GOCE-CT-2003- 506680-WADE

Sixth Frammework Programme (2002-2006)

Research in support of the EU Water Initiative

 

WP2 Site Characterisation 

WADE

OBJECTIVES

APPROACH

STUDY AREAS

STUDY SITES

COMMUNITIY PARTICIPATION

WORK PACKAGES

WP2: Site Characterisation

WP3: Palaeoflood Hydrology

WP4: Hydrological Monitoring

WP5: TDR Demonstration

WP6: Modelling

WP7: Water Management

WP8: Results' Dissemination

PARTICIPATING INSTITUTIONS

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RESULTS

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Objectives

Site characterisation has three principal goals: 1) to determine the general characteristics and dynamics of the selected ephemeral channels; 2) to choose the optimum sites for probe installation and sample collection and 3) identify the role of alluvial aquifers in the socio-economy of the catchments. Site characterisation will integrate information from geomorphic, flood and palaeoflood hydrology, soil and sediment information, knowledge on the local groundwater and its use as a water resource.

Geomorphic Setting

Sedimentologic and geomorphic variables related to the flow and storage of water along ephemeral channels will be evaluated to determine the best sites for installation of soil probes and sampling and to form a foundation for monitoring the results. This will include mapping of the study reaches.

 

Riparian Ecosystems

Evapotranspiration by riparian ecosystems is a major loss component of alluvial aquifers. The riparian ecosystems will be classified and characterised. The distribution of classified riparian plant communities will be mapped along the study reaches using ground mapping with base-maps, photographs and ground truth evaluation. Evaporation losses will be estimated based on existing eco-hydrological studies for the specified classes of riparian vegetation.

Riparian vegetation of the Buffels River: Above, 305a Acocks Aug 27th 1957; Below, 305b, Rohde & Hoffman, Nov 25th 2004.

 

Aquifer Characterisation

The aquifers at the study sites will be delineated and represented in GIS compatible format as polygon maps of the total elevation of the top and base of the aquifer. Aquifer thickness is derived by discretisation of the aquifer boundaries and mathematical raster rendering processes within a GIS environment. The physical properties of alluvial aquifers – their hydraulic properties, conductivity and effective porosity – are estimated based on a combination of field data and previous sedimentological studies. Available stratigraphic classifications are standardized and linked to databases of granulometric studies and respective hydraulic properties in arid alluvial bodies.

 

Socio-economic Characterisation

To evaluate the socio-economic importance of alluvial aquifers in terms of the available water resources within the study catchments. Spatial and temporal patterns of water consumption will be evaluated for the study catchments based on a socio-anthropological approach and working closely with the WADE end-users.