ライフサイエンスコーパス: CO

1 CO(2) and CH(4) were younger than dissolved and particul

2 CO(2) demand in the facility was driven predominantly by

3 CO(2) emissions were consistent across ecosystem types a

4 CO(2) fixation in cereals crops like bread wheat (Tritic

5 CO(2) is converted into biomass almost solely by the enz

6 CO-RADS assesses the suspicion for pulmonary involvement

7 minimum energy consumption of 164 kJ.mol(-1) CO(2) could be achieved.

8 into cylindrical samples and exposed to 100% CO(2) gas at 50% RH for 24 h, during which they cemented

9 ic and water potential, and transfer of (13) CO(2) through EM to explore mechanisms linking stored NS

10 ese proteins phase separate, we compared (13)CO-detect versus (1)H(alpha)-detect experiments, showing

11 on and decomposition of P12(1) /c1-type K(2) CO(3) at the efficient carbon-based catalyst.

12 ar-driven photocatalytic reduction of CO(2) (CO(2) RR) into chemical fuels is a promising route to en

13 e electrode can still produce CO at an O(2) /CO(2) ratio as high as 9:1.

14 l bromides and arylhydrazines employing Cs(2)CO(3) as the base and t-Bu(3)PHBF(4) as the ligand in DM

15 icate (urban) samples indicate that the Na(2)CO(3) solution is significantly less selective for HNO(3

16 ure water, 90 degrees C-water, CDTA and Na(2)CO(3).

17 Well-defined solid sources of NH(4)Pu(V)O(2)CO(3)(s) were placed in two 5-L lysimeters containing NO

18 ctrochemical characterization of [Co(13)C(2)(CO)(24)](4-) in the presence and absence of protons reve

19 H, concurrently producing a high-purity O(2)/CO(2) gas mixture (1:2 molar ratio at stoichiometric ope

20 tures were incubated at 37 degrees C in a 5% CO(2) environment and at days 7 and 14, the specimens we

21 Many photosynthetic organisms employ a CO(2) concentrating mechanism (CCM) to increase the rate

22 the differential conductance imaging with a CO functionalized tip.

23 known as the pyrenoid, in association with a CO(2)-concentrating mechanism that improves photosynthet

24 rters (e.g. Na-H exchangers) by accelerating CO(2) / HCO3- -mediated buffering of acid-base equivalen

25 s, thus enhancing the release of accumulated CO(2) to the atmosphere.

26 y applying this design strategy, we achieved CO(2) electroreduction on copper in 7 M potassium hydrox

27 The additional CO(2) originated from heterotrophic rather than autotrop

28 The residual bridge-adsorbed CO (CO(bridge)) is formed on the as-prepared Cu surface

29 th distilled water or MgSO(4) did not affect CO(2) /H(2) O gas exchange or stomatal conductance signi

30 a hybrid, precious-metal-free coupled AlcOx-CO(2) R electrolyzer.

31 ising technology to simultaneously alleviate CO(2) -caused climate hazards and ever-increasing energy

32 that relatively low temperature and ambient CO(2) exacerbated damage induced by nanoplastics, while

33 pring and an adjacent control site (ambient [CO(2) ]) were grown in a common environment for one gene

34 e in the Wood-Ljungdahl pathway of anaerobic CO and CO(2) fixation.

35 arch on Cu-based catalysts for the CO(2) and CO reduction reactions, surface speciation of the variou

36 e dehydrogenation of formic acid to H(2) and CO(2) .

37 demonstrated by high photosynthetic O(2) and CO(2) fluxes and effective yields of PSI and PSII.

38 -65 adsorbed a large amount of C(2) H(2) and CO(2) through gate-opening and only negligible amount of

39 f species with similar sizes (CO(2)/N(2) and CO(2)/CH(4)), via precise mechanical control of the pore

40 hod of controlling both CO(2) adsorption and CO desorption over supported metal catalysts by employin

41 In bulk electrolyte, alkalinity and CO(2) concentration are inversely correlated to each oth

42 e Wood-Ljungdahl pathway of anaerobic CO and CO(2) fixation.

