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1 at it is experimentally possible to tune the frictional/adhesion properties of a CNT by controlling t
2  show that the earthquake triggered aseismic frictional afterslip on the subduction megathrust, with
3 icroscopy experiments that instead show that frictional ageing arises from the formation of interfaci
4 ependent increase of frictional strength, or frictional ageing, is one manifestation of the 'evolutio
5 tions occur between particles in addition to frictional and elastic forces.
6 by these agents and resisted by interleaflet frictional and tensile stresses.
7 ossibly in general, relies critically on the frictional anisotropy of their scales.
8 el that relates structural directionality to frictional anisotropy reveals that isotropy enhances mov
9 ffold bound to the underlying tube creates a frictional barrier for lipid diffusion; tube elongation
10       In general, along-strike variations in frictional behavior appear to persist over multiple eart
11 , here we identify three distinct regimes of frictional behavior for polyacrylic acid (PAA), polyacry
12                     This direction-dependent frictional behavior is found to correlate strongly with
13 s the data, and is capable of explaining the frictional behavior of faults, across the full range of
14 utive laws are extensively used to model the frictional behavior of faults.
15 ocument a transition from unstable to stable frictional behavior with increasing slip velocity, provi
16  the USL delineates the zone of transitional frictional behavior.
17  achieved, which, in turn, affect the system frictional behavior.
18         Recently, it has been found that the frictional behaviour of two-dimensional materials exhibi
19 ly 0.001 at pressures to over 100 atm, has a frictional behaviour resembling that of articular cartil
20                  This relation suggests that frictional buttressing loss, which increases spreading,
21 udes, and higher run-up; moreover, depth and frictional changes affect tide, surge, and wave characte
22  force microscopy, we compared the nanoscale frictional characteristics of atomically thin sheets of
23 ed transverse mechanical properties, surface frictional characteristics, and chemical resistance demo
24                      The estimated effective frictional coefficient along the Nobeoka Thrust after th
25                                              Frictional coefficient calculations suggest that telomer
26 c in solution and exhibits an unusually high frictional coefficient consistent with the extended, mul
27  in solution as an asymmetric monomer with a frictional coefficient of 1.48 and a Stokes radius of 23
28 he approximation of a single, weight-average frictional coefficient of all particles, determined from
29                                          The frictional coefficient ratio (f/f(0)) of 1.28 calculated
30 edimentation coefficient of 3.96 Svedberg, a frictional coefficient ratio (f/f(0)) of 1.60, and a hyd
31                                          The frictional coefficient was calculated to be 1.7 indicati
32 ce the total mass of the particle, hence its frictional coefficient, f, directly related to its shape
33  is significantly more asymmetric than TFF3 (frictional coefficients 1.25 and 1.12, respectively, p <
34 parently decreased, whereas the ratio of the frictional coefficients is increased.
35 okes radii of 44 and 51 A, respectively, and frictional coefficients of 1.6 and 1.8, respectively).
36    Rrp1 and Rrp1-C274 are both monomers with frictional coefficients of 2.2 and 1.4, respectively.
37 ungarotoxin binding had little effect on the frictional coefficients of AChBP measured by analytical
38 e monitored by CE because differences in the frictional coefficients of the hairpin and coil forms of
39    Further analysis of the Peclet number and frictional coefficients suggested that condylar cartilag
40 to the total mass of the particles and their frictional coefficients, f.
41 tures formation are discovered under extreme frictional conditions which trigger self-organization.
42 ould enable us to formulate physically based frictional constitutive laws, rather than the current em
43 er, there are many situations where multiple frictional contact points between two surfaces are "acti
44  stiff building blocks interacting mainly by frictional contact.
45 o scattered sound pull particles into direct frictional contact.
46            Our results support the idea that frictional contacts are created between jammed particles
47  rest or shearing slowly, repulsion prevents frictional contacts from forming between particles, wher
48 tion despite seemingly ineffective isotropic frictional contacts.
