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Featured researches published by Gary R. Eppich.


Science | 2012

Radar-Enabled Recovery of the Sutter’s Mill Meteorite, a Carbonaceous Chondrite Regolith Breccia

Peter Jenniskens; Marc Fries; Q.-Z. Yin; Michael E. Zolensky; Alexander N. Krot; Scott A. Sandford; Derek W. G. Sears; Robert Beauford; Denton S. Ebel; Jon M. Friedrich; Kazuhide Nagashima; Josh Wimpenny; Akane Yamakawa; Kunihiko Nishiizumi; Yasunori Hamajima; Marc W. Caffee; Kees C. Welten; M. Laubenstein; Andrew M. Davis; Steven B. Simon; Philipp R. Heck; Edward D. Young; Issaku E. Kohl; Mark H. Thiemens; Morgan H. Nunn; Takashi Mikouchi; Kenji Hagiya; Kazumasa Ohsumi; Thomas A. Cahill; Jonathan A. Lawton

The Meteor That Fell to Earth In April 2012, a meteor was witnessed over the Sierra Nevada Mountains in California. Jenniskens et al. (p. 1583) used a combination of photographic and video images of the fireball coupled with Doppler weather radar images to facilitate the rapid recovery of meteorite fragments. A comprehensive analysis of some of these fragments shows that the Sutters Mill meteorite represents a new type of carbonaceous chondrite, a rare and primitive class of meteorites that contain clues to the origin and evolution of primitive materials in the solar system. The unexpected and complex nature of the fragments suggests that the surfaces of C-class asteroids, the presumed parent bodies of carbonaceous chondrites, are more complex than previously assumed. Analysis of this rare meteorite implies that the surfaces of C-class asteroids can be more complex than previously assumed. Doppler weather radar imaging enabled the rapid recovery of the Sutter’s Mill meteorite after a rare 4-kiloton of TNT–equivalent asteroid impact over the foothills of the Sierra Nevada in northern California. The recovered meteorites survived a record high-speed entry of 28.6 kilometers per second from an orbit close to that of Jupiter-family comets (Tisserand’s parameter = 2.8 ± 0.3). Sutter’s Mill is a regolith breccia composed of CM (Mighei)–type carbonaceous chondrite and highly reduced xenolithic materials. It exhibits considerable diversity of mineralogy, petrography, and isotope and organic chemistry, resulting from a complex formation history of the parent body surface. That diversity is quickly masked by alteration once in the terrestrial environment but will need to be considered when samples returned by missions to C-class asteroids are interpreted.


Journal of Analytical Atomic Spectrometry | 2013

235U–231Pa age dating of uranium materials for nuclear forensic investigations

Gary R. Eppich; Ross W. Williams; Amy M. Gaffney; Kerri C. Schorzman

Age dating of nuclear material can provide insight into source and suspected use in nuclear forensic investigations. We report here a method for the determination of the date of most recent chemical purification for uranium materials using the 235U-231Pa chronometer. Protactinium is separated from uranium and neptunium matrices using anion exchange resin, followed by sorption of Pa to an SiO2 medium. The concentration of 231Pa is measured by isotope dilution mass spectrometry using 233Pa spikes prepared from an aliquot of 237Np and calibrated in-house using the rock standard Table Mountain Latite and the uranium isotopic standard U100. Combined uncertainties of age dates using this method are 1.5 to 3.5 %, an improvement over alpha spectrometry measurement methods. Model ages of five uranium standard reference materials are presented; all standards have concordant 235U-231Pa and 234U-230Th model ages.


