ライフサイエンスコーパス: carbonate

1 carbonylation of an o-quinone into a cyclic carbonate.

2 etween azaaryl acetamide and cinnamyl methyl carbonate.

3 ration products, such as lead oxide and lead carbonate.

4 arbon, and oxygen that correspond to calcium carbonate.

5 tures and mercury concentrations of biogenic carbonate.

6 f carbon dioxide with selective formation of carbonate.

7 ate the specific (14)C signature to the lead carbonate.

8 cific six-membered asymmetric cyclic glucose carbonates.

9 ctrophiles generated from allylic tert-butyl carbonates.

10 followed by Mg(OH)(2), and magnesium hydroxy carbonates.

11 the hydrolysis reaction of bis(4-nitrophenyl)carbonate (1) but inhibits that of bis(4-nitrophenyl)thi

12 s, 1-(10H-phenothiazin-2-yl)vinyl tert-butyl carbonate (2APT-D6) was selected for its high potency.

13 xylitol and inulin solutions with a calcium carbonate (5%), where the process was conducted for 120

14 on amorphous hydroxyapatite combined with Ca carbonate, a greater porosity, lower agglomerates and pa

15 Amorphous calcium carbonate (ACC) is an unstable mineral phase, which is p

16 g Raman microspectroscopy, amorphous calcium carbonate (ACC) was observed first in the drops, followe

17 precipitate in the form of amorphous calcium carbonate (ACC).

18 Sodium carbonate addition increased pH and caused a consequenti

19 Upon catalysis, a surface carbonate adsorbate-layer was formed, of which the decom

20 In this work, we studied how carbonate affected the free energy relationship by exami

21 We observed no evidence for carbonate affecting Fe(3+)/Fe(2+) reduction potentials o

22 sphate (TMP), the oxidation-vulnerable anion-carbonate affinities are decoupled because of the prefer

23 The reproduced MgO is spread over land to carbonate again.

24 that in common with woody biomass residues, carbonated agricultural biomass ash-based monoliths have

25 The carbonates, alteration minerals from the Martian near-su

26 nce of the Earth's carbon cycle, we focus on carbonate and bicarbonate ions.

27 tive rates of formation are here compared in carbonate and ether-electrolytes.

28 he pair distribution function from collagen, carbonate and finite crystallite size were examined thro

29 hesis splits CO(2) by electrolysis in molten carbonate and has a carbon negative footprint.

30 alt as food ingredient, based on modified Ca carbonate and hydroxyapatite (FCC), was determined and c

31 Controversial questions included the role of carbonate and macroalgae in BC cycling, and the degree t

32 conveyed Mediterranean Water with excess of carbonate and the arrival of subpolar-origin waters clos

33 All participants received daily calcium carbonate and vitamin D supplementation and were asked t

34 Stable isotope data from enamel carbonates and dentin collagen (childhood diet) and dent

35 approach is proposed to separate the various carbonates and isolate the specific (14)C signature to t

36 id without melting, producing the respective carbonates and oxides as final residues.

37 intimate association between mantle-derived carbonates and sulfides in some mafic-ultramafic magmati

38 ction focus the largest recycling of crustal carbonates and the most intense seismic activity on Eart

39 rove upon the properties of poly(cyclohexene carbonate) and, specifically, they show good thermal sta

40 strongly to low concentrations of fluoride, carbonate, and acetate ions, weakly to phosphate ions, b

41 er comprising poly p-dioxanone, trimethylene carbonate, and glycolide.

42 f synthesis, lower concentrations of lithium carbonate, and higher current density promotes CNS growt

43 f atmospheric carbon dioxide is fixed in the carbonate, and its radiocarbon dating can be used as a p

44 BioCer transformed to carbonated apatite in vivo, and the regenerated bone dis

45 tope and the clumped isotope compositions of carbonate archives.

