ライフサイエンスコーパス: CO2

1 CO2 concentration, and SO4 and nitrogen deposition on tw

2 CO2 is a physiological gas normally produced in the body

3 pped, modified atmosphere packaged (70%O2/30%CO2) and maintained under retail conditions (4+/-0.5 deg

4 analytics exemplified for the analysis of a CO2 stream in a production plant for detection of benzen

5 mine several potential mechanisms of abiotic CO2 uptake in arid and semiarid soils: atmospheric press

6 ed [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment (FACE) and chamber experiments.

7 experimental data from the Soybean Free-Air CO2 Enrichment site showing that the CFE declined with i

8 Although CO2 introduction is possible prior to hydroxide eluent g

9 owth from a population maintained in ambient CO2 and then transferred to elevated CO2 for 20 generati

10 noted with respect to lactate, alanine, and CO2 production.

11 ntury as indicated by an atmospheric CH4 and CO2 concentration model.

12 plasma synthesis of acetic acid from CH4 and CO2 is an ideal reaction with 100 % atom economy, but it

13 bounds for O2/N2, H2/N2, CO2/N2, H2/CH4 and CO2/CH4, with the potential for biogas purification and

14 oceanic factors (e.g., land cover change and CO2-induced warming) to the 2016 drought.

15 Coupled C-S cleavage and CO2 release to yield [(bpy)3Pd3(micro3-S)2](NO3)2 (bpy,

16 ons reduced model sensitivity to climate and CO2 , but only over the course of multiple centuries.

17 methanol, as well as the reactions of CO and CO2 over TMC surfaces.

18 n making related to investment decisions and CO2 emissions policy in the refining sector.

19 carboxylic acids from 1,6- and 1,7-enyes and CO2.

20 al species capable of using both HCO3(-) and CO2 had greater CO2 use as concentrations increased.

21 n and oxidation of organics, inorganics, and CO2 transformation.

22 which may have induced a surge in magma and CO2 fluxes from mid-ocean ridges and oceanic hotspot vol

23 ved from the arylamine starting material and CO2 in the presence of DBU, is dehydrated by activated s

24 D s decreases with increasing methane and CO2 injecting pressure for samples with high D s .

25 ane (DRM), i.e., the reaction of methane and CO2 to form a synthesis gas, converts two major greenhou

26 microbial communities for CCS monitoring and CO2 utilization, and, with examples, demonstrate how syn

27 Here, multiple sensors tracked O2 and CO2, gas pressure (DeltaP) between internal silage and a

28 y and reduce emissions of air pollutants and CO2 from coal use, China is attempting to duplicate the

29 ts for water oxidation, proton reduction and CO2 reduction, and molecular-catalyst-based AP devices,

30 atin D-2 by synchronous extrusion of SO2 and CO2.

31 els by processes such as water splitting and CO2 photoreduction (artificial photosynthesis).

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

33 methanol) directly from sunlight, water and CO2.

34 Recent field studies have reported anomalous CO2 uptake using eddy-covariance techniques in arid and

35 sts absorb a large fraction of anthropogenic CO2 emission, but their ability to continue to act as a

36 sion cross sections (Omega) with He, N2, Ar, CO2, and N2O were measured for the 20 common amino acids

37 and, Greece, are part of the largest arsenic-CO2-rich shallow submarine hydrothermal ecosystem on Ear

38 tilation inhomogeneity improved but arterial CO2 increased despite unchanged respiratory rate and tid

39 was reduced (P < 0.001) at constant arterial CO2 tension and pH (P = 0.27 and P = 0.23, respectively)

40 ely limited, with no differences in arterial CO2 tension or in tidal or minute ventilation between th

41 Prospectively targeted arterial CO2 has the capability to evolve as an alternative to cu

42 Based on the results, during CWI as CO2 partitions into the oil the dissolved gas of the oil

43 azides, isocyantes, and nitriles, as well as CO2 and elemental sulfur (S8 ).

