Feasibility study of the cascading mass ow rate evaluation as a new variant of Gibson's method

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Feasibility study of the cascading mass ow rate evaluation as a new variant of Gibson's method R. Eckerstorfer Andritz Hydro GmbH, Linz, Austria roland.eckerstorfer@andritz.com L. Götsch Andritz Hydro GmbH, Linz, Austria leopold.goetsch@andritz.com J. Lanzersdorfer Andritz AG, Graz, Austria johannes.lanzersdorfer@andritz.com July 29, 2014 Abstract We present a feasibility study of Gibson's method for low and medium head plants using not a single and complete closure of the wicket gates but a stepwise closing procedure. One has to wait until ow stabilizes after each step to initiate another step of abrupt closing operation. Therefore, n steps before complete closure gives n measuring points instead of a single measuring point in applying the common procedure. That decreases the overall time consumption of the test session and reduces the rejected loads impacting the stability of the electrical grid and the mechanical components. In this paper, we show the theoretical basis and the corresponding uncertainty estimation for this variant of Gibson's method. Instationary simulations and results will be presented at the conference. 1

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 2 1 Introduction The application of the Pressure-time method aka Gibson's method on units in hydropower plants is of great interest. It is rather used on turbines than on pumps (e.g., [1]). The minor eorts related to time consumption of installation makes it an attractive alternative compared to other primary ow measurement methods especially on low and medium head units. The successful outcome of a testrun is closely related to the deceleration rate of the water inside the closed piping. The steeper the temporal decrease of ow v/ t the steepness of this value is comparable to that one during an emergency shutdown the better the signal-noise-ratio (SNR) of the pressure signal(s) and the higher the reliability. The so-induced water hammer gives understandably rise to limitations with respect to allowable mechanical stresses. However, operating companies often refuse the application of the Pressure-time method because of the negative impact of the fast loadrejection onto the grid stability. The quality of power grid networks with low capacity suer hard under such circumstances and are able to collapse if the rejected load cannot be compensated. In these cases one has to choose another measuring method, which is most likely more costly, since alternative variants of the Pressure-time method are neither indicated nor recommended by the leading test codes [2, 3, 4]. We discuss the signicance of a new variant of Gibson's method in this publication. This variant diers from the original procedure in applying several small deceleration steps of the water instead of a single and complete deceleration by complete closure of the ow regulation device (e.g., wicket gates). One can test the unit's behavior at n operating points before minimum opening of the closure device instead of a single operating point if using the common procedure. The grid network should suer therewith only from small amount of abrupt load-changes. It can react within an short time frame to compensate the power needs by changing the loads on other energy generating units. Therefore, we should be able to apply this variant of Pressure-time method even on a unit which is part of a small isolated network. Since we could not yet test the new procedure in practice, we have to rely on simulation data obtained from one-dimensional instationary ow calculations by the software SIMSEN to check the feasibility and the limitations. These results will be presented at the conference. Although this paper primarily deals with ow through turbine units in both modes, i.e., using deceleration and acceleration procedure, the workow for testing pumps is similar but is not treated in here.

