Distance from unconditional stability boundary of a two-port network

Unconditional Stability Boundaries of a

Unconditional Stability Boundaries of a Three-Port Network

✍ Rong-Fa Kuo; Tah-Hsiung Chu 📂 Article 📅 2010 🏛 IEEE 🌐 English ⚖ 446 KB

Unconditional Stability of a Three-Port

Unconditional Stability of a Three-Port Network Characterized with S-Parameters

✍ Boehm, J.F.; Albright, W.G. 📂 Article 📅 1987 🏛 IEEE 🌐 English ⚖ 559 KB

Distance of a complex coefficient stable

Distance of a complex coefficient stable polynomial from the boundary of the stability set

✍ Alfredo C. Desages; Liliana Castro; Hernán Cendra 📂 Article 📅 1991 🏛 Springer US 🌐 English ⚖ 642 KB

Calculation of the transient reflection

Calculation of the transient reflection from a two-port network with a nonlinear resistor load

✍ Sailing He 📂 Article 📅 1997 🏛 John Wiley and Sons 🌐 English ⚖ 101 KB

Consequently, it is important to recover such properties and to take the advantage of the energy radiated into the dielectric substrate. One solution is to use a lens placed at the back of the antenna, the focal point of this lens being at the gap level. Consequently, the radiation in the dielectric

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