Transcript
Page 1: Ф fl Ф Hyperspatial Thermal Imaging of Surface …

Hyp

ers

patia

l Therm

al I

mag

ing

of S

urf

ace H

ydro

therm

al F

eatu

res

at

Pilg

rim H

ot

Sp

ring

s,

Ala

ska u

sing

a s

mall

Unm

anned

Aeria

l Sys

tem

(sU

AS

)

Un

ivers

ity o

f A

lask

a F

airb

an

ks.

*C

orr

esp

on

din

g a

uth

or:

ch

rist

ian

@h

ase

lwim

mer.co

.uk

Ch

risti

an

Ha

se

lwim

me

r* , R

ayja

n W

ilso

n,

Co

rey U

pto

n,

An

up

ma

Pra

ka

sh

, G

we

n H

old

ma

nn

, a

nd

Gre

g W

alk

er

Ac

kn

ow

led

ge

me

nts

Th

is r

ese

arc

h i

s fu

nd

ed

by

the D

ep

art

men

t o

f E

nerg

y G

eo

therm

al

Tech

no

log

ies

Pro

gra

mm

e (

CID

: D

E-E

E0

00

28

46

) an

d t

he A

lask

a E

nerg

y A

uth

ority

Ren

ew

ab

le E

nerg

y F

un

d R

ou

nd

III.

Re

fere

nc

es

1.

Lis

s, S

.A. and

Mo

tyka, R

.J. (1

994) P

ilgrim

Sp

ring

s K

GR

A, S

ew

ard

Penin

sula

, A

lask

a: A

ssess

ment

of fluid

geo

chem

istr

y. G

eo

therm

al R

eso

urc

es

Co

uncil

Transa

ctio

ns,

Vo

l. 18.

2.

Hase

lwim

mer, C

.E., P

rakash

, A

., a

nd

Ho

ldm

ann,

G.

(2011)

Geo

therm

al

Exp

lora

tio

n a

t P

ilgrim

Ho

t S

pring

s, A

lask

a u

sing

airb

orn

e t

herm

al

infr

are

d r

em

ote

sensi

ng

. G

eo

therm

al

Reso

urc

es

Co

uncil

35th

Annual M

eeting

, O

ct

23-2

6, S

an D

ieg

o, C

alif

orn

ia.

3.

Hase

lwim

mer, C

.E.,P

rakash

, A

., a

nd

Ho

ldm

ann,

G., (

2013)

Quantify

ing

the h

eat flux a

nd

outfl

ow

rate

of

ho

t sp

ring

s usi

ng

airb

orn

e t

herm

al

imag

ery

: case

stu

dy

fro

m P

ilgrim

Ho

t S

pring

s,

Ala

ska, R

em

ote

Sensi

ng

of

Envi

ronm

ent,

136, 37-4

6, htt

p:/

/dx.d

oi.o

rg/1

0.1

016/j.r

se.2

013.0

4.0

08.

1. O

ve

rvie

w

• Very

hig

h s

patial

reso

lutio

n (

hyp

ers

patial)

therm

al

rem

ote

sensi

ng

fro

m s

mall

Un

man

ned

Aerial

Sys

tem

s (s

UA

S) has

po

tential t

o c

ontr

ibute

to

map

pin

g a

nd

mo

nito

ring

of

geo

therm

al f

eatu

res.

• sU

AS

dep

loye

d a

t P

ilgrim

Ho

t S

pring

s, A

lask

a w

ith t

he a

im o

f ass

ess

ing

th

e p

ote

ntial

an

d

pra

cticalit

ies

of

usi

ng

su

ch a sy

stem

fo

r g

eo

therm

al

exp

lora

tio

n an

d q

uan

tita

tive

re

sou

rce

ass

ess

ment.

• 4 c

m t

herm

al

imag

ery

pro

vid

ed

an u

np

reced

ente

d c

ap

ab

ility

fo

r m

ap

pin

g h

ot

sprin

gs,

seep

s,

and

th

e s

urf

ace fl

ow

of

geo

therm

al fl

uid

s.

