Additional tangential and normal stress close to the wall in the motion of a two-component flow

The effect of slip on the motion of a sp

The effect of slip on the motion of a sphere close to a wall and of two adjacent spheres

✍ L. M. Hocking 📂 Article 📅 1973 🏛 Springer 🌐 English ⚖ 931 KB

Investigation of the local component of

Investigation of the local component of the neutron noise in a BWR and its application to the study of two-phase flow

✍ G. Kosály; Lj. Kostić; L. Miteff; G. Varadi; K. Behringer 📂 Article 📅 1977 🏛 Elsevier Science 🌐 English ⚖ 806 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