2.1 Definition of the pressure recovery through sudden expansions and the phenomena associated
Before discussing the existing PR models, it is important to explain as a first step how the pressure recovery is calculated. The passage of the two-phase flow, as a single-phase flow, through the sudden expansion causes its deceleration in the area just downstream called the recovery region; this deceleration causes an increase of the static pressure. When it reaches its maximum, the static pressure begins to decrease, joining the pressure gradient downstream of the singularity: the flow re-establishes. The pressure recovery is calculated by extrapolating the linear lines representing the gradient of the pressure upstream and downstream of the singularity at the location of the sudden expansion, as shown in Fig. 1. The difference between the intersections of these two lines at the location of the sudden expansion (position z = 0) gives the pressure recovery.
Due to the difference in physical properties between the gas and the liquid (i.e., density and viscosity), the two phases don’t decelerate in the same way downstream of the singularity. Thus, the downstream region close to the singularity exhibits recirculation zones (Salhi, 2010, Roul and Dash, 2011). The latter lead to a redistribution of the void fraction (Ahmed, 2007; Roman et al., 2020; Liang et al., 2022) and a modification of the flow regime or sub-regime downstream the singularity (Attou et al., 2000; Kondo et al., 2002; Arabi et al., 2018, 2021b; Zhang and Goharzadeh, 2019). The hydrodynamics parameters (Aloui and Souhar, 1996b; Ahmed et al., 2008; Rosero et al., 2021) as well as the heat transfer characteristics (Lobanov et al., 2019; Chinak et al., 2019), in the case of non-isothermal flows, are also disturbed.
2.2 Existing pressure recovery models
In this section, we have started with the presentation of existing PR models in the case of single-phase flow in order to better understand the two-phases models.
Solving the momentum equation inside the control volume between the upstream and downstream (after the flow recovery) pipes gives Eq. 2, which is known as the Borda-Carnot equation.
$$PR= \frac{\sigma (1-\sigma ){G}_{1}^{2}}{\rho }$$
2
where G1 is the total upstream mass flux and ρ the fluid density.
The mechanical energy balance equation leads to the following equation:
$$PR= \frac{\frac{1}{2}(1-{\sigma }^{2}){G}_{1}^{2}}{\rho }$$
3
Regarding the two-phase flow, a variety of models have been developed through the years. These models are summarized in Table 1. The analytical models are obtained by applying the homogenous or heterogeneous model to the single-phase conservation equations (momentum or mechanical energy). The model of Romie (1958) was obtained by applying the heterogeneous model to the single-phase momentum conservation equation. The model of Delhaye (1981) is based on the assumption that the void fraction, upstream (α1) and downstream (α2) the singularity, remains constant. Lottes (1958), in his model, assumed that the dynamic pressure recovery occurs only on the liquid phase. For Chisholm and Sutherland (1969), the PR is the product of the liquid pressure recovery (PRL) and the two-phase multiplier (\({\text{ф}}_{L}^{2}\)).
Ahmed et al. (2007) developed an analytical expression by adding two terms to the pressure recovery model of Romie (1958). The first is the pressure difference between the upstream flow and the downstream face of the expansion, whereas the second one is due to the shear stress in the developing region downstream of the enlargement. The exponent r, used in the model of Attou and Bolle (1997) is a correction factor that depends on the nature of the working fluids. The authors recommended to use r = -1.4 for air-water mixture and r = 1 for a water-steam mixture.
Wadle (1989) proposed a semi-empirical model which was not developed from the theoretical momentum or mechanical energy conservation equations. Thus, this model is based on the assumption that the pressure recovery is proportional to the dynamic pressure difference caused by the deceleration of the two phases due to the sudden expansion. This model recourses to an empirical coefficient K. Based on his experimental data, Wadle (1989) suggested to use different values of K for air-water and steam-water systems. Owen et al. (1992) found that their experimental results were well correlated with Wadle's model using K = 0.22. The difference between this value and those suggested by Wadle (1989) can be explained by the geometry used as well as the conditions of each experiment. Using experimental results obtained with sudden expansions of the area ratio of 0.26 and 0.39, Chen et al. (2007) modified the empirical coefficient of Wadle's model by correlating it with the aspect ratio.
