欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2019, Vol. 30 ›› Issue (6): 1823-1832.doi: 10.13287/j.1001-9332.201906.009

• 稳定同位素生态学专栏 • 上一篇    下一篇

江苏高邮大气降水氢氧同位素特征及水汽来源

隋明浈1, 高德强1, 徐庆1,*, 何冬梅2, 王磊2, 王婷1   

  1. 1中国林业科学研究院森林生态环境与保护研究所, 国家林业和草原局森林生态环境重点实验室 北京 100091;
    2江苏省林业科学研究院, 南京 211153
  • 收稿日期:2018-11-16 出版日期:2019-06-15 发布日期:2019-06-15
  • 通讯作者: * E-mail: xuqing@caf.ac.cn
  • 作者简介:隋明浈,女,1991年生,博士研究生. 主要从事稳定同位素生态学研究. E-mail: cafsmz@163.com
  • 基金资助:
    林业公益性行业专项(201504423)和国家自然科学基金项目(31670720,31170661)资助

Characteristics of hydrogen and oxygen isotopes in precipitation and moisture sources in Gaoyou, Jiangsu Province, China

SUI Ming-zhen1, GAO De-qiang1, XU Qing1,*, HE Dong-mei2, WANG Lei2, WANG Ting1   

  1. 1Key Laboratory of Forest Ecology and Environment of the National Forestry and Grassland Administration, Reserch Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China;
    2Jiangsu Academy of Forestry, Nanjing 211153, China
  • Received:2018-11-16 Online:2019-06-15 Published:2019-06-15
  • Supported by:
    This work was supported by the Special Fund for Forest Scientific Research in the Public Welfare (201504423) and National Natural Science Foundation of China (31670720, 31170661)

摘要: 为了研究江苏高邮局地水循环特征,应对气候变化和减缓洪涝灾害.本研究采集江苏高邮自2015年7月—2017年10月的121个大气降水样品及环境因子数据,分析该区大气降水氢氧同位素特征,揭示不同季节水汽来源及影响因素.结果表明: 大气降水δD(δ18O)季节变化明显,冬半年偏正,夏半年偏负;过量氘值亦呈现冬高夏低;年尺度上,大气降水中δD(δ18O)与温度和降水量皆为负相关关系,呈现“反温度效应”和“降水量效应”;季节尺度上,均未呈现出“温度效应”,秋冬两季呈现出“降水量效应”;HYSPLIT气团轨迹模型结果进一步表明,江苏高邮夏季水汽主要来源于我国南海、印度洋及太平洋,而春、秋、冬季水汽主要来源于亚欧大陆、大西洋、北冰洋水汽混合及局地蒸发.大气降水δD(δ18O)值的季节变化主要受到季风活动以及厄尔尼诺-南方涛动(ENSO)的影响,降水中氢氧同位素值清晰地记录了厄尔尼诺向拉尼拉之间的过渡.

Abstract: It is necessary to examine the characteristics of hydrological cycle in Gaoyou area of Jiang-su Province in response to climate change and flood disasters. In this study, 121 atmospheric rain samples were collected and environmental factors were recorded from July 2015 to October 2017. We analyzed the hydrogen and oxygen stable isotopic composition of rain and identify moisture sources in this area. Results showed that the hydrogen and oxygen isotopic composition of rain had an seasonal variation, which was positive in the winter but negative in the summer. D-excess value was higher in winter than that in summer. On the annual scale, significantly negative relationships between δD (δ18O) and temperature and between δD (δ18O) and precipitation indicated the “anti-temperature effect” and “precipitation amount effect”, respectively. On the seasonal scale, there was no obvious “temperature effect” but “precipitation amount effect” in autumn and winter. Results from the HYSPLIT model showed that the precipitation in this area came mainly from ocean evaporation that was influenced by the Chinese South Sea, Indian Ocean and Pacific Ocean. Precipi-tation in other seasons mainly came from the water vapor mixture from the Eurasian continent, Atlantic Ocean, Arctic Ocean, as well as local evaporation. The seasonal pattern of δD and δ18O values in precipitation was mainly influenced by monsoon activity and El Niño-Southern Oscillation (ENSO). In addition, the precipitation isotopes clearly indicated the shift in climates from El Niño to La Niña.