43 ange of C-based substrates, including CO and CO(2), is also discussed, and remaining challenges in un

44 only carbon-containing products were DME and CO(2) .

45 ly monitored soil temperature, moisture, and CO(2) for a three-year period (2015-2017), encompassing

46 n species diversity under simultaneous N and CO(2) enrichment was associated with greater community b

47 strate simultaneous solvent regeneration and CO(2) desorption in a continuous system using a H(2)-rec

48 mong these gaseous molecules, NO, H(2)S, and CO occupy a special place because of their widely known

49 re responsible for the largest anthropogenic CO(2) emissions and are key to effective emission reduct

50 strial biosphere in mitigating anthropogenic CO(2) emissions.

51 ither stored or emitted to the atmosphere as CO(2).

52 he application of chitosan nanoaggregates as CO(2) responsive emulsifier, used to promote the swellin

53 f explosive reagents or toxic gases, such as CO, as the C1 synthon.

54 till persist, albeit to a reduced extent, at CO(2) reduction current densities up to 150 mA/cm(2).

55 was, thus, a response to coeval atmospheric CO(2) decline and continental-scale Antarctic glaciation

56 Elevated atmospheric CO(2) (eCO(2) ) generally increases carbon input in rice

57 d its interactions with elevated atmospheric CO(2), eutrophication, and plant community composition o

58 of an annual source or sink for atmospheric CO(2).

59 t (440 ppm) and projected future atmospheric CO(2) concentrations (800 ppm).

60 with periods of decreased global atmospheric CO(2) concentration during the LGM, confirming the concl

61 ion of carbon dioxide, including atmospheric CO(2), into methanol, under ambient conditions.

62 ce of terrestrial carbon flux on atmospheric CO(2) concentrations (DeltaCO(2) ) is estimated from the

63 use efficiency that track rising atmospheric CO(2) .

64 Rising atmospheric CO(2) is intensifying climate change but it is also driv

65 emissions estimation through the atmospheric CO(2) inversion process.

66 shifted to the night period when atmospheric CO(2) is fixed by phosphoenolpyruvate carboxylase and st

67 t loading (0.025 mol %, 70 degrees C, 30 bar CO(2)).

68 odynamics of biochemical conversions because CO(2) is an intermediate and end-product of the digestio

69 proposed as an alternative precursor because CO can easily desorb under electron exposure.

70 e chosen from the SCS approach, and biogenic CO(2) in biorefineries is captured, transported by pipel

71 The biogenic CO(2) is composed of sources such as biofuel combustion

72 demonstrate a new method of controlling both CO(2) adsorption and CO desorption over supported metal

73 data from experiments that manipulated both CO(2) and P for young individuals of woody and non-woody

74 n betaCA3-mediated basal immunity under both CO(2) conditions.

75 O(2) to chemical feedstocks, which uses both CO(2) and renewable energy(3-8).

76 Robust estimates of CO(2) budget, CO(2) exchanged between the atmosphere and terrestrial b

77 s methanol activation on ReO(4), followed by CO insertion into the terminal methyl species.

78 asal ABA signaling in stomatal regulation by CO(2) and, as hypothesized here, vapor-pressure deficit.

79 2% (n = 10, decay-corrected) based on [(11)C]CO(2) with a radiochemical purity of >98% and molar acti

80 ne and the long-term storage of the captured CO(2).

81 tert-butylphosphinito)phenyl) that catalyzes CO(2) hydrogenation to formate with faster rates at lowe

82 interaction of gas reactants and catalyzing CO oxidation.

83 ty-onset healthcare facility-associated CDI (CO-HCFA-CDI), incidence of vancomycin-resistant Enteroco

84 es, providing advective fingerprints of city CO(2) emissions.

85 The residual bridge-adsorbed CO (CO(bridge)) is formed on the as-prepared Cu surface with

86 nd leakiness ( ), the amount of concentrated CO(2) that escapes the bundle-sheath cells, for the chil

87 In meiosis, crossover (CO) formation between homologous chromosomes is essentia

88 Areas of diffuse CO(2) degassing exhibit increasing mantle CO(2) flux and

89 n CO(2)RR and also make direct use of dilute CO(2) feedstocks.

