| 川西亚高山云杉人工林恢复过程中表层土壤碳动态变化 |
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| 引用本文： | 姜发艳,孙辉,林波,刘庆.川西亚高山云杉人工林恢复过程中表层土壤碳动态变化[J].应用生态学报,2009,20(11):2581-2587. |
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| 作者姓名： | 姜发艳 孙辉 林波 刘庆 |
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| 作者单位： | 1.四川大学环境科学与工程系,成都 610065;2.中国科学院成都生物研究所,成都 610041 |
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| 基金项目： | 国家自然科学基金重点项目,国家自然科学基金,中国科学院成都生物研究所知识创新工程领域前沿项目,西部之光人才计划项目,中国科学院知识创新工程西部行动计划项目 |
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| 摘 要： | 对川西亚高山云杉原始林及其皆伐迹地上云杉人工林不同演替阶段（22、47和65年）表层（0～30 cm）土壤碳储量及活性有机碳含量进行了分析.结果表明：在0～10、10～20和20～30 cm土层中，土壤总有机碳（TOC）储量分别由22年生云杉人工林的9587、7908和71.55 t·hm-2减少到65年生云杉人工林的56.12、34.75和31.06 t·hm-2，且47和65年生云杉人工林各层土壤TOC储量小于原始林（88.08、71.16和64.81 t·hm-2）；各层土壤易氧化有机碳（EOC）含量分别由原始林的3589、26.91和26.00 g·kg-1 减少到65年生云杉人工林的20.25、14.50和12.36 g·kg-1，土壤微生物生物量碳（MBC）含量由原始林的524.44、273.26和257.97 mg·kg-1减少到65年生云杉人工林的 312.41、186.95和152.18 mg·kg-1，颗粒态有机碳（POC）含量由原始林的40.23、27.10和19.55 g·kg-1减少到65年生云杉人工林的12.33、7.31和5.32 g·kg-1.川西亚高山云杉原始林在转变为人工林后相当长的时间内，土壤有机碳及活性碳一直处于净消耗状态.
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| 关 键 词： | 亚高山森林土壤 易氧化有机碳 微生物生物量碳 颗粒态有机碳 可燃物含水率 加拿大火险天气指标系统 塔河 凋落物 |
Dynamic changes of topsoil organic carbon in subalpine spruce plantation at different succession stages in western Sichuan Province |
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| JIANG Fa-yan,SUN Hui,LIN Bo,LIU Qing.Dynamic changes of topsoil organic carbon in subalpine spruce plantation at different succession stages in western Sichuan Province[J].Chinese Journal of Applied Ecology,2009,20(11):2581-2587. |
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| Authors: | JIANG Fa-yan SUN Hui LIN Bo LIU Qing |
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| Affiliation: | 1.Department of Environmental Science and Engineering, Sichuan University, Chengdu 610065, China|;2.Chengdu Institute of Biology, Chinese ademy of Sciences, Chengdu 610041, China |
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| Abstract: | Soil samples at 0-30 cm depth were collected from the primary spruce(Picea asperata)forest and its plantations at different succession stages(22-,47-,and 65-year-old)in subalpine zone of western Sichuan Province to study the dynamic changes of soil organic carbon stock and labile organic carbon content.The soil total organic carbon(TOC)stocks in 0~(-1)0,10-20,and 20-30 cm soil layers decreased from 95.87,79.08,and 71.55 t·hm~(-2) in 22-year-old plantation to 56.12,34.75,and 31.06 t·hm~(-2) in 65-year-old plantation,respectively,and the TOC stocks in these soil layers in 47 and 65-year-old plantations were less than those(88.08,71.16 and 64.81 t·hm~(-2),respectively) in primary forest.The easily oxidizable organic carbon(EOC) contents in 0~(-1)0,10-20,and 20-30 cm soil layers decreased from 35.89,26.91,and 26.00 g·kg~(-1) in primary forest to 20.25,14.50,and 12.36 g·kg~(-1) in 65-year-old plantation,the microbial biomass carbon(MBC)contents decreased from 524.44,273.26,and 257.97 mg·kg~(-1) in primary forest to 312.41,186.95,and 152.18 mg·kg~(-1) in 65-year-old plantation,and the particulate organic carbon(POC) contents decreased from 40.23,27.10,and 19.55 g·kg~(-1) in primary forest to 12.33,7.31,and 5.32 g·kg~(-1) in 65-year-old plantation,respectively.The results suggested that within the long succession period of primary P.asperata forest to its plantations in the subalpine zone of western Sichuan Province,soil TOC and labile organic carbon were in the state of net consumption. |
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| Keywords: | subalpine forest soil easily oxidizable organic carbon microbial biomass carbon particulate organic carbon |
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