'Flow equation' diaporamas de présentation

Functional renormalization group for the effective average action

Functional renormalization group for the effective average action. physics at different length scales. microscopic theories : where the laws are formulated effective theories : where observations are made

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Unification from Functional Renormalization

Unification from Functional Renormalization. Wegner, Houghton. /. Effective potential includes all fluctuations. Unification from Functional Renormalization. fluctuations in d=0,1,2,3,... linear and non-linear sigma models vortices and perturbation theory bosonic and fermionic models

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788 views • 77 slides

Emergence of new laws with Functional Renormalization

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Functional renormalization group equation for strongly correlated fermions

Functional renormalization group equation for strongly correlated fermions. collective degrees of freedom. Hubbard model. Electrons on a cubic lattice here : on planes ( d = 2 ) Repulsive local interaction if two electrons are on the same site

899 views • 70 slides

540 views • 53 slides

LAYER-PROPERTY FLOW PACKAGE

LAYER-PROPERTY FLOW PACKAGE. The Layer-Property Flow ( LPF ) Package is an internal flow package like the BCF Package, thus the two should not be used simultaneously. Computes conductance components and the rate of water movement into and out of storage.

794 views • 44 slides

Critical Fluctuation s in the Polyakov L oop -Quark-Meson model and HIC

Critical Fluctuation s in the Polyakov L oop -Quark-Meson model and HIC. Role of q uantum and t hermal fluctuations near chiral phase transition Functional Renormalization Group (FRG) in PQM model FRG in P QM model at work:

418 views • 29 slides

WATER CONTROL STRUCTURES

1.93k views • 26 slides

Chiral models: predictions under mean field dynamics

Quantum Fluctuation and scaling in the Polyakov loop -Quark-Meson model. Chiral models: predictions under mean field dynamics Role of Quantum and Thermal fluctuations: Functional Renormalization Group (FRG) Approach

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Lecture 7 & 8

Lecture 7 & 8. Refraction of q Equivalent K for fractured media. Refraction of q. Flow across boundary is equal Pressure at interface is the same in both PMs. Example.

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Lecture 7

Lecture 7. Refraction of q Equivalent K for fractured media. Refraction of q. Flow across boundary is equal Pressure at interface is the same in both PMs. Example.

194 views • 14 slides

Transport Modeling in Groundwater

Transport Modeling in Groundwater. Components of a Mathematical Model Governing Equation Boundary Conditions Initial conditions (for transient problems). In full solute transport problems, we have two mathematical models: one for flow and one for transport.

166 views • 14 slides