Air Barriers as Oil-Spill Containment Devices

1972 ◽  
Vol 12 (02) ◽  
pp. 126-142 ◽  
Author(s):  
Warren T. Jones

Jones, Warren T., Shell Pipe Line Corp., Houston, Tex. Abstract As a part of a program to evaluate oils pill containment devices, an experimental investigation of air barriers was performed. Previously published relationships for air barriers operating in still water were verified. Tests involving a current were conducted in a recirculating test tank in water 7 ft deep. The structure of the bubble plume was found to change with increasing current, and a phenomenological explanation was developed. phenomenological explanation was developed. During all of these tests, measurements of the magnitude of the surface current showed it to be very turbulent. Tests with oil on the water surface showed this turbulence to be the major factor in the failure of an air barrier completely to retain oil in the presence of a current. The combination of turbulence and the inherent instability of flowing, stratified fluids tears drops off the bottom of the oil slick in the stagnation region. The downward flow in this region then transports the oil drops below the surface current produced by the air barrier, and the main current carries the drops through the barrier. On the downstream side, the drops gradually rise to the surface. The main body of the slick is retained upstream of the barrier, and observation from above the surface of murky waters would not reveal these drops surfacing far downstream of the barrier. Varying orifice size and spacing had no effect on the surface current turbulence or mean velocity. Large quantities of spilled oil have been recovered at a prototype installation by placing the barrier at an angle to the current. The final phase of the investigation was concerned with the use of an air barrier across the mouth of an enclosed body of still water a slip, cove, or marina. Thickness of oil retained by the barrier in still water as a function of operating conditions has been obtained experimentally, and tentative limits on the use of this formulation for prototype spills are given. Introduction Air barriers have been used as breakwaters, to guard against salt water intrusion into fresh water regions, to keep harbors free of ice during winter, and as a means of preventing sediment deposition in critical areas. In recent years they have been proposed and installed as oil containment devices. An air barrier is basically a pipe with holes spaced along its length that is laid under water on the bottom (Fig. 1). Air is supplied to the pipe (manifold), exits through the holes (orifices) pipe (manifold), exits through the holes (orifices) and rises to the water surface. Water is entrained by the upward flow of air bubbles and moves vertically with the air. At the surface, the air bubbles escape and the water flow becomes two horizontal surface currents moving in opposite directions away from the manifold location:The object of this program was to give the operating personnel, who might conceivably be involved with an oil spill, some idea of the capabilities of containment and removal equipment currently available. A review of this program has been given by Milz. Air barriers were included in the equipment surveyed and evaluated; experiments were conducted to evaluate the effects of a current on an air barrier and, if possible, to determine the conditions under which an air barrier would fail to retain oil. LITERATURE REVIEW The majority of the work applicable to oil containment has been found in the literature on pneumatic breakwaters. Green gives a general pneumatic breakwaters. Green gives a general review of this literature. SPEJ p. 126

The conditions under which an outward-flowing surface current can prevent the passage of waves coming in from the sea are investigated mathematically. Two types of current are considered: ( a ) a current with uniform velocity extending to a depth h ; ( b ) a current with velocity decreasing uniformly and vanishing at depth h . They have very similar effects. The mean velocity required to stop waves of given frequency is rather greater in case ( a ) than in case ( b ). The water current produced by a curtain of air bubbles from a perforated tube on the sea bottom is investigated theoretically on the assumption that the bubbles are very small. Evans (1955) has measured the surface currents produced in a tank by a bubble curtain and finds them smaller than predicted. The discrepancy is partly due to the fact that the bubbles were not very small.


