CC BY
19
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
UDC 622.649
RESEARCH ON REGIMES OF LIMONITE ORE HYRDOTRANSPORT FOR THE CONDITIONS OF PERDO SOTO ALBA PLANT
RAUL IZQUIERDO PUPO \ ALBERTO TURRO BREFF 2
1 Institute of Mining and Metallurgy, Moa, Republic of Cuba
2 University of Guantanamo, Guantanamo, Republic of Cuba
The paper examines regular flow patterns of high-concentrated limonite pulp with significant content of finest grains. Engineering procedures have been developed to calculate basic parameters of limonite ore hydrotransport in turbulent and structured regimes. Trustworthiness of scientific statements, conclusions and recommendations is justified by theoretical research, establishment of analytical dependences, results of laboratory and industrial experiments. Practical regularities of behavior have been identified for the coefficient of hydraulic resistance, depending on pulp density in the range 35-45 % in case of pulp flow in structured regime, as well as regularity of pressure losses in case of pulp flow in horizontal and inclined pipelines in turbulent regime.
Key words: hydrotransport, flow regimes, limonite ore, pulp, rheological properties
How to cite this article: Raul Izquierdo Pupo, Alberto Turro Breff. Research on Regimes of Limonite Ore Hydrotransport for the Conditions of Pedro Sato Alba Plant. Zapiski Gornogo instituta. 2017. Vol. 224, p. 240-246. DOI: 10.18454/PMI.2017.2.240
Introduction. Increase in production of nickel and cobalt due to opening of new nickel plants in Punta Gorda and Las Camariocas and further improvement of technological processes and equipment, used by operating enterprises, is one of the key development objectives for nickel-cobalt industry of Cuba. For 50 years the haulage of limonite ore from the quarry to Pedro Soto Alba plant has been performed by hydrotransport. However, the quarry reserves will have been depleted by 2025. Therefore today various projects are being designed to organize transportation from the new deposit Moa-East to the plant. Existing difference of geodesic altitudes (65 m) between the deposit and the point where pulp is loaded into hydroseparators is an important condition, emphasizing the possibility to use gravity transfer, as it does not consume any energy. Pedro Soto Alba plant is the only enterprise in Cuba that applies hydrotransport of limonite ore. In the pulp processing station, limonite ore is watered down to the mass concentration 25-30 %. Under the gravity particles of the size -0,833 mm are fed into the hydroseparator, using concrete and cast iron pipelines 610 mm in diameter and 5129 m in length. The pipeline is divided into 54 sections, in-between which there are wells, where velocity of the pulp decreases. The flow velocity varies in the range 1-1.4 m/s. Results of experiments have shown that settling velocity of the pulp is higher on the exit from processing station than on the entry to hydroseparator.
After hydroseparators, thickened pulp (45-48 % of solid mass) is transported with the help of centrifugal pumps; the pipeline is 460 m long and 508 mm in diameter; average flow velocity varies from 0.3 to 0.57 m/s. Apart from limonite ore, the pulp contains solid serpentine fraction (up to 5 %), which crusts at the bottom of a pipeline, reducing its useful section and causing pressure losses. Hence, when designing a new pulp processing facility, it is necessary to introduce technical measures preventing serpentine fraction from entering hydroseparators.
Preliminary estimations and practical data by other researchers suggest the presence of vis-coplastic properties in the limonite pulp.
Analysis of related publications and operation of hydrotransport facilities has shown that, despite its wide application and abundance of experimental research on hydrotransport, there is still no theory and analytical model that would describe the flow structure of viscoplastic pulp. Enormous diversity of physical and mechanical properties of viscoplastic pulp and conditions of its hydro-transportation limits applicability of proposed calculation formulas, therefore in most cases it is impossible to define transportation parameters with the precision, necessary for practical purposes.
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
Efficiency of hydrotransport is determined by flow velocity, concentration and pressure losses. Proposed methods of calculating these parameters are based on Shvedov-Bingham law of viscoplastic flow, derived using continuum dynamics, and require relevant adjustments, relying on experimental research of specific pulp flow.
Research methods included: analysis of literature sources, experience of operating hydrotransport facilities of limonite pulp in Cuba and scientific integration of research on fine-grain suspension-carrying flows; theoretical and experimental investigations of rheological properties and transportation parameters of limonite pulps; planning of experiments and processing of experimental data using methods of mathematical statistics and regression analysis. A procedure has been developed to calculate parameters of limonite pulp hydrotransport facility in structured and turbulent regimes [5].
