Tadulako University Palu Bogor Agricultural University
Promoting sustainable land-use management:
water, carbon and nutrient turnover
Tadulako University Palu Bogor Agricultural University
Objectives
•
Present key results
•
Draw conclusions for agricultural and forest
management
Tadulako University Palu Bogor Agricultural University
Aboveground biomass, premontane natural forests
Tadulako University Palu Bogor Agricultural University
Tadulako University Palu Bogor Agricultural University
Slide 6
Meteorological flux tower in
Tadulako University Palu Bogor Agricultural University
CO
2
fl
ux
(g
(
C)
m
-2
d
-1
)
OCT ' 03
JAN ' 04
APR
JUL
OCT
JAN ' 05
MAR
CO
2
fl
ux
(g
(
C)
m
-2
d
-1
)
OCT ' 03
JAN ' 04
APR
JUL
OCT
JAN ' 05
MAR
-10 -8 -6 -4 -2 0 2 4 6 8
R
EF
bP
g -10 -8 -6 -4 -2 0 2 4 6 8R
EF
bP
gEcosystem Respiration 1760 g C m
-2
year
-1
Net turbulent uptake 970 g C m
-2
year
-1
Gross photosynthesis 2730 g C m
-2
year
-1
-10 -8 -6 -4 -2 0 2 4 6 8
R
EF
bP
g -10 -8 -6 -4 -2 0 2 4 6 8R
EF
bP
gEcosystem Respiration 1760 g C m
-2
year
-1
Net turbulent uptake 970 g C m
-2
year
-1
Gross photosynthesis 2730 g C m
-2
year
-1
Measured net ecosystem exchange flux F
c
,
extrapolated respiration flux RE, and
the sum of both fluxes Pg (gross photosynthesis)
Tadulako University Palu Bogor Agricultural University
Slide 8
CO
2
fluxes between the atmosphere: forest vs. cacao
Tadulako University Palu Bogor Agricultural University
Land use types and net ecosystem productivities:
scenarios
Tadulako University Palu Bogor Agricultural University
Slide 10
Land use types and net ecosystem productivities:
model results
Tadulako University Palu Bogor Agricultural University
Ibrom et al., 2007
Tadulako University Palu Bogor Agricultural University
Slide 12
Sap flux of cacao and shade trees
Tadulako University Palu Bogor Agricultural University
Cacao tree water use vs. canopy gap fraction
Köhler et al. 2009
(R
2
adj
= 0.39, p = 0.043, n = 9)
Tadulako University Palu Bogor Agricultural University
Gumbasa river watershed
Catchment size:
1275 km²
R²=0.83
c
c
c
c
c
c
#
³
#
³
#
³
#
³
#
³
#
/
#
/
c
c
c
c
c
c
c
c
0
10
20 Kilometers
auto m atic s tage reco rde r
#
³
stag e record er - Fo restry d ep artm ent
#
/
clim ate statio n
c
clim ate statio n - S TOR M A p ro ject
c
main irriga tio n ch an nel Lo re Li nd u Natio n al Parc PALU R IVER w atersh ed
Gauging stations
R
2= 0.86
automatic stage recorder
stage recorder
–
Forestry
climate station
climate station STORMA
main irrigation chanel
Lore Lindu National
Park
Palu river watershed
Gerold & Leemhuis 2008
Tadulako University Palu Bogor Agricultural University
Modeling discharge of the river discharge, Gumbasa
watershed: effects of land cover change
Slide 15
01
/01
/03
01
/03
/03
01
/05
/03
01
/07
/03
01
/09
/03
01
/11
/03
di
sc
har
ge
[
m
m
d
-1
]
0
2
4
6
8
10
12
14
16
actual land use
land use scenario A1
land use scenario A2
Discharge (2003):
s
tatus quo 2003:
590 mm
land use scenario A1: 838 mm
+ 42%
1200m annual crops
Land use scenario A2: 724 mm
+ 23%
1200m change into cacao
Tadulako University Palu Bogor Agricultural University
0
1
2
3
4
5
6
7
8
Di
s
c
h
a
rge (
m
m
d
-1
)
Direct flow
Interflow
Base flow
Kleinhans et al. 2004
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
2003
Tadulako University Palu Bogor Agricultural University
Nutrient balance of maize and agroforest
Tadulako University Palu Bogor Agricultural University
Summary
land use types & land use gradients
•
High carbon storage in forests of Sulwesi
•
High carbon uptake by forest
•
Shade trees enhance transpiration from agrofrests
•
River discharge change with land cover change suggested
Tadulako University Palu Bogor Agricultural University
Implications
•
Very important to conserve remaining forests
Tadulako University Palu Bogor Agricultural University
Drought experiments
Premontane rainforest
Tadulako University Palu Bogor Agricultural University
Tadulako University Palu Bogor Agricultural University
