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土壤中^(14)C-葡萄糖的周转及其与土壤特性的关系 被引量:1

TURNOVER OF ^(14)C-GLUCOSE IN SOILS AND ITS RELATIONSHIP WITH SOIL CHARACTERS
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摘要 研究了1 4 C 葡萄糖在 1 3种土壤中的周转。周转可以分为 3个阶段 :0~ 3d ,周转速率为 1 3× 1 0 - 1 ~ 2 5× 1 0 - 1 /d ,半周转期为 3~ 5d;3~ 2 8d,周转速率为 0 7×1 0 - 2 ~ 1 2× 1 0 - 2 /d ,半周转期为 5 8~ 97d ;2 8~ 2 94d,周转速率为 0 5× 1 0 - 3× 1 4×1 0 - 3/d ,半周转期为 491~ 1 5 0 4d。相关性分析表明 ,1 4 C 葡萄糖周转速率与土壤代谢熵 (qCO2 )呈显著性正相关 ;3~ 2 8d周转速率与土壤理化性质和生物学性质都无显著的相关性 ;2 8~ 2 94d周转速率与土壤总有机碳、全氮、CEC呈显著或极显著负相关 ,与土壤砂粒含量呈显著正相关。这一阶段1 4 C 葡萄糖的周转与土壤性质密切相关。 The turnover of 14 C\|glucose added in 13 soils was studied.The turnover rate of 14 C\|glucose can be divided into three phases:0~3d,3~28d and 28~294d.The range of the turnover rate and half\|life of 14 C\|glucose were 1\^3×10 -1 ~2\^5×10 -1 d -1 and 3~5d,0\^7×10 -2 ~1\^2×10 -2 d -1 and 58~97d, 0\^5×10 -3 ~1 4×10 -3 d -1 and 491~1504d,respectively.Correlation analysis showed that from 0 to 3days the turnover rate of 14 C\|glucose had significant positive correlation with soil qCO\-2,from 3 to 28days,the turnover rate of 14 C\|glucose had no significant correlation with soil physico\|chemical and biological properties.The turnover rate of 14 C\|glucose had significant or highly significant negative correlation with soil total organic carbon,tatal nitrogen,CEC and significant positive correlation with soil sand content during the period from 28 to 294days.Turnover of 14 C\|glucose during the third period has close correlation with soil properties.
出处 《核农学报》 CAS CSCD 北大核心 2001年第1期57-64,共8页 Journal of Nuclear Agricultural Sciences
基金 教育部出国留学人员回国基金 国家重点基础研究发展规划项目课题! (批准号 :G19990 1180 9)资助 浙江省自然科学基金! (RC990 32
关键词 葡萄糖 周转速率 土壤生物学特征 土壤理化性质 碳14标记 ^(14)C-glucose turnover rate soil properties
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参考文献6

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共引文献28

同被引文献37

  • 1吴建国,艾丽,朱高,田自强,苌伟.祁连山北坡云杉林和草甸土壤有机碳矿化及其影响因素[J].草地学报,2007,15(1):20-28. 被引量:32
  • 2孙波,车玉萍,林心雄.测定土壤有机物质中^(12)C及^(14)C分解速率的密闭培养法[J].土壤,1997,29(1):51-53. 被引量:20
  • 3尹云锋,蔡祖聪.利用δ^(13)C方法研究添加玉米秸秆下红壤总有机碳和重组有机碳的分解速率[J].土壤学报,2007,44(6):1022-1027. 被引量:26
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  • 7Urbanek E, Smucker A J M, Horn R. Total and fresh organic carbon distribution in aggregate size classes and single ag- gregate regions using natural J3C/J2C tracer [ J]. Geoderma, 2011, 164 : 164 - 171.
  • 8Tan Z, Lal R, Owens L, et al. Distribution of light and heavy fractions of soil organic carbon as related to land use and tillage practice [J]. Soil Tillage Research, 2007, 92:53 -59.
  • 9Mikha M M, Rice C W, Milliken G A. Carbon and nitrogen mineralization as affected by drying and wetting cycles [ J ]. Soil Biology and Biochemistry, 2005, 37:339 -347.
  • 10Ahmad W, Singh B, Dijkstra F A, et al. Temperature sensitivity and carbon release in an acidic soil amended with lime and mulch. [J]. Geoderma, 2014, 214/215: 168-176.

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