ライフサイエンスコーパス: crystallite

1 served at the surface and inside the growing crystallite.

2 3 A and can assemble in bilayer and trilayer crystallites.

3 point defects and the size of the graphitic crystallites.

4 to induce formation of larger donor polymer crystallites.

5 results in a gradual reduction of the Li2O2 crystallites.

6 ular hemoglobin and convert it into hemozoin crystallites.

7 he surface indicates nanostructured lamellar crystallites.

8 decay, depending on the size of the Se nano-crystallites.

9 size of and rotational disorder between the crystallites.

10 ayer, decorated with structurally related 3D crystallites.

11 ork as the driving force for the twisting of crystallites.

12 are effectively suppressed by the nanoscale crystallites.

13 stallites until they interlock with adjacent crystallites.

14 on within its protein layers between apatite crystallites.

15 tivated diffusion of water in and out of the crystallites.

16 formed via a merger of individual rod-shaped crystallites.

17 lated to the length scale of the polyalanine crystallites.

18 causes massive changes in the shape of lead crystallites.

19 ntal measure of properties of the nucleating crystallites.

20 dried on the ZnSe crystal contains silk III crystallites.

21 to other scattering sources like the mineral crystallites.

22 structure aligned with elementary cellulose crystallites.

23 within amorphous regions between polyolefin crystallites.

24 cts with spontaneous self-rotation of chiral crystallites.

25 of common corn and potato starches to C-type crystallites.

26 heme which is rapidly converted to hemozoin crystallites.

27 olved imaging at the nanoscale on individual crystallites.

28 antially increase the fraction of 2D surface crystallites.

29 es and fluctuations on the surface of the 2D crystallites.

30 elt interface with the growth of the Se nano-crystallites.

31 e coupled 1:1 by electron conduction through crystallites.

32 yields enamel with disordered hydroxyapatite crystallites.

33 arated and electronically decoupled graphene crystallites.

34 anneling through the pores of polymeric nano-crystallites.

35 ctating the size and symmetry of the growing crystallites.

36 c ice leads to the formation of more compact crystallites.

37 e of the seed undergo nucleation to form new crystallites.

38 bedded with nanosized hydroxyapatite mineral crystallites.

39 le size, suggesting detection limits down to crystallites 100 nm in diameter under low magnification

40 A mean crystallite ~ 50 nm size is evidenced by TEM analysis.

41 ssue composed of thousands of hydroxyapatite crystallites aligned in parallel within boundaries fabri

42 nal interfaces in nanocomposites like grain, crystallite and phase boundaries.

43 Birefringence, B-type crystallites and acid hydrolysis decreased on HMT.

44 ally heterogeneous sample with nm-sized LGPS crystallites and amorphous material.

45 butions from acid layers associated with the crystallites and ionic aggregates dispersed in the amorp

46 nctions form between high-bandgap 2D surface crystallites and lower-bandgap 3D domains.

47 rbonate and silica, and over the assembly of crystallites and other nanoscale building blocks into co

48 DNA-directed assembly of nanoparticles into crystallites and polycrystalline aggregates.

49 ically, mineral rods (at tens of mum scale), crystallites and prisms (at mum and sub-mum scale), and

50 Tanzanian fossils are formed from fibre-like crystallites and show archeopyles and exquisitely constr

51 Here, we demonstrate how motions of crystallites and the defects between them can arise with

52 to control the nucleation and growth of COF crystallites and their self-assembly to desired COF nano

53 ength scales smaller than 100 nm (individual crystallites) and greater than 50 um (multiple rods) are

54 sizes/concentrations, rounded shapes/surface crystallites, and co-association with non-physiological

55 ng structure at the interface of neighboring crystallites, and this method holds special significance

56 Affected crystallites appeared more radiolucent and morphological

57 However, the CF mouse enamel crystallites appeared to have a rough granular surface c

58 Nafion crystallites (approximately 10 vol%), which form physica

59 k distribution of RuDCBPY centers within MOF crystallites are also estimated with the use of confocal

60 de-supported crystallites, where the rodlike crystallites are either oriented largely normal to the e

61 orescence spectroscopy revealed that the COF crystallites are highly emissive compared to their respe

62 ults unambiguously demonstrate that hemozoin crystallites are identical to synthetic beta-hematin.

