J. Marvin Herndon

J. Marvin Herndon (born 1944) is an American interdisciplinary scientist, who earned his BA degree in physics in 1970 from the University of California, San Diego and his Ph.D. degree in nuclear chemistry in 1974 from Texas A&M University. For three years, J. Marvin Herndon was a post-doctoral assistant to Hans Suess and Harold C. Urey in geochemistry and cosmochemistry at the University of California, San Diego. He is the President of Transdyne Corporation in San Diego, California. He has been profiled in Current Biography, and dubbed a “maverick geophysicist” by The Washington Post.[1][2] He is most noted for deducing the composition of the inner core of Earth as being nickel silicide, not partially crystallized nickel-iron metal.[3] More recently, he has suggested planetocentric nuclear fission reactors as energy sources for the gas giant outer planets.[4] and stellar ignition by nuclear fission[5]

Publications

References

  1. ^ Current Biography 64: 45-49, 2003,http://www.NuclearPlanet.com/profile.htm
  2. ^ http://www.washingtonpost.com/ac2/wp-dyn/A13080-2003Mar23
  3. ^ Herndon, J. M. (1979) The nickel silicide inner core of the Earth. Proc. R. Soc. Lond. A368, 495-500.
  4. ^ Herndon, J. M. (1992) Nuclear fission reactors as energy sources for the giant outer planets. Naturwissenschaften 79, 7-14.
  5. ^ Herndon, J. M. (1994) Planetary and protostellar nuclear fission: Implications for planetary change, stellar ignition and dark matter. Proc. Roy. Soc. Lond., A455, 453-461.

External links