ライフサイエンスコーパス: carbon dioxide

1 g drought, which leads to a large release of carbon dioxide.

2 les such as water, hydrogen, oxygen, proton, carbon dioxide.

3 onsequently the atmospheric concentration of carbon dioxide.

4 emperature and atmospheric concentrations of carbon dioxide.

5 bonds may be used for the transformation of carbon dioxide.

6 e-2-one moiety accompanied by the release of carbon dioxide.

7 shed avoidance of acidic fumes, ammonia, and carbon dioxide.

8 al cycle that enables capture and release of carbon dioxide.

9 of separating, compressing, and transporting carbon dioxide.

10 the tricarboxylic acid cycle (TCA cycle) to carbon dioxide.

11 upling with dialkylzinc reagents and loss of carbon dioxide.

12 ow levels of blood oxygen and high levels of carbon dioxide.

13 ective and energy-efficient removal of trace carbon dioxide.

14 lymers via alternating copolymerization with carbon dioxide.

15 uli that may respond to human body odours or carbon dioxide.

16 f dimethyl carbonate (DMC) from methanol and carbon dioxide.

17 t energy conversion is mainly used to reduce carbon dioxide.

18 ic-stretch rovibrational band of atmospheric carbon dioxide.

19 ing enzymatically converted into ammonia and carbon dioxide.

20 ved intermediate occurs to give ethylene and carbon dioxide.

21 the rate of electron transport from water to carbon dioxide.

22 pro-oxidant constituents of exhaust, namely, carbon dioxide (13%), carbon monoxide (0.68%) and nitrog

23 Carbon dioxide accumulation is a major concern for the e

24 Carbon dioxide adsorption in metal-organic frameworks ha

25 -ketocarboxylates 1(COOLi) in the absence of carbon dioxide allowed reactions to take place with nitr

26 sensing tag for the determination of oxygen, carbon dioxide, ammonia, and relative humidity readable

27 olvated MFM-188a exhibits exceptionally high carbon dioxide and acetylene adsorption uptakes with the

28 Here we report the binding domains of carbon dioxide and acetylene in a tetra-amide functional

29 ally and subsequent decarboxylation produces carbon dioxide and biuret.

30 richia coli normally oxidizes formic acid to carbon dioxide and couples that reaction directly to the

31 The developed catalyst activates carbon dioxide and delivers over 16% yield of DMC withou

32 ) as well as carbon stable isotope ratios of carbon dioxide and methane, above and below the pycnocli

33 he polynitro-CNT decomposition are nontoxic: carbon dioxide and molecular nitrogen.

34 phase behavior of systems containing water, carbon dioxide and organics has been important in severa

35 include rising atmospheric concentrations of carbon dioxide and other greenhouse gasses and resulting

36 illata were fractionated using supercritical carbon dioxide and pressurized liquid (ethanol and water

37 rongly resembles past changes in atmospheric carbon dioxide and terrigenous dust flux in the tropical

38 of controlled architecture in supercritical carbon dioxide and their use as stabilizers for water/ca

39 ce conductance as a response to increases in carbon dioxide and, more recently, to an abrupt decrease

40 Thermal insulation (carbon dioxide and/or hydrodissection), temperature moni

41 Methane, carbon dioxide, and BC were measured simultaneously, all

42 tarate oxygenase reaction to give succinate, carbon dioxide, and sometimes pyrroline-5-carboxylate oc

43 esis system producing primarily acetate from carbon dioxide, and their transcriptional activity was m

44 ensated hypercapnia [normal pH with elevated carbon dioxide], and hypercapnic acidosis) during the fi

45 t photodissociation to give iron(II) and the carbon dioxide anion radical.

46 , cyclohexene oxide, phthalic anhydride, and carbon dioxide-are investigated using a single dizinc ca

47 Using carbon dioxide as a feedstock to produce synthetic fuels

48 The sequence thus represents the use of carbon dioxide as a removable directing group for the se

49 For the efficient utilization of carbon dioxide as feedstock in chemical synthesis, low-e

50 pact of anthropogenic greenhouse gases after carbon dioxide, but our understanding of the global atmo

51 , and ameliorate atmospheric accumulation of carbon dioxide by 'pumping' carbon to the deep sea.

