Feldspathic sandstone as an emerging soil stabilizer for aeolian sand in the Mu Us Sandy Land: insights into particle size distribution

Stabilization of aeolian sand is essential for achieving desertification control, soil and water conservation, and agricultural development in sandy lands. Feldspathic sandstone is a soft clay rock widely found in the Mu Us Sandy Land. The purpose of this study was to ascertain the mechanism for aeolian sand stabilization with feldspathic sandstone from the perspective of particle size distribution. Feldspathic sandstone was added to aeolian sand at different ratios (<i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:0, 1:1, 1:2, 1:5, and 0:1, where <i>m</i> <sub>f</sub> is the mass of feldspathic sandstone and <i>m</i> <sub>s</sub> is the mass of aeolian sand). The results showed that the soil texture was modified upon addition of feldspathic sandstone. The content of particles <0.05 mm increased with increasing addition ratio of feldspathic sandstone, in contrast to the downward trend observed for particles >0.05 mm. Consequently, the soil texture changed from sand to sandy loam, then loam, and finally silty loam. The addition of feldspathic sandstone ameliorated aeolian sand, resulting in a broader particle size distribution and lower particle size uniformity. Continuously well-graded soil was obtained at <i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:5 (coefficient of uniformity: 54.71; coefficient of curvature: 2.54) or 1:2 (coefficient of uniformity: 76.21; coefficient of curvature: 1.12). While the addition of feldspathic sandstone solved the problem of single particle size distribution in aeolian sand, the presence of aeolian sand prevented soil compaction caused by the high clay content of feldspathic sandstone. Findings of this study indicate that the addition of feldspathic sandstone to aeolian sand leads to the mixing of various sized particles and continuous gradation of the soil. Although a higher addition ratio of feldspathic sandstone is more favorable for soil texture improvement, <i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:5 is recommended for practical application in terms of particle gradation and cost effectiveness.

Authors

Institutions

Publication Details

Journal
PeerJ
Published
2024-11-25
DOI
https://doi.org/10.7717/peerj.18577
Citations
2
Primary Topic
Aeolian processes and effects
Type
article
Field-Weighted Citation Impact
1.03

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Feldspathic sandstone as an emerging soil stabilizer for aeolian sand in the Mu Us Sandy Land: insights into particle size distribution

Shenglan Ye, Lu Zhang, Juan Li, Jichang Han et al.
2 citations
PeerJ
Aeolian processes and effects
1.03
article

Feldspathic sandstone as an emerging soil stabilizer for aeolian sand in the Mu Us Sandy Land: insights into particle size distribution

Shenglan Ye, Lu Zhang, Juan Li, Jichang Han, Dan Wu
article en
2 citations

Abstract

Stabilization of aeolian sand is essential for achieving desertification control, soil and water conservation, and agricultural development in sandy lands. Feldspathic sandstone is a soft clay rock widely found in the Mu Us Sandy Land. The purpose of this study was to ascertain the mechanism for aeolian sand stabilization with feldspathic sandstone from the perspective of particle size distribution. Feldspathic sandstone was added to aeolian sand at different ratios (<i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:0, 1:1, 1:2, 1:5, and 0:1, where <i>m</i> <sub>f</sub> is the mass of feldspathic sandstone and <i>m</i> <sub>s</sub> is the mass of aeolian sand). The results showed that the soil texture was modified upon addition of feldspathic sandstone. The content of particles <0.05 mm increased with increasing addition ratio of feldspathic sandstone, in contrast to the downward trend observed for particles >0.05 mm. Consequently, the soil texture changed from sand to sandy loam, then loam, and finally silty loam. The addition of feldspathic sandstone ameliorated aeolian sand, resulting in a broader particle size distribution and lower particle size uniformity. Continuously well-graded soil was obtained at <i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:5 (coefficient of uniformity: 54.71; coefficient of curvature: 2.54) or 1:2 (coefficient of uniformity: 76.21; coefficient of curvature: 1.12). While the addition of feldspathic sandstone solved the problem of single particle size distribution in aeolian sand, the presence of aeolian sand prevented soil compaction caused by the high clay content of feldspathic sandstone. Findings of this study indicate that the addition of feldspathic sandstone to aeolian sand leads to the mixing of various sized particles and continuous gradation of the soil. Although a higher addition ratio of feldspathic sandstone is more favorable for soil texture improvement, <i>m</i> <sub>f</sub>:<i>m</i> <sub>s</sub> = 1:5 is recommended for practical application in terms of particle gradation and cost effectiveness.

PeerJVol. 12
Ministry of Natural Resources (CN), Land Consolidation and Rehabilitation Center (CN), Shaanxi Provincial Land Engineering Construction Group
Shaanxi Provincial Land Engineering Construction Group
Life in Land
Openalex Percentile: Top 24%
Aeolian processes and effects
1.03
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.