GFM 2

lectures 3 and 4

lectures 3 and 4


Kartei Details

Karten 17
Sprache English
Kategorie Naturkunde
Stufe Universität
Erstellt / Aktualisiert 13.01.2013 / 13.01.2013
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on Mohrs circle

.

equation for straight line on a Mohrs circle

.

what does c represent on a Mohrs circle

cohesion

graph of confining pressure and stress

.

how much bigger are compressive strengths of rocks than tensil

10-20

temperature and strain rate graph

.

pore pressure and strength graph

.

what is dilatancy

when volume increases with compression

2 methods of measuring dilatancy

fluid flowing into or out of pores

strain gauges to measure longitudingal and lateral strains.

What is an acoustic emmission

The propagation of a microcrack causes an elastic wave, which can be detected audibly

4 stages of brittle failure

1 closing of cracks and pore space

2 elastic behavior

3 microcracking

4 break-microcracks link to form hear plane

Posissons Ratio

the ratio between strain imposed on a sample in one direction and the resulting strain perpendicular to this direction

U

total energy

(Griffith’s cracks)

Um

mechanical energy

(Griffith’s cracks)

Us

Surface energy

(Griffith’s cracks)

equilibrium point on Griffith's cracks graph

.

mu

(Mohrs)

internal friction