Journal of Jilin University(Earth Science Edition) ›› 2023, Vol. 53 ›› Issue (4): 1185-1194.doi: 10.13278/j.cnki.jjuese.20220042

Previous Articles     Next Articles

Experiment on Concrete Building Erosion by Underground Water in Gypsum Rock Formation

Wang Fugang1, Pan Huilin1, Li Shengwei2, Wang Donghui2, Wu Mingjie1, Ping Shifei1, Cao Yuqing1   

  1. 1.  Key Laboratory of Groundwater Resources and Environment(Jilin University), Ministry of Education, Changchun 130021, China
    2. Chengdu Center,China Geological Survey, Chengdu 610081, China
  • Received:2022-02-24 Online:2023-07-26 Published:2023-08-10
  • Supported by:
    the Project of China Geological Survey (DD20189210,DD20211402)

Abstract: During underground engineering construction in gypsum-enriched formations, the reaction between  gypsum and groundwater leads to the dissolution of Ca2+ and SO42-, which enhances the erosion effect on the concrete foundation of underground structures and affects the safety of underground engineering. In order to investigate the erosion characteristics and mechanisms of concrete under different  formation environmental conditions, commonly used C20 and C30 concrete in underground engineering construction were studied. The study focused on the gypsum-containing formation  conditions in the southern part of Chengdu basin and explored the erosion characteristics and mechanisms of concrete in both gypsum-containing and non-gypsum-containing formations under changing underground temperature conditions. The results show that: 1) The erosion degree of C20 and C30 concrete in gypsum-containing formations is significantly greater than in non-gypsum-containing formations. Under the erosionby different geological groundwater, the  maximum mass change rates of C20 and C30 concrete are 1.80% and 0.87%, with the maximum compressive strength reduction rates of 20.14% and 12.80%, respectively. C30 concrete exhibits a smaller attenuation in compressive strength under different groundwater conditions, making it more suitable as a construction material for underground engineering. 2) Increasing temperature enhances the erosion effect of SO42- on concrete, leading to a decrease in compressive strength. Among them, the maximum compressive strength reduction rates of C20 concrete under Quaternary and Guankou  Formation groundwater erosion reach 6.89% and 3.89%, respectively. 3) Concrete erosion occurs from the outside to the inside, where Ca2+ and SO42- in groundwater recrystallize to form gypsum on the  external surfaces of the concrete and then diffuse along cracks towards the interior, resulting in the formation of ettringite crystals, expansion forces, crack formation, and a decrease in compressive strength. Through correlation analysis, a relationship equation between the mechanical properties of concrete and temperature was established, achieving quantitative calculation of long-term changes in the mechanical properties of concrete in gypsum-containing formation engineering construction.

Key words: concrete, gypsum, erosion, compressive strength, dissolution, groundwater

CLC Number: 

  • P642.2
[1] Zhao Yongsheng, , Dai Zhenwei.

Sepiolite Modified Soil-Bentonite Slurry Barrier Wall Cut-off Heavy Metal Cation Pollution in Groundwater

#br#

#br#

#br# [J]. Journal of Jilin University(Earth Science Edition), 2023, 53(5): 1549-1559.