Recommendations have been elaborated for the design of a new hydrotransportation line Moa-East in Pedro Soto Alba plant. Fig. 1 shows distribution of flow velocity and stress in the pipeline, and Fig.2 contains a generalized rheological curve of limonite pulp [5, 9].
Results of preliminary estimations of rheological properties of limonite pulp, performed on capillary viscosimeter, demonstrate that rheological curves can be described using Bulkley-Herschel model [5]
T = T0 + kyn
(1)
To describe deformational behavior of concentrated suspensions, showing signs of viscosity anomaly, Yu.K.Safronov proposed the following dependence [6]:
-9 = k
9m
T~Tn
\Xk X0 )
(2)
where t0 - yield stress; Tk - stress, associated with total disintegration of the structure; n - flow index; k - concentration ratio; 9 - fluidity. Taking into account that
1
9
1
we obtain
dr = dx. AP
(3)
Plugging expressions (2) and (3) into Newton equation, we get
Fig. 1. Distribution of flow velocity and stress in the pipeline
x = = -1
dU dr
(4)
T, Pa
1. Under stress t0 < t < Ta the flow occurs in structured regime with practically intact structure.
2. In stress range between Ta and tk the flow occurs in transition regime with continuously disintegrating structure.
3. Under stress t > tk the flow occurs in turbulent regime
100 500 y, s
Fig.2. Generalized rheological curve of limonite pulp
n
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
dU = -
kVn
U =
(Tk -T0)n (n + 1)
R(TR-To)^ -r(T-To)n+:];
(Tk-T)n (n + 1)
[r(tr-To)n+: -r(T-To)n+:].
(5)
(6)
Equation (6) is correct for values r0 < R0, r = r0, t = t0, U = U0. Velocity of the flow core equals:
k9m
U 0 =
(Tk -To)n(n +1)
R(Tr -To)n
Pulp flow rate is expressed as follows:
Q = Qi + Qo,
Qo = n ro2 Uo, dQ1 = 2%rUdr.
(7)
(8) (9)
(10)
Plugging into equation (10) the value of velocity, calculated using formula (6), and integrating, we get the flow rate equation for annular zone Q1 . From this, overall flow rate equals:
Q =
4%lk (AP -to) n
AP^m(Tk -To)n(n +1)
Rr0 + Rl(AP -to)n+' -
ro2 2rol(AP -To) n+'
n + 2 AP(n + 3)
Al 2(AP -T0)n+2 AP 2(n + 4)
+
+
^r02kR(AP -to) n+' nm(Tk - To)n(n +1)
(11)
Obtained equation (11) allows to compute the flow rate of limonite pulp in the pipeline, depending on rheological properties of the pulp and hydraulic parameters of the flow, which can be identified by experiment.
Performed research on geologic properties of limonite pulp indicated that, when deformation gradient exceeds 500 s-1, there is a direct proportion between internal shear and velocity gradient. Experiments on capillary viscosimeter showed that, when velocity gradient is lower than 100 s-1, experimental dependence is graphically represented as a straight line.
Basing on the analysis carried out, it has been proposed to describe limonite pulp flow with a rheological curve, containing three sections [4, 5].
According to suggested model, limonite pulp flow is determined by a set of equations:
t = t0 + ny; тeк, ^ L n = 1;
t = t0 + kyn; Te[xa, xk]; T = nminT; T > Tk , n = 1. Pressure losses of the pulp flow can be expressed by the following dependence:
i = FI Re, Y, — | + F21 F1,—.
(12)
' 'D J
D
(13)
The first function F1 in expression (13) operates with viscosity forces, the second function F2 -with gravitational ones.
Viscosity forces are critical for the flow of viscoplastic suspensions. Thus, processing of experimental results has been performed using Reynolds (Re) and Ilyushin (I) criteria as similarity parame-
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
ters for structured regime (function A/D). For turbulent regime viscosity forces are of secondary importance, and sometimes a dimensionless group n (function F2) is used as similarity parameter [2].
Most researchers (V.V.Traynis, A.B.Smoldyrev, Yu.K.Safonov, V.B.Filatov and others) use simplified Buckingham equation to calculate pressure losses of viscoplastic pulp flow. From this equation after some manipulations Z.Lanzhinov and V.B.Filatov have obtained the following expression, defining coefficient of hydraulic resistance:
64| I + —
^-V^ ■ (14)
Re
where N = 8. To calculate X for limonite pulp flow it is necessary to obtain the value of N by experiment.
Pressure losses of suspension-carrying flow in turbulent regime can be retrieved from the expression:
ir = i0(l + ack) (15)
where a, c, k - densities of water, solid phase and pulp; i0 - specific pressure losses of the water flow.