52 ermenters, followed by complete oxidation to carbon dioxide by heterotrophic sulfate-reducing bacteri

53 All-inorganic polynuclear units for reducing carbon dioxide by water at the nanoscale are introduced,

54 The reduction of carbon dioxide by water with sunlight in an artificial s

55 el variation was not influenced by change in carbon dioxide (C), but increased as much as 41% and 23%

56 Carbon dioxide can be electrochemically reduced to hydro

57 known how predicted increases in atmospheric carbon dioxide (CO2 ) and air temperature affect silicon

58 decompose stored organic carbon and release carbon dioxide (CO2 ) and CH4 .

59 ystem N cycling and its response to elevated carbon dioxide (CO2 ) and N addition.

60 s of carbon in their soils and can sequester carbon dioxide (CO2 ) at a greater rate per unit area th

61 Described for the first time is that carbon dioxide (CO2 ) can be successfully inserted into

62 important role in regulating the atmospheric carbon dioxide (CO2 ) concentrations and thus affecting

63 Models predicting ecosystem carbon dioxide (CO2 ) exchange under future climate chan

64 forcing relative to potential long-term net carbon dioxide (CO2 ) exchange.

65 t zone of northwestern Canada, boreal forest carbon dioxide (CO2 ) fluxes will be altered directly by

66 in these systems is far greater than that of carbon dioxide (CO2 ) in the atmosphere, and annual flux

67 Elevated carbon dioxide (CO2 ) levels are known to induce stomata

68 gnized for their role in the terrestrial net carbon dioxide (CO2 ) uptake, which depends largely on p

69 Carbon dioxide (CO2 ), a primary product of oxidative me

70 increased nitrogen (N) deposition, elevated carbon dioxide (CO2 ), and increased precipitation - on

71 ((14) C) of dissolved organic carbon (DOC), carbon dioxide (CO2 ), and methane (CH4 ) exported from

72 and N deposition (30 kg N ha(-1) yr(-1) ) on carbon dioxide (CO2 ), methane (CH4 ) and nitrous oxide

73 Carbon dioxide (CO2 ), methane (CH4 ), and nitrous oxide

74 climate via greenhouse gas (GHG) exchange of carbon dioxide (CO2 ), methane (CH4 ), and nitrous oxide

75 f methane (CH4) is significantly higher than carbon dioxide (CO2) and its enteric production by rumin

76 d the responses of soil nitrous oxide (N2O), carbon dioxide (CO2) and methane (CH4) emissions to manu

77 adation of dissolved organic matter (DOM) to carbon dioxide (CO2) and partially oxidized compounds is

78 We report that the environmental stress of carbon dioxide (CO2) anesthesia converts an asymptomatic

79 Anthropogenic emissions of carbon dioxide (CO2) are causing ocean acidification, lo

80 Using carbon dioxide (CO2) as a feedstock for commodity synthe

81 s with a significant drawdown of atmospheric carbon dioxide (CO2) at that time.

82 Gross primary production (GPP)-the uptake of carbon dioxide (CO2) by leaves, and its conversion to su

83 derable attention for their potential use in carbon dioxide (CO2) capture technologies because they a

84 le reveal distinct structures of atmospheric carbon dioxide (CO2) caused by known anthropogenic and n

85 t for the full amplitude of past atmospheric carbon dioxide (CO2) concentration variability over glac

86 between boreal summer insolation and global carbon dioxide (CO2) concentration, which explains the b

87 Plants buffer increasing atmospheric carbon dioxide (CO2) concentrations through enhanced gro

88 id-state materials for carbon capture at low carbon dioxide (CO2) concentrations, namely, from confin

89 lectrochemical systems (BESs), which convert carbon dioxide (CO2) directly to methane (CH4), promise

90 ting the feasibility of accelerating gaseous carbon dioxide (CO2) dissolution into a continuous aqueo

91 monoxide (CO), particulate matter (PM), and carbon dioxide (CO2) emission rates were measured for th

92 egate criteria for fleet fuel efficiency and carbon dioxide (CO2) emission rates.

