure of the underground laboratory, the effect seems good. This study can provide useful reference and technical support for the geological analysis and engineering design of the high-level radioactive waste disposal project in China.

Key wordshigh-level radioactive waste disposal    Xinchang block    3D geological modeling    application of model
收稿日期: 2019-01-05      出版日期: 2019-05-31
:  X771  
基金资助:国家自然科学基金资助项目(41502308)
作者简介: 罗辉(1982- ),男,高级工程师,主要从事高放废物地质处置选址和场址评价方面的研究工作。Email: luo1029hui@163.com
引用本文:   
罗辉, 王驹, 蒋实, 赵宏刚, 金远新. 高放废物地质处置新场岩体三维地质模型构建与应用[J]. 物探与化探, 2019, 43(3): 568-575.
Hui LUO, Ju WANG, Shi JIANG, Hong-Gang ZHAO, Yuan-Xin JIN. Construction and application of three-dimensional geological model in Xinchang Block for high-level radioactive waste disposal. Geophysical and Geochemical Exploration, 2019, 43(3): 568-575.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2019.0254      或      https://www.wutanyuhuatan.com/CN/Y2019/V43/I3/568
Fig.1  1 甘肃北山新场岩体交通位置
Fig.2  新场岩体地质简图
Fig.3  联井剖面空间分布
Fig.4  物探剖面初步解译的地质剖面
Fig.5  物探剖面XC11初步地质解译
Fig.6  新场岩体三维地质模型
a—提取地质界线生成地表模型;b—生成不同岩性单元模型;c—断裂模型;d—岩体地质模型,包含断裂和岩性信息 1—第四系;2—咸水井群变质中基性火山岩;3—敦煌群鱼脊山组变质岩;4—红柱滩单元角闪辉绿岩;5—新场单元二长花岗岩;6—机井沟单元块状花岗闪长岩;7—鸳鸯沟单元片麻状二长花岗岩;8—红柳井南山单元片麻状花岗闪长岩; 9—钻孔;10—地质界线;11—断层线;12—断裂面
Fig.7  BS35钻孔三维设计
钻孔编号 钻孔方位角/(°) 钻孔顶角/(°) 断层倾角/(°)
BS35 110 11 81~83
钻孔编号 揭露断裂
孔深/m
平距/m 钻孔位置和方位设计
的主要考虑因素
BS35 590~600 197 研究F31断裂特征
Table 1  BS35钻孔设计参数
Fig.8  地下实验室场址与断裂的关系
Fig.9  地下实验室空间立体图(草案)
[1] Savage D . The Scientific and Regulatory Basis for the Geological Disposal of Radioactive Waste[M]. Chichester: John Wiley and Sons, 1995.
[2] 王驹 . 高放废物地质处置: 进展与挑战[J]. 中国工程科学, 2008,10(3):58-65.
[2] Wang J . Geological disposal of high level radio active waste:Progress and challenges[J]. Engineering Sciences, 2008,10(3):58-65.
[3] 潘自强, 钱七虎 . 高放废物地质处置战略研究[M]. 北京: 原子能出版社, 2009.
[3] Pan Z Q, Qian Q H. Research on geological disposal strategy of high level radioactive waste[M]. Beijing: Atomic energy publishing house2009.
[4] PosivaOy. Okliluoto site description 2008 Part 1 and 2[R]. Posiva OY, 2009.
[5] SKB. Site description of forsmark at completion of the site investigation phase[R]. SvenskKärnbränslehantering AB, 2008.
[6] 赵宏刚, Kunz Herbert , 王驹. 甘肃北山旧井地段三维地质建模及RockFlow在核素迁移模拟研究中的应用[J]. 岩石力学与工程学报, 2007,26(2):3989-3994.
[6] Zhao H G, Kunz H, Wang J . 3D geological modelling in Jiujing block,Beishan area,Gansu Province and application of rockflow to nuclides migration simulation[J]. Chinese Journal of Rock Mechanics and Engineering, 2007,26(2):3989-3994.
[7] 罗辉, 王驹, 蒋实 , 等. 高放废物地质处置地下实验室新场候选场址三维地质建模[J]. 铀矿地质, 2017,34(1):53-59.
