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高CO_2浓度条件下农田土壤有机质的化学稳定性研究
引用本文:马红亮,朱建国,谢祖彬,刘钢,曾青.高CO_2浓度条件下农田土壤有机质的化学稳定性研究[J].农业环境科学学报,2007,26(6):2211-2215.
作者姓名:马红亮  朱建国  谢祖彬  刘钢  曾青
作者单位:1. 福建师范大学地理科学学院,福建省亚热带资源与环境重点实验室,福建,福州,350007
2. 中国科学院南京土壤研究所,土壤与农业可持续发展国家重点实验室,江苏,南京,210008
基金项目:中国科学院知识创新工程项目;国家自然科学基金;国家自然科学基金;重大国际合作项目;国家重点基础研究发展计划(973计划);福建省青年科技人才创新基金
摘    要:大气CO2浓度升高显著增加作物生物量,从而使进入土壤的有机碳增加,这势必会影响土壤碳的稳定和积累。采取利用化学方法获得的具有不同化学稳定性的有机物,间接地研究大气CO2浓度升高以后通过直接影响秸秆生物量和化学成分对土壤碳变化的影响。结果显示,相对于对照处理:高CO2浓度处理使土壤经Na2S2O8化学氧化后的抗氧化部分,在LN、NN和HN水平下,分别增加16.4%、21.7%和降低3.8%;使土壤经硫酸水解后的第一组分分别降低2.2%,增加9.5%和7.5%,第二组分分别增加4.7%、17.6%和降低4.9%,第三组分分别增加7.3%,降低4.2%和2.6%。表明土壤有机质的化学稳定性有所增加,可能与高CO2浓度条件下向土壤输入的有机质量及化学组成有关,且受N水平的影响较大。

关 键 词:高CO2浓度  秸秆  土壤碳  Na2S2O8氧化  H2SO4水解
文章编号:1672-2043(2007)06-2211-05
修稿时间:2006-11-21

Chemical Stability of Soil Organic Matter from Field Under Elevated CO2
MA Hong-liang,ZHU Jian-guo,XIE Zu-bin,LIU Gang,ZENG Qing.Chemical Stability of Soil Organic Matter from Field Under Elevated CO2[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2007,26(6):2211-2215.
Authors:MA Hong-liang  ZHU Jian-guo  XIE Zu-bin  LIU Gang  ZENG Qing
Institution:1. Fujian Provincial Key Laboratory of Subtropical Resources and Environment, College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; 2. State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
Abstract:Elevated atmospheric CO2 concentration significantly increase crops biomass, which will input more carbon into soil to affect soil carbon stability and accumulation. Chemical techniques were used to obtain organic matter fractions with different chemical stabilities, in order to investigate the indirect influence of elevated CO2 on soil carbon based on the change of crops biomass and chemical characteristics. Compared to ambient CO2, at LN, NN and HN level, elevated CO2 increased the parts that could not be removed by Na2S2O8 (SOC) by 16.4%, 21.7% and decreased it by 3.8% after treated by Na2S2O8, respectively. After soil treated with H2SO4 hydrolysis, labile pool I was decreased by 2.2%, increased by 9.5% and 7.5%, labile pool II increased by 4.7%, 17.6% and decreased by 4.9%, and recalcitrant pool increased by 7.3%, decreased by 4.2% and 2.6% due to elevated CO2 at LN, NN and HN level, respectively. These results indicated that the chemical stability of soil organic matter increased, partly due to the change of biomass and chemical characteristics of straw added in soil and N level.
Keywords:elevated atmospheric CO_2  straw  soil carbon  Na_2S_2O_8 oxidation  H_2SO_4 hydrolysis
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