Effect of Pipe Inclination on the Pipe Flow Head Losses For

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    International Journal of Civil Engineering and Technology (IJCIET), ISSN 0976 6308

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    EFFECT OF PIPE INCLINATION ON THE PIPE FLOW HEAD

    LOSSES FOR DIFFERENT SAND CONCENTRATIONS

    Mahmoud Ali Refaey EltoukhyFaculty of Engineering, Shobra, Banha University, Egypt

    ABSTRACT

    This paper presents results of an experimental study pertaining to the behavior of

    sand-water (two-phase) flows in inclined pipes, a phenomenon that is generally witnessed atthe canal intakes which aligned at desert area, and dredging processes. The experiments were

    conducted in a modern hydraulics laboratory to study the effect of sand concentration and

    pipe inclination on the pipe flow head losses. The pipe inclination angle was varied from 0

    to 90 in upward and downward directions and the sand concentration in water was regulated

    up to 15% by volume. It was concluded that the head losses of the downward sloping pipe

    flow are always lower than the head losses of the horizontal flow and these are always lower

    than the head losses of the upward sloping pipe flow, regardless of the concentration and

    inclination angle. The experiment results were analyzed in the light of earlier published data

    and useful empirical correlations have been developed to determine the head losses of

    horizontal flow, alongwith upward and downward sloping pipe flows.

    Keywords: head loss, sand - water mixture, inclined pipes, sand concentration

    INTRODUCTION

    Most of the applications of hydraulic transport in the past have been in the minerals

    industries. Generally, such industrial facilities are located in remote areas with insufficient

    road or rail infrastructure. Therefore, pipeline transport has been preferred and recognized as

    the most cost effective method of transporting huge quantities of minerals over long

    distances, across difficult terrain. The solid particles invariably being heavier than the

    conveying liquid are transported in lower part of the channel. This unique pattern has been a

    subject of special study and is presented in this paper. The effect of flow velocity, sand

    concentration and the sloping pipe inclination angle on the head loss were investigated. The

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    head losses determined for the horizontal portion of the pipeline were compared with

    correlations found in the literature. A pipe loop system was built, allowing variation of flow

    velocity, sand concentration and pipe inclination.

    OVERVIEW OF THE PRIOR PUBLISHED DATA

    Wasp et al., (1999) found that the flow of solid-liquid slurries in pipes differs from the

    flow of homogeneous liquids in a variety of ways. The complete range of velocities is

    possible with liquids, whereas nature of the flow, i.e., laminar, transition, or turbulent, can be

    characterized based on the knowledge of physical properties of the fluid and the pipe system.

    The characterization of slurry flow is not as simple as for liquid flow mainly for two reasons:

    firstly the properties of the solid particles to be accounted for are superimposed on the

    properties of the liquid, and also the effect of the particles on the mixture properties;

    secondly, depending on the particular conditions, a range of slurry behavior is possible.

    Kaushal et al (2005), and Kaushal and Tomita (2007) carried out experimental study for

    concentration of distributions in slurry pipeline by using - ray densitometer. Theirmeasurements show that, pressure gradient profiles of equivalent fluid for finer particles were

    found to resemble with water data except for 50% concentration, however, more skewed

    pressure gradient profiles of equivalent fluid were found for coarser particles. Experimental

    results indicate absence of near-wall lift for finer particles due to submergence of particles in

    the lowest layer into the viscous sub layer and presence of considerable near-wall lift for

    coarser particles due to impact of viscous-turbulent interface on the bottom most layer of

    particles and increased particleparticle interactions.

    Richardson, et al., (1999) found that, in homogenous flow systems, the presence of

    the solids can have a significant effect on the system properties, usually resulting in a sharp

    increase in viscosity as compared to that of the carrier fluid. In heterogeneous flow systems,

    solids are not evenly distributed and in horizontal flow, pronounced concentration gradient

    exists along the vertical axis of the pipe, even at high velocities. Particle inertial effects aresignificant, i.e., the fluid and solid phases to a large extent retain their separate identities, and

    the increase in the system viscosity over that of the carrier liquid is usually quite small.

    Heterogeneous slurries tend to be of lower solid concentrations and have larger particle sizes

    than homogeneous slurries. Raudkivi, (1989), found that in vertical pipes the velocity of

    solids for upward flow is less than the fluid velocity, but is greater for downward flow. The

    difference is approximately the value of the settling velocity.

