ON STEADY HOMOGENEOUS SAND-WATER FLOWS IN A VERTICAL CONDUIT

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dc.contributor.author Gallo F.
dc.contributor.author Woods A.W.
dc.date.accessioned 2022-10-30T05:34:03Z
dc.date.available 2022-10-30T05:34:03Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=6466611
dc.identifier.citation Sedimentology, 2004, 51, 2, 195-210
dc.identifier.issn 0037-0746
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/39290
dc.description.abstract In this paper, an idealized model of the steady-state phase of the flow in a vertical conduit leading to a sand volcano eruption is developed from first principles. The model assumes that a sand-water mixture flows upwards, driven by an overpressure at the base of a vertical cylindrical conduit (or a two-dimensional fracture) and opposed by gravity, viscous resistance and turbulent drag. The conditions for flow are analysed in detail, and the mechanisms controlling the eruption rates are studied quantitatively. The flow predictions are in accordance with our observations of analogous vigorous sand eruptions at deepwater oil fields. For sufficiently high flow velocities (u > 10u T ) and small sand fractions (s < 0·2), the flow may be well mixed and homogeneous. If these conditions are not met, the flow may either become two phase or does not develop. Combining geological considerations with the steady homogeneous model, it is possible to predict the behaviour of the vigorous quasi-steady stage of a sand volcano eruption. It is shown that, based on the average density of the overlying sediments, there are a range of overpressures for which sand volcanoes may develop.
dc.subject SAND VOLCANOES
dc.subject SANDSTONE DYKES (DIKES)
dc.subject SANDSTONE INTRUSIONS
dc.title ON STEADY HOMOGENEOUS SAND-WATER FLOWS IN A VERTICAL CONDUIT
dc.type Статья


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