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Schematic of a Conventional Surface Water Treatment Plant

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Title: Schematic of a Conventional Surface Water Treatment Plant


1
Schematic of a Conventional Surface Water
Treatment Plant
2
Filtration Processes
  • Filtration is used to remove
  • 1) Suspended particulate material such as small
    flocs or precipitant particles not removed in the
    settling of coagulated or softened waters.
  • 2) Turbidity-removal process such as direct
    filtration of a raw water.
  • 3) Pathogenic organisms such as Giardia Lamblia
    and Cryptosporidium. (3 - 10 ?m)

3
Filtration Processes
  • Types of filtration operations used in water
    treatment are
  • 1) Pressure Filtration
  • Expensive, Primary use in wastewater and
    industrial wastewater treatment,
  • Small Systems Q typically 2 to 4 gpm/ft2.
  • 2) Gravity Filtration Type
  • a) High Rate (2-10 gpm/ft2) or rapid sand
    filtration usually operates in the declining rate
    mode of operation, the most widely filtration
    process in water treatment.
  • b) Low Rate (0.05 gpm/ft2) or slow sand filters
    used mainly in Germany for groundwater recharge
    but also used in some small communities where a
    low turbidity surface water is used.

4
Filtration Processes
Typical Pressure Filter
5
Filtration Processes
Typical Gravity Filter
6
Filtration Processes
Gravity filtration rates will decline with time
as illustrated below
7
Filtration Process
  • Backwashing
  • Typically 50 bed expansion during backwashing
  • Water Backwash Rate 15 - 30 gpm/ft2
  • Air Backwash Rate 80 - 100 m/hr
  • Backwash Cycle Time 10 - 30 minutes

8
Filtration Process
  • Rapid Sand Filtration
  • Sand Only 0.3-0.8 mm in diameter (Effective
    size, d10)
  • 24-32 inches deep
  • uniformity coefficient ? (1.4-1.8) d60/d10
  • void fraction of bed, ? 0.4
  • Multimedia (Anthracite and Sand)
  • Coal 0.8-2 mm diameter,
  • ? 0.5 void fraction of bed
  • uniformity coefficient ? 1.4-1.8
  • ?coal 1.4
  • Sand 0.3-0.8 mm diameter, ? 0.4
  • uniformity coefficient ? 1.4-1.8
  • ? ? 2.6
  • Depths coal--8-24 inches
  • sand--10-24 inches

9
Filtration Process
  • Typical Sieve Analysis of Two Filter Media

10
Filtration Process
  • Example Grain Size Distribution

11
Filtration Process
  • d10 is the sieve size that 10 of the total
    weight of the sample is passing.

12
Filtration Process
  • Problem With Backwashing

Problem
Solution
13
Filtration Process
  • DEEP FILTRATION MECHANISMS
  • Calculation of the particle size which will just
    fit through the media

For DP 1 ?m Dm 6.49x10-4 cm For DP 100
?m Dm 6.49x10-2 cm
Rm (Rm RP) 0.866 RP 0.154 Rm DP 0.154 Dm
14
Filter Hydraulics
  • For design purposes it is important to describe
    the headloss through porous filters. In gravity
    filtration, the driving force is the head of
    water above the filter that overcomes the
    headloss through the filter which enables
    filtration of water. The headloss is a function
    of the following variables

15
Filter Hydraulics
  • In water treatment, gravity filtration is the
    normal mode of filter operation.
  • Clean Filter Headloss 1.5 to 2.5 ft.
  • Backwash Occurs when Hf 8 - 10 ft.
  • The Carmen- Kozeny Equation describes the
    headloss in granular filters.

16
Filter Hydraulics
  • The following expression can be used to calculate
    the headloss through a clean filter media

1
Carmen-Kozeny Equation
17
Filter Hydraulics
  • Friction Factor Correlation

2
3
18
Filter Hydraulics
The Carmen-Kozeny equation and NR includes a
correction factor for granular materials which
are not spherical. The term is called particle
sphericity, ?.
  • ? 1.0 for spherical particles
  • 0.73 for pulverized coal angular sand
  • 0.95 Ottawa sand
  • 0.82 for rounded sand

19
Filter Hydraulics
  • Now that we have developed a headloss expression
    for uniform sized filter medium in a filter bed,
    the same expression can be modified for
    non-uniform filter medium.
  • The results of a sieve analysis will give the
    weight fraction between each adjacent sieve size,
    Xij. The average particle size, dij, is assumed
    to be halfway between the sieve sizes and is
    called the equivalent diameter.

di and dj are the sieve openings. This is called
the geometric mean particle size.
20
Filter Hydraulics
  • The depth of the particles between adjacent sieve
    sizes can be taken as Xij L and Eq. 1 can be
    rewritten as

4
This equation assumes that the filter bed is
stratified by size and the porosity is uniform
throughout the bed.
21
Filter Hydraulics
  • Notes
  • Equations 1 and 4 are applicable only to clean
    filters.
  • Porosity changes with time as particles
    accumulate.
  • A constant filter velocity will require an
    increase in the driving force to match the
    headloss resulting from the decrease in the
    porosity.

22
Filter Hydraulics
  • Notes
  • In filter operation, a filter run is decreased
    when sufficient solids have deposited onto the
    filter media to
  • 1) Exhaust the available driving source.
  • 2) Cause the filter velocity to drop below a
    predetermined level.
  • 3) Exhaust the storage capacity of the bed so
    that solids begin to appear in the effluent.
  • At this point the filter must be backwashed

23
Filter Backwash Hydraulics
  • Particle in Fluid

24
Filter Backwash Hydraulics
  • Force balance on a collector particle being
    backwashed.

25
Filter Backwash Hydraulics
26
Filter Backwash Hydraulics
5
  • where hfb head loss required to initiate
    expansion (m)
  • L bed length (m)
  • (1-?) fraction of packed bed occupied by the
    granular media (-)
  • ?m density of the medium (Kg/m3)
  • ?w density of the water (Kg/m3)

27
Filter Backwash Hydraulics
Lfb

L
?
?fb
  • The headloss through the expanded bed is same as
    the headloss required to initiate expansion
    because the buoyant force of the bed is constant.

28
Filter Backwash Hydraulics
  • Mass of Packed Bed Mass of Fluidized Bed

6
7
29
Filter Backwash Hydraulics
  • ?fb f(terminal settling velocity of the
    particles and the backwash velocity)

The relationship between backwash velocity and
terminal settling velocity of the particles is
8
VB backwash velocity (QB/A) Vt terminal
settling velocity of the filter media
30
Filter Backwash Hydraulics
  • The terminal settling velocity of the collector
    particles can be calculated based on Newtons Law
    of Settling.

31
Filter Backwash Hydraulics
  • The depth of the fluidized bed and backwash
    velocity for a given medium size can be related
    as

9
This equation can be modified for a stratified
bed of non-uniform sized collector particles
10
32
Filter Backwash Hydraulics
  • Assuming uniform porosity in the packed bed, Lij
    will be the depth of the layer of media
    represented by Xij. The expression of this layer
    is represented by

11
33
Filter Hydraulics
  • The total expansion is the sum of the individual
    layers

12
Total expansion is usually 120 to 155 percent of
the unexpanded bed. The optimum expansion for
hydraulic backwashing occurs at expanded
porosities of 0.65 to 0.70.
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