EGU23-3821
https://doi.org/10.5194/egusphere-egu23-3821
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Analyzing the rheological behavior of medium fine iron ore slurry.

Stuti Mishra1 and Deo Raj Kaushal2
Stuti Mishra and Deo Raj Kaushal
  • 1Research Scholar, Civil Engineering, Indian Institute of Technology, New Delhi, India (stuti.mishra@civil.iitd.ac.in)
  • 2Professor, Civil Engineering, Indian Institute of Technology, New Delhi, India (Deo.Raj.Kaushal@civil.iitd.ac.in)

A slurry pipeline is a specially designed pipeline used to transport the tailings, wastes from the mining, ores like iron or coal to long distances. A commercially tested solution for the transport of iron ore slurry over the farthest distances in a pipeline includes various parametric checks. For the slurry to move without any hassle in the pipe maintaining the required velocity, it is important to keep some parameters in the desired limits, the most important of which is the rheological characteristics of the slurry. The rheological characteristics gives us an idea about the viscous properties, stress strain behavior of the iron ore exhibiting in its surrounding. The rheological parameters of the iron ore slurry were measured using a high precision Anton paar RheoloabQC Rheometer. At different concentrations the samples were tested keeping the particle size to be same for all the observations. While the method has been kept the same for the experiments, different rotating tools are used in the rheometer to check the accuracy of the data as well as to draw a comparison on the data obtained from them for each level of concentration. Our study majorly deals with a comparative assessment of the performance of the various rotating tools to study the rheology of the iron ore slurry.

How to cite: Mishra, S. and Kaushal, D. R.: Analyzing the rheological behavior of medium fine iron ore slurry., EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-3821, https://doi.org/10.5194/egusphere-egu23-3821, 2023.