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1 rts-per-thousand levels of atmospheric water vapour.
2 into pure (99.9%) liquid antimony and sulfur vapour.
3 ying a magmatic reservoir with vol% exsolved vapour.
4 ed inside the confined area is released as a vapour.
5 rent to greenhouse gases, most notably water vapour.
6 purpose of modulating the alkali background vapour.
7 nt repeatability in exposure to the methanol vapour.
8 l membranes and is less susceptible to water vapour.
9 c conditions, as well as for saturated argon vapour.
10 alysis of volatile and semi-volatile organic vapours.
11 lei originate from nucleation of atmospheric vapours.
12 differentiation between different gases and vapours.
13 n-3-ol (octenol) and R-(-)-carvone (carvone) vapours.
14 from monoterpenes in mixtures of atmospheric vapours.
15 ly assign enrolled patients 2:1 to segmental vapour ablation (treatment group) or standard medical ma
17 tandard medical management, targeted thermal vapour ablation of more diseased segments and preservati
19 ions of tropospheric O3 precursors and water vapour abundance determine the climate response of oxida
21 ovide new estimates of impact-produced H(2)O vapour abundances for models investigating termination o
22 nditions in winter, air pollutants and water vapour accumulate in a shallow planetary boundary layer
23 rmining D, based on measuring both the water vapour adsorption isotherm of a given substance, and its
24 rated by their performances in water/organic vapour adsorption, as well as long-term ultrastability u
27 ixing of the fluid phase to form an H2O-rich vapour and a hydrosaline phase in equilibrium with the s
28 bedo: and bulk surface conductance for water vapour and decreases aerodynamic surface temperature.
29 h it; it is a key component of all life; its vapour and droplets fill the lower atmosphere; and even
30 2O3-delta (BSCF) in the presence of both H2O vapour and electron irradiation using environmental tran
31 be the sources of the observed jets of water vapour and icy particles and to exhibit higher temperatu
32 how temporal variations of atmospheric water vapour and its isotopic composition (delta(18) OV ) infl
33 ater exists in many forms, including liquid, vapour and numerous crystalline and amorphous phases of
35 grees C and assessed for their colour, water vapour and oxygen transfer rate, textural, functional gr
37 ation-driven ITCZ dynamics may provoke water vapour and vegetation feedbacks in northern mid-latitude
43 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
50 th two spectroscopic techniques, namely cold vapour atomic absorption spectroscopy (CV-AAS) and a dir
53 stallization and sequestration of CO(2) into vapour bubbles, producing spurious barometric estimates.
54 moisture conditions to (18) O-depleted water vapour (c. - 200 per thousand) at high relative humidity
55 te that millions of strontium atoms from the vapour can be captured in a magneto-optical trap (MOT).
56 +5 degrees Celsius, nitric acid and ammonia vapours can condense onto freshly nucleated particles as
57 d their oxidation in mixtures of atmospheric vapours can suppress both particle number and mass of se
58 ted for in the measurement of sulphuric acid vapour, can participate in the growth process, leading t
59 eved by exposing non-vdW solids to chalcogen vapours, can be controlled using the enthalpies and vapo
62 as water (for example, a 100 per cent water vapour composition), or it could contain high-altitude c
63 technology mostly involves the conventional vapour compression cycle, but the materials used in this
64 , USA shows increases in stratospheric water vapour concentrations that cannot be fully explained by
65 n (curvature) effect, which inhibits organic vapour condensation on the smallest particles (the nano-
66 ticles can grow by sulfuric acid and organic vapour condensation to diameters sufficiently large to p
67 to cloud droplets under supersaturated water vapour conditions is described by classic Kohler theory.
