Diplomarbeit, 2013
95 Seiten, Note: A
Geowissenschaften / Geographie - Phys. Geogr., Geomorphologie, Umweltforschung
1. CHAPTER 1
1.1 INTRODUCTION
1.1.1 BACKGROUND
1.2 AIMS AND OBJECTIVES OF THE WORK
1.3 LAYOUT OF THE THESIS
2. CHAPTER 2
2.1 LITERATURE REVIEW
2.1.1 OIL SPREADING UNDER ICE
2.2 OIL MIGRATION UNDER ICE
2.3 MODELLING OIL SPREADING UNDER ICE
2.4 CONCLUSIONS
3. CHAPTER 3
3.1 METHODOLOGY
3.3 EXPERIMENTAL PROCEDURE
4. CHAPTER 4
4.1 RESULTS AND DISCUSSION
4.1.1 INTRODUCTION
4.2 LABOROTARY OBSERVATIONS
4.3 FIELD OBSERVATIONS
4.3.1 Flow profile under river ice
4.4 DISCUSSION OF RESULTS
4.5 MAIN FINDINGS
5. CHAPTER 5
5.1 DEVELOPMENT OF THE SPILL RESPONSE DEVICE
5.1.1 INTRODUCTION
5.2 DEFINING REQUIREMENTS FOR DEVICE
5.4 DESIGN BACKGROUND
5.4.1 Vertical Velocity of Oil Droplets
5.4.2 Flow Velocity in River
5.4.3 Oil Droplets Surfacing Point and Installation Angle
5.4.4 Oil Surfacing Point When Velocity Profile Is Known
5.5 SUMMARY OF ASSUMPTIONS
5.6 EXPERIMENTAL WORK
5.7 RESULTS
5.7.1 Effective Installation Angle
5.7.2 Effective Channel Spacing
5.7.3 Effective Channel Form
5.7.4 Clogging
5.7.5 Effective Channel Material
5.8 CONCLUSIONS
5.9 RECOMMENDATIONS
6. CHAPTER 6
6.1 CONCLUSIONS AND RECOMMENDATIONS
6.1.1 GENERAL RECOMMENDATIONS
6.2 CONCLUSIONS
6.3 RECOMMENDATIONS FOR FUTURE STUDY
The primary aim of this research is to evaluate the effectiveness of current oil spill response methods in ice-covered rivers and to develop a functional concept device for localizing oil spills in such challenging environments.
4.2 LABOROTARY OBSERVATIONS
Experiments were conducted in circulating flume with dimensions 4 x 0.4 x 0.4 (m) with real ice. (For details of equipment and procedures used in experiments, please refer to Methodology chapter).
Oil was released through a 0.2 mm diameter (of head) syringe at the flow rate of 2 ml/s, therefore, the velocity of oil at discharge was 16 cm/s. Immediately after release, there was a jet phase that consisted of high-velocity oil. The jet phase was dissipated quickly within about 5 cm of the release point. Droplet sizes were in the range of one to five mm. Then, oil droplets started to rise as a plume due to differential density between the continuous medium (water) and oil. Visually, it was seen that droplets were rising at different rates. Very small droplets that were less than one mm rose at a rate of 5 cm/s, while bigger droplets reached the water-ice interface in a couple of seconds (30 cm/s) Upon reaching ice, oil droplets remained its form and later coalesced to form a thick layer of oil. It was clear that even under the very smooth ice the oil spreading was retarded due to the presence of ice.
CHAPTER 1: Provides the introduction and motivation for the research, highlighting the challenges of oil spills under ice.
CHAPTER 2: Reviews previous research and existing mathematical models regarding oil spreading and migration under ice cover.
CHAPTER 3: Details the experimental setup, flume configurations, and field observation procedures used for data collection.
CHAPTER 4: Presents the results of laboratory experiments and field observations concerning oil movement and river flow profiles.
CHAPTER 5: Introduces the development of an Under-Ice Channel (UIC) concept device, its design criteria, and testing results.
CHAPTER 6: Summarizes the key research findings, provides conclusions, and offers recommendations for future study and industry practice.
Oil spill, ice-covered river, spill response, pipeline rupture, oil migration, ice slotting, diversionary plywood, hydrodynamics, flow velocity, under-ice channel, oil containment, laboratory flume, environmental pollution, spill localization, cold-weather response.
The work focuses on determining the efficacy of current oil spill response strategies, specifically the method of cutting ice slots to contain spills, within ice-covered river environments.
The research examines oil behavior under ice, the insufficiency of existing current-based recovery methods, and the design of new, specialized equipment for cold-weather oil localization.
The goal is to determine if current-based oil recovery methods are sufficient in lowland rivers and to develop a more effective, device-based approach for spill containment.
The study combines small-scale laboratory experiments in a circulating flume with field observations of flow profiles in a natural, ice-covered river.
The main sections cover literature reviews on oil dynamics, detailed methodologies for experimental and field work, results of these tests, and the conceptual design and validation of an Under-Ice Channel (UIC).
Key terms include oil spill, ice-covered river, spill response, under-ice channel, and oil migration.
The author concludes that these methods are often scientifically unjustified in many lowland rivers because the current beneath the ice is frequently too weak to initiate or sustain the movement of oil toward the slots.
Ice roughness significantly increases the threshold velocity required to move spilled oil; even small irregularities in the ice significantly impede the movement of the oil slick.
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