1 / 44

Sustainable Groundwater Management of the Iullemeden Aquifer System

Explore the geometry, recharge, discharges, and piezometry of the Iullemeden aquifer system, focusing on water balance and effective management strategies using environmental tracers and remote sensing. Discover insights on groundwater balance estimates, age dating with tracers, and potential overexploitation prevention.

pearce
Download Presentation

Sustainable Groundwater Management of the Iullemeden Aquifer System

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Groundwater Management of the Iullemeden Aquifer System C. Alberich, W. Kinzelbach IHW, ETH Zürich, Switzerland A. Dodo Direction National de Ressources en Eau Niamey, Niger

  2. Contents • Geometry and boundary conditions of model • Recharge estimation • Discharges • Piezometry • Water balance • Conclusions

  3. Iullemmeden Basin

  4. Geometry and Boundary Conditions Cristallin Rock B Primary Argiles d‘Irhazer Ci -Ch Marin Cretaceous Adrar des Iforas Massif de l‘Aïr Ct Tombouctou Gao Detroit Soudanaise Rift Oriental LAKE TCHAD Niamey Sokoto N‘guru Kano Maiduguri A

  5. (Greigert,1979) Continental Terminal Paleocene - Ypresian Marine and Lacustrine Upper Cretaceous Iullemmeden aquifer system Continental intercalaire - Continental hamadien Argiles d‘Irhazer - Serie Izegouandane West of Massif de l‘Aïr Primary

  6. 19 19 18 18 17 17 16 16 15 15 1? 14 14 13 13 12 12 11 11 1 2 3 4 5 6 7 8 9 1 2 3 4 5 6 7 8 9 [Cr6a-5] [Cr6b] [Cr7] Upper Cretaceous Marine and Lacustrine Formations / Paleocene - Ypresian 19 18 17 16 15 14 13 12 11 1 2 3 4 5 6 7 8 9 Calc. à Neobilites Calcaires et argiles Lower sandstones Term I Calc. à Nigecigeras Term IV à Libycoceras ismaeli and mudstones Série Calc. Blancs Argiles sableuses Term II Mosasaurus shales Term V Rima Group Sables à Cocodriliens Série Marnes et Calcaires Upper sandstones TermVI-VII Paleocene Term III and mudstones (Sokoto Group)

  7. Nigeria Niger / Mali Model Gwandu Ct3 Ct3 Ct2 Ct2 Ct1 Gwandu Ct1 Sokoto Terms VI and VII Terms IV and V Rima Terms I to III Lower sedimentary complex [Cr6-5] to [Cr7] Gundumi - Illo Ci -Ch

  8. Radier,1959 Greigert,1961 Greigert and Pougnet,1967 Greigert,1979 Ogilbee andAnderson, 1965/1973 Oteze, 1976 Pallas, 1971 Boundary Conditions Cristallin Rock Primary Argiles d‘Irhazer Ci -Ch Marine Cretaceous Adrar des Iforas Massif de l‘Aïr Ct Anefis Agades Tombouctou Gao Detroit Soudanaise Rift Oriental Taouardeï Zinder LAKE TCHAD Niamey Sokoto N‘guru Kano Maiduguri

  9. Bottom of lower sedimentary complex

  10. Top of lower sedimentary complex

  11. Top of CT1 (blue)

  12. Top of CT2 (orange)

  13. Top of CT3 (yellow)

  14. Recharge • Single most important figure for sustainable management. • Water balance methods and Darcy formula notoriously inaccurate (factor of 10) • Environmental tracers can often be better (factor of 2-3) • Tracers used: Tritium, Tritium-3He, CFC (Freons), SF6, Chloride • Remote sensing info combined with groundwater flow and transport models allow to test hypotheses on recharge mechanisms (areal and concentrated recharge) • Use of precipitation and evapotranspiration maps obtained with RS methods can help at delineating zones

  15. Sampling for CFC in groundwater (Niger)

  16. ATMOSPHERIC CFC CONCENTRATIONS IN THE ATMOSPHERE F12 F11

  17. Tritium Concentration in Rainwater

  18. Principle of Age Dating With Tracers Result: Pore velocity u = L/t delay t With porosity we obtain specific flux q = nu With area we obtain total flux Q = qA L

  19. Evapotranspiration for the 5th March 1992 calculated from NOAA-AVHRR using SEBAL mm/d

  20. Precipitation map from METEOSAT (Example 1-10 June 1995) mm/10d 10° – 20° North 0° – 10° East

  21. Tritium corrected to 1985 related to depth to the water table 0

  22. Tritium in wells(1967-2000)

  23. NDVI from Landsat TM of Feb. 1986

  24. NDVI Spot image 30.9.96

  25. Survey of Mares (from satellite image)

  26. Survey of Mares (ground truth /satellite)

  27. Population Distribution in the Iullemmeden Estimated water consumption 50 l/person/day Inhabitants/km2 or more

  28. Vertical Distribution of Abstractions by Wells

  29. Discharge by Evapotranspiration • Potential ET • 2000 mm/a • Digital terrain model • Extinction depth for evapotranspiration • up to 50 m • Evaporation by vapour transport (Coudrain-Ribstein) • E = 71.7 z -1.49 (E in mm/a, z in m) • in Iullemmeden basin negligible

  30. Piezometry of CI (observed)

  31. Piezometry of CT1 (observed)

  32. Piezometry of CT2 (observed)

  33. Piezometry of CI (computed)

  34. Piezometry of CT1 (computed)

  35. Piezometry of CT2 (computed)

  36. Groundwater balance (first rough estimate from model) + 70 m3/s - 50 m3/s - 10 m3/s - 10 m3/s

  37. Conclusions 1 • Model concept available due to previous work • Mechanisms of recharge can only be identified in more local studies, generalization to the total area requires related remote sensing data • Distributed input data such as discharges rely heavily on proxi data such as population maps, soil maps and remote sensing data • Accuracy of model fluxes still has to verified. In this task environmental tracers are useful

  38. Conclusions 2 • Presently overexploitation has not yet started • New technology can help to do a better job in resource assessment than has been possible in the past • Besides the donor driven activities in Niger which lead to a large number of new wells a strategic consideration of the whole is necessary

More Related