Methods for the integration, modelling and presentation of high-resolutionregional hydrochemical baseline survey data

Citation
B. Smith et al., Methods for the integration, modelling and presentation of high-resolutionregional hydrochemical baseline survey data, J GEOCHEM E, 64(1-3), 1998, pp. 67-82
Citations number
18
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF GEOCHEMICAL EXPLORATION
ISSN journal
03756742 → ACNP
Volume
64
Issue
1-3
Year of publication
1998
Pages
67 - 82
Database
ISI
SICI code
0375-6742(199811)64:1-3<67:MFTIMA>2.0.ZU;2-N
Abstract
The completion of the high-resolution (ca. 1 sample per 1.5 km(2)) geochemi cal survey of Wales and part of the West Midlands by the British Geological Survey has created a unique data set containing over 13,500 site-specific hydrochemical and stream-sediment analyses for a typical suite of over 21 m ajor and trace components. The collection of such a wide range of data over an area with contrasting geology, soils, geomorphology and land use has en abled the delineation and study of hydrochemical processes on a regional ba sis. Methods are presented describing transformations performed from basic concentration-based data (pH, conductivity and 21 major and trace elements) into hydrochemically relevant trilinear and solubility diagrams predicting aqueous speciation and ionic domination. These data are then displayed and interpreted using a series of thematic composites. The utility of coupling speciation diagrams, based upon pure ideal systems, with Geographical Info rmation Systems for describing processes controlling hydrogeochemical evolu tion at a regional scale is described. The validity of using solubility dia grams to describe large regional hydrochemical data sets is tested using ge ographically linked representations of aqueous saturation and chemical spec iation generated from the individual modelling of each sample using PHREEQC . Comparison of the pure and real (PHREEQC) systems for calcite and gypsum indicated that there was a small over-prediction in the pure system; the gr eatest differences occurred in samples of the highest ionic strength. (C) 1 998 The Natural Environment Research Council.