Journal of Geographical Sciences >
Spatial patterns and controlling factors of the evolution process of karst depressions in Guizhou province, China
Zhang Tao (1998-), Master Candidate, specialized in karst depression resource evaluation and engineering development. E-mail: zhangtaogzu@163.com |
Received date: 2022-12-15
Accepted date: 2023-07-20
Online published: 2023-10-08
Supported by
The Science and Technology Foundation of Guizhou Province(2022-212)([2020]1Z052)
National Natural Science Foundation of China(42167025)
Karst depressions are common negative topographic landforms formed by the intense dissolution of soluble rocks and are widely developed in Guizhou province. In this work, an inventory of karst depressions in Guizhou was established, and a total of approximately 256,400 karst depressions were extracted and found to be spatially clustered based on multidistance spatial cluster analysis with Ripley's K function. The kernel density (KD) can transform the position data of the depressions into a smooth trend surface, and five different depression concentration areas were established based on the KD values. The results indicated that the karst depressions are clustered and developed in the south and west of Guizhou, while some areas in the southeast, east and north have poorly developed or no clustering. Additionally, the random forest (RF) model was used to rank the importance of factors affecting the distribution of karst depressions, and the results showed that the influence of lithology on the spatial distribution of karst depressions is absolutely dominant, followed by that of fault tectonics and hydrological conditions. The research results will contribute to the resource investigation of karst depressions and provide theoretical support for resource evaluation and sustainable utilization.
ZHANG Tao , ZUO Shuangying , YU Bo , ZHENG Kexun , CHEN Shiwan , HUANG Lin . Spatial patterns and controlling factors of the evolution process of karst depressions in Guizhou province, China[J]. Journal of Geographical Sciences, 2023 , 33(10) : 2052 -2076 . DOI: 10.1007/s11442-023-2165-z
Figure 1 Basic characteristics of Guizhou province, southwest ChinaNote: The lower right map indicates the geographical location of Guizhou province; the blue overlay area indicates the location of karst depressions; the dark blue line indicates the Miaoling watershed, which divides the Yangtze River basin and the Pearl River basin, with the Yangtze River basin to the north and the Pearl River basin to the south; the black dashed line is the tectonic unit demarcation line, and I1-III indicate the tectonic unit codes; the circular icons and notes indicate the geographical location and names of typical geomorphic wonders in Guizhou. |
Table 1 Data used and corresponding sources |
Data | Time | Spatial resolution | Format | Source |
---|---|---|---|---|
Digital elevation model (DEM) | 2011 | 12.5 m×12.5 m | TIF | National Aeronautics and Space Administration (https://urs.earthdata.nasa.gov) |
Geological map of Guizhou province | 2009 | 1:500,000 | JPG | Geological Cloud (https://geocloud.cgs.gov.cn/) |
Hydrogeological map of Guizhou province | 1985 | 1:500,000 | JPG | Geological Cloud (https://geocloud.cgs.gov.cn/) |
Average annual rainfall | 1960-2018 | - | TXT | China Meteorological Data Network (https://data.cma.cn/) |
Vegetation cover | 2021 | 30 m×30 m | TIF | Geospatial Data Cloud (https://www.gscloud.cn/) |
Figure 2 Brief description of depression identification stepsNote: (a) Import of a 12.5 m DEM and preliminary processing; (b) Filling of the DEM to obtain overflow elevation; (c) Identification and extraction of closed depressions by the contour tree method; (d) Aerial view of a sample depression by a UAV. |
Table 2 Typical negative landforms and their characteristics |
Negative terrain type | Definition/Characteristics |
---|---|
Karst depression | It refers to the common type of closed negative landform formed by karst processes acting on rock in karst areas, the lack of surface drainage outlets, forms a closed shape, mostly circular, surrounded by low mountains or peak forests, the bottom is “pot shaped”, the radius is tens of metres to thousands of metres, the area is generally from a few square kilometres to more than ten square kilometres (Gao et al., 2012). |
Sinkholes (tiankeng) | A karst negative terrain with steep walls, depth and diameter up to hundreds of metres developed in karstic carbonate areas (Shui et al., 2015). |
