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1 he aqueous phase) on isoamyl nitrite (in the organic phase).
2 t Nile Red becomes chemically "gated" in the organic phase.
3 dynamic barrier for the salt transfer to the organic phase.
4 cid-insoluble carbonate or a more refractory organic phase.
5 n of metal cations by the surfactants in the organic phase.
6 l and creating water-in-oil emulsions in the organic phase.
7 tion subsequently occurs entirely within the organic phase.
8 issipation in the interfacial portion of the organic phase.
9 complex in the aqueous phase and ANE in the organic phase.
10 ol in single water droplets dispersed in the organic phase.
11 approximately 59% of the uranyl ion into the organic phase.
12 nsfer catalyst" to bring silver ion into the organic phase.
13 ain either in the interphase or in the lower organic phase.
14 or of water monomers that penetrate into the organic phase.
15 es from the droplet slowly dissolve into the organic phase.
16 lorate or phosphate) from the water into the organic phase.
17 than expected diffusion coefficients for the organic phase.
18 to buffer the activity of protons within the organic phase.
19 rate and the degree of convection within the organic phase.
20 ion could be resolved with a high content of organic phase.
21 ution of model basic drugs among aqueous and organic phases.
22 ts of organic substances between aqueous and organic phases.
23 sulfur isotopic compositions in sulfide and organic phases.
24 s controlled by manipulating the aqueous and organic phases.
25 ine B from an aqueous phase (DI water) to an organic phase (1-octanol) were performed to determine th
26 tract hydrocarbon reaction products into the organic phase after a suitable incubation period, was de
27 phobic species dissolved or suspended in the organic phase along with the amphiphilic copolymer can b
28 s phase, whereas isoamyl alcohol forms a new organic phase along with the unreacted isoamyl nitrite.
30 , and fluorous molecules partition out of an organic phase and into a fluorous phase in a standard li
32 ological samples is to partition CoQ into an organic phase and separate it from contaminants by high-
33 ith the hydrophobic side oriented toward the organic phase and the hydrophilic side toward the water.
34 d transfers of potassium between aqueous and organic phases and complexation of potassium with dibenz
35 related with an increase in transport of the organic-phase anion tetraphenylborate, TPB-, and an incr
36 fers of hydrophilic ions between aqueous and organic phases are ubiquitous in biological and technolo
37 able to extract NH4NO3 from an aqueous to an organic phase, as inferred from (1)H NMR spectroscopic a
38 l4 ](-) ions through hydrogen bonding in the organic phase, as shown by EXAFS, mass spectrometry meas
39 uch as extractions of sugars from water into organic phase, as well as in homogeneous organic media,
40 form hydroxide ion bridged dimers within the organic phases, as indicated by a significant blue shift
41 how water structures and penetrates into the organic phase at two different liquid-liquid systems: th
42 pically pass with difficulty from water into organic phases because of water's superior solvation pow
43 e extracted from an aqueous solution into an organic phase by all of the perfluoroalkylated macrocycl
44 their rapid phase transfer to a butanol/TCE organic phase can be achieved by adding NaCl and creatin
45 a combination of photo-switching dopants and organic phase-change materials as a way to introduce an
47 for Pd-NZVI reacted with TCE in the butanol organic phase compared to Fe(II) oxides in the aqueous p
48 r mole of Fe(0)) from Pd-NZVI in the butanol organic phase compared to the same reaction with TCE in
49 onally, titration of active phenoxide in the organic phase confirmed the presence of both phenol and
50 ent and a weak carboxylic acid buffer and an organic phase containing an acidic organophosphorus extr
52 articles were homogeneously dispersed in the organic phase containing trimesoyl chloride prior to the
53 tic boundary between an aqueous phase and an organic phase, control was achieved on the micrometer to
54 s and the strongest four components from the organic phase, country of origin was correctly identifie
56 s and the strongest four components from the organic phase, designed to classify according to species
57 tivity, and influence of sample stirring and organic-phase diffusion coefficient on the response char
60 detector and accompanying flow cell for the organic phase enriched with the reaction product and (b)
62 e liquid chromatography fractionation of the organic phase extract, the PQH2 content was quantitative
65 ploration of its reactivity in the condensed organic phase has been hampered by the lack of an approp
71 abel an organic-in-water emulsion, where the organic phase is an ionic liquid [P6,6,6,14][FAP]/toluen
73 MF product is continuously extracted into an organic phase (methylisobutylketone) modified with 2-but
75 One of the most common combinations for the organic phase of dental restorative materials is BisGMA
76 a useful technology for imaging mineral and organic phases of bones and for assessing their spatial
78 s, where large diffusion coefficients in the organic phase often lead to substantial sample depletion
81 he dispersive solvent, proportion of aqueous/organic phase, pH and flow rates have been carefully eva
82 "dangling") OH group that protrudes into the organic phase, plays a key role in catalyzing reactions
83 ctions, and evaporative concentration of the organic phase prior to gas chromatography-mass spectrome
84 f dilauroylphosphatidylcholine (DLPC) to the organic phase produces an interface dominated by DLPC ad
85 tammogram of the O2(-) anion transfer to the organic phase provides a unique signature for unambiguou
86 ic compounds partition preferentially to the organic phase rather than the aqueous phase for the stud
87 ential electroosmotic pumping of aqueous and organic phase, respectively, from the solvent reservoirs
89 simulate absorption into the above-mentioned organic phases, respectively, whereas soot, ammonium sul
90 ctions between these water molecules and the organic phase result in substantial orientation of these
93 SOA formation is less sensitive than that of organic-phase SOA to atmospheric conditions that are not
95 erves as a semiseparation dimension using an organic-phase step-elution gradient in combination with
96 irmed by the fact that an immobile condensed organic phase such as PVC was protected from the photoca
102 ring directly the transfer of nitrate to the organic phase, the enhancement of transfer of the cation
103 eriments, when the volume ratio of insoluble organic phase to aqueous one was 2:1 and the reaction te
105 ation rate (kobs of 0.413 day(-1) in butanol organic phase versus 0.099 day(-1) in aqueous phase).
106 rged intermediates from the interface to the organic phase via favorable partitioning of hydrophilic/
109 of the tetraalkylammonium phenoxides in the organic phase was identified as the primary factor influ
113 ted geometric mean concentrations during the organic phase were generally lower for all children, and
114 erally leads to dissociated complexes in the organic phase when used as a diluent in extraction studi
115 tract peptides from aqueous solution into an organic phase, where the peptides bind to the interior f
116 croemulsion droplets that then formed in the organic phase, while the high MW target protein was excl
117 d-NZVI) when reacted with TCE in a 1-butanol organic phase with limited amounts of water results in 5
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