ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
广西桂林凉风洞秋冬季滴水和沉积物氧同位素对极端降水的记录研究
  
关键词:extreme precipitation  drip water  sediments  hydrogen and oxygen isotopes
基金项目:国家自然科学基金项目(编号: 41501222; 41530316; 41701235);广西青年科学基金项目(编号: 2014GXNSFBA118227);中国地质调查局地质调查项目(编号: DD20160305)
作者单位E-mail
吴夏 中国地质科学院岩溶地质研究所, 国土资源部、广西岩溶动力学重点实验室
中国地质大学(北京) 
wuxia@karst.ac.cn 
潘谋成 中国地质科学院岩溶地质研究所, 国土资源部、广西岩溶动力学重点实验室  
曹建华 中国地质科学院岩溶地质研究所, 国土资源部、广西岩溶动力学重点实验室  
朱晓燕 中国地质科学院岩溶地质研究所, 国土资源部、广西岩溶动力学重点实验室  
张美良 中国地质科学院岩溶地质研究所, 国土资源部、广西岩溶动力学重点实验室  
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摘要:
The Effect of Extreme Precipitation on Stable Isotope Compositions of Drip Water and Sediments during Autumn and Winter at Liangfeng Cave in Guilin, Guangxi
      In recent years, extreme climate events have increased dramatically due to global environmental change. As environment information recording time is short, it is necessary to interpret extreme climate events in stalagmites. In this study, precipitation, drip water and sediments were monitored with high resolution from September 2017 to January 2018 in Liangfeng Cave, Guilin City, Guangxi. The precipitation samples were measured for δD and δ18O isotope values. The results indicate that δD and δ18O isotope compositions of precipitation have obvious positive variations caused by water vapor source in the study area. The local meteoric water line (LMWL) is δD = 8.8 δ18O + 16.38. The precipitation is the only source for Liangfeng cave, its oxygen isotope signals are reflected in the drip waters, and are recorded in the sediments. Nevertheless, cave drip waters may be mixed caused by precipitation which dropped in the old days before entering the cave and precipitation which dropped in the old days affected by evaporation effect through the epikarst. Therefore, δ18O values of drip water show more positive excursion than precipitation. However, δ18O of the sediment response time of extreme precipitation events are different due to the influence of different hydrogeochemical processes. Therefore, monitoring δ18O of drip water and sediment response process to environmental information can provide accurate interpreting paleoclimate information recorded by oxygen isotope in the stalagmite.
WU Xia,PAN Mou-cheng,CAO Jian-hua,ZHU Xiao-yan,ZHANG Mei-liang.2018.The Effect of Extreme Precipitation on Stable Isotope Compositions of Drip Water and Sediments during Autumn and Winter at Liangfeng Cave in Guilin, Guangxi[J].Acta Geoscientica Sinica,39(1):53-61.
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