80% of plot area was covered by plastic panels (March 07- mid April 08);
n=3 roof (treatment) plots, n=3 control plots
G Moser
Tadulako University Palu Bogor Agricultural University
Soil water content
Tree sap flux
Cacao bean
Tadulako University Palu Bogor Agricultural University
Cacao yield
Desiccation period Rewetting period
0
20
40
60
80
100
120
C
a
ca
o
b
e
a
n
d
ry
m
a
s
s
(k
g
h
a
2
w
k
)
-1
-1
2007
2008
Control
Roof
March
May
July
Sep
Nov
Jan
March
May
July
*
Roof closure
-10%, p>0.05
-55%, p<0.05
Tadulako University Palu Bogor Agricultural University
- 40%, p < 0.05)
01Feb07
01Jun07
01Oct07
01Feb08
01Jun08
S
oi
l
w
ater
sto
rage
(
mm
)
0
300
400
500
600
C
a
c
a
o
0.0
0.6
0.8
1.0
1.2
S
o
il
w
a
te
r
sto
rag
e
(
m
m
)
Roo
f
to c
o
nt
rol
rati
o
Roof closure
S
a
p
flux
ca
ca
o
-11%, p>0.05
Control
Tadulako University Palu Bogor Agricultural University
Complementary use of soil water
deuterium signal
-70
-60
-50
-40
Plant water
0.0- 0.1
0.1- 0.3
0.3- 0.5
0.5- 0.7
0.7- 1.0
S
o
il
w
a
te
r
(d
e
p
th
in
m
)
-70
-60
-50
-40
A
B
Cacao
Gliricidia
D (
‰
)
D (
‰
)
δ
δ
Cacao
Gliricidia
Tadulako University Palu Bogor Agricultural University
0
20
40
60
80
100
0-30
30-100
S
o
il
d
e
p
th
in
te
rv
a
l
(c
m
)
Cacao Jan 07
Gliricidia Jan 07
Proportion of water uptake from a given soil depth interval (%)
Tadulako University Palu Bogor Agricultural University
Root water potential
-14
-12
-10
-8
-6
-4
-2
0
R
o
o
t
w
a
te
r
p
o
te
n
ti
a
l
(b
a
r)
R
C
R
C
R
C
R
C
R
C
Feb 07
July 07
Aug 07
Sep 07
Mar 08
Cacao
Feb 07 Jul 07 Aug 07 Sep 07 Mar 08
-14
-12
-10
-8
-6
-4
-2
0
R
o
o
t
w
a
te
r
p
o
te
n
ti
a
l
(b
a
r)
R
C
R
C
R
C
R
C
R
C
Gliricidia
Moser et al. under review
Osmotic adjustment in cacao
Cacao
Gliricidia
Control
Tadulako University Palu Bogor Agricultural University
CO
2
soil efflux
CO
2
effl
ux
(M
g
C
m
-1
h
-1
)
Experiment period
Period of roof closure
Tadulako University Palu Bogor Agricultural University
CO
2
efflux response to soil moisture
Volumetric water content (m
3m
-3)
CO
2
effl
ux
(M
g
C
m
-1
h
-1
)
(Adj R
2
= 0.338, n = 94)
Tadulako University Palu Bogor Agricultural University
cacao drought experiment
•
Cacao yield was little influenced for several months; a strong
(~50%) reduction was observed at the end of the experiment
•
Little response of tree water use to drought
•
Cacao and Glriricidia trees use soil water resources complementary
Tadulako University Palu Bogor Agricultural University
Implications
•
Cacao is a suitable crop even where short dry spells occur
Tadulako University Palu Bogor Agricultural University
(
m
3 m
3 )
10cm control 10cm roof 0 .3 0 .4 0 .5 0 .6 0 .7
Throughfall displacement period
(
m
3 m
3 )
40cm control 40cm roof 0 .3 0 .4 0 .5 0 .6 0 .7 ( m
3 m
3 )
150cm control 150cm roof 0 .3 0 .4 0 .5 0 .6 0 .7
03/2007 06/2007 09/2007 12/2007 03/2008 06/2008 09/2008 12/2008 03/2009 06/2009
Soil moisture
Köhler, unpublished
10 cm
40 cm
150 cm
Roof closure
Tadulako University Palu Bogor Agricultural University
Sap flux: all trees
0.4
0.5
0.6
0.7
0.8
0.9
1.0
J
s
R
a
ti
o
ro
o
f
o
v
e
r
c
o
n
tr
o
l
0
25
50
75
100
125
150
175
200
225
250
275
300
325
350
Day of year 2008
Complete dataset: roof plots devided by control plots
Tadulako University Palu Bogor Agricultural University
0
2
4
6
8
10
S
te
m
w
o
o
d
p
ro
d
u
c
ti
o
n
(M
g
h
a
y
r
)
-1
-1
Control
Roof
Stem wood production (2nd year)
Tadulako University Palu Bogor Agricultural University
CO
2
soil efflux
CO
2
e
ff
lux
(
M
g
C
m
-1
h
-1
)
Experiment period
Period of roof closure
Tadulako University Palu Bogor Agricultural University
CO
2
soil efflux vs. soil moisture
CO
2
effl
ux
(M
g
C
m
-1
h
-1
)
(Adj R
2
= 0.79, n = 93)
Tadulako University Palu Bogor Agricultural University
forest drought experiment
•
Little response in tree sap flux to drought
•
Tree diameter growth was significantly reduced
Tadulako University Palu Bogor Agricultural University
Overall summary
•
Old-growth forest is to be conserved
•
Agroforestry is a promissing option in
post-forest landscapes