For pulp transportation in inclined pipelines hydraulic slope can be defined from the formula:
iH = ir (ir - i0)cosak2, (16)
where a - slope angle of the pipeline.
Values of coefficients K1 and K2 in the course of limonite pulp flow should also be estimated experimentally.
Grain size analysis of limonite ore has shown that it contains predominantly fine grains (-0.045 mm, 86.87 %), average density of the solid matter is 3400 kg/m3.
Rheological parameters of the pulp have been measured by rotary viscosimeter RV [4-6, 9]. The method of experimental data processing is presented in the form of dependence between average velocity gradient in the gap y and shear stress t. Experimental rheological curves, shown in Fig.3, can be described by Shvedov-Bingham equation:
t = T0 + n^rY, (17)
where t0 - initial shear stress.
Examination of dependences t = Fy demonstrates that limonite pulps with concentration S > 30 % form spatial structures [7].
Results of processing experimental data:
Concentrations 0.30 0.35 0.40 0.45
Regression equation t = 0.131y t = 0.58 + 0.152y t = 2 + 0.170y t = 5.57 + 0.194y
Investigations of hydrotransport parameters of limonite pulp have been carried out for concentrations 25, 30, 35, 40, 45 % of solid mass. After the processing of data, i(U) dependences have been retrieved for pulp flow along the pipelines 100 and 150 mm in diameter (Fig.4).
It can be seen from graphs in Fig.4 that, from the position of concentration and flow velocity, hydrotransport of limonite pulp can occur in three regimes: structured, transitional and turbulent. Thus, experimental data confirm results of earlier tests on viscosimeters and a proposed physico-mathematical model.
Executed experimental tests allowed to estimate values of coefficients k1, k2 and N: k1 = 3.31; k2 = 4.53; N = 2.3.
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
a, Pa 16
14 12 10 8 6 4 2
0
Y, s
Fig.3. Rheological curves of limonite pulp for mass concentrations 30 % (1); 35 (2); 40 (3); 45 (4)
i, Pa/m 1200 1000 800 600 400 200
0
0.5
1.5
2.5 U m/s
Basing on performed theoretical and experimental research, a procedure to calculate hydrotransport parameters of limo-nite pulp has been developed. The idea behind engineering calculation of transportation parameters, taking into account input properties of the fine-grain limonite pulp (production capacity, transportation distance, density), is in estimating operational characteristics of the pipeline and pumps, which guarantee transportation of required volumes of solid material with minimal economic costs and stable performance of the technological system [3].
Calculation procedure is the following. First, the transportation regime of li-monite pulp is determined, which is defined by technological specifics of Pedro Soto Alba plant and depends on concentration of the solid ore, the content of which is determined by processing technology and varies from 25 to 48 % in mass [5].
Depending on solid ore concentration, pulp transportation from the processing station to the plant occurs either in structured, or in turbulent regime.
In structured regime, specific pressure losses are defined as follows:
Fig.4. i(U) dependence for limonite pulp flow along the pipeline 100 mm in diameter with mass concentrations: 1 - water; 2 - 25 %; 3 - 30; 4 - 35; 5 - 40; 6 - 45
i =
^U 2Pst 2D
(19)
AP, MPa
1.1
0.9 0.7
0.5
0.3
1.2
1.3
1.4
1.5
1.6
1 3
6 78
1.7 U, m/s
Fig.5. Pressure losses in the pipeline depending on velocity, diameter (D = 0.438; 0.415; 0.366; 0.317; 0.266 m) and pulp concentration (25 % - curves 1-5; 30 % - 6-9)
where X - coefficient of hydraulic resistance; U - velocity of pulp flow; pst -pulp density; D - pipeline diameter.
Coefficient of hydraulic resistance X is calculated using formula (14), depending on Re and I criteria
Re =
UDp s
nst
I = -T0 D
(20)
Rheological parameters t0 and nst, obtained with rotary viscosimeter, are estimated using the graph in Fig.5.
In turbulent regime, hydraulic resistance is computed by formulas (15) and (16), taking into account coefficients k\ and k2, obtained by experiment.
1
2
3
4
1
2
éRaul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes ofLimonite Ore Hydrotransport..
Obtained values of specific pressure losses are used to calculate required pump head and to choose its type, providing established parameters. Flow rate of the pulp is calculated and compared to the estimated value [1, 8].
To perform calculations for designed hydrotransportation line Moa-East, a computer program has been developed, aimed at estimating pressure losses AP for different pipeline diameters and concentrations. Results of calculations are presented in Fig.6. Graphs in Fig.6 allow to estimate capacity of solid ore production facility depending on the velocity, pipeline diameter and solid mass concentration.