2011 ◽  
Vol 11 (1) ◽  
pp. 24-32 ◽  
Author(s):  
randy fertel

The source of 25 to 30 percent of America’s seafood, the Mississippi River Delta’s cornucopian world is now uncertain. And yet, even if shrimp, oysters, and finfish are unaffected by the BP Oil Spill—a big if—one can already reflect on the passing of the culture once built upon gathering them. For almost three centuries, levees made life possible along the riverbanks and in the wetlands beyond. Those same levees also ensured the wetlands would eventually melt away into the Gulf. Cutting off the silt left behind during annual river inundations subjected the fragile land to erosion. Sulfur, natural gas, and oil production companies dug twenty thousand miles of canals to gain more direct routes to their fields and to pump out their mineral wealth. This caused salt-water intrusion that killed off plant life and caused more erosion. The world that sustained my Plaquemines ancestors was less subject to collapse following disasters not only because the ecosystem before the wetlands’ ongoing loss was then more vibrant, complex, and robust; but also because their lives, especially their culinary lives, were more vibrant, complex, and robust. Life was hard, but when it came to putting food on the table, life followed the seasons.


Ground Water ◽  
1980 ◽  
Vol 18 (2) ◽  
pp. 147-151 ◽  
Author(s):  
B. K. Panigrahi ◽  
A. Das Gupta ◽  
A. Arbhabhirama

Author(s):  
Hossein Gholizadeh ◽  
Doug Bitner ◽  
Richard Burton ◽  
Greg Schoenau

It is well known that the presence of entrained air bubbles in hydraulic oil can significantly reduce the effective bulk modulus of hydraulic oil. The effective bulk modulus of a mixture of oil and air as pressure changes is considerably different than when the oil and air are not mixed. Theoretical models have been proposed in the literature to simulate the pressure sensitivity of the effective bulk modulus of this mixture. However, limited amounts of experimental data are available to prove the validity of the models under various operating conditions. The major factors that affect pressure sensitivity of the effective bulk modulus of the mixture are the amount of air bubbles, their size and the distribution, and rate of compression of the mixture. An experimental apparatus was designed to investigate the effect of these variables on the effective bulk modulus of the mixture. The experimental results were compared with existing theoretical models, and it was found that the theoretical models only matched the experimental data under specific conditions. The purpose of this paper is to specify the conditions in which the current theoretical models can be used to represent the real behavior of the pressure sensitivity of the effective bulk modulus of the mixture. Additionally, a new theoretical model is proposed for situations where the current models fail to truly represent the experimental data.


2016 ◽  
Author(s):  
Karin Ebert ◽  
Karin Ekstedt ◽  
Jerker Jarsjö

Abstract. Future sea level rise as a consequence of global warming will affect the world's coastal regions. Even though the pace of sea level rise is not clear, the consequences will be severe and global. Commonly the effects of future sea level rise are investigated for relatively vulnerable development countries; however, a whole range of varying regions need to be considered in order to improve the understanding of global consequences. In this paper we investigate consequences of future sea level rise along the coast of the Baltic Sea island of Gotland, Sweden, with the aim to fill knowledge gaps regarding comparatively well-suited areas in non-development countries. We study both the quantity of loss of infrastructure, cultural and natural values for the case of a two metre sea level rise of the Baltic Sea, and the effects of climate change on seawater intrusion in coastal aquifers, causing the indirect effect of salt water intrusion in wells. We conduct a multi-criteria risk analysis by using Lidar data on land elevation and GIS-vulnerability mapping, which gives formerly unimaginable precision in the application of distance and elevation parameters. We find that in case of a 2 m sea level rise, 3 % of the land area of Gotland, corresponding to 99 km2, will be inundated. The features most strongly affected are items of touristic or nature values, including camping places, shore meadows, sea stack areas, and endangered plants and species habitats. In total, 231 out of 7354 wells will be directly inundated, and the number of wells in the high-risk zone for saltwater intrusion in wells will increase considerably. Some values will be irreversibly lost due to e.g. inundation of sea stacks and the passing of tipping points for sea water intrusion into coastal aquifers; others might simply be moved further inland, but this requires considerable economic means and prioritization. With nature tourism being one of the main income sources of Gotland, monitoring and planning is required to meet the changes. Seeing Gotland in a global perspective, this island shows that holistic multi-feature studies of future consequences of sea level rise are required, to identify overall consequences for individual regions.


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