ライフサイエンスコーパス: organic

1 Five highly polar organic acids in serum were successfully quantified, and

2 Ga stress induces root secretion of organic acids such as citrate and malate.

3 ing amino acids, amino acid derivatives, and organic acids, was performed by high-resolution LC/MS te

4 ontents of 3/2-methyl-1-butanol, acetoin and organic acids.

5 articles and SRE, as well as with individual organic acids.

6 We investigated direct emissions of primary organic aerosol (POA) and photochemical production of SO

7 Secondary organic aerosol (SOA) formation during photo-oxidation o

8 re and concentration dependence of secondary organic aerosol (SOA) yields has been investigated for t

9 w that at least two-thirds of the decline in organic aerosol can be explained by changes in anthropog

10 Organic aerosol contributes a significant fraction of PM

11 global chemistry climate model EMAC with the organic aerosol module ORACLE to predict the phase state

12 rees C and observe negligible evaporation of organic aerosol via dilution.

13 Organic aerosols can exist in highly viscous or glassy p

14 We also show that a very rich mixture of organic aerosols is emitted from the sea surface.

15 nsumption of animal products, land use under organic agriculture remains below the reference scenario

16 by dissolved organic carbon (DOC), volatile organic analysis by gas chromatography/mass spectrometry

17 atography/mass spectrometry, and nonvolatile organic analysis by liquid chromatography/mass spectrome

18 The mixing of the organic and aqueous phases is confined under a quasi-2D

19 Perceptions of production methods for organic and conventional milk are changing, with consume

20 l remove differences previously reported for organic and conventionally produced milk.

21 The performance of bulk organic and hybrid organic-inorganic heterojunction phot

22 py (DRIFTS) is capable of detecting specific organic and inorganic bonds in metal complexes and miner

23 um MS profile, even in the presence of other organic and inorganic components, together with the mini

24 sphorus transfer reagent for a wide range of organic and inorganic substrates has been investigated.

25 ean annual temperature (MAT) was similar for organic and mineral soils (0.029 degrees C(-1) ).

26 g an ionization method that can ionize small organics and large biomolecules with different propertie

27 cations as key intermediates in atmospheric, organic, and enzymatic reactions.

28 rate) include two "drug" transporters of the organic anion transporter (OAT) family: OAT1 (SLC22A6, o

29 Here, we investigated the role of organic anion transporting polypeptide (OATP) transporte

30 sence of anhydro Zn(II) acetate and a strong organic base (DBU).

31 loped algorithm for J modulation in flexible organic biradicals, supports this hypothesis.

32 organic carbon (C) accumulation via mineral-organic C interactions but Oxisols often have low organi

33 ic C interactions but Oxisols often have low organic C.

34 ntly, porous solids fabricated from discrete organic cages have garnered much interest due to their e

35 High metal oxides are believed to facilitate organic carbon (C) accumulation via mineral-organic C in

36 as primarily affected by the content of soil organic carbon (C), soil C:N ratio, and clay content, wh

37 measure the aerobic degradation of dissolved organic carbon (DOC) adsorbed to granular activated carb

38 x, suggesting that the leaching of dissolved organic carbon (DOC) from litter layer to the topsoil is

39 raction organic carbon (HFOC), and dissolved organic carbon (DOC) were fractionated in sediment sampl

40 ion consisted of a mass balance by dissolved organic carbon (DOC), volatile organic analysis by gas c

41 luenced winter-summer patterns for dissolved organic carbon (DOC), with higher winter DOC in smaller

42 action organic carbon (LFOC), heavy fraction organic carbon (HFOC), and dissolved organic carbon (DOC

43 Light fraction organic carbon (LFOC), heavy fraction organic carbon (HF

44 Light-absorbing organic carbon (OC), also termed brown carbon (BrC), fro

45 ources, which contribute the largest part to organic carbon (OC, 67 +/- 3%) and its sub-constituents

46 Restoration of soil organic carbon (SOC) in agricultural soils can not only

47 Results extend the understanding of how organic carbon and nitrite loads modulate N2O accumulati

48 and significant reductions in water-soluble organic carbon and nitrogen (p < 0.01) in household air

49 ination of enhanced nitrification and higher organic carbon availability.

50 )C) record becomes insensitive to changes in organic carbon burial rate, due to counterbalancing chan

51 The high burial rate of organic carbon correlates with a significant drawdown of

52 Organic carbon in atmospheric particles comprises a larg

53 here clearly indicates that light-absorbing organic carbon in winter Beijing, the capital of China,

54 Soil organic carbon is projected to increase in Australia (9%

55 Similar to sea spray aerosol, organic carbon markers were most frequently observed in

56 This study summarizes the factors affecting organic carbon storage in regional and national scale, a

57 donor for autotrophs and causes fixation of organic carbon that could serve as a nutrient for OPs.