90 consequence of anthropogenic carbon dioxide (CO(2) ) emissions, strongly impacts marine ecosystems.

91 Autotrophic carbon dioxide (CO(2) ) fixation by microbes is ubiquitous in the enviro

92 tions to investigate the net carbon dioxide (CO(2) ) seasonal cycle and its climatic and environmenta

93 offset summer photosynthetic carbon dioxide (CO(2) ) uptake.

94 increased concentrations of carbon dioxide (CO(2)) [i.e., the CO(2) fertilization effect (CFE)] sust

95 important sources of mantle carbon dioxide (CO(2)) emission into Earth's atmosphere(1-3).

96 net H(2) oxidation and dark carbon dioxide (CO(2)) fixation than those from the carbonate catchment,

97 ng potential 86-125x that of carbon dioxide (CO(2)) over a twenty-year period, is the main component

98 ls of 0.5 to 2 gigatonnes of carbon dioxide (CO(2)) per year with extraction costs of approximately U

99 f several pollutants such as carbon dioxide (CO(2)), tropospheric ozone (O(3)), and particulate matte

100 mand and the need to replace carbon dioxide (CO(2))-emitting fossil fuels with renewable sources have

101 e factors (warming, elevated carbon dioxide [CO(2) ], increased precipitation, increased drought, inc

102 For example, during CO(2) reduction, production of CO often requires balanci

103 that a synchronous movement can occur during CO-CO collisions, whereby a bump is followed by a move s

104 Additionally, using the product itself (i.e. CO) as the local pH probe allows us to investigate CO(2)

105 ays to elevate local CO(2) concentrations (e[CO(2) ]) by +150 umol/mol.

106 RS-CoV-2 PCR, and likelihood ratios for each CO-RADS score were used for rational selection of diagno

107 Electrocatalytic CO(2) reduction (ECR) is a promising technology to simul

108 Electrochemical CO[Formula: see text] reduction is a potential route to

109 activity and selectivity for electrochemical CO(2) reduction (CO(2)R) to CO.

110 efficiency of up to 95% for electrochemical CO(2) reduction to CO.

111 ork together to enable rapid electrochemical CO(2) reduction at moderate overpotential.

112 In this study, the electrochemical CO(2) reduction mechanism over the Cu catalysts with var

113 ytic performance for CO(2) electroreduction (CO(2) R) to CO; this activity has often been attributed

114 as stimulated by warming (+152.7%), elevated CO(2) (+19.6%), and increased precipitation (+73.1%) but

115 In addition, elevated CO(2) decreased foliar Bt protein content at 1 N level.

116 hlorococcus strain in co-culture at elevated CO(2) .

117 pressure bioreactors will result in elevated CO(2) partial pressure (pCO(2)).

118 Understanding the impact of elevated CO(2) (eCO(2) ) in global agriculture is important given

119 igated plant-mediated influences of elevated CO(2) (eCO(2) ) on endogenous immune responses of monarc

120 mage induced by nanoplastics, while elevated CO(2) and warmer temperatures reflecting climate change

121 offspring were grown in ambient or elevated [CO(2) ] growth chambers.

122 at plant methylomes may respond to elevated [CO(2) ] over multiple generations.

123 Excess CO(2) and limited H(2) in the feedstock gas is not favor

124 mic advantages of this approach for favoring CO(2) reduction at mild potentials, along with guideline

125 d the Lewis adduct [{(NHC)C(Ph)}P(IMe(4))]Fe(CO)(4) (5) [IMe(4) = C(NMeCMe)(2)].

126 The direct coupled, vapor-fed CO(2)R cell yields a total Faradaic efficiency of up to

127 sus N(2) uptake at 298 K, except the 19-fold CO(2) uptake for CTH-12 containing Cu(II) dinuclear padd

128 revealed a faradaic selectivity of 36 % for CO in 0.1 M KHCO(3) at -1.1 V vs. RHE, similar to that o

129 the scene for a host of new applications for CO(2)-derived polymers.

130 eed to have been lower-closer to 0.6 bar-for CO(2) to have oxidized the micrometeorites.

