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Environment
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Estimation of Emission changes about green house effect gasses by land-cover changes
using remote sensing and GIS in Sumatra Island, Indonesia
Aboveground carbon stock changes
Aboveground carbon content estimation of each land cover was calculated by multiplying
the area of each land cover with carbon stock per unit area. Table 3 has showed the changes of
aboveground carbon due to land cover changes. Total above ground carbon stock decrease
from 6.16 x 10 8 ton in 1986 to 5.66 x 10 8 ton in 1992 or loss of about 0.50 x 10 8 ton within 6
years equal to 8.3 millions ton per year. The loss of aboveground carbon was mainly came
from primary forest conversion. IPCC have divided the loss of aboveground carbon content
into on site and off-site release. These two categories were classified further into direct
burning (fuel wood and slash and burn agricultural) and decomposition process release of
unburned biomass (Houhton et.al., 1996). Thus the amount of carbon and GHG released to
the atmosphere were depended on these processes. Estimation of the amount carbon and GHG
release need yearly basis time series of spatial data and the information on commercial wood
and fuel wood harvest, and burning efficiency data of each land cover type.
Soil Greenhouse gas emission changes
GHG flux of soil varies depend on type the site condition and season. The comparisons
below were made based on flux measurement conducted in November 1997 in several sites of
Jambi Province. The calculation results of total flux based on 1986 and 1992 land cover data
for major land cover presented in Table 4. Comparison of the total GHG flux of the two
periods of time studies could not be performed since there are still no information on GHG
flux of soil surface under cash crops plantation and secondary forest. However, it seems that
the conversion of natural forest will cause on the decrease of methane gas absorption and
induce the increase of nitrous oxide and carbon dioxide flux emission.
Table 4 Greenhouse gases flux changes between 1986 and 1992
Land- use/Land cover class | Total flux of CO2 (mg/day) |
Total flux of N2O (mg/day) | Total flux of CH4 (mg/day) |
| 1986 | 1992 | 1986 | 1992 | 1986 | 1992 |
Primary forest | 1.69x1014 | 1.28x1014 | 3.2x109 | 2.43x109 | -1.45x1010 | -1.10x1010 |
Secondary forest | 0.00 | 5.75x1012 | 0.00 | 7.03x108 | 0.00 | -3.36x109 |
Logged forest | 1.24x1014 | 1.54x1014 | 2.48 x109 | 3.08x109 | -1.04x1010 | -1.29x1010 |
Fallow land | 1.31x1014 | 8.46x1013 | 4.51 x109 | 2.91x109 | -1.00x1010 | -6.47x109 |
| Grassland | 7.76x1012 | 7.58x1012 | 1.42 x108 | 1.38x108 | 0.00 | 0.00 |
Bare land | 2.44x1010 | 2.44x1010 | 5.67x105 | 5.67x105 | -6.25x105 | -6.25x105 |
Cash crops plantation* | 1.87x1013 | 6.75x1013 | 4.68x108 | 1.69x109 | 0.00 | 0.00 |
Paddy field | - | - | 9.63x107 | 6.23x107 | 7.22x108 | 4.67x108 |
Upland field | 0.00 | 2.41x1012 | 0.00 | 4.03x107 | 0.00 | 0.00 |
Cultivated land and Secondary vegetation | 8.00x1013 | 9.02x1013 | 3.43 x109 | 3.87x109 | -3.33x109 | -3.75x109 |
Cultivated lands and Settlement | 6.85x1012 | 8.33x1012 | 1.16 x108 | 1.41x108 | 0.00 | 0.00 |
| Total flux | 536.5x1012 | 548.3x1012 | 14.4 x109 | 15.1x109 | -37.5x109 | -37.0x109 |
Note : calculations were made based on field measurement in November 1997, conducted by IC-SEA
* : assumed flux of CH4 and CO2 of cash crops plantation are equal upland, while flux of N2O is equal to three times
of upland field flux due to intensive fertilizer application.
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