Figure-1
A number of different flow regimes may occur during natural flow in vertical tubing. In order to describe each, let us first talk about oil well and assume that the pressure at the base of the tubing is above the bubble point. In such a case the flow regime at that point will consist of liquid flow ( Figure 2 ).
Upward movement of the liquid is accompanied by reduced pressures and, as the pressure drops below the bubble point, gas bubbles begin to form. These bubbles slip upward through the rising column of liquid, with the larger bubbles going up more rapidly than the smaller. This can be called as bubble flow.
Further up the tubing, as pressure continues to drop, more gas will be released from the solution and the larger bubbles grow steadily by overtaking and coalescing with the smaller ones. Eventually a stage may be reached at which the larger gas bubbles will be formed and fill almost the entire cross section of the tubing and, as they move upward, carry between them slugs of oil containing small gas bubbles. This is referred to as plug or slug flow. It is the most efficient natural lift regime because it uses the gas to full effect rather than losing its potential lifting power to the slippage that occurs during bubble flow. However it will create an unstable flow condition in the pipe that there will be large fluctuations in both pressure and flow rate.
More higher in the tubing, the pressure will be less and lower, the gas may break through and form a continuous channel in the center of the string, with oil moving slowly upward in an annular ring on the inside wall of the tubing. this is called as annular flow. Such annular flow is clearly inefficient.
Finally, if the tubing is of considerable length so that a large pressure drop exists from the bottom to top, the annulus of liquid may almost disappear, leaving only the flow of gas carrying a mist of liquid droplets. Now we have what is called mist flow and it is characteristic of many oil wells with very high gas oil ratio or liquid gas ratio.
Further up the tubing, as pressure continues to drop, more gas will be released from the solution and the larger bubbles grow steadily by overtaking and coalescing with the smaller ones. Eventually a stage may be reached at which the larger gas bubbles will be formed and fill almost the entire cross section of the tubing and, as they move upward, carry between them slugs of oil containing small gas bubbles. This is referred to as plug or slug flow. It is the most efficient natural lift regime because it uses the gas to full effect rather than losing its potential lifting power to the slippage that occurs during bubble flow. However it will create an unstable flow condition in the pipe that there will be large fluctuations in both pressure and flow rate.
More higher in the tubing, the pressure will be less and lower, the gas may break through and form a continuous channel in the center of the string, with oil moving slowly upward in an annular ring on the inside wall of the tubing. this is called as annular flow. Such annular flow is clearly inefficient.
Finally, if the tubing is of considerable length so that a large pressure drop exists from the bottom to top, the annulus of liquid may almost disappear, leaving only the flow of gas carrying a mist of liquid droplets. Now we have what is called mist flow and it is characteristic of many oil wells with very high gas oil ratio or liquid gas ratio.
In wet gas flow, Pressure drop and the critical gas flow rate are functions of pipe diameter, pipe profile, fluid properties, liquid-to-gas ratio, temperature and so on. If the gas flow rate is above the critical gas flow rate, the flow is friction-dominated, which means that the frictional pressure drop is the majority in creating the total pressure drop. Pressure drop increases with the gas flow rate increases. Due to relatively high gas velocity then the liquid, so then the liquid holdup will be small, and no liquid accumulation will be formed. Then it is dominated by the flow patern of Stratified-wavy flows, and the system is stable. However, if the gas flow rate is below the critical gas flow rate, the flow becomes gravity-dominated. Gravitational pressure drop now becomes larger than frictional pressure drop, and the total pressure drop increases as gas flow rate decreases. Liquid holdup is very sensitive to pipe inclination. A small change of inclination angle. Liquid accumulates in the sections as well as the gas causing pressure build-up at upstream. When the upstream pressure becomes high enough, the accumulated liquid is pushed up to downstream in a large liquid slug at a high velocity; this is called a terrain slug. The system operated in this region will be unstable, with large fluctuations in both of pressure and liquid flow rate.
The description of tubing flow regimes and pressure losses that occur is an extremely complex subject. In practice not all of these flow regimes are present simultaneously in a single tubing string. On the other hand, two, three or even more may occur at the same time. In any case, identifying the flow regime is the first step in determining the tubing pressure drop.