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1  discharge from the surrounding grounded ice sheet.
2 ds, can contain a significant amount of beta-sheet.
3 antized triangular nanopores through an h-BN sheet.
4 elerated future retreat of the Antarctic Ice Sheet.
5 eractions with proteases at the end of the A-sheet.
6 ase (matrix phase) in a pre-stretched Nafion sheet.
7 thic two- or three- strand antiparallel beta sheet.
8  (CASE) Index, alongside the background data sheet.
9 te as an extra beta-strand in a central beta-sheet.
10 ysis biomechanics in peptide aptamers and GO sheets.
11 ulated interconnected network of tubules and sheets.
12 nanoparticles encapsulated by large graphene sheets.
13 M, which indicated attachment of NR on po-Gr sheets.
14 twist angle in bilayer and trilayer graphene sheets.
15 crobial sanitization with scalable, flexible sheets.
16  the fibril axis into tight self-associating sheets.
17 particles directionally sintered into porous sheets.
18 uds (cellular aggregates) to epithelial cell sheets.
19 outhern Ocean as a consequence of larger ice sheets.
20 usions specifically enriched in amyloid beta-sheets.
21 f electron delocalization through the 2D COF sheets.
22 gment, 15-25 WT, forms non-toxic labile beta-sheets.
23 rticles on the 2D carbon nanomaterial planar sheets.
24 ntrollable, antibiotic-releasing nanofibrous sheets.
25 ystalline powders and exfoliated micron-size sheets.
26 ucture when interacting with extended silica sheets.
27 )), H-bonded parallel- and antiparallel-beta-sheets (1690cm(-1)) and H-bonded beta-turns (1664cm(-1))
28 milarly, reactive center loop insertion into sheet A decreased heparin binding because it disturbs th
29 o assess relationships between Antarctic ice-sheet (AIS) dynamics, climate change and sea level.
30 -bonded molecules stacked in an antiparallel sheet alignment.
31  [URE3] are folded in-register parallel beta-sheet amyloids of Sup35p and Ure2p, respectively.
32 ices act as a transient intermediate to beta-sheet and fibril formation of pEAbeta (3-42).
33                        We used lattice light-sheet and quantum dot-enabled synaptic contact mapping m
34 ical in the cytosol and acquires a more beta-sheet and random coil character in the nucleus.
35  stitching image columns, pivoting the light-sheet and sectioning the heart mechanically, we establis
36 rt survey composed of the respondent profile sheet and the Social Skills Inventory.
37 conjugation into the combined graphene oxide sheets and are responsible for the highly conductive nat
38 cated icosahedron and fabricated on flexible sheets and further folded either into a concave or conve
39 es (ca. 3 nm in size), together with the rGO sheets and in situ generated amorphous carbon that serve
40  FAM134B, responsible for the turnover of ER sheets and SEC62 that regulates ER recovery following st
41 ive proteins are often formed by curved beta sheets, and the ability to control beta-sheet curvature
42 phase shift of the perfectly modulated light sheet are demonstrated.
43 scopy and X-ray analyses have shown that the sheets are crystalline.
44                          Graphene oxide (GO) sheets are mixed with the aptamer-QDs.
45 trate this concept, planar and 3D-structured sheets are preprogrammed to evolve into bio-inspired sha
46 tional angles in a freestanding bilayer MoS2 sheet as directly observed using an aberration-corrected
47  engraving of polymethyl methacrylate (PMMA) sheet as off surface matrix was integrated in very close
48 nsitive to the history of the Laurentide Ice Sheet as the coastline lies along the ice sheet's periph
49 an electrochemical immunosensor employing Au sheet as working electrode, Fe3O4 magnetic nanoparticles
50 allography reveals that the macrocyclic beta-sheet assembles to form double-walled nanotubes, with an
51 vide non-covalent cross-linking through beta-sheet assembly, reinforced with a polymer backbone to im
52                       The respondent profile sheet assessed demographic profile and social media use
53 sheets were deposited on 1.00mm thick copper sheet at 850 degrees C using acetylene (C2H2) as carbon
54 protein that folds into an antiparallel beta-sheet at the A/W interface and presents strong intermole
55 the melting history of the Fennoscandian Ice Sheet at the end of the last deglaciation ( approximatel
56 t) anomaly was reported in the Greenland ice sheet at the Younger Dryas boundary (YDB) (12,800 Cal B.
