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1 the subjective experience of one's self (ego dissolution).
2 fidic conditions and subsequent Fe reductive dissolution.
3 nated by calcium carbonate precipitation and dissolution.
4 variables involved in the performance of the dissolution.
5 hest extraction of CuO NPs, while minimizing dissolution.
6 g the pH dependence of O(2)(*-)-mediated AFO dissolution.
7 perties, such as morphology, composition and dissolution.
8 Au core-shell nanocubes undergoing oxidative dissolution.
9 nto this microenvironment to promote CaCO(3) dissolution.
10 ntimicrobial lipids, and facilitate membrane dissolution.
11 n cell binding and extracellular virion (EV) dissolution.
12 NPs translocates from the lungs mainly after dissolution.
13 e Carbon ecosystems are sites of net CaCO(3) dissolution.
14 e deformation, and mineral precipitation and dissolution.
15 condensates, and oppose condensate reentrant dissolution.
16 including lipid interdigitation and bilayer dissolution.
17 hence the occurrence or not of LLPS upon ASD dissolution.
18 duced during elongation stimulate condensate dissolution.
19 e associated with positively experienced ego dissolution.
20 where the lowered polarity of water enhances dissolution.
21 t mechanisms of amyloid formation and fibril dissolution.
22 had significantly higher extractability and dissolution.
23 ed into soluble forms by sulfate-driven acid dissolution.
24 d for implant biofilm removal may lead to Ti dissolution.
26 flow-through and one flow-by) indicated 50% dissolution after 5 to 6 days at non-saturating conditio
28 fibrils, a potential method of cell-mediated dissolution, amyloid-like fibrils were labeled with the
29 rly vulnerable to ocean acidification due to dissolution and a reduction in shell-building carbonate
30 OF composites exhibit significantly enhanced dissolution and achieves high supersaturation in simulat
33 n strategies are widely used for alleviating dissolution and diffusion of polysulfides, but they expe
35 e(III)-reducing bacteria which favor mineral dissolution and drive mobilization of both iron and carb
38 ous sources such as atmospheric inputs, rock dissolution and fertilizer residues, and their concentra
40 imated groundwater recharge, suggesting that dissolution and leaching may be responsible for SIC loss
42 ion is achieved by a combination of chemical dissolution and mechanical chip removal and ocean acidif
43 ere specifically favorable for retarding bio-dissolution and mechanical decay of scaffolds in vitro.
44 silicate addition, for reducing both pyrite dissolution and metalliferous drainage, may be applicabl
45 the subsurface and 2) the coupled carbonate dissolution and pyrite oxidation at depth in the rock.
47 er tendency of unwanted transition-metal-ion dissolution and side-reactions in Jahn-Teller-active oxi
49 tion protocol likely contributed to atrazine dissolution and subsequent underestimation of sorbed che
50 on processes associated with electrochemical dissolution and sulfur crossover through the membrane in
51 ion dictates phosphorylation-mediated fibril dissolution and that the hydrophobic effect drives fibri
52 ses drastically, suggesting the preferential dissolution and the formation of more stable Fe oxides.
