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Compressive and Tensile Strength Anisotropy of Friable Sandstone and Thin-Bed Shale of the Pleistocene Erin Formation: Insights for Safe Operating Mud Weight Windows for Vertical and Horizontal Wells

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Abstract

The compressive and tensile strengths are essential parameters used for determining the safe mud weight window (SMWW) during borehole drilling, especially in friable rocks where the SMWW tends to be narrow; therefore, the margin for wellbore instability issues is high. However, these parameters are seldom reported for friable rocks because of the difficulties and challenges faced while recovering and preparing friable cores and outcrop samples for strength testing. This study evaluates the compressive and tensile strengths of friable rocks under dry and saturated conditions and investigates how strength anisotropy affects the SMWW. Unconfined compressive strength, confined compressive strength (up to 130 MPa effective pressure), and Brazilian (tensile strength) measurements were made perpendicular and parallel to the outcrop bedding of the friable sandstone and thin-bed shale lithofacies of the Erin Formation, Southern Trinidad. Although this formation is one of the main petroleum reservoirs, there are no published data on the rock strength. The results show that strength anisotropy exists and is larger under saturated conditions. Under confinement, the friable rocks accumulated large strain (an average of 20% strain) and experienced significant strain hardening causing the strength to be high. The ratio of the yield strength to failure strength is < 0.2 under dry conditions. Thin section analysis of tested specimens shows intragranular fracturing across quartz grains, leading to grain crushing and pore collapse. Cataclastic flow within the specimens and no stress drop after the peak stress suggest the friable rocks failed in a ductile manner. The effect of the strength anisotropy on the SMWW for the sandstone and thin-bed shale was determined for wells orientated in the principal stress directions (\({\sigma }_{\mathrm{v}}, {\sigma }_{\mathrm{h}}\mathrm{ and }{\sigma }_{\mathrm{H}}\)), of a normal faulting stress regime, at depths of 3400–6900 feet. The upper mud weight limit of the SMWW is not influenced by the tensile strength anisotropy. However, the lower mud weight of the SMWW was influenced by the compressive strength anisotropy, predominantly for \({\sigma }_{\mathrm{v}}\) and \({\sigma }_{\mathrm{h}}\) aligned wells that are penetrating through the saturated friable sandstone. Since the rocks are friable, drilling outside of the SMWW by 5–8%, if forecasted using the strongest compressive strength, can result in wellbore instability.

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Abbreviations

\({P}_{\mathrm{m},\mathrm{max}}\) :

Maximum mud pressure (ppg)

\({P}_{\mathrm{m},\mathrm{min}}\) :

Minimum mud pressure (ppg)

\({P}_{\mathrm{p}}\) :

Pore pressure (psi)

\({\sigma }_{1}\) :

Axial force (kN)

\({\sigma }_{3}\) :

Confining pressure (MPa)

\({\sigma }_{\mathrm{h}}\) :

Minimum principal horizontal stress (psi)

\({\sigma }_{\mathrm{H}}\) :

Maximum principal horizontal stress (psi)

\({\sigma }_{\mathrm{c}}\) :

Peak compressive strength (MPa)

\({\sigma }_{\mathrm{t}}\) :

Tensile strength (MPa)

\({\sigma }_{\mathrm{v}}\) :

Vertical principal stress (psi)

C*:

Yield strength (MPa)

c o :

Cohesion

D :

Specimen’s diameter (mm)

F :

Maximum load at failure (N)

L :

Specimen’s length (mm)

LMW:

Lower mud weight limit (ppg)

MD:

Measured depth (ft)

MDT:

Modular dynamics tester

SMWW:

Safe mud weight window (ppg)

t :

Specimen’s thickness (mm)

UCS, \({\sigma }_{O}\) :

Unconfined compressive strength (MPa)

UMW:

Upper mud weight limit (ppg)

θ :

Angle between loading direction and bedding plane

\(\varphi \) :

Internal friction angle (degrees)

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Acknowledgements

The authors would also like to thank Ramnarine Harrypersad, Bassiah Harrypersad and David A. Daniel for their assistance in sample retrieval and transport.

Funding

The authors would like to thank the Campus Research and Publication Fund Committee, University of the West Indies, St. Augustine Campus, for funding the consumables of this research.

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Adele Marie Harrypersad-Daniel and Oshaine Omar Blake wrote the main manuscript including sections: Abstract, Introduction, Laboratory measurements, Laboratory results, Discussion and Conclusion. They also created all figures and tables except for Figs. 1, 4 and 5. The author Ryan Ramsook co-wrote the section titled Geological Setting and Study Area and created Figs. 1, 4 and 5. All authors were involved in reviewing the manuscript.

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Correspondence to Adele Marie Harrypersad-Daniel.

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Harrypersad-Daniel, A.M., Blake, O.O. & Ramsook, R. Compressive and Tensile Strength Anisotropy of Friable Sandstone and Thin-Bed Shale of the Pleistocene Erin Formation: Insights for Safe Operating Mud Weight Windows for Vertical and Horizontal Wells. Pure Appl. Geophys. 180, 4191–4218 (2023). https://doi.org/10.1007/s00024-023-03384-x

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