首页 | 本学科首页   官方微博 | 高级检索  
     检索      

阿拉善沙漠高原降水化学特征与离子来源判别
引用本文:陈堂清,饶文波,金可,郑芳文,张文兵,王帅,王雅宁.阿拉善沙漠高原降水化学特征与离子来源判别[J].环境科学研究,2018,31(12):2083-2093.
作者姓名:陈堂清  饶文波  金可  郑芳文  张文兵  王帅  王雅宁
作者单位:河海大学地球科学与工程学院, 江苏 南京 210098
基金项目:国家自然科学基金项目(No.41273015)
摘    要:为查明我国北方沙漠地区降水化学组成及来源,在阿拉善沙漠高原阿右旗气象站采集了2013—2015年的降水样品,测定了降水pH、EC(电导率)及主要离子当量浓度.结果表明:阿拉善沙漠阿右旗气象站降水pH和EC的范围分别为6.66~8.05和35~1 237 μS/cm;Ca2+、SO42-、Na+和Cl-为降水中的主要离子,其总和占总离子的85%以上.降水pH、EC和主要离子当量浓度是反映空气质量的基本参数,较高的降水pH反映出当地降水具有明显的碱性特征.与其他地区相比,该地区降水的EC和可溶性离子日均湿沉降通量也较高,且随月份有较大的变化,表明干旱沙漠粉尘对当地降水水化学的贡献较大.根据离子来源相对贡献的计算结果发现,降水中92.8%的SO42-和98%的NO3-来自人为源,98.8%的Ca2+和88.7%的K+为陆地来源,55%的Mg2+为海洋源,24.8%的Na+来自矿物风化,极少部分Cl-为人为源.研究显示:除降水中的NH4+外,其他主要离子之间的相关性表明各种成因物质在风力作用下同时进入了大气;基于NH4+](NH4+的当量浓度)与K+](K+的当量浓度)相关性分析,降水中的NH4+来自生物质燃烧、肥料使用、动物粪便等. 

关 键 词:降水化学    离子来源    沉降通量    人为污染    沙漠高原
收稿时间:2018/2/2 0:00:00
修稿时间:2018/8/22 0:00:00

Chemical Characteristics and Major Ion Sources of Precipitation in the Alxa Desert Plateau
CHEN Tangqing,RAO Wenbo,JIN Ke,ZHENG Fangwen,ZHANG Wenbing,WANG Shuai and WANG Yaning.Chemical Characteristics and Major Ion Sources of Precipitation in the Alxa Desert Plateau[J].Research of Environmental Sciences,2018,31(12):2083-2093.
Authors:CHEN Tangqing  RAO Wenbo  JIN Ke  ZHENG Fangwen  ZHANG Wenbing  WANG Shuai and WANG Yaning
Institution:College of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China
Abstract:In order to determine the chemical composition and source of precipitation in the desert areas of northern China, precipitation samples collected at the Ayouqi weather station in the Alxa Desert Plateau during 2013-2015 were analyzed for pH, EC (electrical conductivity), and the major ion concentrations. The results show that the pH and EC values of precipitation vary from 6.66 to 8.05 and from 35 to 1237 μS/cm, respectively. Ca2+, SO42-, Na+ and Cl- are the dominant in precipitation, accounting for more than 85% of the total ion concentration. The pH, EC values and the major ions are the basic parameters of air quality. The high pH values reflect the alkaline characteristics of local precipitation. The EC values and wet deposition fluxes in the Alxa Desert Plateau are higher than that in other places and vary with months. These results show that mineral dust from arid deserts contributes greatly to the chemistry of local precipitation. According to the calculations of the ion source contributions, 92.8% SO42- and 98% NO3- in precipitation were from the anthropogenic pollution, 98.8% Ca2+ and 88.7% K+ originated from the terrestrial sources, 55% Mg2+ was of marine origin, 24.8% Na+ came from mineral weathering and a tiny part of Cl- was related to the anthropogenic input. The overall results suggest that the good correlations among the major ions, except NH4+, in the precipitation, indicating that various types of materials were synchronously carried into the atmosphere by wind. The good correlation of NH4+ with K+ in the precipitation indicated that NH4+ probably resulted from biomass burning, fertilizer usage, animal manure and so on. 
Keywords:precipitation chemistry  ion sources  deposition fluxes  anthropogenic pollution  desert plateau
本文献已被 CNKI 等数据库收录!
点击此处可从《环境科学研究》浏览原始摘要信息
点击此处可从《环境科学研究》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号