ライフサイエンスコーパス: dissolution

1 d eliminated as proximal causes for boehmite dissolution.

2 ndicate that there was no significant copper dissolution.

3 ed Mg/S batteries by suppressing polysulfide dissolution.

4 ion processes, also referred to as transient dissolution.

5 ine capsule took 3 times longer to reach 80% dissolution.

6 channeling, and increasingly limited calcite dissolution.

7 cture of boehmite inhibited delamination and dissolution.

8 changing balance between CO2 production and dissolution.

9 to 4 degrees C due to accelerated reductive dissolution.

10 ing particle precipitation, aggregation, and dissolution.

11 reaction kinetics and negligible polysulfide dissolution.

12 as considered to be the mechanism that drove dissolution.

13 plates of both species were not affected by dissolution.

14 than river water due to inhibition of oxide dissolution.

15 ith low light, HA alone did not change their dissolution.

16 examine the impact of the crystal defects on dissolution.

17 ct effluent to assess the individual mineral dissolution.

18 model was then used to estimate that bubble dissolution accounts for approximately 10% of methane ac

19 n situ and to estimate the local enthalpy of dissolution across a defined temperature range.

20 The benign dissolution advantageously maintains the morphology of t

21 ccurrence of potential procedural artifacts (dissolution, agglomeration) using a dissolved/particulat

22 ages and what would be expected from mineral dissolution alone suggest that there is erosion of the a

23 Despite greater thrombus dissolution, alpha2-antiplasmin inactivation alone, or i

24 occlusive thrombi, thereby leading to their dissolution and arterial recanalization.

25 lasmin inactivation on experimental thrombus dissolution and bleeding.

26 ations were controlled by dicalcium silicate dissolution and Ca-Si-H precipitation, leading to relati

27 roved to be more effective in catalyzing CO2 dissolution and can sufficiently alleviate the negative

28 to spatial distribution of silicate mineral dissolution and carbonate mineral precipitation.

29 and mineral spatial distributions on mineral dissolution and carbonation reactions in fractured basal

30 ng gel (PPT-gel) in mice, indicating greater dissolution and cellular uptake of PNC than PPT.

31 plained by models that consider only mineral dissolution and development of an altered layer.

32 omoted 2,6-DMHQ oxidation both via reductive dissolution and heterogeneous catalysis while goethite m

33 ybrid electrolyte limits lithium polysulfide dissolution and is, thus, ideally suited for Li-S cells.

34 osage formulations depends on their release, dissolution and its permeability through the gastrointes

35 However, the polysulfide dissolution and low electronic conductivity of sulfur ca

36 affect rice uptake of As, the kinetics of Si dissolution and nutrient availability can also affect As

37 od is simpler, avoiding solvent evaporation, dissolution and partition in a separating funnel; moreov

38 , indicating an association between titanium dissolution and peri-implantitis.

39 aces, we observe in situ nano- to microscale dissolution and pit formation (qualitatively similar to

40 e Bi-birnessite-layered structure during its dissolution and precipitation process for stabilizing an

41 ext] in solution is a direct measure of both dissolution and precipitation reactions across a large r

42 ficacy, essentially by accelerating thrombus dissolution and preventing rethrombosis.

43 nhance LNAPL (light nonaqueous phase liquid) dissolution and produce bioavailable soluble compounds.

44 nstrated the enhancement of organic compound dissolution and production of soluble compounds due to t

45 Fe(III) phases derived from the progressive dissolution and re-oxidation of native Fe(III) oxides ac

46 Light increased their dissolution and release of dissolved Cd.

47 o solution as V(V) during dicalcium silicate dissolution and some V was incorporated into neo-formed

48 The leakage of anthocyanin during CaCO3 core dissolution and storage was also inhibited by two polysa

49 Our results suggest that brucite dissolution and struvite precipitation were coupled at t

50 does not always result in efficient thrombus dissolution and subsequent blood vessel recanalization.

51 the dependencies between the process of FeS2 dissolution and the degradation of H2O2 through the Fent

52 the Northeast Atlantic exhibit greater shell dissolution and the inability to upregulate their metabo

53 tive organic carbon, including the reductive dissolution and transformation of ferric iron (Fe) oxide

54 ils: atmospheric pressure pumping, carbonate dissolution, and percolation of soil water through the v

55 temsavir (35), a prodrug designed to address dissolution- and solubility-limited absorption issues.

