IMHE OpenIR  > 山地表生过程与生态调控重点实验室
applicationandverificationofsimultaneousdeterminationofcellulose13cand18oinpiceashrenkianatreeringsfromnorthwesternchinausingthehightemperaturepyrolysismethod
Xu Guobao1; Liu Xiaohong1; Sun Weizhen1; Chen Tuo1; Zhang Xuanwen1; Zeng Xiaomin2; Wu Guoju1; Wang Wenzhi3; Qin Dahe1
2018
Source Publication干旱区科学英文版
ISSN1674-6767
Volume010Issue:006Pages:864
AbstractStable isotopes in tree-ring cellulose provide important data in ecological,archaeological,and paleoenvironmental researches,thereby,the demand for stable isotope analyses is increasing rapidly.Simultaneous measurement of cellulose δ^13C and δ^18O values from tree rings would reduce the cost of isotopic commodities and improve the analytical efficiency compared with conventional separate measurement.In this study,we compared the δ^13C and δ^18O values of tree-ringα-cellulose from Tianshan spruce(Picea schrenkiana)in an arid site in the drainage basin of the Urumqi River in Xinjiang of northwestern China based on separate and simultaneous measurements,using the combustion method(at 1050°C)and the high-temperature pyrolysis method(at 1350°C and 1400°C).We verified the results of simultaneous measurement using the outputs from separate measurement and found that both methods(separate and simultaneous)produced similar δ^13C values.The two-point calibrated method improved the results(range and variation)of δ^13C and δ^18O values.The mean values,standard deviations,and trends of the tree-ring δ^13C obtained by the combustion method were similar to those by the pyrolysis method followed by two-point calibration.The simultaneously measured δ^18O from the pyrolysis method at 1400°C had a nearly constant offset with that the pyrolysis method at 1350°C due to isotopic-dependence on the reaction temperature.However,they showed similar variations in the time series.The climate responses inferred from simultaneously and separately measured δ^13C and δ^18O did not differ between the two methods.The tree-ring δ^13C and δ^18O values were negatively correlated with standardized precipitation evapotranspiration index from May to August.In addition,the δ^18O was significantly correlated with temperature(positive),precipitation(negative),and relative humidity(negative)from May to August.The tree-ring δ^13C and δ^18O values determined simultaneously through the high-temperature pyrolysis method could produce acceptable and reliable stable isotope series.The simultaneous isotopic measurement can greatly reduce the cost and time requirement compared with the separate isotopic measurement.These results are consistent with the previous studies at humid sites,suggesting that the simultaneous determination of δ^13C and δ^18O in tree-ringα-cellulose can be used in wide regions.
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/31507
Collection山地表生过程与生态调控重点实验室
Affiliation1.中国科学院
2.陕西师范大学
3.中国科学院成都山地灾害与环境研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
Xu Guobao,Liu Xiaohong,Sun Weizhen,et al. applicationandverificationofsimultaneousdeterminationofcellulose13cand18oinpiceashrenkianatreeringsfromnorthwesternchinausingthehightemperaturepyrolysismethod[J]. 干旱区科学英文版,2018,010(006):864.
APA Xu Guobao.,Liu Xiaohong.,Sun Weizhen.,Chen Tuo.,Zhang Xuanwen.,...&Qin Dahe.(2018).applicationandverificationofsimultaneousdeterminationofcellulose13cand18oinpiceashrenkianatreeringsfromnorthwesternchinausingthehightemperaturepyrolysismethod.干旱区科学英文版,010(006),864.
MLA Xu Guobao,et al."applicationandverificationofsimultaneousdeterminationofcellulose13cand18oinpiceashrenkianatreeringsfromnorthwesternchinausingthehightemperaturepyrolysismethod".干旱区科学英文版 010.006(2018):864.
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