49                                              Frictional contrast is inverted and magnified at loads a
50 onal results independently indicate that the frictional contributions of multiple, coupled but well-s
51 sional mobility in membranes, which includes frictional coupling across an interstitial water layer.
52                     We furthermore find that frictional coupling between local normal stress variatio
53 in the model, we estimate the coefficient of frictional coupling between T Cell receptors or LFA-1 an
54  retrograde flow in the cortex together with frictional coupling between the filopodial and cortical
55                          Ligand mobility and frictional coupling of receptors to the cytoskeleton wer
56 in-generated tension on one hand, and on the frictional coupling of the ligand-receptor complexes wit
57 raint revealed switching between two states: frictional coupling to retrograde flow and Arp2/3-depend
58     We discuss a sorting mechanism, based on frictional coupling to the actin cytoskeleton, that is c
59 form and exceeded the rate expected for pure frictional coupling with the overlying mucus layer; henc
60 ism and its dependence on the solute-solvent frictional coupling.
61       The 2 tissues also exhibited different frictional dependencies on sliding speed and normal load
62                 Here we show that jamming of frictional, disk-shaped grains can be induced by the app
63                      A substantial amount of frictional dissipation in the atmosphere occurs in the m
64 ing to experimental turnover, the calculated frictional dissipation of less than k(B)T per rotation i
65          A torsional viscoelastic model with frictional dissipation quantitatively reproduces the dyn
66               However, the resulting overall frictional dissipation remains small (compared to the vi
67 gle of the modulus (representing fluid-solid frictional dissipation) increased 15-fold from 55 Hz in
68                    The stripes and resulting frictional domains appear on monolayer and multilayer gr
69               Here we demonstrate that these frictional domains derive not from structural features i
70 owing us to create arbitrary arrangements of frictional domains within a single flake.
71 be due to atmospheric jet streams and/or low frictional drag at the bottom of the atmosphere.
72 owth patterns are related to a time evolving frictional drag between the moving charged glass particl
73 re calculated by multiplying their estimated frictional drag coefficients with their velocities relat
74              A growing aggregate experiences frictional drag forces exerted on it by fluid moving ove
75 o an electron-hole plasma abruptly, and only frictional drag is observed.
76                                              Frictional drag measurements, performed inside a bespoke
77 investigated the effect of shear stress, the frictional drag of blood flowing over the cell surface,
78 an enthalpy input and surface dissipation by frictional drag, can physically connect the LMI to LI.
79  results are fundamentally important to both frictional dynamics and the dynamics of earthquakes with
80 ble and unstable failure, and is governed by frictional dynamics via the interplay of fault frictiona
81 e solvent viscosity, and dry friction, where frictional effects arise due to the interactions within
82                                              Frictional effects due to the chain itself, rather than
83                                              Frictional, electronic, and other associated phenomena a
84 ently conjugated to three unique polypeptoid frictional end labels and mixed together.
85 , we conclude that the damping is related to frictional energy dissipation during interfacial sliding
86 layer breathing modes in the layer-dependent frictional energy dissipation process of graphene layers
87 ntional triboelectric nanogenerator converts frictional energy into electricity by producing alternat
88                Some earthquakes may occur by frictional failure owing to high pore pressure that migh
89 es on the subduction interface-effectively a frictional failure response to the driving stress.
90 tile transition, where high pressures render frictional failure unlikely.
91 to 10/s, comparable to seismic velocities of frictional fault surfaces.
92 observe a transition from growth of a single frictional finger to simultaneous growth of multiple fin
93 ntinuum model based on the simple notions of frictional flow and tension-free separation describes co
94 hanics of undulatory swimming in a "granular frictional fluid" and compare the predictions to our pre
95 es that the noninertial swimming occurs in a frictional fluid.
