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1 arboxylic group and the liberation of carbon dioxide.
2 hrough uptake and storage of heat and carbon dioxide.
3 upwelling, each affecting atmospheric carbon dioxide.
4 ransport oxygen to tissues and remove carbon dioxide.
5 ctroreduction of nitrogen oxides over carbon dioxide.
6 dback on the atmospheric inventory of carbon dioxide.
7  for long-term exposure to UFPs and nitrogen dioxide.
8 bedo under high levels of atmospheric carbon dioxide.
9 olymerizations of other epoxides with carbon dioxide.
10 xpanding anoxic zones and atmospheric carbon dioxide.
11 gative potential required to activate carbon dioxide.
12 ere, in longevity, as aerial carbon - carbon dioxide.
13 rom oxidizing methane via methanol to carbon dioxide.
14 ecies, reactive nitrogen species, and sulfur dioxide.
15 ssions and capture excess atmospheric carbon dioxide(1,2).
16                      The antioxidants sulfur dioxide (50 ppm) and ascorbic acid (100 ppm) were added
17 obliquity-induced lag, in turn, makes carbon dioxide a delayed climate amplifier in the late Pleistoc
18                                Rising carbon dioxide, acclimation, adaptation, and migration can infl
19       Large point source emissions of sulfur dioxide accounted for 6.685 [95% confidence interval (CI
20 ct alone acted as catalytic sites for carbon dioxide activation and hydrogen dissociation and their c
21 extended electrochemical window, high carbon dioxide activity, significantly reduced evaporative loss
22    ML predictions for the methane and carbon dioxide adsorption capacities of several tens of thousan
23 re model identified particulate and nitrogen dioxide air pollution inside the home, urine cotinine le
24 inflammation within the population [Nitrogen Dioxide | American Lung Association].
25 cted net effect of rising atmospheric carbon dioxide and air temperature(7-9).
26  role is the rapid interconversion of carbon dioxide and bicarbonate in the cells, where carbon dioxi
27 composites with different ratios of titanium dioxide and bismuth vanadate [TiO(2)]/[BiVO(4)] give ris
28 on and polycarbonate selectivity) for carbon dioxide and cyclohexene oxide copolymerization.
29                                       Carbon dioxide and epoxide copolymerization is an industrially
30  product of aqueous reactions between sulfur dioxide and formaldehyde.
31 p historical decreases in atmospheric carbon dioxide and global temperatures.
32  ketones/styryl methyl ketones with selenium dioxide and malononitrile to afford a series of alpha-ca
33 ure) from two global warming gases of carbon dioxide and methane via dry reforming is environmentally
34 stable isotope signatures of methane, carbon dioxide and nitrate and monitored microbial community co
35  in the global balance of atmospheric carbon dioxide and oxygen.
36 ses ethyl carbamate, biogenic amines, sulfur dioxide and proteins used as technological ingredients s
37 e aboveground surface area to collect carbon dioxide and sunlight and a large underground surface are
38 ced the leakage of deeply sequestered carbon dioxide and thus contributed to the lower atmospheric ca
39                                  Free sulfur dioxide and volatile acidity are parameters related to t
40 ing decarboxylation and conversion to carbon dioxide and water.
41 arine air, related to the presence of sulfur dioxide and/or organic precursors in ship emissions.
42 er-ocean warming, increased dissolved carbon dioxide, and acidification will affect the distribution
43 y between Hb (hemoglobin) and oxygen, carbon dioxide, and nitric oxide-the three-gas respiratory cycl
44 gen oxides, including nitric oxide, nitrogen dioxide, and nitrous oxide, on carbon dioxide electrored
45 he trioxidocarbonate radical anion, nitrogen dioxide, and the glutathionyl radical, via one-electron
46 enation of isocoumarines, benzothiophene 1,1-dioxides, and ketones.
47      In this process, many bubbles of carbon dioxide are instantly formed in the sample matrix.
48 ry have largely employed commercial titanium dioxide as a proxy for its photochemically active fracti
49 ls and chemicals using greenhouse gas carbon dioxide as the carbon feedstock.