    Coiado and Diniz, (2001), studied the solid-water flow in inclined pipes. Based on the

    collected experimental data, the adopted methods and the experimental conditions, it was

    concluded that the head losses values for the downward sloping pipes are always lower than

    the head losses for the horizontal pipe, and these are always lower than the head losses for the

    upward sloping pipes, regardless of the inclination angles and concentrations. Whereas, in

    case of downward sloping length of water-sand slurry flow, the presence of sand decreases

    the head losses values corresponding to the inclination angle and increasing concentration.

    C. Kim et al, (2008), made an experimental study on the transport of sand-water

    mixtures in circular and square pipelines, focusing on the economic transport of solid

    particles. The measured data of the hydraulic gradient, solid effect, and deposition-limit

    velocity for both circular pipe and square duct were compared and analyzed. The hydraulic

    gradient of water in the circular pipe was found larger than that in the square duct because of

    the secondary flow in the square duct. The hydraulic gradient of sand-water mixture in the

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    International Journal of Civil Engineering and Technology (IJCIET), ISSN 0976 6308

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    47

    square duct was larger than that in the circular pipe. It was found that the hydraulic gradient

    of the slurry flow in the circular and square pipelines increases with the volumetric delivered

    concentration and Reynolds number.

    D.R. Kaushal, et al, (2012), simulated Pipeline slurry flow of mono- dispersed fineparticles at high concentration numerically using Mixture and Eulerian two-phase models. It

    was found that, pressure drop predictions by both MIxture and Eulerian two-phase models for

    flow of water show good agreement with the experimental data. Whereas, in case of

    comparison between measured and predicted pressure drops at different concentrations,

    namely, 30%, 40% and 50%, the Mixture model fails to predict pressure drops correctly, the

    amount of error increasing rapidly with the concentration. However, Eulerian model gives

    fairly accurate predictions for pressure drop at all the efflux concentrations and for flow

    velocities considered in the present study.

    The published materials about two-phase (solid-liquid) flow are mostly related to

    horizontal pipe flow. There are a limited number of studies concerning the effect of pipe

    inclination on two-phase flow energy loss. In htis backdrop, this paper studies the effect of

    the pipe inclination on the pipe flow head losses for different sand concentrations, andpresents its results in the forms of curves and equations to compute the head loss, given the

    sand water mixture flow velocity, the pipe angle of inclination, and the sand concentration in

    volume.

    EXPERIMENTAL APPARATUS

    The general layout of the apparatus is shown in Fig. 1. This apparatus is used to reach

    the objectives proposed in this paper. It consists of a pipe loop system, and was fabricated in

    the professional Hydraulics Laboratory. The sand water mixtures were prepared in the main

    tank, which had dimensions of 0.80 m length, 0.70 m width, and 0.80 m depth. The mixture

    was maintained homogeneous in the main tank by the use of an auxiliary pump. Then, the

    homogeneous mixture was pumped, through a pipeline with diameter of 0.75 m. The pipelinewas made up of horizontal and inclined pipes. The head loss measurements for the sand-

    water mixture flow were carried out in the pipelines. The sand used in the experiment was

    uniform with median grain size d50 = 0.20 mm, and relative density of 2.67, with

    concentrations 15 % up in volume. The pipe inclination angle used was varied from 0o

    (horizontal position) to 90o

    (vertical position), for each upward and downward inclinations.

    During the sand water mixture flow through the pipeline, for different velocities and

    concentrations of the mixture, the following parameters were measured: a) the head losses in

    the horizontal, upward, and downward inclinations; b) the discharge; and c) the concentration

    of the sand in water. The discharge was measured by dividing a volume of the outlet mixture

    by the corresponding time. The concentration of the mixture was determined using a tank to

    measure the volume and one balance. Whereas, the head losses in the horizontal, upward, and

    downward sloping lengths were measured by differential manometer.