131 2) in the feedstock gas is not favorable for CO(2) hydrogenation to methanol, causing low activity an

132 ve shown promising catalytic performance for CO(2) electroreduction (CO(2) R) to CO; this activity ha

133 ) (-1) h(-1) with near-unity selectivity for CO generation and meanwhile excellent stability.

134 In(delta+) -N(4) atomic interface sites for CO(2) electroreduction to formate with high efficiency.

135 col provides a sustainable, indirect way for CO(2) methanation as the process can be repeated multipl

136 vation of CO(2) and the C-O coupling to form CO are low energy steps.

137 he best performances reported for metal-free CO(2) reduction electrocatalysts.

138 modeling, targeting methanol formation from CO(2)/H(2) feeds at 170 degrees C and 1-8 bar pressure.

139 ng of fluid transport pathways in rocks from CO(2)-induced salt precipitation reduces injectivity and

140 solved, sectorally disaggregated fossil fuel CO(2) (FFCO(2)) emission data products.

141 over removal (17.6 +/- 2.8 vs 18.8 +/- 3.0 g CO(2)e MJ(-1)), but were notably lower under sorghum for

142 study region (13.6 +/- 3.0 vs 22.5 +/- 3.1 g CO(2)e MJ(-1)).

143 or ethanol vehicles ranged from 20 to -179 g CO(2)e MJ(-1): maize stover >> miscanthus ~ switchgrass

144 ed more than respiration, leading to greater CO(2) uptake.

145 could result in delayed reductions in gross CO(2) emissions, with consequent high risk of overshooti

146 s the longest continuous northern hemisphere CO(2) record, shows an increasing SCA before the 1980s (

147 evel of agreement for global and hemispheric CO(2) budgets in the 2000s.

148 termediate trapped in a crystal of the hIDO1-CO-Trp complex, where CO is photolyzed from the heme iro

149 g the highest for known MIECs, but also high CO(2) tolerance.

150 The role of betaCA3 in the high CO(2) -mediated response in tomato and two other Solanac

151 on PdH/NbN are critical to achieving higher CO(2) RR activity.

152 s compared with regions with somewhat higher CO rates [4].

153 ther) is required to selectively hydrogenate CO(2) to methanol on catalysts containing Cu and ZrO(2).

154 tainty in future fuel prices, a hypothetical CO(2) cap, and an extended renewable portfolio standard.

155 alcove in forming and stabilizing the Ni(I)-CO intermediate in the Wood-Ljungdahl pathway of anaerob

156 Structural equation modeling identified CO(2) as the dominant limitation on J(CO2) on the clay s

157 sidual ~15% are consistent with the class II CO pathway.

158 technology, whereas fundamental advances in CO(2) electrolysis are still needed to enable short-term

159 thin film Ag cathode on a Ge ATR crystal in CO(2)-saturated 0.1 M KHCO(3) over a range of potentials

160 catalyst concentrations, and zeroth order in CO(2) pressure.

161 ane with high FE and high conversion rate in CO(2)RR and also make direct use of dilute CO(2) feedsto

162 er) to 290% (restored prairie) reductions in CO(2)e compared to petroleum and were similar for electr

163 man actions are causing concurrent shifts in CO(2) , temperature, precipitation regimes and nitrogen

164 hydrogenation is one of the major topics in CO(2) conversion into value-added liquid fuels and chemi

165 zed by reaction with electrophiles including CO(2) and aldehydes, whereas CF(3) radical addition furn

166 teracting environmental stressors, including CO(2), temperature, light, and nanoplastics.

167 wide range of C-based substrates, including CO and CO(2), is also discussed, and remaining challenge

168 iably, but overall positively, to increasing CO(2) concentrations, generating negative feedbacks to c

169 constrained by elemental budgets, indicated CO(2) sequestration rates of 2-4 t CO(2) /ha, 1-5 years

170 niform increases in leaf-level intercellular CO(2) and intrinsic water use efficiency that track risi

171 the local pH probe allows us to investigate CO(2) RR without the interference of additional probe mo

172 intensity from 2.4 +/- 0.1 to 1.6 +/- 0.1 kg CO(2) eq per kg milk, FeCo reduced it to 2.2 +/- 0.1, wh

173 hereas FoFeCo increased it to 2.7 +/- 0.2 kg CO(2) eq per kg milk because of land use change emission

174 (p)(I) (g( ) > g(||) ~ 2) surprisingly lacks CO.

