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פותח על ידי קלירמאש פתרונות בע"מ -
Revisiting the boundary layer structure used in Craig and Gordon's model of isotope fractionation in evaporation
Year:
2008
Authors :
טנאי, יוסף
;
.
Volume :
44
Co-Authors:
Tanny, J., Institute of Soil, Water and Environmental Sciences, Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel, H.I.T. Holon Institute of Technology, Holon, Israel
Cohen, J., Faculty of Aerospace Engineering, Technion - Israel Institute of Technology, Haifa, Israel
Facilitators :
From page:
11
To page:
21
(
Total pages:
11
)
Abstract:
Craig and Gordon's (CG) model of isotope fractionation in evaporation was derived more than 40 years ago and was based on the turbulent boundary layer structure model acceptable at that time. That view suggested that turbulent flows consist of eddies with a wide range of length scales moving randomly in the flow domain. There is evidence that some parameters in CG model do not fully correspond to data in the literature. Owing to advances in fluid dynamics research techniques, it has been shown in recent decades that the apparent chaotic flow in turbulent boundary layers is in fact governed by few well-organised structures. This article reviews the major characteristics of these coherent structures based on available results from experimental, numerical and theoretical studies of turbulent and laminar boundary layers. The review points on some differences between past and present views of the boundary layer structure and on their relation and possible influence on power laws in CG model.
Note:
Related Files :
chemistry
Conference paper
conference proceeding
isotope
Models, Biological
turbulent boundary layer
water
עוד תגיות
תוכן קשור
More details
DOI :
10.1080/10256010801887091
Article number:
Affiliations:
Database:
סקופוס
Publication Type:
מאמר מתוך כינוס
;
.
Language:
אנגלית
Editors' remarks:
ID:
20817
Last updated date:
02/03/2022 17:27
Creation date:
16/04/2018 23:39
Scientific Publication
Revisiting the boundary layer structure used in Craig and Gordon's model of isotope fractionation in evaporation
44
Tanny, J., Institute of Soil, Water and Environmental Sciences, Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel, H.I.T. Holon Institute of Technology, Holon, Israel
Cohen, J., Faculty of Aerospace Engineering, Technion - Israel Institute of Technology, Haifa, Israel
Revisiting the boundary layer structure used in Craig and Gordon's model of isotope fractionation in evaporation
Craig and Gordon's (CG) model of isotope fractionation in evaporation was derived more than 40 years ago and was based on the turbulent boundary layer structure model acceptable at that time. That view suggested that turbulent flows consist of eddies with a wide range of length scales moving randomly in the flow domain. There is evidence that some parameters in CG model do not fully correspond to data in the literature. Owing to advances in fluid dynamics research techniques, it has been shown in recent decades that the apparent chaotic flow in turbulent boundary layers is in fact governed by few well-organised structures. This article reviews the major characteristics of these coherent structures based on available results from experimental, numerical and theoretical studies of turbulent and laminar boundary layers. The review points on some differences between past and present views of the boundary layer structure and on their relation and possible influence on power laws in CG model.
Scientific Publication
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