96  show Piezo1 (Fam38a) channels as sensors of frictional force (shear stress) and determinants of vasc
97               By measuring the change in the frictional force above the protein nanopatterns as a fun
98 isposed areas, hemodynamic shear stress, the frictional force acting on the endothelial cell surface
99 ocity, the slope of the relation between the frictional force and velocity was nearly fivefold larger
100 cally, Coulomb drag has been attributed to a frictional force arising from momentum transfer whose di
101 y an applied electric field is balanced by a frictional force arising from their frequent collisions
102  vertical pipe jacking machine and soil, the frictional force between follow-up pipes and soil, and g
103  additive thrust of the jacking machine, the frictional force between vertical pipe jacking machine a
104         We also show that a reduction of the frictional force by orders of magnitude, associated with
105                    Flowing blood generates a frictional force called shear stress that has major effe
106                    Here, we demonstrate that frictional force characteristic of flow in the lymphatic
107                   Between these regimes, the frictional force decreases by an order of magnitude and
108              Endothelial cells transduce the frictional force from blood flow (fluid shear stress) in
109    Decreased cell stiffness and cell-surface frictional force leads to an increase in transportabilit
110 ntact line friction, which characterizes the frictional force on the contact line.
111 odynamic stimulus of fluid shear stress, the frictional force produced by blood flow.
112                       Flowing blood exerts a frictional force, fluid shear stress (FSS), on the endot
113                  Circulating blood generates frictional forces (shear stress) on the walls of blood v
114 sponse to the entropic, electrophoretic, and frictional forces acting on it.
115                 The endothelium senses these frictional forces and, in response, releases various vas
116 erefore be crucial in three dimensions where frictional forces are likely to be modest.
117 undled F-actin filaments, we show that these frictional forces are unexpectedly large, scale logarith
118 e limits on the static and dynamic interwall frictional forces between nested nanotubes.
119 ar relationship between trajectory shape and frictional forces between pili and the surface: strong p
120                                        These frictional forces critically regulate vascular function.
121 ted to shear, the system shows extremely low frictional forces dependent on the salinity of the mediu
122 ogically relevant range, which confirms that frictional forces dominate during sand-swimming by the s
123 l relative to those from solvent, so solvent frictional forces drive the folding process.
124 n this model will enable detailed studies of frictional forces in more complex biomimetic systems, pr
125 ht energy into mechanical energy to overcome frictional forces in the environment, providing insight
126                                 We find that frictional forces increase nonlinearly with MAP velocity
127                   Shear stress caused by the frictional forces of a fluid moving over a cell monolaye
128 try conditions are met at the same time: the frictional forces of each body against the surface must
129                                              Frictional forces originating from random solvent and pr
130 ty-dependent proteasome gating kinetics that frictional forces originating from random solvent motion
131                   The adhesion, cohesion and frictional forces present during the removal of dry mud
132 ce (TIRF) microscopy to directly measure the frictional forces produced by the mitotic crosslinking p
133 f the transduction channels produce internal frictional forces that can dominate viscous drag on the
134 h enough to outrun adaptation, we found that frictional forces were maximal within the narrow region
135 nally described using only gravitational and frictional forces within a granular material.
136  attracting water to the surface, overcoming frictional forces, and reducing surface tension.
137 ntly by solvent-derived rather than internal frictional forces.
138 ions, the concerted motions result in higher frictional forces.
139 stress variations, and identify a predictive frictional formulation that captures this effect.
140 ea, the nature of the jamming transition for frictional grains is less clear.
141 red static structure and chaotic dynamics of frictional granular matter has occupied scientists for c
142                                              Frictional healing is one such property, which describes
143 mineralogical criteria to quantify coseismic frictional heat in natural faults at temperatures lower
144 f a few tens of centimeters in production of frictional heat.
145 welts begin to form when the average rate of frictional heating exceeds 0.1-0.4 MW m(-2), while the a
146                                    In UHPLC, frictional heating from the eluent flowing through the c
147 at of crystallization as well as viscous and frictional heating in areas of strain localization.
148 tures and mineralogical changes to constrain frictional heating on the fault plane.
149                                     Further, frictional heating results in axial thermal gradients of
150  in line with local current contrasts, while frictional imaging indicates qualitative variations in t
151 recognized as being the result of stick-slip frictional instabilities.