44 d undergo N-dependent changes as atmospheric CO2 concentrations rise, having global-scale implication

45 Elevated atmospheric CO2 may widen the disparity in protein intake within cou

46 is of renewable bioproducts from atmospheric CO2 Growth and metabolism of cyanobacteria are inherentl

47 e orbitally driven variations in atmospheric CO2 concentration between [Formula: see text]150 and 700

48 d ecosystems to slow the rise in atmospheric CO2 concentrations may be smaller than previously assume

49 esponses of plants to changes in atmospheric CO2 concentrations, and fire, as well as what are likely

50 e responses to future changes in atmospheric CO2 concentrations, and thus feedbacks to climate change

51 Large amplitude variations in atmospheric CO2 were associated with glacial terminations of the Lat

52 y by the low partial pressure of atmospheric CO2 (Ca ) experienced during the last glacial period is

53 and higher partial pressures of atmospheric CO2 (pCO2 = 400 and 1000 ppmv).

54 tions between the growth rate of atmospheric CO2 concentrations and the El Nino-Southern Oscillation

55 Rising atmospheric CO2 and carbon metabolism 33 III.

56 sponses to changing climate and atmospheric [CO2] in the boreal forest.

57 toward commercialization of adsorption-based CO2 capture technologies, in addition to other attribute

58 o calculate CO2 on an absorbed light basis ( CO2.a ) and enabled comparison with nine TBMs.

59 tion for industrial packed and fluidized bed CO2 capture systems due to large particles with a diamet

60 pecies-specific developmental effects before CO2 and climate effects are inferred.Intrinsic water-use

61 wever, the electrochemical reactions between CO2 (0.04 % in ambient air) with Li anode may lead to th

62 pseudorevertant strains were not induced by CO2 , consistent with reports that CO2 directly stimulat

63 RelB is processed by CO2 in a manner dependent on a key C-terminal domain loc

64 However, greater values of CH4 -C:CO2 -C ratios lead to a greater global warming potential

65 lpha) from measured reflectance to calculate CO2 on an absorbed light basis ( CO2.a ) and enabled com

66 Despite high simulated per-capita CO2 emissions from LUC in early phases of agricultural d

67 ion defective mutant, is sufficient to cause CO2 sensitivity, which can occur even in the absence of

68 o 11.8 ppm revealed that certain chemisorbed CO2 species are engaged in very strong HBs.

69 can be explained by declining chloroplastic CO2 concentration (cc ) at low PPFD.

70 ow with H2:CO2 or syngas (a mixture of H2/CO/CO2) makes these microorganisms ideal chassis for sustai

71 ese climate anomalies by assimilating column CO2, solar-induced chlorophyll fluorescence, and carbon

72 d catalysts are found to exhibit competitive CO2 capacities (0.67-0.91 mmol g(-1) at 25 degrees C and

73 mines the cost of separating and compressing CO2 across 18 industrial processes.

74 proposal is to use the cycle to concentrate CO2 inside individual chloroplasts.

75 4 cycle-a biochemical pump that concentrates CO2 near RubisCO increasing assimilation efficacy.

76 n atmospheric carbon dioxide concentration ([CO2 ]) is critical for understanding and predicting the

77 by integrating components of a cyanobacteria CO2-concentrating mechanism will necessitate co-introduc

78 K (-11 mK to -335 mK) by 2100 due to delayed CO2 response.

79 the environmental stress of carbon dioxide (CO2) anesthesia converts an asymptomatic rhabdovirus inf

80 cant drawdown of atmospheric carbon dioxide (CO2) at that time.

81 Trapping with carbon dioxide (CO2) gave the respective O-[Zr] bonded cyclic boratacarb

82 ater caused by anthropogenic carbon dioxide (CO2) is anticipated to influence the growth of dinitroge

83 d with a fractional ablative carbon dioxide (CO2) laser.

84 to release large amounts of carbon dioxide (CO2) to the atmosphere in response to increasing tempera

85 Carbon dioxide (CO2) which constitutes a major part of the biogas is gen

86 quilibrium between bicarbonate and dissolved CO2.

