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1 tes in the immediate vicinity of the nearest microcrack.
2 nt matrix, fluid is also squeezed out of the microcrack.
3 for the creation of the new surfaces of the microcrack.
4 resent pores in an aligned clay compact or a microcrack.
5 ess remodelling resulting in accumulation of microcracks.
6 ptions of osteocyte canaliculi around linear microcracks.
7 ity of the bone matrix, and the evolution of microcracks.
8 interaction and coalescence of many tensile microcracks.
9 om 30% to 110% strain without any noticeable microcracks.
10 tural levels, which occurs by the process of microcracking.
11 ly enhanced resistance to contact damage and microcracking.
12 e in permeability is observed, likely due to microcracking.
13 at reducing perforations but may also cause microcrack accumulation, leading to a loss of microstruc
14 We observe reversible planar gliding and microcracking along the (003) plane in a single-crystall
16 -ceramics (< 1 microm) showed minimal matrix microcracking and BFS values of [mean (SD) MPa]: M1A = 2
18 ed cell attachment and mineralization around microcracks and a higher expression of osteocalcin -an o
19 be lower, thereby limiting the formation of microcracks and minimizing the development of tangential
22 Os, including anisotropic lattice evolution, microcracking, and surface degradation, as a result of w
23 in subchondral bone (SCB) sclerosis, fatigue microcracks, and matrix damage that can progress to para
24 -type cracks as well as inter- and intra-rod microcracks, and that the lengths of these cracks are se
26 ystal-glass thermal mismatches which produce microcracking around larger crystals-agglomerates are as
30 rphyritic andesites, implicating progressive microcracking as the cause of permanent inelastic strain
31 s manifested by the nucleation of many sharp microcracks at the external boundary that rapidly propag
33 hod is applied to image key features such as microcracks, carbides, heat affected zone, and dendrites
34 matrix constituents (collagen and mineral), microcrack characteristics, and trabecular architecture
37 ography, we have fully resolved sequences of microcrack damage as cracks grow under load at temperatu
41 ge and extended cellular processes deep into microcracks, delivering mitochondria to chondrocytes.
44 the magnitude of the increase or decrease in microcrack density after several firings is sufficiently
45 lly significant negative correlation between microcrack density and multiple firings (r2 = 0.15, p =
46 hly significant positive correlation between microcrack density and multiple firings (r2 = 0.24, p =
48 rcelains that exhibit a measurable change in microcrack density as a function of multiple firings, th
52 measurements presented here show that these microcracks do not permit uniform access to the adjacent
53 : We reconstruct the complete spatiotemporal microcracking dynamics, with micrometer/nanosecond resol
55 rmation about the potential effect of enamel microcracks (EMCs) on the underlying tooth structures.
56 ng acoustic phonon emissions from individual microcracking events we show that the onset of a seconda
57 or concrete surface, subsequent formation of microcracks exposes the substrate's near-infrared emissi
58 e form of median-type cracks and distributed microcracks, extending preferentially along the boundari
60 tic mudstones is first observed along planar microcracks, followed by slow penetration into the surro
66 thode, which should be maximized to suppress microcrack formation, the main cause of capacity fading
67 e lattice potentially large enough to induce microcrack formation, which are abundant below the hypha
68 eactions, significant phase transitions, and microcrack formation, which lead to considerable interna
70 nsistent with observations of the closure of microcracks formed parallel to the covalent-sp(2)-bonded
71 T3-E1 mouse osteoblastic cells in biomimetic microcracked hydroxyapatite substrates, differentiated i
73 circumferential surface cracking, orthogonal microcracking in laminated sublayers and geometrically c
74 two energy-dissipating mechanisms: multiple microcracking in the outer layers at low mechanical load
76 llographic nucleation and growth of multiple microcracks in abundant poor-deformability microstructur
77 This contraction leads to the formation of microcracks in and around the crystals and the developme
79 show that the elastic stress around tensile microcracks in three dimensions promotes a mutual intera
86 results suggest that mineral dissolution and microcracking may have acted in a synergistic way at the
90 captures oriented mesoscale frictional slip, microcrack opening, and splitting with microbuckling.
91 they play a central role in the formation of microcracks or bedding delaminations which ultimately do
93 arying validation accuracy to detect cracks, microcracks, Potential Induced Degradations (PIDs), and
95 micro-mechanisms directly by controlling the microcracking rate to slow down the transition in a uniq
97 er perforations but more numerous and larger microcracks than both fracture and non-fracture controls
98 is known about bone microsctructure and the microcracks that are precursors to its fracture, but lit
99 porcelains are often partially encircled by microcracks that are the result of the thermal expansion
106 g real-world cases, such as shaded areas and microcracks, which were accurately predicted by the syst
108 is associated with more brittle fracture and microcracks without altering the average length of the c