50 ketones/styryl methyl ketones using selenium dioxide as the selenating agent under simple reaction co
51 ion of Stattic (6-nitrobenzo[b]thiophene-1,1-dioxide) as a "specific" STAT3 inhibitor that is often u
52                                       Carbon dioxide at high flow rates (up to 4.0 mL/min) is deliver
53  mineral carbonates only decompose to carbon dioxide at temperatures above 700 degrees C.
54 t)-can explain the lag of atmospheric carbon dioxide behind climate during glacial inception and degl
55 f 2H-benzo[e][1,2,4]thiadiazin-3(4H)-one-1,1-dioxides (BTD).
56 croalgae not only perform fixation of carbon dioxide but also produce valuable byproducts such as lip
57 ynthesis of chiral 1,2,5-thiadiazolidine-1,1-dioxides by an enantioselective ring-closing 1,5-C-H ami
58 n the gaseous nature of the resulting carbon dioxide byproduct.
59 nium-containing minerals other than titanium dioxide can also photocatalyze trace gas uptake, that sa
60 th 6 equiv of the base 1,2-benzothiazine 1,1-dioxides can be prepared in most cases as the main produ
61 emperature liquid-phase materials for carbon dioxide capture and we propose here that they can also b
62  providing sufficient oxygenation and carbon dioxide clearance, while limiting the harmful effects of
63 s in the electrochemical reduction of carbon dioxide (CO(2) ) and carbon monoxide (CO) on copper surf
64  wetlands in sequestering atmospheric carbon dioxide (CO(2) ) and mitigating climate change has recei
65 oxide (N(2) O), methane (CH(4) ), and carbon dioxide (CO(2) ) are affected by complex interactions of
66                    Rising atmospheric carbon dioxide (CO(2) ) concentrations may warm northern latitu
67  (OA), a consequence of anthropogenic carbon dioxide (CO(2) ) emissions, strongly impacts marine ecos
68                           Autotrophic carbon dioxide (CO(2) ) fixation by microbes is ubiquitous in t
69                    The conductance of carbon dioxide (CO(2) ) from the substomatal cavities to the in
70                        Methanation of carbon dioxide (CO(2) ) is attractive within the context of a r
71                  Chronically elevated carbon dioxide (CO(2) ) levels can occur in confined spaces suc
72 e observations to investigate the net carbon dioxide (CO(2) ) seasonal cycle and its climatic and env
73  and can offset summer photosynthetic carbon dioxide (CO(2) ) uptake.
74 climation to elevated temperature and carbon dioxide (CO(2) ).
75 driven by increased concentrations of carbon dioxide (CO(2)) [i.e., the CO(2) fertilization effect (C
76 ure (TEE), oxygen (O(2)) consumption, carbon dioxide (CO(2)) and metabolic heat (H(prod)) production,
77 ating bills and increase damages from carbon dioxide (CO(2)) and other pollutants.
78 creasing concentration of atmospheric carbon dioxide (CO(2)) and rising earth-surface temperature, wh
79        BAGs sense the respiratory gas carbon dioxide (CO(2)) and, in a context-dependent manner, swit
80 ylamine in water medium under a 1 atm carbon dioxide (CO(2)) atmosphere.
81 oach, that this compound is ideal for carbon dioxide (CO(2)) capture in addition to other anthropogen
82 ity induced by ethyl butyrate (EB) or carbon dioxide (CO(2)) closes within 48 h after eclosion.
83 s between the apparent photosynthetic carbon dioxide (CO(2)) compensation point in the absence of day
84 nels led to a substantial increase in carbon dioxide (CO(2)) conversion and methanol yield in CO(2) h
85 missions as increased noise in the HC/carbon dioxide (CO(2)) correlation measurement.
86 rifts are important sources of mantle carbon dioxide (CO(2)) emission into Earth's atmosphere(1-3).
87  mean temperatures relies on reducing carbon dioxide (CO(2)) emissions and on the removal of CO(2) by
88                         Anthropogenic carbon dioxide (CO(2)) emissions contribute to the greenhouse e
89                          Yet, data on carbon dioxide (CO(2)) emissions from these sediments are too s
90 tes and their contributions to offset carbon dioxide (CO(2)) emissions.
91 ctivities, and in turn energy use and carbon dioxide (CO(2)) emissions.