63 The crystallites are isometric with markedly rough surfaces

64 arp 4.7 A reflections indicate that the beta-crystallites are likely to be elongated along the H-bond

65 This suggests that the beta-crystallites are nearly hexagonally packed.

66 TEM analysis reveals that Pt crystallites are not perfect cubooctahedrons, and that l

67 n the catalyst is oxidized at 1073 K, the Pt crystallites are oriented with respect to the underlying

68 The magnetic crystallites are the end result of a progression from a

69 ues, where either amorphous films or faceted crystallites are the norm.

70 These crystallites are weakly bound to the crystal surface and

71 O(2) surfaces and 17 unique Li(2)O surfaces; crystallite areal fractions were determined through appl

72 The ACP ribbons convert into hydroxyapatite crystallites as the ribbons elongate.

73 The shape factor of the crystallites, as determined by SAXS, showed a continuous

74 ize, and lattice parameter of hydroxyapatite crystallites) associated with a pigmentation line in den

75 or cinchonidine chiral molecules from their crystallites asymmetrically adsorbed on the complex surf

76 We find that stacking-disordered critical crystallites at 230 kelvin are about 14 kilojoules per m

77 is based on light scattering by the nascent crystallites at 340 nm and monitors mineral formation at

78 tructures that assemble into two-dimensional crystallites at the air-water interface.

79 fundamental microstructural elements of the crystallite being formed, such as surface orientation or

80 state, even with atomic resolution, despite crystallites being submicrometer in size.

81 genin antibodies localized amelogenin to the crystallites but not to the inter-crystalline spaces.

82 d shown to have resulted in shrinkage of the crystallites by approximately one-third in a direction p

83 is optically active, and a study of several crystallites by Mueller matrix microscopy shows that the

84 ocations, and the regions between individual crystallites, called grain boundaries, act as obstacles

85 Due to the pillared nature, the crystallites can be exfoliated into nanosheets by sonica

86 be systematically controlled by varying the crystallite characteristics, for instance dimensions and

87 The crystallite clusters seemed to diffuse from the IOL inte

88 An estimation of an isobaric thermal crystallite coefficient, k , analogous with the isobaric

89 ise to superlattices with less strain in the crystallites compared to traditional designs.

90 reement with preferential dissolution of the crystallite core in acidic media.

91 es that the structure of nanometre-sized ice crystallites corresponds to that of hexagonal ice, the t

92 Consequently, the Si-rich crystallites could form, float and be sedimented to the

93 res constructed from layered two-dimensional crystallites could prove to be advantageous.

94 nal analysis of the preferred orientation of crystallites (crystallographic texture) involves X-ray d

95 CFTR knockout mice have enamel with crystallite defects, retained protein, and hypomineraliz

96 istinct effects work synergistically to bias crystallite deformations toward a subset of the availabl

97 n growth the preferred orientation of sodium crystallites depends on film thickness.

98 show highly increased population of face-on crystallite despite intrinsic crystallinity of polymers.

99 The conditions present during enamel crystallite development change dramatically as a functio

100 hin starch granules, suggestive of imperfect crystallite development.

101 By tuning the average crystallite dimension in the film from tens of nanometer

102 ts are found to be comparable to the typical crystallite dimensions seen in scanning electron microsc

103 ch consist of a network of anthradithiophene crystallites dispersed in an amorphous matrix composed p

104 inlet air temperature, percentage of inulin crystallite dispersion and Q content were studied on the

105 ed to parboiling, which was an indicative of crystallites disruption.

106 chiometric H2O provides a 4-fold increase in crystallite domain areas, representing the first rationa

107 ses are characterized as a function of COF-5 crystallite domain size in four different samples, which

108 The graphene fibers exhibit a submicrometer crystallite domain size through high-temperature treatme

109 conia growth and morphology by embedding the crystallites during seeding and growth.

110 ns that are mechanically processed into beta-crystallites during thread formation.

