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作 者:房飞[1,2] 胡玉昆[1] 公延明[1,2] 杨秀娟[1,2] 柳妍妍[1]
机构地区:[1]中国科学院新疆生态与地理研究所干旱区生物地理与生物资源重点实验室,新疆乌鲁木齐830011 [2]中国科学院研究生院,北京100049
出 处:《中国沙漠》2013年第3期777-781,共5页Journal of Desert Research
基 金:国家重点基础研究发展计划项目(2009CB825103)资助
摘 要:以古尔班通古特沙漠南缘原始盐漠为研究对象,测定不同深度的土壤有机碳和土壤微生物碳含量,以分析它们之间的响应关系。结果表明:(1)在土壤垂直剖面上,土壤微生物碳(SMC)含量与有机碳(SOC)含量呈现极显著正线性相关(R2=0.63,p=0.0003)。(2)SMC出现了2个明显的改变界面(20cm,80cm),0~20、20~80、80~500cm值分别为:2.24~3.06、0.19~0.72、0.0017~0.0097mg.kg-1;0~20cm和20~80cm的SMC差异极显著(p<0.0001),20~80cm和80~500cm的SMC差异显著(p<0.05)。(3)对应于SMC的土壤层划分,SOC在0~20cm、20~80cm和80~500cm同样具有一定的分层性。(4)我们把具有不同微生物活性的有机碳层分别定义为活性、惰性、稳定性有机碳库,土壤垂直剖面上微生物碳的分布很好地表征了土壤中活性、惰性、稳定性有机碳库的分布;通过对这3种碳库所在土层进行合理划分,可以定量分析土壤中3种有机碳库的储量。The goal of the present research was to analyze the response relation of soil organic carbon (SOC) to soil microbial carbon (SMC) at different depths of original salt desert in the southern boundary of the Garbantunggut Desert. The results showed that: In the soil vertical profile, SMC and SOC presented a significant positive linear correlation (R2 =0. 63, p=0. 0003). SMC exhibited two obvious changed-interfaces, 20 cmand80 cm, theSMCat the depth of 0--20 cm, 20--80 cm and 80--500 cm was 2.24--3.06, 0.19-- 0.72, and 0. 0017--0. 0097 mg.kg-1, respectively; the SMC at 0--20 cm and 20--80 cm were significant different (p〈0. 0001), that at 20--80 cm and 80--500 cm were also significant different (p=0. 013). Corresponding to the soil division based on SMC, the SOC also had some certain stratification. We defined organic carbon layers with different microbial activity as active, inert, and stable organic carbon library. The soil microbial carbon in the vertical profile presented a good characterization of the distribution of the active, inert, and stable organic carbon library. Therefore, these three kinds of organic carbon library can be quantified by reasonable analyzing their locations at different depths of soil vertical profile.
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