Selection of supportive data sets and representative outputs of the three dimensional hyporheic model of the River Bure, UK.
Authors: | |
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Owners: | Cagri Gokdemir |
Type: | Resource |
Storage: | The size of this resource is 158.8 MB |
Created: | Apr 28, 2018 at 9:41 a.m. |
Last updated: | Apr 28, 2018 at 5:24 p.m. |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 1973 |
Downloads: | 47 |
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Abstract
The combined effect of stream morphology, water discharge and heterogeneity of the hydraulic conductivity of stream-bed sediments on hyporheic exchange processes was aimed to be revealed. Hyporheic flow dynamics and their effects on dissolved oxygen were investigated in an heterogeneous and morphologically complex low-gradient sub-reach of River Bure, UK. The work was applied by combining field measurements with detailed numerical simulations. The data provided in this contribution contains: (1) Field data; Stream Water Discharge, stream velocity, floodplain water table, stratigrafic data for the sediment, and topographic data with surface and subsurface water dissolved oxygen concentrations, (2) Some part of Model data; particle set data from simulations, imposed water surface elevation boundaries for subsurface model, and supportive codes for data visualization and analysis (see details on README file).
Subject Keywords
Coverage
Spatial
Temporal
Start Date: | 09/07/2013 |
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End Date: | 02/16/2014 |












Content
Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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Education, Audiovisual and Culture Executive Agency of the European Commission | Erasmus Mundus Fellowship |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
Name | Organization | Address | Phone | Author Identifiers |
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Nadim K. Copty | Bogazici University, Turkey | Istanbul, Turkey |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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