ライフサイエンスコーパス: vapour

1 c conditions, as well as for saturated argon vapour.

2 ed inside the confined area is released as a vapour.

3 rent to greenhouse gases, most notably water vapour.

4 purpose of modulating the alkali background vapour.

5 rts-per-thousand levels of atmospheric water vapour.

6 into pure (99.9%) liquid antimony and sulfur vapour.

7 ying a magmatic reservoir with vol% exsolved vapour.

8 differentiation between different gases and vapours.

9 n-3-ol (octenol) and R-(-)-carvone (carvone) vapours.

10 of large amounts of extremely low-volatility vapours.

11 -volatile compounds directly from the baking vapours.

12 alysis of volatile and semi-volatile organic vapours.

13 lei originate from nucleation of atmospheric vapours.

14 ly assign enrolled patients 2:1 to segmental vapour ablation (treatment group) or standard medical ma

15 eased upper lobe segments with bronchoscopic vapour ablation led to clinical improvement.

16 tandard medical management, targeted thermal vapour ablation of more diseased segments and preservati

17 We detected water vapour absorption at a wavelength of 1.4 micrometres.

18 The recent discovery of water vapour absorption near Ceres and previous detection of b

19 ions of tropospheric O3 precursors and water vapour abundance determine the climate response of oxida

20 nditions in winter, air pollutants and water vapour accumulate in a shallow planetary boundary layer

21 rmining D, based on measuring both the water vapour adsorption isotherm of a given substance, and its

22 rated by their performances in water/organic vapour adsorption, as well as long-term ultrastability u

23 experiments, it has been shown that organic vapours alone can drive nucleation.

24 down to ~1 ppb) detection of a wide range of vapour analytes is achieved, representing orders of magn

25 ixing of the fluid phase to form an H2O-rich vapour and a hydrosaline phase in equilibrium with the s

26 emi-volatile and therefore partition between vapour and condensed phases in the atmosphere and both t

27 bedo: and bulk surface conductance for water vapour and decreases aerodynamic surface temperature.

28 h it; it is a key component of all life; its vapour and droplets fill the lower atmosphere; and even

29 2O3-delta (BSCF) in the presence of both H2O vapour and electron irradiation using environmental tran

30 be the sources of the observed jets of water vapour and icy particles and to exhibit higher temperatu

31 how temporal variations of atmospheric water vapour and its isotopic composition (delta(18) OV ) infl

32 turn's moon Enceladus emits a plume of water vapour and micrometre-sized ice particles from a series

33 ater exists in many forms, including liquid, vapour and numerous crystalline and amorphous phases of

34 of rapeseed oil significantly reduces water vapour and oxygen permeability.

35 densed phases in the atmosphere and both the vapour and particulate forms undergo chemical reactions.

36 ation-driven ITCZ dynamics may provoke water vapour and vegetation feedbacks in northern mid-latitude

37 pers for controlling the movement of fluids, vapours and solids between complex environments.

38 ts and guest molecules, exposure to reactive vapours, and external stimuli such as heat, light or mec

39 s the data for reactions of the 2-3-ring PAH vapour are quite extensive and generally consistent, suc

40 In addition, water vapour around Ceres has recently been reported, possibly

41 The presence of water vapour around Ceres was suggested by a marginal detectio

42 Here we report the detection of water vapour around Ceres, with at least 10(26) molecules bein

43 We use the models' water vapour as a transfer function between data sets that ove

44 lain most subsequent growth, leaving organic vapours as the most plausible alternative, at least in t

45 mplete condensation of a bulk silicate Earth vapour at an ambient pressure that is higher than 10 bar

46 rger trapped atom samples can be loaded from vapour at higher pressure, after which the pressure is r

47 asmonate (MeJA) and methyl salicylate (MeSA) vapours at 10 and 100micromoll(-1) was investigated as a

48 ransmission spectrum-from a cloud-free water-vapour atmosphere to a Venus-like one.

49 pectrometry (GFAAS); and for mercury by cold vapour atomic absorption spectrometry (CVAAS).

50 tration and determination of mercury by cold vapour atomic absorption spectrometry is described.

