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Entropy 2014, 16(7), 3808-3812; doi:10.3390/e16073808

Entropy Generation in Steady Laminar Boundary Layers with Pressure Gradients

1,2,*  and 3
Received: 16 April 2014 / Revised: 3 July 2014 / Accepted: 7 July 2014 / Published: 10 July 2014
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Abstract: In an earlier paper in Entropy [1] we hypothesized that the entropy generation rate is the driving force for boundary layer transition from laminar to turbulent flow. Subsequently, with our colleagues we have examined the prediction of entropy generation during such transitions [2,3]. We found that reasonable predictions for engineering purposes could be obtained for flows with negligible streamwise pressure gradients by adapting the linear combination model of Emmons [4]. A question then arises—will the Emmons approach be useful for boundary layer transition with significant streamwise pressure gradients as by Nolan and Zaki [5]. In our implementation the intermittency is calculated by comparison to skin friction correlations for laminar and turbulent boundary layers and is then applied with comparable correlations for the energy dissipation coefficient (i.e., non-dimensional integral entropy generation rate). In the case of negligible pressure gradients the Blasius theory provides the necessary laminar correlations.
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MDPI and ACS Style

McEligot, D.M.; Walsh, E.J. Entropy Generation in Steady Laminar Boundary Layers with Pressure Gradients. Entropy 2014, 16, 3808-3812.

AMA Style

McEligot DM, Walsh EJ. Entropy Generation in Steady Laminar Boundary Layers with Pressure Gradients. Entropy. 2014; 16(7):3808-3812.

Chicago/Turabian Style

McEligot, Donald M.; Walsh, Edmond J. 2014. "Entropy Generation in Steady Laminar Boundary Layers with Pressure Gradients." Entropy 16, no. 7: 3808-3812.

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