turnover of wetland sediments on mineralization of carbon, nitrogen and phosphorus
DESCRIPTION
Turnover of wetland sediments on mineralization of carbon, nitrogen and phosphorus. Qingren Wang* and Yuncong Li Tropical Research and Education Center Department of Soil and Water Science IFAS, University of Florida. ASA-CSSA-SSSA 2009, Pittsburgh, PA. Outline. - PowerPoint PPT PresentationTRANSCRIPT
Turnover of wetland sediments on mineralization of carbon, nitrogen and phosphorus
Qingren Wang* and Yuncong Li
Tropical Research and Education Center
Department of Soil and Water Science
IFAS, University of Florida
ASA-CSSA-SSSA 2009, Pittsburgh, PA
Outline
• Brief introduction about the Everglades wetland
• Recycling of carbon in wetland system• Experiment setup, sampling and analysis• Results, conclusion and discussion
TREC-Homestead
Florida Bay
Natural ecosystem
National Park
Eco-Environment in south Florida
Agriculture
Natural Eco-environment in the Everglades wetland
Bulrush: Scirpus rubiginosus
Sawgrass:Cladium jamaicense
• Wetlands are an important part of the global carbon inventory: up to 1/3 of total global soil carbon is stored in wetlands
• Carbon in wetlands is relatively stable• Carbon accumulation is based on vegetation
types and soil fertility • Decomposition rate depends on water content
and temperature
Why carbon in wetlands?
Importance of wetlands
Mitra et al, 2005, Curr. Sci.
Chauhan, 2007: http://sites.google.com/site/ashvinichauhan/syntrophic-methanogenic-associations-in-florida-wetlands
Carbon cycling in wetlands
Hypothesis
Sediment mineralization was dependant on vegetation type and temperature at the same moisture and other conditions
Experiment• Intact sediment columns were collected
from wetland sites with two different main vegetations: Bulrush and Sawgrass (both are native plants).
• Kept these columns in three growth chambers with temperature at: 30, 25, and 20 oC, respectively.
• Carbon emission and nutrient mineralization were monitored through sampling without disturbing the sediments for 380 days.
Sediment collection & experiment setup
Sample analyses
• Carbon analysis: LiquiTOC• Nitrate and ammonium:
Seal AQ2+• Ortho phosphorus: Auto-
analyzer (AA-3)
• Turnover of sediments for C, N, and P with
time.
• Sediment mineralization vs. vegetation type.
• Effect of temperature on sediment turnover.
Major results
Carbon mineralization rate
0 50 100 150 200 250 300 350 4000
200
400
600
800
1000
1200
1400
1600Sawgrass Bulrush
Time (day)
CO
2-C
(mg/
kg)
Accumulative CO2-C with time
0 50 100 150 200 250 300 350 4000
2000
4000
6000
8000
10000
12000
14000
16000
f(x) = 2132.37154546737 ln(x) − 471.097993785414R² = 0.974241697877589
f(x) = 2604.96473012374 ln(x) − 651.218840685348R² = 0.972346265959714
Sawgrass Logarithmic (Sawgrass)
Bulrush Logarithmic (Bulrush)
Time (day)
Acc
umul
ated
CO
2-C
(mg/
kg)
Expressed by exponential growth model
Sawgrass Bulrusha 13285.65 11023.78b 0.0273 0.0261R2 0.977 0.969
y = a * Exp(-bx) x-time (days), and y-accumulative amount of CO2-C released from sediments
Impacted by temperature (CO2–C)
30 25 200
100200300400500600700800
aa
b
Sawgrass
CO2-
C (m
g/kg
)
Temperature (oC)
30 25 200
100200300400500600700800
ab
c
Bulrush
Nitrogen mineralization
0 50 100 150 200 250 300 350 4000
20
40
60
80
100
120 Nitrate N
SawgrassSeries3Bulrush
NO3-
N (m
g/kg
)
0 50 100 150 200 250 300 350 4000
0.2
0.4
0.6
0.8
1
1.2 Ammonium N
SawgrassSeries3Bulrush
NH4-
N (m
g/kg
)
Outlier
Time (day)
Accumulative N
0 50 100 150 200 250 300 350 4000
100
200
300
400
500
600
Sawgrass
Bulrush
Accu
mul
ativ
e N
O3-
N (m
g/kg
)
0 50 100 150 200 250 300 350 4000
1
2
3
4
5
6
7
f(x) = 1.3889456641 ln(x) − 1.9691750021R² = 0.907716209017961
f(x) = 0.4011311855 ln(x) − 0.5210457688R² = 0.952714208066964
SawgrassLoga-rithmic (Saw-grass)Bulrush
Acc
umul
ativ
e N
H4-N
(mg/
kg)
Time (day)
Phosphorus mineralization
0 50 100 150 200 250 300 350 4000
0.05
0.1
0.15
0.2
0.25
0.3
0.35
SawgrassSeries3Bulrush
Time (day)
Orth
o-P
(mg/
kg) Outlier
Accumulative phosphorus
0 50 100 150 200 250 300 350 4000
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4Sawgrass
Bulrush
Time (day)
Acc
umul
ativ
e P
(mg/
kg)
Impacted by temperature (NO3–N)
30 25 2005
101520253035404550
b
a
c
Sawgrass
NO
3-N
(mg/
kg)
30 25 200
10
20
30
40
50
b
a a
Bulrush
Temperature (o C)
Impacted by temperature (NH4-N)
30 25 200.250.260.270.280.29
0.30.310.320.33 Sawgrass
NH
4-N
(mg/
kg)
Temperature (o C)
30 25 200.250.260.270.280.29
0.30.310.320.33
a
b
aBulrush
Impacted by temperature (P)
30 25 200.002
0.004
0.006
0.008
0.01
0.012
0.014
0.016
0.018
aa
Sawgrass
Orth
o-P
(mg/
kg)
30 25 200
0.0020.0040.0060.008
0.010.0120.0140.0160.018
a
b b
Bulrush
Temperature (o C)
Conclusions (1)• The turnover of organic C was rapid in the first 100 days.
• The accumulative amount of C mineralized can be well
described by an exponential growth model.
• Nitrogen turnover was low at first 100 days and sharply
increased afterwards.
• Phosphorus mineralization was low throughout the whole
experimental period.
•
Conclusions (2) • Sawgrass had a greater turnover on C and N but lower
on P than did bulrush.
• High temperature improves the turnover of organic C
and NH4-N for both species but that of P only for bulrush.
• The turnover of NO3-N was the greatest at 25 oC,
especially for sawgrass.
• Factors in controlling the turnovers are rather
complicated, C:N ratio (18.9 in sawgrass vs. 13.8 in
bulrush) might be one of them.