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Justifying API Bentonite Rheological Behavior Through Its Forming Size Fractions

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Abstract

Bentonite represents one of the main players in the stability of the drilling mud. Its particle size and particle size distribution affect the physical properties of the drilling mud especially the rheological properties. Therefore, a specific particle size distribution was recommended by American Petroleum Institute (API) for use in drilling mud. To clarify the effect of individual size and size distribution, in this study, the bentonite sample was classified into different size fractions. Each size fraction was tested separately in terms of controlling properties such as filtration loss, plastic viscosity, gel strength, cake thickness, and packing density. The effect of each size fraction on the rheological properties of the suspension was correlated to the behavior of the whole particle size distribution in the bentonite sample. The results indicate that the coarser the particles, the higher the rheological properties; in this case, the API mixture is the highest. The filtration loss and cake thickness for the API mixture are lower than that of the individual size fractions due to its wider size distribution due to the filling of voids between larger particles with smaller ones, which lead to bed compaction and consequently lower fluid loss and cake thickness.

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Authors and Affiliations

  1. Mining, Petroleum and Metallurgical Engineering Dept., Cairo University, Cairo, Egypt

    R. M. Farag, A. A. El-Midany & S. E. El-Mofty

  2. Petroleum Engineering Dept., Suez University, Suez, Egypt

    A. M. Salem

  3. Civil Engineering Department, College of Engineering, Bisha University, P.O. Box 551, Bisha, 61922, Saudi Arabia

    S. E. El-Mofty

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  1. R. M. Farag
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  2. A. M. Salem
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  3. A. A. El-Midany
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  4. S. E. El-Mofty
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Correspondence to A. A. El-Midany.

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Farag, R.M., Salem, A.M., El-Midany, A.A. et al. Justifying API Bentonite Rheological Behavior Through Its Forming Size Fractions. Mining, Metallurgy & Exploration 37, 537–542 (2020). https://doi.org/10.1007/s42461-019-00157-w

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  • DOI: https://doi.org/10.1007/s42461-019-00157-w

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