• H

eat

bud

get

mo

del w

as

use

d t

o e

stim

ate

the h

ot

spring

heat flux a

nd

dis

ch

arg

e r

ate

fo

r p

art

of

the g

eo

therm

al

are

a f

rom

the c

alib

rate

d F

LIR

im

ag

ery

, w

hic

h w

as

co

mp

are

d a

gain

st i

n-s

itu

measu

rem

ents

.

4.

Da

ta P

rep

roc

essin

g

• D

ifficu

ltie

s w

ith

p

ho

tog

ram

metr

ic

pro

cessin

g

ap

pro

ach

led

to

u

se

of

sem

i-au

tom

ate

d

mo

saic

kin

g w

ith

PT

Gu

i u

sin

g a

uto

matic e

xp

osu

re

ad

just

men

t.

• M

osaic

m

an

ually

re

gis

tere

d

to

hig

h

reso

luti

on

airb

orn

e v

isib

le im

ag

e u

sin

g A

rcM

ap

.

• F

LIR

TA

U

2

is

un

calib

rate

d

cam

era

: m

osaic

calib

rate

d

usin

g

measu

red

te

mp

era

ture

s o

f

gro

un

d ta

rgets

su

ch

as

ho

t sp

rin

gs

and

b

lack

bo

dy

tarp

s.

5.

Ma

pp

ing

Su

rfa

ce

Hyd

roth

erm

al F

ea

ture

s

• 4

cm

reso

lutio

n t

herm

al

imag

ery

pro

vid

es

very

deta

iled

pic

ture

of

the l

ocatio

ns

and

exte

nts

of

ho

t sp

rin

gs

an

d t

he s

urf

ace o

utfl

ow

of

geo

therm

al fl

uid

s.

6. H

ot

Sp

rin

g H

ea

t F

lux E

sti

ma

tio

n

• H

eat

bud

get

mo

del

use

d t

o e

stim

ate

ho

t sp

ring

heat flux a

nd

outfl

ow

rate

fo

r p

art

of

the

geo

therm

al a

rea.

Heat

bud

get

for

a w

ate

r b

od

y (in

Watt

s) is

exp

ress

ed

as:

• M

od

el

inp

uts

: 1

) F

LIR

im

ag

ery

fo

r h

ot

wate

rs;

2)

atm

osp

heri

c

pro

pert

ies;

3) ave

rag

e t

em

pera

ture

of

no

n-g

eo

therm

al s

urf

ace p

oo

ls.

• sU

AS

FL

IR d

eri

ve

d h

ea

t fl

ux =

0.5

3 M

W,

low

er

than p

revi

ous

resu

lts

fro

m a

irb

orn

e F

LIR

[3] =

0.7

5 a

nd

0.8

6 M

W f

or

2010 a

nd

2011 d

ata

.

• R

esu

lts

co

mp

are

d ag

ain

st

heat flu

x esti

mate

s d

eri

ved

fr

om

in

-sit

u

me

asu

rem

en

ts o

f th

e fl

ow

ra

te (se

e c

ulv

ert

locatio

n o

n p

anel 5

).

• In

-situ fl

ow

rate

use

d t

o c

alc

ula

te a

dve

cti

ve

he

at fl

ux (Ф

adv)

thro

ug

h

the c

ulv

ert

(at

the m

easu

red

wate

r te

mp

) and

to

tal

ho

t sp

rin

g h

ea

t fl

ux

( Фge

o at

the h

ot

spring

tem

p o

f 81˚C

) usi

ng

:

Фad

v/ge

o = ṁ

(hs-h

amb)

w

here

ṁ is

th

e m

ass

flo

w r

ate

(l/s)

an

d h

s, h a

mb

are

en

thalp

ies

of

wate

r (k

J/k

g)

at

the s

prin

g (

in

this

case

fo

r b

oth

th

e m

easu

red

tem

p a

nd

ho

t sp

rin

g t

em

p) an

d a

mb

ien

t w

ate

r te

mp

era

ture

s.

