A. L. D. Kilcoyne
Lawrence Berkeley National Laboratory
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Featured researches published by A. L. D. Kilcoyne.
Science | 2012
Christopher Pöhlker; K. T. Wiedemann; B. Sinha; Manabu Shiraiwa; Sachin S. Gunthe; M. L. Smith; Hang Su; Paulo Artaxo; Qi Chen; Yafang Cheng; Wolfgang Elbert; Mary K. Gilles; A. L. D. Kilcoyne; Ryan C. Moffet; Markus Weigand; Scot T. Martin; Ulrich Pöschl; Meinrat O. Andreae
Salty Origins of Fresh Water Cloud droplets above the Amazonian rain forest form mostly around organic aerosols, but the source of the aerosols has been a mystery. Pöhlker et al. (p. 1075) report that particles rich in potassium salts emitted by Amazonian vegetation can act as the seeds for the growth of organic aerosol particles that function as condensation nuclei for water droplets. These specks of biogenic salts provide a surface for the condensation of low- or semi-volatile organic compounds formed by the atmospheric oxidation of isoprene and terpenes, molecules produced in great abundance by many kinds of Amazonian plants. Potassium salt particles account for the previously mysterious initiation sites of aerosol growth above the Amazonian rainforest. The fine particles serving as cloud condensation nuclei in pristine Amazonian rainforest air consist mostly of secondary organic aerosol. Their origin is enigmatic, however, because new particle formation in the atmosphere is not observed. Here, we show that the growth of organic aerosol particles can be initiated by potassium-salt–rich particles emitted by biota in the rainforest. These particles act as seeds for the condensation of low- or semi-volatile organic compounds from the atmospheric gas phase or multiphase oxidation of isoprene and terpenes. Our findings suggest that the primary emission of biogenic salt particles directly influences the number concentration of cloud condensation nuclei and affects the microphysics of cloud formation and precipitation over the rainforest.
Geology | 2011
George D. Cody; Neal S. Gupta; Derek E. G. Briggs; A. L. D. Kilcoyne; Roger E. Summons; Fabien Kenig; Roy E. Plotnick; Andrew C. Scott
The conventional geochemical view holds that the chitin and structural protein are not preserved in ancient fossils because they are readily degradable through microbial chitinolysis and proteolysis. Here we show a molecular signature of a relict chitin-protein complex preserved in a Pennsylvanian (310 Ma) scorpion cuticle and a Silurian (417 Ma) eurypterid cuticle via analysis with carbon, nitrogen, and oxygen X-ray absorption near edge structure (XANES) spectromicroscopy. High-resolution X-ray microscopy reveals the complex laminar variation in major biomolecule concentration across modern cuticle; XANES spectra highlight the presence of the characteristic functional groups of the chitin-protein complex. Modification of this complex is evident via changes in organic functional groups. Both fossil cuticles contain considerable aliphatic carbon relative to modern cuticle. However, the concentration of vestigial chitin-protein complex is high, 59% and 53% in the fossil scorpion and eurypterid, respectively. Preservation of a high-nitrogen-content chitin-protein residue in organic arthropod cuticle likely depends on condensation of cuticle-derived fatty acids onto a structurally modified chitin-protein molecular scaffold, thus preserving the remnant chitin-protein complex and cuticle from degradation by microorganisms.
Advanced Materials | 2016
Suhas Kumar; Catherine Graves; John Paul Strachan; Emmanuelle Merced Grafals; A. L. D. Kilcoyne; Tolek Tyliszczak; Johanna Nelson Weker; Yoshio Nishi; R. Stanley Williams
Oxygen migration in tantalum oxide, a promising next-generation storage material, is studied using in operando X-ray absorption spectromicroscopy. This approach allows a physical description of the evolution of conduction channel and eventual device failure. The observed ring-like patterns of oxygen concentration are modeled using thermophoretic forces and Fick diffusion, establishing the critical role of temperature-driven oxygen migration.
