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2020 Vol. 39, No. 1

Display Method:
Karst hydrogeologic structures of the shale-gas exploration and exploitation area in Fuling, Chongqing
ZHU Jiliang, XU Mo, SUN Jianping, KANG Xiaobing, SHI Xiaodi
2020, 39(1): 1-10. doi: 10.11932/karst2019y32
Abstract:
Influenced by the carbonate facies and karst development degree, the types and characteristics of karst hydrogeological structures are different. Such a structural feature leads to variable pollutants in groundwater. In the shale gas development zone of Sichuan and Chongqing with widespread carbonate, the distribution of groundwater system and its cyclic evolution are more complicated. The identification of karst hydrogeological structure can provide effective guidance for the development and utilization of shale gas, and reduce or even avoid pollution of groundwater by shale gas development. Taking the area of Jiaoshiba-Luoyunba, a typical area of the Fuling shale gas exploration and exploitation zone in Chongqing as an example, this work studies the distribution characteristics of carbonate rocks, the development of karst and the occurrence and dynamic cycle of karst water in the shale gas exploration and exploitation area.Four types of karst aquifers, T1j-T2l, T1d, P2c-P2w and P1y, and the two types of concentrating and dispersing modes, are summarized. The system analysis method is used to extract four karst hydrogeological structures, gentle mono-slope, layered, anticline-folded multi-layer, and fault hydrogeological structures, of which the former two are of a pipeline-crack medium with smooth groundwater runoffs, prone to karst water pollution. In the latter two types of structures, the karst medium is dominated by crack networks with finite depth and extension, thus the distance and range of pollutant migration are small and the pollution capacity is limited.
A brief review on the factors affecting deposition of travertines in hot springs
LIU Haisheng, ZHOU Xun, ZHANG Yuqi, HAI kuo, YU Mingxiao, TAN Mengru, SHANG Ziqi
2020, 39(1): 11-16. doi: 10.11932/karst20200101
Abstract:
Travertines or tufas are non-marine carbonate precipitates around springs, rivers, lakes and caves, a manifestation of material migration in water cycles on lands. Studying the formation of travertines is helpful to understand the material migration regularity in local hydrologic circulation processes and indirectly examine the conditions of paleo-climate and paleo-hydrogeology. There are various travertines deposits near some of the hot springs. This paper presents a brief review on the formation of travertines from hot springs and the main factors controlling the deposition of travertinesand their interrelation. Research suggests that hydrochemical conditions are the material basis and necessary conditions for travertine deposition, which are the sufficient conditions for travertine deposition. Biological effects may accelerate the travertine deposition and the depositional environment may indirectly control the travertine deposition through changing hydrochemical or hydrodynamic conditions.
Effect of exogenous water and acid on karst carbon sink in the Wanhuayan underground river system
LIU Pengyu, ZHANG Liankai, HUANG Qibo, QIN Xiaoqun
2020, 39(1): 17-23. doi: 10.11932/karst2019y39
Abstract:
The petrochemical weathering process in the basin is an important part of the global carbon cycle.In recent years,increasing attention has focused on the effects of exogenous water (silicate weathering) and exogenous acid on the global carbon cycle in the estimation of hydrochemical carbon sink fluxes in the watershed.In this study,the Wanhuayan underground river system is selected as the study area,where the proportions of silicate rock distribution area and carbonate rock distribution area are 64% and 36%,respectively.In 2017,a one-year sampling monitoring was carried out at the entrance of the cave,and the ion composition of 13 water points in the Wanhuayan underground river system was monitored in April and September,respectively.The chemical weathering rate and CO2 consumption flux of the basin rocks were calculated by using the hydrochemical equilibrium method and Galy model.The process of rock weathering and carbon cycle in the system was analyzed.The results show that the rate of CO2 consumption by rock weathering in the Wanhuayan underground river system is 31.02 t?(km2?a)-1,with dominant carbonate weathering which is 20 times that of silicate rock dissolution.Moreover,carbonate weathering accounts for 92.16% of CO2 consumption in the whole basin.The contribution rate of different rock weathering types to carbon flux is 87.06%,of which carbonate dissolved carbonate rocks is the largest.The external water in the upper reaches of the basin has a great role in promoting the karst carbon sink. After the external water imported,the carbon sink rate of carbonate rock can be twice that of the non-external water sink in the basin.Sulphuric acid dissolved carbonate rocks took the second place,accounting for 9.24%;carbonate weathered silicate rock is the smallest,which is 3.7%.The influence of sulphuric acid on rock weathering should be removed when calculating carbon sink in river basins.
