Martin E. Keillor
Pacific Northwest National Laboratory
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Featured researches published by Martin E. Keillor.
Physical Review Letters | 2011
P. S. Barbeau; N. S. Bowden; B. Cabrera-Palmer; J. Colaresi; J. I. Collar; S. Dazeley; P. De Lurgio; J. E. Fast; N. Fields; C. Greenberg; Todd W. Hossbach; Martin E. Keillor; Jeremy D. Kephart; M. G. Marino; Harry S. Miley; M. L. Miller; John L. Orrell; D. C. Radford; D. Reyna; O. Tench; T.D. Van Wechel; J. F. Wilkerson; K. M. Yocum
We report on several features in the energy spectrum from an ultralow-noise germanium detector operated deep underground. By implementing a new technique able to reject surface events, a number of cosmogenic peaks can be observed for the first time. We discuss an irreducible excess of bulklike events below 3 keV in ionization energy. These could be caused by unknown backgrounds, but also dark matter interactions consistent with DAMA/LIBRA. It is not yet possible to determine their origin. Improved constraints are placed on a cosmological origin for the DAMA/LIBRA effect.
Review of Scientific Instruments | 2012
Ricco Bonicalzi; Michael G. Cantaloub; Anthony R. Day; Luke E. Erikson; J. E. Fast; Joel B. Forrester; Erin S. Fuller; Brian D. Glasgow; Lawrence R. Greenwood; E. W. Hoppe; Todd W. Hossbach; Brian J. Hyronimus; Martin E. Keillor; Emily K. Mace; Justin I. McIntyre; Jason H. Merriman; Allan W. Myers; Cory T. Overman; Nicole R. Overman; Mark E. Panisko; Allen Seifert; Glen A. Warren; Robert C. Runkle
Pacific Northwest National Laboratory recently commissioned a new shallow underground laboratory, located at a depth of approximately 30 meters-water-equivalent. This new addition to the small class of radiation measurement laboratories located at modest underground depths houses the latest generation of custom-made, high-efficiency, low-background gamma-ray spectrometers and gas proportional counters. This paper describes the unique capabilities present in the shallow underground laboratory; these include large-scale ultra-pure materials production and a suite of radiation detection systems. Reported data characterize the degree of background reduction achieved through a combination of underground location, graded shielding, and rejection of cosmic-ray events. We conclude by presenting measurement targets and future opportunities.
Journal of Environmental Radioactivity | 2012
S. R. Biegalski; Theodore W. Bowyer; Paul W. Eslinger; J.A. Friese; Lawrence R. Greenwood; Derek A. Haas; James C. Hayes; Ian Hoffman; Martin E. Keillor; Harry S. Miley; M. Moring
The March 11, 2011 9.0 magnitude undersea megathrust earthquake off the coast of Japan and subsequent tsunami waves triggered a major nuclear event at the Fukushima Dai-ichi nuclear power station. At the time of the event, units 1, 2, and 3 were operating and units 4, 5, and 6 were in a shutdown condition for maintenance. Loss of cooling capacity to the plants along with structural damage caused by the earthquake and tsunami resulted in a breach of the nuclear fuel integrity and release of radioactive fission products to the environment. Fission products started to arrive in the United States via atmospheric transport on March 15, 2011 and peaked by March 23, 2011. Atmospheric activity concentrations of (131)I reached levels of 3.0×10(-2) Bqm(-3) in Melbourne, FL. The noble gas (133)Xe reached atmospheric activity concentrations in Ashland, KS of 17 Bqm(-3). While these levels are not health concerns, they were well above the detection capability of the radionuclide monitoring systems within the International Monitoring System of the Comprehensive Nuclear-Test-Ban Treaty.
arXiv: Nuclear Experiment | 2006
S. R. Elliott; M. Akashi-Ronquest; Mark Amman; J. F. Amsbaugh; Frank T. Avignone; H. O. Back; C. Baktash; A. S. Barabash; P.S. Barbeau; J. R. Beene; M. Bergevin; F. E. Bertrand; M. Boswell; V. Brudanin; W. Bugg; T. H. Burritt; Y.D. Chan; T.V. Cianciolo; J. I. Collar; Richard J. Creswick; M. Cromaz; J. A. Detwiler; P. J. Doe; J. A. Dunmore; Yu. Efremenko; V. Egorov; H. Ejiri; James H. Ely; J. Esterline; Horacio A. Farach
Building a Ovββ experiment with the ability to probe neutrino mass in the inverted hierarchy region requires the combination of a large detector mass sensitive to Ovββ, on the order of 1-tonne, and unprecedented background levels, on the order of or less than 1 count per year in the Ovβ β signal region. The MAJORANA Collaboration proposes a design based on using high-purity enriched 76Ge crystals deployed in ultralow background electroformed Cu cryostats and using modern analysis techniques that should be capable of reaching the required sensitivity while also being scalable to a 1-tonne size. To demonstrate feasibility, the collaboration plans to construct a prototype system, the MAJORANA DEMONSTRATOR, consisting of 30 kg of 86% enriched 76Ge detectors and 30 kg of natural or isotope-76-depleted Ge detectors. We plan to deploy and evaluate two different Ge detector technologies, one based on a p-type configuration and the other on n-type.
