Dissolution And Rise Velocity Of Small Air Bubbles In Water And Salt Water

Author(s):  
R. Detsch ◽  
I. Harris
Keyword(s):  
2021 ◽  
Vol 932 ◽  
Author(s):  
Vikash Pandey ◽  
Dhrubaditya Mitra ◽  
Prasad Perlekar

We present a direct numerical simulation (DNS) study of buoyancy-driven bubbly flows in the presence of large-scale driving that generates turbulence. On increasing the turbulence intensity: (a) the bubble trajectories become more curved and (b) the average rise velocity of the bubbles decreases. We find that the energy spectrum of the flow shows a pseudo-turbulence scaling for length scales smaller than the bubble diameter and a Kolmogorov scaling for scales larger than the bubble diameter. We conduct a scale-by-scale energy budget analysis to understand the scaling behaviour observed in the spectrum. Although our bubbles are weakly buoyant, the statistical properties of our DNS are consistent with the experiments that investigate turbulence modulation by air bubbles in water.


Fluids ◽  
2021 ◽  
Vol 6 (12) ◽  
pp. 437
Author(s):  
Andrea Cioncolini ◽  
Mirco Magnini

Shapes and rise velocities of single air bubbles rising through stagnant water confined inside an annular channel were investigated by means of experiments and numerical simulations. Fast video imaging and image processing were used for the experiments, whilst the numerical simulations were carried out using the volume of fluid method and the open-source package OpenFOAM. The confinement of the annular channel did not affect the qualitative behavior of the bubbles, which exhibited a wobbling rise dynamic similar to that observed in bubbles rising through unconfined liquids. The effect of the confinement on the shape and rise velocity was evident; the bubbles were less deformed and rose slower in comparison with bubbles rising through unconfined liquids. The present data and numerical simulations, as well as the data collected from the literature for use here, indicate that the size, shape, and rise velocity of single bubbles are closely linked together, and prediction methods that fail to recognize this perform poorly. This study and the limited evidence documented in the literature indicate that the confinement effects observed in non-circular channels of complex shape are more complicated than those observed with circular tubes, and much less well understood.


2019 ◽  
Vol 123 (24) ◽  
pp. 15131-15138 ◽  
Author(s):  
Piotr Pawliszak ◽  
Vamseekrishna Ulaganathan ◽  
Bronwyn H. Bradshaw-Hajek ◽  
Rogerio Manica ◽  
David A. Beattie ◽  
...  

2013 ◽  
Vol 94 ◽  
pp. 60-68 ◽  
Author(s):  
Shahram Amirnia ◽  
John R. de Bruyn ◽  
Maurice A. Bergougnou ◽  
Argyrios Margaritis

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


Author(s):  
Raveesha P ◽  
K. E. Prakash ◽  
B. T. Suresh Babu

The salt water mixes with fresh water and forms brackish water. The brackish water contains some quantity of salt, but not equal to sea water. Salinity determines the geographic distribution of the number of marshes found in estuary. Hence salinity is a very important environmental factor in estuary system. Sand is one major natural aggregate, required in construction industry mainly for the manufacture of concrete. The availability of good river sand is reduced due to salinity. The quality of sand available from estuarine regions is adversely affected due to this reason. It is the responsibility of engineers to check the quality of sand and its strength parameters before using it for any construction purpose. Presence of salt content in natural aggregates or manufactured aggregates is the cause for corrosion in steel. In this study the amount of salinity present in estuary sand was determined. Three different methods were used to determine the salinity in different seasonal variations. The sand sample collected nearer to the sea was found to be high in salinity in all methods.  It can be concluded that care should be taken before we use estuary sand as a construction material due to the presence of salinity.


2008 ◽  
Vol 37 (3) ◽  
Author(s):  
Jacek Urbański ◽  
Agata Ślimak

Assessing flood risk and detecting changes of salt water inflow in a coastal micro-tidal brackish marsh using GISIn order to assess changes in salt water inflow and potential flood risks due to sea level rise in a micro-tidal Beka brackish marsh on the Polish Baltic Coast GIS was used. Such wetlands are important elements of coastal zone natural environments. Creating a geodatabase within a GIS system makes it possible to carry out broad analyses of complex systems, such as coastal wetlands. The results indicate that a 40 cm sea-level rise would considerably increase the frequency of flooding in the investigated area, in part because of the small range of the annual sea level oscillations there. A map of the index of changes in saltwater inflow, created with the help of cost-weighted distance (functions), shows that changes which have occurred along the shore, consisting of filling in the drainage channel outlets, have likely had a significant impact on the vegetation of the area.


2018 ◽  
Author(s):  
Timothy Duignan ◽  
Marcel Baer ◽  
Christopher Mundy

<div> <p> </p><div> <div> <div> <p>The surface tension of dilute salt water is a fundamental property that is crucial to understanding the complexity of many aqueous phase processes. Small ions are known to be repelled from the air-water surface leading to an increase in the surface tension in accordance with the Gibbs adsorption isotherm. The Jones-Ray effect refers to the observation that at extremely low salt concentration the surface tension decreases in apparent contradiction with thermodynamics. Determining the mechanism that is responsible for this Jones-Ray effect is important for theoretically predicting the distribution of ions near surfaces. Here we show that this surface tension decrease can be explained by surfactant impurities in water that create a substantial negative electrostatic potential at the air-water interface. This potential strongly attracts positive cations in water to the interface lowering the surface tension and thus explaining the signature of the Jones-Ray effect. At higher salt concentrations, this electrostatic potential is screened by the added salt reducing the magnitude of this effect. The effect of surface curvature on this behavior is also examined and the implications for unexplained bubble phenomena is discussed. This work suggests that the purity standards for water may be inadequate and that the interactions between ions with background impurities are important to incorporate into our understanding of the driving forces that give rise to the speciation of ions at interfaces. </p> </div> </div> </div> </div>


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