The responses of soil organic carbon mineralization and microbial communities to fresh and aged biochar soil amendments

被引:78
|
作者
Liu, Zhiwei [1 ,2 ]
Zhu, Mengtao [1 ,2 ]
Wang, Jiameng [1 ,2 ]
Liu, Xiuxia [1 ,2 ]
Guo, Wenjie [1 ,2 ]
Zheng, Jufeng [1 ,2 ]
Bian, Rongjun [1 ,2 ]
Wang, Genmei [3 ]
Zhang, Xuhui [1 ,2 ]
Cheng, Kun [1 ,2 ]
Liu, Xiaoyu [1 ,2 ]
Li, Lianqing [1 ,2 ]
Pan, Genxing [1 ,2 ]
机构
[1] Nanjing Agr Univ, Inst Resource Ecosyst & Environm Agr, Nanjing 210095, Jiangsu, Peoples R China
[2] Jiangsu Collaborat Innovat Ctr Solid Organ Waste, Nanjing, Jiangsu, Peoples R China
[3] Nanjing Forestry Univ, Coll Biol & Environm, Nanjing, Jiangsu, Peoples R China
来源
GLOBAL CHANGE BIOLOGY BIOENERGY | 2019年 / 11卷 / 12期
基金
中国国家自然科学基金;
关键词
dissolved organic matter; fresh; aged biochar; phospholipid fatty acid; SOC mineralization; soil microbial community composition; ACID RICE PADDY; TEMPERATURE SENSITIVITY; METABOLIC QUOTIENT; C-MINERALIZATION; DECOMPOSITION; MATTER; BIOMASS; BACTERIAL; SEQUESTRATION; RESPIRATION;
D O I
10.1111/gcbb.12644
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
While biochar soil amendment has been widely proposed as a soil organic carbon (SOC) sequestration strategy to mitigate detrimental climate changes in global agriculture, the SOC sequestration was still not clearly understood for the different effects of fresh and aged biochar on SOC mineralization. In the present study of a two-factorial experiment, topsoil samples from a rice paddy were laboratory-incubated with and without fresh or aged biochar pyrolyzed of wheat residue and with and without crop residue-derived dissolved organic matter (CRM) for monitoring soil organic matter decomposition under controlled conditions. The six treatments included soil with no biochar, with fresh biochar and with aged biochar treated with CRM, respectively. For fresh biochar treatment, the topsoil of a same rice paddy was amended with wheat biochar directly from a pyrolysis wheat straw, the soil with aged biochar was collected from the same soil 6 years following a single amendment of same biochar. Total CO2 emission from the soil was monitored over a 64 day time span of laboratory incubation, while microbial biomass carbon and phospholipid fatty acid (PLFA) were determined at the end of incubation period. Without CRM, total organic carbon mineralization was significantly decreased by 38.8% with aged biochar but increased by 28.9% with fresh biochar, compared to no biochar. With CRM, however, the significantly highest net carbon mineralization occurred in the soil without biochar compared to the biochar-amended soil. Compared to aged biochar, fresh biochar addition significantly increased the total PLFA concentration by 20.3%-33.8% and altered the microbial community structure by increasing 17:1 omega 8c (Gram-negative bacteria) and i17:0 (Gram-positive bacteria) mole percentages and by decreasing the ratio of fungi/bacteria. Furthermore, biochar amendment significantly lowered the metabolic quotient of SOC decomposition, thereby becoming greater with aged biochar than with fresh biochar. The finding here suggests that biochar amendment could improve carbon utilization efficiency by soil microbial community and SOC sequestration potential in paddy soil can be enhanced by the presence of biochar in soil over the long run.
引用
收藏
页码:1408 / 1420
页数:13
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