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Spatial and temporal variability of soil N2O and CH4 fluxes along a degradati...CIFOR-ICRAF
1) The document studied the spatial and temporal variability of soil N2O and CH4 fluxes along a degradation gradient in a palm swamp peat forest in the Peruvian Amazon.
2) It found that forest degradation altered micro-scale N2O and CH4 emissions, with N2O and CH4 fluxes varying between intact, medium, and highly degraded sites.
3) However, site-scale annual emissions of N2O and CH4 were found to be homogeneous among intact, medium, and highly degraded sites, though precipitation increases were found to increase CH4 emissions.
Day 4a Bio Cf Ci Madagascar André Aquino Bio Cf Training Jan08theREDDdesk
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Spatial and temporal variability of soil N2O and CH4 fluxes along a degradati...CIFOR-ICRAF
This study examined the spatial and temporal variability of soil N2O and CH4 fluxes along a degradation gradient in a palm swamp peat forest in the Peruvian Amazon. The researchers measured fluxes monthly for 3 years at intact, medium degradation, and high degradation sites. At the microscale, N2O and CH4 fluxes varied between hummocks and hollows and between live and cut palm trees depending on the degradation level. At the macroscale, annual N2O fluxes were similar across sites but annual CH4 fluxes increased with precipitation. Water table level, temperature, and soil nitrification rates influenced the fluxes. While degradation altered microscale emissions, site-scale emissions were homogeneous. Climate change may increase CH4
Degradation of palm swamp peatlands in the Peruvian Amazon severely raises em...CIFOR-ICRAF
Presented by Kristell Hergoualc'h, at International Wetlands Virtual Conference: Traditional knowledge & innovative science in wetland research & management, on 14 Oct 2021
Is it possible to mitigate greenhouse gas emissions from agricultural soil by...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 3.2, Managing SOC in: Grasslands and livestock production systems, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Cornelia Rumpel, from CNRS – INRA – ENS - France, in FAO Hq, Rome
C sequestration of a grazed permanent grasslands: uses of complementary metho...ExternalEvents
This presentation was presented during the 1 Parallel session on Theme 3.2, Managing SOC in: Grasslands and livestock production systems, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Ms. Katja Klumpp, from INRA – France, in FAO Hq, Rome
This presentation shows how soil carbon can help combat climate change. The presentation was held by Louis Verchot (Director, Soils Research Area, CIAT/WLE) at the Soils Advantage event, part of the Agriculture Advantage 2.0 series at COP24.
Spatial and temporal variability of soil N2O and CH4 fluxes along a degradati...CIFOR-ICRAF
1) The document studied the spatial and temporal variability of soil N2O and CH4 fluxes along a degradation gradient in a palm swamp peat forest in the Peruvian Amazon.
2) It found that forest degradation altered micro-scale N2O and CH4 emissions, with N2O and CH4 fluxes varying between intact, medium, and highly degraded sites.
3) However, site-scale annual emissions of N2O and CH4 were found to be homogeneous among intact, medium, and highly degraded sites, though precipitation increases were found to increase CH4 emissions.
Day 4a Bio Cf Ci Madagascar André Aquino Bio Cf Training Jan08theREDDdesk
The document summarizes a REDD+ project in Madagascar called the Mantadia Biological Corridor. The project aims to reduce deforestation and support reforestation efforts across 425,000 hectares of protected areas and 3,020 hectares designated for habitat restoration. It seeks to generate carbon credits while also conserving biodiversity and improving local livelihoods through agroforestry and sustainable agriculture programs. Key challenges include developing effective restoration techniques, securing land tenure, funding, coordination across stakeholders, and ensuring long-term monitoring and community benefits from reduced deforestation.
Spatial and temporal variability of soil N2O and CH4 fluxes along a degradati...CIFOR-ICRAF
This study examined the spatial and temporal variability of soil N2O and CH4 fluxes along a degradation gradient in a palm swamp peat forest in the Peruvian Amazon. The researchers measured fluxes monthly for 3 years at intact, medium degradation, and high degradation sites. At the microscale, N2O and CH4 fluxes varied between hummocks and hollows and between live and cut palm trees depending on the degradation level. At the macroscale, annual N2O fluxes were similar across sites but annual CH4 fluxes increased with precipitation. Water table level, temperature, and soil nitrification rates influenced the fluxes. While degradation altered microscale emissions, site-scale emissions were homogeneous. Climate change may increase CH4
This presentation was presented during the 1 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Miguel Taboada, from INTA - Argentina, in FAO Hq, Rome
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This document discusses challenges and options for monitoring emissions reductions from peatland management. It outlines that drained peatlands are a major source of carbon emissions and conservation and rewetting efforts could significantly reduce emissions. Monitoring direct greenhouse gas fluxes is expensive, so the document proposes using proxies like water levels, vegetation, and subsidence which correlate to emissions and can be monitored more cost effectively over large areas. It concludes that emission reductions from rewetting and conservation practices on peatlands can meaningfully contribute to climate change mitigation.