152 e conditions for the emergence of stick-slip frictional instability-the mechanism for earthquakes-by
153                 Evidently, information about frictional interaction is embedded within neural mechani
154 mework accounting for the material-dependent frictional interaction of water molecules, ions and the
155  impulse due to each bounce we find that the frictional interaction with the surface is strongly enha
156                                              Frictional interactions are considered at the interface
157 s illustrated significant dissipation due to frictional interactions at the exit.
158         Because sieve tube structure defines frictional interactions in the tube system, the presence
159 ous object appears within a context implying frictional interactions with another rotating object; vi
160 entation plays a key role in determining the frictional interactions, thus offering the chance to spe
161 between the membrane and substrate dominates frictional interactions, which enables determination of
162                              We analyzed the frictional interface between necessary cost containment
163 the population of microjunctions forming the frictional interface between two solids is central to fi
164         Sliding at a quasi-statically loaded frictional interface can occur via macroscopic slip even
165 e within kinetochores and a separate passive frictional interface located at least 20 nanometers away
166        We introduce a microscopic model of a frictional interface that includes asperity-level disord
167                                              Frictional interfaces are found in systems ranging from
168 in both active, force-producing and passive, frictional interfaces with microtubules whose relative l
169 ating in the hydrolysis direction under high frictional loads and low ATP concentrations, a coordinat
170 h R712G and F750L were less able to overcome frictional loads measured in the loaded motility assay.
171                                       At low frictional loads, the 120 degrees steps alternate with t
172 cumulate tectonic stress more easily in long frictional locking periods, large earthquakes are theref
173 hat thermal losses are more significant than frictional losses at lower Reynolds number.
174                                     However, frictional losses dominate over thermal losses at higher
175 nherent inefficiencies are attributed to (i) frictional losses required to overcome hydraulic resista
176  trajectory of each particle, and the entire frictional, many-degrees-of-freedom system, organizes it
177 ion of force chains in both frictionless and frictional materials from the undeformed structure, with
178 ased attachment force 600-fold above that of frictional measurements of the material.
179 ol the stability of mineral phases and hence frictional-mechanical processes associated with earthqua
180                           This generalizable frictional mechanism may act in concert with other hypot
181 gradual transition between the tunneling and frictional mechanisms.
182 nts of the scallop theorem can be escaped in frictional media if two asymmetry conditions are met at
183 ecorded by the presence of pristine quenched frictional melt.
184             These data are consistent with a frictional model of TCR coupling to cytoskeletal flow, w
185 ide motion using a rate- and state-dependent frictional model that incorporates a nonlocal stress bal
186 aults and tremor, contrary to predictions of frictional models of tremor.
187                                              Frictional motion between contacting bodies is governed
188  accelerating rupture fronts at the onset of frictional motion by performing high-temporal-resolution
189 o-called bimaterial interfaces, the onset of frictional motion is often mediated by highly localized
190 s elucidated by a mathematical model for the frictional motion of the colony interface, with friction
191                     The most general type of frictional motion takes place when the two bodies are no
192 tion delivered via a spontaneously migrating frictional nasojejunal tube, or to continued nasogastric
193 rgranular repulsion and its influence on the frictional nature of granular contacts is central to thi
194 rve at the elbow results in a tractional and frictional neuritis with classical symptoms of periphera
195 icant pumping energy is required to overcome frictional pressure losses in the spacer-filled feed cha
196 s to the conductive Pt-coated tip during the frictional process.
197 er not only the evolution of plate interface frictional processes but also the dynamic boundary condi
198 thquake motion and the most general types of frictional processes.
199                                 However, the frictional properties and conditions that sustain these
200 ee-energy profiles are quasiharmonic and the frictional properties correspond to highly overdamped mo
201         We find that lithologic contrasts in frictional properties do not necessarily determine the l
202                                          The frictional properties of individual carbon nanotubes (CN
203 on apparatus to elucidate the effects of the frictional properties of objects during initial contact.