57 ermining the relative stability of different sheets at a given doping level.
58 of the nanostructures or their internal beta-sheet backbone, but must involve accessible adaptive con
59                                        Light-sheet-based fluorescence microscopy (LSFM) features opti
60 proximately 345 K, above which the Te square sheets become disordered with no q-vector.
61 atterns, in which crease folding requires no sheet bending, and random patterns with high-energy fold
62 terns with high-energy folding, in which the sheet bends as much as creases fold.
63  via the formation of an intermolecular beta-sheet between the membrane-proximal (third) Fibronectin
64 stable clothes by inserting the bent polymer sheets between two fabrics.
65 the peptide in its active form within silica sheets by interface-specific vibrational spectroscopy in
66 obility exceeding 2000 cm(2) V(-1) s(-1) and sheet carrier density above 1.07 x 10(13) cm(-2) .
67                      Cultured epidermal cell sheets (CES) containing undifferentiated cells are usefu
68 argeted helix-(pi-sheet)-helix and helix-(pi-sheet)-coil assemblies occur without compromising intrin
69  assemblies, a mix of sequence-defined helix-sheet-coil and helix-sheet-helix architectures, are Natu
70 accurate coupling between atmosphere and ice sheet components in climate models.
71 apeptides transform from alpha-helix to beta-sheet conformation.
72                                  Stable bent-sheet conformations were shown to prevail in chlorinated
73 ing a beta hairpin and an anti-parallel beta sheet consisting of strands from the top and bottom mole
74 y and variable levels of intermolecular beta-sheet content in their protein shells.
75 25 degrees C for 18min exhibited higher beta-sheet contents and more chemical bonds such as hydrophob
76                     The alpha-helix and beta-sheet contents decreased, while aggregated beta-sheet, t
77 modeling studies have suggested that the ice sheet contribution to future sea level rise could have b
78 ese oligomers undergo an alpha-helix to beta-sheet conversion catalyzed by lipid vesicles and disrupt
79  due to the ability of the non-covalent beta-sheet cross-links to reassemble, the hydrogels can self-
80 ange from multi-beta-strand barrels, to beta-sheet cups and baskets covered by alpha-helical lids, to
81 investigated the mechanisms controlling beta-sheet curvature by studying the geometry of beta sheets
82  the computational models, showing that beta-sheet curvature can be controlled with atomic-level accu
83 beta sheets, and the ability to control beta-sheet curvature would allow design of binding proteins w
84                       Moreover, the graphene sheets dampen capillary waves such that rotational aniso
85 e, we report the synthesis of MoS2 monolayer sheets decorated with isolated Co atoms that bond covale
86 odulation spectroscopy to reveal a bipolaron sheet density >10(10) cm(-2) at the interface between an
87 ra were erupted though the center of the ice sheet, deposited near WAIS Divide and preserved in the W
88 ted beta-sheets with an increased inter-beta-sheet distance and a higher solvent exposure than WT-alp
89 mical measurements in the West Antarctic Ice Sheet Divide, Byrd, and other ice cores to document a un
90 ic interactions between residues in the beta-sheet domain that reduce the width of the cavity.
91  in regions between the alpha-helix and beta-sheet domains.
92 entary Fe sources, such as the Antarctic ice sheet, due to the difficulty of locating and interrogati
93 andmasses were covered by the Laurentide ice sheet during the Last Glacial Maximum (18,000 years befo
94 st vulnerable part of the West Antarctic Ice Sheet, during the Holocene epoch (from 11.7 thousand yea
95 hat the MPT was initiated by a change in ice sheet dynamics and that longer and deeper post-MPT ice a
96                    We argue that neither ice sheet dynamics nor CO2 change in isolation can explain t
97  loess sedimentation rate, Fennoscandian ice sheet dynamics, and sea level changes is proposed.
98 y (and then possible feedback) and ocean-ice sheet dynamics, respectively, rather than simple propaga
99 posite direction to the movement of a single sheet electron beam bunch in the experiment.
100 w, and present a challenge for modelling ice-sheet evolution and projecting global sea-level rise fro
101 s is in contrast to the expectation that ice sheets expand in colder climates and shrink in warmer cl
102       Loss of HSP hairpin proteins causes ER sheet expansion, partial loss of ER from distal motor ax
103                                        Light-sheet fluorescence microscopy (LSFM) serves to advance d
104                                        Light-sheet fluorescence microscopy and optical projection tom
105                            Multicolour light sheet fluorescence microscopy provided information about
106 ic microparticles, in both cases using light-sheet fluorescence microscopy to optically access the in
107 esign can be manufactured using origami-like sheet folding and bonding methods.
