Impact of wetting-drying cycles and acidic conditions on the soil aggregate stability of yellow-brown soil

• Published in: Journal of mountain science Vol. 21; no. 6; pp. 2075 - 2090
• Main Authors: Xia, Zhenyao, Ni, Yuanzhen, Liu, Deyu, Wang, Di, Xiao, Hai
• Format: Journal Article
• Language: English
• Published: Heidelberg Science Press 2024; Springer Nature B.V
• Subjects: Acid rain; Acidic soils; Acidity; Aggregates; Brown soils; Bulk density; Calcium ions; Canyons; Correlation analysis; Disintegration; Drying; Earth and Environmental Science; Earth Sciences; Ecological function; Ecology; Environment; Environmental factors; Geography; Magnesium; Original Article; Particle size distribution; Regression analysis; Size distribution; Soil; Soil aggregates; Soil density; Soil stability; Stability; Terrestrial ecosystems; Wetting; Soil aggregate stability; Soil disintegration; yellow-brown soil; Wetting-drying cycles; Acidic conditions
• ISSN: 1672-6316; 1993-0321; 1008-2786
• DOI: 10.1007/s11629-023-8264-6

Soil aggregate is the basic structural unit of soil, which is the foundation for supporting ecosystem functions, while its composition and stability is significantly affected by the external environment. This study was conducted to explore the effect of external environment (wetting-drying cycles and acidic conditions) on the soil aggregate distribution and stability and identify the key soil physicochemical factors that affect the soil aggregate stability. The yellow-brow soil from the Three Gorges Reservoir area (TGRA) was used, and 8 wetting-drying conditions (0, 1, 2, 3, 4, 5, 10 and 15 cycles) were simulated under 4 acidic conditions (pH = 3, 4, 5 and 7). The particle size distribution and soil aggregate stability were determined by wet sieving method, the contribution of environmental factors (acid condition, wetting-drying cycle and their combined action) to the soil aggregate stability was clarified and the key soil physicochemical factors that affect the soil aggregate stability under wetting-drying cycles and acidic conditions were determined by using the Pearson’s correlation analysis, Partial least squares path modeling (PLS–PM) and multiple linear regression analysis. The results indicate that wetting-drying cycles and acidic conditions have significant effects on the stability of soil aggregates, the soil aggregate stability gradually decreases with increasing number of wetting-drying cycles and it obviously decreases with the increase of acidity. Moreover, the combination of wetting-drying cycles and acidic conditions aggravate the reduction in the soil aggregate stability. The wetting-drying cycles, acidic conditions and their combined effect imposes significant impact on the soil aggregate stability, and the wetting-drying cycles exert the greatest influence. The soil aggregate stability is significantly correlated with the pH, Ca 2+ , Mg 2+ , maximum disintegration index (MDI) and soil bulk density (SBD). The PLS–PM and multiple linear regression analysis further reveal that the soil aggregate stability is primarily influenced by SBD, Ca 2+ , and MDI. These results offer a scientific basis for understanding the soil aggregate breakdown mechanism and are helpful for clarifying the coupled effect of wetting-drying cycles and acid rain on terrestrial ecosystems in the TGRA.