The most compact barite sediment can be characterized as a non-elastic dense wet particle sediment where the packing of the particles and the particle size of the grains varies. To fully understand the packing mechanism of the consolidated barite sediments characterization of barite powder (both dry and wet) is important.
In this study we have done comparable measurements with a Jenike shear test, which measures direct shear strength under different loading conditions, and compared these to rheological measurements using an Anton Paar powder module under the same loading conditions. Experiments were performed on both dry and wet (by 2.5 wt% and 5 wt% water) barite and with 1, 3, 6 and 9 kPa loading.
The results from the Jenike test and the powder module were found to be complimentary. At a low water content, the sample showed an increase in flowability, while with a high-water content a decrease the flowability was observed compared to that of dry barite.