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Flow through Soils II (ch8)
23

Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Dec 16, 2015

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Gregory Harn
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Page 1: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flow through Soils II(ch8)

Page 2: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

2D flow

Vel. vectors are confined to a single plane

1D flow vel vectors parallel

2D flow vel vectors not necessarily parallel

wall

soil

Page 3: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Laplace’s Equation

dxx

vv xx

zv

xv

1D flow - Darcy’s law 2D flow - Laplace’s equation

dzz

vv zz

x

z

dz

dx L

Rate of in vel in z-dir

Page 4: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Laplace’s Equation

Laplace’s equation

“represents energy loss through any resistive medium”

Assumptions

Darcy is valid

S = 100%

is of constant volume

Isotropic kx = kz

Homogeneous k = same throughout

Page 5: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Remember main point = get Q

Examples

Q beneath a dam Q in excavations

Solving

Mathematics

02

2

2

2

z

h

x

h

Graphical

Flownets

Page 6: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets

Flowline

wall

impervious

Equipotential line

Flowpath – “channel” between two flowlines

Equipotential line – along any eqpl, the total head is the same

Page 7: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets

1st eqpl: starts in inlet

last eqpl: ends at outlet

impervious

1st eqpl

Of soil

last eqpl

Page 8: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets

vel

Flowline

Flowline

node

eqpl

Requirements:

Perpendicular crossings at nodes

Maintain “squareosity”

Page 9: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets

X

Mistake – redraw!

Page 10: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets - Example

10m

14m

2m

L = 100 m

k = .1 cm/s

2m

A

B

Page 11: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets - Example

h = 14 – 2 = 12 m

h at first eq = 24 m

Q = h L k (NFP/NED)

Q = 0.3 m3/sec

NFP = 3

NED = 12

h at last eq = 12 m

Page 12: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets - Example

h at first eq = 24 m

Head loss per drop = h/NED = 12 / 12 = 1 m

he at A = 8 m

h at A = 24 – 8 = 16 m

hp at A = h – he = 16 – 8 = 8 m

uA = (hp)(w) = 78.5 kPa

Page 13: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Flownets - Example

h at first eq = 24 m

Head loss per drop = h/NED = 12 / 12 = 1 m

he at B = 10 m

h at B = 24 – 9 = 15 m

hp at B = h – he = 15 – 10 = 5 m

uB = (hp)(w) = 49 kPa

Page 14: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Uplift pressures

Concrete dam

uuplift

Concrete dam

= W/A

If uuplift ~ , structure can float away!

Page 15: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Uplift Pressures

Case 1 (no flow)

u = (hp)(w) = uhydrostatic

Draw flownet

Compute h at several points along the structure’s base

Determine hp at these points

Case 2 (with flow)

Find u at these points by u = (hp)(w)

Page 16: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Filters

Problem

- water pressure

- soil filter

- Soil particles migrate out

Sol.

- drains

Problem

Sol.

Page 17: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Filters

2 filter purposes

Allow adequate drainage

Soil retained is called base soil

Disallow particle migration

Filter soil

Page 18: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Filters

2 filter failure types

Clogging: base clogs filter pores – (k decreases)

Piping: base migrates through filter

Page 19: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

D

dmax

D

dmax

Simple Cubic Packing

D/dmax = 2.4

Tetrahedral Packing

D/dmax = 6.5

Interstice SizesFilters - principles

Page 20: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Arching Bridging

Filters - principles

Page 21: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

To disallow particle migration

To allow adequate drainage (maintain proper k)

Terzaghi’s Filter criteria

5485

15 tod

D 54

15

15 tod

D

Page 22: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

See table 8.2 in book… Example:

Sherard’s Filter criteria

Page 23: Flow through Soils II (ch8). 2D flow Vel. vectors are confined to a single plane 1D flow vel vectors parallel 2D flow vel vectors not necessarily parallel.

Example (see notes (pad (lined sheet))…

Example: Filter selection