Show simple item record

contributor authorMustafa Turan
date accessioned2017-05-08T21:08:55Z
date available2017-05-08T21:08:55Z
date copyrightSeptember 1992
date issued1992
identifier other%28asce%290733-9372%281992%29118%3A5%28776%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/40475
description abstractBackwashing of deep bed filters is achieved by fluidizing the filter media. A mathematical model for velocity gradient in two‐dimensional turbulent flow that can also be applied to flow in fluidized beds in the transitional state was developed. The theory of fluidization in a circular cross‐section column was presented. The existence of a viscous sublayer around each fluidized solid particle and the laminar sublayer thickness at the wall were neglected. To evaluate the theoretical expressions, numerical applications are carried out for filter‐bed materials of two different types of sands and anthracite coal. An indirect verification of the existence of an optimum porosity around 0.70‐0.75 during filter backwashing was observed in the laboratory experiments. The velocity gradient in backwashing of granular filters was found to be a function of power dissipation in a unit volume and coefficient
publisherAmerican Society of Civil Engineers
titleVelocity Gradient in Filter Backwashing
typeJournal Paper
journal volume118
journal issue5
journal titleJournal of Environmental Engineering
identifier doi10.1061/(ASCE)0733-9372(1992)118:5(776)
treeJournal of Environmental Engineering:;1992:;Volume ( 118 ):;issue: 005
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record