ライフサイエンスコーパス: crystallite

1 served at the surface and inside the growing crystallite.

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

3 are effectively suppressed by the nanoscale crystallites.

4 stallites until they interlock with adjacent crystallites.

5 on within its protein layers between apatite crystallites.

6 yields enamel with disordered hydroxyapatite crystallites.

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

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

9 lated to the length scale of the polyalanine crystallites.

10 causes massive changes in the shape of lead crystallites.

11 ntal measure of properties of the nucleating crystallites.

12 dried on the ZnSe crystal contains silk III crystallites.

13 to other scattering sources like the mineral crystallites.

14 arated and electronically decoupled graphene crystallites.

15 anneling through the pores of polymeric nano-crystallites.

16 ctating the size and symmetry of the growing crystallites.

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

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

19 bedded with nanosized hydroxyapatite mineral crystallites.

20 3 A and can assemble in bilayer and trilayer crystallites.

21 results in a gradual reduction of the Li2O2 crystallites.

22 ular hemoglobin and convert it into hemozoin crystallites.

23 he surface indicates nanostructured lamellar crystallites.

24 size of and rotational disorder between the crystallites.

25 ayer, decorated with structurally related 3D crystallites.

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

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

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

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

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

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

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

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

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

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

36 Affected crystallites appeared more radiolucent and morphological

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

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

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

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

41 The crystallites are isometric with markedly rough surfaces

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

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

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

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

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

47 These crystallites are weakly bound to the crystal surface and

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

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

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

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

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

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

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

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

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

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

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

59 The crystallite clusters seemed to diffuse from the IOL inte

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

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

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

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

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

65 hin starch granules, suggestive of imperfect crystallite development.

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

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

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

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

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

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

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

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

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

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

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

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

78 Enamel crystallites form in a protein matrix located proximal t

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

80 The crystallite formation process was compared with respect

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

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

83 ic function of guiding enamel hydroxyapatite crystallite formation.

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

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

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

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

88 Crystallites from fish are morphologically diverse and s

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

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

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

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

93 ing assembly of matrix proteins that control crystallite habit.

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

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

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

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

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

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

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

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

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

103 Each crystallite is composed of several orthogonal unit cells

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

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

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

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

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

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

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

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

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

113 0 kelvin are about 14 kilojoules per mole of crystallite more stable than hexagonal crystallites, mak

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

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

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

117 f enamel formation when nucleation of enamel crystallites occurs.

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

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

120 Crystallites of different sizes were clearly visible fro

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

139 Pure lead crystallites proved extremely resistant to oxidation.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

164 Large crystallites sublimated by escape of particles from the

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

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

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

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

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

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

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

172 Crystallite thickness was independent of location in bot

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

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

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

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

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

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

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

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

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

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

183 These nanosized crystallites were kinetically protected against further

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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