87 tially as an endolith when lacking dissolved CO2.

88 ing the effective concentration of dissolved CO2 near the electrode surface through rapid equilibrium

89 Oils with limited capacity for dissolving CO2, such as heavy hydrocarbon components, are responsib

90 hat have an infinite capacity for dissolving CO2, such as light pure hydrocarbon components.

91 owth by Ca. P. anaerolimi whereby DPO drives CO2 reduction to formate, which is then assimilated into

92 on exposure to high temperature, oxygen, dry CO2, sulfur-containing compounds, nitrogen oxides, oxyge

93 Its dynamic CO2 uptake also matched well with its static condition.

94 rice yield in response to elevated [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment (FACE) an

95 ood predictor of instantaneous net ecosystem CO2 exchange and 3) functional diversity of leaf N conce

96 t for developing practical or cost-effective CO2 technologies.

97 the complex can selectively electrocatalyze CO2 reduction to CO in tetrahydrofuran at -0.48 V vs NHE

98 in the rate-limiting step of electrochemical CO2 reduction catalysis mediated by planar polycrystalli

99 Elevated CO2 can only weakly reduce these yield losses, in contra

100 ical results suggest that combined, elevated CO2 and temperature will lead to long-term declines in t

101 onal soil C models and suggest that elevated CO2 might increase turnover rates of new soil C.

102 that the response of assemblages to elevated CO2 are correlated with inorganic carbon physiology.

103 ambient CO2 and then transferred to elevated CO2 for 20 generations (HC).

104 um tricornutum, after growing under elevated CO2 (1000 muatm, HCL, pHT : 7.70) for 1860 generations,

105 Will elevated CO2 offset warming-induced changes in carbon metabolism?

106 than HS93-4118 at both ambient and elevated [CO2 ].

107 aily C assimilation was greater at elevated [CO2 ] in both cultivars, while stomatal conductance was

108 r sites was due almost entirely to elevated [CO2 ].

109 edicting rice yield in response to elevated [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment

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

111 7942 to improve glucose utilization, enhance CO2 fixation and increase chemical production.

112 warming and energy crises by removing excess CO2 from the atmosphere and converting it to value-added

113 The excess CO2 flux is resulted primarily from reduction in vegetat

114 ent in designing high-capacity but expensive CO2 sorbent for developing practical or cost-effective C

115 n be reduced while maintaining total expired CO2 (VCO2tot = VCO2ML + VCO2NL) and arterial PCO2 consta

116 Extracorporeal CO2 removal may provide the physiologic prerequisites fo

117 real membrane oxygenation and extracorporeal CO2 removal.

118 Indeed, both extracorporeal CO2 removal and extracorporeal oxygen delivery affect th

119 hypoxemia development during extracorporeal CO2 removal.

120 a is frequent during low-flow extracorporeal CO2 removal combined with ultraprotective mechanical ven

121 rates comparable to low-flow extracorporeal CO2 removal devices (blood flow < 500 mL/min) in a large

122 arable with existing low-flow extracorporeal CO2 removal in a large animal model, but the final dialy

123 Minimally invasive extracorporeal CO2 removal is an accepted supportive treatment in chron

124 Minimally invasive extracorporeal CO2 removal removes a relevant amount of CO2 thus allowi

125 flow systems providing mainly extracorporeal CO2 removal, are increasingly applied in clinical practi

126 ndeed, for the same amount of extracorporeal CO2 extraction, it is possible to reduce the FIO2, reduc

127 radigm to the emerging use of extracorporeal CO2 removal (ECCO2R) for ultraprotective ventilation in

128 While the effect of extracorporeal CO2 removal on the respiratory quotient of the native lu

129 at 25 degrees C and 0.15 bar), extraordinary CO2 /N2 selectivities (98-205 at 25 degrees C), and exce

130 Compared to significant climatic factors, CO2 had on average an approximately three-, four-, or fi

131 fficiently, many algae operate a facultative CO2 concentrating mechanism (CCM).

