1
CRICOS Provider Number 00025B Acknowledgements This research has been conducted with the support of Energi Simulation and The University of Queensland Centre for Coal Seam Gas (UQ-CCSG) and its industry members – APLNG, Arrow Energy, Shell and Santos. Dr Mohsen S. Masoudian 1 [[email protected]], Dr Christopher Leonardi 1 , Dr Zhongwei Chen 1 , Prof. Jim Underschultz 2 , Prof. Suzanne Hurter 3, 4 1 The University of Queensland, School of Mechanical and Mining Engineering 2 The University of Queensland Energy Initiative 3 The University of Queensland Centre for Coal Seam Gas 4 Energi Simulation Industrial Research Chair Mechanisms of natural surface movement in the Surat Basin Surface movement in FA1 Summary Ground surface movement can be due to natural processes and human activities. This project aims to understand the mechanisms of ground surface movement and their individual contributions to net movement. A large Interferometric Synthetic Aperture Radar (InSAR) dataset covering the Surat Cumulative Management Area was analysed, focusing on areas where there are no active coal seam gas (CSG) wells. These non-production areas have been examined to develop an understanding of background surface movement. Four focus areas, showing measureable changes over time, exhibited an overall downward surface movement (subsidence). Three focus areas showed cycles of subsidence and uplift that appear to be closely correlated with rainfall events – as shown in the results for FA1. The soil types in these three areas were found to be in agreement with the hypothesis that the observed surface movement is due to rainfall infiltration-induced consolidation of the shallow soil layers and also subsequent moisture-induced shrinkage and swelling. This investigation has provided a foundation for further research into the complex problem of surface movement, and in particular, the deconvolution of the various contributions that occur at different depths, length and time scales. UQ-CCSG Annual Research Review 2018 Centre for Coal Seam Gas

3, 4 , Prof. Suzanne Hurter - University of Queensland...Microsoft PowerPoint - UQ-CCSG Research Review 2018 - Poster - Masoudian, Mohsen - v2 FINAL [landscape].pptx Author uqsmoo10

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Page 1: 3, 4 , Prof. Suzanne Hurter - University of Queensland...Microsoft PowerPoint - UQ-CCSG Research Review 2018 - Poster - Masoudian, Mohsen - v2 FINAL [landscape].pptx Author uqsmoo10

CR

ICO

S Pr

ovid

er N

umbe

r 000

25B

Ackn

owle

dgem

ents

This

rese

arch

has

bee

n co

nduc

ted

with

the

supp

ort o

f Ene

rgiS

imul

atio

n an

d Th

e U

nive

rsity

of Q

ueen

slan

d C

entre

for C

oal S

eam

Gas

(UQ

-CC

SG) a

nd it

s in

dust

ry m

embe

rs –

APLN

G, A

rrow

Ene

rgy,

She

ll an

d Sa

ntos

.

Dr M

ohse

n S.

Mas

oudi

an1

[m.m

asou

dian

@uq

.edu

.au]

, Dr C

hris

toph

er L

eona

rdi1 ,

Dr Z

hong

wei

Che

n1, P

rof.

Jim

Und

ersc

hultz

2 , Pr

of. S

uzan

ne H

urte

r3, 4

1 The

Uni

vers

ity o

f Que

ensl

and,

Sch

ool o

f Mec

hani

cal a

nd M

inin

g En

gine

erin

g 2 T

he U

nive

rsity

of Q

ueen

slan

d En

ergy

Initi

ativ

e 3 T

he U

nive

rsity

of Q

ueen

slan

d C

entr

e fo

r Coa

l Sea

m G

as 4

Ener

gi S

imul

atio

n In

dust

rial R

esea

rch

Cha

ir

Mec

hani

sms

of n

atur

al s

urfa

ce m

ovem

ent i

n th

e Su

rat B

asin

Surf

ace

mov

emen

t in

FA1

Sum

mar

yG

roun

d su

rface

mov

emen

t can

be

due

to n

atur

al p

roce

sses

and

hum

an a

ctiv

ities

. Th

is p

roje

ct a

ims

to u

nder

stan

d th

e m

echa

nism

s of

gro

und

surfa

ce m

ovem

ent a

nd

thei

r ind

ivid

ual c

ontri

butio

ns to

net

mov

emen

t. A

larg

e In

terfe

rom

etric

Syn

thet

ic A

pertu

re R

adar

(InS

AR) d

atas

et c

over

ing

the

Sura

t Cum

ulat

ive

Man

agem

ent A

rea

was

ana

lyse

d, fo

cusi

ng o

n ar

eas

whe

re th

ere

are

no a

ctiv

e co

al s

eam

gas

(CSG

) wel

ls. T

hese

non

-pro

duct

ion

area

s ha

ve b

een

exam

ined

to d

evel

op a

n un

ders

tand

ing

of b

ackg

roun

d su

rface

mov

emen

t. Fo

ur fo

cus

area

s, s

how

ing

mea

sure

able

cha

nges

ove

r tim

e, e

xhib

ited

an o

vera

ll do

wnw

ard

surfa

ce m

ovem

ent (

subs

iden

ce).

Thre

e fo

cus

area

s sh

owed

cyc

les

of

subs

iden

ce a

nd u

plift

that

app

ear t

o be

clo

sely

cor

rela

ted

with

rain

fall

even

ts –

as

show

n in

the

resu

lts fo

r FA1

. The

soi

l typ

es in

thes

e th

ree

area

s w

ere

foun

d to

be

in

agre

emen

t with

the

hypo

thes

is th

at th

e ob

serv

ed s

urfa

ce m

ovem

ent i

s du

e to

ra

infa

ll in

filtra

tion-

indu

ced

cons

olid

atio

n of

the

shal

low

soi

l lay

ers

and

also

su

bseq

uent

moi

stur

e-in

duce

d sh

rinka

ge a

nd s

wel

ling.

Th

is in

vest

igat

ion

has

prov

ided

a fo

unda

tion

for f

urth

er re

sear

ch in

to th

e co

mpl

ex

prob

lem

of s

urfa

ce m

ovem

ent,

and

in p

artic

ular

, the

dec

onvo

lutio

n of

the

vario

us

cont

ribut

ions

that

occ

ur a

t diff

eren

t dep

ths,

leng

th a

nd ti

me

scal

es.

UQ

-CC

SG A

nnua

l Res

earc

h R

evie

w

2018

Cen

tre

for C

oal S

eam

Gas