53 fficient polarizing agents, providing, after dissolution and transfer (10 s), a (13) C liquid-state p
56 c interruption of the reaction for sampling, dissolution, and (bio)chemical analysis to monitor their
57 cantly reduced evaporative loss and material dissolution, and importantly, greatly suppressed competi
59 ions between oil-gas phase transfer; aqueous dissolution; and densities and volumes of liquid oil dro
61 ion of drug compounds in the solution during dissolution (as is commonly done), we monitor the decrea
62 ue to a greater leaf surface affinity and Cu dissolution, as determined computationally and experimen
64 position at 1 week post implantation, graft dissolution at 3 weeks, epithelialization of the ocular
65 data suggest that reef flat corals reach net dissolution at an aragonite saturation state (Omega(AR))
66 infrared spectroscopy showed that forsterite dissolution begins and electrical impedance spectroscopy
67 oil pH and organic matter content affect the dissolution behavior of CuO NP in soil in a predictable
72 nking were sensitive to the proximity to the dissolution ("boiling") temperature of the dense liquid:
73 on in target cell binding and an increase in dissolution, both of which correlated with a small-plaqu
74 (<6 h) via inhibiting arsenopyrite oxidative dissolution, but increased arsenic mobility over a longe
75 dification to regulate droplet formation and dissolution, but the physical basis of the regulatory me
76 id water required for the aqueous phase acid dissolution, but variability in WS-Fe was mainly driven
79 tored during rest periods, and lithium metal dissolution (corrosion) was observed in all electrolytes
80 t of galvanic interaction on reducing pyrite dissolution decreased with increasing pH and was greater
81 ), in terms of three components: enthalpy of dissolution (DeltaH(diss)), enthalpy of formation of aqu
82 t the anode carbon active material initiates dissolution, diffusion, and deposition of reaction side
83 lity, however, the phase solubility test and dissolution/disintegration tests (water and artificial s
85 eted NMR-based metabolomic workflow based on dissolution dynamic nuclear polarization (d-DNP) for the
87 ar magnetic resonance (NMR) monitoring using dissolution dynamic nuclear polarization (D-DNP) to ampl
89 e mostly to single voxel measurements unless dissolution dynamic nuclear polarization (dDNP) is used
96 alytic effect of Fe(II) on ligand-controlled dissolution even at submicromolar Fe(II) concentrations
98 of the experimental design on the results of dissolution experiments of metal and metal oxide NPs is
100 Additional simulations indicate that aqueous dissolution, fluid density changes, and gas-oil phase tr
102 osed solid explosives to quantify in situ MC dissolution fluxes using dissolved MC gradients near the
105 window of 3.3 V, suppresses transition metal dissolution from the cathode, and ensures singular inter
108 properties of bioelectronic implants such as dissolution in body fluids, biocompatibility, mechanical
109 through antisolvent precipitation, involving dissolution in ethanol or glacial acetic acid followed b
111 hout sacrificing their dynamic formation and dissolution in response to physicochemical stimuli.
112 d gold nanoparticles (AuNPs), stable against dissolution in the absence of specific ligands, were add
115 play an important role in AFO photoreductive dissolution in the presence of the chosen surrogate of n
117 onation, phase transformation, and metal-ion dissolution in transition-metal oxides upon exposure to
120 hat reactive iron minerals undergo reductive dissolution inside anoxic microsites of primarily unsatu
121 has been variously ascribed to drilling mud dissolution, interaction with pore fluids or shale excha
124 pendence of LMCT-mediated AFO photoreductive dissolution is mainly controlled by the influence of pH
125 be dominated by solid coating, whereas post dissolution it is dominated by receptor-bound drug (3.7
127 capability depends on the complex growth and dissolution kinetics of lithium sulfide (Li(2)S) and sul
128 NOM) and light on silver nanoparticle (AgNP) dissolution kinetics with particular emphasis on determi
129 oS(2) by NOM was mainly attributed to slower dissolution kinetics with rapid initial oxidation (i.e.,
131 were traced to geogenic sources (weathering, dissolution, leaching) and anthropogenic emissions from
133 e associated with negatively experienced ego dissolution, lower levels in hippocampal glutamate were
134 on microscopy (TEM) imaging reveals that the dissolution mechanism changes from predominantly edge-se
136 lso provide new insights into the V(2) O(5) -dissolution mechanisms for different Zn-salt aqueous ele
137 study, the degree of supersaturation in the dissolution medium generated by the crosslinked systems
138 same nuclei undergoing growth, fluctuation, dissolution, merging and/or division, which are regulate
141 fested by cytoskeletal remodelling, junction dissolution, migration and extracellular matrix turnover
142 after (57)Fe(II), suggesting that catalyzed dissolution occurred at or near the site of (57)Fe incor
147 the contribution of O(2)(*)(-) to reductive dissolution of AFO is dependent on conditions such as th
148 on of AFO by O(2)(*)(-) occurs following the dissolution of AFO, and hence, the contribution of O(2)(
151 echanism via which NOM affects the oxidative dissolution of AgNPs, (ii) the role of photogenerated or
152 d reactive oxygen species (ROS) in oxidative dissolution of AgNPs, and (iii) the mechanism of formati
153 the kinetics and mechanism of photoreductive dissolution of amorphous iron oxyhydroxide (AFO) in view
154 Dealloying typically occurs via the chemical dissolution of an alloy component through a corrosion pr
159 f their many components is the formation and dissolution of biomolecular condensates through liquid-l
160 red that permethylation affords the complete dissolution of both soluble and insoluble polysaccharide
161 disintegration, have emerged to explain the dissolution of Cahokia, the largest prehistoric populati
162 emonstrate, using a mathematical model, that dissolution of calcium that has aggregated within the mi
163 km/s correspond with growth of porosity from dissolution of chlorite, the most reactive of the abunda
165 Mn from the alloy appeared to discourage the dissolution of Cr in the molten fluoride salts which is
166 cs of acute hypoxia; (ii) the initiation and dissolution of distinct hemodynamic niches; (iii) tumor
167 cantly accelerate rates of ligand-controlled dissolution of Fe(III) (hydr)oxides at circumneutral pH.
