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Monodisperse and polydisperse colloid transport in water-saturated fractures with various orientations: Gravity effects

Chrysikopoulos Constantinos, Scott C. James

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URIhttp://purl.tuc.gr/dl/dias/BD0AACBA-B776-4111-A9A2-2D3E041F9D5A-
Αναγνωριστικόhttps://doi.org/ 10.1016/j.advwatres.2011.06.001 -
Γλώσσαen-
Μέγεθος7 pagesen
ΤίτλοςMonodisperse and polydisperse colloid transport in water-saturated fractures with various orientations: Gravity effectsen
ΔημιουργόςChrysikopoulos Constantinosen
ΔημιουργόςΧρυσικοπουλος Κωνσταντινοςel
ΔημιουργόςScott C. Jamesen
ΠερίληψηNumerical experiments are conducted to examine the effects of gravity on monodisperse and polydisperse colloid transport in water-saturated fractures with uniform aperture. Dense colloids travel in water-saturated fractures by advection and diffusion while subject to the influence of gravity. Colloids are assumed to neither attach onto the fracture walls nor penetrate the rock matrix based on the assumptions that they are inert and their size is larger than the pore size of the surrounding solid matrix. Both the size distribution of a colloid plume and colloid density are shown to be significant factors impacting their transport when gravitational forces are important. A constant-spatial-step particle-tracking code simulates colloid plumes with increasing densities transporting in water-saturated fractures while accounting for three forces acting on each particle: a deterministic advective force due to the Poiseuille flow field within the fracture, a random force caused by Brownian diffusion, and the gravitational force. Integer angles of fracture orientation with respect to the horizontal ranging from ±90 are considered: three lognormally distributed colloid plumes with mean particle size of 1 lm (averaged on a volumetric basis) and standard deviation of 0.6, 1.2 and 1.8 lm are examined. Colloid plumes are assigned densities of 1.25, 1.5, 1.75 and 2.0 g/cm3. The first four spatial moments and the first two temporal moments are estimated as functions of fracture orientation angle and colloid density. Several snapshots of colloid plumes in fractures of different orientations are presented. In all cases, larger particles tend to spread over wider sections of the fracture in the flow direction, but smaller particles can travel faster or slower than larger particles depending on fracture orientation angleen
ΤύποςPeer-Reviewed Journal Publicationen
ΤύποςΔημοσίευση σε Περιοδικό με Κριτέςel
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2015-09-19-
Ημερομηνία Δημοσίευσης2011-
Βιβλιογραφική ΑναφοράS. C. James , C.V. Chrysikopoulos , "Monodisperse and polydisperse colloid transport in water-saturated fractures with various orientations: Gravity effects " ,Advanc. in Wat.Resou. ,vol.3,no.10, pp. 1249–1255,2011.doi : 10.1016/j.advwatres.2011.06.001 en

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