Organic fertilizer prepared by thermophilic aerobic fermentation technology enhanced soil humus and related soil enzyme activities

Author:

Xu Hongli12,Wang Shuqiang13,Jiang Nan145,Xie Hongtu145,Chen Zhenhua145,Zhang Yulan145ORCID,Li Shouzhong2

Affiliation:

1. Institute of Applied Ecology, Chinese Academy of Sciences Shenyang China

2. School of Geographical Sciences Fujian Normal University Fuzhou China

3. University of Chinese Academy of Sciences Beijing China

4. Key Laboratory of Conservation Tillage and Ecological Agriculture, Liaoning Province Shenyang China

5. National Field Observation and Research Station of Shenyang Agro‐Ecosystems Shenyang China

Abstract

AbstractOrganic fertilizer (OF) prepared from chicken manure in a high‐temperature aerobic fermenter contains high levels of nitrogen, phosphorus and potassium. The effect of high‐nutrient OF substitution for chemical fertilizer (CF) on soil organic carbon stability is worth exploring. We used OF to replace CFs for supplying crops, and we set five OF replacement rates as 0, 25%, 50%, 75% and 100% in the black soil zone of Northeast China. We explored the variations in soil humus carbon contents, enzyme activities and nutrient contents (0–10 cm and 10–20 cm). Two‐way ANOVA results showed that interaction between soil depth and OF substitution significantly affected soil pH, total nitrogen, organic carbon, available potassium, water‐soluble carbon substance (WSSC) and activities of soil β‐galactosidase (β‐gal), N‐acetyl‐β‐D‐glucosaminidase (NAG) and cellobiohydrolase. The treatments of OF75 and OF100 increased soil pH, and the content of soil organic carbon, humic acid carbon (HAC), fulvic acid carbon (FAC), WSSC, total phosphorus, available phosphorus (AP), total potassium and available potassium was increased in OF75 and OF100 treatment. Treatments of OF75 and OF100 increased the tested soil enzyme activities except for oxidase activities of 0–10 cm soil layer. There was a positive correlation between HAC and AP contents, and a positive correlation between FAC and soil pH, total nitrogen and available potassium contents. The key influencing factors of soil FAC were the activities of NAG, α‐galactosidase and β‐gal. It can be concluded that OF substitution promoted soil humus carbon accumulation by affecting hydrolase activity related to carbon conversion.

Publisher

Wiley

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