Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Mineralogical Magazine Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Mineralogical Magazine; December 2003; v. 67; no. 6; p. 1157-1170; DOI: 10.1180/0026461036760155
© 2003 Mineralogical Society of Great Britain and Ireland
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (10)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hutchens, E.
Right arrow Articles by McLean, J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The role of heterotrophic bacteria in feldspar dissolution — an experimental approach

E. Hutchens1,2, E. Valsami-Jones1,*, S. McEldowney2, W. Gaze3 and J. McLean4

1 Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK
2 School of Biosciences, The University of Westminster, 115 New Cavendish Street, London W1M 8JS, UK
3 Department of Biological Sciences, University of Warwick, Coventry CV4 7AL, UK
4 Arcadis Geraghty & Miller International, Inc., 2 Craven Court, Newmarket CB8 7FA, UK

* E-mail: E.Valsami-Jones{at}nhm.ac.uk

This paper presents the results of a laboratory study on the influence of heterotrophic bacteria on dissolution of a silicate mineral (K-feldspar) under a variety of growth conditions. Twenty seven strains of heterotrophic bacteria were isolated from a feldspar-rich soil (Shap, NW England). Liquid and solid minimal aerobic media (C/N-sufficient, K-limited, Fe-limited, N-limited and glucose/NH4Cl only) at 26°C were used for isolation of the bacteria. The media selected bacterial isolates that were fast-growing aerobic heterotrophs able to use glucose as the sole source of carbon and energy. The extent of mineral dissolution (in the presence of the isolates) was assessed after 48 h of incubation by measuring the release of Al from the K-feldspar by ICP-AES. More detailed dissolution experiments were carried out with one of the strains, Serratia marcescens, an isolate that was very effective in enhancing feldspar dissolution. The main conclusions of this study are: (1) the degree of enhancement of K-feldspar dissolution varied with bacterial isolate and growth conditions; (2) enhancement of dissolution began during stationary phase growth; (3) the production of chelating compounds (exopolymers, siderophores, pigments) during the stationary phase might be a possible mechanism for bacterially enhanced K-feldspar dissolution; (4) the frequent sub-culturing of isolates can have a significant effect on their physiological characteristics and may possibly influence their capacity to enhance mineral dissolution.

KEYWORDS: K-feldspar, dissolution, heterotrophic bacteria, Serratia marcescens




This article has been cited by other articles:


Home page
Mineral MagHome page
E. Valsami-Jones and D. A. C. Manning
Environmental Mineralogy: introduction to a thematic set of papers arising out of sessions held at IMA 2002, Edinburgh, UK
Mineralogical Magazine, December 1, 2003; 67(6): 1123 - 1125.
[Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of Great Britain and Ireland