George D. Cody

ORCID: 0000-0003-4176-3648
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About
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Research Areas
  • Astro and Planetary Science
  • Isotope Analysis in Ecology
  • Planetary Science and Exploration
  • High-pressure geophysics and materials
  • Glass properties and applications
  • Advanced NMR Techniques and Applications
  • Astrophysics and Star Formation Studies
  • NMR spectroscopy and applications
  • Thin-Film Transistor Technologies
  • Geological and Geochemical Analysis
  • Hydrocarbon exploration and reservoir analysis
  • Nuclear Physics and Applications
  • Methane Hydrates and Related Phenomena
  • Silicon and Solar Cell Technologies
  • Origins and Evolution of Life
  • Superconducting Materials and Applications
  • Paleontology and Stratigraphy of Fossils
  • Silicon Nanostructures and Photoluminescence
  • Physics of Superconductivity and Magnetism
  • Granular flow and fluidized beds
  • Mineral Processing and Grinding
  • Spacecraft and Cryogenic Technologies
  • Crystallography and molecular interactions
  • Space Exploration and Technology
  • Coal Properties and Utilization

Carnegie Institution for Science
2016-2025

Geophysical Laboratory
2012-2021

University of Oxford
2018

University of Arizona
2017

Rutgers, The State University of New Jersey
2000-2009

Bainbridge State College
2009

Rütgers (Germany)
2009

Rutgers Sexual and Reproductive Health and Rights
2009

University of Washington Tacoma
2009

Seoul National University
2008

The effect of thermal and structural disorder on the electronic structure hydrogenated amorphous silicon is investigated by measurement shape optical absorption edge as a function temperature evolution hydrogen. data are consistent with idea that additive, suggest disorder, rather than hydrogen content, fundamental determining factor in band gap.

10.1103/physrevlett.47.1480 article EN Physical Review Letters 1981-11-16

The Stardust spacecraft collected thousands of particles from comet 81P/Wild 2 and returned them to Earth for laboratory study. preliminary examination these samples shows that the nonvolatile portion is an unequilibrated assortment materials have both presolar solar system origin. contains abundance silicate grains are much larger than predictions interstellar grain models, many high-temperature minerals appear formed in inner regions nebula. Their presence a proves formation included...

10.1126/science.1135840 article EN Science 2006-12-15

The detailed balance method for calculating the radiative recombination limit to performance of solar cells has been extended include free carrier absorption and Auger in addition losses. This applied crystalline silicon where limiting efficiency is found be 29.8 percent under AM1.5, based on measured optical spectrum published values coefficients. assumed textured maximum benefit from light-trapping effects.

10.1109/t-ed.1984.21594 article EN IEEE Transactions on Electron Devices 1984-05-01

We adopt a statistical mechanical approach toward the optics of textured and inhomogeneous optical sheets. As general rule, local light intensity in such medium will tend to be <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2 n^{2}(x)</tex> times greater than externally incident intensity, where xmlns:xlink="http://www.w3.org/1999/xlink">n(x)</tex> is index refraction sheet. This enhancement can contribute...

10.1109/t-ed.1982.20700 article EN IEEE Transactions on Electron Devices 1982-02-01

Sedimentary rocks at Yellowknife Bay (Gale crater) on Mars include mudstone sampled by the Curiosity rover. The samples, John Klein and Cumberland, contain detrital basaltic minerals, calcium sulfates, iron oxide or hydroxides, sulfides, amorphous material, trioctahedral smectites. smectite has basal spacing of ~10 angstroms, indicating little interlayer hydration. Cumberland both ~13.2 angstroms. larger suggests a partially chloritized magnesium facilitating H2O retention. Basaltic minerals...

10.1126/science.1243480 article EN Science 2013-12-10

Optical, electrical, and electron-microscopy studies on granular Ag-Si${\mathrm{O}}_{2}$ Au-Si${\mathrm{O}}_{2}$ films, prepared by cosputtering the metal insulator, were made over composition range 10-90% volume Si${\mathrm{O}}_{2}$. Electron diffraction patterns indicate crystalline metals with lattice constants equal to those of bulk metals. For films less than 50-vol% Si${\mathrm{O}}_{2}$ structure consists amorphous inclusions in a continuous matrix; for more Si${\mathrm{O}}_{2}$,...

10.1103/physrevb.8.3689 article EN Physical review. B, Solid state 1973-10-15
Donald M. Hassler C. Zeitlin R. F. Wimmer‐Schweingruber Bent Ehresmann Scot Rafkin and 95 more J. L. Eigenbrode D. E. Brinza Gerald Weigle Stephan Böttcher Eckart Böhm Söenke Burmeister Jingnan Guo Jan Köhler César Martı́n G. Reitz Francis A. Cucinotta Myung‐Hee Y. Kim David Grinspoon M. A. Bullock Arik Posner Javier Gómez‐Elvira A. R. Vasavada J. P. Grotzinger MSL Science Team Osku Kemppinen David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank M. E. Schmidt Shuai Li R. E. Milliken Kevin M. Robertson V. Z. Sun Michael B. Baker Christopher S. Edwards B. L. Ehlmann K. A. Farley J. L. Griffes Hayden Miller Megan Newcombe C. Pilorget M. S. Rice K. L. Siebach Katie Stack Edward M. Stolper Claude Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall Guy Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla-García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló

The Radiation Assessment Detector (RAD) on the Mars Science Laboratory’s Curiosity rover began making detailed measurements of cosmic ray and energetic particle radiation environment surface 7 August 2012. We report discuss absorbed dose equivalent from galactic rays solar particles martian for ~300 days observations during current maximum. These provide insight into hazards associated with a human mission to an anchor point which model subsurface environment, implications microbial survival...