    EXPERIMENTAL WORK

    The experimental work consists of two main sets of experiments. The first set consists

    of 126 runs, and it used to measure the head losses through the upward inclination pipeline at

    different mixture velocities and for different sand concentrations. The angles of the pipeline

    inclination were 5o, 10

    o, 25

    o, 35

    o, 45

    oand

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    Rubber pipe

    Tank auxiliary pump main pump

    Fig. 1. The Apparatus Layout

    90o. The sand concentrations used for each angle of inclination are 5 %, 10 %, and 15 % in

    volume. The second set of experiments consists of 118 runs, and the pipeline inclination

    angles were as that of the first set except that, the pipeline inclination was downward. Fifty

    runs were carried out to measure the head losses through the horizontal pipeline at three

    different sand concentrations. The horizontal pipeline runs results, are analyzed with the

    upward and downward pipeline inclination's results. In the light of above conclusions, the

    sand water mixture velocity should be greater than the deposition limit (critical) velocity,

    which is the mean mixture velocity at the limit of stationary deposition. From Durand (1953)

    and Gibert (1960) for the used sand, the mixture velocity should be greater than 1.88 m/s in

    all runs to maintain that the sand particles are always in suspension state.

    RESULTS AND DISCUSSION

    Two empirical equations were developed to calculate the head losses of the water-

    sand mixture as a function of flow Froud's number, Fn, the sand concentration, C, and the

    inclination angle, , of upward and downward flows in inclined pipes. The equations were

    developed by several curve fittings. First of all, the apparatus was calibrated through

    comparison of the measured head losses in a horizontal pipeline with that measured by E. M.

    Coiado, (2001), Fig. (2), which shows that the measured and Coiado results are almost

    identical.

    FLOW THROUGH UPWARD INCLINATION PIPELINE

    For the first set of experiments, the sand water mixture was pumped through the

    pipeline which was laid in upward inclination positions. The used pipeline inclination angles

    are 0o

    (horizontal position), 5o, 10

    o, 25

    o, 35

    o, 45

    o, and 90

    o(upward vertical position). The

    head losses were measured in the pipeline in each inclination position for three sand

    concentrations, i.e., 5%, 10%, and 15%.

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    The results of the flows through upward inclination Pipeline were analyzed. The

    effect of each sand-water mixture velocity represented in Froude's number, F n, the pipeline

    angle of inclination, , and the sand

    Fig. 2. Apparatus Calibration, for C = 10%, and pipe inclination angle 10o

    upward

    concentration, C on the head losses in the pipeline was developed. It was found that the

    hydraulic gradient increases with increasing sand water mixture velocity. For example, for C

    = 10% and = 35o, if the sand water mixture velocity increases from 3.3 m/s to 5.2 m/s, the

    hydraulic gradient increases from 0.27 to 0.37, meaning thereby that increase of 57.5% in the

    mixture velocity results in increasing 37% in the hydraulic gradient, as indicated in Fig. (3).

    Another runs of experiments were carried out through varying the sand

    concentrations up to 15%, to study the effect of sand concentration on the head losses in

    upward pipeline inclination. It was found that increase in the sand concentration results in

    increasing hydraulic gradient. For example, for pipeline inclination angle of 25o

    and sand

    water mixture velocity of 3.75 m/s, changing sand concentration from 10% to 15%, the

    hydraulic gradient changes from 0.21 to 0.265, thereby showing that 50% increase in sandconcentration yields 26% increase in the hydraulic gradient in the pipeline, as shown in Fig.

    (4).

    The effect of pipeline inclination angle was studied by changing from 0o

    (horizontal

    pipeline) to 90o

    (vertical pipeline). Experiments showed that the hydraulic gradient of the

    pipeline increases as its upward angle of inclination increases, Fig. (5). For example, at sand

    concentration C = 10 %, when the upward inclination angle increases from =10o

    to 45o, the

    hydraulic gradient increases from 0.199 to 0.296, implying that increase of 35% in upward

    inclination angle of pipeline results into 49% increase in the hydraulic gradient.

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    0.3

    0.35

    2 3 4 5 6 7

    Froude's Number, Fn

    Hydrau

    licGradient,(i)

    Present

    Coiado, 2001

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    Fig. 3 Variation of the hydraulic gradient with the sand water mixture velocity for C=

    10% and = 35o

    Fig. 4 Effect of sand concentration on the hydraulic gradient, for = 25o

    and v = 3.75

    m/s (Upward)

    0

    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    2 2.5 3 3.5 4 4.5 5 5.5 6

    Froude's Number, Fn

    Hydraulicgradient(i)

    = 0

    Up 5

    Up 10

    Up 25

    Up 35

    Up 45

    Up 90

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    0.3

    0.35

    0.4

    2 2.5 3 3.5 4 4.5 5 5.5 6 6.5

    Froude's Number, Fn

    HydraulicGradient,(i)

