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Posttreatment fines migration

Posttreatment fines migration is quite common in sandstone acidizing. It may be difficult to avoid in many cases. The reaction of HE with clays and other aluminosilicate minerals and quartz can release undissolved fines. Also, new fines may be generated as a result of partial reaction with high-surface-area minerals, particularly clays and certain zeolites, in which they more rarely occur. [Pg.40]


See other pages where Posttreatment fines migration is mentioned: [Pg.36]    [Pg.40]    [Pg.36]    [Pg.40]    [Pg.36]    [Pg.40]    [Pg.36]    [Pg.40]   
See also in sourсe #XX -- [ Pg.40 ]

See also in sourсe #XX -- [ Pg.40 ]




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