TY - JOUR
T1 - Loop energy
T2 - A useful indicator of the hardness of minerals from depth-sensing indentation tests
AU - Masuda, Toshiaki
AU - Omori, Yasutomo
AU - Sakurai, Ryoko
AU - Miyake, Tomoya
AU - Yamanouchi, Mirai
AU - Harigane, Yumiko
AU - Okamoto, Atsushi
AU - Michibayashi, Katsuyoshi
N1 - Funding Information:
The authors thank Mototsugu Sakai for encouraging this study, Nozomi Kimura for critical discussions, Hideki Mori for help with sample preparation, and Sayuri Miyagishima for operating RIDER II and logistical support. The authors also thank Yuli Milman for constructive suggestions and Ian Alsop for kind comments. This study was financially supported by the Japanese Society for the Promotion of Science ( 16340152 to TM).
Publisher Copyright:
© 2018 Elsevier Ltd
PY - 2018/12
Y1 - 2018/12
N2 - Depth-sensing indentation tests were performed to obtain the loop energy (equivalent to the energy consumed to produce the indentation) and the residual depth of the indentation using a triangular pyramidal diamond indenter for the minerals in Mohs hardness scale except for diamond, as well as other minerals (apophyllite, forsterite, and tourmaline), at a maximum load ranging from 30 to 100 mN. A new graphic presentation is proposed that shows the hardness of minerals in log(penetration depth)−log(loop energy) space. The data for each mineral under different loads give a straight regression line with a slope of 2.6–2.9 (except for talc, which yields a slope of 2.2), while the data for different minerals under a given load yield a straight regression line with a slope of 1.1–1.2. A theoretical analysis of ideal materials, in terms of log(penetration depth)−log(loop energy) space, shows the existence of two series of parallel regression lines with slopes of 3 (data for each mineral at different loads) and 1 (data for different minerals under a given load). The results show a slight deviation between the measured and theoretical slopes, probably reflecting a progressive change in the mechanical properties of the minerals during the indentation tests.
AB - Depth-sensing indentation tests were performed to obtain the loop energy (equivalent to the energy consumed to produce the indentation) and the residual depth of the indentation using a triangular pyramidal diamond indenter for the minerals in Mohs hardness scale except for diamond, as well as other minerals (apophyllite, forsterite, and tourmaline), at a maximum load ranging from 30 to 100 mN. A new graphic presentation is proposed that shows the hardness of minerals in log(penetration depth)−log(loop energy) space. The data for each mineral under different loads give a straight regression line with a slope of 2.6–2.9 (except for talc, which yields a slope of 2.2), while the data for different minerals under a given load yield a straight regression line with a slope of 1.1–1.2. A theoretical analysis of ideal materials, in terms of log(penetration depth)−log(loop energy) space, shows the existence of two series of parallel regression lines with slopes of 3 (data for each mineral at different loads) and 1 (data for different minerals under a given load). The results show a slight deviation between the measured and theoretical slopes, probably reflecting a progressive change in the mechanical properties of the minerals during the indentation tests.
KW - Depth-sensing indentation test
KW - Loop energy
KW - Mohs hardness scale
KW - New graphic presentation
KW - Penetration depth
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U2 - 10.1016/j.jsg.2018.09.004
DO - 10.1016/j.jsg.2018.09.004
M3 - Article
AN - SCOPUS:85053813805
SN - 0191-8141
VL - 117
SP - 96
EP - 104
JO - Journal of Structural Geology
JF - Journal of Structural Geology
ER -