Biochar application on paddy and purple soils in southern China: soil carbon and biotic activity

Soil carbon reserves are the largest terrestrial carbon pools. Common agricultural practices, such as high fertilization rates and intensive crop rotation, have led to global-scale environmental changes, including decreased soil organic matter, lower carbon/nitrogen ratios and disruption of soil car...

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Published inRoyal Society open science Vol. 6; no. 7; p. 181499
Main Authors Yan, Shen, Niu, Zhengyang, Zhang, Aigai, Yan, Haitao, Zhang, He, He, Kuanxin, Xiao, Xianyi, Wang, Nianlei, Guan, Chengwei, Liu, Guoshun
Format Journal Article
LanguageEnglish
Published England The Royal Society 01.07.2019
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Summary:Soil carbon reserves are the largest terrestrial carbon pools. Common agricultural practices, such as high fertilization rates and intensive crop rotation, have led to global-scale environmental changes, including decreased soil organic matter, lower carbon/nitrogen ratios and disruption of soil carbon pools. These changes have resulted in a decrease in soil microbial activity, severe reduction in soil fertility and transformation of soil nutrients, thereby causing soil nutrient imbalance, which seriously affects crop production. In this study, 16S rDNA-based analysis and static chamber-gas chromatography were used to elucidate the effects of continuous application of straw biochar on soil carbon pools and the soil microbial environments of two typical soil types (purple and paddy soils) in southern China. Application of biochar (1) improved the soil carbon pool and its activity, (2) significantly promoted the release of soil CO and (3) improved the soil carbon environment. Soil carbon content was closely correlated with the abundance of organisms belonging to two orders, Lactobacillales and Bacteroidales, and, more specifically, to the genus . These results suggest that biochar affects the soil carbon environment and soil microorganism abundance, which in turn may improve the soil carbon pool.
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Electronic supplementary material is available online at https://dx.doi.org/10.6084/m9.figshare.c.4545914.
ISSN:2054-5703
2054-5703
DOI:10.1098/rsos.181499