Unconfined compressive strength

UCS (also frequently named C0)Critical stress value at which a rock body fails brittlely under compresion. It may be determined directly via a uniaxial test under unconfined compressive conditions (σ1>>σ23=0 MPa) or by a series of triaxial tests (σ123≠0 MPa). In the latter case it is necessary to determine peak strength at several confining pressure stages (either via various single stage tests or via one multi stage experiment) and to draw a regression line through all peak strength data points to unravel the peak strength at 0 MPa as the UCS. This indirect way to determine UCS yields higher stress values than the direct measurements due to the fact that during confining pressure buildup in triaxial deformation tests microfractures are closing which will remain open during an unconfined compressive test. Consequently, only indirect UCS determination gives data for intact rock and only those data can be used for comparison with other data for the same rock type. Rock UCS values roughly range from 1 MPa (weakly consolidated sandstone) to 350 MPa (granite and basalt).

A A A
Login
 

News

29.04.2026 · DGMK Spring conference 2026

The DGMK/ÖGEW spring conference is on the road for the second time, and – as always – we’ll be there!

Come and see us in Münster at Stand 32 on the upper floor; we look forward to seeing you!

03.02.2026 · Project HENRI

Gesteinslabor Dr. Eberhard Jahns is project and research partner within the HENRI (Hydrogen Energy Reservoir) project.

Our main focus is on determining the impact of H2 on the cap rock. Besides other parameters, we measure the capillary threshold pressure using various gases and gas mixtures of hydrogen and methane.

Results were presented at the third HENRI conference in Bratislava in September 2025

 

23.06.2025 · SCAN

 

We are pleased to be part of the Dutch subsurface research for geothermal heat SCAN.

Further information can be found on the official homepage:

https://scanaardwarmte.nl/english/