• To

tal

ho

t sp

rin

g h

ea

t fl

ux f

rom

co

mb

ine

d s

UA

S/i

n-s

itu

= s

UA

S F

LIR

-derive

d h

eat flu

x (

0.5

3

MW

) +

calc

ula

ted

ad

vective

flux (0.4

2 M

W) =

0.9

5 M

W

• To

tal h

ot

sp

rin

g h

ea

t fl

ux f

rom

in

-sit

u o

nly

= 2

.93 M

W

• D

iffe

ren

ces

du

e to

p

oo

r calib

ratio

n o

f sU

AS

F

LIR

an

d p

ossib

le u

nd

ere

stim

atio

n

of

FL

IR

ap

pro

ach w

hen c

om

pare

d t

o in

-situ m

easu

rem

ents

.

7. O

utc

om

es

• sU

AS

acq

uired

hyp

ers

patial th

erm

al im

ag

ery

map

ped

cm

-scale

ho

t sp

ring

s and

seep

s, a

nd

th

e

exte

nts

of

ho

t w

ate

r w

ith m

uch g

reate

r d

eta

il th

an a

irb

orn

e t

herm

al i

mag

ery

.

• T

IR im

ag

ery

sho

ws

chang

es

in h

ot

spring

s p

oss

ibly

rela

ted

to

surf

ace h

ydro

log

ical c

on

ditio

ns.

• sU

AS

therm

al

imag

ery

did

no

t p

rovi

de r

elia

ble

est

imate

s o

f th

e h

ot

spring

heat flu

x d

ue t

o

sig

nifi

cant

err

ors

in t

em

pera

ture

calib

ratio

n o

f th

e d

ata

: d

ue t

o u

se o

f uncalib

rate

d c

am

era

.

• T

his

wo

rk h

ighlig

hte

d p

ractical is

sues

to b

e a

dd

ress

ed

befo

re s

UA

S c

an c

om

pete

with

airb

orn

e

therm

al i

mag

ing

such a

s sU

AS

batt

ery

life

, flig

ht

pla

nnin

g,

and

use

of

calib

rate

d s

enso

rs.

3. sU

AS

Da

ta C

olle

cti

on

• A

ery

on

Sco

ut

quad

co

pte

r eq

uip

ped

with F

LIR

TA

U 2

: 640 x

480 p

ixels

co

verin

g 7

.5 -

13

.5 μ

m.

• S

urv

ey flo

wn o

ver

Pilg

rim

Ho

t S

pring

s o

n 2

4/7

/2013:

calm

day

with h

igh

clo

ud

co

ver.

• 10

0m

flyi

ng

heig

ht

= ~

4cm

therm

al i

mag

ery

, flig

ht

lines

pla

nned

aro

und

exte

nt

of

ho

t sp

rin

gs

an

d

therm

al f

eatu

res

map

ped

fro

m ~

1.5

m a

irb

orn

e t

herm

al i

mag

ery

(flo

wn

in 2

01

0).

• ~

20 m

ins

batt

ery

life

(re

quired

fre

quent

retu

rns

to b

ase

), f

ully

auto

no

mo

us

execu

tio

n o

f su

rvey.

• C

oin

cid

en

t co

llectio

n o

f calib

ratio

n d

ata

: ho

t sp

ring

+ t

arp

tem

pera

ture

s, a

tmo

sph

eric v

ariab

les.

2.

Pilg

rim

Ho

t S

pri

ng

s,

Ala

sk

a

• G

eo

therm

al

syst

em

lo

cate

d ~

75

km

NE

of

No

me o

n S

ew

ard

Pen

insu

la.

• S

hallo

w 9

0ºC

aq

uifer

fed

fro

m d

eep

er

rese

rvo

irs

of

at

least

~1

10

-15

0ºC

[1

].

• D

OE

/AE

A f

un

ded

pro

ject

to u

nd

ert

ake

reso

urc

e e

xp

lora

tio

n a

nd

ass

ess

men

t.

