A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools
There is little information in scientific literature regarding the modifications induced by check dam systems in flow regimes within restored gully reaches, despite it being a crucial issue for the design of gully restoration measures. Here, we develop a conceptual model to classify flow regimes in...
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2014-05-01
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doaj-03fa892a7e264bdcb4d5401855c18b162020-11-24T22:00:25ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-05-011851705172110.5194/hess-18-1705-2014A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-poolsC. Castillo0R. Pérez1J. A. Gómez2Institute for Sustainable Agriculture, CSIC, Apartado 4084, 14080 Cordoba, SpainUniversity of Cordoba, Dept. of Rural Engineering, Campus Rabanales, Leonardo Da Vinci Building, 14071 Cordoba, SpainInstitute for Sustainable Agriculture, CSIC, Apartado 4084, 14080 Cordoba, SpainThere is little information in scientific literature regarding the modifications induced by check dam systems in flow regimes within restored gully reaches, despite it being a crucial issue for the design of gully restoration measures. Here, we develop a conceptual model to classify flow regimes in straight rectangular channels for initial and dam-filling conditions as well as a method of estimating efficiency in order to provide design guidelines. The model integrates several previous mathematical approaches for assessing the main processes involved (hydraulic jump, impact flow, gradually varied flows). Ten main classifications of flow regimes were identified, producing similar results when compared with the IBER model. An interval for optimal energy dissipation (ODI) was observed when the steepness factor <i>c</i> was plotted against the design number (DN, ratio between the height and the product of slope and critical depth). The ODI was characterized by maximum energy dissipation and total influence conditions. Our findings support the hypothesis of a maximum flow resistance principle valid for a range of spacing rather than for a unique configuration. A value of <i>c</i> = 1 and DN ~ 100 was found to economically meet the ODI conditions throughout the different sedimentation stages of the structure. When our model was applied using the same parameters to the range typical of step-pool systems, the predicted results fell within a similar region to that observed in field experiments. The conceptual model helps to explain the spacing frequency distribution as well as the often-cited trend to lower <i>c</i> for increasing slopes in step-pool systems. This reinforces the hypothesis of a close link between stable configurations of step-pool units and man-made interventions through check dams.http://www.hydrol-earth-syst-sci.net/18/1705/2014/hess-18-1705-2014.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
C. Castillo R. Pérez J. A. Gómez |
spellingShingle |
C. Castillo R. Pérez J. A. Gómez A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools Hydrology and Earth System Sciences |
author_facet |
C. Castillo R. Pérez J. A. Gómez |
author_sort |
C. Castillo |
title |
A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
title_short |
A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
title_full |
A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
title_fullStr |
A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
title_full_unstemmed |
A conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
title_sort |
conceptual model of check dam hydraulics for gully control: efficiency, optimal spacing and relation with step-pools |
publisher |
Copernicus Publications |
series |
Hydrology and Earth System Sciences |
issn |
1027-5606 1607-7938 |
publishDate |
2014-05-01 |
description |
There is little information in scientific literature regarding the
modifications induced by check dam systems in flow regimes within restored
gully reaches, despite it being a crucial issue for the design of gully
restoration measures. Here, we develop a conceptual model to classify flow
regimes in straight rectangular channels for initial and dam-filling
conditions as well as a method of estimating efficiency in order to provide
design guidelines. The model integrates several previous mathematical
approaches for assessing the main processes involved (hydraulic jump, impact
flow, gradually varied flows). Ten main classifications of flow regimes were
identified, producing similar results when compared with the IBER model. An
interval for optimal energy dissipation (ODI) was observed when the steepness
factor <i>c</i> was plotted against the design number (DN, ratio between the
height and the product of slope and critical depth). The ODI was
characterized by maximum energy dissipation and total influence conditions.
Our findings support the hypothesis of a maximum flow resistance principle
valid for a range of spacing rather than for a unique configuration. A value
of <i>c</i> = 1 and DN ~ 100 was found to economically meet the ODI
conditions throughout the different sedimentation stages of the structure.
When our model was applied using the same parameters to the range typical of
step-pool systems, the predicted results fell within a similar region to that
observed in field experiments. The conceptual model helps to explain the
spacing frequency distribution as well as the often-cited trend to lower <i>c</i>
for increasing slopes in step-pool systems. This reinforces the hypothesis of
a close link between stable configurations of step-pool units and man-made
interventions through check dams. |
url |
http://www.hydrol-earth-syst-sci.net/18/1705/2014/hess-18-1705-2014.pdf |
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