Time and Temperature Dependence of Tensile Fracture Strength for Unidirectional CFRP

2000 ◽  
Vol 2000 (0) ◽  
pp. 103-104
Author(s):  
Masayuki Nakada ◽  
Yasushi Miyano
Keyword(s):  
Temperature Dependence ◽  
Fracture Strength ◽  
Tensile Fracture ◽  
Tensile Fracture Strength

Tensile fracture strength of 2124Al–10vol.% SiCp composite compact tension specimens

2010 ◽  
Vol 31 (6) ◽  
pp. 2987-2993 ◽  
Author(s):  
T. Parameshwaranpillai ◽  
P.R. Lakshminarayanan ◽  
B. Nageswara Rao
Keyword(s):  
Fracture Strength ◽  
Compact Tension ◽  
Tensile Fracture ◽  
Tensile Fracture Strength

Reliability of tensile fracture strength of Co-based metallic glass microwires by Weibull statistics

2019 ◽  
Vol 6 (10) ◽  
pp. 106565
Author(s):  
Wei-Bing Liao ◽  
Chenchen Jiang ◽  
Shang Xu ◽  
Libo Gao ◽  
Hongti Zhang ◽  
...  
Keyword(s):  
Metallic Glass ◽  
Fracture Strength ◽  
Tensile Fracture ◽  
Weibull Statistics ◽  
Tensile Fracture Strength

Effects of drawing on the tensile fracture strength and its reliability of small-sized metallic glasses

2010 ◽  
Vol 58 (7) ◽  
pp. 2564-2576 ◽  
Author(s):  
Y. Wu ◽  
H.H. Wu ◽  
X.D. Hui ◽  
G.L. Chen ◽  
Z.P. Lu
Keyword(s):  
Fracture Strength ◽  
Metallic Glasses ◽  
Tensile Fracture ◽  
Tensile Fracture Strength

Relationship between joint spacing and bed thickness in sedimentary rocks: effects of interbed slip

1998 ◽  
Vol 135 (5) ◽  
pp. 637-655 ◽  
Author(s):  
SHAOCHENG JI ◽  
ZHEMING ZHU ◽  
ZICHAO WANG
Keyword(s):  
Shear Strength ◽  
Fracture Strength ◽  
Sedimentary Rocks ◽  
Tensile Fracture ◽  
Formation Mechanisms ◽  
Joint Spacing ◽  
Tensile Fracture Strength ◽  
Mechanical Models ◽  
Bed Thickness ◽  
The Relationship

This paper consists of three parts. The first part presents a critical review of previous mechanical models on the relationship between joint spacing (s) and bed thickness (t) in sedimentary rocks. The second part describes a new mechanical model dealing with the effects of interbed slip on joint spacing. The third part presents the comparison between theoretical results of the model and joint data measured from Cambrian flysch sediments at Plage Victor in the Saint-Jean-Port-Joli area of the Quebec Appalachians. This study demonstrates two formation mechanisms of tensile joints: near-end fracturing takes place in the layers with smaller tensile fracture strength (C0<30 MPa) and smaller interbed shear strength (τ0<20 MPa) while mid-point fracturing occurs in those layers with larger C0 (>50 MPa) and τ0(>30 MPa) values. For the rocks with moderate tensile fracture strength (30<C0<50 MPa) and interbed shear strength (20<τ0<30 MPa), the near-end fracturing and mid-point fracturing take place preferentially in the thicker and thinner brittle layers, respectively. In the regime of near-end fracturing, the correlation between s and t is linear and independent of the thickness of the bounding non-jointing layers (d). In the regime of mid-point fracturing, however, the s–t relationship can be either linear or non-linear, depending on the variation of d value. The present study also suggests that the near-end fracturing is probably the prevailing process for the formation of tensile joints in bedded sedimentary rocks and that the coefficient of joint spacing (K) defined by the ratio of s to t is considered as an indicator of C0/(2τ0) for the jointed layer.

Tensile fracture strength of boron/aluminum laminates with holes and slits

2001 ◽  
Vol 301 (2) ◽  
pp. 244-252 ◽  
Author(s):  
P.K.Govindan Potti ◽  
B.Nageswara Rao ◽  
V.K Srivastava
Keyword(s):  
Fracture Strength ◽  
Tensile Fracture ◽  
Tensile Fracture Strength
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