𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Electromagnetoelastic equations for ferroelectrics based on a micromorphic dielectric model

✍ Scribed by Maurizio Romeo

Publisher
Springer Vienna
Year
2011
Tongue
English
Weight
266 KB
Volume
223
Category
Article
ISSN
0001-5970

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Yang–Baxter equation-based potential mod
Yang–Baxter equation-based potential model for a one-dimensional fermion system
✍ Gao-Yuan Chiang; Chin-Rong Lee; Hsiang-nan Li 📂 Article 📅 1999 🏛 Elsevier Science 🌐 English ⚖ 160 KB

We propose a velocity-dependent d-function potential model for a one-dimensional fermion system, under which the two-particle interchange operators in the Bethe hypothesis satisfy the Yang-Baxter equation. This model, proportional to the product of the momenta of two interacting particles, is not tr

Modelling overland flow based on Saint-V
Modelling overland flow based on Saint-Venant equations for a discretized hillslope system
✍ Guang-Te Wang; Shulin Chen; Jan Boll; C. O. Stockle; D. K. McCooL 📂 Article 📅 2002 🏛 John Wiley and Sons 🌐 English ⚖ 148 KB 👁 1 views

## Abstract Mathematical modelling of overland flow is a critical task in simulating transport of water, sediment and other pollutants from land surfaces to receiving waters. In this paper, an overland flow routing method is developed based on the Saint‐Venant equations using a discretized hillslop

A fast modelling tool for plate heat exc
A fast modelling tool for plate heat exchangers based on depth-averaged equations
✍ Marko Lyytikäinen; Taija Hämäläinen; Jari Hämäläinen 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 433 KB

In this study, the depth-averaged flow and energy equations for plate heat exchangers are presented. The equations are derived by integrating the original 3D flow and energy equations over the height of the gap between the bottom and top plates. This approach reduces the equations from 3D to 2D but

A model for the chromosphere-corona tran
A model for the chromosphere-corona transition region based on radio observations and on hydrodynamical conservation equations
✍ P. Lantos 📂 Article 📅 1972 🏛 Springer 🌐 English ⚖ 727 KB

In order to avoid the disagreements and difficulties now found in the interpretation of quiet-Sun UV observations concerning the chromosphere-corona transition region, 6-and ll-cm maps obtained at cycle maximum with the Nanqay radiotelescope are used in combination with existing measurements of the

A 3-D model based on Navier–Stokes equat
A 3-D model based on Navier–Stokes equations for regular and irregular water wave propagation
✍ Bin Li 📂 Article 📅 2008 🏛 Elsevier Science 🌐 English ⚖ 680 KB

A spatial fixed s-coordinate is used to transform the Navier-Stokes equations from the sea bed to the still water level. In the fixed s-coordinate system only a very small number of vertical grid points are required for the numerical model. The time step for using the spatial fixed s-coordinate is e