51 th two spectroscopic techniques, namely cold vapour atomic absorption spectroscopy (CV-AAS) and a dir

52 for determination of mercury in rice by cold vapour atomic fluorescence spectrometry (CV AFS) is prop

53 sted for their mechanical, optical and water vapour barrier properties.

54 s abundant, essentially non-volatile organic vapours, but the sources and compositions of such vapour

55 moisture conditions to (18) O-depleted water vapour (c. - 200 per thousand) at high relative humidity

56 te that millions of strontium atoms from the vapour can be captured in a magneto-optical trap (MOT).

57 further demonstrate how these low-volatility vapours can enhance, or even dominate, the formation and

58 ted for in the measurement of sulphuric acid vapour, can participate in the growth process, leading t

59 as water (for example, a 100 per cent water vapour composition), or it could contain high-altitude c

60 presumed global long-term increases in water vapour concentrations in the lower stratosphere.

61 vapour record extends back to 1988 and water vapour concentrations largely follow tropical tropopause

62 , USA shows increases in stratospheric water vapour concentrations that cannot be fully explained by

63 n (curvature) effect, which inhibits organic vapour condensation on the smallest particles (the nano-

64 ticles can grow by sulfuric acid and organic vapour condensation to diameters sufficiently large to p

65 to cloud droplets under supersaturated water vapour conditions is described by classic Kohler theory.

66 The influence of water vapour conditions on mass transport and barrier properti

67 equilibrium effects, PLA was conditioned in vapour contact with the aroma compounds at concentration

68 As proof of concept, vapours containing approximately 1% of two chiral monote

69 studies predict that low-volatility organic vapours contribute during initial growth, direct evidenc

70 optical properties of metalorganic chemical vapour deposited (MOCVD) InGaN/GaN multiple quantum well

71 rical specimens, with electron beam physical vapour deposited coatings, were tested with internal coo

72 conductivity mapping of large area chemical vapour deposited graphene films on sapphire, silicon dio

73 d our analysis shows that the doped chemical vapour deposited graphene has good optical properties in

74 Chemical vapour deposited graphene rather than exfoliated or epit

75 he selective deposition of metal at chemical vapour deposited graphene's line defects, notably grain

76 isualization of grain boundaries in chemical vapour deposited monolayer MoS2 samples with multiphoton

77 A central question in the study of vapour-deposited glasses, particularly in light of new k

78 is technique by realizing arrays of chemical-vapour-deposited graphene light emitters.

79 tor Schottky junction, by comparing chemical vapour-deposited graphene transferred on semiconductor s

80 el considered here, structures that arise in vapour-deposited materials are statistically identical t

81 anar heterojunction solar cell incorporating vapour-deposited perovskite as the absorbing layer can h

82 of p-doping exhibited in large area chemical vapour deposition (CVD) graphene field effect transistor

83 phene-based microwave devices using Chemical Vapour Deposition (CVD) graphene whose sheet resistance

84 dy, we have demonstrated the use of chemical vapour deposition (CVD) grown-graphene to develop a high

85 fabrication techniques, among which chemical vapour deposition (CVD) is one of the most promising for

86 Current methods of chemical vapour deposition (CVD) of graphene on copper are compli

87 eview focuses on the solution based chemical vapour deposition (CVD) of main group materials with par

88 nstrate that in an oxygen-activated chemical vapour deposition (CVD) process, half-millimetre size, B

89 ificantly up-scaled the traditional chemical vapour deposition (CVD) production for NPs from mg level

90 synthesized on Pt and Cu foil using chemical vapour deposition (CVD), multilayer h-BN is still absent

91 atomic-layered MoS2 synthesised by chemical vapour deposition (CVD).

92 f hexagonal boron nitride (h-BN) by chemical vapour deposition (CVD).

93 um and low cost Electrostatic Spray Assisted Vapour Deposition (ESAVD) method has been used to produc

94 ymer topcoat deposited by initiated chemical vapour deposition (iCVD).

95 A versatile Rotary Chemical Vapour Deposition (RCVD) technique for the in-situ synth

96 -of-the-art growth methods based on chemical vapour deposition allow the synthesis of one-centimetre-

97 at is observed in graphene grown by chemical vapour deposition and at the LaAlO3-SrTiO3 interface, ma

98 re fabricated using plasma enhanced chemical vapour deposition and their individual emission characte

99 ther the ultra-stable glassy films formed by vapour deposition are ever equivalent to those obtained

100 a graphitic nanoribbon by utilizing chemical vapour deposition conditions.