111 This implies that stacking-disordered ice crystallites either are more stable than hexagonal ice c

112 ved by controlled orientation of the polymer crystallites enabling the most efficient and fastest cha

113 During enamel maturation, hydroxyapatite crystallites expand in volume, releasing protons that ac

114 Increasing Sn contents within MFI crystallites facilitates Pt sintering and, thus, occurri

115 tion of the longer alkanes with polyethylene crystallites, first of all, reveals three preferred poly

116 t number fluctuations mediated by motions of crystallites, five-seven defects pairs, and grain bounda

117 hology and composition of 3 nm M0.1Ce0.9O2-x crystallites for CO oxidation catalysis and other applic

118 Enamel crystallites form in a protein matrix located proximal t

119 ering is used to investigate the kinetics of crystallite formation during and shortly after spin cast

120 The crystallite formation process was compared with respect

121 obic interactions, water exclusion, and beta-crystallite formation required to produce strong insolub

122 iting different crystallization pathways and crystallite formation times from minutes (CN, DPE) to 1.

123 ic function of guiding enamel hydroxyapatite crystallite formation.

124 ns that are believed to guide enamel mineral crystallite formation.

125 d near indents and that they are the same as crystallites formed during annealing without deformation

126 roscopy showed that the segment long spacing crystallites formed from the intermediate state were ide

127 sts of parallel arrays of elongated apatitic crystallites forming an intricate three-dimensional micr

128 Crystallites from fish are morphologically diverse and s

129 sed quantum dots (GQDs) by extraction of the crystallites from the amorphous matrix of the GO sheets.

130 ory of grain boundary (the interface between crystallites, GB) structure has a long history(1) and th

131 PSi crystallites generated from p-Si exhibit a hole-depletio

132 meloblastin overexpression influences enamel crystallite habit and enamel rod morphology.

133 These findings suggest enamel crystallite habit and rod morphology are influenced by t

134 ing assembly of matrix proteins that control crystallite habit.

135 Most of these crystallites have dimensions less than 100 nm and would

136 ine-grained (mostly < 2 mum) high Mg-calcite crystallites (i.e., > 4 mole % MgCO(3)) are their domina

137 rous individual microparticles and tenacious crystallites in a flowing water environment.

138 rved adjacent to partially dissolved apatite crystallites in dentin treated with the 15% 10-MDP prime

139 The crystallites in DI-II dentin, on the other hand, remaine

140 g the radiation induced formation of Se nano-crystallites in pure Se and in binary AsSe(4) glass-form

141 The ability to stabilize very small Pt crystallites in supported-metal catalysts following hars

142 ze, so that the size distribution of zeolite crystallites in the combined population may be tuned, fo

143 , pore anisotropy, and dimensions of titania crystallites in the films.

144 namel formation, enamelin is found among the crystallites in the rod and interrod enamel and comprise

145 he critical step is the formation of the ice crystallite, indicating that the mechanism is classical.

146 d enamel organization by altering protein-to-crystallite interactions and crystallite stacking while

147 t the interface can be composed of nanoscale crystallites interleaved by a web of interfaces that com

148 s to stratify the explorations of a bcc-CsCl crystallite into orthogonal directions according to disp

149 Each crystallite is composed of several orthogonal unit cells

150 The growth of enamel crystallites is assisted by enamel proteins and proteina

151 of individual molecules and nanometre-sized crystallites is defined by large intensity fluctuations,

152 tion regarding the orientation of individual crystallites is obtained by noting how the polarization

153 he preparation of mono-disperse, defect-free crystallites just 1-10 nm in size, ways to control the s

154 adsorption and diffusion of H2O into CuPcTs crystallites leads to a mixed CuPcTs-H2O phase at RH > 6

155 ating frozen particles that contain multiple crystallites leads to Ostwald ripening and annealing of

156 lvent additive 1,8-diiodooctane, show donor "crystallite" length scales on the order of 15-35 nm and

157 the coexistence of ordered surface water and crystallite-like ice structures, evident in the superpos

158 In addition, SEM images revealed crystallite-like structures on the dynamically loaded me

159 The vaterite crystallites making up the spherulites have excellent re

160 le of crystallite more stable than hexagonal crystallites, making their ice nucleation rates more tha

161 ripening, while larger NCs sinter slowly by crystallite migration and coalescence.