Journal of Radioanalytical and Nuclear Chemistry | 2014

Constraints on fallout melt glass formation from a near-surface nuclear test

Gary R. Eppich; K. B. Knight; Timothy W. Jacomb-Hood; Gregory D. Spriggs; Ian D. Hutcheon

We present major element and actinide composition data from a population of fallout glass samples produced from a single near-surface nuclear detonation. Glass major element compositions indicate that composition of local geology is a primary control on bulk fallout chemical composition. Uranium isotope compositions indicate that vaporized, residual fuel was incorporated into the melts prior to solidification, likely within seconds, and are consistent with two-component mixing between naturally-occurring uranium and residual uranium fuel. Model ages of the residual fuel in fallout are systematically inaccurate, biased towards older ages, and are consistent with two-component mixing between naturally-occurring daughter nuclides in local sediment and decay-derived daughter nuclides from residual nuclear fuel. Multiple processes such as mixing, agglomeration of melted sediment-derived droplets, and incorporation of condensates must all occur within the timescale between sediment melting and melt solidification.


Radiochimica Acta | 2015

Nuclear forensic analysis of uranium oxide powders interdicted in Victoria, Australia

Michael J. Kristo; Elizabeth Keegan; Michael Colella; Ross W. Williams; Rachel E. Lindvall; Gary R. Eppich; Sarah Roberts; Lars E. Borg; Amy M. Gaffney; Jonathan Plaue; K. B. Knight; Elaine Loi; Michael Hotchkis; Kenton Moody; Michael J. Singleton; Martin Robel; Ian D. Hutcheon

Abstract Nuclear forensic analysis was conducted on two uranium samples confiscated during a police investigation in Victoria, Australia. The first sample, designated NSR-F-270409-1, was a depleted uranium powder of moderate purity (∼ 1000 μg/g total elemental impurities). The chemical form of the uranium was a compound similar to K2(UO2)3O4 · 4H2O. While aliquoting NSR-F-270409-1 for analysis, the body and head of a Tineid moth was discovered in the sample. The second sample, designated NSR-F-270409-2, was also a depleted uranium powder. It was of reasonably high purity (∼ 380 μg/g total elemental impurities). The chemical form of the uranium was primarily UO3 · 2H2O, with minor phases of U3O8 and UO2. While aliquoting NSR-F-270409-2 for analysis, a metal staple of unknown origin was discovered in the sample. The presence of 236U and 232U in both samples indicates that the uranium feed stocks for these samples experienced a neutron flux at some point in their history. The reactor burn-up calculated from the isotopic composition of the uranium is consistent with that of spent fuel from natural uranium (NU) fueled Pu production. These nuclear forensic conclusions allow us to categorically exclude Australia as the origin of the material and greatly reduce the number of candidate sources.


Water Resources Research | 2016

Bayesian nitrate source apportionment to individual groundwater wells in the Central Valley by use of elemental and isotopic tracers

Katherine M. Ransom; Mark N. Grote; Amanda Deinhart; Gary R. Eppich; Carol Kendall; Matthew E. Sanborn; A. Kate Souders; Joshua Wimpenny; Qing-Zhu Yin; Megan Young; Thomas Harter

Groundwater quality is a concern in alluvial aquifers that underlie agricultural areas, such as in the San Joaquin Valley of California. Shallow domestic wells (less than 150 m deep) in agricultural areas are often contaminated by nitrate. Agricultural and rural nitrate sources include dairy manure, synthetic fertilizers, and septic waste. Knowledge of the relative proportion that each of these sources contributes to nitrate concentration in individual wells can aid future regulatory and land management decisions. We show that nitrogen and oxygen isotopes of nitrate, boron isotopes, and iodine concentrations are a useful, novel combination of groundwater tracers to differentiate between manure, fertilizers, septic waste, and natural sources of nitrate. Furthermore, in this work, we develop a new Bayesian mixing model in which these isotopic and elemental tracers were used to estimate the probability distribution of the fractional contributions of manure, fertilizers, septic waste, and natural sources to the nitrate concentration found in an individual well. The approach was applied to 56 nitrate-impacted private domestic wells located in the San Joaquin Valley. Model analysis found that some domestic wells were clearly dominated by the manure source and suggests evidence for majority contributions from either the septic or fertilizer source for other wells. But, predictions of fractional contributions for septic and fertilizer sources were often of similar magnitude, perhaps because modeled uncertainty about the fraction of each was large. For validation of the Bayesian model, fractional estimates were compared to surrounding land use and estimated source contributions were broadly consistent with nearby land use types.


