Difference of Soil Aggregates Composition, Stability, and Organic Carbon Content between Eroded and Depositional Areas after Adding Exogenous Organic Materials
Open Access
- 14 February 2022
- journal article
- research article
- Published by MDPI AG in Sustainability
- Vol. 14 (4) , 2143
Abstract
Black soil in northeastern China has suffered widespread soil degradation due to long-term cultivation while causing eroded–depositional landscapes, leading to soil-associated carbon redistribution. In agricultural systems, adding exogenous organic material to degraded soil is a common measure to improve soil aggregate stability and soil quality. However, differences in soil properties may alter the decomposition and turnover of organic material in aggregates. Using a uniform method to restore the eroded (E) and depositional (D) soils is inefficient. Therefore, an indoor constant temperature and humidity incubation experiment with the addition of three organic materials, namely, straw (S), biochar (B), and swine manure (M), was designed with an equal amount of carbon. Soil aggregate composition, stability, and organic carbon from eroded and depositional soils were analyzed for evaluating the amendment efficiency of soil quality by exogenous organic material addition. The main results were as follows: adding straw and swine manure could effectively promote >2-mm aggregates formation (E: 7.1%, 8.8%; D: 17.3%, 8.6%) and significantly improved the mean weight diameter (MWD) (E: 0.45 mm, 0.52 mm; D: 0.96 mm, 0.54 mm), while the addition of biochar significantly increased the proportion of 0.25–2-mm aggregates (E: 7.9%; D: 10.9%), but the effect of improving MWD was less than straw and swine manure. All the three organic materials could significantly increase soil total organic carbon (TOC) (S, B and M: 1.95, 3.12 and 2.46 g·kg−1) in the eroded area, and the effect of biochar was the best, whereas it was not significant for the soil in the depositional area. Specially, adding swine manure and adding straw is more beneficial to the restoration of eroded areas and depositional areas, respectively.Keywords
Funding Information
- National Key R&D Program of China (2021YFD1500700 and 2021YFD1500600)
This publication has 32 references indexed in Scilit:
- Positive and negative carbon mineralization priming effects among a variety of biochar-amended soilsSoil Biology and Biochemistry, 2011
- Turnover of soil organic matter and of microbial biomass under C3–C4 vegetation change: Consideration of 13C fractionation and preferential substrate utilizationSoil Biology and Biochemistry, 2011
- The impact of agricultural soil erosion on biogeochemical cyclingNature Geoscience, 2010
- Soil aggregation and distribution of carbon and nitrogen in different fractions under long-term application of compost in rice–wheat systemSoil and Tillage Research, 2009
- The Impact of Agricultural Soil Erosion on the Global Carbon CycleScience, 2007
- Quantifying water‐stable soil aggregate turnover and its implication for soil organic matter dynamics in a model studyEuropean Journal of Soil Science, 2005
- Soil erosion and the global carbon budgetEnvironment International, 2003
- Soil macroaggregate turnover and microaggregate formation: a mechanism for C sequestration under no-tillage agricultureSoil Biology and Biochemistry, 2000
- Total carbon and nitrogen in the soils of the worldEuropean Journal of Soil Science, 1996
- Carbon and Nitrogen Distribution in Aggregates from Cultivated and Native Grassland SoilsSoil Science Society of America Journal, 1993