56 At zero PO4(3-) loading, reductive dissolution appears to be constrained by the rapid trans

57 e analyzed, and strategies for circumventing dissolution are suggested.

58 These bubbles are subject to dissolution as they rise, and dissolution rates are stro

59 Factors triggering titanium dissolution, as well as the role of titanium corrosion i

60 In this regard, the dissolution behavior of boehmite (gamma-AlOOH) and gibbs

61 Here we show that complex silicate material dissolution behaviors can emerge from a simple positive

62 by warming-induced bleaching and postmortem dissolution, but the finding here that ACC particles are

63 Here we present the mechanism of metals dissolution by highly acidic sulfate aerosol and the eff

64 An alternative process consists of calcite dissolution by slurry flow of micron-size calcite partic

65 h makes ferrihydrite more prone to reductive dissolution by the 2,6-DMBQ/2,6-DMHQ redox couple.

66 Regulating intermediary polysulfide dissolution by understanding the metamorphosis is essent

67 he observed trend of H2O2, showing that FeS2 dissolution can act as a natural Fenton reagent, influen

68 We show that crystalline doxorubicin dissolution can be described by a first order rate const

69 Calcite dissolution can increase pH slightly and cause As re-ads

70 e and Fe(2+), which is a product of greigite dissolution, can react with dissolved HS(-) to form FeS,

71 Olivine dissolution caused a significant increase in alkalinity

72 ed to promoting the thermodynamically driven dissolution common for molecule-sized species.

73 Our findings indicate that dissolution, concentration, and aging time are important

74 oncentration, slurry feed concentration, and dissolution contact time.

75 he solution, from which the rate of platinum dissolution could be determined.

76 The cellular uptake and intracellular dissolution could be influenced by drug concentration, i

77 e exception of Mn, which underwent reductive dissolution, CWs were sinks for the studied metals.

78 We then interpret our dissolution data in a framework that incorporates both s

79 eory gives the partial molar Gibbs energy of dissolution, Deltag2, allowing calculation of Henry's co

80 This dissolution depends on the trimming activity of Hsp104,

81 etic resonance imaging (MRI) sensitivity and dissolution DNP can be used to perform in vivo real-time

82 -precipitation shifts significantly toward a dissolution-dominated mechanism below about [Formula: se

83 and growth as well as medial epithelial seam dissolution during palatal fusion.

84 Hyperpolarization by dissolution dynamic nuclear polarization (D-DNP) has eme

85 (p27) was nuclear spin hyperpolarized using dissolution dynamic nuclear polarization (D-DNP).

86 single aliquot of a ligand hyperpolarized by dissolution dynamic nuclear polarization (D-DNP).

87 The advent of dissolution Dynamic Nuclear Polarization (dDNP) and isot

88 energy metabolism and sperm motility we used dissolution Dynamic Nuclear Polarization (dDNP) for the

89 Results indicate that dissolution dynamics become increasingly important with

90 anism for nanoscale material degradation and dissolution (e.g., crevice corrosion) of polycrystalline

91 The solid-to-solid electroreduction and dissolution-electrodeposition mechanisms can easily lead

92 e coverages are made and their resistance to dissolution evaluated using a microfluidic technique.

93 n DNA recombination and must be processed by dissolution (for double HJ) or resolution to ensure geno

94 The mineral dissolution from image analysis was comparable to that m

95 include the role of excipients in assisting dissolution from the MNs, the intrinsic hydrophobicity o

96 tic non-reductive release of Fe (desorption, dissolution) from particulate iron-notably lithogenic-li

97 sensitive to small changes in pH, and shell dissolution has already been observed in areas where ara

98 via a starch-like process, namely successive dissolution, hydrolysis and fermentation in the same rea

99 We study dissolution in a chemically heterogeneous medium consist

100 ation in submerged conditions, revealing CuO dissolution in a concentration-dependent manner.

101 To achieve acceleration of CO2 dissolution in acidic brine containing high salinity con

102 l concept and studied the kinetic process of dissolution in cancer cells.

103 activity of CoPi occurs with negligible film dissolution in neutral pH for typical cell geometries an

104 Near-equilibrium calcite dissolution in seawater contributes significantly to the

105 ee text] is a rate-limiting step for calcite dissolution in seawater.

106 detailed mechanisms responsible for calcite dissolution in seawater.

107 s a key determinant in producing a two-stage dissolution in the calcite.

108 nCu dissolution in the presence of SRE was the predominant i

109 cidification and increased carbonate mineral dissolution in the USA's largest estuary.The potential c

110 NPs by controlling both droplet assembly and dissolution in vitro.

111 mple anion-exchange protocol that allows the dissolution in water of various hydrophobic metal-organi

112 hysicochemical processes from the process of dissolution in water to protein folding, but its origin

113 bio-elastomers were hydrophobic and resisted dissolution in water, hence the release of betanin was d

114 uired for such an "armored bubble" to resist dissolution, in fact engineering a 2D yield stress inter

115 Faster dissolution increased the simulated flows of water-solub

116 erge from a simple positive feedback between dissolution-induced cation release and cation-enhanced d

117 of accelerating gaseous carbon dioxide (CO2) dissolution into a continuous aqueous phase with the use

118 d-state structure persists in solution after dissolution into either D2 O or [D6 ]DMSO.

119 itrosamine and nitramine formation after its dissolution into the amine solvent.

120 photosensitive dye that is protected against dissolution into the LCLC by a liquid crystalline polyme

121 gest that nanoparticle collision and electro-dissolution is a highly dynamic process driven by fast p

122 find a range of pressures over which bubble dissolution is arrested for armored bubbles.

123 es at the site of pulmonary emboli, thrombus dissolution is halted by alpha2-antiplasmin.

124 maticity as key NOM properties affecting the dissolution kinetics and bioavailability of soluble meta

125 erties could be used in the incorporation of dissolution kinetics into predictive models for environm

126 We demonstrate rapid dissolution kinetics of the microneedles in skin.

127 Here, we analyze the dissolution kinetics of the polar zinc-terminated (000-1

128 The CuO NP dissolution kinetics were modeled by a first-order disso

129 s, as well as a means of closely controlling dissolution kinetics.

130 aterials to be determined by analyzing local dissolution kinetics.

131 n-induced cation release and cation-enhanced dissolution kinetics.

132 Such incongruent dissolution led to solid phases with different compositi

133 The connected continuous process of allene dissolution, lithiation, Li-Zn transmetallation, and asy

134 Despite many studies on far-from-equilibrium dissolution, little is known about the detailed mechanis

135 Sulfate-driven metals dissolution may account for sulfate-health associations

136 ework also indicates a significant change in dissolution mechanism at [Formula: see text], which we i

137 Additionally, the dissolution method produces a discrete Al cluster on a s

138 )14 (H2 O)18 (SO4 )5 (Al8 ) through a simple dissolution method.

139 rify the performance of a widely used bubble dissolution model, and the model was then used to estima

140 ution kinetics were modeled by a first-order dissolution model.

141 The close balance of precipitation and dissolution near equilibrium can alter the chemical comp

142 nditions, yielding Fe(II) from FeS oxidative dissolution, nitrite from denitrification, and U(VI) fro

143 wed following the coupled process of calcite dissolution, nucleation of precipitates at the calcite s

144 Dissolution of 7 in pyridine leads to the isolation of [

145 between interfacial rheology and macroscopic dissolution of [Formula: see text] 100 [Formula: see tex

146 ion leads to formation of surface oxides and dissolution of a limited thickness GaAs cap material (</

147 The sintering process involves dissolution of a surface passivation layer of zinc oxide

148 can be turned into a porous material through dissolution of a water-soluble material.

149 Here we demonstrate the true dissolution of a wide range of important 2D nanomaterial

150 Dissolution of adsorbates into organic matter may also a

151 vironmentally representative concentrations, dissolution of Ag was dominant and aggregation was negli

152 microscopy demonstrated internalization and dissolution of AgNPs within microglia and formation of n

153 ay form in natural water systems through the dissolution of aluminum-containing minerals in acidic su

154 Dissolution of apatite-P (Ap-P), the major mineral phase

155 contaminated coastal soils through reductive dissolution of arsenic-bearing mineral oxides in both se

156 and 3.4-fold, respectively, which increased dissolution of ascending petroleum fluids by 25%.

157 ion with surface complexation reactions; (2) dissolution of available calcite plays a critical role i

158 Dissolution of CaCO3, present in trace amounts in India

159 a fracture in the Duperow Dolomite, causing dissolution of calcite and dolomite that result in the f

160 eralization of desalinated water consists of dissolution of calcite particles by flow of acidified de

161 show that during fluid-rock interaction, the dissolution of carbonate minerals in Eagle Ford shale le

162 FFs with hydrochloric acid cause substantial dissolution of carbonate minerals, as expected, increasi

163 lant-induced local acidification, leading to dissolution of carbonates and release of phosphate, and

164 systems, the aggregation, sedimentation, and dissolution of CdSe quantum dots (QDs) in seawater were

165 Initial dissolution of cement phases occurs in the 10-20 nm pore

166 rature had surprisingly little effect on the dissolution of cerrusite, hydrocerussite, chloropyromorp

167 at the active sites are defects formed after dissolution of Co and Mo cations.

168 The dissolution of CO2 bubbles at different pH levels and sa

169 g L(-1) showed a significant increase in the dissolution of CO2 bubbles, but increasing from 30 to 50

170 portant in geologic carbon storage where the dissolution of CO2 in flowing water increases fluid acid

171 Dissolution of CO2 into the suspension creates solute gr

172 cysteine protease with a crucial role in the dissolution of cohesion among sister chromatids during c

173 leavage per se is insufficient for efficient dissolution of cohesion in early anaphase; subsequent Sm

174 changing Scc1 cleavage efficiency, promoting dissolution of cohesion.

175 Using dynamic light scattering analysis, the dissolution of colloids over a time span triggered by th

176 Dissolution of CP 3 in DMSO favors Co-S bond heterolysis

177 fects of common environmental ligands on the dissolution of Cr(III)-(oxy)hydroxide solids and associa

178 Thus, ligand-promoted dissolution of Cr-containing solids, a redox-independent

179 Results indicate that the dissolution of Cu ions from CuNPs drive microbial inhibi

180 increase in extractability was attributed to dissolution of CuO NPs in the soil.

181 Timely dissolution of cytosolic aggregates requires the mitocho

182 confirm that sand patties undergo a gradual dissolution of DOM in both the dark and in the light, bu

183 e the latter is caused by the deposition and dissolution of elemental lithium during cycling.

184 as been well-studied, the disaggregation and dissolution of existing amyloid fibrils is less known.

185 e chemical degradation of PAM, likely due to dissolution of Fe(2+) at low pH.

186 esults also suggest that while the reductive dissolution of Fe(III) oxides reduced the number of sorp

187 at low DO in water (<4 mg L(-1)), reductive dissolution of ferric Fe oxides was associated with mobi

188 prairies from eolian processes, or increased dissolution of fine-grained magnetite in forest soils du

189 Importantly, dissolution of FUS inclusions using engineered Hsp104 di

190 Dissolution of gaseous NH3 in MP medium maintained neutr

191 We propose that loss of adhesion by the dissolution of homogalacturonan in the middle lamellae i

192 n Hsp70/40 is present, yet essential for the dissolution of Hsp104-specific substrates, such as yeast

193 progressive loss of vascular cells and slow dissolution of inter-vascular junctions, which result in

194 ity, especially where algae procure iron via dissolution of iron oxide particles as a result of eithe

195 ches to represent and quantify the reductive dissolution of iron oxides, the concomitant release of s

196 Effective removal or dissolution of large blood clots remains a challenge in

197 Dissolution of lithium polysulfides, volume expansion of

198 fide occur at early stage accompanied by the dissolution of long-chain polysulfide, and solid-state t

199 fluorescence, it is possible to quantify the dissolution of nanocrystals in a biological environment.

200 bumin concentration was also found to reduce dissolution of nanoparticles in seawater with up to 3.3

201 Dissolution of NETs via DNase I did not alter anti-glome

202 ility to analyze potential transformation or dissolution of NPs in cells, we consider this method as

203 l nuclei is unveiled, featuring formation/re-dissolution of nuclei, two-dimensional aggregation and n

204 e bilayer which could be associated with the dissolution of ordered microdomains (i.e., lipid rafts).

205 A strategy to halt dissolution of particle-coated air bubbles in water base

206 The cathodic dissolution of platinum, resulting from the oxygen reduc

207 Maintenance and dissolution of pluripotency are tightly controlled by ph

208 The dissolution of polysulfide intermediates, however, resul

209 mostly depends on the electrolyte due to the dissolution of polysulfides into the electrolyte, along

210 version into the amorphous form enhances the dissolution of poorly soluble drugs, however the barrier

211 Our group previously observed the dissolution of Pt nanoelectrodes at moderately negative

212 Dissolution of pulmonary emboli by alpha2-antiplasmin in

213 With sufficient light, HA increased the dissolution of QDs, while with low light, HA alone did n

214 onditions which facilitate optimal reductive dissolution of schwertmannite.

215 ontradicts a control of atmospheric boron by dissolution of seasalts.

216 Aqueous dissolution of silicate glasses and minerals plays a cri

217 evious studies, we consider three processes: dissolution of solid doxorubicin, protonation/deprotonat

218 total P is dissolved, largely as a result of dissolution of surface-bound forms.

219 In this study, we compared the dissolution of test plates and spines as well as the spi

220 e undesired parasitic reactions, such as the dissolution of the additive in the electrolyte.

221 Complete dissolution of the ash and low mass boat provided high t

222 r-by-Layer assembly of the BSA-TA shells and dissolution of the CaCO3 cores was suggested as the most

223 he evolution of the CH-depleted zone and the dissolution of the cement surfaces utilizing a reduced-d

224 a' phase, (Ni, Co)3Al, followed by selective dissolution of the gamma matrix phase.

225 ehavior are found due to etching and partial dissolution of the initial ZIF-8 crystals.

226 -micelles using Pt nanoparticles followed by dissolution of the interior region in good solvent for P

227 We propose that after the dissolution of the naive ES-cell pluripotency network du

228 le is released to a liquid medium due to the dissolution of the nanocrystal, its fluorescence is quen

229 The dissolution of the nanoparticle into thousands of porphy

230 hese UAPs was found correlated well with the dissolution of the particles.

231 he first stage is characterized by a uniform dissolution of the pore space, while the second stage fo

232 only 50% of the supersaturation attained by dissolution of the single drug systems.

233 ke of the Zn forms, most likely due to rapid dissolution of the ZnO NPs.

234 channels and the faster fragmentation during dissolution of these tablets.

235 was a major component of biofilm matrix, and dissolution of this fibrin scaffold greatly increased su

236 hesized that there is an association between dissolution of titanium from dental implants, which sugg

237 O3(-) (low delta(15)N, high delta(18)O) from dissolution of unexploded NH4NO3 blasting agents in oxic

238 The reaction rate constants (km) for the dissolution of uranyl-vanadate (U-V) minerals predominan

239 l = -0.3 to -0.1 per thousand) suggested the dissolution of ZnS (enriched in light isotopes) in the r

240 min(-1), and the lowest time to achieve 50% dissolution or t1/2 of 1.88 +/- 0.05 min.

241 days, whereas CuxS NPs showed no significant dissolution over the time scales studied.

242 NP, and high stability (i.e., no detectable dissolution) over 24 h across a pH range of 5-9.

243 hrough porosity is an important indicator of dissolution pattern.

244 low characteristic (dolomite) can change the dissolution patterns in the medium with a homogeneous fl

245 Dissolution patterns reflect the balance between the dem

246 be the species responsible for the platinum dissolution phenomenon.

247 conditions, which include nonstoichiometric dissolution, potential pore water saturation in the seab

248 espread carbonate mineral, through a coupled dissolution-precipitation mechanism.

