The chemistry of Norwegian groundwaters: III. The distribution of trace elements in 476 crystalline bedrock groundwaters, as analysed by ICP-MS techniques

被引:118
作者
Frengstad, B [1 ]
Skrede, AKM
Banks, D
Krog, JR
Siewers, U
机构
[1] Norges Teknisk Naturvitenskapelige Univ, Inst Geol & Bergteknikk, N-7491 Trondheim, Norway
[2] Norges Geol Undersokelse, N-0304 Oslo, Norway
[3] Bundesanstalt Geowissensch & Rohstoffe, D-30631 Hannover, Germany
[4] Norges Geol Undersokelse, N-7491 Trondheim, Norway
关键词
groundwater; crystalline bedrock; trace elements; ICP-MS; drinking water; hydrochemistry;
D O I
10.1016/S0048-9697(99)00413-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Four hundred and seventy-six groundwater samples from boreholes in Nonwegian crystalline bedrock have been analysed by ICP-MS techniques. The results for 53 trace elements are presented as cumulative frequency distribution diagrams and are compared with relevant international drinking water norms. A range of trace elements appear to be enriched in granitic waters and depleted in anorthositic waters which is to be expected as generally granitic rocks are enriched in trace elements above those in anorthosites. A selection of elements which may be toxic in excess when present in drinking water are further discussed (Be, Tl, Th, U, Cd, Pb, As, Ni, and Hg). For uranium, 18% of the samples exceed the American maximum admissible concentration of 20 mu g/l; 7% of the samples fail to meet the Russian drinking water norms for beryllium of 0.2 mu g/l. For some parameters such as U, Be and Tl, no Norwegian drinking water regulations are set, while the American and the Russian norms differ significantly from each other. Between 0 and 1.5% of the wells exceed Nonwegian drinking water norms for each of the other selected elements. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:21 / 40
页数:20
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