PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR

An observation tools of Rayleigh-Benard Convection (RBC) has been developed. Observation set up made from glass box limited by two plates, i.e, bottom and top plates. The bottom plate is hotter than the top plate which has function to heat horizontal layers of fluid from below. The used media to obs...

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Bibliografische gegevens
Hoofdauteurs: , Marni Mansur, S.Pd., , Yusril Yusuf, S.Si., M.Eng., D.Eng.
Formaat: Thesis
Gepubliceerd in: [Yogyakarta] : Universitas Gadjah Mada 2011
Onderwerpen:
ETD
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author , Marni Mansur, S.Pd.
, Yusril Yusuf, S.Si., M.Eng., D.Eng.
author_facet , Marni Mansur, S.Pd.
, Yusril Yusuf, S.Si., M.Eng., D.Eng.
author_sort , Marni Mansur, S.Pd.
collection UGM
description An observation tools of Rayleigh-Benard Convection (RBC) has been developed. Observation set up made from glass box limited by two plates, i.e, bottom and top plates. The bottom plate is hotter than the top plate which has function to heat horizontal layers of fluid from below. The used media to observe fluid dynamics is water which mixed by sawdust of teakwood as representation of water particle motion. Raising of water layer tickness is distance between two plates (d) causes raising of the velocity of the water particle motion at the convection ilustrated by the bifurcation diagram. Raising of d also causes the convection radius change. Observed also pattern of flow from laminer to turbulen as result of d which ever greater.
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institution Universiti Gadjah Mada
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publisher [Yogyakarta] : Universitas Gadjah Mada
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spelling oai:generic.eprints.org:901532014-08-20T02:52:39Z https://repository.ugm.ac.id/90153/ PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR , Marni Mansur, S.Pd. , Yusril Yusuf, S.Si., M.Eng., D.Eng. ETD An observation tools of Rayleigh-Benard Convection (RBC) has been developed. Observation set up made from glass box limited by two plates, i.e, bottom and top plates. The bottom plate is hotter than the top plate which has function to heat horizontal layers of fluid from below. The used media to observe fluid dynamics is water which mixed by sawdust of teakwood as representation of water particle motion. Raising of water layer tickness is distance between two plates (d) causes raising of the velocity of the water particle motion at the convection ilustrated by the bifurcation diagram. Raising of d also causes the convection radius change. Observed also pattern of flow from laminer to turbulen as result of d which ever greater. [Yogyakarta] : Universitas Gadjah Mada 2011 Thesis NonPeerReviewed , Marni Mansur, S.Pd. and , Yusril Yusuf, S.Si., M.Eng., D.Eng. (2011) PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=52621
spellingShingle ETD
, Marni Mansur, S.Pd.
, Yusril Yusuf, S.Si., M.Eng., D.Eng.
PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title_full PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title_fullStr PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title_full_unstemmed PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title_short PENGAMATAN GERAK KONVEKSI RAYLEIGH-BENARD SEBAGAI FUNGSI KETEBALAN LAPISAN AIR
title_sort pengamatan gerak konveksi rayleigh benard sebagai fungsi ketebalan lapisan air
topic ETD
work_keys_str_mv AT marnimansurspd pengamatangerakkonveksirayleighbenardsebagaifungsiketebalanlapisanair
AT yusrilyusufssimengdeng pengamatangerakkonveksirayleighbenardsebagaifungsiketebalanlapisanair