Non-local behavior in Geomorphology: Vaughan R Voller, [email protected] NCED Summer Institute,...
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Transcript of Non-local behavior in Geomorphology: Vaughan R Voller, [email protected] NCED Summer Institute,...
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
Objectives
-- Define anomalous diffusion
-- Illustration of normal, sub and super diffusion
--Outline some very basic elements of factional calculus
-- Provide an explicit physical connection between the order of fractional derivatives and sub and super diffusion processes
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
Despite our best efforts we can not be in two places at once
Hence our intuitive physical sense of the world is based on LOCAL information
Local
At a point
dx
dq
slope
At an instant
dt
dv
rate
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
DEPENDENT PATH
dx
dq
dt
dv
But many physical process are NON-LOCAL
Holdup – releaseDepends on time scale
Extensive developing literature that argues that these non local processCan be described by Fractional Derivatives
dx
dq
dx
dv 1,0
!!! How on earth do we associate these constructs with our intuitively locally?
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
A physically incomplete but meaningful analogy to describe anomalous diffusion
How will drop of colored water spread out on tissue after time t ?
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
How will drop of colored water spread out on tissue after time t ?
rsubrn
rsup
If blot radius grows as
21
~ trn
Diffusion is said to be normal
If the time exponent differs from ½ Diffusion is said to be anomalous
Supper Diffusion
21
sup ;~ tr
Sub Diffusion
21;~ trsub
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
How will drop of colored water spread out on tissue after time t ?
rsubrn
rsup
21
~ trnnormalSupper Diffusion
21
sup ;~ tr
Sub Diffusion
21;~ trsub
Described by
)( Ct
C
Transientchange in volume
Divergence of flux(volume balance)
1,0),(
Ct
C
1,0 How do the exponents in the frac. Dervs. relate to sub or supper diffusion
non zero waitnon local flux
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
1,0 How do the exponents in the frac. Dervs. relate to sub or supper diffusion ?
To answer we consider a well known limit problem for flow in porous media
fixed head 00 hh
0x
0)( shfixed head
)(tsx sharp Moving Front between saturated and dry
Water supply saturated dry
Gov. equ.(mass con + Darcy)
)(0,0 tsxx
h
x
Note transient limits
Extra volume balance condition at front
dt
ds
x
h
ts
)(
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
)(0,0 tsxx
h
x
Extra volume balance condition at front
dt
ds
x
h
ts
)(
solution satisfying conditions
s
xh 1
sub here
21
20)0(,1 tssdt
dss
Darcy Flux assumes normal diffusionThis results in advance of saturated region with characteristic time scale 2
1
~ t
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
)(0,0 tsxx
h
x
Now let us look at problem with fractional derivatives
dt
sd
x
h
ts )(
If our fractional derivatives are Caputo derivatives (see below) then we can easily solve this problem. The result is a wetting front that moves as
1,0,11
0,~
ts
So choice of fractional exponents allows us to Move from a sub to super diff. behavior
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
To solve fractional derivative version of problem we use Caputo derivatives
10,)(
1
1)(
0
dd
dfx
dx
xfd x
a
Can evaluate using Lapalce transform
xfLsdx
xfdL
)( 0)(limand 10
0
xf
xIF
For solution of problem all you need to know is that
1or 1if,
1
1 and 0constant)(
xx
x
x
gamma function
1
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
)(0,0 tsxx
h
x
Now let us look at problem with fractional derivatives
dt
sd
x
h
ts )(
s
xh 1
solution satisfying conditions
sx
h )1(
Atssdt
sds 0)0(,1
11
)1(
)1()1(
A1
10
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
)(0,0 tsxx
h
x
dt
sd
x
h
ts )(
s
xh 1 Ats
11
)1(
)1()1(
A1
10
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
01h
0x
0)( sh
)(tsx
saturated dry
)(0,0 tsxx
h
x
dt
sd
x
h
ts )(
Ats 11
0
Observations: For appropriate choices of fractional derivativesSuper >.5, normal = .5 , or sub <.5 diffusion can be realized
If only flux fractional derivative is used 0 < < 1, = 1 then ONLYSuper diff can be realized
If only trans. fractional derivative is used 0 < < 1, = 1 then ONLYSub diff can be realized
Non-local behavior in Geomorphology: Vaughan R Voller, [email protected]
NCED Summer Institute, 4:30-6:00 pm, August 19, 2009
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
0 0.5 1 1.5 2
time(t)
dist
ance
s
=0.95
=0.5
=0.75
=0.05
=0.25
)1,1.(05.0 ),2.,3.(25.0 ),5.,75.(5.0 )052632.,1(95.0
Figure 1: Movement of the liquid/solid interface for choices of time fractional and flux fractional derivatives
.
)1333.,85.(75.0
This simple problem has allowed for a “trivial” solution to aFractional PDE. A solutionthat has provided a clear physicalconnection between the orderof the fractional derivative and thenature of the anomalous diffusion