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3 directly image individual aluminum ions at a mica-water interface and show how adsorbate populations
4 fer solutions on the ionic conductivity of a mica surface was investigated to find appropriate condit
5 use monoclonal IgG, and glucose oxidase on a mica substrate has been accomplished by scanning electro
8 how contour lengths of the SWNT brushes on a mica surface from 200 nm to 2.0 microm and an average he
9 and detachments of two DNA tile systems on a mica surface imaged with an atomic force microscope (AFM
11 m studied is a double bilayer supported on a mica surface in which the top bilayer (which is not in d
12 lity of PIEZO1 under force in membranes on a mica surface, and show that PIEZO1 can be flattened reve
17 , dsDNA and nascent RNA were adsorbed onto a mica surface and imaged under continuously flowing buffe
18 e deposition process of DNA molecules onto a mica surface for imaging under the scanning force micros
20 oth ends of the molecule tend to attach to a mica substrate, probably due to their local positive cha
22 GroEL and GroES that have been adsorbed to a mica surface can be resolved directly by the AFM in aque
31 le cell adhesion strengths on Intersleek and mica, indicating that Navicula diatoms secrete extracell
34 s modulate the competition among quartz- and mica-dominated microscopic damage processes, resulting i
35 nitude of opposing forces between silver and mica surfaces (representing nanosilver and sand grains)
36 the formation of Fe(II)-bearing smectite and mica in 40 days, the most rapid process and first specif
39 olecules electrostatically immobilized on AP-mica and those photocross-linked on trioxalen-functional
43 film deposited on a rigid substrate such as mica, by the compression of a plastic polymer stamp with
44 ion between films or between a film and bare mica; however, addition of Ca(2+) and Fe(3+) induced sig
45 strates: hydrophilic negatively charged bare mica and positively charged 3-aminopropyl triethoxysilan
46 n monomers, while on negatively charged bare mica surfaces, it forms a film of monomers that exhibits
52 ing the acting intermolecular forces between mica and metal surfaces modified with self-assembled mon
55 information for understanding scCO(2)-brine-mica interactions in saline aquifers with different brin
57 ution of EDL structure at negatively charged mica-water interfaces, revealing transition from the Lan
60 polymer epitaxially grow on freshly cleaved mica substrates, and their in-plane and out-of-plane gro
63 DNA molecules deposited onto freshly cleaved mica, are able to equilibrate on the surface as in an id
67 ured the interactions between two tau-coated mica surfaces, whereas "asymmetric" experiments examined
69 used aminopropyltriethoxysilane-derivatized mica surface and permits resolution of structure on the
70 Illite in shales is a mixture of detrital mica and its weathering products with diagenetic illite
71 llite is a general term for the dioctahedral mica-like clay mineral common in sedimentary rocks, espe
72 DNA molecules deposited onto glow-discharged mica or H+-exchanged mica do not equilibrate on the surf
73 rk shows how a physical understanding of DNA-mica binding can be used to guide studies of the higher-
76 oplates deposited on mechanically exfoliated mica and highly ordered pyrolytic graphite flakes used a
77 ysis of the specific forces involved in film-mica interactions and the impact of ion ordering under e
78 ran (THF) and cyclohexane on atomically flat mica substrates, thus permitting a structural characteri
81 rials show that the choice of surface (gold, mica, glass, etc.) may be used to modulate the aggregate
82 e confinement in 2D materials like graphene, mica, or hexagonal boron nitride has been reported, thei
88 the results highlights that the hydrophilic mica surface used to image via liquid AFM and the high c
89 ansition accurately in strongly hydrophilic (mica) capillaries and remains qualitatively valid for we
92 luid-phase/ordered-phase domain structure in mica-supported bilayers composed of 1,2-dimyristoyl-sn-g
95 the Macusani Volcanic Field in Peru, lithium mica crystal clasts hosted by a tuffaceous mudstone repr
96 ighlighting volcanogenic-sedimentary lithium mica deposits as a promising exploration target in peral
97 rare-metal granites and pegmatites, lithium micas are increasingly considered a resource for lithium
98 icles (basalt, granite, hematite, magnetite, mica, milky quartz, and clear quartz) to quantify the ca
99 mples of RIM images of a synthetic membrane (mica with pores filled with the ion-selective polymer Na
101 l conductivity of proton-exchanged monolayer micas can reach above 100 S cm(-2) at 500 degrees C, wel
102 ltra-thin and environment-friendly muscovite mica which is the first time beta-Ga(2)O(3) epitaxy grow
