Upload
others
View
0
Download
0
Embed Size (px)
Citation preview
Soil
Ind
icat
ors
of Q
uee
nsla
nd W
etla
nds 18 Mile Swamp
North Stradbroke Island
Study AreaThe 18 Mile Swamp is located on North Stradbroke Island, South-East Queensland.
The swamp is approximately 3000 ha in size which runs along the eastern side of the island1.
This site is an example of a coastal and sub-coastal non-floodplain grass, sedge, herb swamp with organic soils in the South-East Queensland Bioregion.
Climate2
0
100
200
300
400
500
600
700
800
900
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov DecMonth
Rai
nfal
l-Eva
pora
tion
(mm
)
0
5
10
15
20
25
30
35
40
Tem
pera
ture
(Deg
.C)
Rain Evap
Temp (min) Temp (max)
The study area is situated within a subtropical climatic region with a wet and dry season. Rainfall exceeds evaporation in the majority of months. The average annual rainfall within the area is 1668 mm.
Landform and Inundation
Open depression swamp within a coastal dune system Permanent freshwater inundation from groundwater and overland flow
Soils3 Podosols and Organosols4 Swamps with Baumea spp., Juncus spp. and Lepironia articulata
(RE 12.2.1����2.2.1����
Geology� Estuarine, floodplain and tidal delta deposits
Disturbance Little to no disturbance
Soil
In
dic
ator
s of
Q
ue
ensl
and
W
etla
nd
s Location GDA94 • MGA Coordinates : �491�8 E, 69��931 N, Zone �6 • Lat/Long : -27.�1944 S, 1�3.49777 E
Landscape Diagram
Site 124
Foredune Outer zone
Water table
Site 125
Site 126
Saturated zone
Track 1.3m
Site 128 Site 127
Sedge species Isolated Melaleuca quinqunervia
60 m
Soil ProfilesSite 124
0.08 m
A11
0.� m
0.7 m
1.0 m
A12
A21e
A22e
Site 127Site 128
0.1 m
P11
0.6 m
P12
0.1 m
P11
0.3 m
P12
Fibrous loam, dark colours and presence of sulfidic materials all indicate a permanently reduced
environment
Low chroma values in the surface 0.08 m is the only wetland soil indicator observed
For soils dominated by sand textures, low chroma values alone are not considered good indicators of
wetland soils without additional indicators
such as organic materials, redox
features (like mottles��� or ferruginous root channels and pore
linings6
Soil
In
dic
ator
s of
Q
ue
ensl
and
W
etla
nd
s Soil Indicators Present (within 0.3 m of surface)
Indicator7 Site 124 Site 125 Site 126Organic materials and organic carbon (OC)*
No organic materials OC: 1.82%
Organic materials to 0.3 m OC: 26.3%
Organic materials to 0.3 m OC: 34.4%
Matrix colour Greyish brown to brown Reddish brown to Olive Black to greyish brown
Chroma (thickness of layer)** Present (0.08 m��� Present (0.1 m��� Present (0.3 m���
Mottles and Segregations Not present Not present Not present
Depth to groundwater Not present 0.0� m 0.01 m
Ferruginous root channel and pore linings
Not present Not present Not present
pH*8 Very strongly acid Strongly acid Very strongly acid
Texture Sand Loam Loam
Acid sulfate material Not present Present Present
Electrical Conductivity (EC)8 Non saline Slightly saline Slightly saline
Indicator7 Site 127 Site 128 Organic materials and organic carbon (OC)*
Organic materials to 0.3 m OC: 38.6%
Organic materials to 0.3 m OC: 27.9%
Matrix colour Black Black
Chroma (thickness of layer)** Present (0.3 m��� Present (0.3 m���
Mottles and Segregations Not present Not present
Depth to groundwater 0.02 m 0.03 m
Ferruginous root channel and pore linings
Not present Not present
pH*8 Very strongly acid Very strongly acid
Texture Loam Loam
Acid sulfate material Present Present
Electrical Conductivity (EC)8 Non saline Slightly saline
*Organic carbon % (Dumas method) and pH taken from surface (0-0.1 m) **Chroma value is less than or equal to 2
Summary of Field Observations• Presence of swamp hummock microrelief is typical of a saturated environment
• Organic materials are indicative of a reduced and permanently inundated environment
• High water tables and poor external drainage indicate the swamp is permanently inundated
• Hydrogen sulfide gas detected in swamp indicates the presence of acid sulfate materials
References1. DEWHA (2008). Australian Wetlands Database. [online]. Available at http://www.environment.gov.au/water/publications/environmental/wetlands/database/ [accessed 21/08/08].
