Isotopic signature is a powerful tool to discriminate methane(CH_(4)) source types and constrain regional and global scale CH_(4) budgets.Peatlands on the Qinghai-Tibetan Plateau are poorly understood about the isotop...Isotopic signature is a powerful tool to discriminate methane(CH_(4)) source types and constrain regional and global scale CH_(4) budgets.Peatlands on the Qinghai-Tibetan Plateau are poorly understood about the isotopic signature of CH_(4) due to the limited experimental conditions.In this study,three campaigns of diurnal air samples spacing 2-3 h were taken from an alpine peatland on the eastern Qinghai-Tibetan Plateau to investigate its source signal characteristics.Both CH_(4) concentration and its stable carbon isotope(δ^(13)C-CH_(4)) were measured to derive the carbon isotopic signature of the CH_(4) source using the Keeling plot technique.Diurnal variation patterns in CH_(4) concentration and δ^(13)C-CH_(4) were observed during summertime,with depleted δ^(13)C-CH_(4) signals and high CH_(4) concentration appearing at nighttime.The δ^(13)C-CH4 signature during summer was calculated to be-71 % ± 1.3%,which falls within the range of other wetland studies and close to high-latitude peatlands.The boundary layer dynamic and CH_(4) source were supposed to influence the measured CH_(4) concentration and δ^(13)C-CH_(4.)Further investigations of CH_(4) isotopic signals into the nongrowing season are still needed to constrain the δ^(13)C-CH_(4) signature and its environmental controls in this region.展开更多
Wetlands store large amounts of carbon stocks and are essential in both global carbon cycling and regional ecosystem services.Understanding the dynamics of wetland carbon exchange is crucial for assessing carbon budge...Wetlands store large amounts of carbon stocks and are essential in both global carbon cycling and regional ecosystem services.Understanding the dynamics of wetland carbon exchange is crucial for assessing carbon budgets and predicting their future evolution.Although many studies have been conducted on the effects of climate change on the ecosystem carbon cycle,little is known regarding carbon emissions from the alpine wetlands in arid northwest China.In this study,we used an automatic chamber system(LI-8100A)to measure ecosystem respiration(ER)in the Bayinbuluk alpine wetland in northwest China.The ER showed a significant bimodal diurnal variation,with peak values appearing at 16:30 and 23:30(Beijing time,UTC+8).A clear seasonal pattern in ER was observed,with the highest value(19.38μmol m-2 s-l)occurring in August and the lowest value(0.11μmol m-2 s-1)occurring in late December.The annual ER in 2018 was 678 g C m-2 and respiration during the non-growing season accounted for 13%of the annual sum.Nonlinear regression revealed that soil temperature at 5 cm depth and soil water content(SwC)were the main factors controlling the seasonal variation in ER.The diurnal variation in ER was mainly controlled by air temperature and solar radiation.Higher temperature sensitivity(Qio)occurred under conditions of lower soil temperatures and medium SWC(25%≤SWC≤40%).The present study deepens our understanding of CO,emissions in alpine wetland ecosystems and helps evaluate the carbon budget in alpine wetlands in arid regions.展开更多
基金financially supported by the Strategic Priority Research Program of Chinese Academy of Sciences (Grant No.XDB40010000)the National Natural Science Foundation of China (Grant Nos.41907288,41673119,and 41773140)+1 种基金the Science and Technology Foundation of Guizhou Province (Grant Nos.[2019]1317 and [2020]1Y193)supported by the“Light of West China”Program and the CAS Scholarship。
文摘Isotopic signature is a powerful tool to discriminate methane(CH_(4)) source types and constrain regional and global scale CH_(4) budgets.Peatlands on the Qinghai-Tibetan Plateau are poorly understood about the isotopic signature of CH_(4) due to the limited experimental conditions.In this study,three campaigns of diurnal air samples spacing 2-3 h were taken from an alpine peatland on the eastern Qinghai-Tibetan Plateau to investigate its source signal characteristics.Both CH_(4) concentration and its stable carbon isotope(δ^(13)C-CH_(4)) were measured to derive the carbon isotopic signature of the CH_(4) source using the Keeling plot technique.Diurnal variation patterns in CH_(4) concentration and δ^(13)C-CH_(4) were observed during summertime,with depleted δ^(13)C-CH_(4) signals and high CH_(4) concentration appearing at nighttime.The δ^(13)C-CH4 signature during summer was calculated to be-71 % ± 1.3%,which falls within the range of other wetland studies and close to high-latitude peatlands.The boundary layer dynamic and CH_(4) source were supposed to influence the measured CH_(4) concentration and δ^(13)C-CH_(4.)Further investigations of CH_(4) isotopic signals into the nongrowing season are still needed to constrain the δ^(13)C-CH_(4) signature and its environmental controls in this region.
基金the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB40010300)the National Natural Science Foundation of China(41907288,41673119 and 41773140)+1 种基金the Science and Technology Foundation of Guizhou Province([2019]1317 and[2020]1Y193)the Opening Fund of the State KeyLaboratoryof Environmental Geochemistry(SKLEG2021214).
文摘Wetlands store large amounts of carbon stocks and are essential in both global carbon cycling and regional ecosystem services.Understanding the dynamics of wetland carbon exchange is crucial for assessing carbon budgets and predicting their future evolution.Although many studies have been conducted on the effects of climate change on the ecosystem carbon cycle,little is known regarding carbon emissions from the alpine wetlands in arid northwest China.In this study,we used an automatic chamber system(LI-8100A)to measure ecosystem respiration(ER)in the Bayinbuluk alpine wetland in northwest China.The ER showed a significant bimodal diurnal variation,with peak values appearing at 16:30 and 23:30(Beijing time,UTC+8).A clear seasonal pattern in ER was observed,with the highest value(19.38μmol m-2 s-l)occurring in August and the lowest value(0.11μmol m-2 s-1)occurring in late December.The annual ER in 2018 was 678 g C m-2 and respiration during the non-growing season accounted for 13%of the annual sum.Nonlinear regression revealed that soil temperature at 5 cm depth and soil water content(SwC)were the main factors controlling the seasonal variation in ER.The diurnal variation in ER was mainly controlled by air temperature and solar radiation.Higher temperature sensitivity(Qio)occurred under conditions of lower soil temperatures and medium SWC(25%≤SWC≤40%).The present study deepens our understanding of CO,emissions in alpine wetland ecosystems and helps evaluate the carbon budget in alpine wetlands in arid regions.
