http://www.thestarphoenix.com/touch/story.html?id=10331200

Soft geoengineering could mitigate change

BY PAUL HANLEY, THE STARPHOENIX OCTOBER 28, 2014

Climate change looms over our children's future.

For those not confident in global targets to reduce C02 emissions,
geoengineering - the deliberate large-scale intervention in the Earth's
natural systems to counteract climate change - offers a last-ditch
solution.Proposals have been made to fertilize or increase the alkalinity
of the oceans in order to increase carbon absorption or to release
stratospheric aerosols to block sunlight and cool the atmosphere. While
such proposals are rightly met with skepticism - if not fear - we should
acknowledge that burning fossil fuels, deforestation and cultivation are
inadvertent forms of "reverse geoengineering."

The American soil scientist Rattan Lal and others argue that restoring
vegetation on degraded lands and increasing soil organic carbon (SOC) on
existing farmland has the potential to sequester sufficient CO2 to
substantially mitigate climate change if done on a large scale. This form
of "soft geoengineering" is a safe, win-win solution, since land
restoration and soil improvement also restore watersheds, foster
biodiversity, improve productivity and assist with rural poverty reduction.

The potential to reduce climate change by sequestering atmospheric C02 in
soil and vegetation is huge.Photosynthesis converts 112 billion tons of
atmospheric CO2 into biomass annually. (By comparison, only nine billion
tons of carbon emissions are produced from fossil fuel combustion.)
However, almost all of the CO2 synthesized by plants is returned back to
the atmosphere through plant and soil respiration.According to Lal, if 10
per cent of what plants photosynthesize annually - about 11 billion tons -
could be retained in the biosphere, it would be possible to balance the
global carbon budget, halting climate change.

Lal explains that the atmospheric concentration of CO2 from fossil-fuel
combustion and land-use changes has increased by 30 per cent since 1750,
resulting in gradual global warming. Since the Industrial Revolution,
global emissions of carbon are estimated at around 270 billion tons due to
fossil-fuel combustion and about 136 billion tons due to land-use change
and soil cultivation.Emissions due to land-use change include those from
deforestation, biomass burning, conversion of natural ecosystems to
agriculture, drainage of wetlands and soil cultivation. Depletion of the
SOC pool has contributed around 78 billion tons of carbon to the
atmosphere. Some cultivated soils have lost one-half to two-thirds of the
original SOC.The depletion of SOC is accentuated by soil degradation and
exacerbated by land misuse and soil mismanagement.

Soil is the third-largest carbon sink after oceans and fossil fuels. Soil
contains 4.5 times the sequestration capacity of all vegetation (including
trees) and 3.3 times that of the atmosphere.While Rattan Lal estimates that
10 to 20 per cent of annual greenhouse gas emissions could be removed each
year by sequestering carbon in cultivated land, a study by the Rodale
Institute was more optimistic. It states, "multiple research efforts verify
that practical organic agriculture if practised on the planet's 3.5 billion
tillable acres, could sequester nearly 40 per cent of our current CO2
emissions."

Even by the more conservative estimate, carbon farming holds significant
potential to mitigate climate change.

The global potential of SOC sequestration through the application of
recommended management practices on a large scale, at an average of one ton
per hectare year, is one billion tons of carbon per year, which would
offset one-fourth to one-third of the total human-caused annual net
increase in atmospheric CO2, estimated at 3.3 billion tons per year.The
cumulative potential of SOC sequestration over 25 to 50 years could be as
much as 60 billion tons, close to half of all emissions from land-use
changes since 1750.The potential of soil sequestration to mitigate climate
change of course depends on the extent of the application of recommended
practices.

Some 1.5 billion hectares of land are currently under cultivation. There is
an optimum range of SOC concentration of two to three per cent in the root
zone of most soil types. Given that cultivation has generally led to
substantial decreases in SOC, most soils can benefit from increased SOC
formation.

On top of that is the vast potential to increase SOC formation in billions
of hectares of deforested, degraded and desertified lands should they be
reclaimed.

© Copyright (c) The Starphoenix

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