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Volume 30 Issue 2
Jun.  2011
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LAN Jia-cheng, FU Wa-li, YUAN Bo, PENG Jing-tao, ZHANG Ting, FU Yun. Impact of land use type on soil active organic carbon and its distribution in karst mountain[J]. CARSOLOGICA SINICA, 2011, 30(2): 175-180. doi: 10.3969/j.issn.1001-4810.2011.02.009
Citation: LAN Jia-cheng, FU Wa-li, YUAN Bo, PENG Jing-tao, ZHANG Ting, FU Yun. Impact of land use type on soil active organic carbon and its distribution in karst mountain[J]. CARSOLOGICA SINICA, 2011, 30(2): 175-180. doi: 10.3969/j.issn.1001-4810.2011.02.009

Impact of land use type on soil active organic carbon and its distribution in karst mountain

doi: 10.3969/j.issn.1001-4810.2011.02.009
  • Received Date: 2011-01-17
  • Publish Date: 2011-06-25
  • Soil active organic carbon and its distribution in the soils (0~50cm) under different land use type are studied in Zhong Liang knoll, Chongqing. The results reveal that: 1)the contents of the soil organic carbon (SOC) under different land use types are bamboo land >vegetable land >grassland>woodland >garden >abandoned farmland, and the contents of SOC in the layer between 20 to 50cm deep is more than that between 0 to 20cm; 2) the average contents of soil dissolved organic carbon(DOC) are woodland >bamboo land >abandoned farmland >grassland >garden >vegetable land; 3) the percentage of soil dissolved organic carbon to the total soil organic carbon increased with depth; 4) the easily oxidized organic carbon(EOC) content and its distribution on the profile is consistent with the changes of soil organic carbon content. Correlation analysis shows that the correlation between easily oxidized organic carbon and soil organic carbon gets very significant level (R=0.852,P<0.0001), proving that the EOC is susceptible to the change of SOC.

     

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  • [1]
    沈宏,曹志洪,胡正义.土壤活性有机碳的表征及其生态效应[J].生态学杂志,1999,18(3):32-38.
    [2]
    Coleman D C, Reid C P P, Cole C V. Biological strategies of nutrient cycling in soil systems[J].Advances in Ecological Research,1983,13:1-55.
    [3]
    Wander M M, Traina S J, Stinner B R, et al. Organic and conventional management effects on biologically active soil organic matter pools [J]. Soil Science Society of America Journal, 1994, 58: 1130-1139.
    [4]
    Post W M, Kwon K C. Soil carbon sequestration and land use change: processes and potential [J]. Global Change Biology,2000,6:317-327.
    [5]
    Chantigny M H. Dissolved and water-extractable organic matter in soils: a review on the influence of land use and management practices [J]. Geoderma, 2003, 113: 357 -380.
    [6]
    曹建华,潘根兴,袁道先,等.岩溶地区土壤溶解有机碳的季节动态及环境效应[J].生态环境,2005,14(2):224-229.
    [7]
    莫彬,曹建华,徐祥明,等.岩溶山区不同土地利用方式对土壤活性有机碳动态的影响[J].生态环境,2006,15(6):1224-1230.
    [8]
    庞冬辉,李先琨,何成新,等.桂西峰丛岩溶区的环境特点及农业生态系统优化设计[J].广西植物,2003,25(5):24-29.
    [9]
    覃家科,李先混,姜光辉,等.木美地下河流域主要植被类型物种多样性与恢复对策[J].广西植物,2005,25(6):19-24.
    [10]
    段正锋,傅瓦利,甄晓君,等.岩溶区土地利用方式对土壤有机碳组分及其分布特征的影响[J].水土保持学报,2009,23(2):109-114.
    [11]
    Houghton R A. Woodwell G M. Global elimate change [J]. American Journul of Science, 1989, 260: 18-26.
    [12]
    袁道先.碳循环与全球岩溶[J].第四纪研究,1993,(1):1-6.
    [13]
    Yuan DaoXian. The carbon cycle in karst [J].Annual of Geomorphology, 1997, 108: 91-102.
    [14]
    鲁如坤.土壤农业化学析[M].北京:中国农业科技出版社,2000.
    [15]
    Blair G J, Lefroy R D B, Lisle L. Soil carbon fractions based on their degree of oxidation and the development of a carbon management index for agricultural system[J].Australian Journal Agriculture Research,1995,46:1456-1466.
    [16]
    任天志,StefanoG.持续农业中的土壤生物指标[J].中国农业科学,2000,33(1):68-75.
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