Related Experiment Video
Updated: Sep 10, 2025

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions
Published on: February 15, 2019
Organic materials input promotes the soil aggregate sequestration through changing soil aggregates structure and
Wenting Jiang1, Tingting Li2, Jifu Ma2
1Research and Development Centre of Ecological and Sustainable Application of Microbial Industry of the Loess Plateau in Shaanxi Province, Yan'an University, Yan'an, 716000, Shaanxi, China; State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; Key Laboratory of Applied Ecology of Loess Plateau, Shaanxi Province, Yan'an University, Yan'an, 716000, Shaanxi, China.
Abstract:
The strategic application of organic amendments presents a transformative approach for enhancing agroecosystem sustainability by modulating soil hydrostructural dynamics and carbon sequestration. However, changes in soil moisture, nutrients, aggregate stability, and SOC sequestration under different organic materials type input in farmland of arid northwest China remain uncertain. In this study, an experiment with five treatments (CK: control, LB: smashed leaves and branches, CS: smashed corn stalks, HV: green fertilizer, MS: waste mushroom bran) input applied into the soil. The results indicated that organic materials input management significantly optimizes soil moisture content (SMC), soil water storage (SWS), and water use efficiency (WUE) in both soil depths, and MS treatment elevated SWS by 6.7 %-16.2 % and WUE by 23.7 % relative to CK, while stabilizing moisture fluctuations across critical maize growth stages. The electrical conductivity, soil organic matter, total nitrogen, available phosphorus, available potassium, Fe, Cu and Zn contents differed significantly under organic materials input. Organic materials input enhanced soil carbon sequestration by optimizing aggregate hierarchy, and mean weight diameter (MWD), geometric mean diameter (GMD), while MS reduced soil erodibility K factor by 12.9 %, and amplified aggregate-associated organic carbon stocks by 94.4 % at the 0-20 cm soil depth, outperforming other organic materials input treatments. Soil organic carbon content exhibited strong particle-size dependency with decreasing from >2 mm to <0.25 mm aggregates, and >2 mm aggregates conten of 39.68 %-44.12 % to SOC. Random forest analysis identified microaggregate SOC and K factor as stability drivers. The SEM model showed that the organic materials input, aggregated associated SOC contents and stocks explained 97.1 % of the variation in aggregate-associated SOC stock. In conclusion, the application of waste mushroom bran input enhances the soil aggregate stability by altering soil aggregates structure and soil carbon sequestration, thereby establishing a scientific foundation for developing soil health regulation mechanisms and advancing sustainable agricultural practices.
Related Concept Videos
Deleterious Substances in Aggregate
Another type of impurity is clay and fine material that...
The Soil Ecosystem
Environmental Applications of Microorganisms
Unsoundness of Aggregate due to Volume Change
Porosity and Absorption of Aggregate
When all pores in an aggregate are filled with water, the aggregate is considered saturated and surface-dry. If left in dry air, water will evaporate until the...
Bioremediation

