ライフサイエンスコーパス: carbon dioxide

1 d the carboxylic group and the liberation of carbon dioxide.

2 ing feedback on the atmospheric inventory of carbon dioxide.

3 ice albedo under high levels of atmospheric carbon dioxide.

4 in copolymerizations of other epoxides with carbon dioxide.

5 tween expanding anoxic zones and atmospheric carbon dioxide.

6 high negative potential required to activate carbon dioxide.

7 atmosphere, in longevity, as aerial carbon - carbon dioxide.

8 can increase agricultural output and remove carbon dioxide.

9 e review ten pathways for the utilization of carbon dioxide.

10 er concentration in the alcohol modifier and carbon dioxide.

11 hich the oceans act as a sink of atmospheric carbon dioxide.

12 olumetric working capacities for methane and carbon dioxide.

13 uoride solution in the presence of gas-phase carbon dioxide.

14 iving from oxidizing methane via methanol to carbon dioxide.

15 ation through uptake and storage of heat and carbon dioxide.

16 RBCs) transport oxygen to tissues and remove carbon dioxide.

17 driven upwelling, each affecting atmospheric carbon dioxide.

18 ial electroreduction of nitrogen oxides over carbon dioxide.

19 gas emissions and capture excess atmospheric carbon dioxide(1,2).

20 licate weathering, which removes atmospheric carbon dioxide(3,4).

21 This obliquity-induced lag, in turn, makes carbon dioxide a delayed climate amplifier in the late P

22 Rising carbon dioxide, acclimation, adaptation, and migration c

23 he defect alone acted as catalytic sites for carbon dioxide activation and hydrogen dissociation and

24 luding extended electrochemical window, high carbon dioxide activity, significantly reduced evaporati

25 ML predictions for the methane and carbon dioxide adsorption capacities of several tens of

26 ted with protons as a result of moisture and carbon dioxide adsorption from the air.

27 he expected net effect of rising atmospheric carbon dioxide and air temperature(7-9).

28 primary role is the rapid interconversion of carbon dioxide and bicarbonate in the cells, where carbo

29 ilization and polycarbonate selectivity) for carbon dioxide and cyclohexene oxide copolymerization.

30 Carbon dioxide and epoxide copolymerization is an indust

31 to sharp historical decreases in atmospheric carbon dioxide and global temperatures.

32 However, the lowest measured carbon dioxide and methane concentrations and Antarctic

33 d we hypothesize the increase of atmospheric carbon dioxide and methane from burning, preparing, and

34 de mixture) from two global warming gases of carbon dioxide and methane via dry reforming is environm

35 ns and stable isotope signatures of methane, carbon dioxide and nitrate and monitored microbial commu

36 into subduction zones, affecting atmospheric carbon dioxide and oxygen over Earth's history.

37 ey role in the global balance of atmospheric carbon dioxide and oxygen.

38 The ring-opening copolymerization of carbon dioxide and propene oxide is a useful means to va

39 a large aboveground surface area to collect carbon dioxide and sunlight and a large underground surf

40 on buffer capacity, the radiative forcing of carbon dioxide and the carbon inventory of the ocean.

41 ch reduced the leakage of deeply sequestered carbon dioxide and thus contributed to the lower atmosph

42 Application of exogenous ethylene, carbon dioxide and treatment to high temperatures is not

43 suggesting decarboxylation and conversion to carbon dioxide and water.

44 nic upper-ocean warming, increased dissolved carbon dioxide, and acidification will affect the distri

45 genate methoxy groups to carbon monoxide and carbon dioxide, and it directly converted this species t

46 nterplay between Hb (hemoglobin) and oxygen, carbon dioxide, and nitric oxide-the three-gas respirato

47 n the blood, including the levels of oxygen, carbon dioxide, and pH, and regulate breathing.

48 cooling, decline in the partial pressure of carbon dioxide, and the establishment of permanent polar

49 lactic acid and arterial partial pressure of carbon dioxide, and thickened left ventricular wall with

50 In this process, many bubbles of carbon dioxide are instantly formed in the sample matrix

51 ble fuels and chemicals using greenhouse gas carbon dioxide as the carbon feedstock.

