ISSN 1000-3665 CN 11-2202/P
  • Included in Scopus
  • Included in DOAJ
  • Included in WJCI Report
  • Chinese Core Journals
  • The Key Magazine of China Technology
  • Included in CSCD
Wechat
GUOChang-bao, . Sediment and engineering properties research on the Xiaozhongdian lacustrine clay in Northwest Yunan Province[J]. Hydrogeology & Engineering Geology, 2008, 35(1): 23-27.
Citation: GUOChang-bao, . Sediment and engineering properties research on the Xiaozhongdian lacustrine clay in Northwest Yunan Province[J]. Hydrogeology & Engineering Geology, 2008, 35(1): 23-27.

Sediment and engineering properties research on the Xiaozhongdian lacustrine clay in Northwest Yunan Province

More Information
  • Xiaozhongdian Basin is a NNW-directed fault depression basin which was shaped while the Qinghai-Tibet Plateau intensely upheaved since the end of the Pliocene epoch,where the lacustrine clay of the middle and late Pleistocene is well distributed from the Xiaozhongdian River section.The Yunnan-Tibet Railway in planning will pass through the Xiaozhongdian Basin.The depth of lacustrine clay is above ten meters,which is obviously fine and has texture layer from the outcrop of the Xiaozhongdian.The laboratory testing results indicate that the Xiaozhongdian lacustrine clay is a kind of clay with high dispersion,high liquid limit,high plastic limit and high porosity ratio,whose mechanical characters are high shear strength and low expansibility or middle expansibility,so its engineering property is better.The slope will be destroyed when it experiences alternations of wetting and drying.
  • Related Articles

    [1]SUN Dong, LI Jinxi, CAO Nan, LI Zhiwu, ZHANG Zhipeng, XIE Xiaoguo, YUAN Mengyu, CAI Hongyan. A preliminary study of the geothermal geological characteristics and exploration potential of the Sichuan Basin[J]. Hydrogeology & Engineering Geology, 2023, 50(3): 193-206. DOI: 10.16030/j.cnki.issn.1000-3665.202110028
    [2]ZHAO Zhen, QIN Guangxiong, LUO Yinfei, CHAO Jiahao, GENG Songhe, ZHANG Liang. Characteristics of geothermal water in the Xining Basin and risk of reinjection scaling[J]. Hydrogeology & Engineering Geology, 2021, 48(5): 193-204. DOI: 10.16030/j.cnki.issn.1000-3665.202103058
    [3]ZHOU Hongfu, FENG Zhiguo, SHI Shengwei, WANG Baodi, XU Ruge, RAN tao. Slope engineering geology characteristics and stability evaluation of a grand bridge to Chengdu bank on the Sichuan-Tibet Railway[J]. Hydrogeology & Engineering Geology, 2021, 48(5): 112-119. DOI: 10.16030/j.cnki.issn.1000-3665.202103076
    [4]WANG Meihua, FAN Hongxi, ZHANG Ruolin. An analysis on the literature characteristics of Hydrogeology & Engineering Geology[J]. Hydrogeology & Engineering Geology, 2020, 47(1): 185-191. DOI: 10.16030/j.cnki.issn.1000-3665.201906069
    [5]ZHU Nan, LIU Chunyuan, WANG Wenjing, ZHAO Xianhui. Investigation of engineering geological characteristics of the marshy and lacustrine clays in the Hengshui Lake area[J]. Hydrogeology & Engineering Geology, 2020, 47(1): 125-132. DOI: 10.16030/j.cnki.issn.1000-3665.201904083
    [6]LINing, . Analysis of sustainable groundwater development scenarios for the Chaiwopu Basin in the Urumqi River Basin[J]. Hydrogeology & Engineering Geology, 2010, 37(5): 8-14.
    [7]ZHANGYun, . Engineering geological characteristics of shallow mucky soil in Taicang area,Jiangsu Provience[J]. Hydrogeology & Engineering Geology, 2010, 37(4): 43-47.
    [8]JINHui-jun~, . Zonation and assessment of engineering geology for frozen-ground environments and conditions along the proposed China-Russia Crude Oil Pipeline route[J]. Hydrogeology & Engineering Geology, 2009, 36(4): 102-107.
    [9]WANGYong-gui, . Evolution of the sedimentary environment in the Qaidam Basin over the Quaternary Period[J]. Hydrogeology & Engineering Geology, 2009, 36(1): 128-132.
    [10]HOUGuang-cai, . Groundwater systems and water resources potential in the Ordos Basin[J]. Hydrogeology & Engineering Geology, 2009, 36(1): 18-34.

Catalog

    Article views (963) PDF downloads (420) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return