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Citation:

The Var ia tion Character istics of So ilOrgan ic Carbon and Its InfluenceFactor in D ifferent Developing Stages of Chinese f ir Planta tion s

  • Received Date: 2009-04-10
  • The variation characteristics of soil organic carbon ( SOC) in different develop ing stages of Chinese firp lantations were studied in Dagang mountain of J iangxi Province. Correlation analysis and stepwise regressionanalysiswere used to investigate the influence of soil factors on SOC content. Results showed that SOC contentdecreased with increasing soil dep th. Significant variation characteristics of SOC contentwere found in different soillayers, with coefficient variation in the order of 40 - 60 cm > 20 - 40 cm > 0 - 20 cm, especially in the mediumforest soil. With the growth and development of Chinese fir p lantations, SOC content decreased from juvenile tomedium, and then increased from medium to over-mature. The SOC content had close correlations with totalnitrogen content and alkali-hydrolyzable nitrogen content. The SOC regression equations in different develop ingstages of Chinese fir p lantationswere established with high regression estimation p recision. Compared Beta suggestedthat soil nitrogen was the leading factor of SOC content variation.
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  • [1]

    David M B. Carbon control on spodosol nitrogen, sulfur and phosphorus cycling [M] / / McFeeW W, Kelly J M. Carbon Forms andFractions in Forest Soils. Soil Science Society of America, 1988:329 - 353
    [2]

    Dixon R K, Brown S, Houghton P A. Carbon pools and flux of global forest ecosystem [J]. Science, 1994, 263: 185 - 190
    [3]

    Sundquist E T. The global carbodioxide budget [J]. Science,1993, 259: 935 - 941
    [4]

    Jobbagy E G, Jackson R B. The vertical distribution of soil organiccarbon and itps relation to climate and vegetation [J]. Ecol App l,2002, 10 (2) : 423 - 436
    [5]

    Mann L K. Change in soil carbon storage after cultivation [J]. SoilSci, 1986, 142: 279 - 288
    [6]

    Davison E A. Acherman I L. Change in soil carbon inventions following cultivation of p reviously untilled soils [J]. Biogeochemistry,1993, 20: 161 - 193
    [7] 俞新妥. 杉木栽培学[M]. 福州: 福建科技出版社, 1997

    [8] 邓仕坚, 廖利平, 汪思龙. 间伐效应对杉木火力楠混交林凋落物动态变化的影响[J]. 应用生态学报, 2000, 11 (增刊) :146 - 150

    [9] 邓仕坚, 张家武, 陈楚莹,等. 不同树种混交林及其纯林对土壤理化性质影响的研究[J]. 应用生态学报, 1994, 5 (2) : 126 - 132

    [10] 廖利平, 汪思龙, 陈楚莹,等. 不同发育阶段杉木林凋落物量及其生态功能[J]. 应用生态学报, 2000, 11 (增刊) : 127 - 130

    [11] 邵月红, 潘剑君, 孙 波. 不同森林植被下土壤有机碳的分解特征及碳库研究[J]. 水土保持学报, 2001, 19 (3) : 24 - 28

    [12] 廖利平, 汪思龙, 陈楚莹. 杉木火力楠混交林凋落物量的动态变化: 10 年的观测[J]. 应用生态学报, 2000, 11 (增刊) :131 - 136

