Carlson, K., Goodman, L., & May - Tobin, C. (2015) Modeling relationships between water table depth and
peat soil carbon loss in Southeast Asian plantations.
DOI: 10.1088 / 1748-9326/10 / 7 / 074006 Modeling relationships between water table depth and
peat soil carbon loss in Southeast Asian plantations
Not exact matches
Tangible effects nearby also appear: clinking our
peat soil by water extraction is also a form of land degradation, leading to more
carbon dioxide emissions, and therefore triggering climate change.
Indonesia's sprawling tropical forests and
peat soils act as a massive
carbon storage sink but have been heavily deforested and degraded in recent years, primarily by palm oil companies and the pulp - paper giants Asian Pulp and Paper and Asia Pacific Resources International Ltd..
Unilever was also a player in palm oil trader Wilmar's recent agreement to adopt a no - deforestation policy, which prohibits its suppliers from establishing plantations on lands with large amounts of
carbon — like
peat soils — or lands with a high conservation value (ClimateWire, Dec. 8, 2013).
There's a whole lot of
carbon up there stored in the
peat and other frozen
soils.
He also totally ignores the
carbon sinks like
peat bogs and
soils that may release CO2 and methane as they are warmed.
When these trees are cut down or they burn, the
peat soils underneath are exposed, releasing
carbon dioxide as the
peat oxidizes and decomposes.
North Carolina's Albemarle - Pamlico peninsula is a patchwork of
peat soils called pocosins (Algonquin for «swamp on a hill»), thick deposits of decomposed plant matter that store high amounts of
carbon.
Landowners who restore
peat soils can use this methodology to document and sell
carbon credits on the voluntary
carbon market.
Similarly CIFOR research suggests that the rewetting of drained
peat — a measure to prevent
carbon emissions released from forest fires and
peat degradation - could increase levels of methane from the
soil.
The loss of permafrost is of particular concern — when permafrost melts, it releases
carbon stored in the
soils, and when boreal forests and
peat bogs burn, they release
carbon stored in the trees and
peat.
The fact that these Indonesian rainforests have thick
peat layers as
soil actually makes them impressive
carbon stores.
Judging by satellite and field measurements they concluded the burning
peat soils released more
carbon than the burning vegetation — about 4 to 5 times as much.
These regions are crucial to the global
carbon cycle because they are rich in
soil organic
carbon, which has built up in frozen
soils and
peat layers over thousands of years.
Warming results in more
carbon dioxide release from
soil and
peat moss — it is some 20 % of the fossil fuel emissions.
This includes
carbon on land in vegetation,
soils,
peat and freshwater and in the atmosphere, ocean and surface ocean sediments.
Coastal mangrove forests can contain much more
carbon per unit area than their terrestrial counterparts: This coastal «blue»
carbon has been deposited on every tide over thousands of years and is stored in deep
peat soils.
The
carbon cycle underwrites all life: plants and microbes withdraw
carbon from the atmosphere and some of it gets stored in the
soils, preserved as
peat, or locked away as rock, or frozen as ice to be returned to the planetary system in all sorts of ways,
The study included
carbon dioxide emissions from burning fossil fuels and producing chemicals and cement but excluded emissions from activities like deforestation and logging, forest and
peat fires, the decay of biomass after burning and decomposition of organic
carbon in drained
peat soils.
The interim results are the first time that a GHG emissions profile has been broken down into its «constituent elements of forest
carbon stock change, non-CO2 emissions from biomass burning, CO2 and non-CO2 emissions from mineral
soil, as well as biological oxidation and direct N2 O, dissolved organic
carbon and CH4 emissions from disturbed
peat, and CO2 and non-CO2 emissions from
peat fire.»
However, these models do not yet include many processes and reservoirs that may be important, such as
peat, buried
carbon in permafrost
soils, wild fires, ocean eddies and the response of marine ecosystems to ocean acidification.
• Land Use, Land - Use Change, and Forestry (17 % of 2004 global greenhouse gas emissions)-- Greenhouse gas emissions from this sector primarily include
carbon dioxide (CO2) emissions from deforestation, land clearing for agriculture, and fires or decay of
peat soils.
Because creating the plantations often means burning the tropical forest and draining the underlying
peat soils, there's an initial large release of stored
carbon.
These «degraded» lands however still contain large amounts of
carbon in the case of water logged organic
peat soils.
That is because a healthy forest soaks up
carbon from the atmosphere and stores it as wood,
peat and
soil carbon, some of it for decades, some for millennia.