2. Queensland Department of Natural Resources and Water (2008). SILO [online]. Available at http://www.longpaddock.qld.gov.au/silo/ [accessed 5/11/2007].
3. Isbell RF (2002). The Australian Soil Classification. CSIRO Publishing, Collingwood, Victoria, revised edition.
4. EPA (2008) Regional Ecosystems. [online]. Available at http://www.epa.qld.gov.au/nature_conservation/biodiversity/regional_ecosystems/ [accessed 28/06/08].
5. Bureau of Mineral Resources (1978). Moreton: Australia 1:250,000 Geological Series, Bureau of Mineral Resources, Canberra.
6. Richardson JL and Vepraskas MJ (2001). Wetland Soils: Genesis, Hydrology, Landscapes and Classification. CRC Press, Florida.
7. Bryant KB, Wilson PR, Biggs AJW, Brough DM and Burgess JW (2008). Soil Indicators of Queensland Wetlands: State-wide assessment and methodology. Queensland Department of Natural Resources and Water. Brisbane.
8. Hazelton P and Murphy B (2007). Interpreting Soil Test Results: What do all the numbers mean?. [2nd ed]. CSIRO publishing. Collingwood Victoria.
Soil Indicators of Queensland WetlandsSo
il M
orph
olog
y
Site
124
Clas
sifi
cati
onAu
stra
lian
Soil
Clas
sifi
cati
on
Aer
ic P
odso
lLa
ndfo
rm E
lem
ent
Dun
eslo
peM
orph
olog
ical
Typ
e Lo
wer
slo
peH
oriz
onD
epth
(m
)Bo
unda
ryTe
xtur
eCo
lour
Mot
tles
Coar
se
Frag
men
tsSt
ruct
ure
Segr
egat
ions
Cons
iste
nce
A11
0 to
.08
-fib
ric
sand
dark
gre
yish
bro
wn
(10Y
R42���
no
neno
nesi
ngle
gra
inno
neve
ry w
eak
mod
erat
ely
moi
st
A12
.08
to .
�-
sand
brow
n (1
0YR�
3���no
neno
nesi
ngle
gra
inno
neve
ry w
eak
mod
erat
ely
moi
st
A21
e.�
to
.7-
sand
grey
ish
brow
n (1
0YR�
2���
none
none
sing
le g
rain
none
very
wea
k m
oist
A22
e.7
to
1-
sand
brow
n (1
0YR�
3���
none
none
sing
le g
rain
none
very
wea
k m
oist
A23
e1
to 1
.2�
-sa
ndpa
le b
row
n (1
0YR6
3���
very
few
(<2
%���
fine
(<5
mm
) fa
int
oran
ge m
ottl
es
none
sing
le g
rain
none
very
wea
k w
et
Site
125
Clas
sifi
cati
on
Aust
ralia
n So
il Cl
assi
fica
tion
Te
rric
, Su
lfidi
c, F
ibri
c O
rgan
osol
Land
form
Ele
men
t Sw
amp
Mor
phol
ogic
al T
ype
Clos
ed D
epre
ssio
n H
oriz
onD
epth
(m
)Bo
unda
ryTe
xtur
eCo
lour
Mot
tles
Coar
se
Frag
men
tsSt
ruct
ure
Segr
egat
ions
Cons
iste
nce
P11
