Mineral-Brown Carbonate Soils Of Western Tian Shan, Their Agrochemical Properties And Humus Condition

Research on mineral-brown carbonate soils in the Western Tien-Shan reveals that the ratio of humic acids (Cga) to fulvic acids (Cfa) correlates with soil susceptibility to erosion, influenced by slope exposure and relief. The study found that an increase in this ratio corresponds with higher optical density of humic acids, indicating varying resistance to coagulation among different soils. These differences also reflect varying degrees of susceptibility to erosion and anthropogenic factors, providing insights into the agrochemical properties and humus condition of these mountain soils. The analysis combines field observations and literature data to assess soil fertility and erosion dynamics in this ecologically significant region.

Raupova, N., & Abdullaev, S. (2018). Mineral-Brown Carbonate Soils Of Western Tian Shan, Their Agrochemical Properties And Humus Condition. Zenodo. https://doi.org/10.5281/ZENODO.1173148