92     The oceanic uptake of atmospheric carbon dioxide (CO(2)) emitted by human activities alters the s
93 avenue for solar fuels synthesis from carbon dioxide (CO(2)) fixation but is extremely challenging.
94  rates of net H(2) oxidation and dark carbon dioxide (CO(2)) fixation than those from the carbonate c
95 ogies capable of efficiently removing carbon dioxide (CO(2)) from the flue emissions of natural gas-f
96  patterns of the net uptake fluxes of carbon dioxide (CO(2)) in coastal salt marshes using dimensiona
97           Sequestration of industrial carbon dioxide (CO(2)) in deep geological saline aquifers is ne
98                     The solubility of carbon dioxide (CO(2)) in the moisture and protein components o
99 lerate the low oxygen (O(2)) and high carbon dioxide (CO(2)) of a densely populated fossorial nest.
100 bal warming potential 86-125x that of carbon dioxide (CO(2)) over a twenty-year period, is the main c
101 l CDR goals of 0.5 to 2 gigatonnes of carbon dioxide (CO(2)) per year with extraction costs of approx
102      The electrochemical reduction of carbon dioxide (CO(2)) powered by renewable energy is an attrac
103 ction to hydrogen sulfide (H(2)S) and carbon dioxide (CO(2)) reduction to methane (CH(4)).
104 ds, has potential use for atmospheric carbon dioxide (CO(2)) removal (CDR), which is now necessary to
105 limate change by releasing additional carbon dioxide (CO(2)) to the atmosphere(3-6).
106 e to upgrade greenhouse gases such as carbon dioxide (CO(2)) to valuable fuels and feedstocks; howeve
107 sting is the largest source of CH(4), carbon dioxide (CO(2)), nitrous oxide (N(2)O), and carbon monox
108 r small molecules activation, such as carbon dioxide (CO(2)), nitrous oxide (N(2)O), tetrahydrofuran
109                                       Carbon dioxide (CO(2)), the major product of metabolism, has a
110 tration of several pollutants such as carbon dioxide (CO(2)), tropospheric ozone (O(3)), and particul
111 energy demand and the need to replace carbon dioxide (CO(2))-emitting fossil fuels with renewable sou
112 ed carbonation step involving gaseous carbon dioxide (CO(2)).
113 tal change factors (warming, elevated carbon dioxide [CO(2) ], increased precipitation, increased dro
114 g-term forcing from Deccan volcanism (carbon dioxide [CO(2)]-induced warming) leads to increased habi
115 production and were correlated with nitrogen-dioxide columns at a ratio that is consistent with resul
116 -phenyl-1-thia-2,7-diazaspiro[4,4]nonane 1,1-dioxide (compound E197) prevented pathological bone loss
117 hetic organisms on earth have evolved carbon dioxide concentrating mechanisms to contend with an incr
118                           Atmospheric carbon dioxide concentration ([CO(2) ]) is increasing, which in
119 ns were more sensitive to atmospheric carbon dioxide concentration than to humidity, suggesting that
120 , which acts to lower the atmospheric carbon dioxide concentration.
121 ariates for meteorology, traffic, and sulfur dioxide concentrations (a marker of secondary particle f
122 and two years of elevated atmospheric carbon dioxide concentrations (eCO(2)).
123 res a combination of both atmospheric carbon dioxide concentrations of 1,120-1,680 parts per million
124 edbacks among stomatal sensitivity to carbon dioxide concentrations, soil moisture, and vapor pressur
125 ation, further increasing atmospheric carbon dioxide concentrations.
126 tion Method, and the catalyst shows a carbon dioxide conversion through hydrogenation to hydrocarbons
127 anium oxide crystals, niobium-doped titanium dioxide crystals, niobium-doped barium strontium titaniu
128   Using a phenothiazine-dibenzothiophene-S,S-dioxide donor-acceptor-donor (D-A-D) system, the two phe
129                  Elevated atmospheric carbon dioxide (eCO(2) ) is predicted to increase growth rates
130 lly limit plant responses to elevated carbon dioxide (eCO(2) ), but consensus has yet to be reached o
131 e potential impact of contaminants on carbon dioxide electrolysis is crucial for practical applicatio
132 hyperoxia and other TRPA1 activators (carbon dioxide, electrophiles, and oxidants) in normoxia.
