Elastic Modulus Test
Sample(I): porphyry Location: Trentino Rocktype: porphyric quartzite
Orientation of possible planes of discontinuity or schistocity with respect to the direction of load |
|
|
|
L = 201.0 mm |
Applied
load |
Axial pressure |
Longitudinal |
|
Applied
load |
Axial
pressure |
Longitudinal |
0 |
0 |
0 |
|
323.7 |
129.5 |
2180 |
49.0 |
19.6 |
365 |
|
353.2 |
141.3 |
2364 |
98.1 |
39.2 |
722 |
|
382.6 |
153.0 |
2549 |
117.7 |
47.1 |
856 |
|
412.0 |
164.8 |
2737 |
147.1 |
58.8 |
1056 |
|
441.4 |
176.6 |
2917 |
176.6 |
70.6 |
1242 |
|
470.9 |
188.4 |
3107 |
206.6 |
82.4 |
1432 |
|
500.3 |
200.1 |
3290 |
235.4 |
94.2 |
1620 |
|
529.7 |
211.9 |
3480 |
264.9 |
106.0 |
1810 |
|
557.2 |
223.7 |
3677 |
294.3 |
117.7 |
1994 |
|
578.8 |
231.5 |
breaking |
Breaking load under monoaxial compression: Cο = 231,5 MPa |
||||||
* 1 MPa = 10.2 Kgf/cm^2