Advanced Materials | 2015
Yiyang Li; Sophie Meyer; Jongwoo Lim; Sang-Chul Lee; William E. Gent; Stefano Marchesini; Harinarayan Krishnan; Tolek Tyliszczak; David A. Shapiro; A. L. D. Kilcoyne; William C. Chueh
High-resolution X-ray microscopy is used to investigate the sequence of lithiation in LiFePO4 porous electrodes. For electrodes with homogeneous interparticle electronic connectivity via the carbon black network, the smaller particles lithiate first. For electrodes with heterogeneous connectivity, the better-connected particles preferentially lithiate. Correlative electron and X-ray microscopy also reveal the presence of incoherent nanodomains that lithiate as if they are separate particles.
Beilstein Journal of Nanotechnology | 2013
John Paul Strachan; Jianhua Yang; Luciano A. Montoro; C A Ospina; Antonio J. Ramirez; A. L. D. Kilcoyne; Gilberto Medeiros-Ribeiro; R. Stanley Williams
Summary Metal–insulator–metal (MIM) structures based on titanium dioxide have demonstrated reversible and non-volatile resistance-switching behavior and have been identified with the concept of the memristor. Microphysical studies suggest that the development of sub-oxide phases in the material drives the resistance changes. The creation of these phases, however, has a number of negative effects such as requiring an elevated voltage, increasing the device-to-device variability, damaging the electrodes due to oxygen evolution, and ultimately limiting the device lifetime. In this work we show that the deliberate inclusion of a sub-oxide layer in the MIM structure maintains the favorable switching properties of the device, while eliminating many of the negative effects. Electrical and microphysical characterization of the resulting structures was performed, utilizing X-ray and electron spectroscopy and microscopy. In contrast to structures which are not engineered with a sub-oxide layer, we observed dramatically reduced microphysical changes after electrical operation.
Journal of Physics B | 2011
N C Sterling; D. A. Esteves; R.C. Bilodeau; A. L. D. Kilcoyne; Eddie C. Red; R. A. Phaneuf; A. Aguilar
Absolute photoionization cross-section measurements are reported for Se+ in the photon energy range 18.0–31.0 eV, which spans the ionization thresholds of the 4S3/2 ground state and the low-lying 2P3/2, 1/2 and 2D5/2, 3/2 metastable states. The measurements were performed using the Advanced Light Source synchrotron radiation facility. Strong photoexcitation–autoionization resonances due to 4p → nd transitions are seen in the cross-section spectrum and identified with a quantum-defect analysis.
Journal of Physics B | 2014
A. Müller; S. Schippers; D. A. Esteves-Macaluso; M Habibi; A. Aguilar; A. L. D. Kilcoyne; R. A. Phaneuf; C P Ballance; Brendan M. McLaughlin
We report on experimental and theoretical results for the photoionization of Ag-like xenon ions, Xe
Physical Review A | 2012
Guillermo Hinojosa; A. M. Covington; G. A. Alna'Washi; Mei-Ju Lu; R. A. Phaneuf; M. M. Sant'Anna; C. Cisneros; I. Alvarez; A. Aguilar; A. L. D. Kilcoyne; A. S. Schlachter; C P Ballance; Brendan M. McLaughlin
^{7+}
Journal of Physical Chemistry A | 2008
A. L. D. Kilcoyne; Danqin Feng; Jing Liu; Adam P. Hitchcock; A. L. David Kilcoyne; Tolek Tyliszczak; Norman F. Riehs; E. Rühl; John D. Bozek; David N. McIlroy; Peter A. Dowben
, in the photon energy range 95 to 145~eV. The measurements were carried out at the Advanced Light Source at an energy resolution of
American Mineralogist | 2017
Guoqing Geng; Rupert J. Myers; A. L. D. Kilcoyne; Juyoung Ha; Paulo J.M. Monteiro
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