52 d by GC-MS analyses, and thus, the collected carbon dioxide at 350 degrees C results can be assigned

53 Carbon dioxide at high flow rates (up to 4.0 mL/min) is

54 s other mineral carbonates only decompose to carbon dioxide at temperatures above 700 degrees C.

55 ial tilt)-can explain the lag of atmospheric carbon dioxide behind climate during glacial inception a

56 etic microalgae not only perform fixation of carbon dioxide but also produce valuable byproducts such

57 here a synthetic protocol to the fixation of carbon dioxide by converting it directly into aviation j

58 s, given the gaseous nature of the resulting carbon dioxide byproduct.

59 high-temperature liquid-phase materials for carbon dioxide capture and we propose here that they can

60 e relationship between imidazole acidity and carbon dioxide capture is explored computationally, both

61 ims for providing sufficient oxygenation and carbon dioxide clearance, while limiting the harmful eff

62 of ocean acidification driven by increasing carbon dioxide (CO(2) ) absorption by the ocean as well

63 products in the electrochemical reduction of carbon dioxide (CO(2) ) and carbon monoxide (CO) on copp

64 angrove wetlands in sequestering atmospheric carbon dioxide (CO(2) ) and mitigating climate change ha

65 itrous oxide (N(2) O), methane (CH(4) ), and carbon dioxide (CO(2) ) are affected by complex interact

66 ne (C(2) H(4) ), acetylene (C(2) H(2) ), and carbon dioxide (CO(2) ) can be regulated by temperature.

67 Rising atmospheric carbon dioxide (CO(2) ) concentrations may warm northern

68 ication (OA), a consequence of anthropogenic carbon dioxide (CO(2) ) emissions, strongly impacts mari

69 Autotrophic carbon dioxide (CO(2) ) fixation by microbes is ubiquito

70 The conductance of carbon dioxide (CO(2) ) from the substomatal cavities to

71 Methanation of carbon dioxide (CO(2) ) is attractive within the context

72 Chronically elevated carbon dioxide (CO(2) ) levels can occur in confined spa

73 atellite observations to investigate the net carbon dioxide (CO(2) ) seasonal cycle and its climatic

74 issions and can offset summer photosynthetic carbon dioxide (CO(2) ) uptake.

75 etic acclimation to elevated temperature and carbon dioxide (CO(2) ).

76 easurements of atmospheric oxygen (O(2)) and carbon dioxide (CO(2)) - levels of which increase as the

77 tivity driven by increased concentrations of carbon dioxide (CO(2)) [i.e., the CO(2) fertilization ef

78 ghted median cumulative emissions by 38.3 Tg carbon dioxide (CO(2)) and 0.6 Tg particulate matter (PM

79 composite sorbents that selectively capture carbon dioxide (CO(2)) and can purify biogas to natural

80 xpenditure (TEE), oxygen (O(2)) consumption, carbon dioxide (CO(2)) and metabolic heat (H(prod)) prod

81 hold heating bills and increase damages from carbon dioxide (CO(2)) and other pollutants.

82 n by increasing concentration of atmospheric carbon dioxide (CO(2)) and rising earth-surface temperat

83 BAGs sense the respiratory gas carbon dioxide (CO(2)) and, in a context-dependent manne

84 and arylamine in water medium under a 1 atm carbon dioxide (CO(2)) atmosphere.

85 Carbon dioxide (CO(2)) capture and storage (CCS) has bee

86 ry approach, that this compound is ideal for carbon dioxide (CO(2)) capture in addition to other anth

87 plasticity induced by ethyl butyrate (EB) or carbon dioxide (CO(2)) closes within 48 h after eclosion

88 elations between the apparent photosynthetic carbon dioxide (CO(2)) compensation point in the absence

89 anochannels led to a substantial increase in carbon dioxide (CO(2)) conversion and methanol yield in

90 ve HC emissions as increased noise in the HC/carbon dioxide (CO(2)) correlation measurement.

