Investigating the biochar effects on C-mineralization and sequestration of carbon in soil compared with conventional amendments using the stable isotope (delta C-13) approach
Abbas, Qumber3; Liu, Ruijia3; Imtiaz, Muhammad1; Wang, Ruwei3; Liu, Guijian2,3; Yousaf, Balal2,3
刊名GLOBAL CHANGE BIOLOGY BIOENERGY
2017-06-01
卷号9期号:6页码:1085-1099
关键词Biochar Biowaste Carbon Mineralization Carbon Stable Isotope C-sequestration Priming Effects
DOI10.1111/gcbb.12401
文献子类Article
英文摘要Biomass-derived black carbon (biochar) is considered to be an effective tool to mitigate global warming by long-term C-sequestration in soil and to influence C-mineralization via priming effects. However, the underlying mechanism of biochar (BC) priming relative to conventional biowaste (BW) amendments remains uncertain. Here, we used a stable carbon isotope (delta C-13) approach to estimate the possible biochar effects on native soil C-mineralization compared with various BW additions and potential carbon sequestration. The results show that immediately after application, BC suppresses and then increases C-mineralization, causing a loss of 0.14-7.17 mg-CO2-C g(-1)-C compared to the control (0.24-1.86 mg-CO2-C g(-1)-C) over 1-120 days. Negative priming was observed for BC compared to various BW amendments (-10.22 to -23.56 mg-CO2-C g(-1)-soil-C); however, it was trivially positive relative to that of the control (8.64 mg-CO2-C g(-1)-soil-C). Furthermore, according to the residual carbon and delta C-13 signature of postexperimental soil carbon, BC-C significantly increased (P < 0.05) the soil carbon stock by carbon sequestration in soil compared with various biowaste amendments. The results of cumulative CO2-C emissions, relative priming effects, and carbon storage indicate that BC reduces C-mineralization, resulting in greater C-sequestration compared with other BW amendments, and the magnitude of this effect initially increases and then decreases and stabilizes over time, possibly due to the presence of recalcitrant-C (4.92 mg-C g(-1)-soil) in BC, the reduced microbial activity, and the sorption of labile organic carbon (OC) onto BC particles.
WOS关键词SEA-LEVEL RISE ; DISSOLVED ORGANIC-CARBON ; SHORT-TERM ; PYROLYSIS TEMPERATURE ; MICROBIAL BIOMASS ; ATMOSPHERIC CO2 ; MATTER ; EMISSIONS ; POOLS ; WORLD
WOS研究方向Agriculture ; Biotechnology & Applied Microbiology ; Energy & Fuels
语种英语
WOS记录号WOS:000402743500007
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/5461]  
专题地球环境研究所_黄土与第四纪地质国家重点实验室(2010~)
作者单位1.Huazhong Agr Univ, Microelement Res Ctr, Coll Resources & Environm, Wuhan 430070, Peoples R China
2.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710075, Shaanxi, Peoples R China
3.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China
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Abbas, Qumber,Liu, Ruijia,Imtiaz, Muhammad,et al. Investigating the biochar effects on C-mineralization and sequestration of carbon in soil compared with conventional amendments using the stable isotope (delta C-13) approach[J]. GLOBAL CHANGE BIOLOGY BIOENERGY,2017,9(6):1085-1099.
APA Abbas, Qumber,Liu, Ruijia,Imtiaz, Muhammad,Wang, Ruwei,Liu, Guijian,&Yousaf, Balal.(2017).Investigating the biochar effects on C-mineralization and sequestration of carbon in soil compared with conventional amendments using the stable isotope (delta C-13) approach.GLOBAL CHANGE BIOLOGY BIOENERGY,9(6),1085-1099.
MLA Abbas, Qumber,et al."Investigating the biochar effects on C-mineralization and sequestration of carbon in soil compared with conventional amendments using the stable isotope (delta C-13) approach".GLOBAL CHANGE BIOLOGY BIOENERGY 9.6(2017):1085-1099.
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