unsaturated flow at gardermoen during periods of extreme high infiltration intensities. nils-otto...

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Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department of Hydrology, University of Oslo

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Page 1: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

Unsaturated flow at Gardermoen during periods of extreme

high infiltration intensities.

    

Nils-Otto Kitterød,

Thorgeir Holm and Wai Kwok Wong

Department of Hydrology, University of Oslo

Page 2: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

2

6670000

6672000

6674000

6676000

6678000

6680000

6682000

612000 614000 616000 618000 620000 622000

UTM-E

UT

M-N

Glacier fronts:TrandumHelgebostadVilbergBråtenDanielseter

Location of boreholes and the four most important glacier fronts.

Page 3: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

3

Oslo airport Gardermoen

utm-E

utm-N

616 000 618 000

6672500

6674500

6676500

6678500

614 000

railwayrunways

study area

SW

NE

Page 4: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

4

scatter plot of Ks based on d10/d60

1.00E-12

1.00E-11

1.00E-10

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1.00E-01

150 160 170 180 190 200 210 220

m o.h.

Em

pir

ica

l

Ks

<m

/s>

sampling elevation

0

100

200

300

400

500

600

700

800

150 160 170 180 190 200 210 220 230

m a.s.l.

f(x)

scatter plot of porosity based on d10/d60

0.05

0.10

0.15

0.20

0.25

0.30

150 160 170 180 190 200 210 220

m o.h.

Em

pir

ica

l po

ros

ity

Page 5: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

5

scatter plot of Ks based on d10/d60

1.00E-12

1.00E-11

1.00E-10

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1.00E-01

150 160 170 180 190 200 210 220

m o.h.

Em

pir

ical

K

s <

m/s

>

(emp)

Garderm. average (open)

0

2

4

6

8

10

12

14

16

18

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6

theta_1

the

ta_

2

Garderm. estim.

Garderm. average

Garderm. Min

Garderm. Max

Gustavson(1983)

Supra symetric average on Gustavson

Supra symetric min. on Gustavson

Page 6: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

6

Page 7: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

7

scatter plot of topset Ks

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

6670000 6672000 6674000 6676000 6678000 6680000

UTM-N

Em

pir

ical

K

s <m

/s>

scatter plot of topset Ks

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

614000 615000 616000 617000 618000 619000 620000

UTM-E

Em

pir

ica

l K

s <

m/s

>

scatter plot of topset Ks

1.00E-12

1.00E-11

1.00E-10

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1.00E-01

150 160 170 180 190 200 210 220

m o.h.

Em

piri

cal

Ks

<m/s

>

Page 8: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

8

scatter plot of topset Ks

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

900 1900 2900 3900 4900 5900

distance from Trandum outlet <m>

Em

pir

ica

l K

s <

m/s

>

scatter plot of topset Ks

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1300 2300 3300 4300 5300 6300 7300

distance from Helgebostad outlet <m>

Em

pir

ica

l K

s <

m/s

>

scatter plot of topset Ks

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

0 2.5 5 7.5 10 12.5 15

depth below terrain <m>

Em

pir

ica

l K

s <

m/s

>

Page 9: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

9

Histogram of Ks

0

100

200

300

400

500

600

700

800

900

1.00E-10 1.00E-08 1.00E-06 1.00E-04 1.00E-02 1.00E+00

Ks

N

all

topset

channel

overbank

Histogram of porosity

0

100

200

300

400

500

600

0.00 0.05 0.10 0.15 0.20 0.25 0.30 0.35

porosity

N

all

topset

channel

overbank

0.05

0.07

0.09

0.11

0.13

0.15

0.17

0.19

0.21

0.23

0.25

1.E-09 1.E-08 1.E-07 1.E-06 1.E-05 1.E-04 1.E-03 1.E-02

ks <m/s>

po

ros

ity

topset

Page 10: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

10

scatter plot of Ks

1.00E-12

1.00E-11

1.00E-10

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1.00E-01

150 160 170 180 190 200 210 220

m o.h.

