In this work, K Torri has an extremely significant negative correlation with soil organic carbon (matter) content, which partially confirms the previous research conclusions.
← all excerpts
Characteristics of Soil Erodibility in the Yinna Mountainous Area, Eastern Guangdong Province, China.
3
—
—
The sentences
The content of organic carbon in the topsoil layer was significantly higher than that in the subsoil layer ( p < 0.05), and neither of them showed a significant trend of change with altitude.
The soil particle size composition on the profile showed a trend of gradual increase in the content of fine particles (silt and clay) and a gradual decrease in the content of sand particles with the increase of depth ( Figure 4 ), which was related to strong weathering and leaching in the subtropical region.