169 clude that the catalytic effect of Fe(II) on dissolution of Fe(III)(hydr)oxides is likely important u
176 (>12 kyr-old) aquifer promotes the reductive dissolution of iron oxides and the release of arsenic.
177 w of the recognition that the light-mediated dissolution of iron oxides controls Fe availability in m
180 d where reducing alkaline conditions favored dissolution of iron-manganese- (Fe-Mn-) oxyhydroxides (w
182 e water irrigated areas, suggesting repeated dissolution of land applied fertilizer during recirculat
183 en no current is flowing, demonstrating that dissolution of lithium remains a critical issue for lith
184 to isotope exchange at the surface, with the dissolution of Lp by ligands accelerated by up to 60-fol
186 tics, reflecting the differential and faster dissolution of lumenal versus tissue-embedded coating ow
187 These results demonstrate that oxidative dissolution of magnetite can induce a rich array of stra
189 ew aims to elucidate nanospecific effects on dissolution of metallic NPs in freshwater and similar me
190 e catalyst enables the reversible growth and dissolution of micrometre-sized lithium oxide crystals t
194 rphology of dendritic cells and mediates the dissolution of podosomes, which dendritic cells use to a
195 phosphate and exchangeable Ca(2+) and/or (2) dissolution of poorly crystalline Fe and Al oxides by 1
196 nic interaction and silicate addition on the dissolution of pyrite, the major contributor to acid and
197 e, overexpression of laccase showed enhanced dissolution of quartz phases by etching and pitting.
198 Washout experiments confirmed the rapid dissolution of SGs, accompanied by normalization of TDP-
199 sport resulting from cultivation may enhance dissolution of SIC, altering their local stock at decada
201 cate addition also significantly reduced the dissolution of sphalerite or galena (by 10-44%, except a
204 The synthetic compound ink derived from the dissolution of the bulk binary precursors in the right s
205 iodide ions, thus preventing the consequent dissolution of the cathode-plated iodine as triiodides.
206 al gradients, in agreement with preferential dissolution of the crystallite core in acidic media.
207 d two release processes intracellularly: the dissolution of the dye aggregates into dye molecules and
208 ingle capsule or tablet, measurements of the dissolution of the entire multi-particle capsule or tabl
209 XX interactions saturate, which leads to the dissolution of the gel and the appearance of a liquid ph
213 th conventional voltammetric analyzer, after dissolution of the samples in microwave oven, and with a
217 he more disordered nanoparticles showing the dissolution of tin and platinum species during electroca
220 , and pore water chemical data, suggest that dissolution of V(III)-bearing magnetite, V(III)- and V(I
221 ntify a possible impact of calcium phosphate dissolution on the maintenance of F0F1-ATP synthase acti
224 le sample preparation step that consisted of dissolution or dilution of the samples in water, followe
227 educed corrosion resistance and increased Ti dissolution over 30 days of material aging as compared t
228 ripts are stabilized and stored until P-body dissolution permits transcript reentry into the cytosol.