91 The electrocatalytic reduction of carbon dioxide (CO(2)) could be a powerful tool for gene

92 nental rifts are important sources of mantle carbon dioxide (CO(2)) emission into Earth's atmosphere(

93 global mean temperatures relies on reducing carbon dioxide (CO(2)) emissions and on the removal of C

94 Anthropogenic carbon dioxide (CO(2)) emissions contribute to the green

95 Carbon dioxide (CO(2)) emissions from freshwater ecosyst

96 Yet, data on carbon dioxide (CO(2)) emissions from these sediments ar

97 nding of how global consumption drives local carbon dioxide (CO(2)) emissions with a fine spatial res

98 e absorbs about 25 per cent of anthropogenic carbon dioxide (CO(2)) emissions, the rate of land carbo

99 attributes and their contributions to offset carbon dioxide (CO(2)) emissions.

100 human activities, and in turn energy use and carbon dioxide (CO(2)) emissions.

101 The oceanic uptake of atmospheric carbon dioxide (CO(2)) emitted by human activities alter

102 mising avenue for solar fuels synthesis from carbon dioxide (CO(2)) fixation but is extremely challen

103 faster rates of net H(2) oxidation and dark carbon dioxide (CO(2)) fixation than those from the carb

104 technologies capable of efficiently removing carbon dioxide (CO(2)) from the flue emissions of natura

105 However, the low polarity of supercritical carbon dioxide (CO(2)) has limited the use of SFC for se

106 eristic patterns of the net uptake fluxes of carbon dioxide (CO(2)) in coastal salt marshes using dim

107 Sequestration of industrial carbon dioxide (CO(2)) in deep geological saline aquifer

108 ts of sea surface salinity, temperature, and carbon dioxide (CO(2)) in the Gulf of Mexico (GoM) were

109 The solubility of carbon dioxide (CO(2)) in the moisture and protein compo

110 Converting carbon dioxide (CO(2)) into liquid fuels and synthesis g

111 Net anthropogenic emissions of carbon dioxide (CO(2)) must approach zero by mid-century

112 and tolerate the low oxygen (O(2)) and high carbon dioxide (CO(2)) of a densely populated fossorial

113 h a global warming potential 86-125x that of carbon dioxide (CO(2)) over a twenty-year period, is the

114 e global CDR goals of 0.5 to 2 gigatonnes of carbon dioxide (CO(2)) per year with extraction costs of

115 The electrochemical reduction of carbon dioxide (CO(2)) powered by renewable energy is an

116 Electrochemical carbon dioxide (CO(2)) reduction can in principle conver

117 -) reduction to hydrogen sulfide (H(2)S) and carbon dioxide (CO(2)) reduction to methane (CH(4)).

118 croplands, has potential use for atmospheric carbon dioxide (CO(2)) removal (CDR), which is now neces

119 erate climate change by releasing additional carbon dioxide (CO(2)) to the atmosphere(3-6).

120 ve route to upgrade greenhouse gases such as carbon dioxide (CO(2)) to valuable fuels and feedstocks;

121 Electrochemical conversion of carbon dioxide (CO(2)) to value-added chemicals has attr

122 es are biocatalysts that capture and convert carbon dioxide (CO(2)) under mild conditions and atmosph

123 Attractive cues include carbon dioxide (CO(2)), a major component of exhaled bre

124 Composting is the largest source of CH(4), carbon dioxide (CO(2)), nitrous oxide (N(2)O), and carbo

125 used for small molecules activation, such as carbon dioxide (CO(2)), nitrous oxide (N(2)O), tetrahydr

126 Carbon dioxide (CO(2)), the major product of metabolism,

127 concentration of several pollutants such as carbon dioxide (CO(2)), tropospheric ozone (O(3)), and p

128 global energy demand and the need to replace carbon dioxide (CO(2))-emitting fossil fuels with renewa

129 a managed carbonation step involving gaseous carbon dioxide (CO(2)).