93 urrently offset one-quarter of anthropogenic carbon dioxide (CO2) emissions because of a slight imbal

94 y-mean September sea-ice area and cumulative carbon dioxide (CO2) emissions to infer the future evolu

95 fail to communicate the urgency of reducing carbon dioxide (CO2) emissions.

96 Terrer et al used meta-analysis of carbon dioxide (CO2) enrichment experiments as evidence

97 ce sheet formed on Antarctica as atmospheric carbon dioxide (CO2) fell below ~750 parts per million (

98 quantitative effects of grazing on ecosystem carbon dioxide (CO2) fluxes in this zone remain unclear.

99 Spaceborne observations of carbon dioxide (CO2) from the Orbiting Carbon Observator

100 Trapping with carbon dioxide (CO2) gave the respective O-[Zr] bonded c

101 On the other hand, biological uptake of carbon dioxide (CO2) has the potential to offset the pos

102 Concentrations of atmospheric carbon dioxide (CO2) have continued to increase whereas

103 /aluminum oxide (Cu/ZnO/Al2O3) catalysts for carbon dioxide (CO2) hydrogenation to methanol, the Zn-C

104 olution below its freezing point using solid carbon dioxide (CO2) in an isopropanol bath.

105 ges in climate and the seasonal amplitude of carbon dioxide (CO2) in the Arctic, it is critical that

106 ter pH due to rising levels of anthropogenic carbon dioxide (CO2) in the world's oceans is a major fo

107 the increasing concentration of atmospheric carbon dioxide (CO2) is altering the productivity of the

108 fication of seawater caused by anthropogenic carbon dioxide (CO2) is anticipated to influence the gro

109 Although carbon dioxide (CO2) is highly abundant, its low reactiv

110 Carbon dioxide (CO2) is one of the most abundant species

111 Increasing atmospheric carbon dioxide (CO2) is the principal driver of anthropo

112 owever, existing estimates place atmospheric carbon dioxide (CO2) levels during the Eocene at 500-3,0

113 e (labeled Green+) and artificially elevated carbon dioxide (CO2) levels independent of ventilation.

114 s in the measured growth rate of atmospheric carbon dioxide (CO2) originate primarily from fluctuatio

115 tive than grain surfaces for electrochemical carbon dioxide (CO2) reduction to carbon monoxide (CO) b

116 olecular electrocatalysts for proton-coupled carbon dioxide (CO2) reduction to carbon monoxide (CO).

117 strumental in carbon cycling and atmospheric carbon dioxide (CO2) regulation.

118 stainable energy decarbonization futures and carbon dioxide (CO2) removal rates will be an important

119 s N) has shown an enhanced seasonal cycle of carbon dioxide (CO2) since the 1960s, but the underlying

120 nd the reduction of carbon monoxide (CO) and carbon dioxide (CO2) to hydrocarbons, two reactions usef

121 (BES) is key to the efficient conversion of carbon dioxide (CO2) to methane (CH4) with application t

122 y described as having the capacity to reduce carbon dioxide (CO2) to methane (CH4).

123 ave the capacity to release large amounts of carbon dioxide (CO2) to the atmosphere in response to in

124 ant respiration results in an annual flux of carbon dioxide (CO2) to the atmosphere that is six times

125 ropics, while the growth rate of atmospheric carbon dioxide (CO2) was the largest on record.

126 Carbon dioxide (CO2) which constitutes a major part of t

127 as - a gas mixture containing hydrogen (H2), carbon dioxide (CO2), and carbon monoxide (CO), or with

128 s) were calculated for carbon monoxide (CO), carbon dioxide (CO2), and particulate matter (PM).