Dynamic characteristics and genesis of strontium-rich groundwater in Xintian county, Hunan Province
SU Chuntian, YANG Yang, BA Junjie, LUO Fei, LI Xiaopan, ZHAO Guangshuai
2020, 39(1): 24-33. doi: 10.11932/karst2019y34
Abstract:
In order to understand the dynamic characteristics of Sr-rich groundwater in Xintian county, Hunan Province, two sites were sampled and analyzed regularly for one year(January to December 2017). The results show that the content of Sr2+ in decline spring S045 remains stable in wet , normal and dry seasons with values of 0.27 mg?kg-1, 0.25 mg?kg-1 and 0.26 mg?kg-1, respectively. The hydrogeological characteristics determine that the dilution effect of rainfall on Sr2+ content in the decline spring S045 is limited, which is the main reason for the relative stability of Sr2+ content in this spring throughout the year. The Sr2+ content in the ZK1 well decreases in wet, normal and dry seasons with values of 0.73 mg?kg-1, 0.68 mg?kg-1 and 0.52 mg?kg-1, respectively. The variation of water level caused by the different water circulation conditions leads to different mixing ratios of high strontium subsurface water and low strontium shallow subsurface water, which is the reason why strontium content in the ZK1 well is positively correlated with atmospheric rainfall. Analysis using the ion ratio method shows that the γ(Na?) /γ(Cl?) in the decline spring S045 is 0.78, 0.44 and 0.49, γ(HCO〖_3^-〗+SO〖_4^(2-)〗) /γ(Ca2++Mg2+) is 0.99, 0.98 and 0.96, γ(Na?) /γ(Cl?) in ZK1 well is 75.24, 71.34 and 126.08, and γ(HCO〖_3^-〗+SO〖_4^(2-)〗) /γ(Ca2++Mg2+) is 37.13, 30.54 and 44.89 in wet, normal and dry seasons, respectively. They indicate that the groundwater experienced cation exchange in the ZK1 well. The average values of the γ(Cl?) /γ(Ca2?) coefficients in the decline spring S045 are 1.09×10-2 in wet season, 1.06×10-2 in normal season and 1.05×10-2 in dry season, respectively. The average values of the γ(Cl?) /γ(Ca2?) coefficients in ZK1 well are 1.29 in wet season, 0.98 in normal season and 0.94 in dry season, respectively. The γ(Cl?) /γ(Ca2?) in the ZK1 well is significantly higher than that in the decline spring S045, indicating that the hydrodynamic condition of the ZK1 well is weaker than that of the decline spring S045, and it is an important factor for the higher Sr2+ content in the ZK1 well than that in the decline spring S045.
Health assessment of karst groundwater ecosystem of Jinci spring area
LU Shuaishuai, ZHENG Xiuqing, LI Xuqiang, CHEN Junfeng, ZHANG Yongbo, ZANG Hongfei
2020, 39(1): 34-41. doi: 10.11932/karst2019y18
Abstract:
The concept of karst groundwater ecosystem was proposed, and its characteristics, functions and threats were discussed in this paper. The karst groundwater ecosystem health assessment index system was constructed under the superposition of natural and human factors based on the driving force-pressure-state-impact-response (DPSIR) model. The analytic hierarchy process (AHP) was used to determine the index weights. The health status of karst groundwater ecosystem was determined by the comprehensive assessment method, which was divided into five levels, very healthy, healthy, sub-healthy, unhealthy and diseased. Taking the Jinci spring area as an example, the spatial analysis technique of ArcGIS is used to analyse the health assessment grade of karst groundwater ecosystem. The results show that the coal mining area in the spring area is in an unhealthy state, the eastern plain area and the central runoff area are in a sub-healthy state, the carbonate exposed area and the surrounding area of Fenhe river are in a healthy state, accounting for 29%, 31% and 40% of the total area of Jinci spring area, respectively.
