
Professor Fiona Whitaker
B.Sc., Ph.D.(Bristol)
Expertise
My research group studies interactions between biogeochemistry, hydrogeology and water-rock interaction in aquifers and reservoirs, with a particular focus on carbonate systems, by coupling fieldwork with process-based modelling.
Current positions
Professor of Earth Sciences
School of Earth Sciences
Contact
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Research interests
My research focuses on carbonate sedimentology and diagenesis, integrating field studies of modern environments with numerical modeling, to provide a holistic understanding of the evolution of porosity-permeability in carbonate sediments from birth to burial. My work has included application of these techniques to understanding restless volcanic systems and CO2 sequestration in reservoirs and aquifers. Recently I have focussed on understanding the impact of climate and land-use change on the hydrology of coastal and island aquifers.
Field studies in the Bahamas, Yucatan and Guam include aqueous biogeochemistry, hydrological monitoring and aquifer characterization, and enable quantification of key processes and evaluation of fundamental controls on hydrology, geochemistry and water-rock interaction, with application to hydrogeophysics.
Modeling approaches include hydrological, geochemical and reaction transport modeling (RTM). The latter, an emerging technology which simulates geochemical reactions in systems open to fluid flow, is providing exciting new insights into a range of rock-water interaction systems. Field and modeling studies have informed development an innovative model for prediction of coupled sedimentological and early diagenetic evolution of carbonate platforms (CARB3D+).
Projects and supervisions
Research projects
Hypogene karst: genesis and implications to optimisation of low enthalpy energy resources
Principal Investigator
Managing organisational unit
School of Earth SciencesDates
01/06/2022 to 30/11/2024
Integrated Reaction Transport Modelling of Dolomite Evolution
Principal Investigator
Description
Two basic styles of replacement dolomitisation occur; diffuse dolomites formed at relatively cool temperature and high-temperature dolomites generally related to fractures. The former (which may also be fracture guided) are…Managing organisational unit
School of Earth SciencesDates
01/04/2012 to 31/07/2014
Quantifying and Monitoring Potential Ecosystem Impacts of Geological Carbon Storage (QICS)
Principal Investigator
Managing organisational unit
School of Earth SciencesDates
01/04/2010 to 01/04/2013
Thesis supervisions
The geochemistry and geomicrobiology of a salinity-stratified coastal carbonate aquifer : Yucatan Peninsula, Mexico
Supervisors
Insight into fault-controlled hydrothermal dolomitization using reactive transport modelling
Supervisors
Facies, diagenesis and cycles within the pre-salt deposits from Barra Velha Formation, Santos Basin, offshore Brazil
Supervisors
Water – Rock Interaction in the Eocene and Upper Paleocene Formations, State of Qatar
Supervisors
Physical and biogeochemical drivers of Modern carbonate diagenesis in intertidal sediments of Abu Dhabi
Supervisors
Geochemical modelling of dolomitization
Supervisors
Origin and Early Diagenesis of Evaporites in a Coastal Sab-kha
Supervisors
Hydrochemistry and Environmental isotopes in a mixed carbonate-evaporite system aquifer, Qatar
Supervisors
Publications
Recent publications
15/05/2025Zebra textures in fault-controlled, hydrothermal dolomite bodies
Earth and Planetary Science Letters
Dolomitisation of carbonate platform margins by fault‐controlled geothermal convection
The Depositional Record
Rare preservation of Triassic pedorelicts with biogenic traces from a hot semi-arid upland palaeoenvironment at Portishead, SW England
Proceedings of the Geologists' Association
Solubility product constants for natural dolomite (0–200 °C) through a groundwater-based approach using the USGS produced water database
American Journal of Science
The creation of calcite microcrystals and microporosity through deep burial basinal flow processes driven by plate margin obduction – A realistic model?
Marine and Petroleum Geology