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181.
Developing Canada's National Forest Carbon Monitoring, Accounting and Reporting System to Meet the Reporting Requirements of the Kyoto Protocol 总被引:2,自引:0,他引:2
The rate of carbon accumulation in the atmosphere can be reduced by decreasing emissions from the burning of fossil fuels
and by increasing the net uptake (or reducing the net loss) of carbon in terrestrial (and aquatic) ecosystems. The Kyoto Protocol
addresses both the release and uptake of carbon. Canada is developing a National Forest Carbon Monitoring, Accounting and
Reporting System in support of its international obligations to report greenhouse gas sources and sinks. This system employs
forest-inventory data, growth and yield information, and statistics on natural disturbances, management actions and land-use
change to estimate forest carbon stocks, changes in carbon stocks, and emissions of non-CO2 greenhouse gases. A key component of the system is the Carbon Budget Model of the Canadian Forest Sector (CBM-CFS). The model
is undergoing extensive revisions to enable analyses at four spatial scales (national, provincial, forest management unit
and stand) and in annual time steps. The model and the supporting databases can be used to assess carbon-stock changes between
1990 and the present, and to predict future carbon-stock changes based on scenarios of future disturbance rates and management
actions. 相似文献
182.
S. O. Oikeh R. J. Carsky J. G. Kling V. O. Chude W. J. Horst 《Agriculture, ecosystems & environment》2003,100(2-3):181
Nitrate is prone to leaching in the sandy soils of the West African moist savannas. Better management of nitrogen (N) resources and maize cultivars with enhanced genetic capacity to capture and utilize soil and fertilizer N are strategies that could improve N-use efficiency. In two field experiments conducted at Zaria, northern Nigeria, five maize (Zea mays L.) cultivars planted early in the season were assessed under various N levels for differences in N uptake, soil N dynamics, and related N losses. Cultivar TZB-SR accumulated more N in the aboveground plant parts in both years than the other cultivars. All, except the semi-prolific late (SPL) variety, met about 50–60% of their N demand by the time of silking (64–69 DAP). In both years, SPL had the greatest capacity to take up N during the grain filling period, and it had the highest grain-N concentration and the least apparent N loss through leaching in the second year. There were no significant differences in soil N dynamics among cultivars in both years. At harvest, the residual N in the upper 90 cm of the profile under all the cultivars ranged from 56 to 72 kg ha−1 in the first year and from 73 to 83 kg ha−1 in the second year. Apparent N loss from 0 to 90 cm soil profile through leaching ranged from 35 to 122 kg ha−1 in both years. N application significantly increased N uptake by more than 30% at all sampling dates in the second year of the experiment, but had no effect on apparent N loss. Results indicate that the use of maize cultivars with high N uptake capacity during the grain filling period when maximum leaching losses occur could enhance N recovery and may be effective in reducing leaching losses of mineral N in the moist savanna soils. 相似文献
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The Science of Nature - 相似文献
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