冷湖赛什腾山天文台工程地质选址评价

周保, 孙皓, 魏赛拉加, 张睿, 张俊才, 王栋, 严慧珺, 隋嘉. 冷湖赛什腾山天文台工程地质选址评价[J]. 水文地质工程地质, 2022, 49(4): 165-174. doi: 10.16030/j.cnki.issn.1000-3665.202104075
引用本文: 周保, 孙皓, 魏赛拉加, 张睿, 张俊才, 王栋, 严慧珺, 隋嘉. 冷湖赛什腾山天文台工程地质选址评价[J]. 水文地质工程地质, 2022, 49(4): 165-174. doi: 10.16030/j.cnki.issn.1000-3665.202104075
ZHOU Bao, SUN Hao, WEI Sailajia, ZHANG Rui, ZHANG Juncai, WANG Dong, YAN Huijun, SUI Jia. Site selection evaluation of engineering geology of the Lenghu Saishiteng Mountain Observatory[J]. Hydrogeology & Engineering Geology, 2022, 49(4): 165-174. doi: 10.16030/j.cnki.issn.1000-3665.202104075
Citation: ZHOU Bao, SUN Hao, WEI Sailajia, ZHANG Rui, ZHANG Juncai, WANG Dong, YAN Huijun, SUI Jia. Site selection evaluation of engineering geology of the Lenghu Saishiteng Mountain Observatory[J]. Hydrogeology & Engineering Geology, 2022, 49(4): 165-174. doi: 10.16030/j.cnki.issn.1000-3665.202104075

冷湖赛什腾山天文台工程地质选址评价

  • 基金项目: 青海省重大科技专项(2019-ZJ-A10); 青海省地质环境信息化综合平台资质项目(2021-ZJ-T08)
详细信息
    作者简介: 周保(1982-),男,博士,教授级高级工程师,主要从事工程地质、地质灾害等研究。E-mail:zhb820322@163.com
  • 中图分类号: P112

Site selection evaluation of engineering geology of the Lenghu Saishiteng Mountain Observatory

  • 青海省冷湖赛什腾山具有国际一流的光学天文观测条件,是我国光学天文发展的宝贵战略资源。围绕冷湖赛什腾山天文台建设面临的工程地质选址问题,在收集前人已开展的地质调查成果的基础上,利用遥感影像、无人机航拍、数值模拟和人工地面调查相结合的方法进行工程地质选址评价。为了确保赛什腾山已经确定的2处已建平台和2处空置平台的工程地质稳定性,首先进行了人工地面踏勘、采取岩石样品和模拟地震作用下已建平台的边坡三维响应研究,以确定平台的稳定性;在重点工作区使用InSAR监测分析地形形变,确定重点工作区工程地质稳定性;最后使用BP神经网络模型算法对赛什腾山地区进行区域工程地质稳定性评价。评价结果表明:2处已建平台虽有断层分布但对工程建设的影响较小;2处空置平台场地内及周边未发现断层破碎带及断裂构造通过。基于分析结果,建议尽量减少在填方区布设工程及重要设备,保证填方边坡坡度小于自然休止角,对于人工开挖或填筑形成的碎石土边坡应进行适当工程处理以确保工程安全及设备正常使用,并基于不同层次的评价结果推荐出4 300 m与4 050 m 2个平台。

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  • 图 1  研究区自然地质环境

    Figure 1. 

    图 2  重点工作区

    Figure 2. 

    图 3  节理稳定性

    Figure 3. 

    图 4  优选区

    Figure 4. 

    图 5  区域工程地质稳定性评价

    Figure 5. 

    图 6  所有干涉对的时空基线图

    Figure 6. 

    图 7  地表累积形变量

    Figure 7. 

    图 8  地震作用下边坡三维动力响应

    Figure 8. 

    表 1  断层赋值表

    Table 1.  Fault assignment table

    断层等级缓冲区1缓冲区2缓冲区3缓冲区4缓冲区5
    距离/m赋值距离/m赋值距离/m赋值 距离/m赋值 距离/m赋值
    1级断层1000202000163000124000850004
    2级断层300156001290091200615003
    3级断层100102008300640045002
    4级断层30560490312021501
    下载: 导出CSV

    表 2  岩体、土体强度状况赋值表

    Table 2.  Assignment of rock mass and soil condition

    岩体、土体赋值结果
    晚二叠世坚硬块状侵入岩岩组10
    晚奥陶世坚硬块状侵入岩岩组9
    坚硬、较坚硬的片状熔岩岩组8
    早古生代火山岩岩组7
    较坚硬片状砾、砂、板、千枚岩岩组6
    软硬相间层-薄层状变质砾、砂岩及页岩岩组;软硬相
    间层-薄层状变质岩或碎屑岩夹碳酸盐岩岩组;软硬
    相间层-薄层状碳酸盐岩与变质岩或碎屑岩岩组
    5
    晚奥陶世石英闪长花岗岩4
    软弱层状-薄层状砂泥岩岩组3
    软弱层状砂、泥(灰)岩岩组2
    黏性土、盐渍土、砂类土、卵砾类土1
    苏干湖0
    下载: 导出CSV

    表 3  平台工程适宜性评价

    Table 3.  Platform engineering suitability evaluation

    平台类别评价得分
    已建平台(3830 m平台)6.57942
    已建平台(4200 m平台)7.32686
    空置平台(4100 m平台)7.21152
    空置平台(4000 m平台)7.41247
    推荐平台(4300 m平台)7.62298
    推荐平台(4050 m平台)7.13246
    下载: 导出CSV
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收稿日期:  2021-04-30
修回日期:  2021-11-23
刊出日期:  2022-07-25

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