Standard operating procedure for the analysis of major ions in hydrothermal fluids by ion chromatography.

Standard Operating Procedure aqueous geochemistry hydrothermal fluids ion chromatography major ions

Journal

Open research Europe
ISSN: 2732-5121
Titre abrégé: Open Res Eur
Pays: Belgium
ID NLM: 9918230081006676

Informations de publication

Date de publication:
2023
Historique:
accepted: 20 05 2024
medline: 12 9 2024
pubmed: 12 9 2024
entrez: 12 9 2024
Statut: epublish

Résumé

This standard operating procedure (SOP) describes an ion chromatography (IC) procedure for the major cations and anions in hydrothermal fluids. Hydrothermal fluids are aqueous solutions with a wide range of temperature, salinity, pH and ion species that can be used by microbial metabolism as electron donors and electron acceptors. Due to the high variability of the environmental physical-chemical parameters in these samples, we have developed this protocol taking into account the special features of the matrices analyzed. An Eco IC Metrohm system equipped with a conductivity detector was used. Calibration curves are linear in the 0.1 to 10 mg/L concentration range for cations Ca This manuscript details the standard operating procedure used for the determination of major cations and anions in hydrothermal fluids, which are characterized by a high variability of physico-chemical parameters. Due to the high variability of our samples, we customized the method to compensate for the variability on the physico-chemical parameters. The results are useful to interpret the geochemical processes and for understanding how these processes influence microbial diversity in geothermal systems.

Autres résumés

Type: plain-language-summary (eng)
This manuscript details the standard operating procedure used for the determination of major cations and anions in hydrothermal fluids, which are characterized by a high variability of physico-chemical parameters. Due to the high variability of our samples, we customized the method to compensate for the variability on the physico-chemical parameters. The results are useful to interpret the geochemical processes and for understanding how these processes influence microbial diversity in geothermal systems.

Identifiants

pubmed: 39263358
doi: 10.12688/openreseurope.15605.2
pmc: PMC11387938
doi:

Types de publication

Journal Article

Langues

eng

Pagination

94

Informations de copyright

Copyright: © 2024 Correggia M et al.

Déclaration de conflit d'intérêts

No competing interests were disclosed.

Auteurs

Monica Correggia (M)

Department of Biology, University of Naples Federico II, Naples, Italy.

Luciano Di Iorio (L)

Department of Biology, University of Naples Federico II, Naples, Italy.

Alessia Benedicta Bastianoni (AB)

Department of Biology, University of Naples Federico II, Naples, Italy.

Mustafa Yucel (M)

Institute of Marine Sciences, Middle East Technical University, Mersin, Turkey.

Angelina Cordone (A)

Department of Biology, University of Naples Federico II, Naples, Italy.

Donato Giovannelli (D)

Department of Biology, University of Naples Federico II, Naples, Italy.
Marine Chemistry & Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, USA.
Earth-Life Science Institute, ELSI, Tokyo Institute of Technology, Ookayama, Japan.
Department of Marine and Coastal Science, Rutgers University, New Brunswick, USA.
Istituto per le Risorse Biologiche e Biotecnologiche Marine, IRBIM, National Research Council, Italy, Ancona, Italy.

Classifications MeSH