Karstic Rock Mass of Dam Foundation and Its Physical and Mechanical Properties in the Red Beds of Central Yunnan Province

WANG Kun, WANG Zhong, GAO Qiang

Journal of Changjiang River Scientific Research Institute ›› 2014, Vol. 31 ›› Issue (11) : 1-6.

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Journal of Changjiang River Scientific Research Institute ›› 2014, Vol. 31 ›› Issue (11) : 1-6. DOI: 10.3969/j.issn.1001-5485.2014.11.0012014,31(11):1-6
CHARACTERISTICS AND TESTS OF ROCK MECHANICS

Karstic Rock Mass of Dam Foundation and Its Physical and Mechanical Properties in the Red Beds of Central Yunnan Province

  • WANG Kun1,2, WANG Zhong2, GAO Qiang2
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Abstract

Guanyinyan hydropower station on the Jinsha River is a double fold mixed dam. Its concrete gravity dam foundation is located in the red beds of central Yunnan Province and mainly contains conglomerate and sandstone of J2s stratum, in which dissolution affects the stability of foundation rock mass. According to the distribution of red beds in China, we analysed the deposition and distribution features of red beds in Yunnan and systematically researched the features of karst in red beds of clastic rock as well as some small caves, dissolution holes and cracks. We also conducted tests on the physical and mechanical properties of karstic rock mass in red beds. The results show that the distribution characteristics and mechanical parameters of karstic rock mass could reach the quality of Ⅲa, Ⅲb classes, and meet the dam foundation requirement when appropriately treated. The research achievements provide basis for selecting dam foundation and treating geological defects of karstic rock mass.

Key words

red beds in central Yunnan / solution / physical and mechanical properties of foundation / Guanyinyan hydropower station

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WANG Kun, WANG Zhong, GAO Qiang. Karstic Rock Mass of Dam Foundation and Its Physical and Mechanical Properties in the Red Beds of Central Yunnan Province[J]. Journal of Changjiang River Scientific Research Institute. 2014, 31(11): 1-6 https://doi.org/10.3969/j.issn.1001-5485.2014.11.0012014,31(11):1-6