Water fall hole | An inlet of surface water into the ground, similar in surface shape to a funnel, which opens in the ground and leads to a deep fissure (underground river or cave) in the ground (Peng, 2020). |
Doline | After karst ground is dissolved and karst collapses, a small inverted cone-shaped closed depression landscape with small bottom is formed. Its depth is not large, its slopes are gentle, its edges are not obvious, and its shape is mostly saucer-shaped (He, 2018). |
Karst valley | A landform formed by the chemical dissolution and erosion of soluble rocks by running water in the form of a long depression or valley with a U-shaped surface (Qin et al., 2020). |
Karst basin (BAZI) | It refers to some broad and flat basins or valleys in karst areas, ranging from hundreds to thousands of metres in width and up to tens of kilometres in length. The basins have steep slopes and uniform bottoms, which are flat and open. In southwest China, it is often called BAZI (Zhou et al., 2012). |
Artificial negative terrain | Large-scale negative terrain formed by excavation by humans, such as dry reservoirs, abandoned mines and so on. |
Table 3 Classification of factors influencing the aggregation of the spatial distribution of karst depressions |
Factors | Classification | Reclassification | Normalization | Reference | |
---|---|---|---|---|---|
Internal factors | Rock (Ro) | Dolomite | 1 | 0 | (Ding et al., 2019b) |
Limestone | 2 | 0.2 | |||
Dolomite interbedded with limestone | 3 | 0.4 | |||
Carbonatite intercalated clastic rocks | 4 | 0.6 | |||
Carbonates interbedded with clastic rocks | 5 | 0.8 | |||
Clastic rocks | 6 | 1.0 | |||
Fault (Fa) | 0-1 km buffer zone | 1 | 0 | (ÖZtÜRk, 2018) | |
1-2 km buffer zone | 2 | 0.25 | |||
2-3 km buffer zone | 3 | 0.50 | |||
3-4 km buffer zone | 4 | 0.75 | |||
>4 km buffer zone | 5 | 1.0 | |||
Surface water system (Sr) | 0-0.5 km buffer zone | 1 | 0 | (Cahalan et al., 2018) | |
0.5-1.5 km buffer zone | 2 | 0.33 | |||
1.5-3.0 km buffer zone | 3 | 0.67 | |||
>3.5 km buffer zone | 4 | 1.0 | |||
Underground River (Ur) | 0-0.5 km buffer zone | 1 | 0 | (Panno et al., 2013) | |
0.5-1.5 km buffer zone | 2 | 0.33 | |||
1.5-3.0 km buffer zone | 3 | 0.67 | |||
>3.5 km buffer zone | 4 | 1.0 | |||
External factors | Annual rainfall (Mar) | ≥1300 mm | 1 | 0 | (Xu et al., 2017) |
1200-1300 mm | 2 | 0.33 | |||
1100-1200 mm | 3 | 0.67 | |||
1000-1100 mm | 4 | 1.0 | |||
Slope (Sl) | <5° flat slope | 1 | 0 | (Al-Kouri et al., 2013) | |
6°-15° gentle slope | 2 | 0.25 | |||
16°-25° slope | 3 | 0.50 | |||
26°-35° steep slope | 4 | 0.75 | |||
>35° sharp slope | 5 | 1.0 | |||
Vegetation cover (Vc) | >80% | 2 | 0.25 | (Ding et al., 2019a) | |
80%-60% | 3 | 0.50 | |||
60%-40% | 4 | 0.75 | |||
40%-20% | 5 | 1.0 | |||
<20% | 2 | 0.25 |
Figure 3 Multidistance spatial cluster analysis (a) and Jenks natural breaks (b)Note: KD stands for kernel density. |
Figure 4 Kernel density distribution of karst depressions in Guizhou province, southwest ChinaNote: A stands for Class A superconcentrated; B stands for Class B concentrated; C stands for Class C somewhat concentrated; D stands for Class D weakly concentrated; E stands for Class E nonconcentrated. |
Figure 5 The results of the explanatory strength and precision analysis of the influencing factors of the spatial distribution of karst depressions based on the RF modelNote: Ro stands for rocki; Fa stands for fault. Sr stands for surface water system; Ur stands for underground river; Mar stands for annual rainfall. Sl stands for slope. Vc stands for vegetation cover degree. Whole stands for the karst area of Guizhou province. A stands for Class A superconcentrated. B stands for Class B concentrated. C stands for Class C somewhat concentrated. D stands for Class D weakly concentrated. E stands for Class E nonconcentrated. |
Figure 6 Lithologic reclassification and lithologic distribution of Guizhou province, southwest ChinaNote: CPCR stands for the Carboniferous to lower Permian carbonate unit; TCR stands for Middle and Lower Triassic carbonate unit; CCR stands for middle and upper Cambrian carbonate unit; NCR stands for the noncarbonate rock unit (after Xie et al., 1987; Li, 2001). |
Figure 7 The results of the overlay analysis of geological conditions and karst depressions in Guizhou province, southwest ChinaNote: These plots include the number of depressions developed (histogram), the percentage of the total number of depressions (pie chart), and the density of depressions (dotted line chart). |
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