Rheological behavior of a bentonite mud

Author:

Marum Daniela Martins1,Afonso Maria Diná2,Ochoa Brian Bernardo1

Affiliation:

1. Baker Hughes, a GE company , 29221 Celle, Lower Saxony , Germany

2. Universidade de Lisboa , Instituto Superior Técnico , CeFEMA, Av. Rovisco Pais, 1, 1049-001 Lisbon , Portugal

Abstract

Abstract Predicting drilling fluids rheology is crucial to control/optimize the drilling process and the gas extraction from drilling fluids in logging systems. A Couette viscometer measured the apparent viscosity of a bentonite mud at various shear rates and temperatures. The bentonite mud behaved as a yield-pseudoplastic fluid, and a modified Herschel-Bulkley model predicted the shear rate and temperature effects upon the shear stress. A pipe viscometer was built to seek a correlation between the mud flow rate and the pressure drop and thereby determine refined Herschel-Bulkley parameters. Coupling a rheological model to a pipe viscometer enables the continuous acquisition of apparent viscosities of Newtonian or non-Newtonian fluids at a rig-site surface.

Publisher

Walter de Gruyter GmbH

Subject

Condensed Matter Physics,General Materials Science

Reference52 articles.

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2. [2] Pixler BO. Baroid Mud Analysis Logging. The Log Analyst 1967;7(05).

3. [3] Hammerschmidt SB, Wiersberg T, Heuer VB, Wendt J, Erzinger J, Kopf A. Real-time drilling mud gas monitoring for qualitative evaluation of hydrocarbon gas composition during deep sea drilling in the Nankai Trough Kumano Basin. Geochemical Transactions 2014;15(15).

4. [4] ASME Shale Shaker Committee. Drilling fluids processing handbook. Elsevier: Gulf Professional Publishing; 2011.

5. [5] Marum DM, Afonso MD, Ochoa BB. Enhancement of the Gas Extraction for Reservoir Identification in a New Mud Logging System. GeoConvention 2019; 2019 May 13-15; Calgary, Alberta, Canada. Available from: https://geoconvention.com/wp-content/uploads/abstracts/2019/GC2019_021_Enhancement_of_the_Gas_Extraction_for_Reservoir_Identification_in_New_Mud_Logging_System.pdf.

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