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1 ded with n-dodecane, a high molecular weight volatile organic compound.
2 ation tests, imaging, and breath analysis of volatile organic compounds.
3 clei for the condensation of atmospheric low-volatile organic compounds.
4 d responsive turn-on fluorescence to various volatile organic compounds.
5 lds from photochemical oxidation of biogenic volatile organic compounds.
6 sing sensitivity toward more polar or acidic volatile organic compounds.
7 ng aerosol growth in the presence of gaseous volatile organic compounds.
8 ds, redox cofactor side chains, and biogenic volatile organic compounds.
9 4 +/- 1.2% of the concentration of speciated volatile organic compounds.
10 cluding ammonia, hydrogen sulfide (H2S), and volatile organic compounds.
11 promising materials for sensing of gases and volatile organic compounds.
12 evaluated by injection of mixtures of common volatile organic compounds.
13 nd arrayed ChIMES sensors against a suite of volatile organic compounds.
14 The use of CFEs impacted on the profile of volatile organic compounds.
16 onoxide and carbon dioxide, hydrocarbons and volatile organic compounds, ammonia, hydrogen sulfide, s
18 for nine different SOA types (i.e., distinct volatile organic compound and oxidant pairs) encompassin
21 suggests that long-term exposure to ambient volatile organic compounds and nitrogen dioxide at relat
22 include greenhouse gases, ozone precursors (volatile organic compounds and nitrogen oxides), air tox
23 nosheets, detection of an extensive range of volatile organic compounds and small molecules important
24 sequencing) and their metabolic by-products (volatile organic compounds) and de novo lipogenesis (usi
25 ctions of sunlight with emitted NOx species, volatile organic compounds, and hydroxyl radicals are ce
26 em, and so all of the gases from combustion, volatile organic compounds, and particulate emissions ar
29 y explored the role of chemical pigments and volatile organic compounds as cues for pollinators, but
30 ble of sensing and differentiating gases and volatile organic compounds at part-per-million and part-
31 eriments studying the chemical reactivity of volatile organic compounds at the air/water interface.
32 l rate coefficients for a number of relevant volatile organic compounds at various energetic conditio
36 -3-buten-2-ol (MBO) is an important biogenic volatile organic compound (BVOC) emitted by pine trees a
37 Nitrate radical (NO3) oxidation of biogenic volatile organic compounds (BVOC) is important for night
38 4% to the global carbon emission of biogenic volatile organic compounds (BVOCs) and can be responsibl
39 nsiderable amounts and varieties of biogenic volatile organic compounds (BVOCs) are exchanged between
40 ecies in SOA formed by oxidation of biogenic volatile organic compounds (BVOCs) at the single particl
41 k, basal emission factors (BEFs) of biogenic volatile organic compounds (BVOCs) obtained by Eddy Cova
43 osol (SOA) mass in the oxidation of biogenic volatile organic compounds (BVOCs) through accretion rea
45 s from NO3 oxidation of a series of biogenic volatile organic compounds (BVOCs), consisting of five m
50 del calculations show that sCI from biogenic volatile organic compounds composed the majority of the
51 formation occurs when oxidation products of volatile organic compounds condense onto pre-existing pa
52 for the first time 51 gunshot residue (GSR) volatile organic compounds could be simultaneously detec
54 predominantly at remediation of chlorinated volatile organic compounds (cVOCs) and perfluoroalkyl ac
56 imination between both groups, with 81 fecal volatile organic compounds detected at significantly dif
57 yrosequenced targeting 16S ribosomal RNA and volatile organic compounds determined by solid-phase mic
58 sible changes in resistance upon exposure to volatile organic compounds due to absorption/desorption
59 ompounds are often referred as extremely low-volatile organic compounds (ELVOCs), and thus, they are
60 nt source of indoor and outdoor particle and volatile organic compound emissions with potential delet
62 ] applied under elevated [CO2]), we analyzed volatile organic compound emissions, photosynthetic perf
63 ficant differences in the composition of the volatile organic compounds emissions between PFI and GDI
65 A metabolomic study was conducted on the volatile organic compounds emitted by abscising fruitlet
66 were asked to follow various protocols while volatile organic compounds emitted from their breath, sw
70 hygiene products, perfume, laundry supplies, volatile organic compounds, etc.) do not generate an arr
71 scores with carbon dioxide, ventilation, and volatile organic compound exposures in office workers: a