130 rgo carbonation reactions and thus sequester carbon dioxide (CO(2)).

131 The electroreduction of carbon dioxide (CO(2)RR) to valuable chemicals is a prom

132 ironmental change factors (warming, elevated carbon dioxide [CO(2) ], increased precipitation, increa

133 ly, long-term forcing from Deccan volcanism (carbon dioxide [CO(2)]-induced warming) leads to increas

134 urn scars treated with a fractional ablative carbon dioxide (CO2) laser.

135 olved in high light responses, including the carbon dioxide concentrating mechanism, photorespiration

136 otosynthetic organisms on earth have evolved carbon dioxide concentrating mechanisms to contend with

137 Atmospheric carbon dioxide concentration ([CO(2) ]) is increasing, w

138 illations were more sensitive to atmospheric carbon dioxide concentration than to humidity, suggestin

139 rticles, which acts to lower the atmospheric carbon dioxide concentration.

140 arming and two years of elevated atmospheric carbon dioxide concentrations (eCO(2)).

141 edicted a notable number of anomalously high carbon dioxide concentrations at ground stations, becaus

142 e requires a combination of both atmospheric carbon dioxide concentrations of 1,120-1,680 parts per m

143 tive feedbacks among stomatal sensitivity to carbon dioxide concentrations, soil moisture, and vapor

144 tabilization, further increasing atmospheric carbon dioxide concentrations.

145 and the exponential increases of methane and carbon dioxide concentrations.

146 Combustion Method, and the catalyst shows a carbon dioxide conversion through hydrogenation to hydro

147 guide efforts to engineer biotechnology for carbon dioxide conversion.

148 Elevated atmospheric carbon dioxide (eCO(2) ) is predicted to increase growth

149 otentially limit plant responses to elevated carbon dioxide (eCO(2) ), but consensus has yet to be re

150 ding the potential impact of contaminants on carbon dioxide electrolysis is crucial for practical app

151 energy and carbon losses in low-temperature carbon dioxide electrolysis.

152 ert to hyperoxia and other TRPA1 activators (carbon dioxide, electrophiles, and oxidants) in normoxia

153 ide, nitrogen dioxide, and nitrous oxide, on carbon dioxide electroreduction on three model electroca

154 o a considerable Faradaic efficiency loss in carbon dioxide electroreduction, which is caused by the

155 date the mechanisms of oxygen absorption and carbon dioxide elimination.

156 en oxides, hydrocarbon, carbon monoxide, and carbon dioxide emission rates, the locations of emission

157 removing about 15 per cent of anthropogenic carbon dioxide emissions(1-3).

158 Carbon capture is essential for mitigating carbon dioxide emissions.

159 Atmospheric carbon dioxide enrichment (eCO(2)) can enhance plant car

160 t Research (BIFoR) began to conduct Free Air Carbon Dioxide Enrichment (FACE) within a mature broadle

161 Carbon dioxide/epoxide copolymerization is an efficient

162 liances, corresponding to ~830 [530-4500] Gg carbon dioxide equivalent (CO(2)e(100)).

163 ich we varied GHGE targets [2050: 1.11 kg of carbon dioxide equivalent (kg CO2-eq) per person per day

164 At current technology costs, carbon dioxide equivalent emission prices of $142 and $2

165 limate agreement [$40 to $80 (USD) per tonne carbon dioxide equivalent] would provide an economic jus

166 tprint of a single operation ranged 6-814 kg carbon dioxide equivalents.

167 question, we measured evapotranspiration and carbon dioxide exchange over and under an oak savanna an

168 n dioxide reduction performances once a pure carbon dioxide feed is restored, indicating a negligible

169 ence of nitrogen oxides (up to 0.83%) in the carbon dioxide feed leads to a considerable Faradaic eff

170 Global fossil fuel carbon dioxide (FFCO(2)) emissions will be dictated to a

171 The vast majority of biological carbon dioxide fixation relies on the function of ribulo

172 xygenase and carbonic anhydrase that enhance carbon dioxide fixation.

