Flopping phenomenon of flow behind two plates placed side-by-side normal to the flow direction

Some accelerated flows of generalized Ol

Some accelerated flows of generalized Oldroyd-B fluid between two side walls perpendicular to the plate

✍ S. Hyder Ali Muttaqi Shah 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 390 KB

Unsteady flow of an Oldroyd-B fluid indu

Unsteady flow of an Oldroyd-B fluid induced by the impulsive motion of a plate between two side walls perpendicular to the plate

✍ C. Fetecau; T. Hayat; M. Khan; C. Fetecau 📂 Article 📅 2008 🏛 Springer Vienna 🌐 English ⚖ 568 KB

Erratum to: Unsteady flow of an Oldroyd-

Erratum to: Unsteady flow of an Oldroyd-B fluid induced by the impulsive motion of a plate between two side walls perpendicular to the plate

✍ C. Fetecau; T. Hayat; M. Khan; Corina Fetecau 📂 Article 📅 2010 🏛 Springer Vienna 🌐 English ⚖ 91 KB

Exact solutions for the flow of a genera

Exact solutions for the flow of a generalized Oldroyd-B fluid induced by a constantly accelerating plate between two side walls perpendicular to the plate

✍ Constantin Fetecau; Corina Fetecau; M. Kamran; D. Vieru 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 769 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin