The laminar flow of streams of suspended particles

Starkey, T V

doi:10.1088/0508-3443/7/2/302

Cited by 46 publications

(15 citation statements)

References 5 publications

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“…It seems unlikely on more general rheological grounds discussed by Starkey (37,65,66). Our in vivo measurements support Taylor's extra vivum studies (37,64).…”

Section: Axial Stream Of Erythrocytes In Glass Tubes and Blood Vesselssupporting

confidence: 81%

The Robin Fåhræus Memorial Lecture1

Copley¹

1989

BIR

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“…It seems unlikely on more general rheological grounds discussed by Starkey (37,65,66). Our in vivo measurements support Taylor's extra vivum studies (37,64).…”

Section: Axial Stream Of Erythrocytes In Glass Tubes and Blood Vesselssupporting

confidence: 81%

The Robin Fåhræus Memorial Lecture1

Copley¹

1989

BIR

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“…Since there is resistance at the boundaries, however, a non-uniform vertical velocity gradient is developed in which situation, according to both theory and experiment (e.g. Starkey, 1956;Segre & Silberberg, 1962) forces, in addition to those associated with gravity, could result which act on a particle in a direction transverse to the flow. Whilst no rigorous quantitative definition of the phenomenon is known to the writers, Shaw (1965, p. 141) considered that certainly these forces would be negligible under the viscosities and flow velocities of granitic magmas, although in much lower viscosity magmas, under certain conditions, they should become important.…”

Section: P E Brown and D G Farmermentioning

confidence: 99%

Size-graded layering in the Imilik gabbro, East Greenland

Brown

Farmer

1971

Geol. Mag.

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Rhythmic layering in which the layers grade from coarse base to finer top is described in a plagioclase-pyroxene-olivine gabbro. The medium sizes of the various cumulus minerals at each level have significantly different settling velocities. Variation in the proportions of the cumulus minerals accompanies the size grading. It is shown that these characteristics can reasonably be accounted for if hydrodynamic factors exerted the main control, over-riding any chemical effects.

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“…The study of the flow of non-Newtonian fluids is more recent, yet extensive (see, for instance, Dix & Scott Blair, 1940;Eirich, 1956;Eirich & Riseman, 1949;Jeffery, 1922;Reiner, 1956;Rivlin, 1948;Saffman, 1956;Starkey, 1955Starkey, , 1956Vand, 1948). The flow of blood, especially, has been investigated in earnest by physiologists and physicists alike; among them are: Bayliss (1952, 1959, 19621, Fahraeus and Lindqvist (19311, Haynes (1960, Isenberg (1953), Nygaard and coauthors (19351, Pirofsky (19531, Wells and Merrill (19611, Whitmore (19601, and Wittaker and Winton (1933).…”

Section: Introductionmentioning

confidence: 99%

“…Some interpret is as a Magnus effect, a lateraldeviation exhibited by spinning objects from their line of projection (Haynes, 1962;Haynes & Burton, 1959;Starkey, 1956;Tollert, 1954). Jeffery ( 1922) proposes for its explanation the hypothesis of a minimal energy dissipation.…”

Section: Introductionmentioning

confidence: 99%