249 This coupled dissolution-precipitation process that occurs in a bound

250 This might occur due to dissolution-precipitation reactions when the most recalc

251 This balance of dissolution-precipitation shifts significantly toward a

252 stabilize the schwertmannite surface against dissolution; probably via the formation of strong surfac

253 nin depolymerizations is questionable as the dissolution procedure initiates fragmentation of lignin

254 a novel way for estimating the intracellular dissolution process of the nanocrystals.

255 Additionally, sensitivity analysis of the dissolution process with respect to acid injection rate

256 draulics of resaturation and the dynamics of dissolution processes.

257 time-and potential-resolved electrochemical dissolution profiles revealed that Ir particles dissolve

258 enzyme carbonic anhydrase (CA) increases the dissolution rate across all saturation states, and the e

259 The rate components and the range of dissolution rate are important input parameters in react

260 ntrolled, order-of-magnitude enhancements of dissolution rate are observed relative to powder-form pa

261 sule, 10%w/w nifedipine/PVP, had the highest dissolution rate constant of 0.37 +/- 0.05 min(-1), and

262 loped as a functional assay to determine the dissolution rate constant.

263 First-order dissolution rate constants of CuO NPs increased with inc

264 ne-polymer interaction lead to a significant dissolution rate enhancement.

265 At pH 7, the CdTe dissolution rate increased linearly with dissolved oxyge

266 ug) was chosen as the model drug as enhanced dissolution rate is vital to guarantee oral bioavailabil

267 The mean dissolution rate of the (000-1) crystal surface is more

268 te spectrum analysis, we observed an overall dissolution rate variability of more than 1 order of mag

269 ed plasma (ICP) can determine both manganese dissolution rates and relative Mn(3+) amounts, by compar

270 are subject to dissolution as they rise, and dissolution rates are strongly influenced by bubble size

271 ere, we investigated the linkage between the dissolution rates of copper(II) oxide (CuO) nanoparticle

272 g higher V concentrations limited by kinetic dissolution rates of dicalcium silicate.

273 ensurate with some of the reported reductive dissolution rates of goethite, suggesting Fe(II) release

274 ce layer is observed, with consequent pyrite dissolution rates reduced by more than 90% at neutral pH

275 L(-1)), resulting in a wide range of CuO NP dissolution rates that subsequently influenced Cu uptake

276 saturation horizon (ASH) and high carbonate dissolution rates there, fueled the hypothesis that reef

277 the release of cytotoxic Zn(2+) ions during dissolution reactions.

278 Host-basalt dissolution releases nutrients and energy sources, which

279 uptake mechanisms-edge sorption, interfacial dissolution-reprecipitation-are at play and control anio

280 eduction potential results from clay mineral dissolution resulting in increased Fe(III) contents in t

281 h exudate coated particles undergoing faster dissolution than bare iron oxide particles.

282 tiplasmin inactivation, causing more embolus dissolution than clinical-dose r-tPA alone (P<0.001) or

283 g conditions, jarosite may undergo reductive dissolution, thereby releasing As, Sb, and Fe(2+) coinci

284 from a state of net accretion to one of net dissolution this century.

285 particle stability and accelerated the lead dissolution, thus changing the bioavailability processes

286 The study involved determination of dissolution time under different conditions and solubili

287 of silver detected from AgNPs is due to AgNP dissolution to silver ion.

288 (SEI) but also to accommodate Li deposition/dissolution under the skin in a dendrite/moss-free manne

289 agent that enables rapid disintegration and dissolution upon oral ingestion.

290 esence of natural organic matter, lead oxide dissolution was 36 times greater (36 versus 1277 ppb) at

291 Abiotic dissolution was 39% of total denudation in plant-microbe

292 Thrombus dissolution was markedly accelerated in mice with normal

293 Ease of calcium dissolution was not different between single- and double

294 Calcium dissolution was subjectively scored (easy = 1; intermedi

295 een 1 and 10 mug L(-1), both aggregation and dissolution were important.

296 and buffers caused variable extents of GRCl dissolution which was linearly correlated with CF suppre

297 The precise correlation of metal dissolution with applied potential/current density allow

298 design of remineralization by calcite slurry dissolution with carbonic and sulfuric acids.

299 rength for insertion to pig skin ex vivo and dissolution within 2min.

300 rtlandite (CH)-depleted zone and the surface dissolution zone in the CO2-attacked cement.