132 rmined the quantum yield of CO(2) fixation ( CO2 ) and the convexity factor (theta).

133 are W i across varying tree sizes at a fixed CO2 level and show that ignoring developmental changes i

134 ominent examples include the carboxysome for CO2 fixation and catabolic microcompartments found in ma

135 n, and may have significant implications for CO2 losses from tropical forest soils under future rainf

136 plexes have been thoroughly investigated for CO2 electrochemical and visible-light-driven reduction.

137 )') and heterogeneous rate constant (k0) for CO2 reduction were determined with different quaternary

138 elopment of ultrathin GO-based membranes for CO2 capture.

139 dant enzyme in plants and is responsible for CO2 fixation during photosynthesis.

140 New materials with high selectivities for CO2 adsorption, large CO2 removal capacities, and low re

141 ce is key in controlling the selectivity for CO2 reduction over H2 evolution in aqueous solution.

142 has a low turnover and poor specificity for CO2.

143 Fractional CO2 laser treatment has been reported to improve burn sc

144 d, of whom 26 received at least 1 fractional CO2 laser treatment and 22 received 3 treatments.

145 tment sessions with an ablative fractionated CO2 laser.

146 y evolution to enable biomass synthesis from CO2 in Escherichia coli.

147 e global food productivity, benefiting from [CO2] rich environments.

148 stability issues facing amine-functionalized CO2 adsorbents, including amine-grafted and amine-impreg

149 long-term stability of amine-functionalized CO2 adsorbents.

150 A long-term net CO2 uptake of >200 g CO2 m(-2) yr(-1) is required to offset the positive radi

151 y, activity and stability of next-generation CO2 reduction catalysts, thus opening new avenues for su

152 le of using both HCO3(-) and CO2 had greater CO2 use as concentrations increased.

153 s would result in reductions of 0.19-0.53 Gt CO2 eqa(-1), 4.32-10.6 Gt [Formula: see text] eqa(-1), a

154 lion tonnes (MT) CH4 or 2.72 Gigatonnes (Gt) CO2 -eq (1 MT = 10(12) g, 1 Gt = 10(15) g) from ruminant

155 In particular the ability to grow with H2:CO2 or syngas (a mixture of H2/CO/CO2) makes these micro

156 nd meta-analysis, we assessed whether a high CO2 gap predicts mortality in adult critically ill patie

157 A high CO2 gap was associated with higher lactate levels (mean

158 A high CO2 gap was associated with increased mortality (odds ra

159 A high CO2 gap was not associated with longer ICU or hospital l

160 ons capable of featuring simultaneously high CO2 resistance and O2 permeability and the exploitation

161 of these materials, coupled with their high CO2 capacities and low projected energy costs, highlight

162 hocystis sp. PCC 6803 leads to a unique high-CO2-sensitive phenotype.

163 Developing rice cultivars with higher [CO2] responsiveness incorporated with increased toleranc

164 ent gap between research and applications in CO2 reduction, our review systematically and constructiv

165 oxygen, high pH, and enrichment of (13)C in CO2) indicate that upwelling of cold, nutrient-rich wate

166 ng the chemosensitive response to changes in CO2/H+ than previously thought.

167 he oxygen-18 isotopic ((18)O) composition in CO2 provides an important insight into the variation of

168 r test fleet, the measured 14.5% decrease in CO2 emissions from GDIs was much greater than the potent

169 d a new pathway for significant reduction in CO2 capture energy consumption.

170 Ignoring these reductions in CO2.a and theta could lead to a marked (45%) overestimat

171 re not accounting for observed reductions in CO2.a and theta that can occur at low temperature.

172 Bicarbonate dialysis results in CO2 removal at rates comparable with existing low-flow e

173 enhance synaptic transmission, mice inhaled CO2 to induce an acidosis and activate acid sensing ion

174 as much as half of the glacial-interglacial CO2 change.

