植物生态学报
植物生態學報
식물생태학보
ACTA PHYTOECOLOGICA SINICA
2005年
2期
296-303
,共8页
杨景成%黄建辉%唐建维%潘庆民%韩兴国
楊景成%黃建輝%唐建維%潘慶民%韓興國
양경성%황건휘%당건유%반경민%한흥국
生物量%碳固存%土地利用变化%橡胶园%土壤有机碳
生物量%碳固存%土地利用變化%橡膠園%土壤有機碳
생물량%탄고존%토지이용변화%상효완%토양유궤탄
Biomass%Carbon sequestration%Land use change%Rubber tree plantation%Soil organic carbon
由于温室气体的大量排放引起的全球气候变暖等环境问题日益严重,近年来人们开始考虑通过植被和土壤的碳固存,以缓解大气中CO2浓度的升高速度,减缓温室效应的影响.有研究表明,热带原始森林的保护和人工林的建立能有效地固存大气中的碳.但是,在建立热带种植园和人工林以固存大气CO2的可行性及其碳的固存潜力大小等方面还存在较大争议.云南省西双版纳自治州是我国重要的热带地区之一,目前橡胶(Hevea brasiliensis)园的面积为1.3×105hm2,约占该地区林地面积的14%.在本研究中,选择11块在弃耕后的农田上建立的橡胶园(定植年限为3至38年),初步探讨了橡胶园建立后植被和土壤中碳的固存规律.两个生物量模型(唐建维等的模型和Brown模型)的模拟结果显示,橡胶园建立后植被中生物量的平均增长速率分别为10.2×103和9.4×103k·hm-2·a-1,40和100cm表层土壤碳的平均固存速率分别为0.61×103和0.72×103kgC·hm-2·a-1,植被和100cm表层土壤中碳的平均固存速率为5.82×103和5.42×103kgC·hm-2·a-1,而定植40年后植被和100cm表层土壤碳的固存潜力为232.8 × 103和216.8×103kg C·hm-2.对两个模型的比较结果显示,唐建维等的模型生物量计算结果明显高于Brown模型,尤其是在对中幼龄橡胶园生物量估算时更是如此.
由于溫室氣體的大量排放引起的全毬氣候變暖等環境問題日益嚴重,近年來人們開始攷慮通過植被和土壤的碳固存,以緩解大氣中CO2濃度的升高速度,減緩溫室效應的影響.有研究錶明,熱帶原始森林的保護和人工林的建立能有效地固存大氣中的碳.但是,在建立熱帶種植園和人工林以固存大氣CO2的可行性及其碳的固存潛力大小等方麵還存在較大爭議.雲南省西雙版納自治州是我國重要的熱帶地區之一,目前橡膠(Hevea brasiliensis)園的麵積為1.3×105hm2,約佔該地區林地麵積的14%.在本研究中,選擇11塊在棄耕後的農田上建立的橡膠園(定植年限為3至38年),初步探討瞭橡膠園建立後植被和土壤中碳的固存規律.兩箇生物量模型(唐建維等的模型和Brown模型)的模擬結果顯示,橡膠園建立後植被中生物量的平均增長速率分彆為10.2×103和9.4×103k·hm-2·a-1,40和100cm錶層土壤碳的平均固存速率分彆為0.61×103和0.72×103kgC·hm-2·a-1,植被和100cm錶層土壤中碳的平均固存速率為5.82×103和5.42×103kgC·hm-2·a-1,而定植40年後植被和100cm錶層土壤碳的固存潛力為232.8 × 103和216.8×103kg C·hm-2.對兩箇模型的比較結果顯示,唐建維等的模型生物量計算結果明顯高于Brown模型,尤其是在對中幼齡橡膠園生物量估算時更是如此.
유우온실기체적대량배방인기적전구기후변난등배경문제일익엄중,근년래인문개시고필통과식피화토양적탄고존,이완해대기중CO2농도적승고속도,감완온실효응적영향.유연구표명,열대원시삼림적보호화인공림적건립능유효지고존대기중적탄.단시,재건립열대충식완화인공림이고존대기CO2적가행성급기탄적고존잠력대소등방면환존재교대쟁의.운남성서쌍판납자치주시아국중요적열대지구지일,목전상효(Hevea brasiliensis)완적면적위1.3×105hm2,약점해지구임지면적적14%.재본연구중,선택11괴재기경후적농전상건립적상효완(정식년한위3지38년),초보탐토료상효완건립후식피화토양중탄적고존규률.량개생물량모형(당건유등적모형화Brown모형)적모의결과현시,상효완건립후식피중생물량적평균증장속솔분별위10.2×103화9.4×103k·hm-2·a-1,40화100cm표층토양탄적평균고존속솔분별위0.61×103화0.72×103kgC·hm-2·a-1,식피화100cm표층토양중탄적평균고존속솔위5.82×103화5.42×103kgC·hm-2·a-1,이정식40년후식피화100cm표층토양탄적고존잠력위232.8 × 103화216.8×103kg C·hm-2.대량개모형적비교결과현시,당건유등적모형생물량계산결과명현고우Brown모형,우기시재대중유령상효완생물량고산시경시여차.
The ability for vegetation and soil organic matter (SOM) to sequester atmospheric CO2 has receiveda lot of attention recently. Two management options being considered for enhancing C sequestration from the atmosphere include tropical forest conservation and establishment of plantations; however, there is still considerable debate regarding the appropriateness of using plantations and the sequestration potential of tropical plantations. There are 1.3×105 hm2 of rubber trees ( Hevea brasiliensis ) plantations in Xishuangbanna, southwest China, which account for approximately 14% of the forest lands in this region. In this study, eleven plantations of different ages were selected to investigate C sequestration in the vegetation and soils following the establishment of rubber tree plantations on former arable lands. The results indicated that the average biomass growth rates of the rubber trees, calculated according to two different biomass growth equations, were models. When comparing the two models, our results showed that the biomass calculated based on the equation of Tang et al. was higher than that based on the equation of Brown, especially in young- and middle-aged rubber tree plantations.