Carbon Storage and Distribution in Rubber Plantation during Regeneration

WANG Chun-yan; CHEN Qiu-bo; PENG Yi; LIU Jian-bo; YANG Li-fu; WANG Zhen-hui

Volume 24 Issue 5

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Carbon Storage and Distribution in Rubber Plantation during Regeneration

1.
Rubber Research Institute, Chinese Academy of Tropical Agriculture Sciences, Danzhou 571737, Hainan, China
2.
Environment and Plant Protection Department of Hainan University, Danzhou 571737, Hainan, China
3.
Zunyi Normal College, Zunyi 563002, Guizhou, China
4.
Hainan Provincial Institute of Construction Project Planning & Design, Haikou 570203, Hainan, China

Received Date: 2011-03-28

Abstract

The carbon content and its distribution in rubber (Hevea brasiliensis (Willd. ex A. Juss.) Muell. Arg.) plantation in regeneration period were studied. The results showed that the carbon content in different organs of rubber trees ranged from 29.94% to 52.90% and decreased with the order of leaves > trunk > root >branch> bark > latex. The carbon content of dry samples from the same organ was higher than that of fresh samples. The carbon content in litter layer and understory plant layer were 51.90% and 46.09 %, respectively. The carbon content in the soil was 0.54% and decreased with soil depth, and no significant difference was found between the adjacent two soil layers. The total carbon storage in rubber plantation was 219.68 t·hm-2, of which 140.21 t·hm-2 in the aboveground arbor, about 63.82%, 3.99 t·hm-2 in the litter, about 1.82%, and 75.48 t·hm-2 in the soil layer (0～100 cm), accounted for 34.36 %. The carbon storages in different organs were positively related to the biomass of corresponding organs. The trunk accumulated the highest carbon storage and comprised 55.64% of carbon storage in aboveground arbor.
- Hevea brasiliensis,
- carbon storage,
- carbon content,
- regeneration period

References

[1]	woodwell G M , Whittaker R H, Reiners W A, et al. The biota and the world carbon budget[J]. Science, 1978,199: 141-146
[2]	Post W M , Emanuel W R, Zinke P J, et al. Soil carbon pools and world life zone[J]. Nature, 1982, 298: 156-159
[3]	袁嘉祖,范晓明.中国森林碳汇功能的成本效益分析[J]. 河北林果研究, 1997, 12(1): 20-24
[4]	Kramer P J. Carbon dioxide concentration ,potosynthesis and dry matter production[J]. Bio Science, 1981, 31:29-33
[5]	王效科,冯宗炜.森林生态系统中生物量和碳贮量的研究历史[M]. 北京: 中国科学与技术出版社, 1995:335-347
[6]	马钦彦,陈遐林,王娟,等.华北主要森林类型建群种的含碳率分析[J]. 北京林业大学学报, 2002, 24(5): 96-100
[7]	Zhang H, Zhang G L, Zhao Y G, et al. Chemical degradation of a Ferralsol (Oxisol) under intensive rubber(Hevea brasiliensis) farming in tropical China[J]. Soil & Tillage Research, 2007, 93: 109-116
[8]	杨景成, 黄建辉, 潘庆民, 等.西双版纳不同热带生态系统土壤有机质的光谱学特性[J]. 植物生态学报, 2004, 28(5): 623-629
[9]	房秋兰, 沙丽清.西双版纳热带季节雨林与橡胶林土壤呼吸[J]. 植物生态学报, 2006, 30(1): 97-103
[10]	周文君,沙丽清,沈守艮,等.西双版纳橡胶林土壤呼吸季节变化及其影响因子[J].山地学报,2008, 26(3): 317-325
[11]	池富旺,张培松,罗微,等.中大尺度下橡胶园土壤全氮和有机质含量的空间分布特征[J]. 热带作物学报, 2009, 30(5): 613-619
[12]	杨昆, 管东生. 森林林下植被生物量收获的样方选择和模型[J]. 生态学报, 2007, 27(2): 705-714
[13]	森林土壤有机质的测定及碳氮比的计算.中华人民共和国林业行业标准[S]. 1999, LY/T 1237
[14]	鲍士旦. 土壤农化分析 [M]. 第三版,北京: 中国农业出版社, 2000
[15]	尉海东, 马祥庆.中亚热带不同发育阶段杉木人工林生态系统碳贮量研究[J]. 江西农业大学学报, 2006, 28(2): 239-243,267
[16]	方晰,田大伦,项文化.速生阶段杉木人工林碳素密度、贮量和分布[J].林业科学,2002, 38(3):14-19
[17]	康冰,刘世荣,张广军,等.广西大青山南亚热带马尾松、杉木混交林生态系统碳素积累和分配特征[J]. 生态学报, 2006, 26(5): 1320-1329
[18]	钟羡芳,杨玉盛,高人,等.老龄杉木人工林生态系统碳库及分配[J]. 亚热带资源与环境学报, 2008, 3(2): 11-17
[19]	田大伦,方晰,项文化.湖南会同杉木人工林生态系统碳素密度[J]. 生态学报, 2004, 4(11): 2382-2386
[20]	雷丕锋, 项文化, 田大伦, 等. 樟树人工林生态系统碳素贮量与分布研究[J]. 生态学杂志, 2004, 23(4): 25-30
[21]	何斌, 刘运华, 余浩光, 等. 南宁马占相思人工林生态系统碳素密度与贮量[J]. 林业科学. 2009, 45(2):6-11
[22]	韩氏杰.中国陆地生态系统碳循环的生物地球化学过程[M]. 北京: 科技出版社,2008
[23]	蒋菊生, 王如松. 橡胶林固定CO₂和释放O₂的服务功能及其价值估计[J]. 生态学报, 2002, 22(9): 1545-1551
[24]	尉海东, 马祥庆.不同发育阶段楠木人工林生态系统碳贮量研究[J]. 烟台师范学院学报:自然科学版, 2006, 22(2): 130-133
[25]	周玉荣, 于振良, 赵士洞.我国主要森林生态系统碳贮量和碳平衡[J]. 植物生态学报, 2000, 24(5): 518- 522
[26]	莫江明, 方运霆, 彭少麟, 等.鼎湖山南亚热带常绿阔叶林碳素积累和分配特征[J]. 生态学报, 2003, 23 (10): 1970-1976
[27]	吴仲民, 李意德, 曾庆波, 等.尖峰岭热带山地雨林C素库及皆伐影响的初步研究[J]. 应用生态学报, 1998, 9(4): 341-344
[28]	杨玉盛, 林先富, 俞新妥, 等.杉木套种山苍子模式结构与生物量初步研究[J]. 福建林学院学报, 1991, 11 (4): 341-348
[29]	Cotter M, Martin K, Sauerborn J. How do "Renewable Products" impact biodiversity and ecosystem services-the example of natural rubber in China[J]. Journal of Agriculture and Rural Development in the Tropics and Subtropics,2009, 110 (1): 9-22
[30]	Zhang M, Fu X H, Feng W T, et al. Soil organic carbon in pure rubber and tea-rubber plantations in southwestern China[J]. Tropical Ecology, 2007, 48: 1-7
[31]	Suchanek T H, Mooney H A, Franklin J F, et al. Carbon dynamics of an old-growth forest [J]. Ecosystems, 2004, 7: 421-426

