ライフサイエンスコーパス: emission

1 state-of-the-art GaN:Eu system for red light emission.

2 into planar ones, and generating a directive emission.

3 d in 1.6-fold increase in phenylacetaldehyde emission.

4 tion magnifies the effect of drawdown on CH4 emission.

5 -rich ejecta component may contribute to the emission.

6 acts, such as the magnitude of air pollution emissions.

7 xpected to increase landscape methane (CH4 ) emissions.

8 are an appreciable source of greenhouse gas emissions.

9 forcing associated with higher black carbon emissions.

10 emission categories comprising a majority of emissions.

11 vide an independent comparison with reported emissions.

12 e largest contributions from leaded gasoline emissions.

13 rived from both industrial and motor vehicle emissions.

14 t decreased NH3 emissions, but increased GHG emissions.

15 trees is the dominant source of regional CH4 emissions.

16 nderstanding of biochar's impacts on soil NO emissions.

17 gnificantly elevated exposures to combustion emissions.

18 rvices generates considerable greenhouse gas emissions.

19 y recognized role in regional greenhouse gas emissions.

20 ribute 60%-80% of global natural wetland CH4 emissions.

21 han PFIs due to higher elemental carbon (EC) emissions.

22 iurnal patterns in the rate of tree-stem CH4 emissions.

23 eme, that we name Optical Pump Rectification Emission, a THz field is generated directly on the surfa

24 Global cookstove emissions abatement results in an average surface temper

25 Most emissions across the system (approximately 80%) are effi

26 ituted triarylalkenes as aggregation-induced emission-active fluorogens (AIEgens) are sporadically ex

27 ects of international trade on air pollutant emissions, air quality and health have been investigated

28 coincide with early-20th century industrial emissions, aligning the UFG record with other North Amer

29 driven by decreasing regional atmospheric Hg emissions although they may be partly counterbalanced by

30 ll-optical scheme for ultra-bright gamma-ray emission and dense positron production with lasers at in

31 d energy-sampling and rapid-scan X-ray Kbeta emission and K-edge absorption spectroscopy as well as q

32 ntegration of long-lived Mn(2+) upconversion emission and relatively short-lived lanthanide upconvers

33 Environmental regulations on mercury (Hg) emissions and associated ecosystem restoration are close

34 e of dissipations such as atomic spontaneous emissions and cavity decays.

35 erformed to determine the uncertainty in the emissions and found that the uncertainty was larger for

36 le cerium oxide to reduce particulate matter emissions and increase fuel economy, was captured from t

37 at is attributed to increased local wildfire emissions and long-range (transcontinental) transport.

38 of implementing 12 treatment technologies on emissions and nutrient recovery were further explored th

39 hropogenic emissions, primarily from vehicle emissions and residential fuel burning.

40 r from near the seafloor accompanies methane emissions and stimulates CO2 consumption by photosynthes

41 aint on preindustrial vs. industrial-era LUC emissions and suggests that upper-end scenarios for the

42 how management decisions can impact soil GHG emissions and surface SOC stocks.

43 of magnitude as cities' overall territorial emissions and that local policy leverage to reduce upstr

44 technologies have been implemented to reduce emissions and to facilitate its use as fertilizer, but a

45 d the influence of regional ozone precursors emissions and, thus, greatly enhance O3 attribution to s

46 source attribution of resulting (posterior) emissions, and hence conclusions from such studies shoul

47 air pollutants, particularly from transport emissions, and high exposure to several air toxics befor

48 the magnitude and composition of wetland GHG emissions, and the efficacy of multiscale flux measureme

49 specific PM (-66%), BC (-65%), and PN (-19%) emissions are due to the newer fleet; an increased fract

50 Strong decreases in greenhouse gas emissions are required to meet the reduction trajectory

51 mulate the relationship between VO2 and H2O2 emission as a function of lipid concentration.

52 e current classification of "fresh" tailpipe emissions as nonhygroscopic remains true during nonregen

53 Changes in other gas and PM emissions, as well as impacts on acid and nutrient depos

54 A strong multiband emission associated with optical transitions from the co

55 neration of a spatial pattern of fluorescent emission at the intersection of two structured light bea

56 les to predict jointly productivity and N2 O emissions at field scale is discussed.

