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Mary K. Gilles

Researcher at Lawrence Berkeley National Laboratory

Publications -  109
Citations -  7603

Mary K. Gilles is an academic researcher from Lawrence Berkeley National Laboratory. The author has contributed to research in topics: Aerosol & Particle. The author has an hindex of 44, co-authored 105 publications receiving 6974 citations. Previous affiliations of Mary K. Gilles include University of California, San Diego & Cooperative Institute for Research in Environmental Sciences.

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Journal ArticleDOI

pH dependence of the electronic structure of glycine.

TL;DR: In this article, the carbon, nitrogen and oxygen K-edge spectra were measured for aqueous solutions of glycine by total electron yield near-edge X-ray absorption fine structure (TEY NEXAFS) spectroscopy.
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Chemical speciation of sulfur in marine cloud droplets and particles: Analysis of individual particles from the marine boundary layer over the California current

TL;DR: In this paper, the analysis of individual particles sampled from air masses that originated over the open ocean and then passed through the area of the California current located along the northern California coast was performed.
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Chemical bonding and structure of black carbon reference materials and individual carbonaceous atmospheric aerosols

TL;DR: In this paper, the carbon-tooxygen ratios and graphitic nature of a range of black carbon standard reference materials (BC SRMs), high molecular mass humic-like substances (HULIS) and atmospheric particles are examined using scanning transmission X-ray microscopy (STXM) coupled with nearedge X-Ray absorption fine structure (NEXAFS) spectroscopy.
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Reactions of O(3P) with alkyl iodides: Rate coefficients and reaction products

TL;DR: In this article, the authors measured the rate coefficients for O(3P) with CF3I and CH3I at 213 and 364 K to be: k1(T) = (7.9 ± 0.8) x 10-12 exp[−(175 ± 40)/T] and k2(T ) = (1.0 ± 1.2)
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Lability of secondary organic particulate matter

TL;DR: The mass labilities of films of secondary organic material representative of similar atmospheric organic PM were directly determined by quartz crystal microbalance measurements of evaporation rates and vapor mass concentrations, with strong differences between films representative of anthropogenic compared with biogenic sources.