10.1126/science.1244797 article EN Science 2013-12-10

Organics found in comet 81P/Wild 2 samples show a heterogeneous and unequilibrated distribution abundance composition. Some organics are similar, but not identical, to those interplanetary dust particles carbonaceous meteorites. A class of aromatic-poor organic material is also present. The rich oxygen nitrogen compared with meteoritic organics. Aromatic compounds present, the tend be relatively poorer aromatics than meteorites particles. presence deuterium nitrogen-15 excesses suggest that...

10.1126/science.1135841 article EN Science 2006-12-15

Experiments exploring the potential catalytic role of iron sulfide at 250°C and elevated pressures (50, 100, 200 megapascals) revealed a facile, pressure-enhanced synthesis organometallic phases formed through reaction alkyl thiols carbon monoxide with sulfide. A suite compounds were characterized ultraviolet-visible Raman spectroscopy. The natural such is anticipated in present-day ancient environments wherever reduced hydrothermal fluids pass sulfide–containing crust. Here, pyruvic acid...

10.1126/science.289.5483.1337 article EN Science 2000-08-25

Samples from the Rocknest aeolian deposit were heated to ~835°C under helium flow and evolved gases analyzed by Curiosity’s Sample Analysis at Mars instrument suite. H 2 O, SO , CO O major released. Water abundance (1.5 3 weight percent) release temperature suggest that is bound within an amorphous component of sample. Decomposition fine-grained Fe or Mg carbonate likely source much . Evolved coincident with Cl, suggesting oxygen produced thermal decomposition oxychloride compound. Elevated...

10.1126/science.1238937 article EN Science 2013-09-26
P. R. Mahaffy Christopher R. Webster S. K. Atreya H. B. Franz Michael Wong and 95 more P. G. Conrad D. N. Harpold John J. Jones L. A. Leshin H. L. K. Manning Tobias Owen R. O. Pepin S. W. Squyres M. G. Trainer Osku Kemppinen Nathan Bridges J. R. Johnson M. E. Minitti David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank Gerald Weigle M. E. Schmidt Shuai Li R. E. Milliken Kevin M. Robertson V. Z. Sun Michael B. Baker Christopher Edwards Bethany Ehlmann Kenneth Farley J. L. Griffes J. P. Grotzinger Hayden Miller Megan Newcombe C. Pilorget M. S. Rice Kirsten Siebach Katie Stack Edward M. Stolper Claude Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall Guy Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez‐Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla-García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló Sara Alejandra Sans Fuentes Eduardo Sebastian Martinez J. Torres Roser Urqui-O'Callaghan

Volume mixing and isotope ratios secured with repeated atmospheric measurements taken the Sample Analysis at Mars instrument suite on Curiosity rover are: carbon dioxide (CO2), 0.960(±0.007); argon-40 ((40)Ar), 0.0193(±0.0001); nitrogen (N2), 0.0189(±0.0003); oxygen, 1.45(±0.09) × 10(-3); monoxide, < 1.0 (40)Ar/(36)Ar, 1.9(±0.3) 10(3). The (40)Ar/N2 ratio is 1.7 times greater (40)Ar/(36)Ar 1.6 lower than values reported by Viking Lander mass spectrometer in 1976, whereas other are generally...

10.1126/science.1237966 article EN Science 2013-07-18

The Mars Science Laboratory rover Curiosity scooped samples of soil from the Rocknest aeolian bedform in Gale crater. Analysis with Chemistry and Mineralogy (CheMin) x-ray diffraction (XRD) instrument revealed plagioclase (~An57), forsteritic olivine (~Fo62), augite, pigeonite, minor K-feldspar, magnetite, quartz, anhydrite, hematite, ilmenite. phases are present at, or near, detection limits. also contains 27 ± 14 weight percent amorphous material, likely containing multiple Fe 3+ -...

10.1126/science.1238932 article EN Science 2013-09-26

H 2 O, CO , SO O S, HCl, chlorinated hydrocarbons, NO, and other trace gases were evolved during pyrolysis of two mudstone samples acquired by the Curiosity rover at Yellowknife Bay within Gale crater, Mars. O/OH-bearing phases included 2:1 phyllosilicate(s), bassanite, akaganeite, amorphous materials. Thermal decomposition carbonates combustion organic materials are candidate sources for . Concurrent evolution hydrocarbons suggests presence oxychlorine phase(s). Sulfides likely...