133 trogen dioxide, and nitrous oxide, on carbon dioxide electroreduction on three model electrocatalysts
134 siderable Faradaic efficiency loss in carbon dioxide electroreduction, which is caused by the prefere
135 e mechanisms of oxygen absorption and carbon dioxide elimination.
136 arge-scale hydrogen production, while sulfur dioxide emissions can be effectively used to obtain valu
137  species emitted, nitrogen oxides and sulfur dioxide emissions caused the most cross-state premature
138 ortality, we found that reductions in sulfur-dioxide emissions from large point sources and nitrates
139                                       Sulfur dioxide emissions produced sulfate aerosols that cooled
140 n capture is essential for mitigating carbon dioxide emissions.
141  to three times those associated with sulfur dioxide emissions.
142 rch (BIFoR) began to conduct Free Air Carbon Dioxide Enrichment (FACE) within a mature broadleaf deci
143                                       Carbon dioxide/epoxide copolymerization is an efficient way to
144 varied GHGE targets [2050: 1.11 kg of carbon dioxide equivalent (kg CO2-eq) per person per day (pppd)
145          At current technology costs, carbon dioxide equivalent emission prices of $142 and $215 per
146 agreement [$40 to $80 (USD) per tonne carbon dioxide equivalent] would provide an economic justificat
147 of a single operation ranged 6-814 kg carbon dioxide equivalents.
148 n, we measured evapotranspiration and carbon dioxide exchange over and under an oak savanna and over
149 pb increase in long- and short-term nitrogen dioxide exposure was associated with 3.24 (95% CI: 2.75,
150 g- and short-term PM2.5, ozone, and nitrogen dioxide exposures were all associated with increased mor
151 de reduction performances once a pure carbon dioxide feed is restored, indicating a negligible long-t
152  nitrogen oxides (up to 0.83%) in the carbon dioxide feed leads to a considerable Faradaic efficiency
153                    Global fossil fuel carbon dioxide (FFCO(2)) emissions will be dictated to a great
154       The vast majority of biological carbon dioxide fixation relies on the function of ribulose 1,5-
155  of changes in ocean circulation from carbon dioxide forcing on patterns of ocean warming in both obs
156 ion of delivering oxygen and removing carbon dioxide from all other cells while enduring the shear st
157 mit global climate change by removing carbon dioxide from the atmosphere through the growth of trees.
158 s responsible for the removal of free sulfur dioxide from the reaction medium, and the potassium cati
159 trode (SPCE) modified with graphene/titanium dioxide (G/TiO(2)) nanocomposite to improve the electrod
160         A mechanism for concentrating carbon dioxide has for the first time been successfully transfe
161        The catalytic hydrogenation of carbon dioxide holds immense promise for applications in sustai
162 yer between molybdenum disulfide and hafnium dioxide in a bottom-gate configuration, enhanced the ele
163  a low value for electro-reduction of carbon dioxide in an organic electrolyte.
164 d to reduce the current high level of carbon dioxide in the atmosphere, which is driving climate chan
165  CO(2) and the catalytic reduction of carbon dioxide, including atmospheric CO(2), into methanol, und
166 ly three times the annual atmospheric carbon dioxide increase by fossil fuel burning.
167 ) complexes catalyze the insertion of sulfur dioxide into (het)aryl and alkenyl boronic acids.
168  in the global carbon cycle by fixing carbon dioxide into 1 Gt of biomass annually, yet the fate of f
169 nge, the utilisation or conversion of carbon dioxide into sustainable, synthetic hydrocarbons fuels,
170 Moreover, the direct incorporation of sulfur dioxide into the sulfonylated products via organolithium
171 ly exothermic, expect the case of the sulfur dioxide-involved pathway that is predicted to be endothe
172          Electrochemical reduction of carbon dioxide is a clean and highly attractive strategy for th
173                  Formate oxidation to carbon dioxide is a key reaction in one-carbon compound metabol
174 ess, the (14)C isotope of atmospheric carbon dioxide is fixed in the carbonate, and its radiocarbon d
175 e and bicarbonate in the cells, where carbon dioxide is produced, and in the lungs, where it is relea
176 -yl)-6-(18)F-fluorodibenzo[b,d]thiophene 5,5-dioxide) is a radioligand for estimating the availabilit
177           Nitrous oxide (N(2)O), like carbon dioxide, is a long-lived greenhouse gas that accumulates
178  before present, revealing pronounced carbon dioxide jumps (CDJ) under cold and warm climate conditio
179 oplet followed by dehydration using a carbon dioxide laser.
