1986
DOI: 10.1016/0148-9062(86)90005-7
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Swelling pressure studies of shales

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Cited by 23 publications
(11 citation statements)
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“…In the latter case, crack propagation is controlled by stress corrosion (Atkinson and Meredith 1987). For the relation to (Huang et al 1986), which is negative, that is, of the same sign as tensile stresses. These "negative" pressures are used in the same way as the pore pressure in a saturated rock to derive conventional effective stresses.…”
Section: Effective Stressmentioning
confidence: 97%
“…In the latter case, crack propagation is controlled by stress corrosion (Atkinson and Meredith 1987). For the relation to (Huang et al 1986), which is negative, that is, of the same sign as tensile stresses. These "negative" pressures are used in the same way as the pore pressure in a saturated rock to derive conventional effective stresses.…”
Section: Effective Stressmentioning
confidence: 97%
“…The disjoining pressure is thus a microscopic concept which must be analyzed at the pore scale. The macroscopic swelling pressure which can be measured in natural materials [see, e.g., Madsen and Vonmoos, 1985;Huang et al, 1986;Wong, 1998] is associated with the wellknown swelling properties of certain clays (e.g., smectite). This pressure is currently described as the external stress that has to be applied to a clay-rock sample in order to maintain its mechanical equilibrium (prevent swelling).…”
Section: Introductionmentioning
confidence: 99%
“…These tension cracks produce an increased infiltration of moisture, leading to swelling. The swelling of the rock causes a downward pressure and can create more tensile fractures within the weakly bonded material (Huang et al 1986). This progressive deterioration is what causes the unraveling process between the roof bolts.…”
Section: Shale As a Moisture-sensitive Materialsmentioning
confidence: 99%