175 ion describes the transient increase in leaf CO(2) uptake with an increase in light.

176 s of three treatment arrays to elevate local CO(2) concentrations (e[CO(2) ]) by +150 umol/mol.

177 In this relatively low CO(2) Oligocene world (~300 to 700 ppm), warm climates s

178 cement kiln to improve efficiency and lower CO(2) emissions, or the output gases may be used for oth

179 ry calculations herein reveal that lowering *CO(2) coverage on the Cu surface decreases the coverage

180 ulations, the skew was reduced in the lowest CO regions compared with regions with somewhat higher CO

181 se CO(2) degassing exhibit increasing mantle CO(2) flux and (3)He/(4)He ratios as the rift transition

182 sect taken from a naturally occurring marine CO(2) seep in Levante Bay of the Aeolian island of Vulca

183 route to enrich energy supplies and mitigate CO(2) emissions.

184 exploit the thermolytic decomposition of Mo(CO)(6) in the presence of a surface-stabilizing ligand a

185 compounds show normal (10-fold higher) molar CO(2) versus N(2) uptake at 298 K, except the 19-fold CO

186 ive detection of endogenous carbon monoxide (CO) in live mammalian cells under normoxic and hypoxic c

187 Carbon monoxide (CO) is a cell-signaling molecule (gasotransmitter) produ

188 Marine microalgae sequester as much CO(2) into carbohydrates as terrestrial plants.

189 ecursors such as NHC(H)[HCO(3)] salts or NHC-CO(2) adducts.

190 explained by changes in metabolic rate, nor CO(2) , and there were no changes in the HVR in normoxic

191 nd MSH5 (MutSgamma) to maintain the obligate CO/chiasma and accounts for ~85% of meiotic COs, whereas

192 tes of this flux, derived from surface ocean CO(2) concentrations, have not corrected the data for te

193 (2) catalyst was explained by the ability of CO(2) to partially oxidize the carbon deposit over the s

194 rate-limiting step, while the activation of CO(2) and the C-O coupling to form CO are low energy ste

195 light harvesting and chemical adsorption of CO(2) molecules dramatically, achieving 103.21 mmol g(ca

196 reactant and product states: weak binding of CO is desirable from a selectivity perspective, but weak

197 selectivity perspective, but weak binding of CO(2) leads to low activity.

198 CAs catalyze the conversion of CO(2) to bicarbonate and protons and are involved in var

199 This work shows that efficient conversion of CO(2) to C(2+) products requires a Cu catalyst with a hi

200 aCO(2) ) is estimated from the difference of CO(2) concentrations that were influenced by the land se

201 hyll conductance (g(m) ) is the diffusion of CO(2) from intercellular air spaces (IAS) to the first s

202 e investigate how the Faradaic efficiency of CO formation is affected by the CO(2) partial pressure (

203 The adsorption and electrooxidation of CO molecules at well-defined Pt(hkl) single-crystal elec

204 During obstructive sleep apnea, elevation of CO(2) during apneas contributes to awakening and restori

205 a's future power sector related emissions of CO(2).

206 Robust estimates of CO(2) budget, CO(2) exchanged between the atmosphere and

207 he key fundamental questions in the field of CO(2) electroreduction.

208 ble data on the atmospheric mole fraction of CO(2), measured from six sites across China during 2009

209 the much-publicized environmental impact of CO(2) emission by air traffic, aviation particulate emis

210 The loss of CO from the precursor during electron-induced decomposit

211 e@p-G(2) BDS (y,z=variable) when pressure of CO(2) or Xe, respectively, is applied.

212 ample, during CO(2) reduction, production of CO often requires balancing a trade-off between the adso

213 ting mechanism (CCM) to increase the rate of CO(2) fixation via the Calvin cycle.