230 ile other genomic regions promote condensate dissolution, potentially preventing aggregation of the l
231 d shear zones deforming via diffusion creep, dissolution-precipitation creep and grain boundary slidi
232 ine h-BNNS was achieved through a successive dissolution-precipitation/crystallization process in the
234 We accomplished this by inverting the drug dissolution problem: instead of measuring the increase i
236 LiMn(2) O(4) -like sub-nanodomain formation/dissolution process during each charge/discharge, which
238 solubility data, which demonstrated that the dissolution process is endothermic and non-spontaneous a
240 performance properties, and studies of their dissolution processes define the underlying aspects.
242 for pharmaceutical companies to obtain full dissolution profiles for drug products in a variety of d
243 sensor data revealed significantly different dissolution profiles for the different drugs, and in som
244 and fully-automated technique for obtaining dissolution profiles from single controlled-release pell
245 this technique to measure the single-pellet dissolution profiles of several commercial controlled-re
248 content, soil pH and moisture content on the dissolution rate and solubility of copper oxide nanopart
250 om 5.9 to 6.8 in LUFA 2.2 soil decreased the dissolution rate constant from 0.56 mol(1/3).kg(1/3).s(-
251 (<15 nm) was observed, leading to increased dissolution rate constants and solubility in some cases.
252 es C) is demonstrated here, showing that the dissolution rate of pyrite significantly changes with th
254 crystal, which has much lower solubility and dissolution rate than commercial powder reb B product.
256 suffers from poor aqueous solubility and low dissolution rate, which greatly limits its application,
258 pplied a simple empirical model to determine dissolution rates and a more complex kinetic model that
260 conditions to investigate the mechanisms and dissolution rates of biogenic, noncrystalline UO(2)(s) b
263 ed in the current study were lower than most dissolution rates reported for laboratory experiments, b
264 -type T. denitrificans and nitrate, UO(2)(s) dissolution rates were similar to those of abiotic exper
265 ural convective flows that, in turn, enhance dissolution rates, and simulations show that this feedba
266 siological needs of different biota, mineral dissolution rates, and substrate nutrient availability r
268 and single-cell analysis, we found that foci dissolution rather than formation promoted HSF1 activity
270 roscopy, revealing nonclassical pathways via dissolution-recrystallization of highly hydrated amorpho
271 as a simple anion exchange mechanism without dissolution-recrystallization or interstratification pro
273 nt, the Kirkendall effect, Ostwald ripening, dissolution-regrowth, and the surface-protected hollowin
279 y of protons, 2) better cycling stability by dissolution suppression, and 3) higher Coulombic efficie
280 ize this result, whereas two dynamic abiotic dissolution systems (one flow-through and one flow-by) i
282 can augment and potentially replace current dissolution tests and support product development and qu
284 inating from inhomogeneous Li deposition and dissolution, the formation of dendritic and/or dead Li l
286 bolic activity accelerates calcium carbonate dissolution to rates exceeding accretion by healthy cora
287 on relations between particle properties and dissolution/transformation characteristics of metal and
288 results signify an increased plant-mediated dissolution, uptake, and leaching of radioactive contami
289 M) and atomic force microscopy (AFM), and Ti dissolution via light microscopy and Inductively-coupled
290 2) S composites and inhibits the polysulfide dissolution via the TM S bond, effectively addressing th
292 s enthalpy, entropy and Gibbs free energy of dissolution were obtained using experimental solubility
294 s following amorphous solid dispersion (ASD) dissolution when the drug concentration exceeds the "amo
295 1k) and mPEG(2k)-LA(2).(7k) micelles favored dissolution whereas mPEG(5.4k)-LA(28.5k) micelles favore
296 e of thrombus, thus achieving efficient clot dissolution whilst minimising undesirable side effects.
298 d this work by studying isotope exchange and dissolution with lepidocrocite (Lp) and goethite (Gt) in
299 faces several challenges including complete dissolution with maximum therapeutic efficiency over a s
300 le cycles of 53BP1 repair foci formation and dissolution, with the first cycle taking longer than sub