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Carbon Storage and Distribution in Rubber Plantation during Regeneration

1. Rubber Research Institute, Chinese Academy of Tropical Agriculture Sciences, Danzhou 571737, Hainan, China

2. Environment and Plant Protection Department of Hainan University, Danzhou 571737, Hainan, China

3. Zunyi Normal College, Zunyi 563002, Guizhou, China

4. Hainan Provincial Institute of Construction Project Planning & Design, Haikou 570203, Hainan, China

Received Date: 2011-03-28

Abstract: The carbon content and its distribution in rubber (Hevea brasiliensis (Willd. ex A. Juss.) Muell. Arg.) plantation in regeneration period were studied. The results showed that the carbon content in different organs of rubber trees ranged from 29.94% to 52.90% and decreased with the order of leaves > trunk > root >branch> bark > latex. The carbon content of dry samples from the same organ was higher than that of fresh samples. The carbon content in litter layer and understory plant layer were 51.90% and 46.09 %, respectively. The carbon content in the soil was 0.54% and decreased with soil depth, and no significant difference was found between the adjacent two soil layers. The total carbon storage in rubber plantation was 219.68 t·hm-2, of which 140.21 t·hm-2 in the aboveground arbor, about 63.82%, 3.99 t·hm-2 in the litter, about 1.82%, and 75.48 t·hm-2 in the soil layer (0～100 cm), accounted for 34.36 %. The carbon storages in different organs were positively related to the biomass of corresponding organs. The trunk accumulated the highest carbon storage and comprised 55.64% of carbon storage in aboveground arbor.

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Reference (31)