129 between attractive or aversive responses to carbon dioxide (CO2), depending on its recently experien

130 ocean is the largest sink for anthropogenic carbon dioxide (CO2), having absorbed roughly 40 per cen

131 can release or absorb the greenhouse gases, carbon dioxide (CO2), methane (CH4) and nitrous oxide (N

132 primary standard mixtures (PSMs) comprising carbon dioxide (CO2), methane (CH4), and nitrous oxide (

133 oxygen (O2), ozone (O3), water vapor (H2O), carbon dioxide (CO2), nitrous oxide (N2O), and methane (

134 rminant of the atmosphere-ocean partition of carbon dioxide (CO2).

135 mospheric greenhouse gases methane (CH4) and carbon dioxide (CO2).

136 )] surfaces to hydrogen (H2) and mixtures of carbon dioxide (CO2)/H2 show an absence of carbon (C) 1s

137 impact microbial acclimation and the rate of carbon-dioxide (CO2 ) and methane (CH4 ) production.

138 ield by rising concentrations of atmospheric carbon dioxide ([CO2]) is widely expected to counteract

139 he fluxes of other volcanic gases (including carbon dioxide, CO2) and toxic trace metals (e.g., mercu

140 t, present and future changes in atmospheric carbon dioxide concentration ([CO2 ]) is critical for un

141 Rising atmospheric carbon dioxide concentration ([CO2]) may modulate the fu

142 ccessions under controlled conditions at two carbon dioxide concentrations (400 and 600 ppm) and four

143 arterial pressure, tidal volume, respiratory carbon dioxide concentrations and peroneal nerve muscle

144 ques for investigating dissolved methane and carbon dioxide concentrations and stable isotopic dynami

145 otoplethysmographic arterial pressure, tidal carbon dioxide concentrations and volumes, and peroneal

146 Atmospheric carbon dioxide concentrations have been rising during th

147 non-invasive arterial pressure, respiratory carbon dioxide concentrations, breathing depth and sympa

148 ally climate change and elevated atmospheric carbon dioxide concentrations-are increasing demand for

149 al absorption in cuprous oxide for selective carbon dioxide conversion to carbon monoxide with visibl

150 approach to utilization and valorization of carbon dioxide could be developed at industrially signif

151 cing mesophyll conductance (i.e. the rate of carbon dioxide diffusion from substomatal cavities to th

152 eservoirs when simulating future atmospheric carbon dioxide dynamics.

153 is, ecosystem-level carbon exchange and soil carbon dioxide efflux with local meteorology data.

154 erature solid oxide cells, and in particular carbon dioxide electrolysers, afford chemical storage of

155 atalysts displaying lower overpotentials for carbon dioxide electroreduction and record selectivity t

156 cant reductions in oxygen consumption and of carbon dioxide emission in cancer patients receiving ami

157 We valued the delayed carbon dioxide emissions and found that this program ben

158 Anthropogenic carbon dioxide emissions are known to alter hydrological

159 From 1890 to 2015, anthropogenic carbon dioxide emissions have increased atmospheric CO2

160 economic cost caused by an additional ton of carbon dioxide emissions or its equivalent.

161 Less than half of anthropogenic carbon dioxide emissions remain in the atmosphere.

162 eight saving is crucial for the reduction of carbon dioxide emissions.

163 oxide and their use as stabilizers for water/carbon dioxide emulsions then are covered.

164 on, using data from the Duke Forest Free-Air Carbon dioxide Enrichment (FACE) experiment, a forest ch

165 7 by 1.3 to 2.6% (0.6-1.1 billion mega-grams carbon-dioxide-equivalent (Mg CO2e(-1)) compared to thos

166 ilogram of food waste range from -0.20 kg of carbon dioxide equivalents (CO2e) for anaerobic digestio

167 eal time during the PPV, including end-tidal carbon dioxide (ETCO2), oxygen saturation (SaO2), intra-

168 ntrations of four gaseous compounds, oxygen, carbon dioxide, ethylene, and nitric oxide, change durin

169 Supercritical carbon dioxide extraction of bioactive compounds from gu

170 The Calvin-Benson cycle of carbon dioxide fixation in chloroplasts is controlled by

171 tein organelle, the carboxysome, to catalyze carbon dioxide fixation in the Calvin Cycle.