46 tion of sediments rich in organic matter and carbonates around the dikes and sills releases 18 Gt of

47 lkenes using a JohnPhos ligand and potassium carbonate as a base in dimethylformamide at 105 degrees

48 the waters surrounding CWC communities lose carbonate at a rate of - 0.17 +/- 0.02 mumol kg(-1) ppm(

49 50 wt% sodium carbonate relative to lithium carbonate at an electrolysis temperature of 670 degrees

50 entropy, while the Co(II) centre accelerates carbonate attack by lowering the transition state enthal

51 dioxide to make a series of poly(cyclohexene carbonate-b-decalactone-b-cyclohexene carbonate) [PCHC-P

52 features corresponding to the phosphate and carbonate bands between the benign and malignant groups.

53 an operate up to 6 mA cm(-2) in a commercial carbonate-based electrolyte; omitting the SAW leads to s

54 he C and O K-edges to track the stability of carbonate-based electrolytes, F K-edge to study the elec

55 procedure was furthermore verified on mixed carbonate-bearing paint samples collected from a Baroque

56 he molar ratio of beta-cyclodextrin:diphenyl carbonate (beta-CD:DPC; 1:2, 1:6 and 1:10).

57 nificant association between sugar-sweetened carbonated beverages and a moderately increased risk of

58 A high intake of sugar-sweetened carbonated beverages was associated with a statistically

59 eriments with Lp at pH 7.0 were conducted in carbonate-buffered suspensions to mimic environmental co

60 e disinfection of drinking water (pH 6-9 and carbonate-buffered) was developed to simulate incomplete

61 with different solubility were used: calcium carbonate (CaC), tricalcium phosphate (CaP) and calcium

62 We have studied microbial induced calcium carbonate (CaCO(3)) precipitation (MICP) in three ureoly

63 We directly probe the interface of calcium carbonate (calcite) with natural petroleum oil, syntheti

64 onate (cerussite or hydrocerussite), calcium carbonate (calcite), and/or calcium magnesium carbonate

65 analyses indicate that decomposition of lead carbonate can be achieved at 350 degrees C in TGA diagra

66 on kinetics involved in the precipitation of carbonates can introduce inaccuracies in the derived tem

67 dioxide (CO(2)) fixation than those from the carbonate catchment, indicating adaptation to use H(2) a

68 a is quickly hydrolyzed into ammonia and (bi)carbonate, causing nutrient loss, clogging of collection

69 Carbonate cave deposits (speleothems) have been used wid

70 drate (CCT), tri-Ca phosphate (triCP) and Ca carbonate (CC).

71 llus Shale, including exchangeable sites and carbonate cement.

72 with ash yield and the microstructure of the carbonate-cementing phase was distinct and related to th

73 enting a mixture of carbonates, such as lead carbonate (cerussite or hydrocerussite), calcium carbona

74 13)C, and Mg/Ca to reconstruct surface ocean carbonate chemistry and temperature.

75 Syntheses of carbonate chemistry spatial patterns are important for p

76 nergetically costly changes in CO(2) -driven carbonate chemistry that will be most pronounced in cold

77 diel fluctuations of multiple parameters of carbonate chemistry were greater in the kelp canopy than

78 rivers, such as temperature, pH and seawater carbonate chemistry, and dissolved oxygen, can exceed th

79 soil spiked with various Pb compounds (i.e., carbonate, chloride, phosphate [P], or sulfate) to conve

80 resent the first coupled records of biogenic carbonate clumped isotope paleothermometry and mercury c

81 er-scale mineral grains and microcrystalline carbonate coatings that entombed filamentous cyanobacter

82 a kinetic reaction of aqueous uranyl-calcium-carbonate complexation.

83 (which adsorb (210)Pb) and formation of lead-carbonate complexes (enhancing lead (Pb) mobility).

84 ty of NS was enhanced by increasing diphenyl carbonate concentration.

