ライフサイエンスコーパス: organic compounds

1 mpounds (e.g., carbon disulfide, halogenated organic compounds).

2 t sample origins based on the composition of organic compounds.

3 ocks in the synthesis of chemically relevant organic compounds.

4 of CFEs impacted on the profile of volatile organic compounds.

5 al alkane, branched alkane, and cycloalkane) organic compounds.

6 and aliphatic bonds for MnOx(s) reacted with organic compounds.

7 le in the generation of metabolic energy and organic compounds.

8 perspective to the catalytic applications of organic compounds.

9 obial taxa that may degrade a broad suite of organic compounds.

10 rganic guests, linkers, and ligands in metal-organic compounds.

11 our of the models targeted a single class of organic compounds.

12 ause of the destruction of a wide variety of organic compounds.

13 able mirror images (enantiomers) of selected organic compounds.

14 he bioaccumulation potential and toxicity of organic compounds.

15 chnology for chemical monitoring of nonpolar organic compounds.

16 functional interfaces between inorganic and organic compounds.

17 ides and, to a minor extent, associated with organic compounds.

18 tates ((3)HS*), promoting the degradation of organic compounds.

19 uently used to synthesize perfluoroalkylated organic compounds.

20 bic and anaerobic catabolism of a variety of organic compounds.

21 rbon fixation, converting atmospheric CO2 to organic compounds.

22 the condensation of atmospheric low-volatile organic compounds.

23 e pinking and to maintain the levels of main organic compounds.

24 detect transporter-coupled influx/efflux of organic compounds.

25 for the preparation of enantiomerically pure organic compounds.

26 tion and kexp for 31 reactions of Cl(*) with organic compounds.

27 Mg released from minerals gets trapped into organic compounds.

28 ormation may have triggered the formation of organic compounds.

29 d ChIMES sensors against a suite of volatile organic compounds.

30 pplications of bromine, a total of 107 bromo-organic compounds, 11 other brominating agents, and a fe

31 Of the 292 volatile organic compounds, 26 were up-regulated and 2 down-regul

32 ics, we have previously identified the small organic compounds 5-nonyloxytryptamine and vinorelbine a

33 Chemical analyses of ancient organic compounds absorbed into the pottery fabrics from

34 Halogenated organic compounds, also termed organohalogens, were init

35 nd carbon dioxide, hydrocarbons and volatile organic compounds, ammonia, hydrogen sulfide, sulfur dio

36 The DPS, dedicated to organic compounds' analysis, is discussed in terms of it

37 or the biodegradation assay contains regular organic compounds and (13)C-labeled DIC with (13)C atom

38 powerful tool for the structural analysis of organic compounds and biomolecules but typically require

39 g-term storage has the potential to mobilize organic compounds and distribute them between sediments

40 ons without chemical amendments, value-added organic compounds and high rate H2 were also produced.

41 A connection between the evolution of organic compounds and minerals is made, as Mg released f

42 ps that are capable of oxidizing or reducing organic compounds and of generating reactive oxygen spec

43 ese aerosol particles, which are composed of organic compounds and salts, are of great recent interes

44 detection of an extensive range of volatile organic compounds and small molecules important for many

45 uding hydrolysis and acidogenesis of complex organic compounds and sugars into SCCAs, subsequent chai

46 icroorganisms can catabolize a wide range of organic compounds and therefore have the potential to pe

47 als, including proteins, peptides, synthetic organic compounds and, more recently, DNA.

48 ) composed of microbial cells, extracellular organic compounds, and ferric iron minerals.

49 ruction of hazardous chemicals, synthesis of organic compounds, and many other applications are highl

50 chemical mixture consisting of trace metals, organic compounds, and often, high levels of salts.

51 Total nitrogen oxides, volatile organic compounds, and SO2 emissions are similar in the

52 s are a ubiquitous skeleton of pi-conjugated organic compounds, and their incorporation requires synt

53 Plants can interact with a variety of organic compounds, and thereby affect the fate and trans

54 Halogenated organic compounds are also common intermediates in synth

55 Trace organic compounds are important in environmental analysi

56 Extremely low volatile organic compounds are predicted to be the dominant speci

57 Measurements of particle- and gas-phase organic compounds are reported here for the southeastern

58 ssociated with transformations of brominated organic compounds are still poorly explored.