69 studies predict that low-volatility organic vapours contribute during initial growth, direct evidenc
72 ve evaluation on how the evaporating solvent vapour could prevent or disrupt water vapor condensation
73 ve shown that an active packaging, using RTO vapours, could be employed, by the citrus industry, to e
74 optical properties of metalorganic chemical vapour deposited (MOCVD) InGaN/GaN multiple quantum well
75 rical specimens, with electron beam physical vapour deposited coatings, were tested with internal coo
76 conductivity mapping of large area chemical vapour deposited graphene films on sapphire, silicon dio
77 d our analysis shows that the doped chemical vapour deposited graphene has good optical properties in
79 isualization of grain boundaries in chemical vapour deposited monolayer MoS2 samples with multiphoton
82 el considered here, structures that arise in vapour-deposited materials are statistically identical t
86 of p-doping exhibited in large area chemical vapour deposition (CVD) graphene field effect transistor
87 e have fabricated and characterised chemical vapour deposition (CVD) graphene Hall sensors with wire
88 phene-based microwave devices using Chemical Vapour Deposition (CVD) graphene whose sheet resistance
89 The origin of electron transfer at Chemical Vapour Deposition (CVD) grown monolayer graphene using a
91 dy, we have demonstrated the use of chemical vapour deposition (CVD) grown-graphene to develop a high
93 eview focuses on the solution based chemical vapour deposition (CVD) of main group materials with par
94 nstrate that in an oxygen-activated chemical vapour deposition (CVD) process, half-millimetre size, B
95 ificantly up-scaled the traditional chemical vapour deposition (CVD) production for NPs from mg level
96 synthesized on Pt and Cu foil using chemical vapour deposition (CVD), multilayer h-BN is still absent
99 um and low cost Electrostatic Spray Assisted Vapour Deposition (ESAVD) method has been used to produc
101 k investigates the compatibility of physical vapour deposition (PVD) techniques with a flexible comme
103 -of-the-art growth methods based on chemical vapour deposition allow the synthesis of one-centimetre-
104 at is observed in graphene grown by chemical vapour deposition and at the LaAlO3-SrTiO3 interface, ma
105 y stable 2H phase, thus in standard chemical vapour deposition and vapour transport processes the mat
106 ther the ultra-stable glassy films formed by vapour deposition are ever equivalent to those obtained
107 s incorporated using a low-pressure chemical vapour deposition followed by the decoration of iron nan
108 Here we present a computational study of vapour deposition for a two-dimensional glass forming li
109 s (as-transferred and post-annealed chemical vapour deposition grown monolayer graphene, monolayer gr
111 lass films prepared by a process of physical vapour deposition have been shown to have thermodynamic
112 ectrochemistry of graphene grown by chemical vapour deposition in two-dimensional and three-dimension
113 defects in graphene synthesized by chemical vapour deposition limits its application in biosensing.
114 ike nanowires were synthesized by a chemical vapour deposition method on Si substrates treated withou
116 and chemical (atomic layer deposition, ALD) vapour deposition methods as a functional coating for la
117 e that uses millimetre-scale direct chemical vapour deposition of MoS2 followed by lithographic defin
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 ultrasmall amounts if performed by chemical vapour deposition or advanced synthetic organic methods,
121 lied by physical vapour deposition, chemical vapour deposition or the tip of a scanning tunnelling mi
123 phene, which is primarily rooted in chemical vapour deposition production at elevated temperatures, r
124 cancy in mechanical exfoliation and chemical vapour deposition samples to molybdenum antisite in phys
127 th a newly developed, metal-organic chemical vapour deposition technique, and show high electrical pe
131 layer of diamond using hot filament chemical vapour deposition to produce 'black diamond' (bD) nanost
132 rt the synthesis, by laser-assisted chemical vapour deposition(5), of centimetre-scale, free-standing
133 trapyrroles with metals supplied by physical vapour deposition, chemical vapour deposition or the tip
135 ges over conventional materials deposited by vapour deposition, enabling a path to highly scaled elec
136 hniques such as liquid exfoliation, chemical vapour deposition, mechanical exfoliation, hydrothermal
137 pproach, using graphene obtained by chemical vapour deposition, which allows a proton-deuteron separa
138 apsulated layered Bi2O2Se, grown by chemical vapour deposition, which demonstrate excellent air stabi
149 eoretical modelling, we show how to maximize vapour diffusion fluxat the apex of convex millimetric b
150 s falls is best explained by grain growth by vapour diffusion in ice-rich layers, or by sintering.
154 hanism for the oxidation of uranium in water vapour environments where the transport of hydroxyl spec
155 ation between liquid and vapour, followed by vapour escape during accretionary growth of planetesimal
157 activity and polyphenols were quantified in vapour-extracted juice of nine Austrian, partially endem
159 r, isotopic fractionation between liquid and vapour, followed by vapour escape during accretionary gr
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 porosity (or diffusive conductance to water vapour g(s) ) and CO(2) assimilation rate (A) applies to
166 SunBOTs can, in principle, be used in solar vapour generation devices, as it achieves up to a 400% s
168 ticles over continents, whereas iodine oxide vapours have been implicated in particle formation over
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
174 istribution of gases such as ozone and water vapour in the stratosphere - which affect surface climat
175 pristine conditions but also quantify these vapours in mixtures, and when blended with a variable mo
176 rs that not only selectively detect separate vapours in pristine conditions but also quantify these v
177 osol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamb
178 ew particle formation (NPF) from condensable vapours in the free troposphere has been suggested to co
179 ditions that investigate the role of organic vapours in the initial growth of nucleated organic parti
184 of reactions occurring at the aqueous phase-vapour interface compared with the bulk aqueous phase.He
186 ectly heat high-salinity brines at the water/vapour interface of the membrane distillation element, a
189 on of heavy haze: (1) the dispersal of water vapour is constrained by the shallow PBL, leading to an
193 The nucleation of sulfuric acid and organic vapours is thought to be responsible for the formation o
195 bsorption to variations in atmospheric water vapour, leading to an underestimation in the shortwave a
196 self-amplification mechanism in which water vapour leads to a trapping and massive increase of parti
200 owth of the nanowires was in accordance with vapour-liquid-solid mechanism, followed by Ostwald ripen
203 er of the substrate (and oxygen) between the vapour-liquid-solid tri-phase system and to the surface
204 e of substantial (about 40 per cent by mass) vapour loss from growing planetesimals by this mechanism
205 nction (the point at which solid, liquid and vapour meet) and the nucleation site of each new layer o
206 drules in CB chondrites probably formed in a vapour-melt plume produced by a hypervelocity impact wit
208 e associated with the formation of a dynamic vapour nanobubble around the spaser that leads to giant
210 th is primarily due to more abundant organic vapours of slightly higher volatility (saturation concen
211 fferent organic solvents as their respective vapours or when the solid forms are subject to grinding.