172 ase pattern of soil organic matter decay and carbon dioxide fluxes to the atmosphere, with phases of

173 , requires low environmental oxygen and high carbon dioxide for optimum growth, but the molecular bas

174 neously tasked with permitting the uptake of carbon dioxide for photosynthesis while limiting water l

175 of wellbore cement that has been exposed to carbon dioxide for three decades.

176 propane, n-butane and iso-butane as well as carbon dioxide for two shales and isolated kerogens dete

177 e capacity (gsmax ), and hence the uptake of carbon dioxide for water lost.

178 Carbon dioxide forms covalent complexes with N-heterocyc

179 nickel- or iron-based catalysis, to extract carbon dioxide from a carboxylic acid and economically r

180 xes of methane, nonmethane hydrocarbons, and carbon dioxide from natural gas well pad soils and from

181 which give us shelter and oxygen and remove carbon dioxide from the atmosphere.

182 f organic carbon in marine sediments removes carbon dioxide from the ocean-atmosphere pool, provides

183 form new carbon-carbon bonds by introducing carbon dioxide gas (CO2) or its hydrated form, bicarbona

184 anic solutes between water and supercritical carbon dioxide have been correlated with extended linear

185 ncreases in temperature, water, nitrogen and carbon-dioxide have been maintained for over 15 years.

186 cally unfavourable product for the important carbon dioxide hydrogenation reaction.

187 -based Li-rich garnets react with water and carbon dioxide in air to form a Li-ion insulating Li2 CO

188 nsible for the high uptakes of acetylene and carbon dioxide in MFM-188a.

189 ol on the simultaneous exchange of water and carbon dioxide in terrestrial ecosystems.

190 onse of the brainstem to increased levels of carbon dioxide in the blood is coordinated with the resp

191 We previously demonstrated that carbon dioxide inhalation could induce panic anxiety in

192 During laparoscopic surgery, carbon dioxide insufflation may produce significant hemo

193 Electroreduction of carbon dioxide into higher-energy liquid fuels and chemi

194 ble energy to convert waste products such as carbon dioxide into hydrocarbon fuels.

195 s) catalyse the electrochemical reduction of carbon dioxide into multi-carbon hydrocarbons and oxygen

196 hydrogen that is released is used to convert carbon dioxide into the organic molecules that constitut

197 Carbon dioxide is an essential atmospheric component in

198 Increasing atmospheric carbon dioxide is driving a long-term decrease in ocean

199 Carbon dioxide is Mars' primary atmospheric constituent

200 stry in combination with reduced emission of carbon dioxide is one of the most pressing challenges of

201 Carbon dioxide is the ultimate source of the fossil fuel

202 on monoxide plus water yields dihydrogen and carbon dioxide) is an essential process for hydrogen gen

203 [(11)C]Carbon dioxide itself, [(11)C]carbon monoxide, [(11)C]cy

204 cing procedures, specifically fully ablative carbon dioxide laser or medium-depth chemical peel.

205 rosions occurring after ablative procedures (carbon dioxide laser resurfacing or Jessner solution/tri

206 Tissue-sparing surgical techniques and carbon dioxide laser treatments also are available, but

207 sis of triethylamine (1a) in the presence of carbon dioxide leads to the hydrogenation of CO2, the al

208 hree groups based on a combination of pH and carbon dioxide levels (normocapnia and normal pH, compen

209 de removal may be useful to normalize pH and carbon dioxide levels, but further studies will be neces

210 thysmographic arterial pressure, respiratory carbon dioxide levels, tidal volume and peroneal nerve m

211 le-rat to living in an environment with high-carbon dioxide levels.

212 However, in the absence of organic carbon, carbon dioxide may be fixed via the ribulose bisphosphat

213 rements of the three major greenhouse gases (carbon dioxide, methane, and nitrous oxide) as well as c

214 Diurnal measurements of methane and carbon dioxide mole fraction, and isotopic values at Kin

215 pts an intermediate chemical state between a carbon dioxide molecule and a carbonate ion.

