Modelaci?n Continua en la Subcuenca superior de valle ?tztal
Mountain Rivers are sources for water and sediments and move it into valleys. The steep terrains and streams are often covered with gravel and vegetated sparsely. These bed materials are mobilized and transported under different conditions. If this process happens in the riverbed, it is called bed l...
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Australia / Universidad de Innsbruck / 2015
2017
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oai:localhost:28000-45922017-08-22T08:02:29Z Modelaci?n Continua en la Subcuenca superior de valle ?tztal Carrillo Moreno, Elsa Mariela Achleither, Stefan TRANSPORTE DE SEIMENTOS MODELACI?N NUM?RICA CAUDALES HIDROLOG?A Mountain Rivers are sources for water and sediments and move it into valleys. The steep terrains and streams are often covered with gravel and vegetated sparsely. These bed materials are mobilized and transported under different conditions. If this process happens in the riverbed, it is called bed load transport. The active layer and sub-surface layer form together a mixed layer, where only the active layer interacts directly with the flow, and also an interchange process occurs with the two layers mentioned before. 2017-08-21T14:12:17Z 2017-08-21T14:12:17Z 2015-01-02 masterThesis Carrillo Moreno, Elsa Mariela. (2015). Modelaci?n Continua en la Subcuenca superior de valle ?tztal. (Trabajo de titulaci?n de la Maestr?a en Ingenier?a Ambiental). Universidad de Innsbruck. Australia 84 p. http://repositorio.educacionsuperior.gob.ec/handle/28000/4592 eng 84 p. Australia / Universidad de Innsbruck / 2015 |
institution |
SENESCYT |
collection |
Repositorio SENESCYT |
biblioteca |
Biblioteca Senescyt |
language |
eng |
format |
Tesis de Maestría |
topic |
TRANSPORTE DE SEIMENTOS MODELACI?N NUM?RICA CAUDALES HIDROLOG?A |
spellingShingle |
TRANSPORTE DE SEIMENTOS MODELACI?N NUM?RICA CAUDALES HIDROLOG?A Carrillo Moreno, Elsa Mariela Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
description |
Mountain Rivers are sources for water and sediments and move it into valleys. The steep terrains and streams are often covered with gravel and vegetated sparsely. These bed materials are mobilized and transported under different conditions. If this process happens in the riverbed, it is called bed load transport. The active layer and sub-surface layer form together a mixed layer, where only the active layer interacts directly with the flow, and also an interchange process occurs with the two layers mentioned before. |
author2 |
Achleither, Stefan |
author_facet |
Achleither, Stefan Carrillo Moreno, Elsa Mariela |
author |
Carrillo Moreno, Elsa Mariela |
author_sort |
Carrillo Moreno, Elsa Mariela |
title |
Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
title_short |
Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
title_full |
Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
title_fullStr |
Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
title_full_unstemmed |
Modelaci?n Continua en la Subcuenca superior de valle ?tztal |
title_sort |
modelaci?n continua en la subcuenca superior de valle ?tztal |
publisher |
Australia / Universidad de Innsbruck / 2015 |
publishDate |
2017 |
url |
http://repositorio.educacionsuperior.gob.ec/handle/28000/4592 |
_version_ |
1634995265375043584 |
score |
11,871979 |