[2] Li Shijie, Luo Zujiang, Xu Mingzuan, Zhang Bin. Groundwater Quality Characteristics in Coastal Areas and Its Potential Hazard Analysis to Groundwater Source Heat Pump System in Coastal Areas [J]. Journal of Jilin University(Earth Science Edition), 2023, 53(4): 1204-1215.
[3] Xu Tianfu, Chen Jingyi, Feng Bo, Jiang Zhenjiao. Possible Problems of Groundwater Evrionment  in the Exploitation of Geothermal Energy [J]. Journal of Jilin University(Earth Science Edition), 2023, 53(4): 1149-1162.
[4] Yan Baizhong, Xu Wenjie, Li Yuhan, Sun Jian, Bi Pan, Li Yao, Zhang Xu. Optimal Layout of Pumping and Recharging Wells for Groundwater Source Heat Pump and Parameter Sensitivity [J]. Journal of Jilin University(Earth Science Edition), 2023, 53(1): 218-229.
[5] Li Qin, Jia Zhuo, Li Jiangang, Tang Hongmei, Zhan Cong, Zhao Yongsheng, . Cutoff Phenol Polluted Groundwater with Activated Carbon Modified Soil-Bentonite Slurry Wall [J]. Journal of Jilin University(Earth Science Edition), 2023, 53(1): 251-260.
[6] Bao Xinhua, Yu Hanbo, Ji Liang. Division of Two-Level Protection Area of Changchun Qijia Groundwater Source Based on GMS [J]. Journal of Jilin University(Earth Science Edition), 2022, 52(3): 955-966.
[7] Li Bang, Jiang Chuandong, Wang Yuan, Tian Baofeng, Duan Qingming, Shang Xinlei. Random Noise Suppression for Groundwater Magnetic Resonance Sounding Data Based on Convolutional Neural Network [J]. Journal of Jilin University(Earth Science Edition), 2022, 52(3): 775-784.
[8] He Jin, Zheng Yidi, Deng Qijun, He Xueqin. Groundwater Origin and Hydrochemical Characteristics in Cenozoic Basaltic Aquifer in North China:A Case Study of Zhangbei County,Hebei Province [J]. Journal of Jilin University(Earth Science Edition), 2022, 52(1): 171-.
[9] Li Chaofeng. Hydraulic Connection Coefficient and Quantitative Evaluation of Hydraulic Connection Between Aquifers [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(6): 1801-1810.
[10] Liu Yuanqing, Zhou Le, Li Wei, Wang Xinfeng, Ma Xuemei, Lü Lin, Yin Kai, Meng Shunxiang. Controlling Effect of Mesozoic Tectonic Activities on Present Karst Groundwater Occurrence in Central Mountain Area of Shandong Province [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(6): 1811-1822.
[11] Pan Weiqiang, Zhang Liming, Cong Yu. Relationship Between Shaft Failure with Stress-Relief Groove and Groundwater Level in Thick Loose Strata [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(5): 1578-1586.
[12] Yan Baizhong, Sun Jian, Wang Xinzhou, Li Xiaomeng, Sun Fengbo, Fu Danping. Suitability Zoning of Groundwater Source Heat Pump in Shijiazhuang Based on GIS-FAHP [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(4): 1172-1181.
[13] Wei Wei, Luo Beijing, Ding Ling. Three Decadal Morphodynamic Responses of Hengsha Island Tidal Flat Wetland to Adjacent Engineering in Yangtze Estuary [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(4): 1193-1203.
[14] Yan Baizhong, Sun Fengbo, Li Xiaomeng, Wang Yuqing, Fan Chengbo, Chen Jiaqi. Impact of Climate Change and Human Activities on Groundwater Depth of Gaocheng District in Shijiazhuang City [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(3): 854-863.
[15] Wang Zhe, Fu Yu, Zhu Jingsi, Cao Wengeng. Effect Assessment on Groundwater Recharge for Typical Rivers in North China [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(3): 843-853.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] CHENG Li-ren, ZHANG Yu-jie, ZHANG Yi-chun. Ordovician Nautiloid Fossils of Xainza Region,Tibet[J]. J4, 2005, 35(03): 273 -0282 .
[2] LI Bing-cheng. Preliminary Studies on Holocene Climatic In Fuping,Shaanxi Province[J]. J4, 2005, 35(03): 291 -0295 .
[3] HE Zhong-hua,YANG De-ming,WANG Tian-wu,ZHENG Chang-qing. SHRIMP U[CD*2]Pb Dating of Zircons from Two-Mica Granite in Baga Area in Gangdise Belt[J]. J4, 2005, 35(03): 302 -0307 .
[4] CHEN Li, NIE Lei, WANG Xiu-fan, LI Jin. Seismic Risk Analysis of Some Electric Power Equipment Station in Suizhong[J]. J4, 2005, 35(05): 641 -645 .
[5] JI Hong-jin,SUN Feng-yue2,CHEN Man,HU Da-qian,SHI Yan-xiang,PAN Xiang-qing. Geochemical Evaluation for Uncovered GoldBearing Structures in Jiaodong Area[J]. J4, 2005, 35(03): 308 -0312 .
[6] CHU Feng-you, SUN Guo-sheng,LI Xiao-min,MA Wei-lin, ZHAO Hong-qiao. The Growth Habit and Controlling Factors of the CobaltRich Crusts in Seamount of the Central Pacific[J]. J4, 2005, 35(03): 320 -0325 .
[7] LI Bin, MENG Zi-fang, LI Xiang-bo, LU Hong-xuan, ZHENG Min. The Structural Features and Depositional Systems of the Early Tertiary in the Biyang Depression[J]. J4, 2005, 35(03): 332 -0339 .
[8] LI Tao, WU Sheng-jun, CAI Shu-ming, XUE Huai-ping, YASUNORI Nakayama. Simulation Analysis of the Storage Capacity Based on DEM Before and After Connecting to Yangtze River in Zhangdu Lake[J]. J4, 2005, 35(03): 351 -0355 .
[9] KUANG Li-xiong,GUO Jian-hua, MEI Lian-fu, TONG Xiao-lan, YANG Li. Study on the Upheaval of the Bogeda Mountain Block from Angle of Oil and Gas Exploration[J]. J4, 2005, 35(03): 346 -0350 .
[10] ZHANG Guang-xin, DENG Wei, HE Yan, RAMSIS Salama. An Application of Hydrological Response Units in Assessment of Soil Salinization Risks[J]. J4, 2005, 35(03): 356 -0360 .