Tracer test and analysis of groundwater system in a karst area of southwest China
ZHANG Lang, LI Jun, PAN Xiaodong, HUANG Xiaorong, PENG Cong
2020, 39(1): 42-47. doi: 10.11932/karst2019y36
Abstract:
The study area is located in a karst area of Sichuan Province in southwest China. It hosts intense karst development and complex hydrogeological conditions, where underground karst forms include caves, fissures and conduits. Taking this typical karst area as an example, this paper analyzes the application of tracer tests in karst conduit connectivity and acquisition of hydrogeological parameters, analyzes the karst groundwater runoff regular pattern, and estimates the structural characteristics and hydrogeological parameters of karst underground aquifers. These data will facilitate rapid and accurate determination of the scope of groundwater recharge, analyzing the causes of spring discharge cutoff and pollution, and providing a basis for spring protection. First, a sinkhole is selected as the release point, and the groundwater dew point is taken as the receiving point to judge the actual direction of the underground runoff and the hydraulic relation from the west side and the east side of sinkhole respectively. A quantitative analysis of breakthrough curves of the tracers is carried out by Qtracer2, and the tracer recovery rate, average groundwater velocity, maximum velocity, structural characteristics and hydrogeological parameters of the karst conduit are determined. The results show that there is no direct hydraulic relation between the sinkhole and the receiving points JS01 and JS03. While there is a hydraulic link between the sinkhole and the receiving point JS02, where the karst conduit extremely developed, the aquifer medium is uneven, and the groundwater movement path is relatively smooth, which is a typical turbulent flow state. The main direction of the underground runoff of the sinkhole is from west to east. In the period of heavy rainfall during the wet season, the point JS04 can receive sodium fluorescein, indicating that the underground water level increases during the wet season, which will lead to discharge of partial water volume to the west side of the sinkhole.
Study on the land use coupling evolution of mountain-basin systems in karst areas
ZHAO Yuluan, WEI Xiaofang, LI Xiubin
2020, 39(1): 48-53. doi: 10.11932/karst2019y38
Abstract:
This paper elaborates the necessity of research on the coupling evolution of land use in karst mountain-basin systems, and summaries the progress and issues in this aspect. Then, an analysis framework of the land use coupling evolution mechanism of mountain-basin systems in karst areas is established based on the telecoupling framework model. Next, four issues that need to be addressed are suggested, including coupling evolution process, driving mechanism, management and control mode and effect evaluation of the land use in mountain-basin systems. Finally, thought lines of research and technological approaches are proposed to provide reference for future case study.
Exploration and research on the preservation environment of cave sites: An example of the Zengpiyan site in Guilin
WEI Minjie, JIANG Guanghui, GUO Fang
2020, 39(1): 54-61. doi: 10.11932/karst20200102
Abstract:
Reasonable exploitation, utilization and protection of cave sites are important premises for heritage and development of site culture. Taking the Zengpiyan cave site in Guilin as an example, this work identifies the problems in the process of preservation and development based on the detection and monitoring of the site and the recognition of the hydrogeological units and groundwater characteristics of the site. Then possible measures were suggested for the protection of the site, which will aid in the protection of cave sites under similar conditions. The results show that there are different problems in the three protected areas of the Zengpiyan site, i.e. the core protected area is facing the risk of chemical erosion, the existing protection methods of the first-class protected area lack diversity and the second-class protected area lacks sufficient monitoring. Accordingly, the following measures are put forward, (1) The mechanism of groundwater and reductive environment on the cultural layer erosion should be studied in depth in the core protected area. (2) The management of sewage discharge should be strengthened and the forms and means of cave site protection should be increased in the first-class protected area. (3) The monitoring of environmental indicators should be strengthened and the construction of projects within protected areas should be controlled in the second-class protected area. Furthermore, the protection measures should be extended to general cave sites, including establishing a long-term monitoring system that can show the environmental dynamics; using 3S technology to establish a monitoring network and assist planning; standardizing the exploration and planning management of cave sites; and improving the publicity of cave site protection and public participation capacity through multiple ways.
