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GEOMORPHOLOGY REPORT - CRC LEME

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Question 3: Understanding of the drivers of floodplain health with respect to groundwater<br />

processes<br />

The combined LIDAR and SPOT/ASTER interpretation assisted in mapping floodplain health<br />

and allowed prediction of the geomorphic, soil, and sedimentologic parameters influencing<br />

associated with salt stores and recharge, important to the health of floodplain vegetation.<br />

Integrated products relating to floodplain health are found in the GIS and Atlas and include<br />

the Conductive Groundwater, Conductive Soils, Surface Salinity, Salinity Hazard, and Salt<br />

Store maps.<br />

Question 4: Identification of the high recharge areas in the floodplain?<br />

ASTER and LIDAR interpretation we predict will identify potential areas on the basis of<br />

abandoned or stagnant river channels or scroll bars lacking an impermeable clay drape. These<br />

will need to be field verified, however, especially as stagnant or abandoned channels may<br />

well have their bottoms sealed by clay. This would leave only the youngest meander scroll<br />

bars which lack the pervasive clay drape, or where the clay drape is very thin, as areas of high<br />

potential recharge on the floodplain. Mapping surface recharge are found in the GIS and<br />

Atlas include the Flush Zone Thickness, Flush Zone Conductivities, Extent of Flush Zones,<br />

and Groundwater Recharge maps.<br />

Question 5: What is the extent and thickness of the Blanchetown Clay and the Coonambidgal<br />

Formation?<br />

We can’t answer this question in this area from surface exposures as imaged by satellites or<br />

scanned to form DEMS. Nor are they visible in preliminary field observations. We regard<br />

this question as answerable only through a combination of AEM and bore hole data, as<br />

showing the Thickness of Quaternary Alluvium, Extent of Quaternary Alluvium, and Depth<br />

to Top of Blanchetown Clay maps in the GIS and Atlas.<br />

Question 6: Where is salt stored in the unsaturated zone?<br />

We predict that contextualised analysis of surface soil samples will help identify these areas<br />

of salt storage, backed up by analysis of shallow (above the water table) borehole samples.<br />

integrated products relating to salt stores Conductive Groundwater, Conductive Soils, Surface<br />

Salinity, Salinity Hazard, and Salt Store maps in the GIS and Atlas.<br />

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