180                                       Carbon dioxide levels are mildly elevated on the International
181 ion years(1-5), driven by atmospheric carbon dioxide levels of around 1,000 parts per million by volu
182  contributed to the lower atmospheric carbon dioxide levels of the ice ages.
183 arousal in response to elevated blood carbon dioxide levels, as seen in sleep apnea [3].
184 ivinylbenzene) monolithic columns and carbon dioxide/methanol mobile phase.
185 Py) and catalytic activities (from manganese dioxide -MnO(2)) were independent and complementary with
186 lective electrocatalytic upgrading of carbon dioxide/monoxide to valuable multicarbon oxygenates and
187 adhesives containing nitrogen-doped titanium dioxide nanoparticles (N_TiO(2)).
188 (2)) and nitrogen-fluorine co-doped titanium dioxide nanoparticles (NF_TiO(2)) were synthesized and s
189 er treatment of silver (Ag-NPs) and titanium dioxide nanoparticles (TiO(2)-NPs) via selected area ele
190  to evaluate the bioaccumulation of titanium dioxide nanoparticles (TiO(2)NPs) in edible mussels bred
191  events, and ambient air pollution (nitrogen dioxide, nitrogen monoxide, particulate matter (PM) with
192 nt that rapid oxidation of SO(2) by nitrogen dioxide (NO(2)) and nitrous acid (HONO) takes place, the
193  (BaP), sulfur dioxide (SO(2)), and nitrogen dioxide (NO(2)) over two consecutive 24-h sampling perio
194 rates between 0 and 2.2 +/- 0.4% of nitrogen dioxide (NO(2)) photolysis, equivalent to average atmosp
195 .5)), inhalable particles (PM(10)), nitrogen dioxide (NO(2)), sulfur dioxide (SO(2)), ozone (O(3)), a
196 using low-cost passive samplers for nitrogen dioxide (NO(2)), which complement data from the sparse r
197 O(3)) aerosol (at 540 degrees C) to nitrogen dioxide (NO(2)), whose mixing ratio is monitored via its
198  especially for reactive gases like nitrogen dioxide (NO(2)).
199 ted in elevated levels of gas-phase nitrogen dioxide (NO(2)).
200 ghted concentration of ground-level nitrogen dioxide (NO(2): 60% with 95% CI 48 to 72%), and fine par
201 odels included regional pollutants (nitrogen dioxide [NO(2)] or particulate matter with an aerodynami
202 iameter < 2.5 mug/m3 (PM2.5), PM10, nitrogen dioxide (NO2), and nitrogen oxides (NOx) at the nurses'
203 odynamic diameter <= 10 mum (PM10), nitrogen dioxide (NO2), and sulphur dioxide (SO2) with all-cause
204 fic day-evening-night noise (Lden); nitrogen dioxide (NO2); and particulate matter (PM) with aerodyna
205               The electroreduction of carbon dioxide offers a promising avenue to produce valuable fu
206 er by direct reaction of NaPH(2) with carbon dioxide or by hydrolysis of the phosphaethynolate ion (P
207 ercise test, with an excess pulmonary carbon dioxide output ( VCO2 ).
208 nes, which were investigated in the selenium dioxide oxidation to afford further functionalized diene
209  Patients; NCT02541591) and COMACARE (Carbon Dioxide, Oxygen and Mean Arterial Pressure After Cardiac
210       The model includes transport of carbon dioxide, oxygen, bicarbonate, sucrose/glucose, bacteria,
211 mum (PM10 and PM2.5, respectively), nitrogen dioxide, ozone, and black carbon.
212 Hg, and partial pressures of arterial carbon dioxide ( PaCO2 ), which ranged between 34-50 mmHg.
213 partial pressure (pO(2)), and a lower carbon dioxide partial pressure (pCO(2)).