Em

pir

ica

l K

s <

m/s

>

scatter plot of foreset sand Ks

1.00E-05

1.00E-04

1.00E-03

1.00E-02

900 1900 2900 3900 4900 5900

distance from Trandum outlet <m>

Em

pir

ica

l K

s <

m/s

>

Page 11: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

11

Histogram of Ks

0

100

200

300

400

500

600

700

800

900

1.00E-10 1.00E-08 1.00E-06 1.00E-04 1.00E-02 1.00E+00

Ks

N

all

topset

foreset sand

channel

Histogram of porosity

0

100

200

300

400

500

600

0.00 0.05 0.10 0.15 0.20 0.25 0.30 0.35

porosity

N

all

topset

channel

foreset sand

0.15

0.16

0.17

0.18

0.19

0.20

0.21

0.22

0.23

0.24

0.25

1.E-06 1.E-05 1.E-04 1.E-03 1.E-02

ks <m/s>

po

ros

ity

foreset sand

Page 12: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

12

scatter plot of Ks

1.00E-12

1.00E-11

1.00E-10

1.00E-09

1.00E-08

1.00E-07

1.00E-06

1.00E-05

1.00E-04

1.00E-03

1.00E-02

1.00E-01

150 160 170 180 190 200 210 220

m o.h.

Em

pir

ica

l K

s <

m/s

>

scatter plot of foreset silt Ks

0.00

10.00

20.00

30.00

40.00

50.00

60.00

70.00

80.00

90.00

100.00

900 1900 2900 3900 4900 5900

distance from Trandum outlet <m>

<m

a.s

.l.>

1.00E-10

1.00E-09

1.00E-08

1.00E-07

Em

pir

ical

Ks

<m

/s>

depth below surface

Ks silt

Page 13: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

13

Ks

0

100

200

300

400

500

600

700

800

900

1.00E-10 1.00E-08 1.00E-06 1.00E-04 1.00E-02 1.00E+00

Ks

N

all

topset

foreset sand

channel

foreset silt

porosity

0

100

200

300

400

500

600

0.00 0.05 0.10 0.15 0.20 0.25 0.30 0.35

porosity

N

all

topset

channel

foreset sand

foreset silt

0.05

0.07

0.09

0.11

0.13

0.15

0.17

0.19

0.21

1.E-09 1.E-08 1.E-07 1.E-06

ks <m/s>

po

ros

ity

foreset_silt

Page 14: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

14

Jonasons (1991) d25_d75 method

0

1

2

3

4

5

6

7

8

9

10

0 20 40 60 80 100 120 140

sample

van

Gen

uch

ten

s n

-1

0

1

2

3

4

5

6

7

8

9

lam

bd

a =

n -

1

Jonasons (1991) d25_d75 method

0

10

20

30

40

50

60

0 2 4 6 8 10van Genuchten's n

N

all

topset

foreset

Page 15: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

15

d25_d75

0

10

20

30

40

50

60

70

80

90

100

0.1 10.0 1000.0 100000.01/a (air entry pressure) <cm>

N

Jonasons (1991) d25_d75 method

0.1

1.0

10.0

100.0

1000.0

1.00 10.00

van Genuchten's n

1/a

(air

en

try

pre

ssu

re)

<cm

>

Page 16: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

16

Summary of empirical flow parameter data analyses

Ks <m/s> mY stdY 2.50 % 15.87 % 84.13 % 97.50 %topset_channel 5.49E-04 3.21E-04 1.64E-04 2.76E-04 8.15E-04 1.37E-03foreset_sand 2.83E-04 3.52E-04 2.66E-05 6.73E-05 4.66E-04 1.18E-03foreset_silt 2.38E-08 1.97E-08 4.46E-09 8.91E-09 3.78E-08 7.55E-08

porosity (effective) mY stdY 2.50 % 15.87 % 84.13 % 97.50 %topset_channel 0.22 0.02 0.19 0.20 0.23 0.25foreset_sand 0.23 0.02 0.19 0.21 0.24 0.26foreset_silt 0.14 0.03 0.08 0.11 0.17 0.20

van Genuchten's n mY stdY 2.50 % 15.87 % 84.13 % 97.50 %topset_channel 1.98 0.63 0.73* 1.35 2.60 3.23foreset_sand 4.28 0.56 3.17 3.73 4.84 5.40