204                        Laboratory studies of frictional properties of rocks at slip velocities approa
205 ms behind these remain enigmatic because the frictional properties of shallow subduction zones, usual
206 ical approaches do not provide access to the frictional properties of suspensions.
207            We propose that the structure and frictional properties of the overthrusting plate control
208 ur with injury that appear to compromise the frictional properties of the tissue.
209 d cutaneous afferent encoding of skin-object frictional properties on the basis of three findings.
210  with a model in which spatial variations in frictional properties on the plate interface control tre
211 ches are confounded by a cell's size and its frictional properties with the channel wall.
212 -grain contacts and the resulting changes in frictional properties, as empirically described by rate-
213 ictional dynamics via the interplay of fault frictional properties, effective normal stress and the e
214 subduction earthquakes are influenced by the frictional properties, structure, and composition of the
215 o a wide range of object shapes, weights and frictional properties, to provide optimal and secure han
216 etermined by cell stiffness and cell-surface frictional property, and can be used to probe tumor hete
217                               From this, the frictional ratio (f/f(0)) of sCR1 was calculated to be 2
218     Compact Lp(a), i.e., native Lp(a), had a frictional ratio (f/f0) of 1.2 that was independent of a
219 hat (i) Pol32 is a rod-shaped protein with a frictional ratio f/f(0) = 2.22; (ii) any complex contain
220 a value of 2.0 S at zero concentration and a frictional ratio f/f(o) of 1.2 for both allotypes.
221 34 +/- 0.17 S, which for M = 110 000 gives a frictional ratio f/f0 = 3.2 +/- 0.3.
222 The approximation of a single weight-average frictional ratio is favored by several experimental fact
223  bound detergent and lipids and a reasonable frictional ratio of 1.5, corresponding to a Stokes radiu
224  showed that it is highly asymmetric, with a frictional ratio of 1.66.
225 , a sedimentation coefficent of 6.5 S, and a frictional ratio of 3.01, the sec180e protein appears to
226 incorporated in the form of a weight-average frictional ratio of all species, or in the form of prior
227 ation coefficient of s(20,w)(0)=3.58 S and a frictional ratio of f/f(0)=1.62 indicate an asymmetric s
228 mates of the partial specific volume and the frictional ratio of the macromolecules are used to calcu
229  studied the influence of the weight-average frictional ratio on the quality of the fit, and found th
230 lations based on the classical translational frictional ratio showed that the protein was highly asym
231 tokes radius, sedimentation coefficient, and frictional ratio, and assayed their stability to trypsin
232 istribution of sedimentation coefficient and frictional ratio, c(s,f(r)), which is representative of
233 MALDI mass spectrometry (44.2 kDa) yielded a frictional ratio, f/f(0), of 1.47.
234 coefficient, s(o)(20,w), of 2.71 S yielded a frictional ratio, f/f(0), of 1.65.
235 sedimentation coefficient of 8.5 S and has a frictional ratio, f/f(omicron), of 1.35; these data are
236 he native and activated polysaccharide, with frictional ratio, intrinsic viscosity, sedimentation con
237 ct meniscus position, and the weight-average frictional ratio.
238                                              Frictional ratios calculated from D(z) and molecular wei
239 ii, low sedimentation coefficients, and high frictional ratios, all characteristic of asymmetry which
240                         This new approach to frictional reduction has broad implications for manufact
241 g between local normal stress variations and frictional resistance actually promotes the interface se
242 hBP, the toxin molecules should increase the frictional resistance and thereby alter the hydrodynamic
243 in normal stress, demonstrate that the shear frictional resistance exhibits a significant lag in resp
244 ndings reveal how nonmotor MAPs can generate frictional resistance in dynamic cytoskeletal networks v
245 nding earthquake hazard since laws governing frictional resistance of faults are vital ingredients in
246                 A range of insights into the frictional resistance of faults-one of the main factors
247                                          The frictional resistance on a fault during slip controls ea
248                   Temporal variations of the frictional resistance on subduction-zone plate boundary
249 on is facilitated by along-fault low dynamic frictional resistance, which is controlled by a number o
250 ssional events had suggested the presence of frictional resistance.