101 Here we present a computational study of vapour deposition for a two-dimensional glass forming li

102 Chemical vapour deposition graphene is especially well suited for

103 at least 10 times higher than prior chemical vapour deposition graphene transistor DNA sensors.

104 Here we create, from chemical vapour deposition graphene, field-effect transistor arra

105 lectrostatic assembly together with chemical vapour deposition growth.

106 lass films prepared by a process of physical vapour deposition have been shown to have thermodynamic

107 ectrochemistry of graphene grown by chemical vapour deposition in two-dimensional and three-dimension

108 lecules on diamond and subsequently chemical vapour deposition is employed for the diamond growth.

109 defects in graphene synthesized by chemical vapour deposition limits its application in biosensing.

110 ich can be synthesized via scalable chemical vapour deposition method down to only two layers, could

111 report on an improved Fe-catalyzed chemical vapour deposition method for synthesizing ultra-long alp

112 ike nanowires were synthesized by a chemical vapour deposition method on Si substrates treated withou

113 m enabled using an aerosol-assisted chemical vapour deposition method.

114 and chemical (atomic layer deposition, ALD) vapour deposition methods as a functional coating for la

115 e that uses millimetre-scale direct chemical vapour deposition of MoS2 followed by lithographic defin

116 onto the oxide, by atomic layer and physical vapour deposition of the oxide on graphene or by carbon

117 lly achieved by graphene growth via chemical vapour deposition on a metallic surface, followed by tra

118 nthesis of high-quality graphene by chemical vapour deposition on metallic substrates requires polish

119 eCl3 intercalated graphene grown by chemical vapour deposition on Nickel, and demonstrate values as l

120 xperiments indicate that glasses prepared by vapour deposition onto a substrate can exhibit remarkabl

121 lied by physical vapour deposition, chemical vapour deposition or the tip of a scanning tunnelling mi

122 rous silica as a template through a chemical vapour deposition process.

123 cancy in mechanical exfoliation and chemical vapour deposition samples to molybdenum antisite in phys

124 n samples to molybdenum antisite in physical vapour deposition samples.

125 Here we have refined chemical vapour deposition synthesis to grow highly crystalline i

126 Very recently, the chemical vapour deposition technique (CVD) has shown great promis

127 th a newly developed, metal-organic chemical vapour deposition technique, and show high electrical pe

128 We then used vapour deposition techniques to create p-i-n junction so

129 Graphene films grown by vapour deposition tend to be polycrystalline due to the

130 monolayer MoS2 has been produced by chemical vapour deposition, but has not yet been fully explored.

131 trapyrroles with metals supplied by physical vapour deposition, chemical vapour deposition or the tip

132 reduction compared to conventional chemical vapour deposition, CVD, synthesis.

133 ges over conventional materials deposited by vapour deposition, enabling a path to highly scaled elec

134 pproach, using graphene obtained by chemical vapour deposition, which allows a proton-deuteron separa

135 apsulated layered Bi2O2Se, grown by chemical vapour deposition, which demonstrate excellent air stabi

136 f either mechanically exfoliated or chemical vapour deposition-grown graphene.

137 Here we systematically characterize chemical vapour deposition-grown MoS2 by photoluminescence spectr

138 eter scale domains within 80 min by chemical vapour deposition.

139 eteroepitaxially using metalorganic chemical vapour deposition.

140 echanical exfoliation, physical and chemical vapour deposition.

141 ll structure grown by metal organic chemical vapour deposition.

142 graphene nanoribbons on Ge(001) via chemical vapour deposition.

143 ayer molybdenum disulphide grown by chemical vapour deposition.

144 uter-simulation process that mimics physical vapour deposition.

145 ent conditions, via plasma-enhanced chemical vapour deposition.

146 ophene (DFH-4T), can be easily fabricated by vapour deposition.

147 eoretical modelling, we show how to maximize vapour diffusion fluxat the apex of convex millimetric b

148 s falls is best explained by grain growth by vapour diffusion in ice-rich layers, or by sintering.