57 ss deaths per year from Southeast Asian coal emissions at present, increasing to 69660 (40080-126710)

58 mance of a set of technologies to reduce CO2 emissions at refineries.

59 er red shift of the squaraine absorption and emission bands.

60 We have presented a non-TOF emission-based approach for estimating the attenuation m

61 omposition of the volatile organic compounds emissions between PFI and GDIs, including benzene, tolue

62 uctive status and, thereby, affects isoprene emission, but they do not support the hypothesis that cy

63 tion-denitrification treatment decreased NH3 emissions, but increased GHG emissions.

64 ing soot oxidation and reducing the DPM mass emissions, but lead to a significant increase in the tot

65 US agriculture would reduce agricultural GHG emissions, but would also create a food supply incapable

66 rstanding of the regulation of nitrous oxide emission by denitrifying bacteria in response to differe

67 f the Pb in this feature was from industrial emissions by many nations in the 1980s and 1990s, with t

68 The fluorescence emission can be effectively quenched by gold nanoparticl

69 er visual perception or the raw fluorescence emissions can be masked by background signals or distort

70 al gradient in the Amazonian forest isoprene emission capacity is determined by plant species distrib

71 the potential to be abated, with only a few emission categories comprising a majority of emissions.

72 lth and climate-relevant soot (black carbon) emission characteristics to specific combustion conditio

73 een ambient surface temperatures and EGU air emissions (CO2, SO2, and NOX) using historical data.

74 an be attributed to East Asian anthropogenic emissions, compared with 0.7 ppbv using the sensitivity

75 lities of combined preclinical single photon emission computed tomography (SPECT) and X-ray computed

76 distribution were analyzed by single-photon emission computed tomography (SPECT)/computed tomography

77 btraction ictal and interictal single photon emission computed tomography can demonstrate complex ict

78 Fluorescence emission computed tomography detecting near-infrared aut

79 Using single-photon emission computed tomography/computed tomography lymphos

80 naturally, in particular by plants, and its emissions contribute to ozone destruction in the stratos

81 ant material with applications in catalysis, emissions control and solid-oxide fuel cells.

82 ermined here, we estimate that reducing idle emissions could substantially improve air quality near a

83 In this study, tunable fluorescence emission CQDs originated from chlorophyll were synthesiz

84 fects are sufficient to explain the observed emission current distribution.

85 on will need to focus on the >90% of methane emissions currently unmeasured or unreported.

86 generated an estimated $11.6 million in air emission damages from 2004 to 2013, with 35% of damages

87 PETB) were reconstructed using identical PET emission data but with MR-AC from these intrasubject rep

88 rtifacts are then reconstructed from the PET emission data using the IPAC algorithm.

89 as thermal management, photodetection, light emission, data communication, high-speed electronics and

90 By developing a carbonaceous emissions database for the United States, we show that a

91 Higher efficiency and lower emission demands use of alloys at higher operating tempe

92 monstrate low toxicity and enable stimulated emission depletion (STED) nanoscopy in neurons, human fi

93 By transforming stimulated emission depletion microscopy into a time-resolved ultra

94 assessment, including the quantification of emissions, dominant fate processes, types of analytical

95 Patterning and polarized light emission, e.g., for polarized organic light emitting dio

96 ient and causes an intense greenish-blue ECL emission, easily observable even by naked eye, with quan

97 ion-or brain power-can be viewed as the zero-emissions energy for sustainable development.

98 rgence in recent oil and gas related methane emission estimates between aircraft studies (basin total

99 The lifetime of this sub-band-gap emission exceeds that of the excitonic transition by ord

100 black hole or neutron star often show x-ray emission extending to high energies (>10 kilo--electron

101 Emission factors (EFs) for 39 individual SVOCs are deter

102 Emission factors (EFs) were calculated for carbon monoxi

103 e to intermittent sources and variability in emission factors can lead to wide confidence intervals i

104 The emission factors ranged from 6 x 10(8) to 6 x 10(11) per

105 PM2.5 emission factors were approximately 3 times higher with

106 dado de Huelva", were analyzed by excitation-emission fluorescence spectroscopy.

