Abstract O-03

Abstract OO Big O

OO Big O Joan Krone Denison University Department of Math and CS Granville, Ohio 43023 740-587-6484 [email protected] W. F. Ogden The Ohio State University Neal Avenue Columbus, Ohio 43210 614-292-6007 [email protected] SUMMARY When traditional Big O analysis is rigorously applied to object oriented software, several deficiencies quickly manifest themselves. Because the traditional defin...

690-700 Gw S-o 03

Seepage-face boundaries are common features of unconfined ground water flow. These boundaries exist at the intersection of an unconfined aquifer and a surface water body such as a lake, river, or wetland. The existence of a seepage-face boundary is necessary to provide a physical transition between the internal water-table boundary and the external equipotential boundary when an unconfined aqui...

587-601 GW S-O 03 color

The generalized conceptual model for a fractured bedrock aquifer consists of low-permeability matrix blocks separated by highly permeable fractures that act as preferential pathways for ground water flow. The National Research Council (NRC 1996) summarizes three approaches for simulating ground water flow in fractured aquifers. The most common approach is to represent the system with an equival...

Microsoft Word - ANZMS 2011 Collated Abstract in Word 97-03

Se p 20 03 Five - loop ǫ expansion for O ( n ) × O ( m ) spin models

We compute the Renormalization Group functions of a Landau-GinzburgWilson Hamiltonian with O(n)×O(m) symmetry up to five-loop in Minimal Subtraction scheme. The line n+(m,d), which limits the region of secondorder phase transition, is reconstructed in the framework of the ǫ = 4 − d expansion for generic values of m up to O(ǫ5). For the physically interesting case of noncollinear but planar orde...