Dirk Van MaerckeIMAGINE Final Conference, Budapest, 25.10.2006 1 Development of the HARMONOISE Point-To-Point MODEL Prediction of Excess Attenuation in.

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Dirk Van MaerckeIMAGINE Final Conference, Budapest, Development of the HARMONOISE Point-To-Point MODEL Prediction of Excess Attenuation in Outdoor Noise Propagation Dirk van Maercke CSTB 24, rue Joseph Fourier F Saint-Martin d’Hères FRANCE

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The Point-To-Point module Calculation of excess attenuation:  over any kind of terrain profile, including multiple diffractions & reflections by natural and man-made obstacles  under different representative meteorological conditions  using physical models, based on “recent” progress in outdoor propagation  more accurate than existing (national, ISO based) models  limited computation time  “just good enough”  continuous results, no excessive sensitivity to accuracy of input data  compatible or comparable with basic principles of existing models  ready to be integrated in existing noise mapping software

Dirk Van MaerckeIMAGINE Final Conference, Budapest, INPUT TO THE P2P MODEL  cross-section profile  P i (x i,y i ), i = 0,1,…N where x i+1 > x i  each segment (P i, P i+1 ) = impedance value / class  source and receiver height  h S ±  h S and h R ±  h R  any number of diffractions (thin screens, wedges, thick barriers,…)  no distinction between ground (terrain), road surfaces, embankments, barriers, buildings, roofs,…

Dirk Van MaerckeIMAGINE Final Conference, Budapest, INPUT TO THE P2P MODEL (continued)  Impedance values - User defined - Delany-Bazley (flow resistivity and layer thickness) - Impedance classes (Nord 2000) + predefined impedance values  Frequency range - Default: 1/3 octave bands, 25 – 10000Hz - User defined  Atmospheric conditions - Sound speed (default = 340 m/s) - Temperature and humidity (ISO ) - Sound speed gradient - Turbulence strength

Dirk Van MaerckeIMAGINE Final Conference, Budapest, Point-To-Point Model development  Step-by-step, increasing complexity:  Ground effect  Diffraction  Ground + diffraction  Combined model : ground + multiple diffraction  Meteorological effects  Long time averaging  Approach:  Analytical model (base solution, simple situation)  Heuristics (extension & adaptation to more realistic situations)  Validation against numerical “reference” calculations  Validation against experimental results

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The P2P model : GROUND REFLECTION Chien-Soroka Mixed ground & Fresnel weighting Deep valley solution Roughness, almost flat ground

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The P2P model : WEGDE DIFFRACTION  Hadden & Pierce + heuristics  Approximation (from NMPB):

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The P2P model : simplified diffraction formula

Dirk Van MaerckeIMAGINE Final Conference, Budapest, DIFFRACTION : INSERTION LOSS special case :  >>  Deygout’s approximation

Dirk Van MaerckeIMAGINE Final Conference, Budapest, DIFFRACTION + GROUND

Dirk Van MaerckeIMAGINE Final Conference, Budapest, MULTIPLE DIFFRACTION  two screens, no ground  extension to multiple screens : recursively ! most diffracting edge secondary diffracting edge

Dirk Van MaerckeIMAGINE Final Conference, Budapest, MULTIPLE DIFFRACTION + GROUND binary tree structure !

Dirk Van MaerckeIMAGINE Final Conference, Budapest, MULTIPLE DIFFRACTION & WIDE BARRIERS

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The P2P model : MULTIPLE DIFFRACTION + GROUND transition diffraction no diffraction recursive call

Dirk Van MaerckeIMAGINE Final Conference, Budapest, COMBINED MODEL : COMPUTANIONAL EFFORT ?  the computation time varies as linearly as O(M+N)  instead of O(M N ) !

Dirk Van MaerckeIMAGINE Final Conference, Budapest, METEOROLOGICAL REFRACTION  Linear sound speed gradient  analytical construction of rays  Curved rays… curved ground analogy ? Conformal mapping !

Dirk Van MaerckeIMAGINE Final Conference, Budapest, The Point-To-Point model = DIFFRACTION + GROUND + METEOROLOGICAL REFRACTION After conformal transformation… use “straight ray” model over modified terrain model !

Dirk Van MaerckeIMAGINE Final Conference, Budapest, Fine-tuning the model & secondary effects…  Loss of coherency  Turbulence and scattering (simplified, one parameter)

Dirk Van MaerckeIMAGINE Final Conference, Budapest, VALIDATION AGAINST BEM CALCULATIONS (no meteo) h S = 0.30 m ; h R = 5.00 m ; d = m thin barrier / wedge, h = 2.00 m, d = 10.0 m thin barrier wedge

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (BEM) h S = 0.30 m ; d S = 10.0 m h R = 5.00 m ; d R = 50.0 m h B = 3.00 m; d B = 2.00 m  B = 50 or 2000 kNsm -4 hard soft

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (BEM)  embankments, earth walls, round hill tops, ….  receiver grids : d = 50 / 100 / 250 / 500 m, h = 1.25 / 2.5 / 5.0 / 10 m cylindrical hill top embankment

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (BEM)

Dirk Van MaerckeIMAGINE Final Conference, Budapest, VALIDATION AGAINST GFPE CALCULATIONS (with meteo) h S = 0.30 m ; d = m h R = 2.50 / 10.0 m ;  = 200 kNsm -4 A lin = 0.04 s -1 (R ~ 18 D) h R = 2.5 m h R = 10 m weak linear gradient

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (GFPE) h S = 0.30 m d = m  = 2000 kNsm -4 A lin = 0.04 s -1 (R ~ 18 D) Low source / low receiver ? h R = 5 m h R = 1.25 m h R = 2.5 m

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (GFPE) h S = 0.30 m h R = 2.50m  = 200 kNsm -4 A lin = 0.12 s -1 (R ~ 6 D) Stronger gradients ? d = 500 m d = 100 m d = 250 m

Dirk Van MaerckeIMAGINE Final Conference, Budapest, NUMERICAL VALIDATION (GFPE)

Dirk Van MaerckeIMAGINE Final Conference, Budapest, VALIDATION AGAINT EXPERIMENTAL RESULTS Measurements:2 to 10 weeks, records of sound levels and meteorological parameters (W,  W, 1/L) in 30’ steps Reference models : lin/log sound speed profiles for each point source and for each time period Engineering model : 8 wind directions, 3 wind speeds, 5 stability classes = 120 cases + frequency of occurrence

Dirk Van MaerckeIMAGINE Final Conference, Budapest, VALIDATION AGAINT EXPERIMENTAL RESULTS IMAGINE.WP7 EDF / DEBAKOM

Dirk Van MaerckeIMAGINE Final Conference, Budapest, BUT : A MODEL IS JUST A MODEL…