植物生态学报 ›› 2009, Vol. 33 ›› Issue (3): 535-545.DOI: 10.3773/j.issn.1005-264x.2009.03.012 cstr: 32100.14.j.issn.1005-264x.2009.03.012
所属专题: 生态系统碳水能量通量
孙晓新, 牟长城(
), 石兰英, 程伟, 刘霞, 吴云霞, 冯登军
收稿日期:2008-08-20
接受日期:2009-02-02
出版日期:2009-08-20
发布日期:2009-05-31
作者简介:*E-mail: mccnefu@yahoo.com基金资助:
SUN Xiao-Xin, MU Chang-Cheng(
), SHI Lan-Ying, CHENG Wei, LIU Xia, WU Yun-Xia, FENG Deng-Jun
Received:2008-08-20
Accepted:2009-02-02
Online:2009-08-20
Published:2009-05-31
摘要:
利用静态箱-气相色谱法, 对小兴安岭5种森林沼泽生长季甲烷 (CH4) 排放通量进行研究, 并探讨了温度、地下水位和植被等主要环境因子对CH4排放的影响。结果表明:毛赤杨 (Alnus sibirica) 沼泽、落叶松 (Larix gmelinii) -藓类 (Moss) 沼泽和落叶松-泥炭藓 (Sphagnum spp.) 沼泽的CH4排放有明显的季节变化规律, 而白桦 (Betula platyphylla) 沼泽和落叶松-苔草 (Carex schmidtii) 沼泽CH4通量的季节变化相对较小。落叶松-泥炭藓沼泽有爆发式CH4通量现象出现, 对生长季CH4排放通量影响较大。在生长季内落叶松-泥炭藓沼泽、毛赤杨沼泽和白桦沼泽为大气CH4的源, 而落叶松-苔草沼泽和落叶松-藓类沼泽为大气CH4的汇, 生长季CH4的平均排放通量分别为 (56.08±200.38) 、 (15.34±14.89) 、 (0.64±0.88) 、 (-0.88±1.76) 和 (-0.94±3.00) mg·m-2·d-1。除落叶松-泥炭藓沼泽外, 不同森林沼泽类型间CH4排放通量随地下水位升高而增大;地下水位在-34.5~-30.8cm之间可能存在CH4源与汇的临界点, 季节平均地下水位低于这一位置的森林沼泽为大气CH4的汇。温度对森林沼泽CH4通量的影响比较复杂, 二者间可能为正或负的显著 (p<0.05) 或非显著 (p>0.05) 相关关系。CH4通量与乔木地上生物量有较强的负相关性, 这有可能成为小兴安岭森林沼泽CH4通量的最佳预测因子。
孙晓新, 牟长城, 石兰英, 程伟, 刘霞, 吴云霞, 冯登军. 小兴安岭森林沼泽甲烷排放及其影响因子. 植物生态学报, 2009, 33(3): 535-545. DOI: 10.3773/j.issn.1005-264x.2009.03.012
SUN Xiao-Xin, MU Chang-Cheng, SHI Lan-Ying, CHENG Wei, LIU Xia, WU Yun-Xia, FENG Deng-Jun. METHANE EMISSION FROM FORESTED SWAMPS IN XIAOXING’AN MOUNTAINS, NORTHEASTERN CHINA. Chinese Journal of Plant Ecology, 2009, 33(3): 535-545. DOI: 10.3773/j.issn.1005-264x.2009.03.012
图1 森林沼泽CH4通量的季节变化规律 MCY:毛赤杨沼泽Alnus sibirica swamp BH:白桦沼泽Betula platyphylla swamp LYS-TC:落叶松-苔草沼泽Larix gmelinii-Carex schmidtii swamp LYS-XL:落叶松-藓类沼泽Larix gmelinii-moss swamp LYS-NTX:落叶松-泥炭藓沼泽Larix gmelinii-Sphagnum spp.swamp排放值超出图内的纵坐标时, 直接在图上列出具体数值Values outside of the scale of the figure are given as text on the plot
Fig.1 Seasonal variations of CH4 flux in different forested swamps
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