173 ressing genes involved in H(2) oxidation and carbon dioxide fixation.

174 effect of changes in ocean circulation from carbon dioxide forcing on patterns of ocean warming in b

175 l function of delivering oxygen and removing carbon dioxide from all other cells while enduring the s

176 s to limit global climate change by removing carbon dioxide from the atmosphere through the growth of

177 A mechanism for concentrating carbon dioxide has for the first time been successfully

178 The growth of the global terrestrial sink of carbon dioxide has puzzled scientists for decades.

179 The catalytic hydrogenation of carbon dioxide holds immense promise for applications in

180 hydrostatic pressure (HHP) and high pressure carbon dioxide (HPCD) were applied to the processing of

181 methanol reaction and Fischer-Tropsch based carbon dioxide hydrogenation.

182 senting a low value for electro-reduction of carbon dioxide in an organic electrolyte.

183 (CA6) catalyses the reversible hydration of carbon dioxide in saliva with possible pH regulation, ta

184 required to reduce the current high level of carbon dioxide in the atmosphere, which is driving clima

185 jority of organic carbon is respired back to carbon dioxide in the biosphere, but a small fraction es

186 ontrolling both the quantity and location of carbon dioxide in the polymer chain.

187 The B=S compound reacted with carbon dioxide in the presence of the lithium salt Li[B(

188 s using CO(2) and the catalytic reduction of carbon dioxide, including atmospheric CO(2), into methan

189 oximately three times the annual atmospheric carbon dioxide increase by fossil fuel burning.

190 al and often conflicting roles, facilitating carbon dioxide influx into the plant leaf for photosynth

191 players in the global carbon cycle by fixing carbon dioxide into 1 Gt of biomass annually, yet the fa

192 lize the sun's energy to convert atmospheric carbon dioxide into organic carbon, resulting in diurnal

193 ogenic silica, and photosynthetically fixing carbon dioxide into particulate organic carbon, diatoms

194 ate change, the utilisation or conversion of carbon dioxide into sustainable, synthetic hydrocarbons

195 Electrochemical reduction of carbon dioxide is a clean and highly attractive strategy

196 Formate oxidation to carbon dioxide is a key reaction in one-carbon compound

197 Carbon dioxide is an attractive reagent for organic synt

198 As this carbon dioxide is extracted from air, and re-emitted fro

199 ck process, the (14)C isotope of atmospheric carbon dioxide is fixed in the carbonate, and its radioc

200 dioxide and bicarbonate in the cells, where carbon dioxide is produced, and in the lungs, where it i

201 Nitrous oxide (N(2)O), like carbon dioxide, is a long-lived greenhouse gas that accu

202 Unambiguous detection of the clumped carbon dioxide isotopologue (13)C(16)O(18)O with isotope

203 0 years before present, revealing pronounced carbon dioxide jumps (CDJ) under cold and warm climate c

204 ater droplet followed by dehydration using a carbon dioxide laser.

205 Carbon dioxide levels are mildly elevated on the Interna

206 esuscitation, and the targets for oxygen and carbon dioxide levels in pediatric patients after return

207 40 million years(1-5), driven by atmospheric carbon dioxide levels of around 1,000 parts per million

208 nd thus contributed to the lower atmospheric carbon dioxide levels of the ice ages.

209 An analysis that relates arterial carbon dioxide levels with brain's response to this stim

210 romote arousal in response to elevated blood carbon dioxide levels, as seen in sleep apnea [3].

211 ne-co-divinylbenzene) monolithic columns and carbon dioxide/methanol mobile phase.

212 yzed selective electrocatalytic upgrading of carbon dioxide/monoxide to valuable multicarbon oxygenat

213 The electroreduction of carbon dioxide offers a promising avenue to produce valu

214 ging polymer synthesis with the recycling of carbon dioxide offers a tangible route to transition tow

215 ed either by direct reaction of NaPH(2) with carbon dioxide or by hydrolysis of the phosphaethynolate

216 ity of palladium electrodes for reduction of carbon dioxide or dioxygen, but determining how strain a

217 sive exercise test, with an excess pulmonary carbon dioxide output ( VCO2 ).