References

[1] 高 强,王 忠. 金沙江中游河段观音岩水电站可行性研究报告(第四篇:工程地质) .昆明:中国电建集团昆明勘测设计研究院有限公司,2010. (GAO Qiang, WANG Zhong. Report on the Feasibility of Guanyinyan Hydropower Station in the Middle Reaches of Jinsha River (Fourth Chapter: Engineering Geology). Kunming: Power China Kunming Engineering Corporation, 2010.(in Chinese))
[2] 袁道先,朱德浩.中国岩溶学.北京:北京地质出版社,1994.(YUAN Dao-xian, ZHU De-hao. Karstology of China. Beijing: Beijing Geological Publishing House, 1994. (in Chinese))
[3] 袁道先. 现代岩溶学和全球变化研究.地学前缘,1997,4(1/2):17-25.(YUAN Dao-xian. Modern Karstology and Global Changes. Earth Science Frontiers, 1997, 4(1/2): 17-25.(in Chinese))
[4] 袁道先,李 彬,刘再华. 岩溶与人类生存、环境、资源和灾害.桂林:广西师范大学出版社,1996.(YUAN Dao-xian, LI Bin, LIU Zai-hua. Karst and Human Existence, Environment, Natural Resources and Disaster. Guilin: Guangxi Normal University Press, 1996.(in Chinese))
[5] 邹成杰.水利水电岩溶工程地质.北京:北京水利电力出版社,1994.(ZOU Cheng-jie. Water Conservancy and Hydropower Engineering Geology in Karst. Beijing: Beijing Water Conservancy and Electric Power Press, 1994.(in Chinese))
[5] 李正坤,左重辉.湖南白垩系红色砾岩溶蚀风化特性研究.水利水电科技进展,2001,21(10):80-82.(LI Zheng-kun, ZUO Zhong-hui. Research on the Karst Weathering Characteristics of Hunan Cretaceous Red Conglomerate. Advances in Science and Technology of Water Resources, 2001, 21(10): 80-82.(in Chinese))
[5] 卢书强,许 模,张 强,等. 金沙江某电站钙质砂(砾)岩溶蚀对岩体质量的控制作用. 中国地质灾害与防治学报,2007,18(2):74-77.(LU Shu-qiang, XU Mo, ZHANG Qiang, et al. Control of Calcareous Sandstone Dissolution on Rock Mass Quality in an Hydroelectric Station on the Jinsha River. The Chinese Journal of Geological Hazard and Control, 2007, 18(2): 74-77.( in Chinese))
[6] 程 强,寇小兵,黄绍槟,等.中国红层的分布及地质环境特征.工程地质学报,2004,12(1):34-40.(CHENG Qiang, KOU Xiao-bing, HUANG Shao-bin, et al. The Distribution and Geologic Environment Characteristics of Red Beds in China. Journal of Engineering Geology, 2004, 12(1): 34-40.(in Chinese))
[7] 左重辉,曾晓阳.株洲航电枢纽红层溶蚀风化土固结灌浆试验研究.人民珠江,2004,(5):23-25.(ZUO Zhong-hui, ZENG Xiao-yang. Experimental Research on Consolidation Grouting for Red Solution-weathered Soil for Zhuzhou Navigation Junctions. Pearl River, 2004, (5): 23-25.(in Chinese))
[8] 钟共清.浅论王家厂水库大坝坝基红层砾岩的岩溶水文地质特征.湖南水力,1995,(2):16-18.(ZHONG Gong-qing. Discussion on Karst Hydrogeological Features of Red Conglomerate in Wangjiachang Dam Foundation. Hunan Hydraulics, 1995, (2): 16-18.( in Chinese))
[9] 吴应科,梁永平.长江中上游红层岩溶刍议.中国岩溶,1987,6(2):111-118.(WU Ying-ke, LIANG Yong-ping. Discussion on Karst of Red Bed in the Upper Reaches of the Yangtze River. Carsologica Sinica, 1987, 6(2): 111-118.( in Chinese))
[10] 彭柏兴,刘颖炯,刘 毅.红层溶蚀风化特征及其工程影响.岩土工程学报,2011,33(8):141-145.(PENG Bo-xing, LIU Ying-jiong, LIU Yi. Solution and Weathered Characteristics and Engineering Influences of Red Bed. Chinese Journal of Geotechnical Engineering, 2011, 33(8): 141-145.(in Chinese))
[11] 何宇彬,邹成杰.中国南北方喀斯特水特征对比.中国岩溶,1996,15(3):259-268.(HE Yu-bin, ZOU Cheng-jie. Comparison between Southern and Northern Karst Water Characteristics in China. Carsologica Sinica, 1996, 15(3): 259-268.(in Chinese))
[12] PATERSON K, SWEETING M M. The Pinnacle Karst of the Stone Forest, Lunan, China: An Example of a Subjacent Karst. England: Geo Books Regency House, 1986: 597-607.
[13] BURLEY S D, KANTOROWICZ J D. Thin Section and S.E.M. Textural Criteria for the Recognition of Cement-dissolution Porosity in Sand Stones. Sedimentology, 1986, (33): 587-604.
[14] HUMPHREYS B, SMITH A, STRONG E. Authigenic Chlorite in Late Triassic Sandstones from the Central Graben. North Sea Clay Minerals, 1989, (24): 427-444.
[15] SOMMER F. Diagenesis of Jurassic Sandstones in the Viking Graben. The Geological Society, 1978, 135: 63-67.
[16] OMAR A. HARBI A, MUJTABA K M. Source and Origin of Glacial Paleovalley-fill Sediments (Upper Ordovician) of Sarah Formation in Central Saudi Arabia. Arabian Journal of Geosciences, 2011, 4(5): 825-835.
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