59 thods for the regioselective halogenation of organic compounds are therefore essential in the develop

60 auses changes in the isotopic composition of organic compounds as a result of different vapor pressur

61 d the role of chemical pigments and volatile organic compounds as cues for pollinators, but recent re

62 tage preparation of complex OCF2H-containing organic compounds as well as building blocks for drug di

63 al catalysts is their modification by chiral organic compounds, as most prominently represented by th

64 n of OSPW, which lowers the concentration of organic compounds attributed with toxicity (naphthenic a

65 Thus, soft-ionization energies leading to organic compounds being ionized with limited or no fragm

66 tion energies have been exploited leading to organic compounds being ionized with lower excess intern

67 th of sorption was estimated for three small organic compounds: benzaldehyde, propan-2-ol, and aceton

68 Exchange of atmospheric organic compounds between gas and particle phases is imp

69 Partitioning coefficients of organic compounds between water and supercritical CO2 (s

70 identification of a large number of isomeric organic compounds, both aliphatic and aromatic, between

71 Comprehensive analysis of breath volatile organic compounds (breathomics) provides opportunities f

72 radical (NO3) oxidation of biogenic volatile organic compounds (BVOC) is important for nighttime seco

73 global carbon emission of biogenic volatile organic compounds (BVOCs) and can be responsible for up

74 SOA formed by oxidation of biogenic volatile organic compounds (BVOCs) at the single particle level.

75 Emissions of biogenic volatile organic compounds (bVOCs), are an important element in t

76 formed by the oxidation of biogenic volatile organic compounds (BVOCs).

77 In contrast to soluble compounds, volatile organic compounds can diffuse easily through air- and ga

78 he control, indicating that the oxidation of organic compounds causes the reduction of MnOx(s).

79 eatures in MnOx(s) samples that reacted with organic compounds compared to unreacted MnOx(s).

80 lations show that sCI from biogenic volatile organic compounds composed the majority of the sCIs.

81 n occurs when oxidation products of volatile organic compounds condense onto pre-existing particles.

82 involving sulfuric acid, ammonia, ions, and organic compounds conducted in the CERN CLOUD (Cosmics L

83 There is a growing interest in organic compounds containing the difluoromethyl group, a

84 in redox reactions with surrounding metals, organic compounds, contaminants, and microorganisms.

85 Small organic compounds could be analyzed in water without man

86 minated with a range of chlorinated volatile organic compounds (cVOC).

87 antly at remediation of chlorinated volatile organic compounds (cVOCs) and perfluoroalkyl acids (PFAA

88 Most of VOCs (volatile organic compounds) decreased during withering but few VO

89 cid and nitrogen- containing highly oxidised organic compounds, decreased considerably, which was fol

90 s spectrometric measurements of 20 different organic compounds demonstrate the soft characteristics o

91 spheric deposition, likely via scavenging by organic compounds derived from marine organisms.

92 between both groups, with 81 fecal volatile organic compounds detected at significantly different le

93 ced targeting 16S ribosomal RNA and volatile organic compounds determined by solid-phase microextract

94 y difficult to get preferential transport of organic compounds due to the diffusive nature of their t

95 toxyethanol) and downhole transformations of organic compounds (e.g., carbon disulfide, halogenated o

96 f addition of the low-molecular weight (LMW) organic compounds, easily ionized elements (EIEs), i.e.,

97 te the formation of extremely low volatility organic compounds (ELVOC) from O3 and OH radical oxidati

98 rates are among the extremely low volatility organic compounds (ELVOC) that may play an important rol

99 ith condensation of extremely low-volatility organic compounds (ELVOCs) that have been detected in th

100 ld be classified as extremely low volatility organic compounds (ELVOCs).

