Long-term forward hydrologic fluvial system evolution model

DSpace/Manakin Repository

Long-term forward hydrologic fluvial system evolution model

Show simple item record


dc.creator Vining, Mark Richard
dc.date.available 2011-02-18T20:40:54Z
dc.date.issued 1997-05
dc.identifier.uri http://hdl.handle.net/2346/14463 en_US
dc.description.abstract This work presents a computer model of river sediment transport and the morphologic evolution of the river system, on the scale of thousands to millions of years, with the influence of geologic processes. The computer program runs under Windows '95 or 3.x. Code is written in Borland C++ 5.01. Data input is from eight editable files. The code, sample data, and user instructions are provided. The model is a 1-D finite-difference scheme of longterm average flow conditions. The simulation is discretized into time steps, length cells, sediment grain size classes, and fluvial environments within each cell. The cell landscape is composed of three fluvial environments (channel, alluvial ridge, and floodplain) and the watershed drainage area. Time steps are divided into four steadystate domains which characterize short-term variations in discharge. A time dilation procedure characterizes the varying shape of discharge event hydrographs downstream.
dc.format.mimetype application/pdf
dc.language.iso eng
dc.publisher Texas Tech University en_US
dc.subject Rivers en_US
dc.subject Navasota River en_US
dc.subject Streamflow en_US
dc.title Long-term forward hydrologic fluvial system evolution model
dc.type Dissertation
thesis.degree.name Ph.D.
thesis.degree.level Doctoral
thesis.degree.discipline Geosciences
thesis.degree.grantor Texas Tech University
thesis.degree.department Geosciences
dc.degree.department Geosciences en_US
dc.rights.availability Unrestricted.

Files in this item

Files Size Format View
31295011239893.pdf 21.66Mb PDF View/Open

This item appears in the following Collection(s)

Show simple item record

Browse

My Account