1999
DOI: 10.1023/a:1006258205551
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Cited by 32 publications
(19 citation statements)
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“…Now we discuss experimental data. The T 2 temperature dependence of the electron-phonon scattering rate has been observed experimentally in various materials with a small value of the electron mean-free path: Au, [15][16][17][18] Ag and Mg, 18 Nb, 19 W, 8 CuCr, 20 Ti 1Ϫx Sn x ,Ti 1Ϫx Ge x , Ti 0.97Ϫx Sn 0.03 Sc x , 10,11,21,22 and Sn 1Ϫx Cu x . 23 In relatively pure materials (lϾ10 nm), at temperatures Tу10 K this temperature dependence may be attributed to the interaction with transverse phonons in the clean limit of the Schmid theory (q T lу1).…”
Section: Discussionmentioning
confidence: 99%
“…Now we discuss experimental data. The T 2 temperature dependence of the electron-phonon scattering rate has been observed experimentally in various materials with a small value of the electron mean-free path: Au, [15][16][17][18] Ag and Mg, 18 Nb, 19 W, 8 CuCr, 20 Ti 1Ϫx Sn x ,Ti 1Ϫx Ge x , Ti 0.97Ϫx Sn 0.03 Sc x , 10,11,21,22 and Sn 1Ϫx Cu x . 23 In relatively pure materials (lϾ10 nm), at temperatures Tу10 K this temperature dependence may be attributed to the interaction with transverse phonons in the clean limit of the Schmid theory (q T lу1).…”
Section: Discussionmentioning
confidence: 99%
“…As unsaturated compounds similar to methyl oleate, such as oleic acid, have been observed in the atmosphere, NO 3 oxidation of organic particles likely plays a significant role in the atmosphere. Zhao et al 333 reported uptake coefficient of NO 3 to unsaturated fatty acid particles, finding very large g values of 0.27, 0.53, 0.72 and 1.01 for oleic acid, linoleic acid, g o 10 À3 (170-200 K) 324 Dry salts g = 0.002-0.49 (NaCl), g = 0.1-0.3 (NaBr), g = 0.16-0.2 (KBr), g = 0.33 (KI) 325,326,486 Dust g = 0.009-0.12 (Saharan dust), g = 0.034 (limestone) 327,328 Organics n-Hexadecane: 2.6 Â 10 À3 ; n-octanoic acid: 2.1 Â 10 À3 ; 1-octadecene: 1.6 Â 10 À3 ; 1-hexadecene: 2.3 Â 10 À3 ; heptamethyl nonane: 2.1 Â 10 À3 ; 1-octanol: 7.1 Â 10 À3 ; 7-tetradecene: 5.8 Â 10 À3 ; conjugated linoleic acid: 7.9 Â 10 À3 -( Z 0.12); nonconjugated linoleic acid: 0.15-( Z 0.13); oleic acid: 0.13À( Z0.07); Glycerol: 4.5 Â 10 À4 ; diethyl sebacate: (3.5-4.5) Â 10 À3 ; dioctyl sebacate: 3.9 Â 10 À3 ; squalane: 5.2 Â 10 À3 ; terminal C11 alkene (C 11 H 12 S) monolayer: 0.034; methyl oleate: 0.14; 317,331,332 oleic acid: 0.27; linoleic acid: 0.53; linolenic acid: 0.72; conjugated linoleic acid: 1.01; 333 levoglucosan: 1.3 Â 10 À3 ; abeitic acid: 2.3 Â 10 À3 ; nitroguaiacol: 2.6 Â 10 À2 335 Soot g = o4 Â 10 À4 -0.33 depending on soot type [336][337][338] a All uptake coefficients are at room temperature if not otherwise noted.…”
Section: No 3 Aerosol Uptakementioning
confidence: 99%
“…Nitrate ions are typically present in sea salt aerosols and snowpacks as a result of reactions between halide ions and gaseous nitrogen oxides. These reactions result in the conversion of Cl − and Br − to gaseous halogen products, with a concomitant increase in the number of nitrate ions in the condensed phase. Deposition of inorganic nitrate onto snowpack also occurs. ,, Calculations of nitrate concentrations on the Arctic snowpack quasi-liquid layer suggest that it could be as high as 0.3 μM .…”
Section: Introductionmentioning
confidence: 99%