107 by other factors, including increasing local emissions, food web changes, eutrophication, and respons

108 Results showed that the brake-specific NOx emissions for the LNG trucks equipped with the TWC catal

109 ve significantly altered land-atmosphere CH4 emissions for this region, potentially acting as a posit

110 to measure and analyze unregulated compound emissions for two Euro 6 diesel and gasoline vehicles.

111 ly energetic and long-lived prompt gamma-ray emission from GRB 160625B.

112 itivity, we visualized and controlled phonon emission from individual atomic-scale defects in graphen

113 Chloroform emission from soil has been reported from diverse Arctic

114 d green) multiexcitonic emission, with green emission from the CdS arms emerging only at high excitat

115 The emission from the majority of the surface is dominated b

116 The 1D grating structure converts the blue emission from unpolarised to highly polarised; Highly po

117 effects, we measured gas- and particle-phase emissions from 82 light-duty gasoline vehicles recruited

118 Particulate matter emissions from agricultural livestock operations contain

119 design strategies to control greenhouse gas emissions from agricultural soils or wastewater treatmen

120 lished in peer-review journals on direct N2O emissions from agricultural systems in tropical and sub-

121 nds on the type of fuel, with relatively low emissions from coal and higher contributions from heavy

122 formation during photo-oxidation of primary emissions from cookstoves used in developing countries m

123 air quality is the temperature-dependence of emissions from electricity generating units (EGUs), asso

124 ver the 21(st) century, greenhouse gas (GHG) emissions from freight are projected to grow faster than

125 e OPT scenario, estimated well-to-wheels GHG emissions from full-size BEVs with 100-mile range are 62

126 st fleet, the measured 14.5% decrease in CO2 emissions from GDIs was much greater than the potential

127 Particle emissions from heavy-duty vehicles (HDVs) have significa

128 nt plants, (iv) long-term gaseous and liquid emissions from landfills, (v) waste being recycled, (vi)

129 Despite high simulated per-capita CO2 emissions from LUC in early phases of agricultural devel

130 guidelines to quantify the evolution of CH4 emissions from ruminant livestock during 1890-2014.

131 ashwater units, although intended to control emissions from the absorber, can contribute to additiona

132 ich accounted for 47%-54% of all non-CO2 GHG emissions from the agricultural sector.

133 f the atmospheric flux probably derives from emissions from the combustion of fossil fuels, but the m

134 tom-up' estimates, indicating that large CH4 emissions from trees adapted to permanent or seasonal in

135 Emissions from trees had an average stable carbon isotop

136 Methane (CH4 ) emissions from tropical wetlands contribute 60%-80% of g

137 We show that upstream emissions from urban household consumption are in the sa

138 e system, (ii) export of waste (iii) gaseous emissions from waste treatment plants, (iv) long-term ga

139 We find that approximately 83% of emissions, given the existing suite of technologies, hav

140 to highly polarised; Highly polarised yellow emission has been achieved from the F8BT polymer filled

141 o ruminant and waste sectors.India's methane emissions have been quantified using atmospheric measure

142 PM2.5 precursor emissions have declined over the course of several decad

143 ortality risk per thousand tons of precursor emissions (health damage functions) varied significantly

144 sments that account for spatial variation in emissions impacts.

145 latively short-lived lanthanide upconversion emission in a particulate platform allows the generation

146 on, several of these DNA-CAs exhibited white emission in aqueous solution.

147 ltivars can substantially mitigate paddy CH4 emission in China and other rice growing regions.

148 phyll a] experienced larger increases in CH4 emission in response to drawdown (R(2) = 0.84, p < 0.01)

149 microscopy making use of their fluorescence emission in the near IR.

150 We estimate that total CH4 emissions in 2014 was 97.1 million tonnes (MT) CH4 or 2.

151 The spatial distribution of emissions in gridded inventories (e.g., EDGAR) likely st

152 the share of biodiversity losses due to GHG emissions in the biodiversity footprint increases with i

153 efforts to combat increasing greenhouse gas emissions include their capture into advanced biofuels,

154 livestock sector in drylands had 36% higher emission intensity (CH4 emissions/km(2) ) compared to th

155 many cases be derived directly from relative emission intensity and lifetime.