58 arbored large concentrations of bioavailable organic carbon that fueled anaerobic microbial respirati

59 fers, which is present as pyrite, degradable organic carbon, and geogenic U(IV) minerals.

60 nges in the weathering of isotopically light organic carbon.

61 ent of the biosphere and is a major sink for organic carbon.

62 st aquifer due to the oxidation of dissolved organic carbon.

63 actors derived from this literature model of organic cation sorption, along with phenyltrimethylammon

64 These findings suggest that amino acids and organic cations may interact with the transporter throug

65 n of Kd values for more structurally complex organic cations to homoionic montmorillonites and to het

66 and between plant tissues is facilitated by organic chelators, such as nicotianamine and citrate.

67 lic aromatic hydrocarbons (PAHs), a group of organic chemical contaminants.

68 um catalysis has become an important tool in organic chemistry, its combination with supramolecular h

69 iting applications in the area of host-guest organic chemistry, or to spectroscopically evaluate in-d

70 milarities to the Birch reduction known from organic chemistry.

71 esis as well as the parallels with synthetic organic chemistry.

72 Visible-light-driven oxygen production by an organic chromophore for up to 1 h of operation has been

73 wever, there are complications in the use of organic chromophores arising from the instability of the

74 The properties of organic chromophores necessary for successfully driving

75 Here we identify a complex, nutrient-rich organic coating on co-composted biochar that covers the

76 oscopic mechanisms of atomic desorption from organic coatings.

77 ACs contain metal ions but not organic cofactors, and use ATP to activate substrates th

78 ts that the complex mixture of inorganic and organic components found in whole OSPW are acutely toxic

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

94 The identified halogenated organic compounds, particularly iodinated organic molecu

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

96 for the preparation of enantiomerically pure organic compounds.

97 Current understanding of the specific organic constituents in these hydraulic fracturing waste

98 s novel photocatalyst for the degradation of organic contaminants, and to the authors' knowledge the

99 oral respiration, alongside high particulate organic content of the lagoon sediment, suggests acclima

100 dehydration of alcohols is involved in many organic conversions but has to overcome high free-energy

101 the polaron relaxation energy in solid-state organic D-A blends and show the importance of a reduced

102 cho a suite of core principles that underlie organic Darwinian evolution but also extend them in new

103 cides, pharmaceuticals) comprised 57% of 406 organics detected at least once.

104 the formation of organic monochloramines or organic dichloramines, depending on the chlorine to amin

105 xcluded after randomisation because they had organic disease (n=2 in the PENFS group; n=1 in the sham

106 with less than 1 week of data and those with organic disease identified after enrolment were excluded

107 charge transfer (CT) excitons dissociate at organic donor-acceptor interfaces has been a long-standi

108 This complex was collected in a CH2Cl2 organic drop and absorbance measured at 435nm.

109 ch allowed us to monitor fast blinking of an organic dye, the dissociation kinetics of very short DNA

110 vinyl bromides under synergistic nickel- and organic-dye-mediated photoredox catalysis is reported.

111 cations where both chromium (VI) cations and organic dyes are the main pollutants.

112 Organic electrochemical transistors (OECTs) are promisin

113 ystem and organs of a plant, we manufactured organic electronic devices and circuits in vivo, leverag

114 s a building block in the synthesis of novel organic electronic materials.

115 nce charge transfer efficiency in functional organic electronic materials.

116 odium- and chloride-rich cores surrounded by organic enriched surface layers containing minor inorgan

117 ado, have shown that fine grained, sulfidic, organic-enriched sediments accumulate U in its reduced f

118 lved form as a result of iron binding by the organic exudate.

119 Both organic farming and higher in-field plant diversity enha

120 tional (integrated pest management, IPM) and organic farming, as means to increase the accumulation o

121 e.g. organic light-emitting diodes (OLEDs), organic field-effect transistors (OFETs), solar cells or

122 surfaces were similar to those in studies of organic film buildup on indoor windows.

123 thetic" pH-sensitive protein conjugates with organic fluorophores, carbofluorescein, and Virginia Ora

124 lly friendly fabrication of mesoporous metal-organic framework (mMOF) thin films via the electrochemi

125 ry research into the critical steps in metal-organic framework (MOF) activation involving solvent exc

126 ctane dicarboxylic acid (BODCA)-MOF, a metal-organic framework (MOF) built with a high-symmetry bicyc

127 A recently developed metal-organic framework (MOF) catalyst for the dimerization of

128 C) are synthesized by using a Ni-based metal-organic framework as the precursor for high-temperature

129 , Li and co-workers fabricate a stable metal-organic framework functionalized with tertiary amine gro

130 tylene in a tetra-amide functionalized metal-organic framework, MFM-188, at crystallographic resoluti

131 lective adsorption at Cu(I) sites in a metal-organic framework.

