Stable oxic-anoxic transitional interface is beneficial to retard soil carbon loss in drained peatland-Reference-Cited by-同舟云学术

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Stable oxic-anoxic transitional interface is beneficial to retard soil carbon loss in drained peatland

Published:2023-06 Issue: Volume:181 Page:109024
ISSN:0038-0717
Container-title:Soil Biology and Biochemistry
language:en
Short-container-title:Soil Biology and Biochemistry

Author:

Liu Liangfeng,Tian Jianqing^ORCID,Wang Hongjun,Xue Dan,Huang Xinya,Wu Ning,Wang Meng^ORCID,Xu Xingliang^ORCID,Peng Changhui^ORCID,Wang Yanfen,Chen Huai

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Soil Science,Microbiology

Reference88 articles.

1. Soil organic matter turnover in long-term field experiments as revealed by carbon-13 natural abundance;Balesdent;Soil Science Society of America Journal,1998

2. The effect of the addition of organic materials on the decomposition of an organic soil;Bingeman;Soil Science Society of America Journal,1953

3. Mechanisms of real and apparent priming effects and their dependence on soil microbial biomass and community structure: critical review;Blagodatskaya;Biology and Fertility of Soils,2008

4. The MIQE guidelines: minimum information for publication of quantitative real-time PCR experiments;Bustin;Clinical Chemistry,2009

5. QIIME allows analysis of highthroughput community sequencing data;Caporaso;Nature Methods,2010

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