214 iber/whey protein matrix containing titanium dioxide particles (1% TiO(2)) and essential oil droplets
215 er plants emits more nitrogen oxides, sulfur dioxide, particulate matter, and heavy metals per unit o
216 ends in atmospheric concentrations of carbon dioxide (pCO(2)) has become increasingly relevant as mod
217 sis suggests that partial pressure of carbon dioxide (Pco(2)) is the only environmental factor that s
218  when atmospheric partial pressure of carbon dioxide (pCO(2)) ranged from present-day (>400 parts per
219                    Because industrial carbon dioxide point sources often contain numerous contaminant
220  a subunit of the benzodithiophene-thiophene dioxide polymer, and a carotenoid (neurosporene).
221     The electrocatalytic reduction of carbon dioxide, powered by renewable electricity, to produce va
222 aturation, central venous-to-arterial carbon dioxide pressure difference, and oxygen extraction were
223 lysts showed good performances at low carbon dioxide pressures, attributed to synergic interactions b
224 nic "N problem" is distinct from the "carbon dioxide problem" in being more local and less global, mo
225 is technique relies on the release of carbon dioxide produced in situ during a neutralization reactio
226 ), and higher minute ventilation (VE)/carbon dioxide production (VCO2) (34 +/- 5 versus 32 +/- 5, P =
227 n ventilatory efficiency (ventilation/carbon dioxide production slope).
228  the "natural refrigerants" (ammonia, carbon dioxide, propane, and isobutane).
229 ides using organometallic reagents, a sulfur dioxide reagent, and nitrogen based-nucleophiles.
230    Here, we present a high-resolution carbon dioxide record from 330,000 to 450,000 years before pres
231  the electrocatalysts exhibit similar carbon dioxide reduction performances once a pure carbon dioxid
232                   The electrochemical carbon dioxide reduction reaction (CO(2) RR) to produce synthes
233                                   The carbon dioxide reduction reaction (CO(2)RR), in particular elec
234 ior electrocatalytic activity for the carbon dioxide reduction reaction over their fcc counterparts u
235 rk was developed for electrocatalytic carbon dioxide reduction to carbon monoxide in aqueous solution
236                            Pulse-like carbon dioxide release to the atmosphere on centennial time sca
237  weathering (ERW) is a biogeochemical carbon dioxide removal (CDR) strategy aiming to accelerate natu
238 ate, use of venovenous extracorporeal carbon dioxide removal in patients with status asthmaticus can
239 ect patients receiving extracorporeal carbon dioxide removal is safe and feasible and avoids the dele
240 anical ventilation and extracorporeal carbon dioxide removal support, and complications during extrac
241 ubated while receiving extracorporeal carbon dioxide removal support; none required reintubation.
242 wing the initiation of extracorporeal carbon dioxide removal, blood gas values were significantly imp
243 d complications during extracorporeal carbon dioxide removal.
244 rs after initiation of extracorporeal carbon dioxide removal.
245 of 3,4-dihydro-2H-1,2,3-benzothiadiazine 1,1-dioxides result in a ring opening along the N-N bond, fo
246    We successfully used supercritical carbon dioxide (Sc-CO(2)) technology for manufacturing a "smart
247        A combination of supercritical carbon dioxide (scCO(2)) impregnation of pyrrole and sonochemic
248 -enhanced dispersion by supercritical carbon dioxide (SEDS) and spray drying (SD) were used to microe
249 icyclic cyclopentenones mediated by selenium dioxide (SeO(2)) are disclosed.
250 (ZIFs), is of particular interest for carbon dioxide sequestration.
251           In this study supercritical carbon dioxide (SFE-CO(2)) and pressurized liquid (PLE) extract
252                                      Silicon dioxide (SiO(2)) having low and tunable refractive index
253 E to molecular allergens by means of silicon dioxide (SiO(2)) NPs.
254 n comparison with ascorbic acid (AA), sulfur dioxide (SO(2)) and bentonite.
255 ing Instrument (OMI) for tropospheric sulfur dioxide (SO(2)) and formaldehyde (HCHO) column mass dens
256 iculate sulfate from the oxidation of sulfur dioxide (SO(2)) emitted by coal combustion.
