| 1. |
- Hustad, J.E., et al.
(författare)
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Reactivity measurements of coke particles in five different flow reactors
- 1990
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Ingår i: Rivista dei Combustibili. - 0370-5463. ; 44:10, s. 257-267
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Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
- Experiments on reactivity of 128 μm coke particles in the gas temperature range from 1150 K to 1370 K have been performed in five different flow reactors in the Nordic countries and all the results were calculated by the shrinking particle model. The activation energy is found to be 25 kcal/mol indicating combustion control by the combined effects of chemical kinetic and pore diffusion (zone II combustion). The overall apparent reaction order was found to be 1.0
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| 2. |
- Holgersson, J, et al.
(författare)
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Blood group A glycolipid antigen expression in kidney, ureter, kidney artery, and kidney vein from a blood group A1Le(a-b+) human individual. Evidence for a novel blood group A heptaglycosylceramide based on a type 3 carbohydrate chain.
- 1990
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Ingår i: The Journal of biological chemistry. - 0021-9258. ; 265:34, s. 20790-8
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Tidskriftsartikel (refereegranskat)abstract
- Kidney, ureter, kidney artery, and kidney vein tissue were obtained from a single human transplant specimen. The donors erythrocyte blood group phenotype was A1Le(a-b+). Total non-acid glycolipid fractions were isolated and individual glycolipid components were identified by immunostaining thin layer plates with a panel of monoclonal antibodies and by mass spectrometry of the permethylated and permethylated-reduced total glycolipid fractions. The dominating glycolipids in all tissues were mono- to tetraglycosylceramides. In the kidney, ureter, and artery tissue less than 1% of the glycolipids were of blood group type, having more than 4 sugar residues. In contrast, 14% of the vein glycolipids were of blood group type, and the dominating components were type 1 chain blood group H pentaglycosylceramides and A hexaglycosylceramides. Trace amounts of structurally different blood group A glycolipids (type 1 to 4 core saccharide chains) with up to 10 sugar residues were found in the kidney, ureter, and vein tissues, including evidence for a novel blood group A heptaglycosylceramide based on the type 3 chain in the vein. The only detected A glycolipid antigen in the artery tissue was the blood group A difucosyl type 1 chain heptaglycosylceramide (ALeb) structure. Blood group Lewis and related antigens (Lea, Leb, and ALeb) were expressed in the kidney, ureter, and artery, but were completely lacking in the vein, indicating that the Le gene-coded alpha 1-4-fucosyltransferase was not expressed in this tissue. The X and Y antigens (type 2 chain isomers of the Lea and Leb antigens) were detected only in the kidney tissue.
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| 3. |
- Johnsen, Sigfus J., et al.
(författare)
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A "deep" ice core from east Greenland
- 1992
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Ingår i: MoG Geoscience. ; 29
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Tidskriftsartikel (refereegranskat)abstract
- Pilot studies on the Renland peninsula in Scoresbysund Fjord, East Greenland, indicated that the relatively small and separate Renland ice cap meets most of the criteria defining a favourable ice-core drill-site. In 1988, a Nordic expedition recovered a continuous surface-to-bedrock ice core from the summit. This relatively short core reaches deep into the past, probably throughout the last glaciation and through most of the preceding interglacial, Eem, 125,000 years B.P. The core contains detailed information on temporal changes of the coastal environment, and serves as a valuable complement to the new deep ice cores being drilled in Central Greenland. Core analyses suggest that (1) during Eemian time the East Greenland climate was at least 5ÔC warmer than now, and the precipitation 20% higher; (2) during the last glacial period, the precipitation decreased to a minimum, perhaps only 20% of the present value; (3) the post-glacial climatic optimum was 2,5ÔC warmer than now; (4) the long-term variability of the record is relatively low, due to isostatic movements in the area; and (5) from 70,000 years B.P. the Greenland glacial climate alternated between two quasi-stable stages. The latter point may reflect a chaotic feature of climate. If so, climate predictions will be difficult to access.
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