72 this study the application of fatty acid and volatile organic compound fingerprinting in combination
73 ct herbivory, plants emit elevated levels of volatile organic compounds for direct and indirect resis
75 his study the first computer simulation of a volatile organic compound (formaldehyde) at the air/wate
76 evaluation of the impact of fermentation on volatile organic compounds formation during sourdoughs r
77 ehavior of a mixture of 14 volatile and semi-volatile organic compounds (four aromatic hydrocarbons (
79 f individual substances from a mixture of 23 volatile organic compounds from four chemical groups was
83 vestigate how heat waves affect emissions of volatile organic compounds from urban/suburban vegetatio
84 e fraction is formed by complex reactions of volatile organic compounds, generating secondary organic
87 of SDI has been demonstrated for analysis of volatile organic compounds in air at high sensitivity, w
89 MS) allows for quantitative determination of volatile organic compounds in real time at concentration
92 c alkenes, which are among the most abundant volatile organic compounds in the atmosphere, are readil
93 glyoxal, one of the most abundant oxygenated volatile organic compounds in the atmosphere, on the str
95 important products of gas-phase oxidation of volatile organic compounds in the troposphere; some mode
96 and hydrogen (delta(2)H) isotope analysis of volatile organic compounds in water at concentrations of
98 of chlorine chemistry in the degradation of volatile organic compounds, including the greenhouse gas
99 uced in a flow tube reactor by ozonolysis of volatile organic compounds, including the monoterpenes a
100 reared on irHER1 plants, which released less volatile organic compounds (indirect defense) and had st
101 sed sensors that transduce the sorption of a volatile organic compound into a resistance change.
102 mation was obtained for NH3, CO2, water, and volatile organic compounds levels, illustrating a human
105 lem, mainly because fewer particles and less volatile organic compounds, methane and carbon monoxide
106 ssions of carbon monoxide (CO) and non-CH(4) volatile organic compounds (NMVOC) warm by increasing bo
107 An increase in the detection sensitivity for volatile organic compounds of between 1 and 2 orders of
108 ation of atmospheric gases such as SO2, NO2, volatile organic compounds, organic and inorganic acids,
109 bservations from other shale plays, elevated volatile organic compounds, other than CH4 and C2H6, wer
111 C isotopic composition of several oxygenated volatile organic compounds (OVOCs) from direct sources a
112 radiation and photoproduction of oxygenated volatile organic compounds (OVOCs) from various types of
114 Arctic shipboard observations of oxygenated volatile organic compounds (OVOCs) such as organic acids
115 howing the significant influence of biogenic volatile organic compound oxidation above the forested r
116 and bromine atoms controls the prevalence of volatile organic compounds, ozone, and mercury in the Ar
120 omyces and Saprochaete were investigated for volatile organic compound production using HS-SPME-GC/MS
121 as fabricated to detect methyl salicylate, a volatile organic compound released by pathogen-infected
122 been identified as one of the most important volatile organic compounds released by plants during a b
123 sol is formed through gas-phase oxidation of volatile organic compounds, so-called secondary organic
125 dation is a viable control strategy for most volatile organic compounds, specifically those with a OH
129 e aerosol are also observed upon exposure to volatile organic compounds such as terpenes and near-UV
130 nsists of studying the diffusion of selected volatile organic compounds (such as naphthalene) release
131 e, which often exists in mixtures with other volatile organic compounds, such as toluene and xylene (
135 ogical properties and in the amount of aroma volatile organic compounds that were released in the vap
136 nvironments and reacts rapidly with biogenic volatile organic compounds to form secondary organic aer
137 measurements of NOx, CO2, CO and non methane volatile organic compound tracers in a city that might b
140 ater and sensor channels to perform advanced volatile organic compound (VOC) detection and mixture an
142 oportionally contribute to total methane and volatile organic compound (VOC) emissions from the produ
143 o the sea surface, thereby matching observed volatile organic compound (VOC) emissions to the atmosph
144 increased temperatures cause higher biogenic volatile organic compound (VOC) emissions, which in turn
145 roducts (iox) of isoprene, the most abundant volatile organic compound (VOC) emitted by vascular plan
146 pture, identification, and quantification of volatile organic compound (VOC) patterns in human breath