156 mechanism for the temporal modulation of QD emission intensity at constant optical pumping rate.

157 re dependence of the DBMP-binding energy and emission intensity shows that the DBMP is composed of a

158 ront-Face fluorescence spectroscopy, and the emission intensity trend was investigated at various sul

159 cts of shale gas development on regional NOx emission inventories and dry deposition fluxes to Clean

160 ncluding temporal and spatial variability in emission inventories is important when reconciling inven

161 results provide a basis to evaluate regional emission inventories.

162 nd composition of time and location-specific emission inventories; therefore, including temporal and

163 tudies (basin total for a midday window) and emissions inventories (annualized regional and national

164 ably, the observed decay of the over cut-off emission is found to be critically associated with, and

165 ed climate change intervention, reducing CH4 emissions is an entirely distinct concept from biologica

166 d outputs of wastes, products, residues, and emissions is established and quantified.

167 hat local policy leverage to reduce upstream emissions is larger than typically assumed.

168 ributor to agricultural greenhouse gas (GHG) emissions, it has been suggested that reducing animal ag

169 lands had 36% higher emission intensity (CH4 emissions/km(2) ) compared to that in nondrylands in 201

170 The trend in the S1 --> S0 emission lifetime is consistent with their relative opti

171 Here we report observations of an emission line of singly ionized carbon ([C ii] at a wave

172 Motion-induced change in emission (MICE) can be utilized as an effective sensing

173 is may decrease NH3 (9-11%) and GHG (11-18%) emissions; nitrification-denitrification treatment decre

174 In primary emissions, OA mass spectral fragments associated with ox

175 cies is a low-spin Fe(iii) d(5) complex, and emission occurs from a long-lived doublet ligand-to-meta

176 , prevalent in the Arctic, may see increased emission of geologic CH4 in the future, in addition to e

177 ides favorable conditions for production and emission of greenhouse gases (GHGs).

178 Oxygen is an efficient quencher of emission of many phosphorescent compounds, thus oxygen c

179 quantitatively predict the accumulation and emission of nitrosamines and nitramines.

180 the safety of our consumer products and the emission of potential contaminants into the environment.

181 Multiexcitonic transitions and emission of several photons per excitation comprise a ve

182 The observed changes in near-infrared emission of SWCNTs are important for understanding the i

183 ting in the observation of the typical green emission of Tb.

184 perature and ratio of reactants, the maximum emission of the resulting CDots gradually shifts from bl

185 The half-life and confounding gamma emissions of (52g)Mn are prohibitive to clinical transla

186 To increase energy security and reduce emissions of air pollutants and CO2 from coal use, China

187 The reduction of emissions of mercury is a declared aim of the Minamata C

188 es contributes almost 1/5 of the total field emissions of methane and ethane measured in the Bakken s

189 Emissions of NO from soils occur primarily during denitr

190 The OS emissions of nontraditional toxic species such as HNCO h

191 We investigated direct emissions of primary organic aerosol (POA) and photochem

192 Anthropogenic emissions of the toxic heavy metal mercury (Hg) have sub

193 tional deposits is likely to lead to greater emissions of V to the atmosphere in the near future.

194 Here, we investigate how heat waves affect emissions of volatile organic compounds from urban/subur

195 The effects of vehicle-related emissions on health has been a long-standing question in

196 nitoring the influence of Marcellus well NOx emissions on regional nitrogen deposition.

197 ute to their abundance either through direct emissions or surface reactions.

198 NPs was red-shifted to 596 and 616nm and the emission peak (Tyr) at 410nm was gradually increased wit

199 hat were 2-3nm in size with the fluorescence emission peak of GQDs located at 405nm.

200 quantum wells display extreme absorption and emission polarization anisotropy.

201 king related to investment decisions and CO2 emissions policy in the refining sector.