arXiv: Nuclear Experiment | 2009
Mark Amman; J. F. Amsbaugh; Frank T. Avignone; H. O. Back; A. S. Barabash; P.S. Barbeau; James R. Beene; M. Bergevin; F. E. Bertrand; M. Boswell; V. Brudanin; W. Bugg; T. H. Burritt; Y.D. Chan; J. I. Collar; R. J. Cooper; Richard J. Creswick; J. A. Detwiler; P. J. Doe; Yu. Efremenko; V. Egorov; H. Ejiri; S. R. Elliott; James H. Ely; J. Esterline; Horacio A. Farach; J. E. Fast; N. Fields; P. Finnerty; B. K. Fujikawa
The MAJORANA collaboration is pursuing the development of the so‐called MAJORANA DEMONSTRATOR. The DEMONSTRATOR is intended to perform research and development towards a tonne‐scale germanium‐based experiment to search for the neutrinoless double‐beta decay of 76Ge. The DEMONSTRATOR can also perform a competitive direct dark matter search for light WIMPs in the 1–10 GeV/c2 mass range. It will consist of approximately 60 kg of germanium detectors in an ultra‐low background shield located deep underground at the Sanford Underground Laboratory in Lead, SD. The DEMONSTRATOR will also perform background and technology studies, and half of the detector mass will be enriched germanium. This talk will review the motivation, design, technology and status of the Demonstrator.
Applied Radiation and Isotopes | 2013
Anthony R. Day; Erin S. Fuller; E. W. Hoppe; Martin E. Keillor; B. LeFerriere; Emily K. Mace; J. Merriman; Allan W. Myers; Cory T. Overman; Mark E. Panisko; Allen Seifert; Glen A. Warren; Richard M. Williams
A new ultra-low-background proportional counter was recently developed with an internal volume of 100 cm(3) and has been characterized at pressures from 1-10 atm with P-10 (90% Ar, 10% methane) gas. This design, along with a counting system providing event digitization and passive and active shielding, has been developed to complement a new shallow underground laboratory (30 m water-equivalent). Backgrounds and low-level reference materials have been measured, and system sensitivity for (37)Ar has been calculated.
Health Physics | 2016
Colin E. Okada; Warnick J. Kernan; Martin E. Keillor; Randy R. Kirkham; Rich Sorom; Don Van Etten
AbstractAir sampling systems were deployed to measure the concentration of radioactive material in the air during the Full-Scale Radiological Dispersal Device Field Trials. The air samplers were positioned 100–600 m downwind of the release point. The filters were collected immediately and analyzed in a field laboratory. Quantities for total activity collected on the air filters are reported along with additional information to compute the average or integrated air concentrations.
Applied Radiation and Isotopes | 2009
Harry S. Miley; Ted W. Bowyer; J. E. Fast; James C. Hayes; E. W. Hoppe; Todd W. Hossbach; Martin E. Keillor; Jeremy D. Kephart; Justin I. McIntyre; Allen Seifert
The International Monitoring System (IMS) of the Comprehensive Test Ban Treaty includes a network of stations and laboratories for collection and analysis of radioactive aerosols. Alternative approaches to IMS operations are considered as a method of enhancing treaty verification. Ultra-low background (ULB) detection promises the possibility of improvements to IMS minimum detectable activities (MDAs) well below the current approach, requiring MDA < or = 30 microBq/m(3) of air for (140)Ba, or about 10(6) fissions per daily sample.
Journal of Radioanalytical and Nuclear Chemistry | 2016
Matthew Douglas; Bruce E. Bernacki; Jennifer L. Erchinger; Erin C. Finn; Erin S. Fuller; E. W. Hoppe; Martin E. Keillor; Shannon M. Morley; Crystal A. Mullen; John L. Orrell; Mark E. Panisko; Glen A. Warren; Michael E. Wright
Liquid scintillation counting (LSC) supports a range of environmental science measurements. At Pacific Northwest National Laboratory, we are constructing an LSC system with an expected background reduction of 10–100 relative to values reported in the literature. In this paper, a number of current measurement applications of LSC have been considered with an emphasis on determining which aspects of such measurements would gain the greatest benefit: improved minimum detectable activity (MDA), reduction in sample size, and reduction in total analysis time.
Journal of Radioanalytical and Nuclear Chemistry | 2013
Harry S. Miley; Ted W. Bowyer; Mark D. Engelmann; Paul W. Eslinger; Judah I. Friese; Lawrence R. Greenwood; Derek A. Haas; James C. Hayes; Martin E. Keillor; Robert A. Kiddy; Randy R. Kirkham; Jonathan W. Landen; Elwood A. Lepel; Lance S. Lidey; Kevin E. Litke; Scott J. Morris; Khris B. Olsen; Robert C. Thompson; Blandina R. Valenzuela; Vincent T. Woods; S. R. Biegalski
Aerosol collections were initiated at several locations by Pacific Northwest National Laboratory (PNNL) shortly after the Great East Japan earthquake of May 2011. Aerosol samples were transferred to laboratory high-resolution gamma spectrometers for analysis. Similar to treaty monitoring stations operating across the Northern hemisphere, iodine and other isotopes which could be volatilized at high temperature were detected. Though these locations are not far apart, they have significant variations with respect to water, mountain-range placement, and local topography. Variation in computed source terms will be shown to bound the variability of this approach to source estimation.