103 indentation displacement bursts in muscovite mica are tuned by chemomechanical weakening in a manner
105 al nanoindentation, the surface of muscovite mica deforms by sudden stochastic nanometer-scale displa
109 PD is 4,4-difluoropiperidinium) on muscovite mica and fabricate a series of perovskite-perovskite ver
110 we use natural cleavage defects on Muscovite mica to investigate the activity of topographical featur
112 The adhesion of these molecules to muscovite mica in an aqueous electrolyte solution demonstrates tha
116 mic force microscope-derived phase images of mica, glass, and collagen under the same conditions as u
117 icroscopy, both AFM and NSOM measurements of mica-supported lipid monolayers reveal small domains on
118 enough to cause even dehydration melting of mica, the absence of hydrous minerals, and the match of
121 ngle Rb(+) and H3O(+) ions at the surface of mica in water using high-resolution atomic force microsc
122 two smooth and chemically inert surfaces of mica (a common alumino-silicate clay mineral) bridged or
123 n AFM cantilever and approaching surfaces of mica, gold, or polystyrene, we observed adhesion of the
124 The results suggest that the adhesion on mica is due to weak physical interactions rather than ch
126 rmine the structure of the water adlayers on mica at room temperature as a function of relative humid
128 1 and 30T both formed globular aggregates on mica surface, while 14T-1 also formed nanowires on graph
129 on between AFM data obtained on glass and on mica substrates show no major differences in image fidel
130 icroscopy to investigate S-layer assembly on mica, we show this concept is equally valid during self-
131 ylcholine (DPPC) supported planar bilayer on mica, formed by use of a modified vesicle fusion method
132 the effects of brine cation compositions on mica dissolution, surface morphological change, and seco
133 nanoliposomes with different compositions on mica surface was investigated using Atomic Force Microsc
134 action induces the "upright" conformation on mica, whereas the hydrophobic interaction favors the "fl
135 Ni(2+) ions adopt extended conformations on mica akin to those observed for DNA under similar condit
136 The self-assembly of these constructs on mica surfaces was studied with atomic force microscopy,
139 molecular weight hyaluronan was deposited on mica from dilute aqueous solution and imaged in air.
144 (patches of dipalmitolphosphatidylcholine on mica), and bacteriorhopsin membranes adsorbed to mica.
145 ntly labeled DNA molecules were dispersed on mica and analyzed using time-resolved fluorescence spect
149 epitaxial (4,4-DFPD)(2)PbI(4) array grown on mica via liquid-phase van der Waals epitaxy provides a p
150 th of DNA fragments, deposited and imaged on mica under buffer, was measured as a function of deposit
152 However, if DNA was partially immobilized on mica substrate individual strands with dark foci were st
156 hylammonium bromide (C(18)TAB) monolayers on mica was investigated using atomic force microscopy and
158 tu experimental study of CaCO3 nucleation on mica (muscovite) and quartz, which allows us to obtain t
159 f adsorbed surfactant tubules is observed on mica and graphite substrates, whereas a random arrangeme
160 s, suggesting that conformations observed on mica surfaces may differ significantly from those that p
161 iments on supported lipid bilayer patches on mica are reported to demonstrate the validity of this ap
162 We also show that the epitaxial pattern on mica is ensured by the lattice matching between the anis
164 ormed by wetting and de-wetting processes on mica surfaces at different states of hydration by tappin
165 led to extended self-assembled structures on mica: designed end-to-end interactions produced micromet
168 he surface forces apparatus, we show that on mica surfaces Mefp-5 achieves an adhesion energy approac
170 th very different morphologies, "upright" on mica and "flat" on the highly oriented pyrolytic graphit
172 nts showed that mfp-1 can adhere well to one mica surface, but is unable to then link to another (unl
175 nd in which DNA molecules were adsorbed onto mica strongly enough to be imaged, but loosely enough to
176 aqueous polyethylenimine (PEI) adsorbed onto mica substrates, which has a large concentration and the
178 rgets in solution and, after adsorption onto mica surfaces, can be examined by atomic force microscop
180 ening these vesicles and adsorbing them onto mica to form small, < or =120 nm, largely flat sheets we
181 tached to force microscope tips and opposing mica surfaces in configurations that would either favor
182 confined graphene in comparison with gold or mica surfaces because of specific interactions of the el