218 rectly affects atmospheric concentrations of carbon dioxide over a wide range of timescales.

219 Arrest Patients; NCT02541591) and COMACARE (Carbon Dioxide, Oxygen and Mean Arterial Pressure After

220 The model includes transport of carbon dioxide, oxygen, bicarbonate, sucrose/glucose, ba

221 -548 mmHg, and partial pressures of arterial carbon dioxide ( PaCO2 ), which ranged between 34-50 mmH

222 oxygen partial pressure (pO(2)), and a lower carbon dioxide partial pressure (pCO(2)).

223 ges in temperature (28 and 31 degrees C) and carbon dioxide partial pressures (pCO(2); 650 and 1050 u

224 term trends in atmospheric concentrations of carbon dioxide (pCO(2)) has become increasingly relevant

225 e analysis suggests that partial pressure of carbon dioxide (Pco(2)) is the only environmental factor

226 Ma ago, when atmospheric partial pressure of carbon dioxide (pCO(2)) ranged from present-day (>400 pa

227 Because industrial carbon dioxide point sources often contain numerous cont

228 The electrocatalytic reduction of carbon dioxide, powered by renewable electricity, to pro

229 xygen saturation, central venous-to-arterial carbon dioxide pressure difference, and oxygen extractio

230 ar catalysts showed good performances at low carbon dioxide pressures, attributed to synergic interac

231 hropogenic "N problem" is distinct from the "carbon dioxide problem" in being more local and less glo

232 This technique relies on the release of carbon dioxide produced in situ during a neutralization

233 = 0.007), and higher minute ventilation (VE)/carbon dioxide production (VCO2) (34 +/- 5 versus 32 +/-

234 oup difference in mean change in ventilation/carbon dioxide production slope was -0.3 (95% CI, -1.6 t

235 e and in ventilatory efficiency (ventilation/carbon dioxide production slope).

236 There were parallel reductions in carbon dioxide production, but of lesser magnitude, yiel

237 ence of the "natural refrigerants" (ammonia, carbon dioxide, propane, and isobutane).

238 Here, we present a high-resolution carbon dioxide record from 330,000 to 450,000 years befo

239 ty and carbon burial facilitated atmospheric carbon dioxide reduction contributing to the expansion o

240 ciency, the electrocatalysts exhibit similar carbon dioxide reduction performances once a pure carbon

241 The electrochemical carbon dioxide reduction reaction (CO(2) RR) to produce

242 desirable products such as ethylene from the carbon dioxide reduction reaction (CO(2)RR) remains a ch

243 The carbon dioxide reduction reaction (CO(2)RR), in particul

244 s superior electrocatalytic activity for the carbon dioxide reduction reaction over their fcc counter

245 Electrochemical processes coupling carbon dioxide reduction reactions with organic oxidatio

246 framework was developed for electrocatalytic carbon dioxide reduction to carbon monoxide in aqueous s

247 Pulse-like carbon dioxide release to the atmosphere on centennial t

248 ed rock weathering (ERW) is a biogeochemical carbon dioxide removal (CDR) strategy aiming to accelera

249 ease relies on the large-scale deployment of carbon dioxide removal (CDR) technologies.

250 es to date, use of venovenous extracorporeal carbon dioxide removal in patients with status asthmatic

251 in select patients receiving extracorporeal carbon dioxide removal is safe and feasible and avoids t

252 Venovenous extracorporeal carbon dioxide removal may be lifesaving in the setting

253 Extracorporeal carbon dioxide removal settings, including blood flow an

254 ve mechanical ventilation and extracorporeal carbon dioxide removal support, and complications during

255 lly extubated while receiving extracorporeal carbon dioxide removal support; none required reintubati

256 Following the initiation of extracorporeal carbon dioxide removal, blood gas values were significan

257 ort, and complications during extracorporeal carbon dioxide removal.

258 24 hours after initiation of extracorporeal carbon dioxide removal.

