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We have 51 Geochemistry PhD Projects, Programmes & Scholarships

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Geochemistry PhD Projects, Programmes & Scholarships

We have 51 Geochemistry PhD Projects, Programmes & Scholarships

An embarrassment of riches: reconciling our solar system’s platinum problem

Project Background. The Earth and Mars have too much platinum. This is also true of the rest of the platinum group elements (PGEs), osmium, iridium, ruthenium, rhodium and palladium, all of which are highly-siderophile elements (HSEs) that strongly partition into the metallic cores of planets during differentiation. Read more

Benchmarking major element isotopic compositions of chondritic meteorites

Project Background. Primitive, so-called chondritic, meteorites provide a key, compositional estimate of the proto solar nebula. Planets, that grew from this nebular disk, are expected to inherit its bulk composition and so any observed differences might be attributed to processes involved during their growth (e.g. Read more

PhD in Geographical and Earth Sciences - Paired meteorites: identical or nonidentical twins

Start Date. 01 October 2025. Aim: . The fundamental assumption underpinning the field of meteoritics is that all extraterrestrial rocks that are found in the same strewn field in the aftermath of a meteorite dropping fireball event are identical to each other. Read more

PhD in Geographical and Earth Sciences - The geological evolution of C-complex asteroids and their role in the origins of life on Earth

Start date. 01 October 2025. This project asks whether the terrestrial planets including Earth were made habitable by carbonaceous chondrite meteorites delivering bio-essential ingredients including water, organic compounds, nitrogen and phosphorus. . Read more

Autogenous diagenesis of limestone waste (FES-PhD-2425-01)

Diagenesis refers to the physical, chemical and biological processes that ‘turn’ sediments into rock (1,2). As sediments become buried by natural processes, they are subject to overburden pressure and raised temperatures, albeit lower than those that cause metamorphism (2,3). Read more

Tracking ocean circulation in the Cretaceous ‘Chalk Sea’

Ocean circulation is a fundamental component of the modern climate system but may have operated very differently in the geological past, especially when palaeogeography was different, climates were much warmer and sea-levels were considerably higher. Read more

Towards a holistic understanding of carbonate mineralisation controls

Calcium-carbonates (CaCO. 3. ) are climate-controlling minerals, acting as long-term sinks in the biogeochemical carbon cycle, and playing the role of stable carbon stores in many carbon capture, utilisation and storage (CCUS) technologies. Read more

Retreating glaciers and carbon-cycle feedbacks

Ongoing climate change is causing profound change to the cryosphere. In particular, rising temperatures and changing ice-melt and precipitation patterns drive glacier retreat, exposing new land surfaces to the atmosphere and changing the pathways and residence times of water beneath glacial systems (Moon et al., 2018). Read more

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