183 components such as exfoliated vermiculite or mica platelets have been intensively studied and commerc
185 , formed coacervates that spread evenly over mica, and strongly bonded to mica surfaces (pull-off str
186 ngstrom-wide tubular channels that perforate micas' crystal structure, which, after ion exchange, con
187 esion was most widely observed on phlogopite mica, silica, and calcite surfaces with roughness on the
190 ription assays, performed with radiolabeled, mica-bound transcription complexes, confirmed this rate,
191 containing saponite, talc-saponite, Fe-rich mica (for example, glauconite-nontronite), Fe- and Mg-se
192 d varying topography (mechanically roughened mica and stacked bilayers of dipalmitolphosphatidylserin
195 distance profiles indicate that, when silver-mica systems were exposed to HA, osmotic-steric, electro
196 Hydrocarbon films confined between smooth mica surfaces have long provided an experimental playgro
198 ce of the atomic force microscopy substrate (mica) and the probe, and the interaction between anchore
199 ges of PG-1 on a highly hydrophilic surface (mica) show fibrils with morphological similarities to Ab
200 n, which is observed on model clay surfaces, mica, but not on silica surfaces nor for monovalent K(+)
206 heir height (approximately 1-3 nm) above the mica surface; their lateral dimensions (width and length
207 s of Fn film continued to increase after the mica surface was completely covered, consistent with Fn
209 we have investigated hydration forces at the mica-electrolyte interface as a function of ion valency
210 redicts that hydrolyzed species dominate the mica-water interface, even when unhydrolyzed species dom
211 (vs. Ag|AgCl electrode in solution) for the mica-nickel confined interface of total area approximate
213 es above the recessed hydroxyl groups in the mica lattice, although hypotheses based on hydrated ioni
216 l, the initial surface charge density of the mica surface was determined to be -0.022(1) C/m(2) at pH
217 incommensurate interface between one of the mica surfaces and the laterally ordered solid molecular
219 ely half of the complexes are raised off the mica surface by approximately 1 nm relative to the rest.
220 of intermediate structures 'trapped' on the mica as partially formed toruses of nucleoprotamine.
223 humidity to form a thin film of water on the mica surface that allows electrochemical reactions to ta
224 f colloidal particles (per unit area) on the mica surfaces derived from the retentates increased by a
227 t favorable adsorption of uranyl ions to the mica interface through strong ion-dipole or hydrogen int
228 f the DNA was first allowed to attach to the mica prior to addition of the protamine, well-defined to
229 were contained in one leaflet distal to the mica substrate through qualitative binding experiments w
230 sation is attributed to weak adhesion to the mica surface, counterion-mediated attractive electrostat
231 hat in rotary shadowing the contact with the mica caused a distortion of the protein, weakening the b
232 sine of sufficient length interacts with the mica substrate and phospholipids to create the stationar
237 ble, Mfp3 slow, like Mfp3 "fast" adhesion to mica, is directly proportional to the mol % of Dopa pres
239 mall DNA fragments spontaneously adsorbed to mica and imaged in situ in the presence of divalent ions
241 croscopy of recombinant proteins adsorbed to mica, we show that NSF, the oligomeric ATPase involved i
247 elected transition metal salts, DNA binds to mica tightly enough to be directly imaged in the buffer
248 ead evenly over mica, and strongly bonded to mica surfaces (pull-off strength: approximately 17.0 mJ/
250 om Rhodopseudomonas acidophila were bound to mica surfaces at 300 K and examined by observing their f
251 ethanol on the structure of DNA confined to mica in the presence of Mg2+was examined by varying the
252 n metal cations that effectively bind DNA to mica are Ni(II), Co(II), and Zn(II), which have ionic ra
256 , individual molecules bind independently to mica in the designed orientations, whereas at high K(+)
260 fluid-mobile lithophile elements relative to micas in other volcanogenic and intrusive units in the M
263 Surface Forces Apparatus (SFA), between two mica surfaces fully covered by the polymer demonstrate t
264 ed (i) in the "symmetric" system between two mica surfaces that had been rendered hydrophobic by the
265 The alpha' was 24 mJ/m(2) for the vaterite-mica system and 32 mJ/m(2) for the vaterite-quartz syste
266 e first transferred onto van der Waals (vdW) mica substrates and converted to 2D Janus sheets by surf
268 rphism), and subsequent hypidioblastic white mica (arguably Carboniferous/Permian, Alleghenian orogen
269 resent dates of 257 detrital grains of white mica from this succession, using the 40Ar-39Ar method, a