108 ne aminated peptides that readily adopt beta-sheet folds.
109 try.With the use of the FAOSTAT food balance sheets for Australia, the per capita availability of add
110 odified titanium with and without epithelial sheet formation.
111 es cluster on the inner strands of both beta-sheets forming the fibronectin domains.
112 t a six-helix bundle and a six-stranded beta-sheet, forms a genome-delivery apparatus and joins 89 co
113 their main role is to protect the epithelial sheet from external mechanical strain, how HDs respond t
114         Transplantation of limbal epithelial sheets from explant cultures is one of the standard trea
115 offshore Svalbard to constrain a coupled ice sheet/gas hydrate model, we identify distinct phases of
116                    To determine whether cell sheets generated with long-term passaged (P10) aging hum
117 tive biosensor employing graphene oxide nano-sheets (GO), multiwalled carbon nanotubes (MWCNTs), and
118  of the chondriod callus in the aged P10 MSC sheet groups was significantly larger than in P3 MSC she
119 oups was significantly larger than in P3 MSC sheet groups.
120 sibly associated to hot spots or whole Fermi sheets) has a strong mass enhancement at the QCP, and th
121       We demonstrate that targeted helix-(pi-sheet)-helix and helix-(pi-sheet)-coil assemblies occur
122  sequence-defined helix-sheet-coil and helix-sheet-helix architectures, are Nature-inspired synthetic
123 degree of regioselectivity, leading to a low sheet homogeneity (Hsheet).
124                   The space was divided into sheets (i.e., space between two parallel membranes) and
125 the ventricle from high resolution 4-D light sheet image data.
126             Here, we introduce lattice-light sheet imaging of MDA-MB-231 human breast cancer cells ge
127 ping zebrafish embryos by coupling 4-D light sheet imaging with a stabilized finite element flow solv
128 ential partial collapse of the Antarctic ice sheet in assessing future coastal inundation.
129  Heinrich events, but also suggests that ice sheets in contact with warming oceans may be vulnerable
130 t curvature by studying the geometry of beta sheets in naturally occurring protein structures and fol
131  the mutant proteins assembled into tubes or sheets instead of capsids.
132           We used confocal and lattice light sheet instrumentation and an imaging informatics pipelin
133  cylindrical sheet into a flower, and a flat sheet into a complex canyon-like structure.
134  numerically simulating the growth of a flat sheet into a face, a cylindrical sheet into a flower, an
135 h of a flat sheet into a face, a cylindrical sheet into a flower, and a flat sheet into a complex can
136 te that the distal end of the antithrombin A-sheet is crucial for the last steps of protease inhibiti
137                       The West Antarctic Ice Sheet is one of the largest potential sources of rising
138 the volume of the present East Antarctic Ice Sheet is required to explain many of the approximately 1
139               The most unique feature of the sheets is DNA-directed surface addressability, which is
140 ite in agitated solutions, the size of these sheets is generally limited due to fragmentation along f
141 and of nAu and pi* continuum of polyaromatic sheets is likely to dominate on 700 degrees C biochar.
142 by altering the geometry and topology of the sheet itself.
143  persisting up to and beyond a 100-nanometer sheet length.
144 their C-terminal, self-assemble to form beta-sheet like structures upon mixing.
145 ated, and some connected to needle-shaped or sheet-like cholesterol crystals.
146       To engineer heterotelechelic PPVs in a sheet-like design, we engineer an iterative one-pot cros
147 characteristic novel phenotype consisting of sheet-like invaginations of the sarcolemma.
148 le, where the oil remained connected in thin sheet-like layers in the narrower regions of the pore sp
149 -COF, with a hexagonal layered structure and sheet-like morphology, is synthesized.
150 d structures, in particular, those emulating sheet-like structural aspects using poly(p-phenyleneviny
151                                        Their sheet-like structure derives from two independent polyme
152 y, while both parallel and antiparallel beta-sheet-like structures are realized.
153 nd projecting global sea-level rise from ice-sheet loss.
154 se to an earlier perturbation in driving ice-sheet loss.