175 ns, to the inclusion of these catalysts into CO2 electrolyzers and photo-electrochemical devices, and

176 SPP) spectroscopies were used to investigate CO2 reorientation and spectral diffusion dynamics in SIL

177 piration across all sites, although invoking CO2 effects on vegetation (growth enhancement and increa

178 ductivity and exp(H), while the asymptotic J(CO2) response on the silty clay arose from a net negativ

179 n poorly understood for soil CO(2) efflux, J(CO2), a primary carbon flux from the biosphere to the at

180 We found linear increases in J(CO2) on an alluvial sandy loam and a lowland clay soil,

181 from a single limiting factor, the linear J(CO2) response on the sandy loam was reinforced by positi

182 We identified the trajectory of J(CO2) responses and feedbacks from other resources, plant

183 tified CO(2) as the dominant limitation on J(CO2) on the clay soil.

184 eq) per person per day (pppd); 2030: 2.04 kg CO2-eq pppd; less strict 2030: 2.5 kg CO2-eq pppd; no ta

185 forcing of open-water fluxes (3.5 +/- 0.3 kg CO2 -eq m(-2) yr(-1) ) exceeded that of vegetated zones

186 eded that of vegetated zones (1.4 +/- 0.4 kg CO2 -eq m(-2) yr(-1) ) due to high ecosystem respiration

187 .04 kg CO2-eq pppd; less strict 2030: 2.5 kg CO2-eq pppd; no target], modeled eating patterns (food-b

188 50: 1.11 kg of carbon dioxide equivalent (kg CO2-eq) per person per day (pppd); 2030: 2.04 kg CO2-eq

189 tude and interannual variability of the land CO2 sink.

190 ring the last 50 years has generated a large CO2 concentration in the atmosphere that has led to the

191 high selectivities for CO2 adsorption, large CO2 removal capacities, and low regeneration energies ar

192 activity of the cathode, the as-prepared Li-CO2 batteries exhibit high reversibility, low polarizati

193 and stable photocatalysts for visible light CO2 reduction.

194 midity, we estimated that most of the litter CO2 efflux and decay occurring in the dry season was due

195 ng endoscopic and laparoscopic practice (low CO2 pressures, evacuation through ultrafiltration system

196 3 and 298 K, JUC-62 showed 51% and 34% lower CO2 uptake, respectively, than when UV light was off.

197 this study was: 1) to quantify membrane lung CO2 removal (VCO2ML) under different conditions and 2) t

198 nditions and 2) to quantify the natural lung CO2 removal (VCO2NL) and to what extent mechanical venti

199 monstrate how synthetic biology may maximize CO2 uptake within and above storage sites.

200 The mean CO2.a was 0.045 mol CO(2) mol(-1) absorbed quanta at 25

201 analyses are poorly constrained by measured CO2 exchange in drylands.

202 At 5 degrees C measured CO2.a was markedly reduced (0.025) and 60% lower than TB

203 .044), but as temperature decreased measured CO2.a diverged from TBMs.

204 thermal acclimation was tested by monitoring CO2 and CH4 production, CUE, and microbial biomass.

205 2008 Robeson upper bounds for O2/N2, H2/N2, CO2/N2, H2/CH4 and CO2/CH4, with the potential for bioga

206 absence of moisture stress resulting in net CO2 uptake increases in the shoulder seasons and decreas

207 A long-term net CO2 uptake of >200 g CO2 m(-2) yr(-1) is required to off

208 tock, which accounted for 47%-54% of all non-CO2 GHG emissions from the agricultural sector.

209 We argue that neither ice sheet dynamics nor CO2 change in isolation can explain the MPT.

210 Here, we identify several novel CO2-dependent changes in the NF-kappaB pathway.

211 us eddy covariance flux measurements of NOx, CO2, CO and non methane volatile organic compound tracer

212 with a precision better than 1% for N2, O2, CO2, He, Ar, 2% for Kr, 8% for Xe, and 3% for CH4, N2O a

213 which enables the simultaneous absorption of CO2 and SO2/SO3 from the flue gas.

