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作 者:顾慰祖[1] 陆家驹[1] 陈廷扬[2] 徐其高[2] Norman E.Peters
机构地区:[1]南京水利科学研究院 [2]南京大学物理系,江苏南京210093 [3]U.S.Geological Survey,atlantaga30360
出 处:《水科学进展》2003年第5期535-541,共7页Advances in Water Science
基 金:水利部水利科学基金资助项目;美国USGS资助项目~~
摘 要:对同期降水、江河水和地下水的元素组成,使用中子活化分析方法作了对比试验。降水取自分布于8个气候带的11个站,其海拔高程为5~3659m,年平均降水量为50~1571mm。河水取自各主要江河包括内陆河和海岛的12个测站以及3个实验流域,并在其附近采集地下水。降水中共检出35种元素,各站有19~31种元素,同期均有空间分布。河水中共检出39种元素,各河分别有21~31种元素。地下水中共检出35种元素,各站有30~32种元素。对其浓度组成作了由大于1000μg/L至小于0 01μg/L的分级综合。有些元素含量超出所报道的世界淡水浓度范围,小于其最低值,甚或远大于其最高值。The element composition of natural waters including rainfall, river water and groundwater are tested by neutron activation analyses The rainfall is sampled from 11 stations distributed in all main climate zones of this country with altitude from 5 m ASL to 3?659 m ASL, annual mean precipitation from 50 mm to 1?571 mm The river water are sampled from 12 hydrometric stations of the main rivers of China, including inland rivers, island river and brooks of 3 representative catchments The natural waters are sampled simultaneously 35 elements in rainfall, 39 elements in river water and groundwater are found Concentration of elements are grouped with level greater than 1?000 μg/L to that less than 001 μg/L Many elements are found to be beyond the range of world fresh water concentration reported by Bowen i.e., several elements much higher or lower than Bowen values
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