148 farnesyl diphosphate to trichodiene (TD), a volatile organic compound (VOC), catalysed by a sesquite
149 ation in a polluted marine environment under volatile organic compound (VOC)-limited conditions assoc
151 les result from the condensation of oxidized volatile organic compounds (VOC) and consist of a comple
152 s an original analytical system for studying volatile organic compounds (VOC) coming from the heating
153 ERMOD) and a spatially resolved inventory of volatile organic compounds (VOC) emissions from natural
154 ormance against AMDIS results when analysing volatile organic compounds (VOC) from standard mixtures
157 acer carbon monoxide (CO, up to 57 ppmv) and volatile organic compounds (VOCs) along the pilgrimage r
158 lustrate the capabilities of this system for volatile organic compounds (VOCs) analysis, we subjected
159 gh this source clearly contributes to indoor volatile organic compounds (VOCs) and influences indoor
160 affect emissions of greenhouse gases (GHG), volatile organic compounds (VOCs) and nitrogen oxides (N
161 of gas-phase organic carbon, which includes volatile organic compounds (VOCs) and other compounds wi
163 e the potential to strongly influence floral volatile organic compounds (VOCs) and, in turn, plant-po
165 tigations of cellular processes initiated by volatile organic compounds (VOCs) are limited when model
168 pills by evaluating the "fingerprint" of the volatile organic compounds (VOCs) associated with indivi
169 analytes of interest in this review are (a) volatile organic compounds (VOCs) associated with securi
170 ht can lead to fast uptake of noncondensable Volatile Organic Compounds (VOCs) at the surface of part
171 improves the detection and identification of volatile organic compounds (VOCs) by a colorimetric sens
172 aboratory apparatus to measure the uptake of volatile organic compounds (VOCs) by soot particles.
173 ts primarily based on the rich repertoire of volatile organic compounds (VOCs) derived from the yeast
174 rticles less than 100 nm) and some hazardous volatile organic compounds (VOCs) during printing, altho
176 rosol (SOA) is formed in the atmosphere when volatile organic compounds (VOCs) emitted from anthropog
178 nmental applications including monitoring of volatile organic compounds (VOCs) emitted from natural a
183 und emission rates (E) for 69-89 nonbiogenic volatile organic compounds (VOCs) for each of four surfa
185 ylindrical adsorber during the adsorption of volatile organic compounds (VOCs) from a gas stream onto
186 (HS) system was used to generate vapor-phase volatile organic compounds (VOCs) from a pigpen slurry s
187 vapor intrusion assume that the transport of volatile organic compounds (VOCs) from a source toward a
188 e the emissions of climate-relevant biogenic volatile organic compounds (VOCs) from boreal and subarc
189 t the mechanisms underlying the treatment of volatile organic compounds (VOCs) from industrial off-ga
190 vealed highly enhanced atmospheric levels of volatile organic compounds (VOCs) from primary emissions
192 in emissions of nitrogen oxides (NO(x)) and volatile organic compounds (VOCs) from the fires tend to
193 were used to study uptake of traffic-related volatile organic compounds (VOCs) from urban bicycling.
194 heric chemistry (WRF-Chem) with emissions of volatile organic compounds (VOCs) from vegetation simula
196 have estimated that animal feed emissions of volatile organic compounds (VOCs) have greater O(3) form
197 e the area-specific emission rates (SERs) of volatile organic compounds (VOCs) in a collection of twe
199 the value and classification rate of exhaled volatile organic compounds (VOCs) in asthma diagnosis.
200 Real-time measurements of many low-abundance volatile organic compounds (VOCs) in breath and air samp
203 This was achieved by online sampling of the volatile organic compounds (VOCs) in close vicinity to t
205 agnosis of cancer relies on the detection of volatile organic compounds (VOCs) in exhaled breath samp
206 Brucella exposure that is based on profiling volatile organic compounds (VOCs) in exhaled breath.
208 MOF coating opens the way for the sensing of volatile organic compounds (VOCs) in gaseous media.
209 MS) is a well-known technology for detecting volatile organic compounds (VOCs) in gaseous samples.
210 r in situ analysis and on-site monitoring of volatile organic compounds (VOCs) in moderately complex
211 rum acquisition has allowed the detection of volatile organic compounds (VOCs) in olive oil samples,
212 loped for highly sensitive analysis of trace volatile organic compounds (VOCs) in the atmosphere.
213 e is the major source and sink of nonmethane volatile organic compounds (VOCs) in the atmosphere.
