The interface between fluid-like and solid-like behaviour in two-dimensional granular flows

Interface between fluid- and solid-like

Interface between fluid- and solid-like behaviour in rapid granular flows down bumpy inclines

✍ Chou, Chuen-Shii 📂 Article 📅 1999 🏛 John Wiley and Sons 🌐 English ⚖ 202 KB

Gravity-driven granular #ows down bumpy inclined surfaces were investigated. The #ows consist of a bottom region of an amorphous solid-like granular material interacting with a top region of rapidly agitated grains. Chou theoretically analysed these granular #ows by employing the constitutive theory

The Widom line as the crossover between

The Widom line as the crossover between liquid-like and gas-like behaviour in supercritical fluids

✍ Simeoni, G. G.; Bryk, T.; Gorelli, F. A.; Krisch, M.; Ruocco, G.; Santoro, M.; S 📂 Article 📅 2010 🏛 Nature Publishing Group 🌐 English ⚖ 554 KB

Thermal-, Pressure- and Light-Induced Sp

Thermal-, Pressure- and Light-Induced Spin-Crossover Behaviour in the Two-Dimensional Hofmann-Like Coordination Polymer [Fe(3-Clpy) 2 Pd(CN) 4 ]

✍ Martínez, Víctor; Arcís Castillo, Zulema; Muñoz, M. Carmen; Gaspar, Ana B.; Etri 📂 Article 📅 2013 🏛 John Wiley and Sons 🌐 English ⚖ 711 KB

Investigation on the formation behaviour

Investigation on the formation behaviour of banded texture in thermotropic main-chain liquid crystalline polymers with linear rod-like and two-dimensional mesogenic units

✍ Jianan Hou; Wei Wu; Mao Xu; Zifa Li 📂 Article 📅 1996 🏛 Elsevier Science 🌐 English ⚖ 604 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