149 The presence of both vapours does not lead to the synthesis of alloyed nanocr

150 fabrication of sensors for exhaust gases and vapours due to high selectivity and sensitivity.

151 hree-phase interface between gas or chemical vapour, electrolyte and electrode is crucial for the rea

152 dients and that they move in response to the vapour emitted by neighbouring droplets.

153 hanism for the oxidation of uranium in water vapour environments where the transport of hydroxyl spec

154 ation between liquid and vapour, followed by vapour escape during accretionary growth of planetesimal

155 ass' avocado fruit treated with MeJA or MeSA vapours, especially at 100mumoll(-1).

156 activity and polyphenols were quantified in vapour-extracted juice of nine Austrian, partially endem

157 r, isotopic fractionation between liquid and vapour, followed by vapour escape during accretionary gr

158 m encapsulated in grout was exposed to water vapour for extended periods of time.

159 These vapours form at significant mass yield in the gas phase

160 ess that is accompanied by the loss of water vapour from leaves.

161 This indicates that the ethanol vapour from the backside of the membrane has access to t

162 equency eastward-propagating anomalous water vapour from upstream to the TP that influences precipita

163 and controlled emission of strontium atomic vapours from bulk strontium oxide irradiated by a simple

164 ospheric oxidation of low-volatility organic vapours from the mined oil sands material is directly re

165 The experimental conditions for vapour generation were determined using a full two-level

166 sh samples using the accepted method of cold vapour generation.

167 Vapour growth at low temperature, on the other hand, lea

168 ticles over continents, whereas iodine oxide vapours have been implicated in particle formation over

169 volve sulfuric acid, organic or iodine oxide vapours have yet to be reported.

170 tmospheric gas molecules, particularly water vapour, have been proposed as a coolant; however, becaus

171 as to determine the influence of postharvest vapour heat treatment (VHT) on qualitative and quantitat

172 m shows a response of 12% for 0.5 ppm of TMA vapour in 54% relative humidity, with response and recov

173 es <100 degrees C by dissociation of ethanol vapour in a novel microplasma process.

174 thus further depressing of aerosol and water vapour in a very shallow PBL.

175 Cavitation, the nucleation of vapour in liquids, is ubiquitous in fluid dynamics, and

176 istribution of gases such as ozone and water vapour in the stratosphere - which affect surface climat

177 pristine conditions but also quantify these vapours in mixtures, and when blended with a variable mo

178 rs that not only selectively detect separate vapours in pristine conditions but also quantify these v

179 osol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamb

180 ditions that investigate the role of organic vapours in the initial growth of nucleated organic parti

181 The bubbles contain the sulfur-bearing vapour injected into the atmosphere during eruptions.

182 ass transfer coefficients through a liquid - vapour interface and evaporation rate.

183 ited by molecular reflection from the liquid/vapour interface below a certain length scale, which dep

184 of reactions occurring at the aqueous phase-vapour interface compared with the bulk aqueous phase.He

185 ectly heat high-salinity brines at the water/vapour interface of the membrane distillation element, a

186 lecules from the droplet bulk to the droplet-vapour interface.

187 nd establish its propensity for the solution-vapour interface.

188 e findings define the regime in which liquid/vapour interfaces govern nanofluidic transport and have

189 Liquid/vapour interfaces govern the behaviour of a wide range o

190 ystematically investigate the role of liquid/vapour interfaces in the transport of water across appos

191 components and porous media involving liquid/vapour interfaces.

192 Stratospheric water vapour is a powerful greenhouse gas.

193 on of heavy haze: (1) the dispersal of water vapour is constrained by the shallow PBL, leading to an

194 Sulfuric acid vapour is often involved in nucleation but is too scarce

195 Although water vapour is the main species observed in the coma of comet

196 The nucleation of atmospheric vapours is an important source of new aerosol particles

197 The nucleation of sulfuric acid and organic vapours is thought to be responsible for the formation o

198 ow solvent-free, guard flow-assisted organic vapour jet printing of non-faceted, crystalline microsph

199 of a Chardonnay wine to light from a mercury vapour lamp under controlled temperature conditions show

200 Leidenfrost effect in which drops hover on a vapour layer.

201 bsorption to variations in atmospheric water vapour, leading to an underestimation in the shortwave a

202 self-amplification mechanism in which water vapour leads to a trapping and massive increase of parti

203 is considered the solution-phase analogue to vapour-liquid-solid (VLS) growth.