257 nown carcinogen benzo(a)pyrene (BaP), sulfur dioxide (SO(2)), and nitrogen dioxide (NO(2)) over two c
258 mistry of primary particulate matter, sulfur dioxide (SO(2)), nitrogen oxide (NO(x)), and ammonia (NH
259 s (PM(10)), nitrogen dioxide (NO(2)), sulfur dioxide (SO(2)), ozone (O(3)), and carbon monoxide (CO)-
260  (PM10), nitrogen dioxide (NO2), and sulphur dioxide (SO2) with all-cause infant, neonatal, and postn
261 raction between GNRs and the rutile titanium dioxide substrate.
262 ed on hydrophobically functionalized silicon dioxide substrates via vesicle spreading.
263             Two of the MEMS devices, silicon dioxide surface-micromachined cantilever arrays and zinc
264 reagent to the commercially available sulfur dioxide surrogate, DABSO, generates a metal sulfinate wh
265                Reductions in arterial carbon dioxide tension (> 20 mm Hg) from the initiation of extr
266 els of oxygen, the way the prevailing carbon dioxide tension (Pa(CO(2))) blunts the brain's response
267 ociation between the initial arterial carbon dioxide tension and change over 24 hours on mortality an
268  4,918 of these patients had arterial carbon dioxide tension data available at 24 hours on support.
269          The manipulation of arterial carbon dioxide tension is associated with differential mortalit
270 e reductions (> 20 mm Hg) in arterial carbon dioxide tension over 24 hours were associated with impor
271                      Initial arterial carbon dioxide tension tension was independently associated wit
272 , independent of the initial arterial carbon dioxide tension.
273 he ocean to absorb massive amounts of carbon dioxide, thus limiting the global warming otherwise expe
274 chemistries, including metallic and titanium dioxide (TiO(2)).
275 T wax combined with a UV absorbant (titanium dioxide, TiO(2)).
276 able onset potential for reduction of carbon dioxide to formic acid at -1.45 V vs. Ag/Ag(+), represen
277 r P(=O)CH(2)B carbon nucleophile with carbon dioxide to give a bicyclic product by P-CH(2) attack on
278 n-decalactone, cyclohexene oxide, and carbon dioxide to make a series of poly(cyclohexene carbonate-b
279 11) catalyst from carbon monoxide and carbon dioxide to methanol under a reaction environment with me
280 d cyanobacteria for the conversion of carbon dioxide to useful chemicals via light-driven, endergonic
281 s in the electrochemical reduction of carbon dioxide to value-added products has the potential to ena
282 ose containing pockets of pressurized carbon dioxide, to study rock fractures.
283 how the Earth system responds to high carbon dioxide, underlining a fundamental role for paleoclimato
284 elds (turnover numbers), quantitative carbon dioxide uptake (>99%), and high selectivity for polyol f
285 oth forest production and atmospheric carbon dioxide uptake.
286  An ultrasound-assisted supercritical carbon dioxide (USC-CO(2)) procedure was developed for the extr
287 rude oil, the fuels are produced from carbon dioxide using sustainable renewable hydrogen and energy.
288 ute ventilation required to eliminate carbon dioxide, VE/VCO2) during exercise potently predicts outc
289           We perform experiments on vanadium dioxide VO(2) films, which exhibit a first-order PIPT ac
290                            To date, vanadium dioxide (VO(2) ) is the only known simple transition-met
291                                     Vanadium dioxide (VO(2)) features a pronounced, thermally-driven
292 multilayered device, comprised of a vanadium dioxide (VO(2)) thin film on a silicon substrate with a
293 rongly correlated electron compound vanadium dioxide (VO(2)).
294 frared emission from a thin film of vanadium dioxide (VO(2)).
295 tative, 2-thia-1-azabicyclo[2.1.1]hexane 2,2-dioxide) were synthesized by cyclization of the correspo
296 sed on thin films of tungsten-doped vanadium dioxide where the tungsten fraction is judiciously grade
297 sitive to CH(4), hydrogen (H(2)), and carbon dioxide with a large dynamic range from trace levels (de
298  carbodiimides, carbon disulfide, and carbon dioxide with carbanions or enamines (reference nucleophi
299            We present a new adduct of carbon dioxide with dihydrogenphosphide, that may be prepared e
300 become available for the reduction of carbon dioxide with selective formation of carbonate.

 
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