Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision
Study objectives were to evaluate the equations governing the ice- accretion process to identify proposed scaling parameters and to conduct tests to determine which, is any, of the proposed methods produced scale ice accretions. Study results include: (1) A set of equations that can be used to calcu...
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ftdtic:ADA167976 2023-05-15T16:37:22+02:00 Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision Ruff, Gary A ARNOLD ENGINEERING DEVELOPMENT CENTER ARNOLD AFB TN 1986-03 text/html http://www.dtic.mil/docs/citations/ADA167976 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA167976 en eng http://www.dtic.mil/docs/citations/ADA167976 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost *ICE FORMATION *SCALING FACTOR AERODYNAMICS COMPUTER PROGRAMS DROPS DYNAMIC PRESSURE EQUATIONS FLOW FIELDS ICE IMPINGEMENT LIMITATIONS MACH NUMBER MATHEMATICAL MODELS METEOROLOGY MODEL TESTS MODEL THEORY MODELS PARAMETERS REYNOLDS NUMBER SHAPE THERMAL PROPERTIES THERMODYNAMICS VELOCITY SIMICE COMPUTER PROGRAM METEOROLOGICAL PARAMETERS ICE SHEDDING LPN-AEDC-D188EW PE65807F Text 1986 ftdtic 2016-02-24T19:27:40Z Study objectives were to evaluate the equations governing the ice- accretion process to identify proposed scaling parameters and to conduct tests to determine which, is any, of the proposed methods produced scale ice accretions. Study results include: (1) A set of equations that can be used to calculate test conditions so that scaled ice shapes are produced on geometrically similar bodies was developed and experimentally verified. (2) Posttest evaluation of the scaling parameters based on the actual test conditions was necessary for accurate evaluation of test results. (3) An icing similitude computer code, SIMICE, was developed to calculate similitude conditions using the verified scaling equations. (4) The equations were applicable over the range of meteorological conditions found in natural icing, with the possible exception of velocity. (5) Velocity is the primary limitation of the scaling equations. To maintain scaled flow fields and droplet impingement characteristics, both the model and full-scale velocities must yield a Reynolds number or = 200,000 and the velocity giving the critical Mach number of the body geometry. (6) At values of dynamic pressure of approximately 1.6 psia, shedding characteristics of the ice accretion were observed to affect the final ice shape. Keywords: Aerodynamics: Thermodynamics; Ice formation; Scaling factors; and Thermal models. Revision to report dated Nov 1985, ADA162226. See also Volume 2, ADB097466. Prepared in cooperation with Sverdrup Technology, Inc., Arnold AFS, TN. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Snow Ice and Permafrost *ICE FORMATION *SCALING FACTOR AERODYNAMICS COMPUTER PROGRAMS DROPS DYNAMIC PRESSURE EQUATIONS FLOW FIELDS ICE IMPINGEMENT LIMITATIONS MACH NUMBER MATHEMATICAL MODELS METEOROLOGY MODEL TESTS MODEL THEORY MODELS PARAMETERS REYNOLDS NUMBER SHAPE THERMAL PROPERTIES THERMODYNAMICS VELOCITY SIMICE COMPUTER PROGRAM METEOROLOGICAL PARAMETERS ICE SHEDDING LPN-AEDC-D188EW PE65807F |
spellingShingle |
Snow Ice and Permafrost *ICE FORMATION *SCALING FACTOR AERODYNAMICS COMPUTER PROGRAMS DROPS DYNAMIC PRESSURE EQUATIONS FLOW FIELDS ICE IMPINGEMENT LIMITATIONS MACH NUMBER MATHEMATICAL MODELS METEOROLOGY MODEL TESTS MODEL THEORY MODELS PARAMETERS REYNOLDS NUMBER SHAPE THERMAL PROPERTIES THERMODYNAMICS VELOCITY SIMICE COMPUTER PROGRAM METEOROLOGICAL PARAMETERS ICE SHEDDING LPN-AEDC-D188EW PE65807F Ruff, Gary A Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
topic_facet |
Snow Ice and Permafrost *ICE FORMATION *SCALING FACTOR AERODYNAMICS COMPUTER PROGRAMS DROPS DYNAMIC PRESSURE EQUATIONS FLOW FIELDS ICE IMPINGEMENT LIMITATIONS MACH NUMBER MATHEMATICAL MODELS METEOROLOGY MODEL TESTS MODEL THEORY MODELS PARAMETERS REYNOLDS NUMBER SHAPE THERMAL PROPERTIES THERMODYNAMICS VELOCITY SIMICE COMPUTER PROGRAM METEOROLOGICAL PARAMETERS ICE SHEDDING LPN-AEDC-D188EW PE65807F |
description |
Study objectives were to evaluate the equations governing the ice- accretion process to identify proposed scaling parameters and to conduct tests to determine which, is any, of the proposed methods produced scale ice accretions. Study results include: (1) A set of equations that can be used to calculate test conditions so that scaled ice shapes are produced on geometrically similar bodies was developed and experimentally verified. (2) Posttest evaluation of the scaling parameters based on the actual test conditions was necessary for accurate evaluation of test results. (3) An icing similitude computer code, SIMICE, was developed to calculate similitude conditions using the verified scaling equations. (4) The equations were applicable over the range of meteorological conditions found in natural icing, with the possible exception of velocity. (5) Velocity is the primary limitation of the scaling equations. To maintain scaled flow fields and droplet impingement characteristics, both the model and full-scale velocities must yield a Reynolds number or = 200,000 and the velocity giving the critical Mach number of the body geometry. (6) At values of dynamic pressure of approximately 1.6 psia, shedding characteristics of the ice accretion were observed to affect the final ice shape. Keywords: Aerodynamics: Thermodynamics; Ice formation; Scaling factors; and Thermal models. Revision to report dated Nov 1985, ADA162226. See also Volume 2, ADB097466. Prepared in cooperation with Sverdrup Technology, Inc., Arnold AFS, TN. |
author2 |
ARNOLD ENGINEERING DEVELOPMENT CENTER ARNOLD AFB TN |
format |
Text |
author |
Ruff, Gary A |
author_facet |
Ruff, Gary A |
author_sort |
Ruff, Gary A |
title |
Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
title_short |
Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
title_full |
Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
title_fullStr |
Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
title_full_unstemmed |
Analysis and Verification of the Icing Scaling Equations. Volume 1. Revision |
title_sort |
analysis and verification of the icing scaling equations. volume 1. revision |
publishDate |
1986 |
url |
http://www.dtic.mil/docs/citations/ADA167976 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA167976 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA167976 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766027669337538560 |