globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6155611
论文题名:
博斯腾湖人工和天然芦苇湿地土壤CO_2 、CH_4和N_2 O排放通量
其他题名: Emission fluxes of CO_2,CH_4,and N_2O from artificial and natural reed wetlands in Bosten Lake,China
作者: 王金龙1; 李艳红1; 李发东2
刊名: 生态学报
ISSN: 1000-0933
出版年: 2018
卷: 38, 期:2, 页码:645-652
语种: 中文
中文关键词: 芦苇湿地 ; 土壤 ; 温室气体 ; 全球增温潜势 ; 博斯腾湖
英文关键词: reed wetland ; soil ; greenhouse gases ; global warming potential ; Bosten lake
WOS学科分类: AGRICULTURE MULTIDISCIPLINARY
WOS研究方向: Agriculture
中文摘要: 为研究干旱区淡水湖泊人工、天然芦苇湿地土壤温室气体源汇强度及其影响因素,采用静态箱-气相色谱法,于2015年1月12月对博斯腾湖人工和天然芦苇湿地土壤CO_2、CH_4和N_2O通量进行全年观测。结果表明,人工芦苇湿地土壤CO_2、CH_4和N_2O排放通量变化范围分别为: 10.1588.4mg m~(-2) h~(-1)、2.982.4mug m~(-2) h~(-1)和1.3229.7mug m~(-2) h~(-1),天然芦苇湿地土壤CO_2、 CH_4和N_2O排放通量变化范围分别为10.3469.6mg m~(-2) h~(-1)、3.164.8mug m~(-2) h~(-1)和1.914.3mug m~(-2) h~(-1)。人工和天然芦苇湿地夏季土壤CO_2排放通量均明显高于其他季节,而土壤CH_4和N_2O排放通量较大值多集中在春末夏初。全年观测期间,人工芦苇湿地土壤CO_2、CH_4和N_2O排放通量高于天然芦苇湿地(P>0.05);温度是影响人工、天然芦苇湿地土壤CO_2和N_2O排放通量的关键因素,近地面温度和5cm土壤温度与CO_2和N_2O排放通量呈现极显著的正相关关系(P<0.01) 。土壤CH_4排放通量是温度和水分二者共同影响的,由近地表温度、5cm土壤温度和土壤含水量共同拟合的方程可以分别解释人工、天然芦苇湿地土壤CH_4排放通量的71%、74.5%;土壤有机碳、pH、盐分、NH_4~+-N、NO_3~--N也是人工、天然芦苇湿地土壤CO_2、CH_4和N_2O排放通量的影响因素;人工和天然芦苇湿地土壤均是CO_2、CH_4和N_2O的源。基于100年尺度,由3种温室气体计算全球增温潜势得出,人工芦苇湿地全球增温潜势大于天然芦苇湿地(15150.18kg /hm~2>12484.21kg /hm~2) 。
英文摘要: CO_2,CH_4,and N_2O,have strong warming potentials and are considered to be the primary greenhouse gases in the atmosphere.Global warming caused by the increasing concentrations of atmospheric CO_2,CH_4,and N_2O is one of the hotspots in global change field.Greenhouse gas (GHG) fluxes in reed wetlands are critical in evaluating the source /sink strength of GHG in arid area.We studied the dynamics of soil CO_2,CH_4,and N_2O fluxes using static chamberbased on gas chromatography in two reed wetlands of the freshwater Bosten Lake,located in an arid area of Northwestern China.During a full year of monitoring,environmental variables (including soil moisture,soil temperature,air temperature,pH and salinity) were measured to determine the effects of abiotic factors on soil CO_2,CH_4,and N_2O fluxes in artificial and natural reed wetlands.SPSS 19.0 for Windows was used to analyze the relationships between environmental factors and soil CO_2,CH_4,and N_2O fluxes.The results showed that soil CO_2,CH_4,and N_2O fluxes in the artificial reed wetland were 10.1588.4mg m~(-2) h~(-1),1.3229.7mug m~(-2) h~(-1) and 3.164.8mug m~(-2) h~(-1),respectively,which was comparable with the values from the natural reed wetland.Higher soil CO_2 emissions occurred in summer,whereas CH_4 and N_2O emissions mainly occurred in late spring and early summer.Temperature was the main factor controlling soil CO_2 and N_2O fluxes in both reed wetlands (P < 0.01).Soil CH_4 emission flux was affected by both temperature and moisture.According to regression analysis,the combination of near-surface temperature,top 5cm soil temperature,and soil water content could explain 71% and 74.5% of soil CH_4 flux in artificial and natural reed wetlands,respectively.Soil organic carbon,pH,salinity,NH_4~+-N,and NO_3~--N are also influencing factors of CO_2,CH_4,and N_2O fluxes in artificial and natural reed wetlands.However,the differences in CO_2,CH_4,and N_2O emissions from soils of artificial and natural reed wetlands were caused by differences in soil organic carbon,soluble nitrogen,and biomass.Based on the centennial scale,the soils of artificial and natural reed wetland were " sources" of GHG,and the global warming potential from artificial reed wetland was higher than that from natural reed wetland.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/154627
Appears in Collections:气候变化事实与影响

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作者单位: 1.新疆维吾尔自治区重点实验室新疆干旱区湖泊环境与资源实验室
2.新疆师范大学地理科学与旅游学院, 新疆维吾尔自治区重点实验室新疆干旱区湖泊环境与资源实验室
3., 乌鲁木齐
4.乌鲁木齐,
5.830054
6.830054
7.新疆维吾尔自治区重点实验室新疆干旱区湖泊环境与资源实验室
8.新疆师范大学地理科学与旅游学院
9.中国科学院地理科学与资源研究所
10.中国科学院大学资源与环境学院, 新疆维吾尔自治区重点实验室新疆干旱区湖泊环境与资源实验室
11., 乌鲁木齐
12.乌鲁木齐
13.,
14.北京
15.北京 830054
16.830054
17.100101
18.100190

Recommended Citation:
王金龙,李艳红,李发东. 博斯腾湖人工和天然芦苇湿地土壤CO_2 、CH_4和N_2 O排放通量[J]. 生态学报,2018-01-01,38(2):645-652
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