On the 1D Unsteady Porous Flow Equation: MAST G6-S: Project 1, Wave Action on and in Coastal Structures

H. F. Burcharth; O.H. Andersen

On the 1D Unsteady Porous Flow Equation: MAST G6-S: Project 1, Wave Action on and in Coastal Structures

Forskningsgruppen for Hav og Kystbyggeri

Publikation: Bog/antologi/afhandling/rapport › Rapport › Forskning › peer review

Abstract

The lD unsteady porous flow equation is often given as
I = av + blvlv + c ~ ( 1)

where I is the hydraulic gradient and V is a characteristic velocity. The two first terms compare to the steady flow Forchlieimer equation.

Originalsprog	Engelsk

Udgivelsessted	Aalborg
Forlag	Aalborg Universitetsforlag
Antal sider	11
Status	Udgivet - 1992

Emneord

Large Porosity
Small Porosity
Dimension Analysis
Reynolds Equations

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Citationsformater

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title = "On the 1D Unsteady Porous Flow Equation: MAST G6-S: Project 1, Wave Action on and in Coastal Structures",

abstract = "The lD unsteady porous flow equation is often given asI = av + blvlv + c ~ ( 1)where I is the hydraulic gradient and V is a characteristic velocity. The two first terms compare to the steady flow Forchlieimer equation.",

keywords = "Large Porosity, Small Porosity, Dimension Analysis, Reynolds Equations, Large Porosity, Small Porosity, Dimension Analysis, Reynolds Equations",

author = "Burcharth, {H. F.} and O.H. Andersen",

year = "1992",

language = "English",

publisher = "Aalborg Universitetsforlag",

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TY - RPRT

T1 - On the 1D Unsteady Porous Flow Equation

T2 - MAST G6-S: Project 1, Wave Action on and in Coastal Structures

AU - Burcharth, H. F.

AU - Andersen, O.H.

PY - 1992

Y1 - 1992

N2 - The lD unsteady porous flow equation is often given asI = av + blvlv + c ~ ( 1)where I is the hydraulic gradient and V is a characteristic velocity. The two first terms compare to the steady flow Forchlieimer equation.

AB - The lD unsteady porous flow equation is often given asI = av + blvlv + c ~ ( 1)where I is the hydraulic gradient and V is a characteristic velocity. The two first terms compare to the steady flow Forchlieimer equation.

KW - Large Porosity

KW - Small Porosity

KW - Dimension Analysis

KW - Reynolds Equations

KW - Large Porosity

KW - Small Porosity

KW - Dimension Analysis

KW - Reynolds Equations

M3 - Report

BT - On the 1D Unsteady Porous Flow Equation

PB - Aalborg Universitetsforlag

CY - Aalborg

ER -

On the 1D Unsteady Porous Flow Equation: MAST G6-S: Project 1, Wave Action on and in Coastal Structures

Abstract

Emneord

AUB Link

Fingeraftryk

Citationsformater