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 3 2 Theoretical basis We do not give a detailed mathematical and physical background of the general Pressure-time method since it has already been discussed excellently elsewhere [4, 5]. Consider a turbine operating at high load and under steady head conditions. We start our data recording. The Gibson dierential pressure p G (t) uctuates randomly around the running line pressure p RL. Let us add the index 1 to the last-mentioned symbol, i.e., p RL,1, to indicate that this pressure value belongs to the evaluation procedure of the initial mass ow (ρq) 1. After a fast but partly deceleration of the water in the piping the pressure conditions stabilize again and we end up with a Gibson pressure denoted by the static line pressure p SL. We put the index 1 into this symbol and call it p SL,1. Between the transient stabilization of p RL,1 and p SL,1 the mass ow changed from (ρq) 1 to (ρq) 2, where (ρq) 2 < (ρq) 1. At this stage p G (t) uctuates in stochastic manner around p RL,2. Consequently, we equate this running line pressure with the static line pressure of the previous step p RL,2 = p SL,1 or, generally speaking, p RL,i+1 = p SL,i i {N i < n}. (1) We repeat the procedure of deceleration a total of n times until leakage ow ρq (or zero ow) is reached. See reference [6] for leakage ow determination. After p G (t) stabilizes signicantly at p SL,n we can stop the data recording. The analysis starts now at the very end of the collected data. Mass ow rate (ρq) n is calculated by with (ρq) n = 1 F t n+ t n t n [p G (t) p R (t)] dt + ρq (2) p R (t) p SL,n p RL,n p SL,n = [(ρq)(t)]2 (ρq) 2 (ρq) 2 n (ρq) 2. (3) The parameters t n and t n denote an appropriate choice of the integration starting time and the time length [5], respectively. The behavior of the recovery line pressure p R (t) between the time interval [t n, t n + t n ] needs iterative computation with the previous two equations. Thus, we are able to determine the loss coecient ζ at mean Reynolds number Re n 1 µ t n t n+ t n t n (ρq)(t) dt (4)

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 4 by reordering p RL,n p SL,n (ρq) 2 n (ρq) 2 = 1 2ρ [ α2 A 2 2 ( 1 + ζ(ren ) ) α ] 1 A 2 1. (5) The parameters A 1 and A 2 label the cross-section of the Gibson measurement section 1 (upstream) and 2 (downstream). Since we do not have any information of the available ow prole at both measurement sections, the correction factors α 1 and α 2 are set to unity. Hopping back in time of the recorded data we compute the relevant parameters analogously by (ρq) i = 1 F t i + t i t i [p G (t) p R (t)] dt + (ρq) i+1, (6) p R (t) p SL,i p RL,i p SL,i = [(ρq)(t)]2 (ρq) 2 i+1 (ρq) 2 i (ρq)2 i+1, (7) and Re i 1 µ t i t i + t i t i (ρq)(t) dt (8) ζ(re i ) = ( A2 A 1 ) 2 1 + 2ρA 2 2 p RL,i p SL,i (ρq) 2 i (ρq)2 i+1. (9) We do not require the calculation of the loss coecient dependency on the Reynolds number to determine the contributing mass ow steps. But it reveals the minor value changes with respect to the frictional behavior of uid and pipe wall between both Gibson measurement sections. Hence, this variant elaborates more sensitively on changes in friction than the common procedure does, which uses only one loss coecient for the complete closing procedure. By increasing the number of mass ow steps n one gains an even higher resolution of ζ(re). Anyhow, the integer value of n is limited by the SNR of the pressure measurement devices in use. 3 Uncertainty estimation Detailed uncertainty analyses have already been published for the commonly used procedure [7]. Here, we give a rough estimate of the expectable measurement uncertainty, stated by the expanded uncertainty U[(ρQ) i ] = ku[(ρq) i ]

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 5 [8], in using the cascadian technique. Consider n steps equidistant in massow starting from (ρq) 1 down to zero leakage. That is, (ρq) i = (n + 1 i)/n (ρq) 1 (10) (ρq) n+1 = ρq = 0 kg/s. (11) We assume that the relative standard uncertainty of the measurement conditions 1 u M /(ρq) and of the integration area u(b)/(ρq) remain unchanged for the individual steps. The combined standard uncertainty of the nal cascadian step before zero leakage thus yields u n = u c[(ρq) n ] u2 (B) + u = 2 (F ) + u 2 M (12) (ρq) n (ρq) n including the standard uncertainty of the pipe factor u(f ). We bear in mind that the massow equation for the previous steps consists of the integrational term B i /F and of the subsequent massow (ρq) i+1. Therefore, with the aid of equation (10) we obtain the relative standard uncertainty of massow i recursively by u 2 n + (n i) 2 u 2 i+1 u i = i {N i n}. n + 1 i (13) Expanding u i+1 until u n nally yields u i 1 = (14) u n n + 1 i u c [(ρq) i ] = n + 1 i (15) u c [(ρq) n ] for all i {N i n}, respectively. Equation (15) indicates that the relative standard uncertainty increases with every step-down massow compared to the preceding step; the absolute standard uncertainty decreases vice versa (view eq. 15). The ratio of the corresponding expanded uncertainties coincides with the right-hand side of latter equation consequently. 1 We use this uncertainty proportion to account for any deviation from ideal measurement conditions [2] (e.g., um = (0.25... 1.00%) (ρq)).

