2010
DOI: 10.1080/10916460903030433
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An Offshore Benign WBM System Can Prevent Hard, Brittle Shale Instability

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Cited by 5 publications
(3 citation statements)
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“…Brittle failure is due to: 1) shales becomes weaken due to hydration of micro fracture surfaces, and bedding planes, 2) clay fail when surrounded by a quartz and feldspar matrix which are non-swelling minerals. Brittle shales usually contain a high percentage of kaolinite, illite and chlorite which may become unstable in a high pH environment (Peng et al, 2010). Borehole failure and shape of cuttings, on these occasions, might be very severe depending on the degree of rock anisotropy and the direction of drilling with respect to the lamination (bedding planes) dip, which is also known as the attack angle.…”
Section: Brittle Shalesmentioning
confidence: 99%
“…Brittle failure is due to: 1) shales becomes weaken due to hydration of micro fracture surfaces, and bedding planes, 2) clay fail when surrounded by a quartz and feldspar matrix which are non-swelling minerals. Brittle shales usually contain a high percentage of kaolinite, illite and chlorite which may become unstable in a high pH environment (Peng et al, 2010). Borehole failure and shape of cuttings, on these occasions, might be very severe depending on the degree of rock anisotropy and the direction of drilling with respect to the lamination (bedding planes) dip, which is also known as the attack angle.…”
Section: Brittle Shalesmentioning
confidence: 99%
“…Previous studies evidenced that over 90% of wellbore instability issues were caused by the reduction in shale strength that stemmed from hydration swelling and dispersion of shale formation during the drilling process . In particular, it should be noted that deep hard and brittle shale, which is mainly rich in Illite and develops microscale pores or fractures, is more prone to hydration dispersion, resulting in accidents such as cuttings disintegration, wellbore collapse, and pipe sticking in deep intervals, where high-pressure, high-temperature (HPHT) conditions prevail. , Thus, drilling fluids have attracted more attention from scientists and engineers owing to the growing drilling issues related to elevated temperatures and wellbore instability.…”
Section: Introductionmentioning
confidence: 99%
“…Mechanical and physicochemical mechanisms were introduced to explain the shale instabilities of the wellbore; however, the studies on wellbore instability mechanisms in shale gas wells are still not clear. Shale swelling is the main instability mechanism for expansive shale, which consists of mainly smectite and illite–smectite mixed layers. Different from the conventional shale, organic-rich shale is characterized by a high content of brittle minerals, weak-swelling clay minerals, and naturally developed fractures. Clay minerals of gas shale formation are mainly illite, kaolinite, and chlorite, which are weak expansive and weak dispersive minerals. , So, the inhibition of gas shale hydration is important for maintaining shale stability, but it is not sufficient. In addition, even when drilled with OBDFs, wellbore instability problems are still not completely resolved.…”
Section: Introductionmentioning
confidence: 99%