"Economic
Development and the Environment"
on the Sakhalin Offshore Oil and Gas Fields II
Copyright (C) 1999 by Slavic
Research Center, Hokkaido University.
All rights reserved
Oil and Gas Development on the Sakhalin Island Shelf: An Assessment of Changes in the Okhotsk Sea Ecosystem
Alexander Leonov
- | Annual experimental studies of the transformations of oil hydrocarbons (mainly paraffins with large amounts of long chain n-alkanes in the C20-C35 range) in sediments of a mangrove estuary showed that at first, the decrease in their concentration was determined by physical processes, and then, by biodegradation. Nitrogen deficiency was the main critical factor in limiting the biodegradation rate [73]. |
- | It was determined that at constant low temperatures, the processes of evaporation and weathering were most important in the transformation and spatial distribution of oil products [74]. |
- | Experiments in the Kara Sea showed that only 1% of paraffin hydrocarbon fractions were mineralized per day by microorganisms. The oil-oxidizing activity of microorganisms was developed for about a month after an oil spill in the northern regions. In Arctic waters, the contribution of microorganisms in the self-cleaning of marine waters from oil pollution was about 5% [67]. |
- | In experiments with oil spilled on ice, oil degradation was practically absent because after nine months only a 5% loss in oil mass was registered [67]. |
- | Experiments were conducted to measure the visibility of oil slicks [75], oil photo-oxidation [76], oil biodegradation [77], the stability of oil emulsions [78] and oil dispersants [79], and the ability of marine microorganisms to produce bio-dispersants to degrade crude oil [80]. |