* nonphysical value

1/a [cm] mY stdY 2.50 % 15.87 % 84.13 % 97.50 %topset_channelforeset_sand 10.00 5.00 15.00

’Rock’ parameters entered in TOUGH2 for unsaturated flow computations

Most likely' (E{X}) por. Kx Ky Kz Slr vG_n 1/a- m2 m2 m2 - - [Pa]

topset sand (top2) 0.28 9.26E-10 9.26E-10 9.26E-11 0.23 2.00 300foreset sand (dip1) 0.28 4.77E-10 4.77E-10 4.77E-11 0.20 3.10 1000foreset silt (dip2) 0.20 4.02E-15 4.02E-15 1.08E-15 0.33 2.10 2000

Min (.025 quantile) por. Kx Ky Kz Slr vG_n 1/a- m2 m2 m2 - - [Pa]

topset sand (top2) 0.20 2.57E-10 2.75E-10 2.75E-11 0.08 1.1 100foreset sand (dip1) 0.20 2.25E-10 2.25E-10 2.25E-11 0.04 1.5 500foreset silt (dip2) 0.10 7.52E-16 7.52E-16 2.06E-16 0.25 1.5 1000

Max (.975 quantile) por. Kx Ky Kz Slr vG_n 1/a- m2 m2 m2 - - [Pa]

topset sand (top2) 0.40 2.13E-09 2.13E-09 2.13E-10 0.39 2.5 500foreset sand (dip1) 0.40 2.00E-09 2.00E-09 2.00E-10 0.36 4.6 2500foreset silt (dip2) 0.40 1.27E-14 1.27E-14 3.37E-13 0.35 3.6 3000

Page 17: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

17

-3.7

-2.7

-1.7

-0.7

0 2 4 6 8 10 12

West-East <m>

depth

belo

w s

urf

ace <

m>

-3.7

-2.7

-1.7

-0.7S

-3.7

-2.7

-1.7

-0.7

0 2 4 6 8 10 12

West-East <m>

depth

belo

w s

urf

ace <

m>

-3.7

-2.7

-1.7

-0.7H

250 mm/d100 mm/d42 mm/d15 mm/d10 mm/d5 mm/d

NE (grw 11 m)SW (grw 3.7m)

1/ Kh_Kv Ks por Slr vG_n

Total: 672 flow fields

Page 18: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

18

Page 19: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

19

Søvik and Alfnes et al. (2001) Moreppen tracer test

0.00

0.20

0.40

0.60

0.80

1.00

0.00 5.00 10.00 15.00 20.00 25.00 30.00

time <days>

brom

ide

<rel

ativ

e co

ncen

trat

ion>

0.00

0.20

0.40

0.60

0.80

1.00

br(-2.95m)

br(-3.09m)

42mm/SV/S min

42mm/SV/S max

42mm/SV/H min

42mm/SV/H max

HTO(-2.84m)

HTO(-3.09m)

HTO(-3.30m)

Page 20: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

20

Søvik and Alfnes et al. (2001) Moreppen tracer test

0.00

0.25

0.50

0.75

1.00

0.00 5.00 10.00 15.00 20.00 25.00 30.00

time <days>

<rel

ativ

e co

ncen

trat

ion>

br(-2.95m)

br(-3.09m)

HTO(-2.84m)

HTO(-3.09m)

HTO(-3.30m)

42mm/SV/S min

42mm/SV/S max

42mm/SV/H min

42mm/SV/H max

0.50

0.20

Page 21: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

21

Page 22: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

22

Page 23: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

23

Page 24: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

24

Page 25: Unsaturated flow at Gardermoen during periods of extreme high infiltration intensities. Nils-Otto Kitterød, Thorgeir Holm and Wai Kwok Wong Department

25