Archive | 2015

After Action Report - Kazakhstan NSDD July 2015

Caterina Fox; Gary R. Eppich; Ruth Kips; K. B. Knight; Anthony Belian; Paul Gray; B. Canazaro

On Monday 20 July, Caterina Fox, Ruth Kips and Kim Knight were invited to participate in Kazakhstans nuclear material inventory management working group meeting coordinated by Alexander Vasilliev as nuclear forensics subject matter experts. The meeting included participants from Kazakhstans nuclear regulatory agency (CAESC, the Committee on Atomic and Energetic Supervision and Control) and 3 institutes 1. Institute of Nuclear Physics, INP (Almaty), 2. National Nuclear Center, NNC (Kurchatov), and 3. Ulba Metallurgical Plant, UMP (Oskemen). CAESC requested attendance of an MC&A expert, an IT Specialist, and a Physical Security Specialist from each site. The general meeting concerned considerations for creating unified or compatible systems for nuclear material inventory management. NSDD representatives provided an overview of nuclear forensics and presented considerations for developments of inventory management that might be synergistic with future consideration of development of a National Nuclear Forensics Library to support nuclear forensics investigations.


Meteoritics & Planetary Science | 2014

Fall, recovery, and characterization of the Novato L6 chondrite breccia

Peter Jenniskens; Alan E. Rubin; Qing-Zhu Yin; Derek W. G. Sears; Scott A. Sandford; Michael E. Zolensky; Alexander N. Krot; Leigh Blair; Darci J. Kane; Jason Utas; Robert S. Verish; Jon M. Friedrich; Josh Wimpenny; Gary R. Eppich; Karen Ziegler; Kenneth L. Verosub; Douglas J. Rowland; Jim Albers; Peter S. Gural; Bryant Grigsby; Marc Fries; Robert Matson; M. J. S. Johnston; Elizabeth A. Silber; Peter Brown; Akane Yamakawa; Matthew E. Sanborn; M. Laubenstein; Kees C. Welten; Kunihiko Nishiizumi


Forensic Science International | 2014

Nuclear forensic analysis of an unknown uranium ore concentrate sample seized in a criminal investigation in Australia

Elizabeth Keegan; Michael J. Kristo; Michael Colella; Martin Robel; Ross W. Williams; Rachel E. Lindvall; Gary R. Eppich; Sarah Roberts; Lars E. Borg; Amy M. Gaffney; Jonathan Plaue; Henri Wong; Joel Davis; Elaine Loi; Mark I. Reinhard; Ian D. Hutcheon


Science of The Total Environment | 2012

Evaluation of historical beryllium abundance in soils, airborne particulates and facilities at Lawrence Livermore National Laboratory

Mark Sutton; Richard K. Bibby; Gary R. Eppich; Steven L. Lee; Rachel E. Lindvall; Kent Wilson; Bradley K. Esser


Journal of Radioanalytical and Nuclear Chemistry | 2018

Uranium assay and trace element analysis of the fourth collaborative material exercise samples by the modified Davies-Gray method and the ICP-MS/OES techniques

Aubrey N. Nelwamondo; Lisa P. Colletti; Rachel E. Lindvall; Anna Vesterlund; Ning Xu; Angela Hiong Jun Tan; Gary R. Eppich; Victoria Genetti; Banyana L. Kokwane; Petra Lagerkvist; Boon Kin Pong; Henrik Ramebäck; Lav Tandon; Gert Rasmussen; Zsolt Varga; Maria Wallenius

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Rachel E. Lindvall

Lawrence Livermore National Laboratory

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Amanda Deinhart

Lawrence Livermore National Laboratory

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Amy M. Gaffney

Lawrence Livermore National Laboratory

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Ian D. Hutcheon

Lawrence Livermore National Laboratory

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K. B. Knight

Lawrence Livermore National Laboratory

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Qing-Zhu Yin

University of California

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Ross W. Williams

Lawrence Livermore National Laboratory

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Sarah Roberts

Lawrence Livermore National Laboratory

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