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Major CO2 losses from degradation of Mauritia flexuosa peat swamp forests in western Amazonia
1. Kristell Hergoualc’h, J van Lent, N Dezzeo, LV Verchot, J van Groeningen,
M Lopez, J Grandez
Major carbon losses from degradation of
Mauritia flexuosa peat
swamp forests in western Amazonia
EGU GA 2022, 23-27th May 2022
2. Peruvian peatlands
Key contributor tropical peatlands
Gumbricht et al. (2017)
Amazonian peatlands mainly Mauritia
flexuosa-dominated forests (Hastie et al. 2022)
C-dense ecosystems (746 Mg C ha-1) (Honorio Coronado
et al. 2021)
Recurrent degradation over 30 years: M. flexuosa
palms cut for fruit collection (Horn et al. 2018)
73% M. flexuosa-dominated stands degraded in
pilot area (Hergoualc’h et al. 2017)
3. Experiment
Highly
deg.
Medium
deg.
Intact
Iquitos, Northern Peruvian
Amazon
Degradation gradient
I: Intact
mD: medium degradation
hD: high degradation
Several years, monthly monitoring of soil heterotrophic respiration
(peat C output), litterfall, and root mortality (peat C inputs)
→ Peat C budget = (Sh + DOC) – (Litterfall + Root mortality) (IPCC)
Computed over 1 Y when all fluxes measured simultaneously at all sites
Dissolved organic C: Default value from Southeast Asia
4. Experiment and computations
Biomass measurement 5 years after degradation started (according to
satellite imagery), 1 year before monitoring fluxes
C loss from degradation
Intact site representative degraded sites before degradation
AGB C loss degraded site = (AGB C Intact – AGB C degraded site)
Peat C loss degraded site =
(Peat C stock gained / lost 5 Y degraded site
- Peat C stock gained 5Y Intact site)
-2
0
2
4
6
8
0 2 4 6
Peat
C
budget
(Mg
C
ha
-1
y
-1
)
Year
Intact
mDeg
hDeg
Biomass
measur.
Flux
measur.
Intact: Peat C budget steady state
Degraded: Linear change over
time peat C budget with initial
rate = rate at the Intact site
5. Peat C budget & C stock loss
Peat C fluxes and budget
Degradation ↘ C inputs, ↗ C outputs
-1.8
± 1.8
-0.3
± 0.7
6.0 ±
0.6
-10.0
-6.0
-2.0
2.0
6.0
10.0
Intact mDeg hDeg
Mg
C
ha
-1
y
-1
Root Mort Litterfall Sh DOC
Peat C built up / lost over 5 years
-9 ± 4
-7 ± 3
9 ± 3
-15
-10
-5
0
5
10
15
Intact mDeg hDeg
Peat
built-up
/
lost
(Mg
C
ha
-1
5
y
-1
)
Intact: C Sink
mDeg: C sink lessened
hDeg: Large source of C
⇒
6. Biomass & ecosystem C stock losses
AGB biomass
↘ by 32% and 62% following medium and
high degradation
98 ± 15
67 ± 11
37 ± 11
0
30
60
90
120
Intact mDeg hDeg
AGB
(Mg
C
ha
-1
)
30 ± 19
61 ± 18
2 ± 6
18 ± 7
0
20
40
60
80
100
mDeg hDeg
Total
C
stock
loss
(Mg
C
ha
-1
5
y
-1
)
AGB Peat
79 ± 19
32 ± 20
Ecosystem C losses
High degradation = 2.5 losses medium
degradation
Losses from AGB biomass = 94% and 77% for
medium and high degradation
7. Concluding remarks
1st estimates of ecosystem C loss from degradation undrained
tropical peatlands, for peatlands of South America
1 location over a limited period ⇒ Need for replication along
degradation gradients in ≠ climate (precipitation, water table
fluctuation)
Peat C budget (Mg C ha-1 y-1): Comparison Southeast Asia
Intact -1.8 ± 1.8 ≈ −1.4 ± 1.8 Intact peat swamp forests (Hergoualc’h &
Verchot 2014)
hDeg 6.0 ± 0.6 ≈ 5.3 ± 1.6 Drained degraded peat swamp forests
(Hergoualc’h & Verchot 2014; IPCC)
Peat C budget estimates outside of Southeast Asia and for undrained
degraded peatlands very much needed for countries aiming at
including peatlands in their national climate change strategies