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THE RHEOLOGY OF THE BLOOD. III

The authors have confirmed the fact that blood serum and plasma behave rheologically like a true viscous liquid. It is true for whole blood only to a first approximation, but with this reservation they have studied the available data and extended the equation of Bingham and Durham to cover protein s...

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Detalles Bibliográficos
Autores principales: Bingham, Eugene C., Roepke, Raymond R.
Formato: Texto
Lenguaje:English
Publicado: The Rockefeller University Press 1944
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2142594/
https://www.ncbi.nlm.nih.gov/pubmed/19873406
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author Bingham, Eugene C.
Roepke, Raymond R.
author_facet Bingham, Eugene C.
Roepke, Raymond R.
author_sort Bingham, Eugene C.
collection PubMed
description The authors have confirmed the fact that blood serum and plasma behave rheologically like a true viscous liquid. It is true for whole blood only to a first approximation, but with this reservation they have studied the available data and extended the equation of Bingham and Durham to cover protein solutions of various concentrations and at various temperatures as well as mixtures of proteins and corpuscles present in whole blood. If Φ is the fluidity of whole blood, Φ(1) is the fluidity of water and ΔΦ = Φ – Φ(1), then ΔΦ = β(1) b (1) + β(2) b (2) + β(3) b (3) + ··· where β(1), β(2), β(3), etc., are constants for the fluidity lowering of the salts, albumin, globulin, fibrinogen, and the corpuscles, etc., present in the whole blood. The conclusions from the data referred to are intended to buttress this simple equation (6).
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spelling pubmed-21425942008-04-23 THE RHEOLOGY OF THE BLOOD. III Bingham, Eugene C. Roepke, Raymond R. J Gen Physiol Article The authors have confirmed the fact that blood serum and plasma behave rheologically like a true viscous liquid. It is true for whole blood only to a first approximation, but with this reservation they have studied the available data and extended the equation of Bingham and Durham to cover protein solutions of various concentrations and at various temperatures as well as mixtures of proteins and corpuscles present in whole blood. If Φ is the fluidity of whole blood, Φ(1) is the fluidity of water and ΔΦ = Φ – Φ(1), then ΔΦ = β(1) b (1) + β(2) b (2) + β(3) b (3) + ··· where β(1), β(2), β(3), etc., are constants for the fluidity lowering of the salts, albumin, globulin, fibrinogen, and the corpuscles, etc., present in the whole blood. The conclusions from the data referred to are intended to buttress this simple equation (6). The Rockefeller University Press 1944-09-20 /pmc/articles/PMC2142594/ /pubmed/19873406 Text en Copyright © Copyright, 1944, by The Rockefeller Institute for Medical Research This article is distributed under the terms of an Attribution–Noncommercial–Share Alike–No Mirror Sites license for the first six months after the publication date (see http://www.rupress.org/terms). After six months it is available under a Creative Commons License (Attribution–Noncommercial–Share Alike 4.0 Unported license, as described at http://creativecommons.org/licenses/by-nc-sa/4.0/).
spellingShingle Article
Bingham, Eugene C.
Roepke, Raymond R.
THE RHEOLOGY OF THE BLOOD. III
title THE RHEOLOGY OF THE BLOOD. III
title_full THE RHEOLOGY OF THE BLOOD. III
title_fullStr THE RHEOLOGY OF THE BLOOD. III
title_full_unstemmed THE RHEOLOGY OF THE BLOOD. III
title_short THE RHEOLOGY OF THE BLOOD. III
title_sort rheology of the blood. iii
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2142594/
https://www.ncbi.nlm.nih.gov/pubmed/19873406
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