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The alkali soils of the middle Niger Valley Origins, formation and present evolution
Barbiero L., Van Vliet Lanoe B.
Geoderma 84 (1997) 323-343 - http://hal.archives-ouvertes.fr/hal-00364728
Articles dans des revues avec comité de lecture
Planète et Univers/Sciences de la Terre
The alkali soils of the middle Niger Valley Origins, formation and present evolution
Laurent Barbiero ( ) 1, Brigitte Van Vliet Lanoe 2, 3
1 :  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
2 :  Processus et bilan des domaines sédimentaires (PBDS)
http://www.univ-lille1.fr/geosciences/page_ufr/cnrs_1/umr_pbds.ht
CNRS : UMR8110 – INSU – Université Lille I - Sciences et technologies
Bâtiment SN5 59655 VILLENEUVE D ASCQ CEDEX
France
3 :  Domaines Océaniques
http://www-sdt.univ-brest.fr/
Institut Universitaire Européen de la Mer (IUEM) – Université de Bretagne Occidentale [UBO] – Observatoire des Sciences de l'Univers – CNRS : UMR6538
Technopôle Brest-Iroise, Place Copernic, 29280 Plouzané
France
In Niger Republic, the regional development of irrigation along the river Niger is confronted with an large extension of alkali soils. The study of one of these areas, on the Liptako bedrock, reveals a concentric soil distribution: in a zone of brown soil with abrupt textural change and alkaline in depth (stagnic Solonetz), appears a ring of brown steppe soils (cambic Calcisol), and zones of alkali soils (Solonetz). These alkali soils are not saline but their soil solution is more concentrated than in brown steppe soils. The study of the abrupt contact between brown steppe soils and alkali soils shows morphological and geochemical changes, due to calcite and fluorite precipitation. The detailed study of this contact demonstrates a present transformation of alkali soils into brown steppe soils. Therefore, it appears that soil alkalization is no longer in process on the terraces of the river Niger. The formation of brown steppe soils and alkali soils may be explained by the existence of a former pond. This hypothesis is supported by aerial pictures and microscopic observations. It is also consistent with a recent study of the hydrology of sahelian ponds and with considerations on the chemical quality of the runoff.
Anglais

Geoderma
Publisher Elsevier
ISSN 0016-7061 
internationale
04/11/1997
84
323-343

non-saline alkali soils – sodic soils – soil genesis – de-alkalization – Sahel – Niger

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