204 Nanowire growth by the vapour-liquid-solid (VLS) process enables a high level o

205 conventional Au catalysts, when used during vapour-liquid-solid growth.

206 owth of the nanowires was in accordance with vapour-liquid-solid mechanism, followed by Ostwald ripen

207 tructures during Bi-rich growth, through the vapour-liquid-solid mechanism.

208 ies, can be grown by self-assembly using the vapour-liquid-solid process.

209 Vapour-liquid-solid route and its variants are routinely

210 er of the substrate (and oxygen) between the vapour-liquid-solid tri-phase system and to the surface

211 e of substantial (about 40 per cent by mass) vapour loss from growing planetesimals by this mechanism

212 nction (the point at which solid, liquid and vapour meet) and the nucleation site of each new layer o

213 drules in CB chondrites probably formed in a vapour-melt plume produced by a hypervelocity impact wit

214 is indicated by a maximum increase in water vapour mixing ratios of 2 mmol mol(-1) .

215 confirmed by a plethora of experiments with vapour molecules of various dipole moments, particularly

216 e associated with the formation of a dynamic vapour nanobubble around the spaser that leads to giant

217 ver continents are influenced by atmospheric vapours of anthropogenic origin (for example, ref.

218 rray was tested in nitrogen upon exposure to vapours of R-(-)-1-octen-3-ol (octenol), in the range of

219 th is primarily due to more abundant organic vapours of slightly higher volatility (saturation concen

220 ing the hydride as originating via the water vapour oxidation mechanism.

221 of zeolites and MOFs in the sensing of water vapour, oxygen, NOx, carbon monoxide and carbon dioxide,

222 briefly reviews the current understanding of vapour-particle partitioning of PAHs and the PAH deposit

223 atrix, resulting in films with reduced water vapour permeability (3.48x10(-11)(g/msPa)), increased hy

224 grease barrier properties and reduced water vapour permeability (WVP) after the addition of cellulos

225 Ch drastically reduced the water vapour permeability (WVP) and solubility of gelatin film

226 Tensile strength (TS) and water vapour permeability (WVP) of films decreased, but elonga

227 osan-fish gelatin matrix decreased the water vapour permeability by more than 30%.

228 The percentage of elongation and the water vapour permeability increased while tensile strength, Yo

229 The vapour permeability is weakly affected by irradiation.

230 increased thermal conductivity and decreased vapour permeability of the structured region allows this

231 n of epicatechin was found to increase water vapour permeability significantly to 2.3 g mm/m(2)h kPa

232 for SPI alone whereas rutin decreased water vapour permeability to 1.2 g mm/m(2)h kPa.

233 ased with citral incorporation but the water vapour permeability was not affected by either citral or

234 The water vapour permeability was similar to that of the control f

235 membranes (e.g. O2 and CO2 diffusion, water vapour permeability), which is a key parameter to manage

236 phology (TEM), hygroscopic properties (water vapour permeability, hydrophobicity, sorption isotherms)

237 of the resulting films but not in its water vapour permeability.

238 In this work, a "bio-electronic nose" for vapour phase detection of odorant molecules based on sur

239 paper, we present an array of biosensors for vapour phase detection of odorant molecules based on sur

240 foliated flakes WS2 and MoS2 by metalorganic vapour phase epitaxy.

241 d covers mesosilica and its interaction with vapour phase organic pollutants under the general subjec

242 Here, we report the controlled vapour phase synthesis of molybdenum disulphide atomic l

243 organic compounds that were released in the vapour phase, but no significant difference in the sodiu

244 for the removal of organic pollutants in the vapour phase.

245 f water/TiO2 interfaces involve water in the vapour phase.

246 ed graphene, intermediate seed materials and vapour-phase deposition at high temperature(,) have only

247 e preparation of NHC films in solution or by vapour-phase deposition from the solid state.