216 s hourly water consumption, emissions (i.e., carbon dioxide, nitrogen oxides, and sulfur oxides), and

217 also showed two molecules of the co-product, carbon dioxide, one in the active site and another trapp

218 (11)C]methyl triflate (generated from [(11)C]carbon dioxide or [(11)C]methane).

219 face temperature per doubling of atmospheric carbon dioxide over millennium timescales.

220 uated framework shows excellent affinity for carbon dioxide over nitrogen and adsorbs ca. 3 wt % of C

221 eduction in the partial pressure of arterial carbon dioxide (P aC O2) and cerebral vasoconstriction.

222 = 10(-3.5)) or reduced partial pressures of carbon dioxide (PCO2 = 10(-4.5)).

223 l peatlands now emit hundreds of megatons of carbon dioxide per year because of human disruption of t

224 After establishing carbon dioxide pneumoperitoneum in 6 male piglets and ma

225 CI, -0.2 to 0.2 L/min; P = .72), or partial carbon-dioxide pressure in arterial blood (-0.3 mm Hg; 9

226 We used supercritical carbon dioxide process to encapsulate ATRA in largely un

227 of predicted, and median minute ventilation/carbon dioxide production slope 34.9 (IQR, 27.9-39.4).

228 ion predicted, and higher minute ventilation/carbon dioxide production slope.

229 he sample and relate these quantities to the carbon dioxide reaction front on the cement.

230 th cerebral blood flow, oxygen delivery, and carbon dioxide reactivity remain unknown.

231 pt for ventriculomegaly in the BDG group) or carbon dioxide reactivity with neurological injury.

232 e reaction of lithium enolates 2(Li(+)) with carbon dioxide, readily undergo decarboxylative dispropo

233 of the recently described hydrogen-dependent carbon dioxide reductase (HDCR) complex, which substanti

234 ate as a highly efficient hydrogen-dependent carbon dioxide reductase when gaseous CO2 and H2 are pla

235 also for the hydrogen evolution (Co-N-C) and carbon dioxide reduction (Fe-N-C and Mn-N-C).

236 of 543 s(-1), Km of 57.1 muM), but also the carbon dioxide reduction (kcat of 46.6 s(-1), Km of 15.7

237 both Dd FDH-catalyzed formate oxidation and carbon dioxide reduction are completely inactivated by c

238 ism is here suggested: formate oxidation and carbon dioxide reduction are proposed to proceed through

239 g fresh insights into how to design improved carbon dioxide reduction catalysts.

240 cobalt-phthalocyanine-based high-performance carbon dioxide reduction electrocatalyst material develo

241 QDs show a high total Faradaic efficiency of carbon dioxide reduction of up to 90%, with selectivity

242 report our investigations of electrochemical carbon dioxide reduction over CuAg bimetallic electrodes

243 g of trends in electrocatalytic activity for carbon dioxide reduction over different metal catalysts

244 Electrochemical carbon dioxide reduction to fuels presents one of the gr

245 ctions such as hydrogen peroxide production, carbon dioxide reduction, and nitrogen reduction, where

246 ong the electrocatalysts screened so far for carbon dioxide reduction, which includes metals, alloys,

247 f-replicating route toward solar-to-chemical carbon dioxide reduction.

248 with fossil-based chemicals and fuels, then carbon dioxide refineries envisioned in the future would

249 ssess efficient endosomal escape via a novel carbon dioxide release mechanism without compromising th

250 proximately one-quarter of the anthropogenic carbon dioxide released into the atmosphere each year is

251 phic climate change will require atmospheric carbon dioxide removal (CDR).

252 The dissolved CO2 is removed by a carbon dioxide removal device prior to detection.

253 Mechanical adjuncts such as extracorporeal carbon dioxide removal may be useful to normalize pH and

254 ng solar radiation management techniques and carbon dioxide removal technologies.

255 imum growth, but the molecular basis for the carbon dioxide requirement is unclear.

256 Supercritical carbon dioxide (SC-CO2) extraction of sunflower seed for

257 In this study, supercritical carbon dioxide (SC-CO2) extraction was optimized for ope

258 method based on atomization of supercritical carbon dioxide (SC-CO2)-expanded lipid.

