The future of the subterranean estuary
ByProfessor Willard S. Moore
Research Professor,Distinguished Professor Emeritus
University of South Carolina
时间：9月30日（星期五）10:00-11:30
地点：曾呈奎楼B-206
WILLARD S. MOORE’s CV
Education
B.S., 1962, Chemistry, Millsaps College, Jackson Mississippi
M.A., 1965, Geology, Columbia University, New York, NY
Ph.D., 1969, Earth and Space Sciences, SUNY at Stony Brook, NY
Professional Experience
2000 to present: Research Professor and Distinguished Professor Emeritus, University of South Carolina
2001 to 2004 : Adjunct Scientist, Woods Hole Oceanographic Institution
1981 to 2000: Professor of Geology and Marine Science, Univ. of SC
1981 to 1985: Chairman, Department of Geology, University of South Carolina
1976 to 1981: Associate Professor of Geology and Marine Science, Univ. of SC
1969 to 1976: Oceanographer, U.S. Naval Oceanographic Office, Washington DC
1971: Research Fellow, Geocosmochemistry Group, Tata Institute of Fundamental Research, Bombay, India
Honors, Professional Activities, & Society Membership
Fellow, Hanse-Wissenschaftskolleg, Germany, 2008-2010
Who’s Who in America, 2009
Distinguished Alumni Award, Stony Brook University, 2007
American Geophysical Union, elected Fellow, 2006
B.H. Ketchum Award, Woods Hole Oceanographic Institution, 1999
USC Education Foundation Award for Research in Science & Engineering, 1993
Coastal Ocean Processes (CoOP), Scientific Steering Committee, 1998-2001
NAS/NRC Committee for Reference Materials in Ocean Science, 2001-2002
SCOR, Groundwater Discharge Working Group, 1998-2004
Marine Chemistry, Member Editorial Board, 1993-
NSF Future of Ocean Chemistry in the US, Steering Committee, 1997-1999
Geological Society of America, Assoc. Editor, Bulletin GSA, 1980-1988
American Association for the Advancement of Science
Sigma Xi, President USC Chapter, 1978-79
Oceanographic Society
Geochemical Society
Explorers Club, Chairman Greater Piedmont Chapter, 1995-1996
Total Number of Refereed Publications: 168
Review Articles: 19
US patents: 2
Selected Publications
1. Moore, W. S., Large groundwater inputs to coastal waters revealed by226Ra enrichments. Nature 380, 612-614, 1996.
2. Moore, W. S., The subterranean estuary: a reaction zone of ground water and sea water, Marine Chemistry, 65, 111-126, 1999.
3. Moore, W.S., J.O. Blanton, S. Joye, Estimates of Flushing Times, Submarine Groundwater Discharge, and Nutrient Fluxes to Okatee River, South Carolina, J. Geophys. Res., 111, C09006, doi:10.1029/2005JC003041, 2006.
4. Moore, W.S. and A.M. Wilson, Advective flow through the upper continental shelf driven by storms, buoyancy, and submarine groundwater discharge. Earth and Planetary Science Letters 235, 564-576, 2005.
5. Moore, W.S., Sources and fluxes of submarine groundwater discharge delineated by radium isotopes. Biogeochemistry, 66, 75-93, 2003.
6. Moore, W.S., J. Krest, G. Taylor, E. Roggenstein, S. Joye, & R. Lee, Thermal evidence of water exchange through a coastal aquifer: Implications for nutrient fluxes, Geophys. Res. Letters, 29,10.1029/2002GL014923, 2002.
7. Krest, J. M., W. S. Moore, L. R. Gardner, and J. Morris, Marsh nutrient export supplied by groundwater discharge: Evidence from Ra measurements. Global Biogeochemical Cycles, 14, 167-176, 2000.
8. Crotwell, A.M. and W.S. Moore, Nutrient and Radium Fluxes from Submarine Groundwater Discharge to Port Royal Sound, South Carolina. Aquatic Geochemistry, 9, 191-208, 2003.
9. Windom, H.L., L.F. Niencheski, W.S. Moore, R. Jahnke. Submarine Groundwater Discharge: a Large, Previously Unrecognized Source of Dissolved Iron to the South Atlantic Ocean. Marine Chemistry, 102:252-266, 2006.