214 eal CO2 removal removes a relevant amount of CO2 thus allowing mechanical ventilation to be significa

215 d-basalt eruptions released large amounts of CO2 and CH4 into the atmosphere, causing severe global w

216 xt-generation adsorbents for a wide array of CO2 separations.

217 irst summarize the most important aspects of CO2 capture and green routes to produce H2.

218 Our results show partial re-assimilation of CO2 and H2 by n-butanol-producer C. beijerinckii.

219 pectroscopic studies, molecular catalysis of CO2 reduction remains a highly creative approach.

220 e experimental apparatus based on changes of CO2 partial pressures.

221 The concentration of CO2 in many aquatic systems is variable, often lower tha

222 seudonana, to high and low concentrations of CO2 at the level of transcripts, proteins and enzyme act

223 under elevated vs ambient concentrations of CO2.

224 The contrasting of CO2 fluxes between inland and coastal wetlands globally

225 lent activities for catalyzing conversion of CO2 into cyclic carbonate (conversion >95% at 100 degree

226 We use the correlations of CO2 with trace elements to define an average carbon abun

227 adsorbent lifetime and operational costs of CO2 capture, is a multifaceted issue involving thermal,

228 s seismic cluster records rapid degassing of CO2, suggesting an interval of anomalous fluid source.

229 ing projections in response to a doubling of CO2-from 1.5 degrees C to 4.5 degrees C or greater -rema

230 However, the effects of CO2 enrichment on eutrophic coastal waters are still unc

231 complications because of electroreduction of CO2 to formate.

232 ficiency would then depend on the leakage of CO2 out of a chloroplast.

233 rcing of the climate by increasing levels of CO2 and CH4.

234 g dialysis, we removed 101 (+/-13) mL/min of CO2 (59 mL/min when normalized to venous PCO2 of 45 mm H

235 (MEA)-based postcombustion capture (PCC) of CO2 with distributed, humidity-swing-based direct air ca

236 tudy was to document the pharmacodynamics of CO2 for MBF using prospective end-tidal targeting to pre

237 vable first-day arterial partial pressure of CO2 of >=60 mm Hg.

238 of hydrogen without concurrent production of CO2 (unlike steam reforming) or CO (by complete methanol

239 nditions did not release a large quantity of CO2.

240 hat inhibition is caused by the reduction of CO2 into CO, whose high affinity with platinum triggers

241 f modern energy challenges, the reduction of CO2 into fuels calls for electrogenerated low-valent tra

242 The electrochemical reduction of CO2 is known to be influenced by the identity of the alk

243 and selective electrocatalytic reduction of CO2 to CO or formate - reactions that are very challengi

244 stable electrode for selective reduction of CO2 to ethanol.

245 matrix for the electrocatalytic reduction of CO2.

246 Direct releases of CO2 from litter layer only accounted for 19% increases i

247 result of glaciation may act as a source of CO2 to the atmosphere.

248 demonstrate that the use of two standards of CO2 in air of known but differing delta(13)C and delta(1

249 tailed understanding of the initial steps of CO2 electroreduction on copper surfaces, the best curren

250 of such materials, particularly in terms of CO2 adsorptive properties such as adsorption capacity, s

251 The utilization of CO2 as a carbon source for organic synthesis meets the u

252 he reaction mechanisms are reviewed based on CO2 capture literature as well as biological and atmosph

253 t Soil warming had a much stronger effect on CO2 flux than Air warming.

254 er volatile inventory, particularly of CO or CO2 ices, or contained amorphous ice, which could have t

255 racrine mechanisms, and via input from other CO2 -responsive neurons.

256 system climate sensitivity is K (1sigma) per CO2 doubling, which is notably higher than fast-feedback

257 adjusts stomatal conductance, photosynthetic CO2 and photorespiratory O2 fixation, and starch synthes

258 equivalents, and recycling of N and possibly CO2 through refixation.