Impacts of human activities on net primary productivity of vegetation in Guizhou Province from 2000 to 2014
SHENG Yezi, ZENG Mengxiu, LIN Degen, PENG Haijun, ZHU Lidong, LI Fengquan, YU Yihong, WANG Nengjing
2020, 39(1): 62-70. doi: 10.11932/karst2020y01
Abstract:
Karst rocky desertification, the most significant ecological problem in Guizhou Province, southwestern China, is primarily driven by human activities in recent years. As a main signature of this phenomenon, vegetation degradation can be reflected by Net Primary Productivity (NPP), which is a key indicator of production capacity of the terrestrial ecosystem. However, so far less quantitative analyses have been made on the impact of human activities on vegetative NPP in Guizhou Province, which is of great significance for coordinating the relationship between human activity and karst rocky desertification control, as well as improving the quality of karst eco-environment. In this study, we established the Relative Contribution Index (RCI) by using actual NPP (ANPP) based on MODIS MOD17A3 data and potential NPP (PNPP) based on the Carnegie Ames Stanford Approach (CASA) model. Then, in combination of the classification of karst landform proportion, we analyzed the spatial-temporal variations of human activities and their influence on NPP in Guizhou Province from 2000 to 2014. Finally we discussed the contributions rates of different factors for human activity on RCI values using Correlation Analysis (CA). The results indicate that human activities in Guizhou Province promoted the increase of NPP, and the degree of the influence first increased and then decreased from 2000 to 2014. In the southeastern and northern edges of Guizhou Province where the proportion of karst landform area is less than 51.8%, the RCI value fluctuated violently and was greatly affected by human activities. However, in the areas where the proportion of karst landform is higher than 51.8%, the impact of human activities was relatively weaker and the variation was gentler. Additionally, human activities in the northeast, central and western parts of Guizhou Province generally had negative effects on the ecological environment from 2000 to 2014, while the effects in the southeastern and northern marginal areas were positive. In the past 15 years, the positive impact of human activities on the ecological environment in most areas of central and northern Guizhou Province has increased, while the degree of human intervention in the southwestern marginal area has decreased and the negative interference of human activities in some areas in the southeastern part has increased. Moreover, the CA results show that the total plant coverage area of crops, total agricultural output value, proportion of urban population, gross domestic product per head, disposable income of urban residents and highway mileage had significant positive correlation with RCI values of Guizhou Province during the period from 2000 to 2014, while the population density had a significant negative correlation with RCI values. Among them, agricultural activities played an important role in the negative impact of human activities. On one hand, urbanization and economic development promoted the growth of livable demand and strengthened the positive impact of human activities on the ecological environment; on the other hand, they also expanded the demand for resource development, transportation and public infrastructure. Thus, the destructive interference of human activities on the ecological environment was unavoidable. In addition, compared with other areas, the areas with moderate karst landforms were more likely to be negatively affected by agricultural production, urban development and highway construction.
