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茶园土壤团聚体分布特征及其对有机碳含量影响的研究 被引量:35

Distribution Characteristics of Soil Aggregates and Organic Carbon in Tea Plantation
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摘要 通过野外调查与室内分析相结合的方法,对茶园土壤团聚体的分布及其有机碳的含量及分布进行了研究。结果表明:茶园0-20 cm,20-40 cm土层土壤团聚体的分布均以〉2.00 mm和2-5 mm团聚体为主,分别占总团聚体的比例为56.57%和69.53%。茶园土壤团聚体平均重量直径平均值为1.02 mm,并且随着土壤层次的增加有增加的趋势。茶园0-20 cm土层0.25-0.5 mm粒径土壤团聚体有机碳含量最高,20-40 cm土层〈0.25 mm粒径土壤团聚体有机碳含量最高,而2-5 mm粒径土壤团聚体有机碳含量在0-20 cm和20-40 cm土层均最低。茶园0-20 cm土层,各粒径团聚体中的有机碳分配比例均高于20-40 cm土层土壤。 Distribution of soil aggregates and organic carbon were analyzed in tea plantation through the methods of field investigation and laboratory analysis.The result indicated that the soil granule structure of tea plantation was dominated by 〉5 mm aggregate for all the two soil layers,accounting for 56.57% and 69.53% of all soil aggregate respectively.Mean weight diameter of soil aggregate in tea plantation was 1.02 mm,which tended to increase with descending soil layers.Tea plantation soil aggregate ratio of organic carbon in 0.25-0.5 mm aggregate in 0-20 cm and〈 0.25 mm aggregate in 20-40 cm were the highest and soil aggregate ratio of organic carbon in 2-5 mm were the lowest for all the two soil layers.Tea plantation soil aggregate size of the distribution of the ratio of organic carbon 0-20 cm were higher than 20-40 cm soil layer.
出处 《水土保持学报》 CSCD 北大核心 2009年第5期187-190,199,共5页 Journal of Soil and Water Conservation
基金 四川省教育厅重点项目(2006A008 07ZA059) 四川省教育厅基金项目(2006B009 07ZB063) 四川省科技厅应用基础项目(2008JY0022) 中国科学院山地灾害与地表过程重点实验室开放研究基金
关键词 茶园 土壤团聚体 有机碳 tea plantation soil aggreagte organic carbon
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  • 1Eltiott E T, Cambardella C A. Physical separation of soil organic matter[J]. Agriculture, Ecosystems and Environment, 1991, 34:407-419.
  • 2Puget P, Chenu C, Balesdent J. Dynamic of organic matter associated with particle-size fractions of water-stable aggregate[J]. European Journal of Soil Science, 2000,51 : 595-605.
  • 3Jastrow J D, Boutton T W, Miller R M. Carbon dynamics of aggregate-associated organic matter estimated by 13C natural abundance[J]. Sci. Soc. Am. J. , 1996,60 : 801-807.
  • 4Beare M, Cabrea H M L, Hendfix P F, et al. Aggregate-protected and unprotected organic matter pools in conventional tillage and no-tillage soils[J]. Soil Sci. Soc. Am. , 1994,58 : 787-795.
  • 5Gregorich E G, Ellert B H, Monreal C M. Turnover of soil matter and storage of CO2 residue carbon estimated frorm natural 13C abundance[J]. Can. Soil Sci. , 1995,75 : 151-167.
  • 6Barrios E. Light fraction soil organic matter and available nitrogen following trees and maize[J]. Soil Sci. Soc. Am. , 1997, 61:826-831.
  • 7Christensen B T. Carbon in primary and secondary organ mineral complexes[M]//Cater M R, Stewart A B. Structure and organic matter storage in agricultural soils. Boca Raton, Florida: CRC Press,Inc. 1996.
  • 8王清奎,汪思龙.土壤团聚体形成与稳定机制及影响因素[J].土壤通报,2005,36(3):415-421. 被引量:342
  • 9杨建国,安韶山,郑粉莉.宁南山区植被自然恢复中土壤团聚体特征及其与土壤性质关系[J].水土保持学报,2006,20(1):72-75. 被引量:43
  • 10赵世伟,苏静,吴金水,杨永辉,刘娜娜.子午岭植被恢复过程中土壤团聚体有机碳含量的变化[J].水土保持学报,2006,20(3):114-117. 被引量:64

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