259 24 hours after initiation of extracorporeal carbon dioxide removal.

260 We successfully used supercritical carbon dioxide (Sc-CO(2)) technology for manufacturing a

261 A combination of supercritical carbon dioxide (scCO(2)) impregnation of pyrrole and son

262 olution-enhanced dispersion by supercritical carbon dioxide (SEDS) and spray drying (SD) were used to

263 eworks (ZIFs), is of particular interest for carbon dioxide sequestration.

264 In this study supercritical carbon dioxide (SFE-CO(2)) and pressurized liquid (PLE)

265 cts of interaction among Pt(-), methane, and carbon dioxide shows that the methane activation complex

266 Here we show that these materials have a carbon dioxide storage potential of 2.9-8.5 billion tonn

267 A statistical model including carbon dioxide, temperature, drought and forest dynamics

268 Reductions in arterial carbon dioxide tension (> 20 mm Hg) from the initiation

269 low levels of oxygen, the way the prevailing carbon dioxide tension (Pa(CO(2))) blunts the brain's re

270 the association between the initial arterial carbon dioxide tension and change over 24 hours on morta

271 nation, 4,918 of these patients had arterial carbon dioxide tension data available at 24 hours on sup

272 The manipulation of arterial carbon dioxide tension is associated with differential m

273 eased mortality was observed with a arterial carbon dioxide tension less than 30 mm Hg (odds ratio, 1

274 Large reductions (> 20 mm Hg) in arterial carbon dioxide tension over 24 hours were associated wit

275 A U-shaped relationship between arterial carbon dioxide tension tension at extracorporeal membran

276 Initial arterial carbon dioxide tension tension was independently associa

277 = 0.04), independent of the initial arterial carbon dioxide tension.

278 -century warming, and rely on net removal of carbon dioxide thereafter to undo their initial shortfal

279 lowed the ocean to absorb massive amounts of carbon dioxide, thus limiting the global warming otherwi

280 remarkable onset potential for reduction of carbon dioxide to formic acid at -1.45 V vs. Ag/Ag(+), r

281 d Horner P(=O)CH(2)B carbon nucleophile with carbon dioxide to give a bicyclic product by P-CH(2) att

282 Transformation of carbon dioxide to high value-added chemicals becomes a s

283 epsilon-decalactone, cyclohexene oxide, and carbon dioxide to make a series of poly(cyclohexene carb

284 )O/Cu(111) catalyst from carbon monoxide and carbon dioxide to methanol under a reaction environment

285 gineered cyanobacteria for the conversion of carbon dioxide to useful chemicals via light-driven, end

286 aterials in the electrochemical reduction of carbon dioxide to value-added products has the potential

287 of sucrose containing pockets of pressurized carbon dioxide, to study rock fractures.

288 bserve how the Earth system responds to high carbon dioxide, underlining a fundamental role for paleo

289 ding yields (turnover numbers), quantitative carbon dioxide uptake (>99%), and high selectivity for p

290 t for both forest production and atmospheric carbon dioxide uptake.

291 An ultrasound-assisted supercritical carbon dioxide (USC-CO(2)) procedure was developed for t

292 ossil crude oil, the fuels are produced from carbon dioxide using sustainable renewable hydrogen and

293 athway could scale to over 0.5 gigatonnes of carbon dioxide utilization annually.

294 cy (minute ventilation required to eliminate carbon dioxide, VE/VCO2) during exercise potently predic

295 Thermal treatment of solid methane and carbon dioxide-water mixture in ultrahigh vacuum of the

296 s, particularly in atmospheric monitoring of carbon dioxide, where understanding the adsorption effec

297 and sensitive to CH(4), hydrogen (H(2)), and carbon dioxide with a large dynamic range from trace lev

298 anates, carbodiimides, carbon disulfide, and carbon dioxide with carbanions or enamines (reference nu

299 We present a new adduct of carbon dioxide with dihydrogenphosphide, that may be pre

300 ligand become available for the reduction of carbon dioxide with selective formation of carbonate.