101 fferences in the composition of the volatile organic compounds emissions between PFI and GDIs, includ

102 tional data on key externality costs such as organic compounds emissions to water would improve futur

103 Volatile organic compounds emitted from Xoo rice were significant

104 an profoundly affect the fate of condensable organic compounds emitted into the atmosphere by alterin

105 ates for monitoring the behavior of emerging organic compounds (EOCs) in two catchment basins impacte

106 Finally, multiple alcohol-containing organic compounds exerted inhibitory effects on the Nlrp

107 We observed sulfur-containing organic compounds following SO2 perturbations of monoter

108 ed to predict the toxicity of the quantified organic compounds for fresh water organisms in recipient

109 the purification of volatile or semivolatile organic compounds for radiocarbon analysis using acceler

110 but are indistinguishable for many isomeric organic compounds (for example, linear and branched alka

111 to design new materials for sensing volatile organic compounds, for the first time.

112 contributions from extremely low volatility organic compounds formed during alpha-pinene ozonolysis.

113 f a mixture of 14 volatile and semi-volatile organic compounds (four aromatic hydrocarbons (benzene,

114 The abundance of chlorinated organic compounds frequently exceeds chloride in surface

115 Online liquid/liquid extraction of small organic compounds from a drop of biological fluid presen

116 link as the passive addition and removal of organic compounds from a shared seawater reservoir.

117 and higher emissions of nonmethane volatile organic compounds from DICE-Africa.

118 ped a pipeline for obtaining the aqueous and organic compounds from diseased arterial tissue using tw

119 odynamic drive for the abiotic generation of organic compounds from inorganic precursors.

120 Over 280 organic compounds from ten major homologous series were

121 orts also found leaching of growth-promoting organic compounds from the increasingly popular use of p

122 how heat waves affect emissions of volatile organic compounds from urban/suburban vegetation and cor

123 lls are activated through their TCR by small organic compounds generated during microbial vitamin B2

124 The high utility of halogenated organic compounds has prompted the development of a vast

125 ibution to the phototransformation of marine organic compounds has received little attention.

126 Volatile organic compounds have been recognized as important mark

127 to control the site-selectivity because most organic compounds have many similar C-H bonds.

128 Decades of research on the autooxidation of organic compounds have provided fundamental and practica

129 We used halogenated organic compounds (HOC), a chemical class that is ubiqui

130 g the diversity and abundance of halogenated organic compounds (HOCs) accumulating in high trophic ma

131 s) dominate the sorption of many hydrophobic organic compounds (HOCs) in soils and sediments, thereby

132 formation of highly oxidized multifunctional organic compounds (HOMs) from the ozonolysis of three se

133 Highly oxygenated multifunctional organic compounds (HOMs) originating from biogenic emiss

134 Nonvolatile organic compounds identified were polyethylene glycols (

135 icrobial genes involved in degrading complex organic compounds, implying enhanced potential abilities

136 2SO4 > NaCl > NH4Cl > NH4NO3 for the studied organic compounds, implying the following relative stren

137 s been demonstrated for analysis of volatile organic compounds in air at high sensitivity, which is a

138 d for the quantitation and identification of organic compounds in almost any imaginable sample.

139 Brown carbon (BrC) consists of those organic compounds in atmospheric aerosols that absorb so

140 g implies an increased maximum solubility of organic compounds in atmospheric nanoparticles.

141 and appear to be the most abundant class of organic compounds in bottled water but cannot be detecte

142 A fast detection method to analyze gaseous organic compounds in complex gas mixtures was developed,

143 talytic activities for efficiently degrading organic compounds in contaminated water such as harmful

144 etections of diesel range organics and other organic compounds in domestic wells <600 m from unlined

145 sphorescent metal complexes with inexpensive organic compounds in electroluminescent (EL) devices tha

146 ommonly used to describe sorption of neutral organic compounds in environmental systems, but they are

147 The abundance of halogenated organic compounds in flowback fluids rather than older w

148 The inclusion of organic compounds in freshly emitted sea spray aerosol (

149 uction of sulphuric acid and highly oxidized organic compounds in maintaining atmospheric NPF.

150 on of the occurrence of natural, halogenated organic compounds in marine and terrestrial environments

151 pectrometry in negative ion mode to identify organic compounds in nascent sea spray collected through

152 lines the use of bromine and different bromo-organic compounds in organic synthesis.

153 to highlight important aspects of the bromo-organic compounds in organic synthesis.