132 Covalent organic frameworks (COFs) are crystalline, permanently p

133 Research on covalent organic frameworks (COFs) has recently gathered signific

134 is and optoelectronics, titanium based metal-organic frameworks (MOFs) are one of the most appealing

135 potential commercial applications for metal organic frameworks (MOFs) are tantalizing.

136 Many of the desirable properties of metal-organic frameworks (MOFs) can be tuned by chemical funct

137 Metal-organic frameworks (MOFs) have rapidly grown into a majo

138 Metal-organic frameworks (MOFs) or porous coordination polymer

139 Two porous, chiral metal-organic frameworks (MOFs), Ca14(l-lactate)20(acetate)8(C

140 phenolate-decorated-(metallo)porphyrin metal-organic frameworks (MOFs), ZrPP-n (n = 1, 2), featuring

141 he rational design and construction of metal-organic frameworks (MOFs).

142 entation of ferroelectricity in chiral metal-organic frameworks (MOFs): following a single-crystal to

143 ; and nanostructured materials such as metal-organic frameworks, porous-organic polymers, and mesopor

144 n donors into crystalline G-quadruplex-based organic frameworks, wherein the electron donors and acce

145 such as sarin and sulfur mustard using metal-organic frameworks.

146 ases where hydration or humidification of an organic glass-forming sample result in stiffer mechanica

147 ) to detoxify ROS such as hydrogen peroxide, organic hydroperoxide, and peroxynitrite.

148 No organic impurities are present in the patterned layers,

149 ide perovskite could be as compelling as its organic-inorganic counterpart regarding optoelectronic p

150 The performance of bulk organic and hybrid organic-inorganic heterojunction photovoltaics is often

151 , pi-conjugated semiconductor nanoparticles, organic-inorganic heterostructures, and porphyrin-based

152 power conversion efficiency demonstrated in organic-inorganic hybrid perovskite solar cells (PVSCs),

153 For hybrid organic-inorganic nanomaterials, here we show that by us

154 Organic-inorganic perovskite solar cells have attracted

155 ochemical processing and characterization of organic-inorganic trihalide lead perovskite thin films.

156 nificance such as reduction and oxidation of organics, inorganics, and CO2 transformation.

157 hat exhibits high capacities for radioactive organic iodides uptake.

158 which preserves integumentary structures as organic layers, including continuous fields of epidermal

159 fine structure (EXAFS) data using reference organic ligands demonstrated that Fe(II) was complexed p

160 ials consisting of inorganic nodes linked by organic ligands do however exist in the crystalline or a

161 e tuned by chemical functionalization of the organic ligands that connect their metal clusters into m

162 Using organic ligands with 1, 2, and 3 phenylene rings, we con

163 used in (opto)electronic applications, e.g. organic light-emitting diodes (OLEDs), organic field-eff

164 toe-to-toe with disruptive technologies like organic light-emitting diodes.

165 on the SEI thickens to 70 A and becomes more organic-like.

166 ution of individual atomic columns of Zn and organic linkers in the framework.

167 e production in digesters, permitting higher organic loading rates.

168 Hence, the purification of MPs from organic materials is crucial prior to conducting an iden

169 ions do not contain strontium or chlorinated organic materials.

170 rious reference materials with inorganic and organic matrices as well as widely varying amounts of ur

171 Natural dissolved organic matter (DOM) affects mercury (Hg) redox reaction

172 ces to induce cascading effects on dissolved organic matter (DOM) and microbial communities in the su

173 synthetic water samples containing dissolved organic matter (DOM) extracts and bromide were treated u

174 The quality of dissolved organic matter (DOM) in a wet weather overflow (WWF) can

175 ize origins and transformations of dissolved organic matter (DOM) in five major Arctic rivers (Kolyma

176 Wildfires can elevate dissolved organic matter (DOM) levels due to ash input and algal g

177 amine the molecular composition of dissolved organic matter (DOM) within these lakes using Fourier tr

178 ontent and speciation of sulfur in dissolved organic matter (DOM), which influences the reactivity of

179 oduction and discharge of reactive dissolved organic matter (DOM).

180 and is an important repository of dissolved organic matter (DOM).

181 el of humic-like and nonhumic-like dissolved organic matter (DOM).

182 king due to insufficient information on dead organic matter (DOM).