155 alcites from close to the East Antarctic Ice-Sheet margin, which together suggest that volcanically-i
156 ximately 25% increase in total Greenland ice sheet mass loss ( approximately 1.4 m sea-level equivale
157  and predicting the impacts of Antarctic Ice Sheet melting concerns the vertical distribution of the
158               We demonstrate the first light sheet microscope using propagation invariant, accelerati
159 l expression of GCaMP6s, combined with light sheet microscopy and a novel image processing pipeline,
160 lism was visualized by multiphoton and light sheet microscopy in cultured bovine hair follicles and p
161                This implementation for light sheet microscopy opens up new possibilities across a wid
162 on-uniform refractive index, extending light-sheet microscopy to partially cleared samples.
163          We therefore employed lattice light sheet microscopy to perform three-dimensional, time-laps
164 C-DSLM (cleared tissue digital scanned light-sheet microscopy) as a low-cost method intended to autom
165 mbination of 1) single-objective based light-sheet microscopy, 2) photoconvertible proteins, and 3) f
166                                  Using light-sheet microscopy, early neural development is here follo
167   By quantitative fluorescence lattice light-sheet microscopy, we have shown that ESCRT-III subunits
168 o neighboring patches embedded in a cortical sheet, mimicking the two digit regions, were costimulate
169             Using a standard 3-stranded beta-sheet model, the WW domain, it was found that the pH swi
170                         Earth-system and ice-sheet modelling suggests these contrasting trends were l
171                            However, most ice-sheet models estimate basal traction from satellite-deri
172 lower-resolution data currently used for ice-sheet models, these data show a contrasting topography a
173  in the predictive capability of current ice-sheet models.
174  two complementary pentapeptides from a beta-sheet motif of a protein, being connected to an aromatic
175 no acid interactions in an antiparallel beta-sheet motif.
176      Each cell within a polarized epithelial sheet must align and correctly position a wide range of
177 adable carbon-based electrodes onto a single sheet of paper, and demonstrate its use as a shock senso
178 mensional molecular aggregate (2DMA), a thin sheet of strongly interacting dipole molecules self-asse
179 ells connect via cell-cell junctions to form sheets of cells with separate cellular compartments.
180  curvatures, which shape growing volumes and sheets of cells.
181 es and cell stiffness both in cell pairs and sheets of cells.
182 acrophyte Fucus vesiculosus with laser light sheets of defined spectral composition, while imaging va
183 f slices were wrapped in special three-layer sheets of packaging material, some with a coating of REO
184     Basement membranes (BMs) are thin, dense sheets of specialized, self-assembled extracellular matr
185 om coil structure, evolves into ordered beta-sheet oligomers containing at least 5 strands, and then
186 cial physicochemical features, including the sheet-on-sheet sandwich-like structure, ultrathin nanosh
187  baseline intervention forms and 274 outcome sheets one year later (31%).
188 Fe(II) into predominantly-Fe(III) octahedral sheets or through the adsorption of Fe(II) onto the mine
189 sessed how Fe(II) residing in the octahedral sheets, or Fe(II) adsorbed at the edge sites alters redo
190 om thin peptide films shows features of beta-sheet ordering for both peptides, along with evidence fo
191 d reporter assay in Drosophila ovary somatic sheet (OSS) cells [1].
192 We propose that the appearance of larger ice sheets over the past million years was a consequence of
193 he experimentally observed antiparallel beta-sheet packing.
194 ircuit model is established and the graphene-sheet pattern is designed optimally for maximizing the r
195                         By altering the beta-sheet peptide graft density and concentration, we can ta
196               This self-healing polymer-beta-sheet peptide hybrid hydrogel with tailorable mechanical
197 17 of IAPP (RLANFLV) into a macrocyclic beta-sheet peptide results in a monomeric peptide that does n
198 onalization of its repeating units with beta-sheet peptides to form a hydrogel, it can easily be modi
199 ross-linked via grafted self-assembling beta-sheet peptides to provide non-covalent cross-linking thr
200                                          Ice sheets play a more important role in the global silicon
201 vity, we treated partially oxidized graphene sheets (po-Gr) with NR to obtain po-Gr-NR dispersion by
202 eta-sandwich fold, with the face of one beta-sheet possessing the beta-1,3-glucan-binding surface.
203  Pt anomaly is consistent with Greenland Ice Sheet Project 2 (GISP2) data that indicated atmospheric
204 l hydration network are observed in the beta-sheet protein.
