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Article

The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms

1
School of Karst Science, Guizhou Normal University, Guiyang 550001, Guizhou, China
2
Guizhou Provincial Key Laboratory of Information System of Mountainous Areas and Protection of Ecological Environment, Guizhou Normal University, Guiyang 550001, Guizhou, China
3
Institute of Biology, Guizhou Academy of Sciences, Guiyang 550001, Guizhou, China
*
Author to whom correspondence should be addressed.
Int. J. Environ. Res. Public Health 2020, 17(8), 2889; https://doi.org/10.3390/ijerph17082889
Received: 29 March 2020 / Revised: 17 April 2020 / Accepted: 19 April 2020 / Published: 22 April 2020
(This article belongs to the Section Environmental Remediation and Management)
Karst landforms are widely distributed in Guizhou Province, and the karst terrain is complex. To investigate the spatial distribution characteristics of soil organic carbon (SOC) in topsoil in different karst landforms, a total of 920 samples were taken from different karst landforms. The study areas, Puding, Xingyi, Guanling, Libo and Yinjiang in Guizhou Province, represent the karst plateau (KP), karst peak-cluster depression (KPCD), karst canyon (KC), karst virgin forest (KVF) and karst trough valley (KTV) landforms, respectively. The characteristics of the SOC contents in areas with different vegetation, land use and soil types under different karst landforms were analyzed. The dimensionality of the factors was reduced via principal component analysis, the relationships among SOC content and different factors were subjected to redundancy analysis, and the effects of the main impact factors on SOC were discussed. The results showed that there was a large discrepancy in the SOC contents in the topsoil layers among different types of karst landforms, the changes in the SOC content in the topsoil layer were highly variable, and the discrepancy in the upper soil layer was higher than that in the lower soil layer. The SOC contents in the 0–50 cm topsoil layers in different karst landforms were between 7.76 and 38.29 g·kg−1, the SOC content gradually decreased with increasing soil depth, and the descending order of the SOC contents in different karst landforms was KTV > KVF > KC > KPCD > KP. View Full-Text
Keywords: soil organic carbon (SOC); spatial heterogeneity; impact factor; effect mechanism; different karst landforms; Guizhou Province in SW China soil organic carbon (SOC); spatial heterogeneity; impact factor; effect mechanism; different karst landforms; Guizhou Province in SW China
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MDPI and ACS Style

Wang, X.; Huang, X.; Hu, J.; Zhang, Z. The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms. Int. J. Environ. Res. Public Health 2020, 17, 2889. https://doi.org/10.3390/ijerph17082889

AMA Style

Wang X, Huang X, Hu J, Zhang Z. The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms. International Journal of Environmental Research and Public Health. 2020; 17(8):2889. https://doi.org/10.3390/ijerph17082889

Chicago/Turabian Style

Wang, Xingfu, Xianfei Huang, Jiwei Hu, and Zhenming Zhang. 2020. "The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms" International Journal of Environmental Research and Public Health 17, no. 8: 2889. https://doi.org/10.3390/ijerph17082889

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