    [13] 汪思龙, 廖利平, 于小军,等. 退化杉木林土壤生态恢复过程中氮磷养分的变化[J]. 应用生态学报, 2000, 11 (增刊) :185 - 190

    [14] 盛炜彤, 范少辉. 杉木人工林长期生产力保持机制研究[M].北京: 科学出版社, 2005: 76 - 110

    [15] 张家武, 邓仕坚, 廖利平,等. 杉木连载土壤对其幼树生长的影响[J]. 应用生态学报, 1994, 5 (3) : 241 - 244

    [16] 郑郁善, 陈礼光, 洪 伟. 毛竹杉木混交林生产力和土壤性状研究[J]. 林业科学, 1998, 34 (增刊) : 16 - 25

    [17] 杨玉盛, 何宗明, 陈光水,等. 杉木多代连载后土壤肥力变化[J]. 土壤与环境, 2001, 10 (1) : 33 - 38

    [18] 焦如珍, 杨承栋. 杉木人工林不同发育阶段根际与非根际土壤微生物变化趋势[J]. 林业科学, 1999, 35 (1) : 53 - 59

    [19] 焦如珍, 杨承栋, 孙启武,等. 杉木人工林不同发育阶段土壤微生物数量及其生物量的变化[J]. 林业科学, 2005, 41 (6) :163 - 165

    [20] 焦如珍, 杨承栋, 屠星南, 等. 杉木人工林不同发育阶段林下植被、土壤微生物、酶活性及养分的变化[J]. 林业科学研究,1997, 10 (4) : 373 - 379

    [21] 国家林业局. 森林土壤分析方法[M]. 北京: 中国标准出版社, 1999

    [22] 鲍士旦. 土壤农化分析[M]. 北京: 中国农业出版社, 2005:30 - 106

    [23] 中国土壤学会农业化学专业委员会. 土壤农业化学常规分析方法[M]. 北京: 科学出版社, 1983: 95 - 101

    [24] 中国科学院南京土壤研究所微生物室. 土壤微生物研究法[M]. 北京: 科学出版社, 1985: 40 - 64

    [25] 方 晰, 田大伦, 项文化, 等. 杉木人工林土壤有机碳的垂直分布特征[J]. 浙江林学院学报, 2004, 21 (4) : 418 - 423

    [26] 盛炜彤,杨承栋,范少辉. 杉木人工林的土壤性质变化[J]. 林业科学研究, 2003, 16 (4) : 377 - 385

    [27] 陈楚莹, 廖利平, 汪思龙, 等. 杉木人工林生态学[M]. 北京:科学出版社, 2000

    [28] 周海庭, 郑晓明, 蒲德钦. 影响中学生数学成绩因素的通径分析[J]. 数理统计与管理, 2002 (11) : 15 - 20

    [29] 陈 贤, 王其刚, 关文灵, 等. 番茄品系产量的逐步回归分析[J]. 北方园艺, 2007 (3) : 8 - 9

    [30] 卢纹岱. SPSS forWindows统计分析[M]. 北京:电子工业出版社, 2006: 267 - 312

    [31] 周 莉, 李保国, 周光胜. 土壤有机碳主导影响因子及其研究进展[J]. 地球科学进展, 2005, 20 (1) : 99 - 105

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The Var ia tion Character istics of So ilOrgan ic Carbon and Its InfluenceFactor in D ifferent Developing Stages of Chinese f ir Planta tion s

  • 1. School of Soil andWater Conservation, Beijing Forestry University, Beijing 100083, China
  • 2. Research Institute of Forest Ecology, Environment and Protection, CAF, Beijing 100091, China

Abstract: The variation characteristics of soil organic carbon ( SOC) in different develop ing stages of Chinese firp lantations were studied in Dagang mountain of J iangxi Province. Correlation analysis and stepwise regressionanalysiswere used to investigate the influence of soil factors on SOC content. Results showed that SOC contentdecreased with increasing soil dep th. Significant variation characteristics of SOC contentwere found in different soillayers, with coefficient variation in the order of 40 - 60 cm > 20 - 40 cm > 0 - 20 cm, especially in the mediumforest soil. With the growth and development of Chinese fir p lantations, SOC content decreased from juvenile tomedium, and then increased from medium to over-mature. The SOC content had close correlations with totalnitrogen content and alkali-hydrolyzable nitrogen content. The SOC regression equations in different develop ingstages of Chinese fir p lantationswere established with high regression estimation p recision. Compared Beta suggestedthat soil nitrogen was the leading factor of SOC content variation.

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