183 aling inhibitors hinder clogging but natural organic matter (NOM) has relatively little impact.

184 values (6.3-7.5) and three types of natural organic matter (NOM) isolates at various concentrations

185 climatic influences on the formation of soil organic matter (SOM).

186 reducing the decay of plant litter and soil organic matter (SOM).

187 Interactions between organic matter and mineral matrices are critical to the

188 plants may potentially influence the fate of organic matter associated with soil mineral and aggregat

189 We hypothesise that reductions in organic matter brought about by litter removal may lead

190 ming results in a four-phase pattern of soil organic matter decay and carbon dioxide fluxes to the at

191 of climate and stand characteristics on dead organic matter distribution.Reliable estimates of the to

192 ations suggest that biochemically equivalent organic matter has accumulated in oPOM at a greater rate

193 nhancing the processing and turnover of dead organic matter in soils of arid regions), reduce human e

194 e-of-flight mass spectrometer) and dissolved organic matter in the ocean point to a marine source for

195 but the influence of the influx of riverine organic matter on the trophodynamics of coastal marine f

196 efficiency were the soil properties; a high organic matter or clay content was observed to negativel

197 ate that the sequestered Hg is bound in soil organic matter pools accumulating over millennia.

198 quantified the ecological impact of riverine organic matter subsidies to glacier-marine habitats by d

199 cal to the preservation of soil and sediment organic matter.

200 ossible repositories for the preservation of organic matter.

201 ute to the daily flux of billions of tons of organic matter.

202 rived from heterotrophic remineralization of organic matter.

203 widely observed in transition metal oxides, organic metals, pnictides, and heavy fermion compounds a

204 eams nationwide was assessed using 14 target-organic methods (719 compounds).

205 ics simulations to study the dynamics of the organic methylammonium (MA) cation orientation in a rang

206 To optimize removal of organic micropollutants from the water cycle, understand

207 retail milk samples were analyzed, including organic milk (n=10), conventional milk (n=14) and pastur

208 Organic mixed conductors have garnered significant atten

209 The characterization of organic mixtures by comprehensive two-dimensional gas ch

210 The focus is on methods available for organic molecular crystals, but mention is made wherever

211 other words, the present study suggests that organic molecular heterogeneities can withstand diagenes

212 triplet that represents a building block for organic molecule-based magnets and also serves as a mode

213 In modern cancer therapy, the use of small organic molecules against receptor tyrosine kinases (RTK

214 Supramolecular materials, in which small organic molecules are assembled into regular structures

215 ng of the mechanism of its introduction into organic molecules is important.

216 f organic reactions, either between discrete organic molecules or on the pore surfaces of MOFs, in a

217 Organic molecules with heteroatoms often possess an impo

218 ed organic compounds, particularly iodinated organic molecules, are absent from inland natural system

219 Here we identified a range of small organic molecules, drugs, drug metabolites and drug-like

220 t pipi*/npi* electronic relaxation of hetero-organic molecules.

221 C-H bonds are ubiquitous structural units of organic molecules.

222 r the incorporation of alkynyl moieties into organic molecules.

223 f amino acids can result in the formation of organic monochloramines or organic dichloramines, depend

224 Organic monolayers are soft materials and display signif

225 For example, few single-crystal organic monomers react under topochemical control to pro

226 nthesized and was processed into fluorescent organic nanoparticles (FONs) for determination of import

227 In contrast to traditional organic nitrate therapies, an alternative strategy to re

228 In nonaqueous solvents such as organic nitriles, the prototype TAML activator gave the

229 remium prices for milk from either certified organic or conventional grass-fed cows.

230 fungi obtaining nutrients from recalcitrant organic or mineral sources in the soil, besides increasi

231 n and root phosphatase activity grew best on organic P, whereas the poor N2 fixer and the two non-N2

232 ene cores crosslinked with metal-free purely organic phosphors.

233 hodology is still limited to soils with high organic phosphorus content.

234 molecular design that yields ultranarrowband organic photodetectors.

235 Bulk-heterojunction organic photovoltaic materials containing nonfullerene a

236 efficiency (PCE), commercial applications of organic photovoltaics (OPVs) can be foreseen in near fut

237 ces has been a long-standing question in the organic photovoltaics community.

238 bons are exceptional electron acceptors, and organic photovoltaics fabricated with the ribbons show e

239 rbing BHJ is essential for highly efficient, organic, photovoltaics (OPV)/perovskite hybrid solar cel

240 mental stable isotope analysis of persistent organic pollutants (POPs) has the potential to character

241 Fish are a source of persistent organic pollutants (POPs) in the human diet.

242 rid was evaluated for both chromium (VI) and organic pollutants (using methyl blue (MB) as an example

243 In both environments, complex organic polymers are used as sources of nutrients.

244 als such as metal-organic frameworks, porous-organic polymers, and mesoporous carbons.

