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The Spatiotemporal Variation Characteristics and Influencing Factors of Groundwater Level in Karst Mountainous Areas of Guiyang
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Xiaoqing Song1, 2, 3, Sheng Chen4, Ying Wang2, 3, Xiuchao Pu2, 3, Huan Chen2, 3
Chinese Journal of Underground Space and Engineering | 2026, 22(2) : 706 - 713
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Chinese Journal of Underground Space and Engineering | 2026, 22(2): 706-713
The Spatiotemporal Variation Characteristics and Influencing Factors of Groundwater Level in Karst Mountainous Areas of Guiyang
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Xiaoqing Song1, 2, 3, Sheng Chen4, Ying Wang2, 3, Xiuchao Pu2, 3, Huan Chen2, 3
Affiliations
  • 1.School of Environmental Studies, China University of Geosciences(Wuhan), Wuhan 430078, P. R. China
  • 2.No. 111 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development, Guiyang 550008, P. R. China
  • 3.Geo-Engineering Investigation Institute of Guizhou Province Co., Ltd., Guiyang 550008, P. R. China
  • 4.China Railway Development and Investment Group Co., Ltd, Kunming 650500, P. R. China
Published: 2026-04-20 doi: 10.20174/j.JUSE.2026.02.32
Outline
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In order to study the dynamic changes and amplitude values of groundwater level in karst mountainous areas, taking the karst mountainous city of Guiyang as an example, selecting daily monitoring data and precipitation data from nine groundwater level dynamic observation points from 2022 to 2023, autocorrelation and cross-correlation analysis are used to analyze the response of groundwater level to precipitation and explore the influence of runoff and drainage conditions and terrain slope on the dynamic changes of groundwater level. The results show that: (1) The groundwater level in the study area is buried at a depth of 1.21 ~ 27.68 m, with an annual variation range of 1.54 ~ 11.99 m, and there are significant differences in the spatiotemporal distribution of groundwater level dynamics; (2) The relevant analysis results indicate that there is a significant lag in the response of groundwater level to precipitation signals in the study area, with an average lag time of 0~4 days, and it gradually increases from the supply area to the discharge area; (3) The terrain slope is an important factor affecting the amplitude of groundwater level variation in karst mountainous areas. The terrain slope in the study area is positively correlated with the amplitude and variation of groundwater level, with linear goodness of fit (R2) of 0.65 and 0.78, respectively; (4) The depth of groundwater level gradually decreases from the recharge area to the discharge area, and the range of water level changes from the runoff area to the recharge area to the discharge area.

karst mountain  /  spatiotemporal variability  /  groundwater level dynamic  /  correlation analysis
Xiaoqing Song, Sheng Chen, Ying Wang, Xiuchao Pu, Huan Chen. The Spatiotemporal Variation Characteristics and Influencing Factors of Groundwater Level in Karst Mountainous Areas of Guiyang[J]. Chinese Journal of Underground Space and Engineering, 2026 , 22 (2) : 706 -713 . DOI: 10.20174/j.JUSE.2026.02.32
Year 2026 volume 22 Issue 2
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doi: 10.20174/j.JUSE.2026.02.32
  • Receive Date:2025-03-16
  • Online Date:2026-06-17
  • Published:2026-04-20
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  • Received:2025-03-16
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Affiliations
    1.School of Environmental Studies, China University of Geosciences(Wuhan), Wuhan 430078, P. R. China
    2.No. 111 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development, Guiyang 550008, P. R. China
    3.Geo-Engineering Investigation Institute of Guizhou Province Co., Ltd., Guiyang 550008, P. R. China
    4.China Railway Development and Investment Group Co., Ltd, Kunming 650500, P. R. China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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