213 of zeolites and MOFs in the sensing of water vapour, oxygen, NOx, carbon monoxide and carbon dioxide,
214 grease barrier properties and reduced water vapour permeability (WVP) after the addition of cellulos
216 The percentage of elongation and the water vapour permeability increased while tensile strength, Yo
218 n of epicatechin was found to increase water vapour permeability significantly to 2.3 g mm/m(2)h kPa
220 ased with citral incorporation but the water vapour permeability was not affected by either citral or
222 membranes (e.g. O2 and CO2 diffusion, water vapour permeability), which is a key parameter to manage
223 phology (TEM), hygroscopic properties (water vapour permeability, hydrophobicity, sorption isotherms)
225 In this work, a "bio-electronic nose" for vapour phase detection of odorant molecules based on sur
226 minerals yields H(2) that partition into the vapour phase during decompressional boiling of ascending
228 omplete silanisation of the substrate in the vapour phase followed by site-selective oxygen plasma tr
230 n micro-ring resonator (GOMRR) to a range of vapour phase Volatile Organic Compounds (VOCs) is report
232 organic compounds that were released in the vapour phase, but no significant difference in the sodiu
234 ed graphene, intermediate seed materials and vapour-phase deposition at high temperature(,) have only
238 umper (SJ) area of YNP that are sourced with vapour-phase gas and with the most H(2) in YNP were exam
240 sing techniques such as exfoliation(1-3) and vapour-phase growth(4,5), it is still challenging to obt
241 eterostructures by in situ modulation of the vapour-phase reactants during growth of these two-dimens
243 ents in Beijing shows that atmospheric water vapour plays a critical role in enhancing the heavy haze
246 ored at 5 degrees C, in either a low or high vapour pressure deficit (VPD) environment, to determine
248 titative dependencies of chi on temperature, vapour pressure deficit and elevation; and that these sa
249 o maintain a stable ci/ca ratio because both vapour pressure deficit and temperature were decreased u
251 ability and of the increased temperature and vapour pressure deficit caused by land-atmosphere intera
252 and showed a temporal pattern independent of vapour pressure deficit or temperature, because of endog
253 of chi predicted from growth temperature and vapour pressure deficit were closely correlated to ratio
254 ptimal chi as a function of air temperature, vapour pressure deficit, c(a) and atmospheric pressure.
257 -d before measurement), solar irradiance and vapour pressure deficit, with growth T having the strong
258 alized our measures of WUE across a range of vapour pressure deficits using g(1) , which is a paramet
263 n high-temperature applications at low water vapour pressures where the zeolite framework is generall
267 zed water-ice grains are the usual result of vapour recondensation in ice-free layers, the occurrence
268 ensing applications, especially for chemical vapour remote detection and future air quality monitorin
269 posure to the methanol, ethanol and propanol vapours, respectively, in the atmosphere condition.
271 ured in the subsurface atmosphere under near vapour-saturation conditions and without significant int
272 lorimetric sensors can be tuned for numerous vapour sensing scenarios in confined areas or as individ
276 the need for substrate pre-treatment, via a vapour-solid mechanism enabled using an aerosol-assisted
278 ysical adsorption of halogenated hydrocarbon vapours, such as dibromomethane, the adsorption isotherm
280 high-altitude increase in atmospheric water vapour that was more pronounced at high northern latitud
281 ucleated particles and find that the organic vapours that drive initial growth have extremely low vol
282 hoscopic techniques including valves, coils, vapour thermal ablation, and sclerosant agents have been
284 ice cloud formation, which may confine water vapour to lower altitudes through gravitational fall and
288 -air heat exchanges, modifying in turn ocean vapour transport over land and land surface temperatures
289 s in standard chemical vapour deposition and vapour transport processes the materials normally grow i
290 rown by lateral heteroepitaxy using physical vapour transport, are visible in an optical microscope a
291 association between precipitation and water vapour transport, especially for extreme events, we conc
294 h a spatially modulated profile into lithium vapour, which results in an annular region of ionization
297 xposed to atmospheres containing methylamine vapours with concentrations over the range 2-10 ppm at r
298 affect the distribution of atmospheric water vapour, with potential implications for the atmospheric
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