• A

irb

orn

e F

LIR

pre

vio

usl

y u

sed

to

map

ho

t sp

ing

s an

d q

uan

tify

heat flu

x a

nd

outfl

ow

rate

: ~

4.7

-7 M

Wth

[2

,3].

01

00

20

05

0M

ete

rs0

30

60

ºC

Ho

t p

oo

ls

Aerial P

ho

tog

rap

h09/1

0/2

010

Ho

t sp

ring

s

Airb

orn

e T

herm

al

09/1

0/2

010

Aerial P

ho

tog

rap

h09/1

0/2

010

Airb

orn

e T

herm

al

09/1

0/2

010

Ala

sk

a

Pilg

rim

Ho

tS

pri

ngs

Le

ft: A

ery

on S

co

ut

quad

co

pte

r

Top

le

ft:

calib

ratio

n t

arg

et

(tem

pera

ture

reco

rded

with F

LIR

and

iButt

on lo

gg

er)

. To

p r

igh

t: t

em

po

rary

weath

er

statio

n

y =

0.0

00

8x +

10

.29

8

20

25

30

35

40

45

50

55

60

65 1

00

00

200

00

30

00

04

00

00

500

00

600

00

70

00

0

Dig

ital N

um

ber

Temperature (ºC)

Ab

ove

: lin

ear

gain

and

off

set

use

d t

o c

alib

rate

the

mo

saic

ked

therm

al i

mag

ery

to

surf

ace t

em

pera

ture

Ba

se

im

ag

e: m

osa

icked

FLIR

TA

U 2

therm

al i

mag

ery

o

verlain

on h

igh r

eso

lutio

n a

erial p

ho

tog

rap

h

Culv

ert

: in

-situ h

ot

spring

flo

w r

ate

05

01

00

25

Mete

rs

10

60

ºC

Churc

h

Calib

ratio

n t

arp

Calib

ratio

n t

arp

Airb

orn

e t

herm

al (

~1.5

m p

ixels

) -

09/1

0/2

010

sUA

S t

herm

al (

~4 c

m p

ixels

) -

07/2

4/2

013

010

Mete

rs

Sm

all

sprin

gs

(cm

scale

)

Seep

in

plu

ng

e p

oo

l

Wate

r su

rface fi

lms

sho

w

sub

tle t

em

p d

iffere

nce

sUA

S t

herm

al

Airb

orn

e t

herm

al

05

Mete

rs

Sp

ring

s no

t se

en

in a

irb

orn

e d

ata

Ho

t sp

ring

s no

t se

en

fro

m s

UA

S d

ata

• D

iffere

nces

in

tem

pera

ture

b

etw

een a

irb

orn

e

and

sU

AS

: p

oo

r calib

ratio

n o

f TA

U

2 d

ata

?

• D

iffere

nces

in

locatio

ns

of

ho

t sp

ring

s: lo

wer

wate

r ta

ble

and

chang

e in

surf

ace

outfl

ow

?

0W

att

s1

3

Ab

ove

: est

imate

d h

ot

spring

heat flux f

or

geo

therm

al

po

ols

(in

units

watt

s/p

ixel)

B4

1B

-03

93

Фto

tal =

Фge

o + Ф

ppt +

Фad

v + Ф

evap

+ Ф

sens

+ Ф

rad + Ф

sun

+ Ф

sky

Фge

o =

heat

inp

ut

fro

m g

eo

therm

al fl

uid

s

Фpp

t =

heat

inp

ut

fro

m p

recip

itatio

n

Фad

v =

heat flu

x f

rom

ad

vectio

n/s

eep

ag

e

Фev

ap

= h

eat

loss f

rom

evap

ora

tio

n

Фse

ns

= h

eat

loss v

ia s

en

sib

le h

eat

tran

sfe

r

Фra

d =

heat

loss b

y r

ad

iatio

n

Фsu

n =

heat

inp

ut

fro

m s

ola

r ra

dia

tio

n

Фsk

y =

h

eat

inp

ut

fro

m a

tmo

sp

heric r

ad

iatio

geo

Фad

v

Фpp

sunФ

evapФ

sens

Фra

sky

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