85 In the mid-layer, the carbonate content in the Northeast Atlantic is maintaine

86 of synthetic hydroxyapatites with differing carbonate content, notably in features near 4 angstrom,

87 trations, these wastes have high silicate to carbonate conversion rates.

88 ded to the precipitation solution of calcium carbonate crystallizes the thermodynamically disfavored

89 oxalate crystals (CaOx) or amorphous calcium carbonate cystoliths are spread among most photosyntheti

90 We evaluate these data (and published carbonate delta(238)U data) with a coupled stochastic ma

91 anoxia, with global reconstructions based on carbonate delta(238)U modeling.

92 sotopic composition of lacustrine authigenic carbonates (delta(18)O(carb)) and its spatial distributi

93 Uranium-lead chronology of carbonate deposits (speleothems) in a Siberian cave loca

94 Li cell using a 1 M LiAsF(6) in 1:1 ethylene carbonate/dimethyl carbonate (EC/DMC) electrolyte under

95 harge into the subsurface and 2) the coupled carbonate dissolution and pyrite oxidation at depth in t

96 arbonate (calcite), and/or calcium magnesium carbonate (dolomite).

97 order of magnitude higher than those from a carbonate-dominated catchment.

98 issue, we propose the additions of ethylene carbonate (EC) to the imaging buffer, sequence repeats t

99 encies and cycle lives of LMBs with ethylene carbonate (EC), dimethyl carbonate, ethylene sulfite (ES

100 pplied to dimethoxyethane (DME) and ethylene carbonate (EC), the present methodology shows that both

101 LiAsF(6) in 1:1 ethylene carbonate/dimethyl carbonate (EC/DMC) electrolyte under galvanostatic and i

102 communities differ from other shallow-water carbonate ecosystems, such as reef communities, which re

103 ss, followed by deposition of diamectite and carbonate ejecta represented by large polished striated

104 ate (pH 7.0) and 1.25 V in ammonium hydrogen carbonate electrolyte (pH 8.0).

105 f 5-10 wt% lithium metaborate to the lithium carbonate electrolyte boron dopes the CNTs increasing th

106 As a result, our designed carbonate electrolyte enables a Li anode to achieve a hi

107 -solid-state" electrochemical process in the carbonate electrolyte system.

108 node, a 4 V Li-ion cathode, and a commercial carbonate electrolyte, shows capacity retention of 90.9%

109 In a pure molten lithium carbonate electrolyte, thicker walled CNTs (100-160 nm d

110 f the 4-electron CO(2) reduction in a molten carbonate electrolyte.

111 eveal its internal reaction mechanism in the carbonate electrolyte.

112 ng behavior even with a conventional KPF(6) -carbonate electrolyte.

113 tial of 20 mV for 200 cycles in a commercial carbonate electrolyte.

114 direct air capture) to renew and sustain the carbonate electrolyte.

115 olytes elevate the electrochemical window of carbonate electrolytes by 0.45 V and enable the operatio

116 we restore the inherent anodic stability of carbonate electrolytes by designing a micro-heterogeneou

117 In carbonate electrolytes, the organic-inorganic solid elec

118 pper carbonate nanoparticles (CuNPs) using a carbonate-enriched biomass-free ureolytic fungal culture

119 ct of the digestion process and modifies the carbonate equilibrium.

120 LMBs with ethylene carbonate (EC), dimethyl carbonate, ethylene sulfite (ES), and their combinations

121 e (DMSO) as an additive for a fluoroethylene-carbonate (FEC)-based electrolyte.

122 If the veins on Bennu are carbonates, fluid flow and hydrothermal deposition on Be

123 lcium concentration, by strongly influencing carbonate fluorapatite (CFA) formation, is a key factor

124 loxycarbonate (Alloc), and 9-fluorenylmethyl carbonate (Fmoc), different patterns of O-sulfation can

125 This MgO is spread over land to carbonate for a year by reacting with atmospheric CO(2).

126 itric acid for 12 h, and then in 1 M calcium carbonate for another 12 h, the latter step to neutraliz

127 in euthymic patients with BD treated with Li carbonate for at least 2 years.

