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1 for the creation of the new surfaces of the microcrack.
2 ity of the bone matrix, and the evolution of microcracks.
3 interaction and coalescence of many tensile microcracks.
4 ess remodelling resulting in accumulation of microcracks.
5 tural levels, which occurs by the process of microcracking.
6 ly enhanced resistance to contact damage and microcracking.
7 at reducing perforations but may also cause microcrack accumulation, leading to a loss of microstruc
8 -ceramics (< 1 microm) showed minimal matrix microcracking and BFS values of [mean (SD) MPa]: M1A = 2
10 be lower, thereby limiting the formation of microcracks and minimizing the development of tangential
12 -type cracks as well as inter- and intra-rod microcracks, and that the lengths of these cracks are se
14 ystal-glass thermal mismatches which produce microcracking around larger crystals-agglomerates are as
16 s manifested by the nucleation of many sharp microcracks at the external boundary that rapidly propag
17 hod is applied to image key features such as microcracks, carbides, heat affected zone, and dendrites
18 matrix constituents (collagen and mineral), microcrack characteristics, and trabecular architecture
19 ography, we have fully resolved sequences of microcrack damage as cracks grow under load at temperatu
24 the magnitude of the increase or decrease in microcrack density after several firings is sufficiently
25 lly significant negative correlation between microcrack density and multiple firings (r2 = 0.15, p =
26 hly significant positive correlation between microcrack density and multiple firings (r2 = 0.24, p =
28 rcelains that exhibit a measurable change in microcrack density as a function of multiple firings, th
32 : We reconstruct the complete spatiotemporal microcracking dynamics, with micrometer/nanosecond resol
33 ng acoustic phonon emissions from individual microcracking events we show that the onset of a seconda
34 e form of median-type cracks and distributed microcracks, extending preferentially along the boundari
35 e lattice potentially large enough to induce microcrack formation, which are abundant below the hypha
36 nsistent with observations of the closure of microcracks formed parallel to the covalent-sp(2)-bonded
38 circumferential surface cracking, orthogonal microcracking in laminated sublayers and geometrically c
39 two energy-dissipating mechanisms: multiple microcracking in the outer layers at low mechanical load
41 This contraction leads to the formation of microcracks in and around the crystals and the developme
42 show that the elastic stress around tensile microcracks in three dimensions promotes a mutual intera
47 results suggest that mineral dissolution and microcracking may have acted in a synergistic way at the
53 er perforations but more numerous and larger microcracks than both fracture and non-fracture controls
54 is known about bone microsctructure and the microcracks that are precursors to its fracture, but lit
55 porcelains are often partially encircled by microcracks that are the result of the thermal expansion
60 is associated with more brittle fracture and microcracks without altering the average length of the c
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