Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment
The aim of this study was to analyse stormflow processes and the behaviour of solutes therein (Ca2+, Mg2+, Na+, K+, alkalinity, NO-3 , S24-, Cl-, Si), during flood events in tropical semi-arid conditions. The study site was a small Sahelian catchment (1.4 ha) located in northern Burkina Faso. Runoff and rain water was sampled over a 2-year period (1999 and 2000). In addition to dissolved load, suspended load was measured in the stream water collected at the outlet of the catchment. Isotopic tracing using ô180 was also conducted during two very different flood events. The results indicated that: (i) event water was by far the major contributor to the stream stormflow, with Hortonian overland flow being the main stormflow process at work; (ii) a small fraction of pre-event soil water may have contributed during the recession of heavy flood with wet antecedent conditions; (iii) solute concentrations were higher in runoff compared to rainwater. With the exception of NO-3 and Cl-, the highest concentrations were measured at the onset of floods, and almost always decreased during the rising stage of the hydrographs; (iv) a good correlation was found between suspended load and the concentrations of Ca2+, Mg2', alkalinity and Si. It was concluded that fast physico-chemical interactions between event water and reactive suspended phases may explain most of the chemical changes between rainwater and floodwater. © 2007 Elsevier B.V. All rights reserved.
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dig-cirad-fr-5387462024-12-18T14:12:37Z http://agritrop.cirad.fr/538746/ http://agritrop.cirad.fr/538746/ Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment. Ribolzi Olivier, Karambiri Harouna, Bariac Thierry, Benedetti Marc, Caquineaux Sandrine, Descloitres Marc, Aventurier Alain. 2007. Journal of Hydrology, 337 (1-2) : 104-116.https://doi.org/10.1016/j.jhydrol.2007.01.019 <https://doi.org/10.1016/j.jhydrol.2007.01.019> Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment Ribolzi, Olivier Karambiri, Harouna Bariac, Thierry Benedetti, Marc Caquineaux, Sandrine Descloitres, Marc Aventurier, Alain eng 2007 Elsevier Journal of Hydrology P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 Burkina Faso http://aims.fao.org/aos/agrovoc/c_8081 The aim of this study was to analyse stormflow processes and the behaviour of solutes therein (Ca2+, Mg2+, Na+, K+, alkalinity, NO-3 , S24-, Cl-, Si), during flood events in tropical semi-arid conditions. The study site was a small Sahelian catchment (1.4 ha) located in northern Burkina Faso. Runoff and rain water was sampled over a 2-year period (1999 and 2000). In addition to dissolved load, suspended load was measured in the stream water collected at the outlet of the catchment. Isotopic tracing using ô180 was also conducted during two very different flood events. The results indicated that: (i) event water was by far the major contributor to the stream stormflow, with Hortonian overland flow being the main stormflow process at work; (ii) a small fraction of pre-event soil water may have contributed during the recession of heavy flood with wet antecedent conditions; (iii) solute concentrations were higher in runoff compared to rainwater. With the exception of NO-3 and Cl-, the highest concentrations were measured at the onset of floods, and almost always decreased during the rising stage of the hydrographs; (iv) a good correlation was found between suspended load and the concentrations of Ca2+, Mg2', alkalinity and Si. It was concluded that fast physico-chemical interactions between event water and reactive suspended phases may explain most of the chemical changes between rainwater and floodwater. © 2007 Elsevier B.V. All rights reserved. article info:eu-repo/semantics/article Journal Article info:eu-repo/semantics/publishedVersion http://agritrop.cirad.fr/538746/1/document_538746.pdf application/pdf Cirad license info:eu-repo/semantics/restrictedAccess https://agritrop.cirad.fr/mention_legale.html https://doi.org/10.1016/j.jhydrol.2007.01.019 10.1016/j.jhydrol.2007.01.019 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jhydrol.2007.01.019 info:eu-repo/semantics/altIdentifier/purl/https://doi.org/10.1016/j.jhydrol.2007.01.019 |
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Biblioteca del CIRAD Francia |
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P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 http://aims.fao.org/aos/agrovoc/c_8081 P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 http://aims.fao.org/aos/agrovoc/c_8081 |
spellingShingle |
P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 http://aims.fao.org/aos/agrovoc/c_8081 P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 http://aims.fao.org/aos/agrovoc/c_8081 Ribolzi, Olivier Karambiri, Harouna Bariac, Thierry Benedetti, Marc Caquineaux, Sandrine Descloitres, Marc Aventurier, Alain Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
description |
The aim of this study was to analyse stormflow processes and the behaviour of solutes therein (Ca2+, Mg2+, Na+, K+, alkalinity, NO-3 , S24-, Cl-, Si), during flood events in tropical semi-arid conditions. The study site was a small Sahelian catchment (1.4 ha) located in northern Burkina Faso. Runoff and rain water was sampled over a 2-year period (1999 and 2000). In addition to dissolved load, suspended load was measured in the stream water collected at the outlet of the catchment. Isotopic tracing using ô180 was also conducted during two very different flood events. The results indicated that: (i) event water was by far the major contributor to the stream stormflow, with Hortonian overland flow being the main stormflow process at work; (ii) a small fraction of pre-event soil water may have contributed during the recession of heavy flood with wet antecedent conditions; (iii) solute concentrations were higher in runoff compared to rainwater. With the exception of NO-3 and Cl-, the highest concentrations were measured at the onset of floods, and almost always decreased during the rising stage of the hydrographs; (iv) a good correlation was found between suspended load and the concentrations of Ca2+, Mg2', alkalinity and Si. It was concluded that fast physico-chemical interactions between event water and reactive suspended phases may explain most of the chemical changes between rainwater and floodwater. © 2007 Elsevier B.V. All rights reserved. |
format |
article |
topic_facet |
P10 - Ressources en eau et leur gestion P35 - Fertilité du sol P36 - Érosion, conservation et récupération des sols P40 - Météorologie et climatologie tempête hydrologie zone semi-aride eau souterraine eau superficielle ruissellement alluvion lessivage du sol isotope solute http://aims.fao.org/aos/agrovoc/c_7436 http://aims.fao.org/aos/agrovoc/c_3731 http://aims.fao.org/aos/agrovoc/c_6963 http://aims.fao.org/aos/agrovoc/c_3391 http://aims.fao.org/aos/agrovoc/c_25317 http://aims.fao.org/aos/agrovoc/c_35388 http://aims.fao.org/aos/agrovoc/c_25347 http://aims.fao.org/aos/agrovoc/c_15591 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_24133 http://aims.fao.org/aos/agrovoc/c_8081 |
author |
Ribolzi, Olivier Karambiri, Harouna Bariac, Thierry Benedetti, Marc Caquineaux, Sandrine Descloitres, Marc Aventurier, Alain |
author_facet |
Ribolzi, Olivier Karambiri, Harouna Bariac, Thierry Benedetti, Marc Caquineaux, Sandrine Descloitres, Marc Aventurier, Alain |
author_sort |
Ribolzi, Olivier |
title |
Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
title_short |
Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
title_full |
Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
title_fullStr |
Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
title_full_unstemmed |
Mechanisms affecting stormflow generation and solute behaviour in a Sahelian headwater catchment |
title_sort |
mechanisms affecting stormflow generation and solute behaviour in a sahelian headwater catchment |
publisher |
Elsevier |
url |
http://agritrop.cirad.fr/538746/ http://agritrop.cirad.fr/538746/1/document_538746.pdf |
work_keys_str_mv |
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_version_ |
1819041733815566336 |