128 On submonolayer CoO(x) islands, the carbonates form preferentially at island edges, deactiva

129 actions between the environment and Halimeda carbonate formation at temporal and spatial scales not n

130 Carbonate formation is the primary source of energy and

131 edge structure (XANES) spectroscopy for nine carbonate-free soil samples with diverse chemical and mi

132 ciated with intensive agricultural land use, carbonate geology, and sparse riparian canopy, which sug

133 ol)-block-poly(2-methyl-2-carboxyl-propylene carbonate-graft-dodecanol) (mPEG-b-PCC-g-DC) polymeric n

134 s either 3,4-diacetyl groups or a 3,4-cyclic carbonate group at the reducing end fucoside to mimic th

135 enzyl (ester) or an alkoxycarbonyloxybenzyl (carbonate) group.

136 gy relationship by examining the effect that carbonate has on nitrobenzene reduction rates by Fe(2+)

137 The previously reported carbonate hydrolysis protocol reaches its limitation whe

138 ly pictured as a parallel array of ultrathin carbonated hydroxyapatite (HAp) platelets distributed th

139 ays of extremely long and narrow crystals of carbonated hydroxyapatite called enamel rods.

140 ponsive system is developed from luminescent carbonated hydroxyapatite nanoparticles doped with Eu(3+

141 molecular C-H oxygenations to provide cyclic carbonates, hydroxylated carbamates, or 1,2-diols.

142 Soil carbonates (i.e., soil inorganic carbon or SIC) represen

143 tope contents of the diamonds, indicate that carbonated igneous oceanic crust, not sediment, is the p

144 thetic oxidation, CO(2) activation to cyclic carbonates, imine metathesis, and selective catalytic re

145 rampant generation of lithium hydroxide and carbonate impurities, commonly known as residual lithium

146 and their ability to be bound by mineralised carbonate in a hardened product is examined.

147 Treatment with primary amines and cesium carbonate in a two-step sequence gives rise to 3-amino-2

148 egrees C will avoid the exhaustion of excess carbonate in the Northeast Atlantic.

149 m large-bodied fossil mammals, and pedogenic carbonates in fossil soils, from East Turkana in norther

150 Here we report that 4-billion-year-old (Ga) carbonates in Martian meteorite, Allan Hills 84001, pres

151 ; ester) or an alkoxycarbonyloxybenzyl (ACB; carbonate) in combination with an ACB moiety are describ

152 e, lipids were found concentrated on calcium carbonate inclusions in the ceramics, which suggests tha

153 evealed that highly bioavailable Pb (hydroxy)carbonate (indicative of Pb-based paint) was the major P

154 ver, the nucleophilic attack of the anion on carbonates induces an oxidative breakdown at high potent

155 n along localized shear zones enhanced fluid-carbonate interactions and fluid channelization.

156 omers to maximize coordination of endogenous carbonate ions.

157 flanking a core rich in sodium, fluoride and carbonate ions; this sandwich core is surrounded by a sh

158 ilibrium, the oxygen isotopic composition of carbonate is dependent not only on the temperature but a

159 topic composition of host water in which the carbonate is formed.

160 ctions, and deduced a dual function in which carbonate is responsible for the removal of free sulfur

161 Wettability control of carbonates is a central concept for enhanced petroleum r

162 ic alkylation of Morita-Baylis-Hillman (MBH) carbonates is described.

163 e most widely investigated, poly(cyclohexene carbonate), is limited by its low elongation at break an

164 polymer products-polycarbonates or polyether carbonates-it could provide an economic stimulus to capt

165 release SN-38, conjugated to the antibody by carbonate linkage.

166 possible to obtain terpolymers with tunable carbonate linkages in the polymer chain.