202 A model was developed to estimate total GHG emission potential from Adelie penguin colonies during b

203 es as well as 1/f behaviour in corresponding emission power spectral densities.

204 ctral distribution and reducing multi-photon emission presented open challenges.

205 can be explained by changes in anthropogenic emissions, primarily from vehicle emissions and resident

206 f novel magnetic resonance shift and optical emission probes that are sensitive to the local solution

207 We show that such two-photon emission processes can occur on nanosecond time scales a

208 The results expand the range of emission properties that can be achieved in water with a

209 d excitation wavelength dependent multicolor emission properties.

210 term records at Barrow, AK, suggest that CO2 emission rates from North Slope tundra have increased du

211 These emission rates match those from tropical forest soils, t

212 The corresponding emission rates of MS2 and Phi6 were 547 PFU min(-1) and

213 , and N input rates are a key determinant of emission rates.

214 ing independent monitoring of greenhouse gas emission reduction projects.

215 f phenomena across many energy technologies, emissions reduction, environmental protection, mining ac

216 nd flexible CCS achieves more cost-effective emission reductions than normal CCS under both reduction

217 ently fast that, as a result of ongoing NO x emission reductions, autoxidation is now competing with

218 The temporal patterns of the condensate emission result from the intrinsic disorder and are driv

219 Field emission scanning electron microscopy revealed that etha

220 ould be explained via a hypothetical dynamic emission scenario consistent with combined sewer overflo

221 Under the most extreme emissions scenario, projected declines were highly varia

222 the Representative Concentration Pathway 8.5 emissions scenarios, this study shows that in future cli

223 ut the split limit between traffic and other emission sector contributions such as solvent use remain

224 the intensity and the duration of the light emission signal by factors correlated to their length.

225 adeoffs by regulating air, water, and solids emissions simultaneously and performing regulatory asses

226 We identify strong, likely geologic emissions solely where the permafrost is discontinuous.

227 t or seasonal inundation can account for the emission source that is required to close the Amazon CH4

228 ances (<<1 km) owing to unevenly distributed emission sources, dilution, and physicochemical transfor

229 is divided into continuous and intermittent emission sources.

230 es both the overlap of paper and fluorophore emission spectra and the fluorescence intensity on an im

231 The absorption and emission spectra were found to be widely tunable on the

232 e temperature and excitation power dependent emission spectra, thermal quenching ratios, fluorescence

233 Fe(3+) ions showed quenching behavior in the emission spectra.

234 formed by inductively coupled plasma optical emission spectrometry and the digestion efficiency was e

235 means of inductively coupled plasma optical emission spectroscopy (ICP-OES).

236 using an inductively coupled plasma-optical emission spectroscopy.

237 when setting fuel economy and greenhouse-gas emission standards for passenger cars and light trucks.

238 The average estimated CH4 and N2O emissions tended to be increasing during the period from

239 tor of 2 higher particulate matter (PM) mass emissions than PFIs due to higher elemental carbon (EC)

240 North America and Europe to reduce chemical emissions that contribute to acid rain.

241 availability alters the response of isoprene emission to changes in atmospheric composition.

242 ally have changed 332 of 1732 (19%) positron emission tomographies at low-risk physiological severity

243 pixel range of perfusion in paired positron emission tomographies.

244 Whole-body (18)F-fluodeoxyglucose positron emission tomography ([(18)F]FDG-PET) imaging has an esse

245 Combined positron emission tomography (PET) and computed tomography (CT) c

246 18 ((18)F) fluorodeoxyglucose (FDG) positron emission tomography (PET) and hyperpolarized carbon 13 (

247 ion neuroimaging data consisting of positron emission tomography (PET) and magnetic resonance imaging

248 luorine 18 fluorodeoxyglucose (FDG) positron emission tomography (PET) and survival in patients with

249 y recreationally active males using positron emission tomography (PET) and the MOR-selective radiolig

250 nuation correction (ATAC) for brain positron emission tomography (PET) in an integrated time-of-fligh

251 Positron emission tomography (PET) is a powerful analytical tool

252 the radiosynthesis of heterocyclic positron emission tomography (PET) radioligands using the copper-

253 Radiolabeling with long-lived positron emission tomography (PET) radionuclides, such as mangane

254 to track PD-L1 expression by immuno-positron emission tomography (PET).