154 solved concentrations (Cfree) of hydrophobic organic compounds in sediment interstitial water would b

155 The composition of condensed-phase organic compounds in SOA is measured using several compl

156 This study investigates the role of volatile organic compounds in systemic acquired resistance (SAR),

157 ential in defining the oxidation pathways of organic compounds in the atmosphere but is highly challe

158 , which are among the most abundant volatile organic compounds in the atmosphere, are readily oxidize

159 one of the most abundant oxygenated volatile organic compounds in the atmosphere, on the structure, d

160 etabolomic profiles of proteins and volatile organic compounds in the cheese.

161 hemical processes at the origin of water and organic compounds in the early solar system.

162 porewater has been sufficiently advanced for organic compounds in the low- to midrange of hydrophobic

163 DMSO-d6/GL-d8 is more appropriate for organic compounds in which labile protons are not essent

164 -day atmosphere involves ammonia or biogenic organic compounds, in addition to sulfuric acid.

165 pplicable to the conjugation of a variety of organic compounds, including complex drug molecules, wit

166 water treatment systems contain a variety of organic compounds, including end products from the degra

167 ine chemistry in the degradation of volatile organic compounds, including the greenhouse gas methane.

168 Subliming organic compounds into a stream of nitrogen gas and pass

169 Here, the partitioning of numerous organic compounds into solutions of Na2SO4, NH4Cl, and N

170 norganic salts influence the partitioning of organic compounds into the aqueous phase.

171 dge of biotransformation rates for ionizable organic compounds (IOCs) in fish is required to properly

172 The studied PPCPs included several ionogenic organic compounds (IOCs) such as weak acids and weak bas

173 Assessing the biodegradation of organic compounds is a frequent question in environmenta

174 Electrochemical reduction of halogenated organic compounds is gaining increasing attention as a s

175 zing enzymes in the synthesis of chlorinated organic compounds is important, and providing atomistic

176 ghtforward nucleophilic fluoromethylation of organic compounds is reported.

177 d photo-oxidation of intermediate volatility organic compounds (IVOCs).

178 from the atmospheric oxidation of gas-phase organic compounds leading to the formation of particle m

179 We found extremely low volatile organic compounds, likely from sesquiterpene oxidation,

180 Volatile organic compounds may be volatilized from stems or leave

181 Organic compounds occur in some chondritic meteorites, a

182 n "Inverse Drug Discovery" strategy in which organic compounds of intermediate complexity harboring w

183 he number of possible molecular formulas for organic compounds of relative high molecular mass (e.g.,

184 of both particulate and gaseous atmospheric organic compounds on a global scale.

185 The provenance of water and organic compounds on Earth and other terrestrial planets

186 ion Theory (RAST), to bisolute adsorption of organic compounds onto a hyper-cross-linked polystyrene

187 ation (NPF) pathways and the condensation of organic compounds onto particles.

188 ly adopted, however, only when using colored organic compounds or in photocatalyzed processes induced

189 atmospheric gases such as SO2, NO2, volatile organic compounds, organic and inorganic acids, and even

190 nd secondary metabolites, including volatile organic compounds, over a period of 2 yr.

191 o measure the delta(37)Cl of a wide array of organic compounds overcoming limitations of previous tec

192 n and photoproduction of oxygenated volatile organic compounds (OVOCs) from various types of SOA.

193 hipboard observations of oxygenated volatile organic compounds (OVOCs) such as organic acids, key pre

194 ne atoms controls the prevalence of volatile organic compounds, ozone, and mercury in the Arctic lowe

195 The identified halogenated organic compounds, particularly iodinated organic molecu

196 aluation of a comprehensive set of gas-phase organic compounds present in gasoline motor vehicle exha

197 tified as one of the most important volatile organic compounds released by plants during a biotic str

198 ntities combined with dereplication of known organic compounds represent prerequisites for biological

199 regeneration of activated carbon loaded with organic compounds results in heel build-up that reduces

200 e in which semi- and low-volatility oxidized organic compounds (saturation concentration c* < 100 mug

201 st time, cyclic triazanes, a class of cyclic organic compounds sequentially bearing three all-saturat

202 The concentrations of the semivolatile organic compounds (SOCs) in the soil were not correlated

203 Low volatile organic compounds started to dominate the spectrum when

204 y protecting otherwise bioavailable, reduced organic compounds such as lipids and waxes from decompos