167 ols is often accomplished by attachment with carbonate linkages, which upon photorelease liberate CO(

168 ied based on their sedimentary setting, with carbonate mangroves being less abundant than terrigenous

169 Although isotopic composition of reef carbonate material can be used to reconstruct past tempe

170 , which we attribute to a mix of organic and carbonate materials.

171 s old through U-series dating of an adhering carbonate matrix.

172 Cesium carbonate-mediated anomeric O-alkylation of various prot

173 ions of dissolved inorganic carbon (DIC) and carbonate mineral saturation state (Omega) are controlle

174 metry of the carbonate sites in the hydrated carbonate mineral, hydromagnesite [4 MgCO(3) .Mg(OH)(2)

175 years after CO(2) injection revealed nascent carbonate mineralization that was qualitatively consiste

176 The carbonate minerals are then recollected and re-calcined.

177 c rock dust, including via newly formed soil carbonate minerals whose long-term fate requires assessm

178 carbon in sediments through precipitation of carbonate minerals, thus providing a record of past meth

179 m inflow because calcium is sequestered into carbonate minerals.

180 ient condition for wettability alteration in carbonate minerals.

181 Carbonate molecules occupy the solvation sheath and impr

182 and be used to cement 'raw' biomass in solid carbonated monolithic composites.

183 that the solvation number of fluoroethylene carbonate must be >=1 to ensure the formation of a stabl

184 ices were coated with thin layers of calcium carbonate nanocrystals and the surface was modified to e

185 proteins in the formation of biogenic copper carbonate nanoparticles (CuNPs) using a carbonate-enrich

186 etastable, magnesium-rich, amorphous calcium carbonate nanoparticles that further assemble and transf

187 orous PLA film, was fabricated using calcium carbonate nanoparticles to enhance film porosity leading

188 es, hydrated and anhydrous amorphous calcium carbonate nanoparticles were precursors for skeletal gro

189 using synthetic, amorphous calcium magnesium carbonate nanoparticles.

190 ization within two years, with the resulting carbonates occupying ~4% of the available reservoir pore

191 are hydroxyanions of phosphate, sulfate, and carbonate, often in partnership with charged and neutral

192 degrees C in TGA diagrams, as other mineral carbonates only decompose to carbon dioxide at temperatu

193 1.00 mmol/L (3.10 mg/dl) to 500 mg lanthanum carbonate or matched placebo thrice daily for 96 weeks.

194 e (for instance, carboxylic acids or organic carbonate or nitriles) or into an amine (for instance, a

195 tamin D3 or placebo and 1200 mg/d of calcium carbonate or placebo for 3 or 5 y, and followed after tr

196 MRI data) received 11 (+/-1) days of lithium carbonate or placebo intervention (double-blind), after

197 over 50 wt% of sodium or 30 wt% of potassium carbonate, or at electrolysis temperatures less than 700

198 different labile bonds (i.e., ester, amide, carbonate, or carbamate) that served as labile crosslink

199 hanges in temperature, pCO(2) /pH (and other carbonate parameters), and dissolved oxygen, and discuss

200 hexene carbonate-b-decalactone-b-cyclohexene carbonate) [PCHC-PDL-PCHC].

201 47) and Delta(48) measurements on the single carbonate phase, can identify the origin and quantify th

202 a unique exoskeleton from inorganic calcium carbonate platelets.

203 The impact hit a carbonate platform and released sulfate aerosols and dus

204 ative pentafluorophenyl containing activated carbonate polymer for bioconjugation.

205 produce skeletons exclusively of the calcium-carbonate polymorph aragonite.

206 into commercially attractive poly(propylene carbonate) (PPC) polyols.

207 ed over time and cells surrounded by calcium carbonate precipitates were observed under hydrated cond

208 l activity leads to the formation of calcium carbonate precipitates.

209 One example is microbially induced calcium carbonate precipitation (MICP) in which microbial activi

210 le to delineate regimes dominated by calcium carbonate precipitation and dissolution.