259 o C-C bond breaking would produce protonated CO2, an energetically inaccessible species that can be a

260 rformance of a set of technologies to reduce CO2 emissions at refineries.

261 d globally, and ~1% of global energy-related CO2 emissions, the ambient electrocatalytic nitrogen red

262 trial applications such as soil remediation, CO2 sequestration, and enhanced oil recovery.

263 novel respiratory dialysis system to remove CO2 from blood in the form of bicarbonate.

264 e if our respiratory dialysis system removes CO2 at rates comparable to low-flow extracorporeal CO2 r

265 the posttranslational control of respiratory CO2 refixation and anaplerotic photosynthate partitionin

266 and 31.6% more apigenin than conventional SC-CO2 extraction and HRE, respectively.

267 horter than that required by conventional SC-CO2 extraction and HRE, respectively.

268 f rs4293393 was associated with higher serum CO2 level.

269 onsecutive supercritical carbon dioxide (SFE-CO2) pressurised liquid (PLE) and enzyme-assisted extrac

270 s influencing the biogeochemistry in shallow CO2-rich hydrothermal systems and the importance of coup

271 yer only accounted for 19% increases in soil CO2 flux, suggesting that the leaching of dissolved orga

272 soil is the major cause of rain-induced soil CO2 pulse.

273 ed DOC input in regulating rain-induced soil CO2 pulses and microbial community composition, and may

274 d energy conversion through water splitting, CO2 reduction and/or N2 fixation using photo- and photo(

275 accompanies methane emissions and stimulates CO2 consumption by photosynthesizing phytoplankton.

276 As a climate mitigation strategy, CO2 capture from flue gases of industrial processes-much

277 ium europaeum fruits following supercritical CO2 extraction (at 30MPa and 40 degrees C).

278 Our results also indicate that CO2 component remains soluble in the melt at high pressu

279 Physiologists have long known that CO2 directly affects acid-base and ion regulation, respi

280 nduced by CO2 , consistent with reports that CO2 directly stimulates adenylyl cyclase.

281 The CO2 solubility was measured using a home-made experiment

282 e whether resuscitation aimed at closing the CO2 gap improves mortality in shock.

283 RP may provide a molecular identifier of the CO2 arousal circuit.

284 About half of the CO2 produced came from plant tissue mineralization in in

285 sive and native communities; the rest of the CO2 was produced from SOM mineralization (priming).

286 time to glottis passage and first end-tidal CO2 measurement, degree of glottis visualization, and nu

287 collected mean arterial pressure, end-tidal CO2, and temperature.

288 Over longer timescales, CO2 release could act as a negative feedback, limiting p

289 f the most relevant and recent approaches to CO2-based monomers and polymers are highlighted with par

290 CGA is shown not a major contributor to CO2 formation, as heating of this compound under typical

291 boxylic acids measured indoors correlated to CO2 in daytime, suggesting that human occupants may cont

292 These have previously been linked to CO2 draw-down, but the severe cold climates of the Cryog

293 he upper branch of methyl group oxidation to CO2 as well as membrane-bound heterodisulfide reductase

294 Conversion of pyruvate to CO2 in the T. brucei bloodstream form provides new suppo

295 use many of the PBel neurons that respond to CO2 express calcitonin gene-related peptide (CGRP), we h

296 pacts conclusions on trees' W i responses to CO2 or climate.

297 omposition, plasma albumin, and plasma total CO2 accurately predict the measured pH of blood exiting

298 ith unprecedented catalytic stability toward CO2 reduction.

299 74-III results in a material that can uptake CO2 at low pressures through a chemisorption mechanism.

300 ver, the extraction time required by the USC-CO2 procedure, which used milder conditions, was approxi

301 s and separation units as well as to utilise CO2 and recycle side-products in the process are describ

302 A continuous-wave CO2 laser of wavelength 10.6 mum and a Trumpf Yb-YAG dis