Controlling factors of macroscopic oil-water distribution in fractured-vuggy carbonate reservoirs in west of area 10 in the Tahe oilfield
ZENG Cheng, CHEN Benchi, LI Zongjie, MA Xuejun, XUE Mingxi
2020, 39(1): 71-79. doi: 10.11932/karst2020y001
Abstract:
Ordovician carbonate fractured-vuggy reservoirs in the Tahe oilfield have strong heterogeneity and complex oil-water distribution. It is of great significance for controlling water and stabilizing oil production in fractured-vuggy reservoirs to reveal the macroscopic oil-water distribution law at a regional scale (10 km × 10 km). Based on the work of omni-directional and high-precision three-dimensional seismic data processing, inversion and interpretation, this paper comprehensively analyzes the karst paleostructure and the oil-water regime in the process of oilfield development, and discusses the controlling factors of the macro-horizontal distribution pattern of oil-water in carbonate fractured-vuggy reservoirs in the Tahe oilfield. The results show that a relatively homogeneous paleokarst aquifer was formed in the middle Caledonian Episode I karst period. After hydrocarbon was injected into the paleokarst aquifer medium in the early Hercynian period, deep hydrothermal activity in the late Hercynian period sealed and fixed the fracture-cave body, resulting in fracture-cave separation, and established the present macroscopic distribution pattern of oil and water in the reservoirs.
Study on the genesis mechanism and prevention and control measures of shallow overburden karst collapse in central Guizhou area: An example of Baiyun primary school, Ziyun county, Guizhou Province
YANG Yuanli, MENG Fantao, LI Minghui
2020, 39(1): 80-87. doi: 10.11932/karst20200103
Abstract:
Central Guizhou Province lies in the second topographic step of the plateau,with average altitudes 800-1,600 m,characterized by widely distributed soluble rocks,extremely developed karst landscapes,thin Quaternary soil layers and shallow groundwater with strong groundwater flow dynamics.Karst ground collapse is one of the major geological hazards in this area.In order to clarify the cause and mechanism of karst collapse in the Baiyun primary school,Ziyun county,Guizhou Province,this work carried out field investigations,geophysical exploration,geological drilling of hydrogeology engineering,and tests on rock and soil samples.Comprehensive research indicates that the karst collapse in the Baiyun primary school was a combined effect of special “water-soil-rock” adverse factors.According to the characteristics of geotechnical structure of the collapse area,it is suggested that the comprehensive prevention and control measures of "monitoring prevention+water control+engineering treatment" should be adopted before the site selection of future projects in karst areas of central Guizhou.
Study on "four in one" control technology and its application of karst gas in the Songzao mining area
YUAN Xiangtao, LIU Yan, ZHOU Dongping, JIANG Hecai, CHEN Jingjiang
2020, 39(1): 88-94. doi: 10.11932/karst2019y33
Abstract:
Karst developed well in coal measures strata in the Chongqing area, and some karst contains a large amount of poisonous gas. When karst is uncovered, poisonous gas may be to exhale or outburst. The main component of the poisonous gas is methane. The Songzao mining area hosts the most karst in the Chongqing region, while the Shihao coal mine and Datong No.1 mine are the most serious karst in the Songzao mining area. The coal-bearing strata in this mining area are Longtan formation of upper Permian. The thickness of coal measures strata is 66 meters to 80 meters, with 10-12 layers of coal-bearing strata. The total thickness of coal is 4.01 meters to 9.88 m, 7.58 m on average. Among them, M6, M7 and M11 coal seams in local mineable seams have outburst danger, while the M8 coal seam in the whole area is a serious outburst coal seam.The problem of karst gas has become an important disaster-causing factor affecting and restricting the safety of coal mine production. In order to ensure the construction safety of rock roadways in karst-affected areas and effectively prevent and control the karst gas disaster, the source and the occurrence law of karst gas in the Songzao mining area are analyzed by means of theoretical analysis and site tests. Results show that the main source of karst gas is the coal measures strata located at the top of Maokou limestone, i.e. M12, M11, M10, M9, M8, M7, and M6 coal seams in the mining area. The broom structure, semi-filling karst cave and concealed structure are gas enrichment areas, and low permeability of overburden rock in coal measures strata is also a key factor for generation of karst gas. The 12# gas roadway in the north three mining area of the Shihao coal mine and the W1603E gas roadway in the west No.1 mining area of Datong No.1 coal mine are selected as the test roadways. The "four-in-one" prevention and control technology of karst gas is adopted, which includes,(1) Prediction of small karst gas blocks; (2) Step-by-step local detection measures consisting of geophysical exploration, drilling and drill rod detection; (3) Local karst gas prevention and control technology with winding, draining, ventilating and plugging; (4) Safety protection measures. On-site application shows that strict implementation of "four in one" prevention and control technology can effectively prevent karst gas accidents, and can effectively use karst gas to ensure safe and orderly roadway excavation.