162 mation in the bulk, resulting in 1-3 nm iron crystallites mixed with amorphous LiF.

163 experimental evidence favours the competing crystallite model in the case of amorphous silicon(2-4).

164 m network, but resembles the competing (nano)crystallite model(6).

165 0 kelvin are about 14 kilojoules per mole of crystallite more stable than hexagonal crystallites, mak

166 pectroscopy (EDS), were used to characterize crystallite morphology and composition.

167 ttivity variation with variations in the ITO crystallite morphology and relative concentrations of di

168 mechanical exfoliation where single-layer 2D crystallites must be prepared through an exfoliation pro

169 res that give rise to the orientation of dye crystallites naturally extend to colorless molecular cry

170 lthough the orientational order of cellulose crystallites normal to the plane of the cell wall has no

171 of specific polymorphs, and promoted further crystallite nucleation over a period longer than 40 min

172 f enamel formation when nucleation of enamel crystallites occurs.

173 talytic system was established by depositing crystallites of a mesoporous metal-organic framework (MO

174 because the former possessed double-helical crystallites of a more compact structure.

175 First we show that crystallites of a photoacid generator function as microp

176 d amorphous aggregates and only occasionally crystallites of close-packed micrometre-sized particles.

177 Crystallites of different sizes were clearly visible fro

178 important finding was that individual enamel crystallites of erupted teeth failed to grow together, i

179 mission electron microscopy revealed 2-10 nm crystallites of fcc-UO(2) or alpha-UO(3) depending on th

180 nt opens porosity in the overcoat by forming crystallites of gamma-Al2 O3 .

181 ted a new deep learning pipeline to classify crystallites of hBN based on coarse thickness classifica

182 rrelative spectroscopies, that the nanoscale crystallites of hydroxylapatite (Ca(5)(PO(4))(3)(OH)), w

183 agnetic charges embedded in pseudo-ice, with crystallites of magnetic charges whose size can be contr

184 X-ray diffraction data revealed that crystallites of MoS(2) and WS(2) films are highly orient

185 is shell region, nanostructures comprised of crystallites of ovalbumin self-assemble into a well-defi

186 erconnected (approximately 4-nm in diameter) crystallites of RuO2, supported conformally on the nanos

187 as a mixed structure consisting of graphitic crystallites of sp(2) hybridized carbon and amorphous re

188 Efficient and facile synthesis of nanosized crystallites of these materials is of high significance

189 n attractive pathway of producing sizable 2D crystallites of tin is based on deintercalation of bulk

190 time, prompting lateral translations of the crystallites of torons within quasi-hexagonal periodical

191 luding stable tetrameric clusters and "ionic crystallites" of counter-twisting domains organized on a

192 By depositing TpAzo COF crystallites on C(10)FFVR nanotubes through IC, we produ

193 Further, the new crystallites on development can in turn serve as seeds.

194 hort-range attraction between spheres led to crystallites one to three layers thick.

195 kylether-functionalised layered-pillared MOF crystallites onto substrates via stepwise liquid-phase e

196 particles, we anchor uniform block copolymer crystallites onto the nanoparticle surface.

197 es either are more stable than hexagonal ice crystallites or form because of non-equilibrium dynamica

198 to stresses operating either on surfaces of crystallites or within the bulk.

199 W/mK was measured on a pellet with preferred crystallite orientation along the stacking axis, with pe

200 ion at submicrometer resolution, analysis of crystallite orientation distribution, and unsupervised m

201 of fluorine leads to a more face-on polymer crystallite orientation with respect to the substrate, w

202 ocrystals larger than 80 A into brick-shaped crystallites oriented along the (111) crystallographic d

203 that enamel is a composite ceramic with the crystallites oriented in a complex three-dimensional con

204 quid suspension consisting of lipid lamellar-crystallite particulates immersed in a continuous liquid

205 migration of photogenerated excitons at the crystallite peripheral sites to internal sites, which wa

206 We demonstrate that larger crystallites present smaller band gap and longer lifetim

207 Pure lead crystallites proved extremely resistant to oxidation.

208 opy of the attractive force field around the crystallites represented in part by dipole moments.