    C = 5 %

    C = 10 %

    C = 15 %

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    Sin

    Fig. 5 Effect of the upward pipe inclination angle on the hydraulic gradient, i for C=

    10%

    With a view to accomplish the objectives set for this study, several curve fittings were

    done and sound relationship was established between hydraulic gradient and the affecting

    parameters, i.,e., the Froude's number, the pipeline inclination, and the sand concentration,

    Fig. (6). With parameters factor UPI on the horizontal axis and the hydraulic gradient on the

    vertical axis:

    0779.025.0sin1091.00574.0 += CgD

    vIUP (1)

    Where:

    v : sand water mixture flow velocity, (m/s)

    : pipeline angle of inclinationC: sand concentration in water (% in volume).

    The hydraulic gradient, i , may be calculated for anyUP

    I for a given sand water mixture

    velocity, the pipeline inclination angle, and the sand concentration from Fig. (6). Through

    curve fitting for data in Fig. (6), the following equation was obtained:

    012.00669.1 =UP

    Ii (2)

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    0.3

    0.35

    0.4

    0 0.2 0.4 0.6 0.8 1 1.2

    HydraulicGradient,(i),

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    UPI

    Fig. 6 Upward pipe flow hydraulic gradient variation with the affecting parameters

    By substituting the value of UPI from Equation 1 into Equation 2, the hydraulic gradient canbe directly calculated as under:

    0951.02667.0sin1164.00612.0 += CgD

    vi (3)

    FLOW THROUGH DOWNWARD INCLINATION PIPELINE

    In the second set of experiments, the sand water mixture was pumped through

    the pipeline which was laid in downward inclination positions. The study parameter

    encompassed pipeline inclination angles 0o

    (horizontal position), 5o, 10

    o, 25

    o, 35

    o, 45

    o, and

    90o (downward vertical position). Whereas, all measurements of head losses in the pipelinewere carried out in each inclination position for the three sand concentrations, 5%, 10%, and

    15%.

    The results were analyzed to determine the effect of each of sand water mixture

    velocity represented in Froude's number, Fn, the pipeline angle of inclination, , and the sand

    concentration, C on the head losses in the pipeline. The sand water mixture velocity effect on

    the head loss is shown in Fig. (7). It was found that the hydraulic gradient increases as the

    sand water mixture velocity increases. For example, for C = 10% and = 35o, if the sand

    water mixture velocity increases from 3.28 m/s to 5.2 m/s the hydraulic gradient increases

    0

    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    0 0.1 0.2 0.3 0.4 0.5 0.6

    HydraulicGradient,(i),

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    Fig. 7 Variation of the hydraulic gradient with sand water mixture velocity for C= 10%

    and = 35o

    from 0.024 to 0.175, showing that increase of 58.5% in the mixture velocity results in

    increase of 629% in the hydraulic gradient.

    Another set of experiments was undertaken to study the effect of sand

    concentration on head losses in downward pipeline inclination by varying sand

    concentrations up to 15%. The results showed that the sand concentration is inverselyproportional with the hydraulic gradient. For example, for pipeline inclination angle of 25

    o

    and sand water mixture velocity of 3.75 m/s, changing sand concentration from 10% to 15%,

    results in changing the hydraulic gradient from 0.0778 to 0.063, showing that 50% increase in

    the sand concentration results in 19% decrease in the hydraulic gradient in the pipeline, Fig.

    (8).

    Also, the effect of the pipeline inclination angle on the pipeline hydraulic gradient

    was studied by changing from 0o

    (horizontal pipeline) to 90o

    (vertical pipeline).

    Experiments showed that the hydraulic gradient of the pipeline decreases as its downward

    angle of inclination increases, Fig. (9). For example, at sand concentration C = 10 %, when

    the downward inclination angle increases from =10o

    to 45o, the hydraulic gradient

    decreases from 0.129 to 0.048, showing that with downward inclination angle of the pipelineincreasing by 35%, the hydraulic gradient decreases by 63%.