215 ) has been applied for the quantification of volatile organic compounds (VOCs) in the headspace vapor
216 S) has been applied to the quantification of volatile organic compounds (VOCs) in the headspace vapor
218 en used to detect and quantify the following volatile organic compounds (VOCs) in water: 1,1,1,2-tetr
221 predict adsorption equilibria of n-component volatile organic compounds (VOCs) mixture from single co
224 dy, we profiled the exhaled breath (~450 mL) volatile organic compounds (VOCs) of 47 healthy voluntee
226 sed to create sensors capable of identifying volatile organic compounds (VOCs) on the basis of their
227 m of this study was to determine whether the volatile organic compounds (VOCs) pattern in colorectal
229 has been developed for concentrating gaseous volatile organic compounds (VOCs) prior to gas chromatog
230 wth-stimulating effects are partly caused by volatile organic compounds (VOCs) produced by the bacter
231 nt of emission ratios of a selected group of volatile organic compounds (VOCs) relative to carbon mon
232 hers, these decomposition byproducts include volatile organic compounds (VOCs) responsible for the od
234 ide (SO2), hydrogen (H2), methane (CH4), and volatile organic compounds (VOCs) such as ethylmercaptan
235 ction based on chemical analysis of released volatile organic compounds (VOCs) that emanate from infe
236 Plants synthesize an amazing diversity of volatile organic compounds (VOCs) that facilitate intera
238 that ozone did react with printer-generated volatile organic compounds (VOCs) to form secondary orga
240 station air is currently monitored for trace volatile organic compounds (VOCs) using gas chromatograp
242 etween emulsion structure and the release of volatile organic compounds (VOCs) was investigated using
248 levels of particulate matter (PM2.5) and 58 volatile organic compounds (VOCs) were monitored during
249 -0.54 degrees C for 8 days during which time volatile organic compounds (VOCs) were monitored using S
251 ed enhancements in several potentially toxic volatile organic compounds (VOCs) when compared to backg
252 trometry instrument was used for analysis of volatile organic compounds (VOCs) within exhaled breath
254 ogen oxides (NOx), carbon monoxide (CO), and volatile organic compounds (VOCs)) from East Asia and ex
255 or biological drug delivery, and sensors for volatile organic compounds (VOCs), among many others.
256 ), brown carbon (BrC), carbon dioxide (CO2), volatile organic compounds (VOCs), and polychlorinated d
257 h are formed in the air photochemically from volatile organic compounds (VOCs), declined only 20-21%.
258 ygen concentration, concentration of initial volatile organic compounds (VOCs), energy density, plasm
259 arkers in exhaled breath condensate, exhaled volatile organic compounds (VOCs), gene expression, and
261 for polycyclic aromatic hydrocarbons (PAHs), volatile organic compounds (VOCs), particulate matter (P
262 ns was quantified, including CO(2), PM(2.5), volatile organic compounds (VOCs), polyaromatic hydrocar
264 y was at first applied to the analysis of 31 volatile organic compounds (VOCs), such as alcohols, phe
265 CDFs), polyaromatic hydrocarbons (PAHs), and volatile organic compounds (VOCs), were sampled from dif
266 h affect Nr gas-aerosol partitioning, and of volatile organic compounds (VOCs), which affect oxidant
267 ions of nitrogen oxides (NOx = NO + NO2) and volatile organic compounds (VOCs), whose photochemistry
286 tive of Conventional [high concentrations of volatile organic compounds (VOCs)] and Green (low concen
287 bilities for classification and detection of Volatile Organic Compounds (VOCs, i.e., ethanol, CH(2)Cl
288 ogen dioxide (NO2), sulfur dioxide (SO2) and volatile organic compounds (VOCs, such as benzene, tolue
289 fective chemical sensors for detecting small volatile-organic compounds (VOCs) have widespread applic
290 significant global sources of small oxidized volatile organic compounds, VOCs (e.g., methanol and ace
291 onally, the concentration of smoking-related volatile organic compounds was measured in dwellings of
292 g and screening of MOS sensors, specific for volatile organic compounds, was performed using fuzzy lo
293 groundwater samples revealed trace levels of volatile organic compounds, well below the Environmental
294 ons to carbon monoxide, nitrogen oxides, and volatile organic compounds were found to be very small (
295 urther, preconceptional exposures to several volatile organic compounds were significantly associated
296 are also most active in inducing release of volatile organic compounds when applied to damaged leave
297 e was evaluated using a mixture of six model volatile organic compounds which showed detection limits
298 ce-based chemical sensor (chemiresistor) for volatile organic compounds whose sensitivity can be reve
299 ation to separate a mixture of plant emitted volatile organic compounds with significantly shortened
300 cals, including NH3, SO2, NO2, H2S, and some volatile organic compounds, with particular emphasis on
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