Prof David Dobson
Geology, mineralogy, petrology, perovskites
Professor of Earth Materials
Appointment: | Room: |
|---|---|
| Professor of Earth Materials | Kathleen Lonsdale, G13 |
Courses Taught: | |
| GEOL0039 Earth and Planetary System Science | |
| GEOL0023 Crustal Dynamics and Mountain Building | |
Research Group(s): | |
| Crystallography and Mineral Physics | |
Email Address: | Telephone Number: |
| d.dobson@ucl.ac.uk | 020 3108 6335 (56335) |
Research Summary
long with colleagues at UCL and the Bayerisches Geoinstitut, I perform high-pressure experiments on deep Earth minerals and rocks. We have several high-pressure devices, including multi-anvil presses, Diamond cells and a modified Paris-Edinburgh cell for neutron diffraction.
The core of the Earth is among the most inaccessible and least understood regions of Earth. The solid inner core and liquid outer core consist of iron plus several percent of a light element. Together with Dr Ian Wood and Prof Lidunka Vocadlo, I have been investigating the iron-alloys which are stable at high pressures. We have discovered a new high-pressure phase of FeSi which is a prime core candidate material.
Research Interest
Along with colleagues at UCL and the Bayerisches Geoinstitut, I perform high-pressure experiments on deep Earth minerals and rocks. We have several high-pressure devices, including multi-anvil presses, Diamond cells and a modified Paris-Edinburgh cell for neutron diffraction.
Earth’s Core Materials
Ian Wood and Lidunka Vocadlo, I have been investigating the iron-alloys which are stable at high pressures. We have discovered a new high-pressure phase of FeSi which is a prime core candidate material.
The outer core is responsible for the Earth’s magnetic field. Geodynamo models require a knowledge of the viscosity and diffusivity of the outer core liquid. We have an active programme to measure these properties at high pressure.
Transport Properties of Mantle Materials
Prof John Brodholt and I been investigating the electrical conductivity of mantle minerals olivine, wadsleyite, magnesiowustite and perovskite. We have used these results to test whether the mantle convects in a layered or whole-mantle fashion.
The viscosity of the mantle is very poorly constrained. In the Laboratory for Mineral Ice and Rock Physics, we have a programme to develop new rheological testing apparatus for ultra-high-pressure experiments. These include the Gigapascal Deformation Cell and the modified Paris-Edinburgh-Belt cell. We will use Neutron diffraction to measure deviatoric stresses and strains in situ at the new ENGIN-X beamline at Rutherford Appleton Laboratory.
Along with Prof. Phil Meredith and Steve Boon we are developing new techniques to investigate the origins of deep earthquakes. Our recent work on serpentine dehydration was published in Science and featured in the international press. See what the BBC has to say about our research and Science.
True colour images of partially dehydrated serpentine recovered from 6 GPa (top) and 8 GPa (bottom).
The strikingly different colours are due to the different dehydration reactions at the two pressures:
Serpentine = olivine + enstatite + water (6 GPa) and:
serpentine = phase A + enatatite + water (8GPa).
Both samples showed seismic signals during dehydration, but the type of signal was significantly different.
The outer core is responsible for the Earth’s magnetic field. Geodynamo models require a knowledge of the viscosity and diffusivity of the outer core liquid. We have an active programme to measure these properties at high pressure.
High-pressure experiments on deep Earth materials; synthesis and properties of new Fe-alloy phases relevant to the core; transport properties of mantle mineral rocks and minerals; deep seismicity.