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石家庄地区大气降水氢氧同位素特征分析

2017-06-05朱艺文张福平王虎威刘筱

山东农业科学 2017年5期

朱艺文+张福平+王虎威+刘筱

摘要:研究大气降水中氢氧同位素的特征能够揭示水循环规律。依据全球氢氧稳定同位素监测网(GNIP)提供的大氣降水稳定同位素资料,选择石家庄地区1985―2003年的资料数据,结合气象资料和水汽来源,分析了石家庄地区大气降水氢氧同位素的特征及变化规律,并建立了局地大气降水线方程。结果表明:石家庄地区大气降水的18O春季最为富集,冬季最为贫化,夏秋两季相近;局地大气降水线方程为δD=6.39δ18O-3.75,斜率和截距明显小于全球和中国大气降水线方程,反映该地区偏干旱的气候特征;年尺度上,石家庄地区大气降水δ18O和δD具有一定的温度效应,但降雨量效应极为微弱,只在春夏季较为显著,表明该地区降水同位素受温度的影响作用更大。

关键词:大气降水;氢氧同位素;大气降水线;同位素效应;石家庄

中图分类号:S161.6文献标识号:A文章编号:1001-4942(2017)05-0116-08

Analysis on Characteristics of Stable Hydrogen and

Oxygen Isotopes in Precipitation in Shijiazhuang

Zhu Yiwen, Zhang Fuping, Wang Huwei, Liu Xiao

(College of Tourism and Environment, Shaanxi Normal University, Xian 710062, China)

AbstractThe study on characteristics of hydrogen and oxygen isotopes in precipitation can reveal the regularity of water cycle. Based on the GNIP data, choosing the data of Shijiazhuang area from 1985 to 2003,combined with the meteorological data and the source of water, the characteristics and change regularity of atmospheric precipitation hydrogen and oxygen isotopes were analyzed and the local meteoric water line was established. The results showed that the 18O value of precipitation was the highest in spring, the lowest in winter, and the values in summer and autumn were close. The equation of local meteoric water line was δD=6.39δ18O-3.75. The smaller slope and intercept compared with the global and national atmospheric precipitation reflected its arid climate characteristics. The δ18O and δD of atmospheric precipitation in study area had certain temperature effect,but the precipitation effect was very weak, which was only significant in spring and summer.It indicated that temperature had more effects on precipitation isotopes in this area.

KeywordsPrecipitation;Hydrogen and oxygen isotope;Meteoric water line;Isotope effects;Shijiazhuang

稳定同位素18O和2H(氘,符号D)作为自然界水体中的天然示踪剂,能够敏感地记录水体信息,响应环境变化。大气降水作为水体循环的重要环节,是连接大气圈层和陆地圈层的纽带,其同位素的变化也影响着整个水文循环过程同位素的变化[1]。同位素的分馏作用贯穿于所有的大气降水过程中,氢氧同位素的组分比率也常发生改变。降雨的水汽来源、运移过程、大气环流及当地的气候环境往往是影响同位素组成变化的重要因素[2-4]。因此,大气降水的同位素变化特征不仅能够很好地反演大气过程,追溯水汽来源,反映全球与区域的气候特征[5-7],也能够反映大气水汽循环的整个历史[8],有助于深入了解地球化学和水循环过程。……

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