EGU25-7553, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-7553
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 02 May, 09:50–10:00 (CEST)
 
Room 0.51
Quantifying the contributions of factors influencing the spatial heterogeneity of soil aggregate stability and erodibility in a Mollisol watershed
Lixin Wang
Lixin Wang
  • University of Chinese Academy of Sciences, The Research Center of Soil and Water Conservation and Ecological Environment,Chinese Academy of Sciences and Ministry of Education, China (wanglixin243@mails.ucas.ac.cn)

Soil aggregate stability and erodibility reflect soil resistance to erosion. Although the factors influencing soil aggregate stability and erodibility have been extensively studied, the driving effects of these factors and their interactions remain limited. 184 sampling sites were selected in topsoil (0-20 cm) of a small watershed (1.42 km2) in a Mollisol watershed to measure soil bulk density (BD), soil porosity (SP), soil moisture content (MC), soil organic carbon (SOC), total nitrogen (TN), >0.25 mm water stable aggregates content (WSA> 0.25), mean weight diameter (MWD) and K factor. Pearson correlation analysis, semi-variance function, redundancy analysis (RDA), and structural equation model (SEM) were used to quantify the impact of environmental variables (individual and interaction) on the spatial variations of WSA> 0.25, MWD, and K factor. The findings indicated that higher values of WSA> 0.25 and MWD are observed in the central and western watershed, while the K values tend to be lower in areas with high WSA> 0.25 and MWD values within the watershed. The Exponential model optimally described WSA> 0.25, MWD, and K factor with C0/(C + C0) indicating moderate spatial dependence for MWD (39.79%) and K factor (42.86%), while strong spatial autocorrelation for WSA> 0.25 (7.23%). Soil properties (moisture content, silt content, and bulk density), topography (elevation, SPI, and slope), and land use contributed 46.6%, 41.4%, and 9.1% of the spatial variation in WSA> 0.25, MWD, and K factor, respectively. SEM revealed that silt content, SOC, and water condition played a fundamental role in controlling the spatial variability of WSA> 0.25, MWD, and K factor. Topography exerted both direct or indirect effects by coupling land use or soil properties spatially. Land use had direct or indirect effects on WSA> 0.25 and K factor through regulating MC, but it primarily influences MWD indirectly through impacting MC. These results could clarify the roles and influencing paths of factors controlling the spatial heterogeneity of WSA> 0.25, MWD, and K factor, contributing to optimizing land management strategies.

How to cite: Wang, L.: Quantifying the contributions of factors influencing the spatial heterogeneity of soil aggregate stability and erodibility in a Mollisol watershed, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-7553, https://doi.org/10.5194/egusphere-egu25-7553, 2025.