Viscous stratified flow towards a sink

書誌事項

公開日
1966-03
権利情報
  • https://www.cambridge.org/core/terms
DOI
  • 10.1017/s002211206600082x
公開者
Cambridge University Press (CUP)

この論文をさがす

説明

<jats:p>In this paper the viscous, slightly stratified flow towards a sink is investigated. The fluid is assumed incompressible, linearly stratified in density, and the flow steady. The theoretical portion of this paper includes both the two-dimensional and the axisymmetric cases, whereas the experimental portion includes only the two-dimensional case. The solutions obtained indicate that there exists a with-drawal layer symmetrically situated about the horizontal plane of the sink. The flow occurs in this layer while outside this layer there is essentially no motion. This withdrawal layer grows in thickness with the distance <jats:italic>x</jats:italic> (or <jats:italic>r</jats:italic>) from the sink at a rate proportional to <jats:inline-formula>$x^{\frac{1}{3}}$</jats:inline-formula> (or <jats:inline-formula>$r^{\frac{1}{3}}$</jats:inline-formula>). The velocity distributions <jats:italic>u</jats:italic>(<jats:italic>y</jats:italic>) (or <jats:italic>u</jats:italic>(<jats:italic>z</jats:italic>)) are similar from one station <jats:italic>x</jats:italic> (or <jats:italic>r</jats:italic>) to another.</jats:p>

収録刊行物

被引用文献 (1)*注記

もっと見る

詳細情報 詳細情報について

問題の指摘

ページトップへ