251 ions drifting in a buffer gas have a minimal frictional resisting force, whereas the resisting force
252  proteins can also be regenerated, and their frictional response is reproducible through several malt
253                      A low density of weakly frictional rollers congregates near the sharp leading ed
254 l observations of the interaction of dynamic frictional ruptures with fault (double-) bends of differ
255  local contact temperature, and reducing its frictional shear strength.
256 p-protein interaction, therefore causing the frictional signal to change.
257  edge whereas a denser rear comprises highly frictional sliders.
258 ture with depth precludes brittle failure or frictional sliding beyond a few tens of kilometers, yet
259  heating, just as is sometimes the case with frictional sliding in the crust.
260 he overall commensurability) also evolves in frictional sliding on graphene.
261 hesion and wetting to substrate and ultralow frictional sliding structures.
262 zones, indicating the potential for unstable frictional sliding within natural lawsonite layers.
263 ides (very smooth fault surfaces polished by frictional sliding).
264                                     To model frictional sliding, we introduce a nonlinear viscosity t
265 channel between two parallel planes to model frictional sliding.
266                                              Frictional slip between bodies having different elastic
267  prograde tectonic strain is accommodated by frictional slip on many preexisting faults.
268 constitutive law captures oriented mesoscale frictional slip, microcrack opening, and splitting with
269 ches quickly build force and fail (so-called frictional slippage), whereas at low substrate stiffness
270 he substrate appreciably (a second regime of frictional slippage).
271 he model predicts two distinct regimes: (i) "frictional slippage," with fast retrograde flow and low
272 ovides a good representation of the evolving frictional state during stick-slips.
273    In the tactile sense such constraints are frictional stick-slip events, occurring, amongst other v
274                Earthquakes normally occur as frictional stick-slip instabilities, resulting in catast
275  contacts causing a large reduction in fault frictional strength (i.e., flash weakening).
276 lts are difficult to observe directly, their frictional strength can be estimated indirectly by const
277        This discovery is significant, as the frictional strength of talc at elevated temperatures is
278              This time-dependent increase of frictional strength, or frictional ageing, is one manife
279 re weak when compared to laboratory-measured frictional strength.
280 ns of layer-dependent friction and transient frictional strengthening on graphene.
281 r numerical models, which simulate different frictional strengths in the transform and fracture zone,
282                                 However, the frictional strengths of serpentine minerals are too high
283                        Here we show that the frictional stress between two sliding surfaces bearing s
284             For small strain rates there the frictional stress is essentially independent of the mate
285 mic efficiency eta was 0.036 and the minimum frictional stress was 550 bars.
286 cilitated by high-temperature fluids, reduce frictional stresses and promote failure.
287 s an empirical approach to the behavior of a frictional surface.
288 d: iliopsoas bursitis (IPB), iliotibial band frictional syndrome (ITBFS), and Achilles tendinopathy.
289 lume fraction of the particles approaches in frictional systems the random loose packing limit, varph
290 ulses in realistic rate- and state-dependent frictional systems.
291                                              Frictional tests with a migrating contact area were perf
292 ogy, provide direct evidence that the recent frictional transition scenario applies in real suspensio
293 or nuclear and cell mechanics that shows how frictional transmission of stress from the moving cell b
294 perficial bullous lesions following incident frictional trauma to the skin.
295 superficial bullous lesions that result from frictional trauma to the skin.
296 -defined nanometer pores and can exhibit low frictional water flow inside them, making their properti
297                   The results imply that the frictional weakening in granular materials and the inter
298                                  Inspired by frictional weakening mechanisms thought to operate durin
299                                          The frictional work directly extracted from particles' veloc
300  force hypotheses in grains arise from local frictional yielding, revealing a novel invariance within

 
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