10.1126/science.1245267 article EN Science 2013-12-10

Observations by the Mars Science Laboratory Mast Camera (Mastcam) in Gale crater reveal isolated outcrops of cemented pebbles (2 to 40 millimeters diameter) and sand grains with textures typical fluvial sedimentary conglomerates. Rounded conglomerates indicate substantial abrasion. ChemCam emission spectra at one outcrop show a predominantly feldspathic composition, consistent minimal aqueous alteration sediments. Sediment was mobilized ancient water flows that likely exceeded threshold...

10.1126/science.1237317 article EN Science 2013-05-30

Sedimentary rocks examined by the Curiosity rover at Yellowknife Bay, Mars, were derived from sources that evolved an approximately average martian crustal composition to one influenced alkaline basalts. No evidence of chemical weathering is preserved, indicating arid, possibly cold, paleoclimates and rapid erosion deposition. The absence predicted geochemical variations indicates magnetite phyllosilicates formed diagenesis under low-temperature, circumneutral pH, rock-dominated aqueous...

10.1126/science.1244734 article EN Science 2013-12-10

ABSTRACT We examined the chemical composition of extracellular polymeric substances (EPS) extracted from two natural microbial pellicle biofilms growing on acid mine drainage (AMD) solutions. The EPS obtained a mid-developmental-stage biofilm (DS1) and mature (DS2) were qualitatively quantitatively compared. More than twice as much was derived DS2 DS1 (approximately 340 150 mg per g [dry weight] for DS1, respectively). Composition analyses indicated presence carbohydrates, metals, proteins,...

10.1128/aem.02289-09 article EN Applied and Environmental Microbiology 2010-03-13

The ChemCam instrument, which provides insight into martian soil chemistry at the submillimeter scale, identified two principal types along Curiosity rover traverse: a fine-grained mafic type and locally derived, coarse-grained felsic type. component is representative of widespread soils similar in composition to dust. It possesses ubiquitous hydrogen signature spectra, corresponding hydration amorphous phases found by CheMin instrument. This likely accounts for an important fraction global...

10.1126/science.1238670 article EN Science 2013-09-26
J. C. Stern B. Sutter Caroline Freissinet R. Navarro‐González Christopher P. McKay and 95 more P. D. Archer A. Buch Anna Brunner Patrice Coll J. L. Eigenbrode Alberto González Fairén H. B. Franz D. P. Glavin Srishti Kashyap A. C. McAdam D. W. Ming A. Steele Cyril Szopa J. J. Wray Javier Martín‐Torres María‐Paz Zorzano P. G. Conrad P. R. Mahaffy Osku Kemppinen N. T. Bridges J. R. Johnson M. E. Minitti David A. Cremers J. F. Bell L. A. Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank Gerald Weigle M. E. Schmidt Shuai Li R. E. Milliken Kevin M. Robertson V. Z. Sun Michael B. Baker Christopher S. Edwards B. L. Ehlmann K. A. Farley J. Shechet J. P. Grotzinger Hayden Miller Megan Newcombe C. Pilorget M. S. Rice K. L. Siebach Katie Stack Edward M. Stolper C. Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin Francès Westall G. Israël Christophe Agard Julien Baroukh Christophe Donny Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez‐Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler F. Javier Martín - Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González

Significance We present data supporting the presence of an indigenous source fixed nitrogen on surface Mars in form nitrate. This may indicate first stage development a primitive cycle ancient and would have provided biochemically accessible nitrogen.

10.1073/pnas.1420932112 article EN Proceedings of the National Academy of Sciences 2015-03-23

Samples of the carbonaceous asteroid (162173) Ryugu were collected and brought to Earth by Hayabusa2 spacecraft. We investigated macromolecular organic matter in samples found that it contains aromatic aliphatic carbon, ketone, carboxyl functional groups. The spectroscopic features are consistent with those chemically primitive chondrite meteorites experienced parent-body aqueous alteration (reactions liquid water). morphology carbon includes nanoglobules diffuse associated phyllosilicate...

10.1126/science.abn9057 article EN Science 2023-02-24

Abstract On September 24, 2023, NASA's OSIRIS‐REx mission dropped a capsule to Earth containing ~120 g of pristine carbonaceous regolith from Bennu. We describe the delivery and initial allocation this asteroid sample introduce its bulk physical, chemical, mineralogical properties early analyses. The is very dark overall, with higher‐reflectance inclusions particles interspersed. Particle sizes range submicron dust stone ~3.5 cm long. Millimeter‐scale larger stones typically have hummocky or...

10.1111/maps.14227 article EN cc-by Meteoritics and Planetary Science 2024-06-26

Organic matter in meteorites reveals clues about early Solar System chemistry and the origin of molecules important to life, but terrestrial exposure complicates interpretation. Samples returned from B-type asteroid Bennu by Origins, Spectral Interpretation, Resource Identification, Security-Regolith Explorer mission enabled us study pristine carbonaceous astromaterial without uncontrolled Earth's biosphere. Here we show that samples are volatile rich, with more carbon, nitrogen ammonia than...

10.1038/s41550-024-02472-9 article EN cc-by Nature Astronomy 2025-01-29
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