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机构地区:[1]新疆大学地理学科博士后流动站,新疆乌鲁木齐830046 [2]乌鲁木齐市天山区人民政府,新疆乌鲁木齐830002 [3]乌鲁木齐市环境监测中心站,新疆乌鲁木齐830044
出 处:《新疆大学学报(自然科学版)》2011年第3期278-282,共5页Journal of Xinjiang University(Natural Science Edition)
基 金:教育部重大创新资金培育项目(708090)
摘 要:通过对乌鲁木齐市近12年(1997-2009)降水数据的月平均值分析,得出阴离子浓度在采暖期高于非采暖期.(SO42+NO3)/(Ca2++NH+4)比值在1.67~3.87之间,SO42和Ca2+分别是阴离子和阳离子中比重最大的离子,分别达到82.02%和61.93%,其比重变化直接影响着大气降水中的离子组分比例.SO42浓度随季节变化明显且幅度较大,Ca2+虽有变化但幅度较小.∑阴离子占总离子的百分比约是∑阳离子占总离子的1.6~3.3倍之间,煤炭消耗造成SO42离子大量存在,同时大量Ca2+离子的存在是保证乌鲁木齐市大气降水中阴阳离子平衡的前提.阴、阳离子占总离子比重呈双曲线对称管道形.We analysis the monthly average precipitation data between 1997--2009 in Urumqi. We find that during heating period (October- March) concentration of anions was higher than non-heating period. (SO4 2-+NO3)/(Ca2++NH+) ratio was about 1.67-3.87. The proportion of SO4 2- and Ca2+in anion and cation are maximum, they reached 82.02% and 61.93% respectively. They influence the property of precipitation chemical directly. SO4 2- concentration changes according to the season and its amplitude was large. The percentage of total anion was almost 1.6-3.3 times of total cation. Ca2+also changes but its amplitude is small. Coal consumption produces more SO4 2- ,but it roughly balanced by Ca2+.The percentage of anion and cation in total ion appears hyperbola symmetry duct.
分 类 号:X131.1[环境科学与工程—环境科学]
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