It also exists some purely empirical models. For example, Ahmed et al. (2003) developed their empirical model using their data obtained with air-oil mixture. Wang et al. (2010) compared the predictions of several models (Homogenous models, Richardson, 1958; Chisholm and Sutherland, 1969; Wadle, 1989; Schmidt and Friedel, 1996; Attou and Bolle,1997; Abdelall et al., 2005) with published experimental data. They found that none of the evaluated models can predict accurately all the databases. Then, Wang et al. (2010) proposed a new model by introducing a coefficient to the homogeneous model. A total of 282 experimental data collected from the literature were used to build this empirical coefficient. This coefficient combines four dimensionless parameters, namely: Bond number (Bo), Weber number (We), Froude number (Fr), and liquid only Reynolds number (ReLO). Kourakos (2011) proposed an empirical model to predict the pressure recovery based on its data obtained with two aspect ratios (0.328 and 0.646).
It also exists phenomenological (mechanistic) models that were not reviewed in the present paper. In fact, these kinds of models were built based on the complex phenomena specific for each flow regime (Hewitt, 1983). As a consequence, the mechanistic models recourse to assumptions and input parameters specific for each flow pattern, which limit their use to only one flow regime. As examples of the PR mechanistic models, we can cite the models of Anupriya and Jayanti (2014, 2018) developed for annular flow, and that of Attou et al. (1997) specific for bubbly flow.
Table 1
Summary of existing models to predict PR
Authors and year
|
Model
|
Homogeneous model applied to the momentum balance
|
\(PR=\sigma \left(1-\sigma \right){G}_{1}^{2}\left[\frac{x}{{\rho }_{G}}+\frac{\left(1-x\right)}{{\rho }_{L}}\right]\)
|
(4)
|
Homogeneous model applied to the mechanical energy balance
|
\(PR=\frac{1}{2}\left(1-{\sigma }^{2}\right){G}_{1}^{2}\left[\frac{x}{{\rho }_{G}}+\frac{\left(1-x\right)}{{\rho }_{L}}\right]\)
|
(5)
|
Romie (1958)
|
\(PR=\sigma \left(1-\sigma \right){G}_{1}^{2}\left[\left(\frac{{x}^{2}}{{{\rho }_{G}\alpha }_{1}}+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}\left(1-{\alpha }_{1}\right)}\right)-\sigma \left(\frac{{x}^{2}}{{{\rho }_{G}\alpha }_{2}}+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}\left(1-{\alpha }_{2}\right)}\right)\right]\)
|
(6)
|
Delhaye (1981)
|
\(PR=\frac{\sigma \left(1-\sigma \right){G}_{1}^{2}}{{\rho }_{L}}\left[\frac{\left({\rho }_{L}/{\rho }_{G}\right){x}^{2}}{\alpha }+\frac{{\left(1-x\right)}^{2}}{\left(1-\alpha \right)}\right]\)
|
(7)
|
Lottes (1961)
|
\(PR=\frac{\sigma \left(1-\sigma \right){G}_{1}^{2}}{{\rho }_{L}{\left(1-\alpha \right)}^{2}}\)
|
(8)
|
Chisholm and Sutherland (1969)
|
\(PR={PR}_{L}{ф}_{L}^{2}\)
|
(9)
|
\({PR}_{L}=\frac{\sigma \left(1-\sigma \right){{\left(1-x\right)}^{2}G}_{1}^{2}}{{\rho }_{L}}\)
|
(10)
|
\({ф}_{L}^{2}=1+\frac{{C}_{h}}{X}+\frac{1}{{X}^{2}}\)
|
(11)
|
\(X=\left(\frac{1-x}{x}\right)\sqrt{\frac{{\rho }_{G}}{{\rho }_{L}}}\)
|
(12)
