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Quantitative Characterization of Mining‐Induced Disturbed Aeolian Sandy Soil—A Case Study of Daliuta Mining Area, China

Bibliographic Data

ID21647760
AuthorsDejun Yang (0000-0002-1090-5722, School of Environment Science and Spatial Informatics China University of Mining and Technology Xuzhou China, corresponding author), Minyue Wang (0000-0002-1761-0900, School of Environment Science and Spatial Informatics China University of Mining and Technology Xuzhou China), Ping Luo (0000-0003-1126-0329, School of Environment Science and Spatial Informatics China University of Mining and Technology Xuzhou China), Jiachao Jiang (School of Environment Science and Spatial Informatics China University of Mining and Technology Xuzhou China), Jiachao Jian (China University of Mining and Technology), Xueyu Geng (0000-0002-6499-2251, School of Engineering The University of Warwick Coventry UK, corresponding author)
Year2025
Volume36
Issue9
Pages3094-3104
Publication date2025-05-30
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.5553
OpenAlexW4408338641
LanguageEN
Citations received1
References cited28

Mining leads to soil degradation and land subsidence, resulting in decreased soil quality. However, there are limited studies on the detailed effects of mining activities on soil properties, particularly in western aeolian sand. This study, therefore, quantitatively assessed the aeolian sandy soil disturbance induced by mining activities in the contiguous regions of Shanxi, Shaanxi, and Inner Mongolia. The following soil physical quality indices were measured in the pre (May 2015), mid (October 2015), and postmining period (April 2016), such as the soil water content (SWC), particle size (PS), soil penetration (SP), and soil saturated hydraulic conductivity (SSHC). The results showed that mining activities brought irreversible effects on soil structures. In the pre‐mining period, land subsidence broke up large soil particles, destroying soil structure, leading to decreased PS (218.33 vs. 194.36 μm), SP (4615.56 vs. 2631.95 kPa), and subsequently decreased SSHC (1.12 vs. 0.99 cm/min). Rainfall during the midmining period exacerbated this fragmentation. Thereafter, low temperatures and humidity caused the soil to freeze, allowing the small soil particles to merge into larger ones. Meanwhile, the natural re‐sedimentation, subsidence, and heavy mechanical crushing in the post‐mining period increased PS and SP. The SSHC hence increased to 1.21 cm/min. Furthermore, the evaluation of soil indices from different stress zones showed that the external pulling stress zone always had a higher SSHC than the neutral zone in any mining period, possibly due to the presence of large cracks and high SWC. This study contributes to the understanding of the impact of mining activities on soil physical qualities, providing a theoretical basis and quantitative guidance for the surface damage caused by coal mining in the aeolian sandy area in Western China

Aeolian processes · Archaeology · China · Geography · Geomorphology · Mining engineering · Environmental Science · Geomechanics and Mining Engineering · Geoscience and Mining Technology · Mine drainage and remediation techniques · Geology

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Citations per year1
Citation span2026 - 2026 (1)
Highly citedNo

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