255 labeled Pittsburgh Compound B (PiB) positron emission tomography after long-term prospective follow-u

256 y individuals using [(11)C]-acetate positron emission tomography and cardiovascular magnetic resonanc

257 went magnetic resonance imaging and positron emission tomography for amyloid-beta ((11) C-PiB or (18)

258 Positron emission tomography imaging reveals neuroinflammation as

259 ability; and (iii) this 18F-AV-1451 positron emission tomography retention pattern significantly expl

260 We found that: (i) 18F-AV-1451 positron emission tomography retention was differentially associa

261 ge, and cross-sectional florbetapir positron emission tomography retention, but not with years of edu

262 ed annualized change in florbetapir positron emission tomography retention.

263 11C-(R)-PK11195 positron emission tomography reveals increased inflammation in a

264 Patient 2's emission tomography scan demonstrated a reduction in glu

265 reporting the results of an amyloid positron emission tomography scan is to assign a dichotomous rati

266 levo-dihydroxyphenylalanine dynamic positron emission tomography scans and striatal regions of intere

267 etention, antecedent to 18F-AV-1451 positron emission tomography scans, in the parieto-temporal and p

268 n 18 kDa translocator protein brain positron emission tomography signal, which arises largely from mi

269 r (MDD), highlighting insights from positron emission tomography studies.

270 C]carfentanil and [(18)F]fluorodopa positron emission tomography using a high-resolution scanner.

271 [(18)F]CPFPX positron emission tomography was used to quantify A1AR availabili

272 primates and in human studies using positron emission tomography were not consistent.

273 Positron emission tomography with 18F-florbetapir and fludeoxyglu

274 nal SGLT2 proteins in rodents using positron emission tomography with 4-[(18)F]fluoro-dapagliflozin (

275 beta on Pittsburgh Compound B (PiB) positron emission tomography, gait speed over 4.57 m (15 ft), and

276 and coronary flow reserve (CFR) by positron emission tomography, where submaximal stress precludes a

277 ion of potential tracers for use in positron emission tomography.

278 These opposing emissions trends emphasize the importance of fully funct

279 tation, irrespective of climate modeling and emissions uncertainty, can be as low as 28% with one met

280 positive radiative forcing of increasing CH4 emissions until the end of the 21st century as indicated

281 tions and can substantially explain isoprene emission variability in tropical forests, and use a mode

282 Harmonization reduced climate emissions versus nonharmonized averages.

283 (2) 0.85) between the p-PAH and black carbon emissions was identified with a mass ratio of approximat

284 (PRELIM), that estimates energy use and CO2 emissions was modified to evaluate the environmental and

285 through significant solvatochromic shifts in emission wavelength across the visible spectrum by varyi

286 sized two new luminophores with direct light emission wavelength in the NIR region.

287 Additionally, their emission wavelength was tunable across the entire visibl

288 For some compounds, emission wavelengths are directly correlated to the subs

289 Proper tuning of kinetics and emission wavelengths enables the generation of a spatial

290 try-level reporting or aggregate measures of emissions, we present the identification of gaseous plum

291 Particle number (PN) emissions were 28% and 17% higher with the PPS-M compare

292 Engine related emissions were characterized from twenty-two natural gas

293 ctly into the atmosphere, and 74% of the air emissions were elemental Hg.

294 Energy and GHG emissions were not significantly sensitive to the number

295 Vehicle tailpipe and crankcase emissions were the highest sources of methane.

296 -TCBD-aniline gave rise to an intense, broad emission, which red shifts upon increasing the solvent p

297 O2 -eq m(-2) mostly because of decreased CH4 emissions, while N deposition reduced GWP from 21.0 to -

298 tates that give efficient bluish white-light emissions with photoluminescence quantum efficiencies of

299 of two-colour (red and green) multiexcitonic emission, with green emission from the CdS arms emerging

300 Grazing incidence and grazing emission X-ray fluorescence spectroscopy (GI/GE-XRF) are