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CeREES Centre for Geoenergy

Staff Profiles

Dr Richard Hobbs, PhD

Senior Lecturer in the Department of Earth Sciences
Telephone: +44 (0) 191 33 44295
Room number: Rm 320

Contact Dr Richard Hobbs (email at r.w.hobbs@durham.ac.uk)

Biography

08/1985 - 07/1989 Research Associate, BIRPS, Bullard Labs, University of Cambridge
08/1989 - 03/1990 Senior Research Associate, BIRPS, Bullard Labs, University of Cambridge
04/1990 - 03/1998 Director, BIRPS Core Group, Bullard Labs, University of Cambridge
04/1998 - 09/2003 Principle Investigator, Atlantic Margins Project, Bullard Labs, University of Cambridge
10/2003 - 09/2008 NERC Advanced Research Fellow, Department of Earth Science, University of Durham
10/2008 - Present Senior Lecturer, Department of Earth Science, University of Durham

My research is based around applied wavefield propagation and seismic data processing. In particular, the acquisition and processing of seismic reflection and refraction data and the development of software to investigate the propagation of seismic waves in three dimensional heterogenious media. I am currently involved in a number of projects, described below.

Fast 3-D viscoelastic modelling: critical to improving methodology is understanding of how seismic waves interact with the heterogeneous geology. This project has been funded both by the NERC and DERA and has generated a fast and efficient full-waveform modelling scheme. The code can successfully handle 1, 2 or 3 dimensions with plane, cylindrical or point sources in a model that can contain any combination of material with acoustic, elastic or viscoelastic properties. The principal advantage over other codes, e.g. 3-D finite difference, is that the code can run on any workstation or fast PC and does not require the use of a parallel super computer.

Seismic Oceanography is a new dicipline that brings the power and resolution of the seismic reflection method to bare on Oceanographic issues (EU funded NEST project - GO (Geophysical Oceanography) with a total value of 2.7M Euro). The project undertook joint acquisition and modelling to provide a benchmark calibration of the method in the Gulf of Cadiz where the hot saline water flows out of the Straits of Gibralter and mixes with the North Atlantic Water. We sucessfully tracked a small Meddy (an underwater vortex of Mediterranean Water) and acquired high resolution images of its detailed temperature and salinity structure. This new tool has the potential to address issues on mixing in oceans and provide a means to monitor change. I was also involved in a CNR (Venice) led experiemnt to use seismic oceanography to monitor dense water currents along the western margin  of the Adriatic Sea.

Volcanic Margins Reseach Consortium is a national research effort sponsored by industry focussed on continental margins that have experienced a major volcanic influence, eg the Faroes margin to the northwest of Britain. The extensive extrusive basalt flows and intrusive dykes and sill create problems for traditional mapping of these margins. The project combines traditional geological mapping and innovative remote sensing to help improve understanding of the evolution of these margins.

Bayesian methods provide the means to quantify uncertainty given some observed  data and some prior information about the problem. I am developing techniques based on Bayesian principles, in conjunction with the Department of mathematical Sciences, to provide robust estimates of uncertainty for a range of geophysical problems: the computation of the velocity/depth model used in pre-stack depth migration; uncertainties in predicting over-pressure (GEOPOP3) and of seismic data; and joint uncertainties for combinations of complementary data such as gravity, seismic refraction and magnetotelluric data.

OSCAR is a NERC funded Consortium Grant (Durham, NOC, UCL and Manchester) that aims to map the heat and mass fluxes at a mid-ocean ridge. New ocean crust is formed at the mid-ocean ridge as the Earth's plates move. This crust is rapidly cooled by the hydrothermal circulation of sea-water through cracks and pores which removes the heat but also chemically reacts with the rock to deposit and remove minerals. The waste heat is then disspipated in the abysaal oceans. Recent modelling of ocean circulation has shown that including more accurate maps of this geothermal heat input  has significnat effects on the deep water circulation.

Committee and Society Service

Reviewer for the European Science Foundation

Fellowships

1. 2003: NERC Advanced Research Fellow
2. 2003: Senior Research Fellow, Cambridge

Research Interests

  • Controlled source seismic data (acquisition, processing and interpretation)
  • Seismic Oceanography
  • 3D seismic wavefield modelling
  • Bayesian methods to quantify uncertainty
  • Joint inversion

Selected Publications

Journal papers: academic

Show all publications