[1]	woodwell G M , Whittaker R H, Reiners W A, et al. The biota and the world carbon budget[J]. Science, 1978,199: 141-146
[2]	Post W M , Emanuel W R, Zinke P J, et al. Soil carbon pools and world life zone[J]. Nature, 1982, 298: 156-159
[3]	袁嘉祖,范晓明.中国森林碳汇功能的成本效益分析[J]. 河北林果研究, 1997, 12(1): 20-24
[4]	Kramer P J. Carbon dioxide concentration ,potosynthesis and dry matter production[J]. Bio Science, 1981, 31:29-33
[5]	王效科,冯宗炜.森林生态系统中生物量和碳贮量的研究历史[M]. 北京: 中国科学与技术出版社, 1995:335-347
[6]	马钦彦,陈遐林,王娟,等.华北主要森林类型建群种的含碳率分析[J]. 北京林业大学学报, 2002, 24(5): 96-100
[7]	Zhang H, Zhang G L, Zhao Y G, et al. Chemical degradation of a Ferralsol (Oxisol) under intensive rubber(Hevea brasiliensis) farming in tropical China[J]. Soil & Tillage Research, 2007, 93: 109-116
[8]	杨景成, 黄建辉, 潘庆民, 等.西双版纳不同热带生态系统土壤有机质的光谱学特性[J]. 植物生态学报, 2004, 28(5): 623-629
[9]	房秋兰, 沙丽清.西双版纳热带季节雨林与橡胶林土壤呼吸[J]. 植物生态学报, 2006, 30(1): 97-103
[10]	周文君,沙丽清,沈守艮,等.西双版纳橡胶林土壤呼吸季节变化及其影响因子[J].山地学报,2008, 26(3): 317-325
[11]	池富旺,张培松,罗微,等.中大尺度下橡胶园土壤全氮和有机质含量的空间分布特征[J]. 热带作物学报, 2009, 30(5): 613-619
[12]	杨昆, 管东生. 森林林下植被生物量收获的样方选择和模型[J]. 生态学报, 2007, 27(2): 705-714
[13]	森林土壤有机质的测定及碳氮比的计算.中华人民共和国林业行业标准[S]. 1999, LY/T 1237
[14]	鲍士旦. 土壤农化分析 [M]. 第三版,北京: 中国农业出版社, 2000
[15]	尉海东, 马祥庆.中亚热带不同发育阶段杉木人工林生态系统碳贮量研究[J]. 江西农业大学学报, 2006, 28(2): 239-243,267
[16]	方晰,田大伦,项文化.速生阶段杉木人工林碳素密度、贮量和分布[J].林业科学,2002, 38(3):14-19
[17]	康冰,刘世荣,张广军,等.广西大青山南亚热带马尾松、杉木混交林生态系统碳素积累和分配特征[J]. 生态学报, 2006, 26(5): 1320-1329
[18]	钟羡芳,杨玉盛,高人,等.老龄杉木人工林生态系统碳库及分配[J]. 亚热带资源与环境学报, 2008, 3(2): 11-17
[19]	田大伦,方晰,项文化.湖南会同杉木人工林生态系统碳素密度[J]. 生态学报, 2004, 4(11): 2382-2386
[20]	雷丕锋, 项文化, 田大伦, 等. 樟树人工林生态系统碳素贮量与分布研究[J]. 生态学杂志, 2004, 23(4): 25-30
[21]	何斌, 刘运华, 余浩光, 等. 南宁马占相思人工林生态系统碳素密度与贮量[J]. 林业科学. 2009, 45(2):6-11
[22]	韩氏杰.中国陆地生态系统碳循环的生物地球化学过程[M]. 北京: 科技出版社,2008
[23]	蒋菊生, 王如松. 橡胶林固定CO₂和释放O₂的服务功能及其价值估计[J]. 生态学报, 2002, 22(9): 1545-1551
[24]	尉海东, 马祥庆.不同发育阶段楠木人工林生态系统碳贮量研究[J]. 烟台师范学院学报:自然科学版, 2006, 22(2): 130-133
[25]	周玉荣, 于振良, 赵士洞.我国主要森林生态系统碳贮量和碳平衡[J]. 植物生态学报, 2000, 24(5): 518- 522
[26]	莫江明, 方运霆, 彭少麟, 等.鼎湖山南亚热带常绿阔叶林碳素积累和分配特征[J]. 生态学报, 2003, 23 (10): 1970-1976
[27]	吴仲民, 李意德, 曾庆波, 等.尖峰岭热带山地雨林C素库及皆伐影响的初步研究[J]. 应用生态学报, 1998, 9(4): 341-344
[28]	杨玉盛, 林先富, 俞新妥, 等.杉木套种山苍子模式结构与生物量初步研究[J]. 福建林学院学报, 1991, 11 (4): 341-348
[29]	Cotter M, Martin K, Sauerborn J. How do "Renewable Products" impact biodiversity and ecosystem services-the example of natural rubber in China[J]. Journal of Agriculture and Rural Development in the Tropics and Subtropics,2009, 110 (1): 9-22
[30]	Zhang M, Fu X H, Feng W T, et al. Soil organic carbon in pure rubber and tea-rubber plantations in southwestern China[J]. Tropical Ecology, 2007, 48: 1-7
[31]	Suchanek T H, Mooney H A, Franklin J F, et al. Carbon dynamics of an old-growth forest [J]. Ecosystems, 2004, 7: 421-426

Carbon Storage and Distribution in Rubber Plantation during Regeneration

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通讯作者: 陈斌, bchen63@163.com

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Carbon Storage and Distribution in Rubber Plantation during Regeneration

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