Recharge and dynamics of the Tamanrasset alluvial aquifer (Algerian Sahara)
Abstract 18 O, 2 H). Monthly monitoring of groundwater level in around thirty wells was complemented by automatic recorders with hourly time steps since March 2016 in three wells, along a 600 m transect perpendicular to the wadi bed. The slow response of the water table is visible only two months after the first flood; its maximum rise was 1 m in 2016. Isotopic analyses of rainwater on a daily time scale, of the wadi water on a 1 h time scale during runoff and of groundwater (two complete campaigns in the dry and wet seasons and a specific monitoring of the transect every month) have provided additional information on surface-groundwater transfer.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Recharge and dynamics of the Tamanrasset alluvial aquifer (Algerian Sahara) ; volume:385 ; year:2024 ; pages:345-349 ; extent:5
Proceedings of the International Association of Hydrological Sciences / International Association of Hydrological Sciences ; 385 (2024), 345-349 (gesamt 5)
- Creator
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Hadj-Said, Samia
Zeddouri, Aziez
Taupin, Jean-Denis
Patris, Nicolas
Leduc, Christian
- DOI
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10.5194/piahs-385-345-2024
- URN
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urn:nbn:de:101:1-2404250434298.014523912319
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:03 AM CEST
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Associated
- Hadj-Said, Samia
- Zeddouri, Aziez
- Taupin, Jean-Denis
- Patris, Nicolas
- Leduc, Christian
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