文献类型： 外文期刊

作者： Deng, Shaohong ¹ ; Zheng, Xiaodong ¹ ; Chen, Xiangbi ¹ ; Zheng, Shengmeng ¹ ; He, Xunyang ¹ ; Ge, Tida ¹ ; Kuzyakov, Y ¹ ;

作者机构： 1.Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, Changsha 410125, Hunan, Peoples R China

2.Univ Chinese Acad Sci, Beijing 100039, Peoples R China

3.Guangdong Acad Agr Sci, Inst Agr Resource & Environm, Guangzhou 510640, Guangdong, Peoples R China

4.Chinese Acad Sci, Inst Subtrop Agr, Changsha Res Stn Agr & Environm Monitoring, Changsha 410125, Hunan, Peoples R China

5.Univ Gottingen, Dept Agr Soil Sci, Dept Soil Sci Temperate Ecosyst, D-37077 Gottingen, Germany

6.RUDN Univ, Agrotechnol Inst, Moscow 117198, Russia

7.Kazan Fed Univ, Inst Environm Sci, Kazan 420049, Russia

关键词： Hydrophilic and hydrophobic compounds; Priming effect; Bacterial and fungal biomarkers; Paddy and upland soils; Soil organic matter stabilization; Microbial utilization

期刊名称：BIOLOGY AND FERTILITY OF SOILS （ 影响因子：6.432； 五年影响因子：6.332 ）

ISSN： 0178-2762

年卷期：

页码：

收录情况： SCI

摘要： Hydrophilic and hydrophobic organic compounds extracted from(13)C-labelled maize residues were incubated with soils to evaluate their mineralization and priming effect (PE) caused by their utilization by microbial groups. Two soils with contrasting soil properties were collected from well-drained upland and water-logged paddy. Mineralization of the(13)C-labelled fractions and their PE were quantified by monitoring the CO(2)efflux and(13)C enrichment during a 40-day incubation. The composition of main microbial groups (bacteria and fungi) involved in the utilization of(13)C-labelled fractions was determined based on phospholipid fatty acids (PLFAs) analysis. At the initial stage (6-24 h), hydrophilic fraction had faster mineralization rate (3.6-70 times) and induced 1.5-10 times stronger PE (positive in upland soil and negative in paddy soil) than those of hydrophobic fraction. The(13)C-PLFAs data showed that the incorporation of hydrophilic fraction into bacteria was 11.4-16.4 times greater than that into fungi, whereas the hydrophobic fraction incorporated into fungi was 1.0-1.5 times larger than that into bacteria at day 2. This indicated greater contributions of r-strategists (fast-growing bacteria) for the uptake of hydrophilic fraction versus K-strategists (slow-growing fungi) for hydrophobic fraction. Compared with K-strategists, the r-strategists possessed a much faster metabolism and thus triggered stronger apparent PE by accelerating microbial biomass turnover, resulting in higher mineralization and stronger PE for the hydrophilic than hydrophobic fraction. The slower and less mineralization of both fractions in paddy than in upland soils is due to the suppression of microbial activity and substrate utilization under flooding. At the end of 40-day incubation, the cumulative mineralization of hydrophilic and hydrophobic fractions was similar. Consequnently, microbial mechanisms underlying the utilization of organic compounds with contrasting solubility (hydrophilic or hydrophobic) are crucial for evaluating the stabilization and destabilization (e.g., priming) processes of soil organic matter.