214 f g(m) for accurately modelling net rates of CO(2) assimilation, (ii) on how leaf biochemical and ana

215 The solar-driven photocatalytic reduction of CO(2) (CO(2) RR) into chemical fuels is a promising rout

216 tractive is the electrochemical reduction of CO(2) to chemical feedstocks, which uses both CO(2) and

217 t-in-moisture content, whereas solubility of CO(2) increased with increasing pH.

218 sence and absence of saturating solutions of CO (160 mum) and nitric oxide (100 mum).

219 ements of ships are a considerable source of CO(2) emissions and contribute to climate change.

220 osts of approximately US$80-180 per tonne of CO(2).

221 d significant flight-to-flight variations of CO(2) enhancements downwind of neighboring cities, provi

222 te, and then this favors the protonation of *CO to *CHO, a key intermediate for methane generation, c

223 lable supported Pd catalysts, producing only CO and H(2)O as waste.

224 nt to within 1.1% for total fuel consumed or CO(2) emitted.

225 Along this line, we have developed organic CO prodrugs that allow for packing this gaseous molecule

226 Medications to Enhance Depression Outcomes (CO-MED, n = 665), Establishing Moderators and Biosignatu

227 spiration of available C, greater overwinter CO(2) efflux and greater nutrient availability to plants

228 variance method; during this 19-year period, CO(2) rose 40 ppm, air temperature increased by 1 degree

229 ecosystem production by 8.3% (NEP, 22.25 Pg CO(2) /year) under warming.

230 in soil CH(4) and N(2) O emissions (1.84 Pg CO(2) -equivalent/year) could reduce mitigation potentia

231 nsive mechanistic study of the photochemical CO release from 3-hydroxy-2-phenyl-4H-chromen-4-one, a p

232 productivity and any gain in photosynthetic CO(2) assimilation per unit of leaf area (A) has the pot

233 ivated the same way by the local pressurized CO(2) microenvironment.

234 The electrode can still produce CO at an O(2) /CO(2) ratio as high as 9:1.

235 composite sorbent were carried out with pure CO(2) in a sealed pressure drop apparatus.

236 incer-ligated rhenium complex ((tBu)POCOP)Re(CO)(2) ((tBu)POCOP = 2,6-bis(di-tert-butylphosphinito)ph

237 dride is not sufficiently hydritic to reduce CO(2) to formate, unless the apparent hydricity, which e

238 ctivity for electrochemical CO(2) reduction (CO(2)R) to CO.

239 and yield more robust knowledge of regional CO(2) budgets.

240 and show that the position of the resulting CO directly affects the formation of distinct chromosome

241 ider than originally predicted given revised CO(2) limits and (for the first time) N(2) respiration l

242 thin condensed layers of (eta(3)-C(3)H(5))Ru(CO)(3)Cl.

243 Recently, (eta(3)-C(3)H(5))Ru(CO)(3)X (X = Cl, Br) has been proposed as an alternative

244 iety) cake and defatted hemp seed cake by SC-CO(2) was carried out using Flavorpro 750 MDP and Promod

245 elevated (700 ppm, based on RCP4.5 scenario) CO(2) levels.

246 SFE-CO(2) at optimized parameters yielded 11.8 g/100 g of li

247 mace by consecutive supercritical CO(2) (SFE-CO(2)), pressurized liquid (PLE) and enzyme assisted (EA

248 ng separation of species with similar sizes (CO(2)/N(2) and CO(2)/CH(4)), via precise mechanical cont

249 We measured daily soil CO(2) emission for the first two weeks and every other d

250 rt in yielding the observed patterns of soil CO(2) efflux being out of sync with soil temperature.

251 he contribution of canopy vegetation to soil CO(2) fluxes and belowground productivity.

252 tionally verified by the synthesis of stable CO and 2,6-xylylisocyanide (XylNC) adducts of 1, which d

253 uple ABA receptor mutants show that stomatal CO(2) signaling requires basal ABA and SnRK2 signaling,

254 lled positions in the modifying film, strong CO(2) adsorption and hydrogenation reactivity could be r

255 ation and can offset up to 41% of the summer CO(2) uptake.