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 6 Example We want to apply n = 4 equidistant massow steps from (ρq) 1 to zero ow on the basis of (10). Assuming a relative expanded uncertainty of U[(ρQ) 4 ]/(ρq) 4 = 2.00% (k = 2) for the nal massow before zero ow, we can expect expanded uncertainties for the other massow values according to table 1. Table 1: Expanded uncertainty (k = 2) of massow values using equation (15) i 1 2 3 4 Eq. (15) 4 3 2 1 U[(ρQ) i ] (ρq) i 1.00% 1.15% 1.41% 2.00% Although higher massows really tend to lower relative uncertainty values, the estimation of u(b)/(ρq) requires an individual numerical treatment for each step.

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 7 Nomenclature Symbol Description Unit A Cross-section (m 2 ) B Integration area (Pa s) F Pipe factor (1/m) k Coverage factor (e.g., k = 2 for condence level 95%) (-) ρq Leakage mass owrate (kg/s) ρq Mass owrate (kg/s) n Number of massow steps (-) p G Gibson (dierential) pressure (Pa) p RL Running line pressure (Pa) p SL Static line pressure (Pa) q Leakage volume owrate (m 3 /s) Q Volume owrate (m 3 /s) Re Reynolds number (-) t Time (s) u Standard uncertainty (a.u.) U Expanded uncertainty (= ku c ) (a.u.) u c Combined standard uncertainty (a.u.) u M Standard deviation accounting for the measurement conditions (kg/s) (= (0.25... 1.00%) (ρq)) α Velocity prole coecient ( 1) (-) ζ Loss coecient (-) µ Dynamic viscosity of water (Pa s) ρ Water density (kg/m 3 )

10 th IGHEM Conference, Itajubá/Brazil, September 16-19, 2014 8 References [1] P. ev ík. Verication of Gibson ow measurement. In Proceedings of the International HYDRO Conference, Lyon, France, October 2009. [2] IEC, editor. IEC 60041 Field acceptance tests to determine the hydraulic performance of hydraulic turbines, storage pumps and pump-turbines. IEC, 3 edition, 1991. [3] ASME, editor. ASME PTC 18 Hydraulic turbines and pump-turbines performance test codes. ASME, 2011. [4] IEC, editor. IEC 62006 Hydraulic machines - Acceptance tests of small hydroelectric installations. IEC, 1 edition, 2010. [5] A. Adamkowski and W. Janicki. Selected problems in calculation procedures for the Gibson discharge measurement method. In Proceedings of the 8th International Group for Hydraulic Eciency Measurement (IGHEM) Conference, Roorkee, India, October 21-23, 2010. [6] E. da Costa Bortoni. New developments in Gibson's method for ow measurement in hydro power plants. Flow Measurement and Instrumentation, 19:385390, 2008. [7] H. Hulaas and O.G. Dahlhaug. Uncertainty analysis of Pressure-Time measurements. Technical report, Portland, Oregon, USA, July 30 - August 1, 2006. [8] JCGM, editor. JCGM 100 Evaluation of measurement data Guide to the expression of uncertainty in measurement. JCGM 100:2008. GUM 1995 with minor corrections. BIPM, 1 edition, 2008.