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OUTLINE. IntroductionDevelopment of the ModelNumerical TreatmentPhenomena modelingImplementation into RELAP/SCDAPSIM/MOD3.2ConclusionsDevelopment of a model to predict the transport of released fission products through the RCS, and to calculate the quantities each FP product deposited in the RCS and released to the containment.
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1. FPTRAN: A Volatile Fission Product and Structural Material Transport Code for RELAP/SCDAPSIM EDUARDO HONAISER (Brazilian Navy Technological Center)
SAMIM ANGHAIE (University of Florida)
2. OUTLINE Introduction
Development of the Model
Numerical Treatment
Phenomena modeling
Implementation into RELAP/SCDAPSIM/MOD3.2
Conclusions
Development of a model to predict the transport of released fission products through the RCS, and to calculate the quantities each FP product deposited in the RCS and released to the containment
3. Fission Product Behavior
4. Fission Product Transport (Scope) Vapor phenomena
Adsorption
Condensation
Onto structures
Onto aerosol surfaces
Aerosol nucleation
Aerosol Phenomena
Deposition
Agglomeration
Re-suspension
5. Characteristics of the Model Fixed speciation
Phenomenological and convection model limited to piping system (upper plenum not considered)
Decay heat of deposited FP not considered
Mechanistic model for aerosol nucleation
6. Analytical Equations Vapor species Aerosol Species
7. Transition Analytical-Numerical
8. Numerical Equations Bulk states (vapor+aerosol sections) Surface states (condensed, absorbed, and deposited)
Total number of equations of the system: Sx(B+1+3N)
9. Vapor-Structural Surface Laminar flow (Re<2300)
Leifshitz model (1962)
Turbulent flow
10. Vapor-Aerosol Processes
Homogeneous nucleation
Heterogeneous nucleation
11. Nucleation Pattern Experimental evidence
PBF-SFD and Phebus-FP
experiments
Procedure
Calculate selectively
nucleation rate for Ag and U
Select a model for
homogeneous nucleation
Obtain the particle critical size, defining lower particle size as spectrum limit
12. Homogeneous Nucleation Models Analytical Models
Classical theory (Becker-Doring (1935)
Kinetic theory (Girshick et al (1990)
13. Heterogeneous Nucleation Approach
Diffusion
Continuum region (Kn<<1)
Near Continuum region (Fuchs and Stuggin correction)
14. Aerosol Processes Assumptions Aerosol spherical shape
Empirical evidence
PBF-SFD and Phebus experiments
Synergy
Mathematical
15. Aerosol-Surface Gravitational
Using the concept of mobility
Upper limit of the spectrum: 50 ?m
Laminar diffusion
Gormley and Kennedy (1954)
16. Early Models (theoretical)
Friedlander (1957), Davies (1966) and Beal (1968)
Semi-empirical model (Sehmel-1970)
Empirical Models
Liu (1974), Iam and Chung (1983), Chiang (1996)
Aerosol-Surface (Turbulent)
17. Aerosol-Surface (Thermophoresis) Principle (Continuum)
Brock Solution (1962)
18. Other Models
19. Aerosol-Aerosol (Agglomeration) Brownian agglomeration
Approach (continuum)
Target particle flux from other particles
Equation
Boundary conditions
Continuum/near continuum region
20. Aerosol-Aerosol (Agglomeration) Differential gravitational
Simplified model
Realistic model
Consider the fluid trajectories
Approximations
Fuchs (1964)
Pruppacher and Klett (1978)
21. Turbulent agglomeration
Processes
Diffusivity (small particles)
Inertial (large particles)
Approaches
Leifshitz (1962)
Solution of diffusion equation
Saffman and Turner (1956)
Statistic approach for turbulence
Aerosol-Aerosol (Agglomeration)
22. Implementation Implementation in RELAP/SCDAPSIM/MOD 3.2
23. Verification Robustness of the math solver, positive masses
Global mass error (OK)
Sensitive studies
Synergy
24. Stability
25. Conclusions A FP transport model was developed, using a system of mass balance equations of first order
Aerosol size was treated by a discrete ordinate approach, the convective term was treated using the fractional step method
ODE system was solved using Hindmarsh package
Phenomenological models:
Condensation onto structural surfaces
Condensation onto aerosol surfaces
Aerosol homogeneous nucleation
Aerosol deposition
Gravitational settling, laminar diffusion, turbulent diffusion, thermophoresis
Aerosol Agglomeration
Diffusive, turbulent, and due to gravitational difference
Additional models
Aerosol Re-suspension, deposition onto singularities, vapor adsorption
26. Conclusions
27. Acknowledgments Dr. Chris Allison and Dick Wagner for their support and the use of RELAP/SCDAPSIM for this project