205 , pi-stacking interactions with the graphene sheets provide further pi-delocalization that improves t
206 oduction of a disulfide bond in the bridging sheet region further stabilized the closed conformation
207 se results reveal the importance of the beta-sheet region of lysozyme for initiating self-assembly in
208 s (I476 and V482) were within coiled or beta-sheet regions in domain B distant to the active site.
209 e material in which the alpha-helix and beta-sheet regions of the protein are similar to crystal grai
210        A 28-nanometer-thick gold foil with a sheet resistance of 7 ohms per square showed only a 4% i
211                 The resulting fibres display sheet resistance values as low as 600 Omegasq(-1), demon
212 eport on angle-dependent measurements of the sheet resistances and Hall coefficients of electron liqu
213 etreat may have been a highly non-linear ice sheet response to relatively continuous external forcing
214 th of both NiFe-LDH and carbon in one single sheet results in fully integrated amorphous NiFe-LDH/C n
215      At 3 weeks after transplantation of MSC sheets, results showed more bony callus formed between a
216             We infer rapid and sustained ice-sheet retreat driven by MICI, commencing around 12,300 y
217 ervational evidence that rapid deglacial ice-sheet retreat into Pine Island Bay proceeded in a simila
218  sequestration and subsequent release on ice sheet retreat that led to the formation of a suite of se
219 native-like properties and convert into beta-sheet-rich amyloid-like structures, as indicated by thei
220 ordered, monomeric alpha-synuclein into beta-sheet-rich oligomers and fibrils is associated with mult
221                 We suggest that enhanced ice sheet runoff is primarily associated with albedo effects
222 ce Sheet as the coastline lies along the ice sheet's peripheral bulge.
223 icochemical features, including the sheet-on-sheet sandwich-like structure, ultrathin nanosheets with
224 C), inflowing warm Atlantic Layer water, ice sheet, sea-ice and ice-shelf feedbacks, and sensitivity
225 haracteristic 2D IR features of amyloid beta-sheet secondary structure are created by as few as four
226 cited antibodies to the peptide and the beta-sheet secondary structure conformation.
227 selected to specifically react with the beta-sheet secondary structure of pathological oligomeric con
228  of which reflects the curvature of the beta-sheet segment.
229                                     The beta-sheet self-assembles to form long fibrils with the hydro
230 n vitro and is a major signal for cross-beta-sheet self-association of the 49-mer Phe521Leufs peptide
231 el prefers alpha-helical sequences over beta-sheet sequences.
232 ealed that this protein contained three beta-sheets, seven alpha-helices, and coils.
233                                          The sheet size is on the order of 5 x 5 mum(2).
234  the last glacial period, the Laurentide Ice Sheet sporadically discharged huge numbers of icebergs t
235 mphasize the importance of the ocean for ice sheet stability under the current changing climate.
236 c reticulum (ER) is a network of tubules and sheets stretching throughout the eukaryotic cells.
237 dic region of Ng peptide pries open the beta-sheet structure between the Ca(2+) binding loops particu
238 stinct from the intermolecular parallel beta-sheet structure observed in mature fibrils.
239 ze that NUCB1 binds to the common cross-beta-sheet structure of protofibril aggregates to "cap" and s
240 face region and the extended two-dimensional sheet structure within the nanoframe that minimizes the
241           As a result of their distinct beta-sheet structure, 1-108-alphaS fibrils resist incorporati
242 hydrogen bonding, including an extended beta-sheet structure, as well as aromatic interactions.
243 eracts with the stalk to form a compact beta-sheet structure.
244 sitely charged ionic segments that form beta-sheet-structured hydrogel assemblies via polyion complex
245 ortionation with structural Mn(IV) may alter sheet structures by forming larger and distorted Mn(III)
246 ics in general are more retarded around beta-sheet structures than alpha-helical motifs.
247 urn-helix architectures in which helical and sheet subcomponents conserve their respective integrity.
248 re proteins consist of three sequential beta-sheet subdomains that bind to specific carbohydrates to
249 y different approach to produce nanopores in sheet substrates under dry, ambient conditions, using na
250 with peptides aligned perpendicularly to the sheet surfaces.
251 elop an ultra compact, high resolution light sheet system without beam scanning.
252 se who wish to develop and use bespoke light-sheet systems and to assist in identifying the best appr
253 hin the eastern sector of the Laurentide Ice Sheet than traditional reconstructions for this interval
254 plex 3D structures starts with an epithelial sheet that is patterned by inductive cues that control t
255 ly for the crafting of high aspect ratio, 2D sheets that are densely surface-decorated with DNA.