248 The ability to prepare these films by vapour-phase deposition permitted the analysis of the fi

249 The ease of vapour-phase deposition, applicability to high-resolutio

250 immobilisation of alcohol dehydrogenase into vapour-phase polymerised poly(3,4-ethylene dioxythiophen

251 eterostructures by in situ modulation of the vapour-phase reactants during growth of these two-dimens

252 ents in Beijing shows that atmospheric water vapour plays a critical role in enhancing the heavy haze

253 rmed ionic bond is stable up to 5 Torr water vapour pressure as shown by APXPS.

254 roperties namely: molar mass, melting point, vapour pressure at 20 degrees C, n-octanol-water partiti

255 emes of heat, light intensity (PAR) and high vapour pressure deficit (VPD).

256 titative dependencies of chi on temperature, vapour pressure deficit and elevation; and that these sa

257 o maintain a stable ci/ca ratio because both vapour pressure deficit and temperature were decreased u

258 High atmospheric vapour pressure deficit implies low ci /ca in dry climat

259 and showed a temporal pattern independent of vapour pressure deficit or temperature, because of endog

260 pendency of ci /ca ratios on temperature and vapour pressure deficit, and observed relationships of l

261 Light quantity and quality, vapour pressure deficit, soil water content, and CO2 con

262 Despite the high vapour pressure of methanol, the solar cells are stable

263 The vapour pressure, the molecular weight, the Odor Activity

264 Exposure to deuterated water vapour produced an equivalent deuteride signal at the me

265 hermodynamic cycle, most famously the liquid-vapour Rankine cycle used for steam engines.

266 zed water-ice grains are the usual result of vapour recondensation in ice-free layers, the occurrence

267 In the lower stratosphere, our water vapour record extends back to 1988 and water vapour conc

268 rs, but the sources and compositions of such vapours remain unknown.

269 If magmas are vapour-saturated before eruption, bubbles cause the magm

270 ured in the subsurface atmosphere under near vapour-saturation conditions and without significant int

271 The trimethylamine vapour sensing property of the film was studied by the c

272 lorimetric sensors can be tuned for numerous vapour sensing scenarios in confined areas or as individ

273 Combining vapour sensors into arrays is an accepted compromise to

274 ures/topology of MOFs and the associated gas/vapour separation performance.

275 the need for substrate pre-treatment, via a vapour-solid mechanism enabled using an aerosol-assisted

276 tures from 22 to 50 degrees C and by dynamic vapour sorption (DVS) and dynamic dewpoint sorption (DDS

277 en by water molecules either in liquid or in vapour state.

278 ysical adsorption of halogenated hydrocarbon vapours, such as dibromomethane, the adsorption isotherm

279 Tin oxide nanorods (NRs) are vapour synthesised at relatively lower temperatures than

280 ucleated particles and find that the organic vapours that drive initial growth have extremely low vol

281 hoscopic techniques including valves, coils, vapour thermal ablation, and sclerosant agents have been

282 Use of vapour thermal energy or a sclerosant might allow focal

283 he extreme volume change accompanying liquid vapour transition.

284 The rate of water vapour transmission of the films decreased with citral i

285 pitation over this region is southerly water vapour transport associated with the Asian summer monsoo

286 Here we show that water vapour transport has higher medium-range predictability

287 rown by lateral heteroepitaxy using physical vapour transport, are visible in an optical microscope a

288 association between precipitation and water vapour transport, especially for extreme events, we conc

289 vents have been connected with intense water vapour transport.

290 we demonstrate this possibility in an atomic vapour using optical three-dimensional Fourier-transform

291 Periodic condensations of water vapour very close to, or on, the surface were suggested

292 It was previously concluded that water vapour was generated in ice-rich subsurface layers with

293 The anti-yeast activity of mentha oil and vapours was evaluated against 8 food spoiling yeasts thr

294 h a spatially modulated profile into lithium vapour, which results in an annular region of ionization

295 Thermal atomic vapours, which present a simple and scalable resource, h

296 We efficiently generate water vapour with solar thermal conversion efficiency up to 57

297 for reactions of lower molecular weight PAH vapour with these species as well as for heterogeneous r

298 xposed to atmospheres containing methylamine vapours with concentrations over the range 2-10 ppm at r

299 y driven by iodine oxoacids and iodine oxide vapours, with average oxygen-to-iodine ratios of 2.4 fou

300 e-conductive equilibrium, the required water vapour would need to be supersaturated by many orders of