|
\({C}_{h}=\left[1-\frac{1}{2}\sqrt{\frac{{\rho }_{L}-{\rho }_{G}}{{\rho }_{L}}}\right]\left[\sqrt{\frac{{\rho }_{L}}{{\rho }_{G}}}+\sqrt{\frac{{\rho }_{G}}{{\rho }_{L}}}\right]\)
|
(13)
|
Ahmed et al. [26]
|
\(PR=\sigma \left(1-\sigma \right){G}_{1}^{2}\left[\left(\frac{{x}^{2}}{{{\rho }_{G}\alpha }_{1}}+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}\left(1-{\alpha }_{1}\right)}\right)-\sigma \left(\frac{{x}^{2}}{{{\rho }_{G}\alpha }_{2}}+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}\left(1-{\alpha }_{2}\right)}\right)\right]-\left({P}_{1}-{P}_{0}\right)\left(1-\sigma \right)-\frac{4}{{D}_{2}}\left({\int }_{0}^{{L}_{d}}{\tau }_{d}\left(z\right)dz-{\tau }_{fD}{L}_{d}\right)\)
|
(14)
|
Collier and Thome [60]
|
\(PR=\frac{\left(1-{\sigma }^{2}\right){G}_{1}^{2}}{2\left(\frac{x}{{\rho }_{G}}+\frac{1-x}{{\rho }_{L}}\right)}\left[\frac{{x}^{3}}{{\alpha }^{2}{{\rho }_{G}}^{2}}+\frac{{\left(1-x\right)}^{3}}{{\left(1-\alpha \right)}^{2}{{\rho }_{L}}^{2}}\right]\)
|
(15)
|
Richardson (1958)
|
\(PR=\frac{1}{2}\left(1-{\sigma }^{2}\right){G}_{1}^{2}\left[\frac{{\sigma \left(1-x\right)}^{2}}{{\rho }_{L}\left(1-\alpha \right)}\right]\)
|
(16)
|
Wadle (1989)
|
\(PR=\frac{1}{2}\left(1-{\sigma }^{2}\right){G}_{1}^{2}K\left[\frac{{x}^{2}}{{\rho }_{G}}+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}}\right]\)
|
(17)
|
K = 0.83 for air-water
K = 0.667 for steam-water
|
(18)
|
Owen et al. (1992)
|
K = 0.22
|
(19)
|
Chen et al. (2007)
|
\(K=\frac{1}{1.551-7.64{\sigma }^{2}}\)
|
(20)
|
Schmidt and (1996)
|
\(PR=\frac{{G}_{1}^{2}\left[\frac{\sigma }{{\rho }_{eff}}-\frac{{\sigma }^{2}}{{\rho }_{eff}}-{f}_{e}{\rho }_{eff}\left(\frac{x}{{\rho }_{G}\alpha }-\frac{\left(1-x\right)}{{\rho }_{L}\left(1-\alpha \right)}\right){\left(1-\sqrt{\sigma }\right)}^{2}\right]}{1-{\varGamma }_{e}\left(1-{\sigma }_{1}\right)}\)
|
(21)
|
\(\frac{1}{{\rho }_{eff}}=\frac{{x}^{2}}{{\rho }_{G}\alpha }+\frac{{\left(1-x\right)}^{2}}{{\rho }_{L}\left(1-\alpha \right)}+{\rho }_{L}\left(1-\alpha \right)\left(\frac{{\alpha }_{E}}{1-{\alpha }_{E}}\right)\times {\left[\frac{x}{{\rho }_{G}\alpha }-\frac{1-x}{{\rho }_{L}\left(1-\alpha \right)}\right]}^{2}\)
|
(22)
|
\({\alpha }_{E}=\frac{1}{S}\left[1-\frac{1-x}{1-x\left(1-0.05{We}_{G01}^{0.27}{Re}_{SL1}^{0.05}\right)}\right]\)
|
(23)
|
\(S=\frac{x}{1-x}\frac{\left(1-\alpha \right)}{\alpha }\frac{{\rho }_{L}}{{\rho }_{G}}\)
|
(24)
|
\({We}_{GO1}={G}_{1}^{2}{x}^{2}\frac{{D}_{1}}{{\rho }_{G}{\sigma }^{*}}\frac{\left({\rho }_{L}-{\rho }_{G}\right)}{{\rho }_{G}}\)
|
(25)
|
\({Re}_{SL1}=\frac{{G}_{1}\left(1-x\right){D}_{1}}{{\mu }_{L}}\)
|
(26)
|
\({\varGamma }_{e}=1-{\sigma }^{0.25}\)
|
(27)
|
\({f}_{e}=4.9\times {10}^{-3}{x}^{2}{\left(1-x\right)}^{2}{\left(\frac{{\mu }_{L}}{{\mu }_{G}}\right)}^{0.7}\)
|
(28)
|
\(\alpha =1-\frac{2{\left(1-x\right)}^{2}}{1-2x+\sqrt{1+4x\left(1-x\right)\left(\frac{{\rho }_{L}}{{\rho }_{G}}-1\right)}}\)
|
(29)
|
Attou and Bolle (1997)
|
\(PR=\sigma \left(1-\sigma \right){\theta }_{\sigma }^{r}{G}^{2}\varPhi +\frac{\left(1-{\theta }_{\sigma }^{r}\right)\sigma \left(1-\sigma \right){G}^{2}}{{\rho }_{l}}\)