259 wellbeing and is standard in social cost of carbon dioxide (SCC) models, and of average utilitariani

260 were biorefined by consecutive supercritical carbon dioxide (SFE-CO2) pressurised liquid (PLE) and en

261 he chemistry used by nature to functionalize carbon dioxide should be helpful for the development of

262 Carbon dioxide sorption isotherms were studied to 30 bar

263 ted the use of a synthetic biogas mixture as carbon dioxide source, yielding similarly high MES perfo

264 show that at low pressures up to 15 GPa, the carbon dioxide speciation is dominated by molecular form

265 methyl phosphonate in positive polarity and carbon dioxide, sulfur dioxide, hydrochloric acid, cyano

266 n important role in the observed atmospheric carbon dioxide swings by affecting the partitioning of c

267 A solid phase in the mixed water-carbon dioxide system, previously identified as carbonic

268 The effect of supercritical carbon dioxide technology (SCCD, 14, 16, and 18MPa at 35

269 In particular, monomers such as carbon dioxide, terpenes, vegetable oils and carbohydrat

270 gross primary production (GPP)-the amount of carbon dioxide that is 'fixed' into organic material thr

271 eam or supercritical atmosphere of water and carbon dioxide that was outgassed during magma ocean coo

272 Chemical weathering consumes atmospheric carbon dioxide through the breakdown of silicate mineral

273 at the same time as controlling the level of carbon dioxide, thus precluding them from modelling the

274 idation state +II, it is capable of reducing carbon dioxide to afford a zwitterionic compound, [OP(mu

275 ogeneous and heterogeneous catalysts convert carbon dioxide to carbon monoxide, further deoxygenative

276 rogeneous catalytic hydrogenation of gaseous carbon dioxide to chemicals and fuels.

277 h oleic acid, n-octadecylphosphonic acid, or carbon dioxide to form surface bound n-alkylammonium ole

278 Hydrogen-dependent reduction of carbon dioxide to formic acid offers a promising route t

279 Reducing carbon dioxide to hydrocarbon fuel with solar energy is

280 Direct conversion of carbon dioxide to multicarbon products remains as a gran

281 tive catalyst for electrochemically reducing carbon dioxide to products such as methane, ethene, and

282 this study, we instead add compressed liquid carbon dioxide to the extraction phase to accomplish fas

283 omato oleoresins, extracted by supercritical carbon dioxide, to obtain freeze-dried powders useful as

284 and fully characterized in the reaction with carbon dioxide under mild conditions.

285 tiana (tobacco), resulting in increased leaf carbon dioxide uptake and plant dry matter productivity

286 ibuted to short-term declines in terrestrial carbon dioxide uptake and storage.

287 Stomata are important regulators of carbon dioxide uptake and transpirational water loss.

288 ooling effect resulting from the global land carbon dioxide uptake from 2001 to 2010.

289 n leaf surfaces through which water loss and carbon dioxide uptake occur, are closed in response to d

290 stomatal pores that optimize photosynthetic carbon dioxide uptake with minimal water loss.

291 The electrochemical reduction of carbon dioxide using renewably generated electricity off

292 new efficient (bio)catalysts for atmospheric carbon dioxide utilization.

293 sociations of cognitive function scores with carbon dioxide, ventilation, and volatile organic compou

294 ans formate dehydrogenase (Dd FDH) to reduce carbon dioxide was kinetically and mechanistically chara

295 olactone (BBL), cyclohexene oxide (CHO), and carbon dioxide were realized in one-pot reactions utiliz

296 at of adsorption as low as 20 kJ mol(-1) for carbon dioxide, which could bring a distinct economic ad

297 lungs by determining local concentrations of carbon dioxide, which will be produced by healthy parts

298 The capture of carbon dioxide with chemical solvents is one solution to

299 Supercritical carbon dioxide with ethanol as co-solvent was used to ex

300 Electrochemical reduction of carbon dioxide with renewable energy is a sustainable wa