256 gonberry pomace by consecutive supercritical CO(2) (SFE-CO(2)), pressurized liquid (PLE) and enzyme a

257 indicated CO(2) sequestration rates of 2-4 t CO(2) /ha, 1-5 years after a single application of basal

258 For annual plants, higher temperatures, CO(2) and drought stress increase foliar herbivory.

259 lted in cumulative emissions of 0.06-0.14 Tg CO(2-eq) over the last 40 years in Cockburn Sound.

260 This composition suggested that CO production takes place in two consecutive reactions.

261 ntrol site towards the seep, suggesting that CO(2) exerts a strong control on isotopic fractionation

262 This challenges the view that CO(2) fertilization is the dominant cause of emergent SC

263 The CO(2) solubility of samples decreased linearly with both

264 The CO(2)-OH(-) neutralization reaction and the pH gradient

265 Seed from populations at the CO(2) spring and an adjacent control site (ambient [CO(2

266 in the carbonated products was offset by the CO(2) mineralised (i.e. samples were 'carbon negative',

267 fficiency of CO formation is affected by the CO(2) partial pressure (0.1-0.5 bar) and the proton conc

268 rsely correlated to each other as set by the CO(2)/bicarbonate equilibrium.

269 rations of carbon dioxide (CO(2)) [i.e., the CO(2) fertilization effect (CFE)] sustains an important

270 RR conditions, which greatly facilitates the CO(2) to methane conversion.

271 ecent research on Cu-based catalysts for the CO(2) and CO reduction reactions, surface speciation of

272 As a result, we improve the CO selectivity from 74% for Ag/Zr-fcu-MOF-1,4-benzenedic

273 of properties, a remarkable increase in the CO(2) uptake is observed that reaches 76.6% and 61.6% at

274 We found excess differentiation in the CO(2) vent population for genes central to calcification

275 ndothelial Galpha(q/11) proteins mediate the CO(2)/H(+) effect on cerebrovascular reactivity in mice.

276 in P1, P2 and P3 fragments regardless of the CO(2) or N-fertilizer level.

277 of N(2), like today, the lower limit on the CO(2) mixing ratio is ~0.23.

278 recise spatial and temporal control over the CO release.

279 he Cu surface decreases the coverage of the *CO intermediate, and then this favors the protonation of

280 geneous methanol synthesis catalysts through CO(2) hydrogenation is one of the major topics in CO(2)

281 h simultaneous ligand exchange from Cl(-) to CO.

282 from problematic operation stability due to CO poisoning on surface.

283 electrochemical CO(2) reduction (CO(2)R) to CO.

284 ance for CO(2) electroreduction (CO(2) R) to CO; this activity has often been attributed to the prese

285 o 95% for electrochemical CO(2) reduction to CO.

286 ure of 230 degrees C and 100% selectivity to CO(2).

287 NEE is the difference between the total CO(2) release due to all respiration processes (RECO), a

288 bonds show a distinguished reactivity toward CO(2), depending on the reaction conditions.

289 itigation strategies that rely on ubiquitous CO(2) fertilization as a driver of increased carbon sink

290 USC-CO(2) uses a shorter extraction time (1.83-2.09 times) a

291 l-free catalytic formylation of amides using CO(2) and the catalytic reduction of carbon dioxide, inc

292 increasing energy demands, as it can utilize CO(2) in the atmosphere to provide the required feedstoc

293 We evaluated the impact of varying [CO(2) ], temperature and rainfall conditions on maize yi

294 impacts of agriculture on food-energy-water-CO(2) nexus in other parts of the world to achieve globa

295 show that the stabilized *HOCO and weakened *CO intermediates on PdH/NbN are critical to achieving hi

296 a crystal of the hIDO1-CO-Trp complex, where CO is photolyzed from the heme iron by X-rays at cryogen

297 produces concentrated gas streams from which CO(2) may be readily separated and sequestered, H(2) and

298 While CO, [Formula: see text], HCO, and [Formula: see text] ar

299 light alkanes in shale gas by reacting with CO(2) to produce aldehydes and alcohols.

300 Cu on the catalyst surface under the working CO(2)RR conditions, which greatly facilitates the CO(2)