205 in the ppbv range as well as to semivolatile organic compounds (SVOC) and even highly oxidized organi

206 n efficient conveyer of soluble semivolatile organic compounds (SVOCs) from indoors to outdoors throu

207 Sorption of semivolatile organic compounds (SVOCs) onto interior surfaces, often

208 ss background concentrations of semivolatile organic compounds (SVOCs) over the Central Northern Paci

209 created from a surface film of semivolatile organic compounds (SVOCs) sorbed from the surrounding ai

210 nd alternative plasticizers are semivolatile organic compounds (SVOCs), an important class of indoor

211 The project focused on semivolatile organic compounds (SVOCs), which are frequently found in

212 Here we show that siderophores, organic compounds synthesized by microbes to facilitate

213 Secondary metabolites are defined as organic compounds that are not directly involved in the

214 an identification of a number of FPW related organic compounds that are potentially harmful namely th

215 erates the production of water-soluble polar organic compounds that are relatively more amenable to a

216 standing of interactions between MnOx(s) and organic compounds that are relevant to natural and engin

217 tains a complex and dynamic mix of dissolved organic compounds that coexists with a range of organic

218 the distribution behavior of a wide range of organic compounds that may be present in geologic CO2 st

219 h nearly all atmospheric aerosols containing organic compounds that often contain both hydrophilic an

220 xhaled breath contains thousands of volatile organic compounds that reflect the metabolic process occ

221 They emit complex mixtures of gas-phase organic compounds that vary in volatility and molecular

222 operties and in the amount of aroma volatile organic compounds that were released in the vapour phase

223 is geared toward the utilization of similar organic compounds throughout the water column, with yet

224 to accomplish cooperative mineralization of organic compounds to CH4 and CO2 .

225 related to the time needed for oxidation of organic compounds to form HOMs.

226 ts and reacts rapidly with biogenic volatile organic compounds to form secondary organic aerosol (SOA

227 om transfer (HAT) reactions from a series of organic compounds to the quinolinimide-N-oxyl radical (Q

228 Partitioning of gas-phase organic compounds to the walls of Teflon environmental c

229 ensitively monitor biodegradation of various organic compounds under anoxic or oxic conditions.

230 Here, we report on the volatile organic compounds used by the subterranean root-knot nem

231 Detection of organic compounds used for well stimulation in samples f

232 rbons, which represent an important class of organic compounds used to produce novel graphene-based a

233 The synthesis of complex organic compounds usually relies on controlling the reac

234 volatile organic compounds (VOC) spectra from coffee samples of 7

235 More than 60 volatile organic compounds (VOCs belonging to different groups we

236 the capabilities of this system for volatile organic compounds (VOCs) analysis, we subjected the plan

237 ource clearly contributes to indoor volatile organic compounds (VOCs) and influences indoor chemistry

238 In this study, distributions of volatile organic compounds (VOCs) and the roles on O3 pollution h

239 ential to strongly influence floral volatile organic compounds (VOCs) and, in turn, plant-pollinator

240 Volatile organic compounds (VOCs) are easily measurable from rock

241 of cellular processes initiated by volatile organic compounds (VOCs) are limited when modelling real

242 Volatile organic compounds (VOCs) are released from the food matr

243 In addition, small amounts of volatile organic compounds (VOCs) are released.

244 of interest in this review are (a) volatile organic compounds (VOCs) associated with security applic

245 ess than 100 nm) and some hazardous volatile organic compounds (VOCs) during printing, although very

246 For this study, a volatile organic compounds (VOCs) emission test was developed to

247 Twenty-eight volatile organic compounds (VOCs) emitted from MF were identified

248 pplications including monitoring of volatile organic compounds (VOCs) emitted from natural and anthro

249 Approximately one-third of volatile organic compounds (VOCs) emitted to the atmosphere consi

250 y the fingerprints generated by the volatile organic compounds (VOCs) emitted.

251 asurements included a wide range of volatile organic compounds (VOCs) for a wide range of spark ignit

252 ion rates (E) for 69-89 nonbiogenic volatile organic compounds (VOCs) for each of four surface mining

253 em was used to generate vapor-phase volatile organic compounds (VOCs) from a pigpen slurry sample.

