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    福建长汀河田盆地的马尾松林碳储量时空动态变化

    黄绍霖 徐涵秋 曾宏达 刘智才 王琳

    黄绍霖, 徐涵秋, 曾宏达, 刘智才, 王琳, 2013. 福建长汀河田盆地的马尾松林碳储量时空动态变化. 地球科学, 38(5): 1081-1090. doi: 10.3799/dqkx.2013.106
    引用本文: 黄绍霖, 徐涵秋, 曾宏达, 刘智才, 王琳, 2013. 福建长汀河田盆地的马尾松林碳储量时空动态变化. 地球科学, 38(5): 1081-1090. doi: 10.3799/dqkx.2013.106
    HUANG Shao-lin, XU Han-qiu, ZENG Hong-da, LIU Zhi-cai, WANG Lin, 2013. Analysis of Spatial and Temporal Dynamics of Carbon Storage of Pinus Massoniana Forest in the Hetian Basin in County Changting of Fujian Province, China. Earth Science, 38(5): 1081-1090. doi: 10.3799/dqkx.2013.106
    Citation: HUANG Shao-lin, XU Han-qiu, ZENG Hong-da, LIU Zhi-cai, WANG Lin, 2013. Analysis of Spatial and Temporal Dynamics of Carbon Storage of Pinus Massoniana Forest in the Hetian Basin in County Changting of Fujian Province, China. Earth Science, 38(5): 1081-1090. doi: 10.3799/dqkx.2013.106

    福建长汀河田盆地的马尾松林碳储量时空动态变化

    doi: 10.3799/dqkx.2013.106
    基金项目: 

    教育部创新团队项目 IRT0960

    详细信息
      作者简介:

      黄绍霖(1986-),男,博士生,主要从事环境与资源遥感研究.E-mail: 515742109@qq.com

      通讯作者:

      徐涵秋,E-mail: hxu@fzu.edu.cn

    • 中图分类号: TP79

    Analysis of Spatial and Temporal Dynamics of Carbon Storage of Pinus Massoniana Forest in the Hetian Basin in County Changting of Fujian Province, China

    • 摘要: 以福建省长汀县侵蚀退化严重的河田盆地为例,重点研究该区水土流失生态修复的主要树种——马尾松林的碳储量动态变化.通过2011年的野外样地调查获得了马尾松林的实测数据,并将其与同期SPOT5影像对应样地改进的归一化植被指数(MNDVI)数据进行回归分析,建立了河田盆地2011年马尾松林碳储量的反演模型.进一步通过不变特征法对所获得的2011年模型进行校正,使其能够推广应用于2004年和2009年的马尾松林碳储量反演,以揭示河田盆地马尾松林碳储量在2004—2011年间的时空变化.研究结果表明,这期间河田盆地马尾松林的总碳储量和碳密度均呈逐步上升的趋势:总碳储量由2004年的9.28×105 t增加到2011年的12.49×105 t,碳密度由27.31×10-4 t/m2增加到35.84×10-4 t/m2,总的说明该区马尾松林的碳汇能力在这期间有了明显的增加,而且在2009—2011年间表现得更为明显.

       

    • 图  1  研究区三维示意图

      Fig.  1.  3D-perspective view of the study area

      图  2  研究技术路线

      Fig.  2.  Technical flow chart

      图  3  马尾松和芒萁FieldSpec3的实测高光谱反射光谱曲线

      Fig.  3.  FieldSpec3 measured spectral signature of Pinus massoniana and dicranopteris dichotoma

      图  4  马尾松林碳储量的实测值和预测值统计比较

      Fig.  4.  Comparison between measured and predicted carbon storage of Pinus massoniana forest

      图  5  各研究年份的马尾松林碳储量分布

      Fig.  5.  Spatial variations of the carbon storage of Pinus massoniana forest in the study area

      表  1  马尾松林碳储量反演模型

      Table  1.   Models for retrieving the carbon storage of Pinus massoniana forest

      函数类型 NDVI R2 RMSE MNDVI R2 RMSE
      线性 C=185.35NDVI-91.357 0.386 19.601 C=151.351MNDVI-41.948 0.655 14.685
      对数 C = 100.28ln(NDVI)+72.261 0.346 20.228 C=49.877ln(MNDVI)+67.703 0.525 17.240
      二次多项式 C= 571.38NDVI2-487.83NDVI+102.93 0.447 19.018 C=-148.79MNDVI2+362.235MNDVI+14.232 0.737 13.114
      乘幂 C = 308.23NDVI6.602 0.592 0.805 C = 193.524MNDVI3.103 0.801 0.561
      指数 C = 0.008 3e11.801NDVI 0.617 0.779 C=0.271 6e8.818MNDVI 0.877 0.441
      注:回归方程均通过0.1%的显著性检验.
      下载: 导出CSV