Study on the effectiveness of the microtremor HVSR method in detecting underground river pipelines and caves in karst areas
LIANG Donghui, GAN Fuping, ZHANG Wei, HAN Kai
2020, 39(1): 95-100. doi: 10.11932/karst20200104
Abstract:
The Microtremor HVSR (Horizontal-to-Vertical Spectral Ratio) method is a simple and effective tool in passive-source seismic exploration. When a significant change of velocity of the medium below the measuring site is present, the HVSR curve can exhibit corresponding abnormal shapes. The purpose of this work is explore the effectiveness of this method in detecting underground river pipelines and caves in karst areas. At the Dayanqian village in the Maocun underground river basin,field experiments were carried out,where exists an underground river pipeline exists.The plane position and cave height of this pipeline were determined by precise cave measurement.Three geophysical survey lines were arranged on the ground over the underground river pipeline in the study area, all of which were measured by the microtremor HVSR method and compared by the ground-penetrating radar measurement. The result shows that the anomaly position by the two geophysical methods are basically consistent with the actual plane position of underground river pipeline below the survey lines, which proves that the microtremor HVSR method can be used as an effective tool in the detection of underground river pipelines and karst caves.
Application of GPR scattering matrix to estimating azimuths of underground pipelines
CHEN Jun, CHI Changfeng, XU Dongsheng, LIANG Feng
2020, 39(1): 101-109. doi: 10.11932/karst20200105
Abstract:
This paper analyzes the properties of the scattering matrix S related to the incidence and scattering of ground penetrating radar and electromagnetic field. The four elements in the scattering matrix provide information corresponding to different polarization directions of the incident wave field. Based on this, the Alford rotates of scattering matrix S is used. to estimate the azimuth of the elongated target. Due to low amplitude and noise, the estimation of the angle is actually an unstable process. Therefore, the use of norm as a tool for screening the optimal amplitude is chosen to make the estimation of the angle more accurate and stable. The method is tested by using the simulation data obtained from the three-dimensional model of the metal tube buried in the uniform half space. When selecting the appropriate amplitude, the Frobenius norm ‖S‖F≥0.1?‖S‖F(max) is determined. The results show that the method of estimating the azimuth of the underground pipeline is effective.
Exploration and suggestions on development of the Shenxian cave in Fuping county, Hebei Province
ZHOU Wenlong, GAO Zhandong, WU Kehua, LI Youwei, LI Po, HE Wei
2020, 39(1): 110-118. doi: 10.11932/karst20200106
Abstract:
In 2015,a large karst cave, the Shenxian cave, was discovered by a 1∶50,000 scale hydrogeological survey of Fuping county,a Taihang mountains area. In 2017,we continued focused exploration to this cave by means of paperless cave survey and 3D laser scanning,and two data sets were compared to verify the accuracy of the survey.Tracing element experiments in the underground river of the Shenxian cave confirm that the Shenxian cave is connected with the Jinlong cave.Analysis of the development and evolution of the Shenxian cave and the evaluation of its resources landscape suggests that the geological relic landscape of this cave,especially its some combination forms,are of high value in the karst caves in North China,and some suggestions for protective development are put forward in order to provide precise support for the development of poverty alleviation through tourism in the contiguous and poverty-stricken areas.