    The curve fittings were done for this set of parameters as well to determine

    relationship between the hydraulic gradient and the affecting parameters, i.e, the Froude's

    number, the pipeline inclination, and the sand concentration, which yielded promising results

    as shown in Fig. (10) and the underlying relationship, taking Parameters factor DwnI on the

    horizontal axis and the hydraulic gradient on the vertical axis:

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    0.3

    0.35

    2 3 4 5 6 7

    Froude's Number, Fn

    HydraulicGradient,(i),

    = 0

    Dow 5

    Dow 10

    Dow 25

    Dow 35

    Dow 45

    Dow 90

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    Fig. 8 Effect of sand concentration on the hydraulic gradient, for = 25o

    and v = 3.75

    m/s (Downward)

    Sin

    Fig. 9 Effect of the Downward pipe inclination angle on the hydraulic gradient, i for C=

    10%

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    2 3 4 5 6 7

    Froude's Number, Fn

    HydraulicGradient,(i),

    C = 5 %

    C = 10 %

    C = 15 %

    0

    0.02

    0.04

    0.06

    0.08

    0.1

    0.12

    0.14

    0.16

    0.18

    0 0.2 0.4 0.6 0.8 1 1.2

    HydraulicGradient,(i),

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    DwnI

    Fig. 10 Downward pipe flow hydraulic gradient variation with the affecting parameters

    1346.015.0sin0675.00585.0 += CgD

    vIDwn (4)

    The hydraulic gradient, i may be calculated for anyDwn

    I for a given sand water

    mixture velocity, the downward pipeline inclination angle, and the sand concentration. The

    relationship established by curve fitting for data in Fig. (10), is given as under:

    0031.09848.0 += DwnIi (5)

    The following relationship is obtained by combining Equations (4) and (5), to calculate the

    hydraulic gradient given the values of sand water mixture velocity, the pipeline inclination,and the sand concentration:

    1295.0148.0sin0665.00576.0 += CgD

    vi (6)

    0

    0.05

    0.1

    0.15

    0.2

    0.25

    0.3

    0.35

    0 0.05 0.1 0.15 0.2 0.25 0.3 0.35

    HydraulicGradient,(i),

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    CONCLUSIONS

    This paper gives the results of an experimental study undertaken to determine the

    effects of sand water mixture velocity, the pipeline inclination angle upward and downward,and the sand concentration on the head loss in the pipeline. Based on the experimental data,

    the results of curve fitting, and the resulting mathematical expressions, the following

    conclusions are reached:

    1. The head losses for the downward inclination of the pipeline are always lower thanthe head losses for the horizontal pipe, and these are always lower than the head

    losses for the upward sloping pipes, regardless of the inclination angles and

    concentrations.

    2. For the downward inclination of the pipeline, the presence of sand decreases the headlosses with increasing inclination angle and the sand concentration.

    3. For the water-sand mixture flow in the horizontal pipe, the presence of sand increasesthe head losses as the concentration increases.

    4. For the upward inclination of the pipeline water-sand mixture flow, the presence ofsand increases the values of the head losses with increase in inclination angle and theconcentration.

    5. The curve fitting results and the corresponding equations developed can be used forcalculating the head loss in the pipeline for given sand water mixture velocity, the

    pipeline inclination angle, and the sand concentration.

    REFERENCES

    1. E. M. Coiado and M. G. Diniz, (2001), "Two-Phase (Solid-Liquid) Flow in InclinedPipes", J. Braz. Soc. Mech. Sci. vol.23 no.3 Rio de Janeiro.

    2. D.R. Kaushal, T. Thinglas, Y. Tomita, S. Kuchii, and H. Tsukamoto, (2012), " CFDmodeling for pipeline flow of fine particles at high concentration", International Journalof Multiphase Flow 43, 85100

    3. Durand, R. (1953), " Basic solids in pipes Experimental Research", ProceedingsInternational Hydraulics Conference, Minneaplis, MN, pp. 89 103.

    4. Gibert, R. (1960), "Transport Hydraulique et Refoulement des Mixtures en Conduit",Anna1es des Pontes et Chaussees, 130e Annee, No. 12, et No. 17.

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    6. Kaushal, D.R., Tomita, Y., 2007, "Experimental investigation of near-wall lift ofcoarser particles in slurry pipeline using -ray densitometer" Powder Tech nol. 172,

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    7. Raudkivi, A. J., 1989 "Loose Boundary Hydraulics", Pergamon Press, New York8. Richardson, J. F., Chhabra, R. P., Khan, A. R., 1999 "Multiphase flow ou non-

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    Hidrotransport 14. Maastrich. Netherlands.

    9. Wasp, E. J.; Kenny, J. P.; Gandhi, R. L. 1999. "Solid-Liquid Flow Slurry PipelineTransportation", Series on Bulk Materials Handling. International Standard Book

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