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石羊河流域多水体酸根离子特征及影响因素
引用本文:朱国锋,潘汉雄,张昱,何元庆,郭慧文,杨玲,杨建霞,马惠莹,黄美华,向鹃.石羊河流域多水体酸根离子特征及影响因素[J].中国环境科学,2018,38(5):1886-1892.
作者姓名:朱国锋  潘汉雄  张昱  何元庆  郭慧文  杨玲  杨建霞  马惠莹  黄美华  向鹃
作者单位:1. 西北师范大学地理与环境科学学院, 甘肃 兰州 730000;2. 中国科学院西北生态环境资源研究院, 冰冻圈科学国家重点实验室, 甘肃 兰州 730000
基金项目:国家自然科学基金资助项目(41661005);国家自然科学基金委员会创新研究群体科学基金(41421061);冰冻圈科学国家重点实验室自主课题(SKLCS-ZZ-2017)
摘    要:2014年7月~2015年6月在石羊河流域采集降水、地表水及地下水样品,使用离子色谱仪分析获取样品主要酸根离子含量,研究石羊河流域不同水体酸根离子特征、季节分异及其影响因素.结果显示:石羊河流域不同水体均呈弱碱性,酸根离子组成以SO42-和HCO3-为优势离子,分别占酸根离子总量的38.68%和33.49%;不同季节水体酸根离子浓度差别较大,春季水体中酸根离子浓度最高,夏季最低,地下水季节变异小于地表水;地表水和地下水的酸根离子浓度都呈现出从上游到下游递增的规律,地表水酸根离子浓度大大低于地下水.碳酸盐的风化及蒸发岩溶解是酸根离子的主要来源,人类活动对石羊河流域水体已造成轻度污染.

关 键 词:石羊河流域  酸根离子  不同水体  离子来源  
收稿时间:2017-09-28

Hydrochemical characteristics and control factors of acid anion in Shiyang River Basin
ZHU Guo-feng,PAN Han-xiong,ZHANG Yu,HE Yuan-qing,GUO Hui-wen,YANG Ling,YANG Jian-xia,MA Hui-ying,HUANG Mei-hua,XIANG Juan.Hydrochemical characteristics and control factors of acid anion in Shiyang River Basin[J].China Environmental Science,2018,38(5):1886-1892.
Authors:ZHU Guo-feng  PAN Han-xiong  ZHANG Yu  HE Yuan-qing  GUO Hui-wen  YANG Ling  YANG Jian-xia  MA Hui-ying  HUANG Mei-hua  XIANG Juan
Institution:1. College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China;2. State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730070, China
Abstract:From July 2014 to June 2015, precipitation, surface water and groundwater samples were collected in Shiyang River Basin. The main acid ion contents in the samples were analyzed by ion chromatograph. The characteristics of acid ions in different water bodies of Shiyang River basin, seasonal differentiation and its influencing factors were studied. The results shown that all water samples were mildly alkaline and the acid radical ions consisted of SO42- and HCO3- as dominant ions, which accounted for 38.68% and 33.49% of total anion, respectively. Obvious variations have been perceived during different seasons, which the highest anion content was in spring and the lowest value in summer. Seasonal variation of groundwater was smaller than that of surface water. The concentration of acid root ion in surface water is much lower than that of groundwater. The weathering of carbonate and the dissolution of evaporite were the main sources of acid ion. In addition, the human activities have caused mild pollution to the water body of the Shiyang River Basin.
Keywords:Shiyang River Basin  acid anion  hydrochemical characteristics  anion sources  
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