|
(30)
|
\(\varPhi =\frac{{ẋ}^{2}}{\alpha {\rho }_{g}}+\frac{{\left(1-x\right)}^{2}}{\left(1-\alpha \right){\rho }_{l}}\)
|
(31)
|
\({\theta }_{\sigma }=\frac{3}{1+{\sigma }^{0.5}+\sigma }\)
|
(32)
|
Abdelall et al. (2005)
|
\(PR={\left({P}_{2}-{P}_{1}\right)}_{R}+{\left({P}_{2}-{P}_{1}\right)}_{I}\)
|
(33)
|
\({PR}_{R}=\frac{{G}_{1}^{2}}{2{\rho }^{{\prime }{\prime }2}}\left(1-\sigma \right)\)
|
(34)
|
\({PR}_{I}=\frac{{G}_{1}^{2}}{2{\rho }_{L}}\left[\frac{2{\rho }_{L}\sigma \left(\sigma -1\right)}{{\rho }^{{\prime }}}-\frac{{\rho }_{H}{\rho }_{L}\left(1-{\sigma }^{2}\right)}{{\rho }^{{\prime }{\prime }2}}\right]\)
|
(35)
|
\({\rho }^{{\prime }}=\frac{1}{\left[\frac{\left(1-{x}^{2}\right)}{{\rho }_{L}\left(1-\alpha \right)}+\frac{{x}^{2}}{{\rho }_{G}\alpha }\right]}\)
|
(36)
|
\({\rho }^{{\prime }{\prime }}=\frac{1}{\sqrt{\frac{{\left(1-x\right)}^{3}}{{\rho }_{L}^{2}{\left(1-\alpha \right)}^{2}}+\frac{{x}^{3}}{{\rho }_{G}^{2}{\alpha }^{2}}}}\)
|
(37)
|
Ahmed et al. (2003)
|
\(PR=\frac{1}{2}Z{\rho }_{H}{V}_{M1}^{2}\)
|
(38)
|
\(Z={\left(2.795\times {10}^{-5}+\frac{4\times {10}^{-7}}{{x}^{2}}\right)}^{1/2}\)
|
(39)
|
\({\rho }_{TP}=x{\rho }_{G}+\left(1-x\right){\rho }_{L}\)
|
(40)
|
\({V}_{M1}={V}_{SL1}+{V}_{SG1}\)
|
(41)
|
Wang et al. (2010)
|
\(PR=\left(1-{\varOmega }_{1}+{\varOmega }_{2}\right)\left(1+{\varOmega }_{3}\right)\sigma \left(1-\sigma \right){G}^{2}\left[\frac{x}{{\rho }_{G}}+\frac{\left(1-x\right)}{{\rho }_{L}}\right]\)
|
(42)
|
\({\varOmega }_{1}={\left(\frac{WeBo}{{Re}_{LO}}\right)}^{2}{\left(\frac{1-x}{x}\right)}^{0.3}\frac{1}{{Fr}^{0.8}}\)
|
(43)
|
\({\varOmega }_{2}=0.2{\left(\frac{{\mu }_{G}}{{\mu }_{L}}\right)}^{0.4}\)
|
(44)
|
\({\varOmega }_{3}=0.4{\left(\frac{x}{1-x}\right)}^{0.3}+0.3{e}^{\frac{1.6}{{Re}_{LO}^{0.1}}}-0.4{\left(\frac{{\rho }_{G}}{{\rho }_{L}}\right)}^{-0.2}\)
|
(45)
|
\(Bo=\frac{\left({\rho }_{L}-{\rho }_{G}\right)}{{\sigma }^{*}}\)
|
(46)
|
\(We=\frac{{G}_{1}^{2}{D}_{1}}{{\sigma }^{*}{\rho }_{H}}\)
|
(47)
|
\(Fr=\frac{{G}_{1}^{2}}{{\rho }_{H}^{2}g{D}_{1}}\)
|
(48)
|
\({Re}_{LO1}=\frac{{G}_{1}{D}_{1}}{{\mu }_{L}}\)
|
(49)
|
Kourakos (2009)
|
\(PR=\frac{1}{2}{\rho }_{L}\left({V}_{M1}^{2}-{V}_{M2}^{2}\right)-\frac{1}{2}{\rho }_{L}{Re}_{SL1}^{2}\left(-0.772\sigma -6.2{10}^{-7}{Re}_{SL1}+0.0825\beta +0.706\right)\)
|
(50)
|
\(\beta =\frac{{V}_{SG1}}{{V}_{SL1}+{V}_{SG1}}\)
|
(51)
|
\({Re}_{SL1}=\frac{{G}_{1}\left(1-x\right){D}_{1}}{{\mu }_{L}}\)
|
(52)
|
2.3 Analysis of existing models
After presenting the existing pressure recovery models, it seems important to deeply analyze them. A primary analysis of the models, described above, highlights their great variety, either in the approach used for their developement or in the choice of input parameters (summarized in Table 2). As it appears in the Table, all the models require the use of flux mass (G1) and mass quality (x), except the model of Lottes (1961) which is independent of x. The model of Ahmed et al. (2003) is the only one that does not recourse to the aspect ratio.
