Judul: Emisi Karbon Dioksida Dari Tanaman Kelapa Sawit Pada Lahan Gambut Di Sumatra
Abstrak: Peatlands are formed by decomposed plants residues, with vegetation that are submerged. The process of peat formation occurs when the rate of deposition exceeds the rate of loss of organic materials. Peatlands in the world only 3% of the entire land, but store 30% of the world terrestrial carbon. Indonesia is estimated to have the largest amount of carbon in tropical peat of 57,4 Gt. Over the past 20 years, peatlands have been converted for agriculture. Oil palm plantations in Indonesia are mostly developed on peat soil. In 1990, the area of oil palm on peat land in Sumatra was 17.985 hectares, and substantially increased up to 1.026.922 hectares in 2010. The development of oil palm on peatland involve drainage that can disturb the capacity of peatlands in storing carbon. This literature study aims to assess the effect of drainage on carbon dioxide emissions of oil palm plantations on peatlands in Sumatera. Drainage of peatlands lead to an increase in carbon dioxide emissions. Separation processes in carbon dioxide emissions shows the contribution of peat decomposition, root respiration, plant biomass and fires for land clearing. Heterotrophic respiration (decomposition of peat) contributes 73% of the total soil respiration and the remaining 27% is from autotrophic respiration (root respiration).
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Judul: Dinamika Karbon Tanah Akibat Konversi Lahan dan Hubungannya dengan Penambahan Gas Rumah Kaca di Atmosfer (Studi Kasus : Pulau Sumatera)
Abstrak: Soil is the largest carbon storage in terrestrial ecosystems, thus soil plays an important role in the global carbon cycle. The increasing of human needs in terms of economic, social, and institutional are the factors affecting land use change in order to meet the necessities of life. Changes of vegetation / land cover / land use causes changes in biomass and biomass carbon stock. This conditions affecting amount and distribution of plant’s scrabs and tissue underneath which are the main source of soil organic material, thus will affect the soil organic carbon stock. Overall, if the organic soil material changing, the organic carbon will change as well. Changes in land cover can increase carbon loss through several mechanisms, namely: 1) destroy soil aggregates that protect the soil organic materials from decomposition, 2) stimulate microbial’s activity by improving soil aeration, 3) mixing the fresh organic material into soil which the conditions are more favourable for decomposition rather than in the soil surface. In addition, cultivate land more easily eroded, resulting in the loss of carbon. Moreover, land use can cause soil more easily being eroded. This research is aimed to estimate soil carbon emissions due to land use changes that occurred since 2003 to 2006 on mineral soil and peat soil on first soil layer in Sumatra island using the method of soil carbon emissions estimation created by the IPCC in 2006. The amount of emissions that occur due to land use change in mineral soil is 38.435.198 acres, which its emissions is 83.025 tons/year of C or equal to 304.704 ton/year of CO2. While the changes that occur in peatlands in Sumatra to contribute as much 41.236.091 tons/year of C or equal to 151.336.454 tons/year of CO2 for 6.643.778 acres of land area change.
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Judul: Antibodi anti-idiotipe sebagai kandidat vaksin rabies, Anti-idiotype andibody as a rabies vaccine candidate
Abstrak: Anti rabies serum (ARS) called antibody 1 (Ab1) was used as the antigen to immunize laying chickens. Anti-Ab1 chicken immunoglobulins (IgY), the antiidiotype antibodies against rabies (Ab2) was isolated from chicken blood every week for ten weeks. The highest titer of Ab2 was found at the third week after the last immunization. Immunoglobulin Y was separated by means of ammonium sulfate precipitation, then dialyzed using PBS pH 8.0 for 24 hours at 2 – 8 oC and purified using affinity chromatography column for IgY lead the proteins molecules with 185,000; 95,000 and 49,000 dalton in weigth. Purified IgY was used to immunize New Zealand White rabbit and the antibody response (Ab3) was detected using Agar Gel Precipitation Test (AGPT). The Ab3 showed specific reaction with Ab2 as well as rabies virus. Interestingly, Ab2 and rabies virus express partial identity reaction. This lead the insight, that not all parts of Ab2 are internal image of rabies virus. The efficacy of Ab3 was detected using enzyme linked immunosorbent assay (ELISA) and indicated that the level of Ab3 titer is protective according to WHO standard (more than 0.5 IU/ml). The conclusion of this study is the anti-idiotype antibody can induce protective immune response against rabies virus and can be used as an alternative for rabies anti-idiotype vaccine. Key words : anti-idiotype vaccine, antibody, rabies
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