0 to
.1-
fibri
c lo
ambl
ack
(10Y
R21
��� no
neno
ne-
none
very
wea
k w
et
P12
.1 t
o .3
-fib
ric
loam
very
dar
k gr
eyis
h br
own
(10Y
R32���
none
none
-no
neve
ry w
eak
wet
Site
126
Cl
assi
fica
tion
Au
stra
lian
Soil
Clas
sifi
cati
on
Terr
ic,
Sulf
uric
, Fi
bric
Org
anos
olLa
ndfo
rm E
lem
ent
Swam
pM
orph
olog
ical
Typ
e Cl
osed
Dep
ress
ion
Hor
izon
Dep
th (
m)
Boun
dary
Text
ure
Colo
urM
ottl
esCo
arse
Fr
agm
ents
Stru
ctur
eSe
greg
atio
nsCo
nsis
tenc
e
P11
0 to
.1-
fibri
c lo
ambl
ack
(10Y
R21
��� no
neno
ne-
none
very
wea
k w
et
P12
.1 t
o .3
-fib
ric
loam
very
dar
k gr
eyis
h br
own
(10Y
R32���
none
none
-no
neve
ry w
eak
wet
Soil Indicators of Queensland WetlandsSi
te 1
27Cl
assi
fica
tion
Au
stra
lian
Soil
Clas
sifi
cati
on
Rego
lithi
c, S
ulfu
ric,
Fib
ric
Org
anos
olLa
ndfo
rm E
lem
ent
Swam
pM
orph
olog
ical
Typ
eCl
osed
Dep
ress
ion
H
oriz
onD
epth
(m
)Bo
unda
ryTe
xtur
eCo
lour
Mot
tles
Coar
se
Frag
men
tsSt
ruct
ure
Segr
egat
ions
Cons
iste
nce
P11
0 to
.1�
-fib
ric
loam
blac
k (1
0YR
21���
none
none
-no
neve
ry w
eak
wet
P12
.1�
to .
6-
fibri
c lo
ambl
ack
(10Y
R21
���no
neno
ne-
none
very
wea
k w
et
Site
128
Cl
assi
fica
tion
Au
stra
lian
Soil
Clas
sifi
cati
on
Terr
ic,
Sulf
uric
, Fi
bric
Org
anos
olLa
ndfo
rm E
lem
ent
Swam
pM
orph
olog
ical
Typ
e Cl
osed
Dep
ress
ion
H
oriz
onD
epth
(m
)Bo
unda
ryTe
xtur
eCo
lour
Mot
tles
Coar
se
Frag
men
tsSt
ruct
ure
Segr
egat
ions
Cons
iste
nce
P11
0 to
.1-
fibri
c lo
ambl
ack
(10Y
R21
��� no
neno
ne-
none
very
wea
k w
et
P12
.1 t
o .3
-fib
ric
loam
blac
k (1
0YR
21���
none
none
-no
neve
ry w
eak
wet
Soil
Chem
istr
y
Site
Dep
th (
m)
pH*
EC (
dS/m
)Cl
(m
g/kg
)N
O3-
N (
mg/
kg)
TC%
**TN
%**
124
0.00
-0.1
0�
0.0�
34<1
1.82
0.0�
0.20
-0.3
06.
30.
0321
<10.
16<0
.03
0.40
-0.�
06.
�0.
01<2
0<1
0.09
<0.0
3
12�
0.00
-0.1
0�.
�1.
0�92
1<1
26.3
1.03
0.20
-0.3
04.
20.
7720
0<1
10.3
0.42
126
0.00
-0.1
04.
80.
9�72
81
34.4
1.19
0.20
-0.3
04.
61.
02�6
�<1
28.1
1.07
127
0.00
-0.1
04.
10.
8162
3<1
38.6
0.81
0.20
-0.3
04.
20.
�847
2<1
33.�
0.77
0.40
-0.�
04.
20.
6�49
8<1
36.8
0.9�
128
0.00
-0.1
04.
80.
76�1
12
27.9
1.06
0.20
-0.3
04.
11.
423�
9<1
32.�
0.9
*Aqu
eous
1:�
**To
tal c
arbo
n an
d to
tal n
itro
gen
93
11
66
21
80
64
3