[7] Luo H, Wang J, Jiang S , et al. Study on 3D geological modeling of Xinchang potential underground laboratory site for high-level radioactive waste disposal[J]. Uranium Geology, 2017,34(1):53-59.
[8] 王驹, 徐国庆, 郑华铃 , 等. 中国高放废物地质处置研究进展1985~2004[J]. 世界核地质科学, 2005,22(1):5-16.
[8] Wang J, Xu G Q, Zhen H L , et al. Geological disposal of high level radioactive waste in China:Progress during 1985~2001[J]. World Nuclear Geoscience, 2005,22(1):5-16.
[9] 潘自强, 沈文权 . 2020年前我国核能发展的策略和目标研究[J]. 铀矿地质, 2004,20(5):257-259.
[9] Pan Z Q, Shen W Q . Tactics and targets for nuclear energy development in China by 2020[J]. Uranium Geology, 2004,20(5):257-259.
[10] 王驹, 陈伟明, 苏锐 , 等. 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, 2006,25(4):801-812.
doi:
[10] Wang J, Chen W M, Su R , et al. Geological disposal of high-level radioactive waste and its key scientific issues[J]. Chinese Journal of Rock Mechanics and Engineering, 2006,25(4):801-812.
[11] 王驹, 陈伟明, 金远新 , 等. 向阳山—新场地段1:5万地质调查报告[R]. 核工业北京地质研究院, 2006.
[11] Wang J, Chen W M, Jin Y X , et al. Geological survey report of Xiangyangshan-Xinchang section (1:50,000)[R]. Beijing Research Institute of Uranium Geology, 2006.
[12] 王锡勇, 苏锐, 陈亮 , 等. 基于超声波钻孔电视的深部岩体结构面特征研究[J]. 世界核地质科学, 2014,31(1):31-44.
[12] Wang X Y, Su R, Chen L , et al. Study on structural plane characteristics of deep rock mass based on acoustic borehole TV[J]. World Nuclear Geoscience, 2014,31(1):31-44.
[13] 季瑞利, 张明, 周志超 , 等. 北山预选区钻孔水文地质试验方法研究[J]. 铀矿地质, 2018,34(1):53-59.
[13] Ji R L, Zhang M, Zhou Z C , et al. Research on In-situ Hydraulic Test Method in Beishan Pre-selected Area[J]. Uranium Geology, 2018,34(1):53-59.
[14] 赵星光, 王驹, 马利科 , 等. 高放废物地质处置库北山预选区新场岩体地应力场分布规律[J]. 岩石力学与工程学报, 2014,33(2):3750-375.
[14] Zhao X G, Wang J, Ma L K , et al. Distribution characteristics of geostress field in Xinchang rock block of candidate Beishan area for high level radioactive waste repository in China[J]. Chinese Journal of Rock Mechanics and Engineering, 2014,33(2):3750-375.
[1] 罗辉, 蒋实, 赵宏刚, 李亚伟, 田霄. 三维地质建模在高放废物地质处置预选地段筛选中的应用——以新疆预选区天湖预选地段为例[J]. 物探与化探, 2021, 45(6): 1488-1496.
[2] 蒋实, 罗辉, 陈伟明, 李亚伟, 金远新. 高放废物地质处置算井子地段地质条件适宜性研究[J]. 物探与化探, 2021, 45(5): 1208-1216.
[3] 何育枫, 李晓娟, 佘继红, 陈晔, 徐礼鹏. 基于T-C-V架构的三维城市地质信息共享平台建设[J]. 物探与化探, 2018, 42(4): 804-810.
[4] 林玉祥, 马小伟, 朱传真, 宋喜林, 米晓利, 张岗. 地表化探异常立体解释模型的建立及其意义——以库车坳陷米斯布拉克地区为例[J]. 物探与化探, 2016, 40(4): 705-712.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
京ICP备05055290号-3
版权所有 © 2021《物探与化探》编辑部
通讯地址:北京市学院路29号航遥中心 邮编:100083
电话:010-62060192;62060193 E-mail:whtbjb@sina.com