209 The shape and orientation of the crystallites results in relatively narrow photoluminesce

210 the termini of immobilized, surface-confined crystallite seeds.

211 Instead, individual crystallites seemed to spill out of the enamel when frac

212 sue in mammals, consisting of hydroxyapatite crystallites separated by long and narrow nanochannels.

213 X-ray Li2O2 reflections confirms a platelet crystallite shape.

214 Perovskite films composed of small crystallites show higher yields of superoxide and lower

215 The evolution of crystallite size and microstrain in DNA-mediated nanopar

216 forms two different inclusions differing in crystallite size and the rotational barriers.

217 ding into the rice husk owing to the smaller crystallite size as well as the increased pseudocapacita

218 We establish a quantitative link between the crystallite size established by diffraction and electron

219 tron microscopic images of the material; the crystallite size evolves from several nanometers into th

220 te an increase in CT polarizability when C60 crystallite size exceeds this threshold, and that this c

221 ased material thickness as well as increased crystallite size in the ceramics.

222 c structure, which leads to the reduction of crystallite size in the polymer matrix, consequently aff

223 sium content decreases the average nanoscale crystallite size of disordered calcium carbonate.

224 CO(2) atmosphere or air yielding an average crystallite size of the resultant In(2)O(3) that is appr

225 ne loading but that there is a threshold C60 crystallite size of ~4 nm below which the spatial extent

226 porous silicon nanowires with ultra-thin Si crystallite size of ~4 nm.

227 orted and shown to relate to the increase in crystallite size on reducing molecular weight.

228 ting domains, sometimes loosely described as crystallite size or crystallinity.

229 to diamond-structured carbon with an average crystallite size ranging from 5 to 10 nanometres.

230 function from collagen, carbonate and finite crystallite size were examined through principal compone

231 perimental observations of increased average crystallite size with the addition of water are modeled

232 xhibit a higher crystalline fraction, larger crystallite size, and improved mechanical properties com

233 The striking similarity in crystallite size, morphology, and surface area character

234 lcine porous CFO to 900 degrees C to enhance crystallite size, particle size and spacing, and composi

235 igonal prismatic and octahedral) and smaller crystallite size, which were confirmed via scanning tran

236 cal nanocrystal system CdSe as a function of crystallite size.

237 Peptide crystallites size was increased by cross-linking and aci

238 ific capacitances were obtained when smaller crystallite sized bimetallic Co/Mn-MOFs were grown insid

239 The distribution of crystallite sizes across the arrays is very narrow (stan

240 d pseudocapacitance exhibited by the smaller crystallite sizes and increased porosity.

241 uced from 50 to 6.6 mum, consistent with the crystallite sizes observed in SEM images.

242 es show their core-shell nature with average crystallite sizes of 50 (Cu/C), 18 (Co/C) and 20 nm (Ni/

243 The final products are in the bulk form with crystallite sizes of 50 - 80 mum.

244 O(2), TiO(2), and ZrO(2) materials with mean crystallite sizes of approximately 20, 50, and 15 angstr

245 Crystallite sizes were determined using the Scherrer equ

246 metal substitution or the role of nanoscale crystallite sizes.

247 e the rice husks channels compared to larger crystallite sizes.

248 By contrast, for weak repulsion, crystallites slowly grow and fuse through rearrangement

249 ring protein-to-crystallite interactions and crystallite stacking while diminishing the ability of th

250 electrons and ions into the bulk of the MOF crystallite (stage B), and a final period of the convers

251 Large crystallites sublimated by escape of particles from the

252 n UiO-67-DCBPY is not uniform throughout the crystallites such that RuDCBPY densely populates the out

253 The (110) surface dominates the crystallite surface area.

254 e bulk material and that conductivity at the crystallite surfaces is most responsive to gas adsorptio

255 lomerated V(2) O(5) consisting of very small crystallites (TBA-V(2) O(5) ).

