Analysis on development characteristics and inducement of karst collapse in Shandong Province

WU Ya’nan; YANG Yuntao; JIAO Yuguo; LIU Zhitao; WANG Yanling; ZHAI Daiting; ZHOU Shaozhi; WEI Kai; CHENG Feng

doi:10.11932/karst2023y007

Volume 42 Issue 1

Feb. 2023

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Article Navigation > CARSOLOGICA SINICA > 2023 > 42(1): 128-138, 148

WU Ya’nan, YANG Yuntao, JIAO Yuguo, LIU Zhitao, WANG Yanling, ZHAI Daiting, ZHOU Shaozhi, WEI Kai, CHENG Feng. Analysis on development characteristics and inducement of karst collapse in Shandong Province[J]. CARSOLOGICA SINICA, 2023, 42(1): 128-138, 148. doi: 10.11932/karst2023y007

Citation:

WU Ya’nan, YANG Yuntao, JIAO Yuguo, LIU Zhitao, WANG Yanling, ZHAI Daiting, ZHOU Shaozhi, WEI Kai, CHENG Feng. Analysis on development characteristics and inducement of karst collapse in Shandong Province[J]. CARSOLOGICA SINICA, 2023, 42(1): 128-138, 148. doi: 10.11932/karst2023y007

Citation:

WU Ya’nan, YANG Yuntao, JIAO Yuguo, LIU Zhitao, WANG Yanling, ZHAI Daiting, ZHOU Shaozhi, WEI Kai, CHENG Feng. Analysis on development characteristics and inducement of karst collapse in Shandong Province[J]. CARSOLOGICA SINICA, 2023, 42(1): 128-138, 148. doi: 10.11932/karst2023y007

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Analysis on development characteristics and inducement of karst collapse in Shandong Province

doi: 10.11932/karst2023y007

WU Ya’nan^{1, 2
,},
YANG Yuntao^{1, 2},
JIAO Yuguo^{1, 2
,
,},
LIU Zhitao^{1, 2},
WANG Yanling^{1, 2},
ZHAI Daiting^{1, 2},
ZHOU Shaozhi^{1, 2},
WEI Kai^{1, 2},
CHENG Feng^{1, 2}

1.
Shandong Fifth Institute of Geology and Mineral Exploration, Taian, Shandong 271000, China
2.
Key Laboratory of Karst Collapse Prevention and Control of Shandong Provincial Bureau of Geology and Mineral Resources, Taian, Shandong 271000, China

Received Date: 2021-01-11
Available Online: 2023-02-23

Abstract

Abstract

The karst collapse in Shandong Province has occurred continuously since 1960s, showing the characteristics of wide distribution and great harm. In recent years, with the development of China’s economy, the geological disasters caused by karst collapse have taken place widely and frequently. Therefore, it is significant for us to study development characteristics and inducement of karst collapse. Carbonate rocks chiefly compose soluble rock, and the main rock types are limestone and dolomite, including the transitional type and metamorphic product—marble, which are mainly distributed in the Sinian, Late Cambrian and Ordovician periods. The main geological structure in the study area is fault structure, and most of karst collapses are located in the fault zone, its effecting zones and fold developing area. The aquifer rock group of karst water include limestone and dolomite of Cambrian and Ordovician, and karst development is conducive to vertical precipitation and pore water infiltration. Artificial groundwater exploitation is the main route of water discharge, and mass exploitation has led to landing funnels of karst water in the study area. The change of hydrodynamic field is the most important factor causing karst collapse.Based on previous studies and the results of investigation and monitoring, the spatial and temporal distribution law of karst collapse in Shandong is summarized. Then the background conditions and influencing factors of several main subsidence areas are expounded from the aspects of bedrock characteristics, overburden characteristics, hydrodynamic conditions and external disturbance. Statistical analyses show that the karst collapse in Shandong is mainly distributed in 6 cities such as Jinan, Tai’an, Zaozhuang, Linyi, etc. But new subsidence areas such as Yantai, Jining, etc. have recently experienced increasing trend of karst collapse. Besides, the karst collapse usually occurs in the thin-covered karst area, and the strata are mainly Ordovician Majiagou group, followed by Sanshanzi formation and Cambrian Chaomidian formation. The thickness of soil layer in karst collapse area is less than 30 m, and the structure of overburden layer is mainly composed of multi-element structure, then binary structure and single-element structure, and the sloughing resistance of cohesive soil is related to its water content and porosity ratio. A large fluctuation of karst water level is the most important factor of collapse, and karst groundwater level is most likely to cause collapse when it fluctuates around the bedrock surface. Karst collapse areas in Shandong are mainly distributed in important groundwater source areas; therefore, the water level drop or fluctuation caused by irrational exploitation and utilization of groundwater is the main human-induced factor. The karst collapses in Laiwu iron mining area is obviously affected by the drainage in this area. In addition, the vibration load of the railway in Tai'an City and Dongwangzhuang-Xiwangzhuang of Dongping town is another important human factor.
- karst collapse,
- law of development,
- distribution characteristics,
- inducing factor,
- Shandong Province

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References(38)

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Analysis on development characteristics and inducement of karst collapse in Shandong Province

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