211 rared spectroscopy pinpointed that magnesium carbonate precipitation begins at 1.5 monolayers of adso

212 reshold H(2)O film thickness is required for carbonate precipitation, but a mechanistic understanding

213 We propose here viral mechanisms in carbonate precipitation, leading to stromatolite formati

214 es at the seafloor resulting in low biogenic carbonate preservation.

215 ealigning research priorities to address the carbonate problem is essential if this technology is to

216 ion of 7.7 wt% calcium metaborate to lithium carbonate, produces unusually thin walled CNTs uniform (

217 ue to ocean acidification hindering biogenic carbonate production, which will in turn lead to substan

218 The use of CEM 1 in the carbonated products was offset by the CO(2) mineralised

219 Different temperature sensitivities of carbonate properties and different timescales of influen

220 Carbonate radical anion is a potent one-electron oxidant

221 Instead, carbonate radical anion is formed from the Fenton reacti

222 Fluid-mediated carbonate reduction progressed from discrete domains una

223 Electrolyte conditions of 50 wt% sodium carbonate relative to lithium carbonate at an electrolys

224 the biofilm acidity fluorometrically due to carbonate removal in acidic environments that directly a

225 To represent calcium carbonate reservoir pores, the inner channels of glass m

226 that the pore surfaces are representative of carbonate reservoir rock.

227 for pre-screening EOR surfactants for use in carbonate reservoirs prior to further core and field sca

228 overy by altering the mineral wettability in carbonate reservoirs.

229 s "the phosphate problem." Here we show that carbonate-rich lakes are a marked exception to phosphate

230 molecules is a compelling reason to consider carbonate-rich lakes as plausible settings for the origi

231 In principle, modern carbonate-rich lakes could accumulate up to ~0.1 molal p

232 On the prebiotic Earth, carbonate-rich lakes were likely abundant and phosphate-

233 volatile-rich, redox sensitive rocks such as carbonate-rich lithologies, the breakdown of which can s

234 ng to control the production and location of carbonate-rich magmas.

235 lts from their crystallization from melts of carbonate-rich subducted oceanic crust.

236 These results indicate that reduction of carbonate rocks can exert an important positive feedback

237 suggests that the geochemical properties of carbonate rocks may provide suitable conditions for cert

238 every nuclear waste-generating country, but carbonate rocks may serve as a potential alternative.

239 displacement mechanisms of crude oil in aged carbonate rocks using novel engineered carbon nanosheets

240 rbon and on strain localization in subducted carbonate rocks.

241 ved for naturally derived poly(4,6-d-glucose carbonate)s (PGCs) containing carbonate side chain subst

242 lope for potassium-, calcium-, nitrate-, and carbonate-selective electrodes by combining two or three

243 The fatty tissue and carbonate shells were assessed for accumulation of both

244 (4,6-d-glucose carbonate)s (PGCs) containing carbonate side chain substituents in the 2- and 3-positi

245 Through the water-mediated carbonate-silicate weathering cycle, atmospheric CO(2) p

246 Using a coupled climate and carbonate-silicate weathering model, we quantify the lik

247 We have developed a new class of sodium carbonate/silicone composite sorbents that selectively c

248 We interpret the veins as being composed of carbonates, similar to those found in aqueously altered

249 ) H nuclei perturb the axial symmetry of the carbonate sites in the hydrated carbonate mineral, hydro

250 The basic mechanism of formation of calcium carbonate skeleton in stony corals has been studied for

251 in the Southern Ocean forms a two-component carbonate skeleton, with an inner structure made of high

252 This transition from carbonate slab melting in the transition zone to slab de

253 Carbonate slowed nitrobenzene reduction rates by inducin

254 etermination of nine elements from Brazilian carbonated soft drinks of several flavors and manufactur

255 Conventional carbonate solvents with low HOMO levels are theoreticall

256 o an equivalent octahedral-coordinated M(4+) carbonate species as the resting state in all cases.