      表  2  2004—2011年研究区的马尾松林碳储量统计

      Table  2.   The carbon storage of Pinus massoniana forest in the study area from 2004 to 2011

      时间(年) 面积(104 m2) 碳密度(10-4 t/m2) 总碳储量(105 t)
      2004 33 965.40 27.31 9.28
      2009 35 003.94 33.20 11.62
      2011 34 856.45 35.84 12.49
      下载: 导出CSV

      表  3  2004—2011年间各级马尾松林碳储量的分布统计

      Table  3.   The classified carbon storage of Pinus massoniana forest during the study years

      碳储量范围(10-4 t/m2) 面积所占百分比(%) 碳储量总量所占百分比(%)
      2004年 2009年 2011年 2004年 2009年 2011年
      C≤25 64.46 53.40 57.54 22.86 18.81 17.72
      25<C≤50 19.03 24.53 19.44 25.01 26.61 19.39
      50<C≤75 8.88 12.06 9.51 19.82 22.17 16.26
      75<C≤100 4.09 5.51 5.35 12.85 14.25 12.89
      C>100 3.54 4.50 8.16 19.47 18.16 33.74
      下载: 导出CSV

      表  4  马尾松林碳储量在不同高程的分布特征

      Table  4.   Spatial variations of the carbon storage of Pinus massoniana forest with different altitudes

      时间(年) 高程(m) 面积(104 m2) 面积所占百分比(%) 平均碳储量(10-4 t/m2) 总碳储量(105 t) 总碳储量所占百分比(%)
      2004 ≤400 21 754.93 64.05 17.80 3.87 41.74
      400~600 9 917.48 29.20 37.09 3.68 39.65
      600~800 2 113.22 6.22 73.01 1.54 16.63
      >800 179.78 0.53 101.82 0.18 1.97
      2009 ≤400 22 084.37 63.09 24.36 5.38 46.30
      400~600 10 988.52 31.39 45.56 5.01 43.08
      600~800 1 834.30 5.24 64.13 1.18 10.12
      >800 96.74 0.28 59.42 0.06 0.49
      2011 ≤400 20 621.14 59.16 20.42 4.21 33.70
      400~600 10 608.53 30.43 49.24 5.22 41.82
      600~800 3 321.45 9.53 83.78 2.78 22.28
      >800 305.32 0.88 90.20 0.28 2.20
      下载: 导出CSV

      表  5  马尾松林碳储量在不同坡度的分布特征

      Table  5.   Spatial variations of the carbon storage of Pinus massoniana forest with different slopes

      时间(年) 坡度(°) 面积(104 m2) 面积所占百分比(%) 平均碳储量(10-4 t/m2) 总碳储量(105 t) 总碳储量所占百分比(%)
      2004 ≤5 9 463.51 27.86 22.45 2.12 22.90
      5~15 13 528.01 39.83 22.91 3.10 33.40
      15~25 7 120.64 20.96 32.28 2.30 24.77
      25~35 2 913.87 8.58 42.82 1.25 13.45
      35~45 788.24 2.32 52.38 0.41 4.45
      >45 151.14 0.44 63.00 0.10 1.03
      2009 ≤5 9 251.32 26.43 28.93 2.68 23.03
      5~15 13 680.01 39.08 29.04 3.97 34.19
      15~25 7 773.11 22.21 37.68 2.93 25.20
      25~35 3 262.26 9.32 45.87 1.50 12.88
      35~45 877.88 2.51 52.20 0.46 3.94
      >45 159.36 0.46 55.19 0.09 0.76
      2011 ≤5 9 362.68 26.86 29.56 2.77 22.16
      5~15 13 470.33 38.65 29.37 3.96 31.67
      15~25 7 460.13 21.40 42.19 3.15 25.19
      25~35 3 348.35 9.61 54.95 1.84 14.73
      35~45 1 009.36 2.90 63.70 0.64 5.15
      >45 205.61 0.59 67.12 0.14 1.10
      下载: 导出CSV
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