ライフサイエンスコーパス: organic compound

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

2 mple of a cyclopropenimine-based fluorescent organic compound.

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

4 ocks in the synthesis of chemically relevant organic compounds.

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

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

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

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

9 perspective to the catalytic applications of organic compounds.

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

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

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

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

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

15 he bioaccumulation potential and toxicity of organic compounds.

16 chnology for chemical monitoring of nonpolar organic compounds.

17 functional interfaces between inorganic and organic compounds.

18 the condensation of atmospheric low-volatile organic compounds.

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

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

21 for the preparation of enantiomerically pure organic compounds.

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

23 Mg released from minerals gets trapped into organic compounds.

24 ormation may have triggered the formation of organic compounds.

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

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

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

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

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

30 Halogenated organic compounds, also termed organohalogens, were init

31 Volatile organic compound analysis revealed substantial concentra

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

48 Halogenated organic compounds are also common intermediates in synth

49 Trace organic compounds are important in environmental analysi

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

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

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

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

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

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

56 vapor pressure and aqueous solubility of the organic compound at 25 degrees C and CO2 density to pred

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

58 theoretical calculations indicate that this organic compound becomes metallic at 180 GPa, fueling th

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

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

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

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

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

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

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

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

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

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

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

70 We show for the first time that a specific organic compound class in aerosols, oligomers, is strong

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

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

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

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

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

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

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

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

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

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

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

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

83 Results demonstrated the enhancement of organic compound dissolution and production of soluble c

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

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

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

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

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

89 of indoor and outdoor particle and volatile organic compound emissions with potential deleterious ef

90 oprene dominates global non-methane volatile organic compound emissions, and impacts tropospheric che

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

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

93 rene is the predominant non-methane volatile organic compound emitted to the atmosphere and shapes tr

94 Volatile organic compounds emitted from Xoo rice were significant

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

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

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

98 th carbon dioxide, ventilation, and volatile organic compound exposures in office workers: a controll

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

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

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

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

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

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

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

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

107 The sesquiterpene (-)Englerin A (EA) is an organic compound from the plant Phyllanthus engleri whic

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

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

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

111 Over 280 organic compounds from ten major homologous series were

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

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

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

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

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

117 Volatile organic compounds have been recognized as important mark

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

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

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

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

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

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

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

125 Nonvolatile organic compounds identified were polyethylene glycols (

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

127 2SO4 > NaCl > NH4Cl > NH4NO3 for the studied organic compounds, implying the following relative stren

128 uinones in nature, using such a bio-inspired organic compound in batteries enables access to greener

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

166 ghtforward nucleophilic fluoromethylation of organic compounds is reported.

167 to characterize the intermediate volatility organic compound (IVOC) emissions from a fleet of on-roa

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

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

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

171 Volatile organic compounds may be volatilized from stems or leave

172 Organic compounds occur in some chondritic meteorites, a

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

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

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

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

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

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

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

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

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

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

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

184 ter-sphere charge transfer (Fe(CN)6(4-)) and organic compound oxidation through both direct oxidation

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

186 The identified halogenated organic compounds, particularly iodinated organic molecu

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

188 d Saprochaete were investigated for volatile organic compound production using HS-SPME-GC/MS analysis

189 ated to detect methyl salicylate, a volatile organic compound released by pathogen-infected plants vi

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

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

192 iciencies of the COF NF membrane for a model organic compound, Rhodamine-WT, and a background electro

193 to rationalize the relationship between the organic compound's molecular structure (n-alkane, branch

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

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

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

197 Low volatile organic compounds started to dominate the spectrum when

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

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

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

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

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

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

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

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

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

207 r obtaining all possible stereoisomers of an organic compound that has multiple contiguous stereocent

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

224 nts of NOx, CO2, CO and non methane volatile organic compound tracers in a city that might be conside

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

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

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

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

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

230 sensor channels to perform advanced volatile organic compound (VOC) detection and mixture analysis.

231 he relationship between texture and volatile organic compound (VOC) emission.

232 lly contribute to total methane and volatile organic compound (VOC) emissions from the production sec

233 surface, thereby matching observed volatile organic compound (VOC) emissions to the atmosphere.

234 temperatures cause higher biogenic volatile organic compound (VOC) emissions, which in turn lead to

235 The whole volatile organic compound (VOC) profile can be used to discrimina

236 a polluted marine environment under volatile organic compound (VOC)-limited conditions associated wit

237 ed streptomycetes using an airborne volatile organic compound (VOC).

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

281 tion and to document the underlying 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 eening of MOS sensors, specific for volatile organic compounds, was performed using fuzzy logic.

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

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

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

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

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

294 Chloroform is an example of a halogenated organic compound with natural formation as its primary s

295 moiety could be incorporated in a colorless organic compound with the aim of generating highly react

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