中国西南岩溶山坡水土流失影响下不同土地利用条件下土壤理化性质的空间变异性

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-04-01 DOI:10.1002/esp.5827
Lei Chen, Keli Zhang, Yetong Li
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引用次数: 0

摘要

岩溶山坡一般具有不同的土地利用特征。土地利用和山坡位置严重影响土壤侵蚀,进而影响土壤发育过程和土壤特性模式。然而,岩溶山坡上土地利用对土壤理化性质的影响以及它们之间的空间变化和相互关系还不完全清楚。因此,研究人员选择了九个土壤类型、坡度、海拔、坡面和以往耕作方式相似的地点开展进一步研究。本研究旨在量化中国西南岩溶山坡上不同土地利用对土壤理化性质和化学平衡的影响的空间分布、变异性和相关性。土壤物理特性受坡度和土壤深度的影响较大。土壤容重和粘土含量随土壤深度的增加而增加,而含沙量则相反。在三种土地利用方式中,坡度较低位置的土壤容重变化最大,而坡度较高位置的粘粒和沙粒变化最大。土壤物理特性的平均空间变异系数(CV)依次为:砂(11.08%)>;粘土(7.77%)>;容重(6.85%)>;粉土(3.81%)。土壤化学性质的平均空间变异系数为:可利用钾(44.49%);全磷(16.77%);全碳(16.31%);全氮(13.09%);可利用钾(8.45%);全钾(7.51%)。总体而言,土壤理化性质与岩溶山坡的坡位和土地利用有显著的空间差异。与物理性质相比,土壤化学性质的空间差异更大,而且两者之间存在显著的相关性。研究结果不仅有助于深入了解土地利用对岩溶山坡侵蚀过程和机制的影响,还为岩溶生态系统的可持续恢复提供了科学依据。
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Spatial variability of soil physicochemical properties under different land uses impacted by erosion on karst hillslopes in Southwest China

Karst hillslopes are generally characterized by different land uses. Land use and slope position impact soil erosion seriously, which in turn impacts the process of soil development and the patterns of soil properties. However, the impact of land use on soil physicochemical properties and the spatial variations and correlations between them are not fully understood on karst hillslopes. Therefore, nine sites had similar soil types, slope gradients, elevations, slope aspects and previous tillage practices were selected to conduct further research. This study was conducted to quantify the spatial distribution, variability and correlation of soil physical and chemical properties and stoichiometries as impacted by different land uses on a karst hillslope in Southwest China. Soil physical properties were significantly affected by slope position and soil depth. The soil bulk density and clay content increased with soil depth, while the opposite was true for the sand content. For the three land uses, the soil bulk density varied the most at the lower slope position, while clay and sand particles varied the most at the middle slope position. The mean spatial coefficient of variation (CV) of soil physical properties was ranked as sand (11.08%) > clay (7.77%) > bulk density (6.85%) > silt (3.81%). The mean spatial CV of soil chemical properties was ranked as available K (44.49%) > total P (16.77%) > total C (16.31%) > total N (13.09%) > available P (8.45%) > total K (7.51%). Overall, soil physicochemical properties exhibited significant spatial differences with slope location and land use on karst hillslopes. Soil chemical properties had greater spatial variation than physical properties, moreover, there were significant correlations between them. The results not only contribute to a deeper understanding of the impact of land use on the erosion process and mechanism on karst hillslopes but also provide a scientific understanding of the sustainable restoration of karst ecosystems.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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