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Low-Temperature Acid Weathering in Newhaven, Sussex, United Kingdom, and Its Application to Theoretical Modeling in Radioactive Waste-Disposal Sites

Published online by Cambridge University Press:  28 February 2024

Thierry De Putter ,
Alain Bernard ,
Alain Perruchot ,
Dominique Nicaise  and
Christian Dupuis
Thierry De Putter
Affiliation:
Faculté Polytechnique de Mons, Géologie Fondamentale et Appliquée, 9 rue de Houdain, B-7000 Mons, Belgium
Alain Bernard
Affiliation:
Université Libre de Bruxelles, Géochimie et Minéralogie, CP 160/02, 50, av. F. Roosevelt, B-1050 Bruxelles, Belgium
Alain Perruchot
Affiliation:
Université de Paris-Sud, Géochimie des Roches Sédimentaires, UMR-CNRS 8616, bâtiment 504, F-91405 Orsay cedex, France
Dominique Nicaise
Affiliation:
Faculté Polytechnique de Mons, Géologie Fondamentale et Appliquée, 9 rue de Houdain, B-7000 Mons, Belgium
Christian Dupuis
Affiliation:
Faculté Polytechnique de Mons, Géologie Fondamentale et Appliquée, 9 rue de Houdain, B-7000 Mons, Belgium
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Abstract

Tertiary weathered sediments located immediately to the west of the harbor at Newhaven, Sussex, UK, were investigated by examination of major and trace elements by scanning electron microscope (SEM), microprobe, and inductively coupled plasma mass spectrometer (ICP-MS), and the mineralogy was studied by optical petrography, X-ray diffraction (XRD), transmission electron microscope (TEM), selective leaching, and thermodynamic modeling. Studied outcrops experienced acid leaching by sulfuric acid percolating downward through Tertiary sediments overlying Cretaceous chalk. The progressive neutralization of the percolating acid fluids resulted in “sequentially” layered neoformation of minerals: jarosite, iron oxides, aluminous minerals (sulfates, oxyhydroxides), gypsum, and Fe-Mn oxides. Substantial agreement was found between field observations and mineral assemblages obtained by modeling with the program CHILLER. These results suggest that the initial assumptions on the weathering process and mechanisms are correct. The relevance and implications of this study in the modeling of future denudation and weathering processes of radioactive waste-disposal sites (both deeply buried sites for high-leveI waste and surface sites for low-level waste) are discussed. Neoformed phases, such as jarosite, aluminous minerals, and silico-aluminous gels may play a significant role in the efficient trapping of mobilized pollutant radionuclides.

Keywords

Acid WeatheringAluminous MineralsJarositeRadioactive-Waste SitesSilico-Aluminous GelsThermodynamic Modeling
Type
Research Article
Information
Clays and Clay Minerals , Volume 48 , Issue 2 , April 2000 , pp. 238 - 245
Copyright
Copyright © 2000, The Clay Minerals Society

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