As an alternative option, a combination of gravity and pressurized hydrotransportation is proposed, where the pulp is fed to the final height of the route (58 m) using elevation difference [4, 5]. Hence, the feed station has to be 32 m (2 m as a reserve) higher than the end of the pipeline, i.e. at the level of 90 m. In the initial section of the route, 300 m in length and elevation difference of 33 m, cascading system has to be installed [1]. Slope angle of the chutes should not exceed 1.5 %.
Conclusions
Currently there is no universally accepted, sufficiently justified and experimentally confirmed procedure to calculate hydraulic resistances, associated with viscoplastic pulp flows.
Suggested procedure of calculation, based on Shvedov-Bingham rheological equation, requires relevant adjustments, relying on experimental research.
The main approach to estimating hydraulic resistance is to replace the actual rheological dependency by an empirical formula, close to the experimental flow curve of a specific pulp.
Basing on performed investigations of rheological properties of limonite pulp, a working hypothesis has been proposed, according to which, from the position of concentration and velocity, three zones can be distinguished in the current, characterized by the following flow regimes: structured, transition and turbulent. Basing on this hypothesis, a physical model of limonite fine-grain pulp flow has been developed and its mathematical description prepared.
Performed investigations allowed:
• to establish a dependence in order to estimate coefficient of hydraulic resistance for pulp flow in structured regime;
• to obtain formulas to compute pressure losses for viscoplastic pulp flow in turbulent regime in horizontal pipeline;
• to define the greatest slope angle of pipelines, applicable for limonite pulp transportation, which equals 25 degrees.
Practical recommendations consist in developed procedure to calculate parameters of limonite pulp hydrotransportation facility in turbulent and structured regimes, which allow to obtain better justified and more precise results.
AP, MPa
800
1 1
1 ■T
700 23
"■fT 4 5 6
600
-
500 • — - - 7 8
__
w* -
400 ■r* a- 10
I 1
300 200
1 1.1 1.2 1.3 1.4 1.5 1.6 U, m/s
Fig.6. Capacity of solid ore production depending on velocity, diameter and pulp concentration: (25 % - curves 1-5; 30 % - 6-10)
Raul Izquierdo Pupo, Alberto Turro Breff
Research on Regimes of Limonite Ore Hydrotransport...
REFERENCES
1. Dmitriev G.P., Maharadze L.I., Gogitashvili T.Sh. Pressurized Hydrotransport Systems. Moscow: Nedra, 1991, p. 304 (in Russian).
2. Dzhunusov I. Research on Processes of Mixing and Hydrotransportation of Structured Pulps of Mine Refuses: Avtoref. dis...kand. tehn. nauk. SPGGU. St. Petersburg, 2001, p. 20 (in Russian).
3. Dokukin V.P. Improvement of Operational Performance of Pipeline Transport Systems. SPGGI (TU). St. Petersburg. 2005, p. 84 (in Russian).
4. Manujel' Vega Al'mager. Justification of Technological Scheme and Parameters of the Transportation Complex for High Concentration Pulp in Laterite Quarries (Republic of Cuba): Avtoref. dis.kand. tehn. nauk. SPGGI(TU). St. Petersburg, 2006, p. 220 (in Russian).
5. Raul' Isk'erdo Pupo. Investigation of Parameters and Development of Optimal Regimes of Laterite Hydrotransportation for the Conditions of Pedro Soto Alba Plant: Avtoref. dis.kand. tehn. nauk. Leningradskij gornyj institut im. G.V.Plehanova. Leningrad, 1989, p. 18 (in Russian).
6. Smoldyrev A.E., Safonov Ju.K. Pipeline Transport of Concentrated Pulps. Moscow: Mashinostroenie, 1989, p. 255 (in Russian).
7. Frisman M.L. Rheology of Alkali-Sulphate Mixtures. Moscow: Nauka, 1980, p. 182 (in Russian).
8. Jaltanec I.M., Egorov V.K. Hydromechanization. Moscow: Izd-vo MGU, 1999, p. 335 (in Russian).
9. Izquiedo P.R. Comportamiento Geologico de la Pulpa Lateritica a Bajos Gradients de Velocidad. Revista. Mineriay Geologia. 1989. N 2, p.5-20.
Authors: Raul Izquierdo Pupo, Doctor, Professor, [email protected] (Institute of Mining and Metallurgy, Moa, Republic of Cuba), Alberto Turro Breff, Doctor, Professor, Rector, [email protected] (University of Guantanamo, Guantanamo, Republic of Cuba).
The paper was accepted for publication on 29 November, 2016.