256  The peptide forms amphiphilic parallel beta-sheets that assemble into stacked bilayers with alternat
257 evealed altered packing arrangements of beta-sheets that encompass residues 139 and 186 of PrP(Sc).
258 ontrol two counterpropagating coherent light sheets that generate excitation patterns in the focal pl
259  to be composed of thin (<0.75 microm), flat sheets that sometimes interleave to form rosettes.
260 hrough intermolecular hydrogen bonds to beta-sheets thereby placing the azide and alkyne motifs in pr
261 of the largest glaciers of the Greenland Ice Sheet; these have been major contributors to ice loss in
262 ice-shelf collapse may have caused rapid ice-sheet thinning further upstream-and since the 1940s.
263          When placed into the turn of a beta-sheet, this leads to a pH switch of folding.
264 e of meltwater across the surface of the ice sheet through surface streams and ponds (hereafter 'surf
265 ates and shells, we constrained flat elastic sheets to adopt fixed curvature profiles.
266 trated in this article, the redesign of beta-sheets to contain a global, or local, pH-dependent confo
267 y, the aptamer-conjugated QDs bind to the GO sheets to form a GO/aptamer-QDs ensemble.
268 unit interface, altering the packing of beta-sheets to induce changes that lead to asynchronous pore-
269 used so far for modification of 2-D graphene sheets to make is three-dimensional.
270                  The sensitivity of past ice sheets to volcanic ashfall highlights the need for an ac
271  highlighting the sensitivity of ancient ice sheets to volcanism is scarce.
272 sheets with a previously unobserved silicate sheet topology that contains the uncommon cyclic Si3O9 t
273 et contents decreased, while aggregated beta-sheet, turns and random coil contents increased as tempe
274 roscopy can identify the highly ordered beta-sheets typical of amyloid secondary structure even if th
275 d superconducting symmetrically bonded AuHAu sheets under compression.
276 ed the effect of bending aromatic amide beta-sheets using building blocks that impart curvature.
277 rect electropolymerization of graphene oxide sheets via oxidation of the phenol edge groups on graphe
278 ogical data show that the West Antarctic Ice Sheet (WAIS) advanced to the eastern Ross Sea shelf edge
279                       The West Antarctic ice sheet (WAIS) is highly vulnerable to collapsing because
280 ilar to that observed beneath the extant ice sheet, was also active during the last glacial period.
281 gments flanking a central bent aromatic beta-sheet were then synthesized and shown to form well-defin
282                                 The graphene sheets were deposited on 1.00mm thick copper sheet at 85
283 ubglacial basin before continental-scale ice sheets were established about 34 million years ago.
284 d monomers to alpha-helices and then to beta-sheets when the proteins encounter the cell membrane, an
285 abilized by apolar side chains from adjacent sheets, whereas the hydrated polar interface houses the
286 chelic PPVs is used to realize a parallel pi-sheet, wherein further orthogonal assembly with helical
287 e in the major groove while inserting a beta sheet 'wing' into the adjacent minor groove.
288 igned based on decorated graphene oxide (GO) sheet with alumina (Al2O3) nanocrystals.
289 hrough the decoration of either faces of the sheet with gold nanoparticles through sequence-specific
290 molecular dynamics simulations of perforated sheets with a dense periodic array of holes and observe
291 EO6 and REO2F4 polyhedra connected by Si4O10 sheets with a previously unobserved silicate sheet topol
292                           Programmable stiff sheets with a single low-energy folding motion have been
293              We combined graphene oxide (GO) sheets with a specific peptide aptamer to create a novel
294 haS fibrils consist of strongly twisted beta-sheets with an increased inter-beta-sheet distance and a
295                        The design of protein sheets with architecture and physical properties suitabl
296 s were electrospun to form elastic polymeric sheets with fiber diameters ranging from 350 to 1100 nm
297 rbon stacks is composed of well-preserved 2D sheets with highly accessible interlayer macropores, nar
298 nd Sc atoms, we show evidence for 2D Mo1.33C sheets with ordered metal divacancies and high electrica
299 he materials and verify the presence of beta-sheets within the hybrid hydrogels.
300 e ends in both young P3 MSC and aged P10 MSC sheet-wrapped groups when compared to allograft alone.

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