Utilization of boron as a critical parameter in water quality evaluation: implications for thermal and mineral water resources in SW Germany and N Switzerland

被引:20
作者
Barth, SR [1 ]
机构
[1] Univ Tubingen, Inst Geol & Palaontol, D-72076 Tubingen, Germany
来源
ENVIRONMENTAL GEOLOGY | 2000年 / 40卷 / 1-2期
关键词
boron; boron isotope geochemistry; thermal and mineral water; water quality evaluation;
D O I
10.1007/s002540000155
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In order to investigate the application of the elemental abundance of boron and its stable isotopes, B-10 and B-11, for tracing anthropogenic contamination of variably mineralized thermal and mineral waters, B concentrations and isotopic compositions (delta B-11) were determined for sample pairs collected during surveys in 1984-1986 and 1995 from representative wells discharging water from deep crustal reservoirs within the central European crystalline basement and sedimentary cover (SW Germany and N Switzerland). The data presented show that natural temporal variations in the total B contents of thermal and mineral waters are a common feature, which makes it difficult to recognize admixture of extraneous (anthropogenic) components from B concentrations alone. Delineation of the natural versus anthropogenic origin of solutes and quantification of the relative mixing proportions may thus benefit considerably from the utilization of boron isotypes as an additional parameter. Hypothetical mixing scenarios involving various thermal waters and municipal wastewater effluents form the study area, with the latter being characterized by conspicuously light boron isotopic compositions, reveal that, in certain cases, delta B-11 values provide a superior diagnostic tool for detection of objectionable substances derived from the discharge of man-made boron products.
引用
收藏
页码:73 / 89
页数:17
相关论文
共 59 条
[31]  
LeBlanc DR, 1984, 2218 US GEOL SURV WA
[32]  
Leeman WP, 1996, REV MINERAL, V33, P645
[33]   Utilization of intrinsic boron isotopes as co-migrating tracers for identifying potential nitrate contamination sources [J].
Leenhouts, JM ;
Bassett, RL ;
Maddock, T .
GROUND WATER, 1998, 36 (02) :240-250
[34]   TRACING GROUNDWATER COMPONENTS BY CHEMICAL, ISOTOPIC AND PHYSICAL PARAMETERS EXAMPLE - SCHINZNACH, SWITZERLAND [J].
MAZOR, E ;
VUATAZ, FD ;
JAFFE, FC .
JOURNAL OF HYDROLOGY, 1985, 76 (3-4) :233-246
[35]  
MCMULLEN CC, 1961, GEOCHIM COSMOCHIM AC, V23, P147
[36]  
Michel G, 1997, LEHRBUCH HYDROGEOLOG, V7
[37]   BORON ISOTOPIC COMPOSITIONS OF SOME BORON MINERALS [J].
OI, T ;
NOMURA, M ;
MUSASHI, M ;
OSSAKA, T ;
OKAMOTO, M ;
KAKIHANA, H .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (12) :3189-3195
[38]   THE BORON ISOTOPE GEOCHEMISTRY OF THE KIRKA BORATE DEPOSIT, WESTERN TURKEY [J].
PALMER, MR ;
HELVACI, C .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (17) :3599-3605
[39]  
Palmer MR, 1996, REV MINERAL, V33, P709
[40]   TEMPERATURE AND PH CONTROLS OVER ISOTOPIC FRACTIONATION DURING ADSORPTION OF BORON ON MARINE CLAY [J].
PALMER, MR ;
SPIVACK, AJ ;
EDMOND, JM .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1987, 51 (09) :2319-2323