The mechanistic models are the most rigorous, as they consider the real phenomena occurring in each flow regime (Hewitt, 1983). However, the problem in predicting the flow regimes downstream the singularity, when the flow pattern maps are not valid (Kondo et al., 2002; Arabi et al., 2018; Zhang and Goharzadeh, 2019), adds further complexity to pressure recovery modeling using the phenomenological approach. In addition, these models are also known by their complexity due to their dependance of several parameters. This last statement is also valid for the models of Schmidt and Friedel (1996) and Attou and Bolle (1997).
Table 2
Independent parameters of the existing two-phase PR models
Model
|
Parameters
|
Upstream mass flux (G1)
|
Mass quality (x)
|
Volume flow rate ratio (β)
|
Aspect ratio (σ)
|
Upstream pipe diameter (D1)
|
Liquid density (ρL)
|
Gas density (ρG)
|
Liquid dynamic viscosity (µL)
|
Gas dynamic viscosity (µG)
|
Surface tension (σ*)
|
Upstream void fraction (α1)
|
Downstream void fraction (α2)
|
Homogeneous model applied to the momentum balance
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Homogeneous model applied to the mechanical energy balance
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Romie (1958)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
+
|
Delhaye (1981)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
-
|
Lottes (1961)
|
+
|
-
|
-
|
+
|
-
|
+
|
-
|
-
|
-
|
-
|
+
|
-
|
Chisholm and Sutherland (1969)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Ahmed et al. (2007)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
+
|
Collier and Thome (1994)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
-
|
Richardson (1958)
|
+
|
+
|
-
|
+
|
-
|
+
|
-
|
-
|
-
|
-
|
+
|
-
|
Wadle (1989)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Owen et al. (1993)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Chen et al. (2007)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Schmidt and Friedel (1996)
|
+
|
+
|
-
|
+
|
+
|
+
|
+
|
+
|
+
|
+
|
+
|
-
|
Attou and Bolle (1997)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
-
|
Abdelall et al. (2005)
|
+
|
+
|
-
|
+
|
-
|
+
|
+
|
-
|
-
|
-
|
+
|
-
|
Ahmed et al. (2003)
|
+
|
+
|
-
|
-
|
-
|
+
|
+
|
-
|
-
|
-
|
-
|
-
|
Wang et al. (2010)
|
+
|
+
|
-
|
+
|
+
|
+
|
+
|
+
|
+
|
+
|
-
|
-
|
Kourakos (2011)
|
+
|
+
|
+
|
+
|
+
|
+
|
+
|
+
|
-
|
-
|
-
|
-
|
Based on their own results, Ahmed et al. (2007) found that the PR is affected by the pressure difference between the upstream flow and the downstream face of the expansion, as well as the wall shear stress in the recovery region. However, these two parameters are difficult to estimate, which make this model unsuitable in practice. Furthermore, similar to the models of Romie (1958) and Collier and Thome (1994), this model depends on the value of the void fraction in the downstream pipe, which is also difficult to predict. Indeed, the gas decelerates more rapidly than liquid after crossing the expansion. Therefore, the slip factor and the void fraction increase close to recovery region (Ahmed, 2005). After the flow recovery, the downstream void fraction’s value may decrease or increase compared to the upstream value (Ahmed, 2005; Liang et al., 2022). The relationship between the void fractions on either side of the sudden expansion remains not well correlated. Besides, there is no consensus on the parameter controlling the change of the void fraction, as reported by Ahmed (2005) and Arabi (2019).
