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388                                        12  Carbon Capture and Storage

            be achieved by conservation tillage, crop selection, rotation and intensified crop-
            ping, managing soil biogeochemistry, and manipulation of microbial communities.
              Tilling disturbs the soil resulting in reduced CO 2 storage. Therefore, reduced
            tillage intensity contributes to increased CO 2 storage. It can be achieved by no till,
            ridge till, minimum till, and mulch till. Conservation tillage aims at the reduction of
            soil erosion and the maintenance of water-holding capacity of soils. It is expected to
            restore the loss of CO 2 that was released by historical intensive tillage practice over
            a short period of time.
              Crop selection, rotation, and intensified cropping allow more above-ground
            biomass, and consequently enable more CO 2 storage. Their net carbon storage
            effects will be maximized when applied in conjunction with conservation tillage.
              Soil organic carbon may depend on the soil biological and chemical properties,
            for example, pH. Addition of metal oxides such as CaO and MgO is expected to
            enhance the chemical sorption of CO 2 into the soils. However, this change in pH
            may also change the behaviors of microorganisms in the soils.
              Fungal and bacterial species in the soils play an important role in the release and
            storage of soil organic carbon as well as the emissions of other GHGs such as N 2 O
            and CH 4 . The complexity of microbial community opens another opportunity for
            potential CO 2 storage and/or reduced GHG emissions by multiplication of the
            microbial species. Different ongoing research projects are being conducted to
            evaluate the feasibility of this approach.



            12.8.5.2 Change in Land Use

            Land on the earth can be grouped into, in the increasing order of carbon storage
            share, degraded land < croplands < pasture < grass lands < wetlands < forest. Land
            upgrading in terms of carbon storage capacity is expected to contribute to additional
            CO 2 storage. IPCC (2000) report on land use, land-use change and forestry esti-
            mated that about 1 Gt-C per year could be stored in the short term as a result of the
            regrowth of perennial vegetation and improvements of land management practices
            in croplands, grasslands, and forests. For example, change in land use can be
            achieved by wetland management and restoration and forestry management,
            afforestation, and reforestation.
              Protection and restoration of wetlands presents an opportunity for increased
            underground organic carbon storage. The residence time of the CO 2 stored in
            wetland depends on the plant type and the degree of inundation. Since wetland is
            the second best land in terms of CO 2 storage, only after forest, more CO 2 is released
            into the atmosphere when wetland is drained for uses as agricultural or urban and
            industrial development. Unfortunately, recent research shows that it is challenging
            to restore the lost CO 2 simply by recreating wetlands. More research and devel-
            opment is needed in this area.
              The loss of CO 2 storage in forest can be reduced by reducing logging and
            deforestation. Protection of old trees and regeneration of secondary and degraded
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