CSIR Fourth Paradigm Institute, Bengaluru
Vinod Kumar Gaur is an Honorary Emeritus Scientist at the CSIR Fourth Paradigm Institute, Bengaluru, and a distinguished geophysicist whose six-decade career has advanced the understanding of Earth system processes from India’s shield to the Himalayan collision zone. He earned his M.Sc. (Gold Medal) from Banaras Hindu University in 1955, followed by a D.I.C. at Imperial College London and a Ph.D. from the University of London in 1959. His pioneering work led to the discovery of the “host-rock effect” in geoelectromagnetics and the initiation of seismic tomography in India, including the first quantitative GPS measurement of the Indian plate’s motion. He has served as Director, National Geophysical Research Institute (1983–1989), and Secretary, Department of Ocean Development (1989–1992). A recipient of the Shanti Swarup Bhatnagar Prize (1979) and Fellow of all three national science academies, Prof. Gaur continues to contribute to geophysical research, education, and outreach.
Session 1E: Special Session
Chairperson: Amol Dighe, TIFR, Mumbai
Underground science facility as a multi-science activity
Farsighted recognition of the high potential of underground science facilities for spawning imaginative ideas for testing and formulating incisive hypotheses has led to the creation of multiple such facilities worldwide. These USFs provide opportunities for bringing expertise from diverse fields together. For example, a USF would provide an excellent site for locating an ultra-long period seismograph that would record the normal modes of the Earth at a high signal/noise ratio. Estimating the density field of the Earth independently from normal mode seismology and neutrino tomography can synergize a widespread use of numerical mantle convection models to elucidate and explore the many complex problems of the Earth and its dynamics from first principles. These two independent theoretical formalisms involving a shared quantity with constraints provided by the density functional theory, would yield better estimates of matter density field in the deep Earth, than either would do singly, through a joint inversion or data assimilation framework. Other exciting areas of scientific enquiry are also bound to get energized, not only in particle or nuclear physics, but also in life-related sciences, not to mention the new abilities in technology that would accrue in the process of setting up such a facility. I fondly hope that our deliberations here, bringing out the high desirability of setting up a USF in the country, will be strongly endorsed by the Academy and, in turn, by the authorities whose early decision will ensure that we are not too late in venturing into a scientific arena where several forward-looking societies have already gone ahead.