The estimation of the upstream void fraction is also complicated. The literature is full of models to predict the void fraction in straight pipes. The prediction level of each model depends on the fluids' physical properties, pipe geometry, and flow regime (Marquez-Torres et al., 2020). Therefore, the models developed for the straight pipes are not necessarily valid in pipes fitted with a singularity (Zitouni et al., 2021). Schmidt and Friedel (1996) suggested to use Huq and Loth's correlation (1992) (Eq. 29) to estimate the void fraction in their pressure recovery model, which is based on their experimental results. Doubts remain on the confidence level of this model for conditions different from those of Schmidt and Friedel's experiments.
To demonstrate the consistency of the model based on the momentum balance on the mechanical energy conservation, the evolution of the pressure recovery, in the case of the single-phase, was plotted as a function of the diameter ratio σ0.5 in Fig. 2. The dimensionless normalized singular pressure recovery (Ks), given by Eq. 53, was used instead of the pressure recovery. As shown, for σ = 0, when the downstream cross-section is too large, and for σ = 1, when the cross-section does not change, Ks = 0, which agrees with the physics of the phenomenon. The representation of single-phase flow experimental results collected from various studies (Delhaye, 1981; Suleman, 1990; Aloui and Souhar, 1994; Ahmed, 2005) shows that the momentum equation predicts the majority of the experimental data with a confidence level of ± 20%.
$${K}_{s}=\frac{PR}{\frac{{G}_{1}^{2}}{2\rho }}$$
53
Regarding the homogeneous models, the fact that they neglect the slippage between the two phases leads to an overestimation of the PR predictions, as noted by Abdelall et al. (2005) and Wang et al. (2010). However, the homogeneous model has the advantage of being practical and easy to apply. This aspect led Wang et al. (2010) to propose a correction of this model by incorporating an empirical coefficient. Generally, the empirical models' predictions are valid only within the range of experimental conditions close to those of data used for their development. This observation is also valid with the purely empirical models of Ahmed et al. (2003) and Kourakos (2011). It is important to note that these three models of Ahmed et al. (2003), Wang et al. (2010) and Kourakos (2011) were not validated with independent data. In addition, the model of Wang et al. (2010) has also the disadvantage of being applicable only for cases where (1 - Ω1 + Ω2) (1 + Ω3) > 0.
The modeling approach of Wadle (1989) is interesting since it is based on the Bernoulli principle. The weakness of this approach lies in difficulty to estimate the coefficient K. Indeed, according to Wadle (1989), it depends on the nature of the fluids. Chen et al. (2007) correlated it with the aspect ratio. The use of this model remains limited, since it is not valid in the case when σ ≥ 0.451.
The model of Chisholm and Sutherland (1969), based on the separated flow model, recourses to the two-phase multiplier and the liquid pressure recovery. The separated flow approach remains relatively reliable especially considering its popularity for pressure drop modeling. The latter is notably used for the estimation of frictional pressure drop in the straight pipes (Muzychka and Awad, 2010; Sassi et al., 2020, Arabi et al., 2021a), as well as for the estimation of the pressure drop generated by the presence of different kinds of singularity, such as the bend (Azzi et al., 2000; Azzi and Friedel, 2005; Hayashi et al., 2020), the orifice (Zeghloul et al., 2017), the multi-hole orifice (Zeghloul et al., 2018), the gate and ball valves (Zeghloul et al., 2020), the pump valve (Ma et al., 2020), the Venturi (Messilem et al., 2020) or the static mixer (Hosni et al., 2023). The liquid pressure recovery of the model of Chisholm and Sutherland (1969) is calculated using the Borda-Carnot formula based on the momentum equation. Attou and Bolle (1997) reported that the model of Chisholm and Sutherland (1969) tends to underestimate the results with a mean relative error of -11% for steam-water mixture. The opposite was observed for air-water mixture. Wadle (1989) noted that the model of Chisholm and Sutherland (1969) overestimates their experimental results obtained using steam-water and air-water mixtures, with a mean relative error of 2.1% and 46.4%, respectively.