256 xagonal motifs, which give rise to elongated crystallites that are not able to grow.

257 ntities of faceted nanoparticle superlattice crystallites that can be further shaped into macroscopic

258 long and highly ordered hydroxyapatite (HAP) crystallites that constitute enamel.

259 drophobic properties, compact structures and crystallites that restricted vapor and oxygen permeation

260 cles, leading to the formation of bundles of crystallites, the hallmark structural organization of th

261 th tuftelin, a potential nucleator of enamel crystallites, the yeast two-hybrid system was applied to

262 The crystallite thickness of UO2 was 4 to 5 nm without Fe(2+

263 Crystallite thickness was independent of location in bot

264 ng the physical dimensions of the perovskite crystallites to a few nanometers can also unlock spatial

265 deposited in the previous cycle, causing the crystallites to lengthen with each cycle.

266 ontrolled energy flow from localized surface crystallites to the bulk.

267 At this size, the crystallites transformed into a dense amorphous structur

268 nity of the PbS quantum rods, where each PbS crystallite transforms in a separate PbS/CdS dot-in-dot.

269 t the spherulites are composed of helicoidal crystallites twisted along the <010> growth directions.

270 tions of circular birefringence arising from crystallite twisting and splaying under confinement.

271 ure of this VHDA phase: it rapidly nucleates crystallites, ultimately leading to the formation of a p

272 cooperative flexibility, wherein individual crystallites undergo global structural phase changes in

273 ineral deposition onto the sides of existing crystallites until they interlock with adjacent crystall

274 stacking-disordered ice the stable phase for crystallites up to a size of at least 100,000 molecules.

275 igand into the UiO-67 lattice transforms the crystallites, upon metalation, into single-site, metal-b

276 architecture is destroyed by fracturing the crystallites via grinding, the amount of N2 adsorbed dou

277 By investigating these crystallites, we obtain important clues about the mechan

278 These nanosized crystallites were kinetically protected against further

279 n both DI-II and normal dentin, although the crystallites were significantly thicker in DI-II dentin

280 ization driving force on the size of the ice crystallite when interpreting and extrapolating ice nucl

281 ort of DMMP vapor through individual NU-1008 crystallites, where the relative humidity (RH) of the en

282 of selectively oriented, electrode-supported crystallites, where the rodlike crystallites are either

283 During the reactions, we observed nanosized crystallites which attached to the enamel surfaces or es

284 ed of a network of intimately connected FAPI crystallites which form a mesoporous architecture.

285 rric (Fe(3+)) paramagnetic state in hemozoin crystallites which induce a measurable change in spin-sp

286 temperature, melting strain-induced polymer crystallites (which act as physical crosslinks that secu

287 the presence of approximately 40 A wide beta-crystallites, which constitute the protofilament.

288 the non-crystalline regions and the ordered crystallites, which is likely to originate from its supe

289 was attributed to the appearance of mineral crystallites, which were also detected by x-ray diffract

290 First, beta-hematin crystallites, whose nucleation is promoted by H-DHA, inc

291 of plastic deformation are twinning (whereby crystallites with a mirror-image lattice form) and slip

292 ereas model B views the clays as composed of crystallites with a unique structure that maintains cohe

293 he sequence LLL..., and faceted silicalite-1 crystallites with dimensions less than 100 nm with the s

294 hat for certain "magic" Nw the clusters form crystallites with stable structures, where discrete wate

295 for tailoring two-dimensional (2D) zeolites (crystallites with thickness less than two unit cells) an

296 th intra- and extrafibrillar localization of crystallites, with a tunable mass percentage of inorgani

297 ene (CB) induced the nucleation of polymeric crystallites within 2 min of deposition, increased the o

298 s, whereas Arachnocampa has cross-beta-sheet crystallites within its silk.

299 ed on the growth of multiple pre-existing Mg crystallites within the MgH2 matrix, present due to the

300 taining in the electron microscope, the beta-crystallites would be arranged in 4-mers.