Research status and prospect of karst Tiankengs in Guizhou Province
WU Jin, ZHANG Zhaohui
2020, 39(1): 119-126. doi: 10.11932/karst2019y35
Abstract:
Guizhou Province is located in the southwest of China, east of the Yunnan-Guizhou Plateau, topographically high in the west and low in the east. It is near the southeast continental margin, part of the upstream ecotone of the Yangtze River and the Pearl River. It is an important ecological barrier for the upstream areas of the Yangtze River and the Pearl River. This region hosts typical karst landforms which are widely distributed and of various types, and geographically distinct. Karst carbonate rocks are dominant where karst Tiankeng developed well. Karst Tiankeng is a negative geomorphology, widely present in central, northwest and southern Guizhou Province, China. It is characterized by large number, wide distribution and strong stability of inner environments. Based on the special geomorphology and topography of Guizhou, combined with research reports of karst Tiankeng availlable, this work conducted field investigations and statistical analysis of literature data on this phenomenon. The purpose is to review the research status of the geological background, origin, types and distribution patterns of karst Tiankeng in Guizhou, and puts forward the prospect of its development trend and research direction. The results show that, (1) There are 25 karst sinkholes in total in Guizhou. According to the depth, shape and scale, they are categorized into 3 super sinkholes, 2 large sinkholes, 18 medium sinkholes and 2 small sinkholes (diameter and depth less than 100 m); (2) In lithology, Guizhou karst Tiankeng is mainly composed of early Triassic Yongning town formation, Yelang formation, lower Triassic Luolou formation plus Ziyun formation and middle Triassic Xiaomitang formation plus Liangshuijing formation, including Triassic thick massive limestone, middle Carboniferous and lower Permian thick massive limestone; (3)The genesis of karst Tiankeng in Guizhou includes two types, collapse type and erosion type, and the former is primary; (4) This karst Tiankeng is mainly distributed in central, southern, western and northwestern Guizhou showing a trend of gradual decrease in number and scale from south to north and from west to east, and super or super-large Tiankeng concentrates in the south.
Study on the relationship between spatial distribution of karst caves and drainage density: An example of Guizhou Province
HUANG Liang, ZHAO Weiquan, LYU Sisi, YANG Jiafang, SU Weici
2020, 39(1): 127-136. doi: 10.11932/karst2020y02
Abstract:
Guizhou Province is located in the hinterland of southwest China, an important part of the Yunnan-Guizhou Plateau, with high mountains and deep gorges. It has subtropical humid monsoon climate with large rainfall, where carbonate strata and karst are widely distributed, and karst process is generally developed, resulting in rapid conversion of surface water into groundwater. Here strong dissolution and mechanical abrasion have shaped unique and magnificent karst landforms, such as peak clusters, peak forests, depressions, sinkholes, funnels, and underground rivers. This paper analyzes the relationship between the spatial distribution of caves and the density of river networks based on data of 4,789 caves and an 1∶200,000 hydrogeological map of Guizhou Province, and explains the genesis of such relationship from the perspective of lithology, structure, climate and topography. The results show that the karst caves in Guizhou Province are concentrated in the areas with low and medium river network density, exhibiting a patchy spatial pattern. The normal QQ map largely shows a normal distribution, indicating that the concentration of river network density at cave points is the result of mutual restriction of many factors. The cave points and river network density have a negative correlation in pure carbonate rock, carbonate rock interspersed with non-carbonate rock and non-carbonate rock areas. In carbonate rock area, the density of caves increases with the increases of temperature and precipitation, while the density of river network shows a trend of increase first and then decrease due to the varied degrees of karst development. The centers of folds and faults are the dominant area of cave development, where the density of the river network is relatively low, and the number of caves decreases with the increases of distance. In the terrain area below slope 25°, the number of caves is the largest, and the maximum river network density appears in the gentle area. With the increase of slope, the overall trend is decreasing. In the terrain range of slopes 25° to 30°, the number of caves tends to decrease. The conditions of lithology, structure, and climate have promoted the development of mature surface and underground water circulation systems in Guizhou. The surface water promotes the development of karst caves, which in turn restricts the development of surface runoff, making the density of cave river networks present a trend of concentrated distribution in low and medium values.