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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.
17 obliquity-induced lag, in turn, makes carbon dioxide a delayed climate amplifier in the late Pleistoc
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
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
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
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
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
48 ry have largely employed commercial titanium dioxide as a proxy for its photochemically active fracti
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
54 t)-can explain the lag of atmospheric carbon dioxide behind climate during glacial inception and degl
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
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
67 (OA), a consequence of anthropogenic carbon dioxide (CO(2) ) emissions, strongly impacts marine ecos
72 e observations to investigate the net carbon dioxide (CO(2) ) seasonal cycle and its climatic and env
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,
78 creasing concentration of atmospheric carbon dioxide (CO(2)) and rising earth-surface temperature, wh
81 oach, that this compound is ideal for carbon dioxide (CO(2)) capture in addition to other anthropogen
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
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
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
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
104 ds, has potential use for atmospheric carbon dioxide (CO(2)) removal (CDR), which is now necessary to
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
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
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
119 ns were more sensitive to atmospheric carbon dioxide concentration than to humidity, suggesting that
121 ariates for meteorology, traffic, and sulfur dioxide concentrations (a marker of secondary particle f
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
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
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
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
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
142 rch (BIFoR) began to conduct Free Air Carbon Dioxide Enrichment (FACE) within a mature broadleaf deci
144 varied GHGE targets [2050: 1.11 kg of carbon dioxide equivalent (kg CO2-eq) per person per day (pppd)
146 agreement [$40 to $80 (USD) per tonne carbon dioxide equivalent] would provide an economic justificat
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
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
162 yer between molybdenum disulfide and hafnium dioxide in a bottom-gate configuration, enhanced the ele
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
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
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
178 before present, revealing pronounced carbon dioxide jumps (CDJ) under cold and warm climate conditio
181 ion years(1-5), driven by atmospheric carbon dioxide levels of around 1,000 parts per million by volu
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
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
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
206 er by direct reaction of NaPH(2) with carbon dioxide or by hydrolysis of the phosphaethynolate ion (P
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
212 Hg, and partial pressures of arterial carbon dioxide ( PaCO2 ), which ranged between 34-50 mmHg.
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
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 =
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
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
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
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
248 -enhanced dispersion by supercritical carbon dioxide (SEDS) and spray drying (SD) were used to microe
255 ing Instrument (OMI) for tropospheric sulfur dioxide (SO(2)) and formaldehyde (HCHO) column mass dens
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
264 reagent to the commercially available sulfur dioxide surrogate, DABSO, generates a metal sulfinate wh
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.
270 e reductions (> 20 mm Hg) in arterial carbon dioxide tension over 24 hours were associated with impor
273 he ocean to absorb massive amounts of carbon dioxide, thus limiting the global warming otherwise expe
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
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
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
292 multilayered device, comprised of a vanadium dioxide (VO(2)) thin film on a silicon substrate with a
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