12-14 September, 2011, Lucknow - Earth Science India
12-14 September, 2011, Lucknow - Earth Science India
12-14 September, 2011, Lucknow - Earth Science India
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National Conference on <strong>Science</strong> of Climate Change and <strong>Earth</strong>’s Sustainability: Issues and Challenges ‘A Scientist-People Partnership’<br />
<strong>12</strong>-<strong>14</strong> <strong>September</strong>, <strong>2011</strong>, <strong>Lucknow</strong><br />
SOIL: A NATURAL RESOURCE AS WELL AS AN<br />
IMPORTANT TOOL OF CARBON SEQUESTRATION<br />
M.K. Gupta<br />
Forest Soil & Land Reclamation Division, Forest Research Institute, P.O. New Forest,<br />
Dehradun 248 006.<br />
email: guptamk@icfre.org<br />
Soil is a natural resource and cannot be assumed as a high quality permanent<br />
source of sustainable nutrition for plants. Proper management and utilization of this<br />
natural resources are very important and should be given due priority. Our natural<br />
resources are under tremendous pressure. Our forests are suffering from great pressure<br />
to cater the need of fuel, fodder, timber etc to the large population of the country.<br />
Large-scale deforestation is one of the major causes for increasing CO 2 in the<br />
atmosphere on one hand and depleting nutrients in soil on the other hand. Trees have<br />
the potential to store the carbon for the long time in the wood and thus halting the<br />
depletion of ozone layer. Concentration of atmospheric CO 2 can be lowered either by<br />
reducing emissions or by taking CO 2 out from the atmosphere and stored in the<br />
terrestrial, oceanic or aquatic ecosystems. Soil organic matter contains the largest<br />
terrestrial reservoir of carbon in the biological global carbon cycle. As such, it plays a<br />
major role in the control of carbon dioxide levels in the atmosphere. Soils store 2.5 to<br />
3.0 times as much carbon that stored in plants and two to three times more than the<br />
atmospheric as CO 2. . Soil carbon has much longer residence mean times than the carbon<br />
in the vegetation that the soils support. Changes in forest type, productivity, decay rates<br />
and disturbances can effectively modify the carbon contents of forest soils. Some<br />
reports indicate, up to 87 % decrease in soil organic carbon due to deforestation.<br />
Plantations are consequential to diverting pressure from natural forests by providing<br />
fuel, fodder and timber to the growing population. Soils and vegetation, therefore,<br />
represent potential sinks for this additional carbon and several authors have suggested<br />
afforestation as a possible means of mitigating global climate change. The carbon store<br />
in forest land is the highest followed by agroforestry, agricultural lands and barren<br />
lands. The effect of land use change on soil carbon stock is of concern in the context of<br />
international policy agenda on GHG emission mitigation. Trees enrich the soil through<br />
adding organic matter, nutrient cycling, provide shade to conserve moisture, promote<br />
microbial activities and improve soil physicochemical behaviour. Deforestation results<br />
in increased air movement and facilitates oxidation of organic matter thus emitting CO 2 .<br />
Increase in atmospheric temperature due to climate change is also enhancing the<br />
decomposition of organic matter and release of CO 2 in the atmosphere. Soil organic<br />
carbon is sensitive to impact of anthropogenic activities. There is a major potential for<br />
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