245 Uniform organic (primarily citrate ligands) layer on nAu was obs

246 tions between the primary, genetically based organic processes of evolution and the secondary system

247 The controllable reactivity gives the carbon organic radical great potential as a versatile reducing

248 erviews the basic principles of using stable organic radicals involved in reversible exchange process

249 The use of sunlight to drive organic reactions constitutes a green and sustainable st

250 ay drying technique to perform this class of organic reactions, either between discrete organic molec

251 vel two-electron storage anolyte for aqueous organic redox flow battery (AORFB) applications.

252 stratification during the deposition of the organic-rich (sapropel) interval known as S5.

253 tates) and some terpenoids were found in the organic samples.

254 e measured at significantly higher levels in organic samples.

255 and validated for the elemental analysis of organic samples.

256 The charge-carrier mobility of organic semiconducting polymers is known to be enhanced

257 e-transfer (CT) effect in weakly interacting organic semiconductor mixtures.

258 od is the introduction of nanopores into the organic semiconductor thin films via a simple and robust

259 diffusion, and density of dopants within the organic semiconductor, and, in turn, affect the electron

260 o satisfy the electrical requirements for an organic-semiconductor-based logic chip.

261 Effective implementation of organic semiconductors as a photoactive layer would open

262 selectivity by coating the anode with chiral organic semiconductors from helically aggregated dyes as

263 Here we use a range of organic semiconductors that undergo singlet exciton fiss

264 A 3D array of organic semiconductors was assembled using a DNA scaffol

265 ductivity in, and provide ohmic contacts to, organic semiconductors with very low electron affinity.

266 FFI patients are typically characterized by organic sleep related symptoms, rapidly progressive deme

267 elf-organization of the manifold mineral and organic soil components to distinct mineral assemblages,

268 nding wetland area with saturated and warmer organic soils is expected to increase landscape methane

269 veals a duality in the functional linkage of organic soils to aquatic ecosystems whereby they can hel

270 Fullerene-free organic solar cells show over 11% power conversion effic

271 s great potential for applications in tandem organic solar cells.

272 Sorption of the different organic solutes within the membrane skin layer determine

273 consecutive plugs of immiscible aqueous and organic solutions; the aqueous sample forms the central

274 n the COF membranes is incompatible with the organic solvents used for the COF IP process.

275 more, water, rather than traditional aprotic organic solvents, is used to dissolve the precursors.

276 gainst extreme external stressors, including organic solvents, proteases, and ethylene oxide gas ster

277 lly perform label-free monitoring of various organic solvents.

278 Its structure and its reactivity with organic substrates are demonstrated through a combinatio

279 xidative insertion of a range of unsaturated organic substrates, including azides, isocyantes, and ni

280 Surface tension lowering caused by organic surfactants, which diminishes the Kelvin effect,

281 n heterobimetallic catalysis for sustainable organic syntheses (SOS), highlighting key advances and r

282 he utilization of CO2 as a carbon source for organic synthesis meets the urgent demand for more susta

283 re underexploited as photoredox catalysts in organic synthesis relative to their homogeneous, molecul

284 The importance of microwave irradiation in organic synthesis today is unquestionable, but in many c

285 constructions characteristic of traditional organic synthesis, but can be accomplished under environ

286 is anticipated to find wider applications in organic synthesis, its immediate application to the cons

287 ough C-C bond formation has been a staple of organic synthesis, the direct transfer of primary amino

288 persists as a largely unsolved challenge in organic synthesis.

289 titutes a green and sustainable strategy for organic synthesis.

290 r use for the introduction of P=B units into organic systems.

291 the literature illustrate their potential as organic tracers for treatment operations or in the event

292 tor memory is developed, based on a vertical organic transistor configuration incorporating high-perf

293 A new device architecture for fast organic transistor memory is developed, based on a verti

294 sfer quenching experiments using a series of organic triplet donors (E((3)pipi*) from 1.83 to 0.78 eV

295 -xylylene diradical m-C8H8 is a prototypical organic triplet that represents a building block for org

296 ence of four stacked sandsheets separated by organic units has been recognised and compared to the 20

297 n open-exchange cages permits the release of organic wastes, some of which ultimately reaches the und

298 These organic water-soluble molecules act as, or as part of, c

299 source, is useful for the analysis of small organics with low polarities.

300 ich could help explain low concentrations of organics within some smectite-containing rocks or sedime