4.7 Article

Increased Soil Aggregate Stability by Altering Contents and Chemical Composition of Organic Carbon Fractions via Seven Years of Manure Addition in Mollisols

Journal

AGRICULTURE-BASEL
Volume 13, Issue 1, Pages -

Publisher

MDPI
DOI: 10.3390/agriculture13010088

Keywords

molecular characterization; particulate organic matter; silt and clay fractions; Fourier transform infrared spectroscopy; aromatic components; physical protection

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Through experimental research on Mollisols, it was found that adding agricultural waste could enhance soil aggregate stability, and the dominating factor affecting its stabilization remains controversial. The study investigated the influences of different fertilization managements on the contents and molecular characterization of organic carbon (OC) fractions, and clarified the underlying mechanism of soil aggregate stability change. The addition of manure significantly increased SOC content and crop yield, and improved aggregate stability.
Mollisols include an abundance of soil organic carbon (SOC) which is easily influenced by fertilization management. Manure addition could enhance soil aggregate stability; however, the dominating factor affecting its stabilization remains controversial. The fertilization practices were initiated in 2012 to investigate the influences of different fertilization managements on the contents and molecular characterization of organic carbon (OC) fractions, and to clarify the underlying mechanism of soil aggregate stability change. NoF (non-fertilizer), CF (only chemical fertilizer), CF + DM (chemical fertilizer plus single dairy manure at 15 t ha(-1)), and CF + 2DM (chemical fertilizer plus double dairy manure at 30 t ha(-1)) treatments were established. This research was aimed at exploring the potential mechanism that affects aggregate stability in Mollisols through the variation of contents and chemical composition of OC fractions, and screening out the appropriate fertilization practice on promoting SOC stabilization and crop yield under 7-year manure addition. Compared to CF, 7-year manure addition significantly enhanced SOC content by 17.4-35.9% at 0-10 cm depth, which was evidenced from the contribution of increased aromatic compounds with 4.3-19.9%. Simultaneously, compared with CF, CF + DM and CF + 2DM both significantly enhanced dissolved organic carbon and easily oxidizable organic carbon contents by 12.5-37.7% at a 0-30 cm soil layer. In regard to soil aggregates, the increased OC content and mass percentage of macroaggregates, and the decreased mass percentage of free microaggregates both improved aggregate stability under manure addition at 0-30 cm soil layer, which was proven to be the increment in mean weight diameter (MWD) and geometric mean diameter (GMD) values by 17.6-22.1%. Moreover, CF + DM and CF + 2DM raised aromatic compound amounts of POM fractions within macroaggregates [M(c)POM] by 5.6-11.6% and within free microaggregates (Fm-POM) by 4.3-10%. Furthermore, CF + DM and CF + 2DM both significantly increased maize yield by 5.7% and 4.2% compared to CF, but no significant difference was observed between CF + DM and CF + 2DM treatments. Collectively, physical protection through the occlusion within aggregates of POM might be the central mechanism for soil aggregate stability of manure addition in Mollisols. The manure addition of 15 t ha(-1) was the effective management method to enhance SOC stabilization and crop yield in Mollisols.

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