257 te, the perturbed shell contains two sets of carbonate species distinguished by their proximity to th

258 rolysis is base-catalyzed, but the impact of carbonate species had not been studied.

259 This work showed that the carbonate species have an enhanced catalytic impact with

260 n at RT, and CO only adsorbed in the form of carbonate species that are stable up to 260 degrees C.

261 ures, followed by the development of surface carbonate species under steady-state conditions.

262 critically control the formation of calcium carbonate structures.

263 etalation of ester-, amide-, carbamate-, and carbonate-substituted 2-phenyl-2-oxazolines with mixed l

264 Regression models were generated to predict carbonate substitution from peak position within the PDF

265 nthetic hydroxyapatites with a wide range of carbonate substitution.

266 fronted with samples presenting a mixture of carbonates, such as lead carbonate (cerussite or hydroce

267 es of LHCEs with model electrolyte solvents (carbonate, sulfone, phosphate, and ether) on the stabili

268 ion of calcium carbonate to a molten lithium carbonate supports the electrosynthesis of thinner walle

269 Estimates of carbonate system parameters from delta(11)B and B/Ca mea

270 tted by human activities alters the seawater carbonate system.

271 and the high ion-transport kinetics from the carbonate systems, this facile strategy provides cells w

272 t reduced nitrogen inputs, particularly over carbonate terrane, are critical for limiting nitrate con

273 hropogenic carbon (C(ant)) and a decrease in carbonate that is unequivocal in the upper and mid-layer

274 ted the role of the basic additive potassium carbonate, the use of which is crucial for efficient rea

275 ty tenfold, and that the addition of calcium carbonate to a molten lithium carbonate supports the ele

276 hat the newly formed dentine comprises equal carbonate to phosphate ratios and mineral to matrix rati

277 s study, we compiled data on methane-derived carbonates to build a proxy time series of methane emiss

278 growth of poorly conducting Li fluorides and carbonates to ensure efficient Li(+) transport.

279 alates, acetates, etc.), aryl carbamates and carbonates, to aryl ethers (anisoles, diaryl ethers, ary

280 at higher temperatures, and propose a novel carbonate-tungstate formulation for application to soure

281 e arrival of subpolar-origin waters close to carbonate undersaturation.

282 in the presence of sodium hydride or cesium carbonate, underwent nucleophilic cyclization to afford

283 erpolymers with comparable thiocarbonate and carbonate units exhibited a refractive index of 1.501 wi

284 Terpolymers with thiocarbonate and carbonate units randomly distributed in the polymers' ma

285 s, which in turn interact with the different carbonates upon heating.

286 n the functionalised graphene oxide and poly(carbonate-urea)urethane with the trade name "Hastalex" i

287 Without Mn(II), the oxidation of Pb(II) carbonate was an autocatalytic process.

288 In this study, fluoroethylene carbonate was used as the SEI enabler due to its ability

289 Electron-deficient allylic carbonate was used to generate the highly reactive palla

290 (ROP) of six-membered cyclic d-glucose-based carbonates was found to result in significantly differen

291 In the carbonate-water system, at equilibrium, the oxygen isoto

292 (PET), polyvinyl chloride, and polypropylene carbonate), were identified in a snowpit from the Austri

293 cribed the data collected in the presence of carbonate when we accounted for the effect it had on the

294 converted to inorganic O (e.g., newly formed carbonates) when samples are ashed.

295 a perturbed occlusion shell of ~8 disordered carbonates which bridge to the bulk.

296 Mixing 4 mM sodium carbonate with the 2 mM tungstate was enough to promote

297 c benzylation of Morita-Baylis-Hillman (MBH) carbonates with 2-methylbenzophenone (MBP) derivatives a

298 llenging alkyl-substituted secondary allylic carbonates with benzylzinc reagents, which are prepared

299 species can selectively precipitate mineral carbonates with enhanced mechanical properties, however,

300 ling between global seawater DIC and shallow carbonate, without burying organic matter or generating