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During printing test for buildability, mixture A can easily reach up to 40 layers without notable deformation, while all other mixtures deformed noticeably and fell down before the 35th layer.
If notable deformation resulted from sectioning, we utilized these block-face photographs to register each deformed HE slide back to its original shape at the time of gross sectioning.
Finally, a large-scale printing was carried out with mixture A and a structure with the height of 80 cm was printed successfully without notable deformation.
To investigate the durability against consecutive stretching and releasing, the R s of the sample was measured during cyclic stretching tests (10,000 cycles at up to 100% tensile strain with a rate of 2.54 mm s−1) and it was almost constant without notable deformation, as plotted in Figure 5b.
Similar(56)
Several mechanisms were deemed to contribute to the overall strains; such were higher elastic-but also higher irreversible shear strains in the epoxy matrix and the fibers; damage within the epoxy; conceivably also in the fibers; appearance of microcracks in epoxy-rich regions; possibly separation of the interfaces, and also notable creep deformation at higher loads.
The notable differences (deformations, intensities and shifts) in RMN, ATMN and BTMN before adsorption were observed at the following wavenumbers, 3339, 2925, 1740, 1452, 1241 and 1026 cm−1.
Prior to the EOF analysis, I corrected for the CME time series by subtracting the CME time series obtained by stacking 38 position time series of the GEONET stations that are equipped with 02-type pillars and are outside the region 140 143°E by 37 40°N where notable coseismic/postseismic deformations associated with the foreshock are observed.
This notable increase in deformation capacity of the heat-damaged columns is attributed to the heat-induced micro-cracking and the removal of water which makes concrete soft and more porous.
The strength increment due to TRM strengthening was observed to range from 128% to 136% when the URM test walls were loaded in-plane and from 575% to 786% when the URM test walls were loaded out-of-plane, with a notable increment in deformation capacity and ductility.
Deformation associated with an eruption is more likely to be 'central' (< 5 km from the volcano) than 'offset' (≥ 5 km distant), although there are a few notable examples of distal deformation accompanying eruption (e.g., Jay et al., 2014).
Viscoelastic deformation was a notable characteristic of the organic component.
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