254 rusion assume that the transport of volatile organic compounds (VOCs) from a source toward a building

255 ssions of climate-relevant biogenic volatile organic compounds (VOCs) from boreal and subarctic fores

256 We isolated 11 volatile organic compounds (VOCs) from strain KM2501-1, of which

257 to study uptake of traffic-related volatile organic compounds (VOCs) from urban bicycling.

258 mistry (WRF-Chem) with emissions of volatile organic compounds (VOCs) from vegetation simulated with

259 hemical sensors for detecting small volatile-organic compounds (VOCs) have widespread applications in

260 and classification rate of exhaled volatile organic compounds (VOCs) in asthma diagnosis.

261 measurements of many low-abundance volatile organic compounds (VOCs) in breath and air samples are a

262 ng opens the way for the sensing of volatile organic compounds (VOCs) in gaseous media.

263 sition has allowed the detection of volatile organic compounds (VOCs) in olive oil samples, including

264 Vapor intrusion (VI) by volatile organic compounds (VOCs) in the built environment presen

265 Plants emission of Volatile Organic Compounds (VOCs) is involved in a wide class of

266 The volatile organic compounds (VOCs) obtained by solid-phase microex

267 Volatile organic compounds (VOCs) of honey samples were extracted

268 study was to determine whether the volatile organic compounds (VOCs) pattern in colorectal cancer (C

269 Volatile organic compounds (VOCs) play important roles in the env

270 lating effects are partly caused by volatile organic compounds (VOCs) produced by the bacterium.

271 , hydrogen (H2), methane (CH4), and volatile organic compounds (VOCs) such as ethylmercaptan (EM), ac

272 Monitoring of volatile organic compounds (VOCs) was achieved using a minute sam

273 cently, photochemical production of volatile organic compounds (VOCs) was reported at a nonanoic acid

274 Totally, 61 volatile organic compounds (VOCs) were identified in the headspac

275 In total, 71 volatile organic compounds (VOCs) were identified in the headspac

276 ements in several potentially toxic volatile organic compounds (VOCs) when compared to background val

277 Atmospheric oxidation of volatile organic compounds (VOCs) yields a large number of differ

278 es (NOx), carbon monoxide (CO), and volatile organic compounds (VOCs)) from East Asia and explicitly

279 med in the air photochemically from volatile organic compounds (VOCs), declined only 20-21%.

280 tion and to document the underlying volatile organic compounds (VOCs).

281 cts in the atmospheric oxidation of volatile organic compounds (VOCs).

282 in root exudates or are emitted as volatile organic compounds (VOCs).

283 ence switching properties for polar volatile organic compounds (VOCs).

284 gerprints (76 masses per sample) of volatile organic compounds (VOCs).

285 pecific N-nitrosamines (TSNAs), and volatile organic compounds (VOCs).

286 onventional [high concentrations of volatile organic compounds (VOCs)] and Green (low concentrations

287 ide (NO2), sulfur dioxide (SO2) and volatile organic compounds (VOCs, such as benzene, toluene, ethyl

288 Our small collection of these versatile organic compounds was enriched by newly synthesized deri

289 xGC-TOFMS), an unresolved complex mixture of organic compounds was identified in the aquifer.

290 eening of MOS sensors, specific for volatile organic compounds, was performed using fuzzy logic.

291 ty in vitro and a wide range of phenolic and organic compounds were identified.

292 reconceptional exposures to several volatile organic compounds were significantly associated with 11%

293 onds has attracted interest for constructing organic compounds which have application in pharmaceutic

294 chemical structure "space," e.g. the set of organic compounds which possesses some minimal set of de

295 Earth's atmosphere contains a multitude of organic compounds, which differ by orders of magnitude r

296 As such, remarkable sensing of water-soluble organic compounds with a sensitivity of free spectral ra

297 A viscosity database for organic compounds with atmospherically relevant function

298 c method to investigate the adsorption of 21 organic compounds with diverse functional groups to NIST

299 luding NH3, SO2, NO2, H2S, and some volatile organic compounds, with particular emphasis on the chall

300 Water-soluble organic compounds (WSOCs) were extracted from corn stalk