The Arckaringa subregion of the Lake Eyre Basin bioregion is located in northern SA and contains the majority of the Neales-Peake catchment. It also intersects the southernmost watercourse in the Macumba catchment, Woolridge Creek. As only the most upstream 38 km of Woolridge Creek lies within the boundaries of the Arckaringa subregion and the creek is of low hydrologic significance to the Macumba catchment, rarely connecting to the main drainage lines, it is not considered further in this report. The Macumba catchment is further described in the Pedirka subregion report. The south-east of the Arckaringa subregion also contains much of the Warriner Creek and Margaret Creek subcatchments, though very little is known of these subcatchments and no hydrologic data have been collected. The Arckaringa subregion, Neales-Peake and Macumba catchments are shown in Figure 29.
In recent times, several dedicated data-gathering projects in the Neales-Peake catchment have delivered a 13 year inventory cataloguing data relevant to the persistence of waterholes in the catchment, including water quality, though there is still a pronounced knowledge gap in terms of volumetric data. In spite of the short time scale, missing and unreliable stage data, and lack of flow data, the data collected on the Neales-Peake catchment represent the most comprehensive dataset of all western Lake Eyre Basin river systems.
The waterholes of the Neales-Peake catchment can be divided into those that are saline and flushed only during flow events and those that are mostly fresh and may slowly increase in salinity as they lose water to evaporation and transpiration of local flora in periods of no flow. Found mostly in the upper reaches of the catchment, the mostly fresh waterholes have salinities similar to those of floodwaters (100 to 200 mg/L), which increases to 500 to 1,400 mg/L in periods of little to no flow whereas the predominantly saline waterholes have salinities ranging from 20,000 mg/L at Algebuckina Waterhole to over 250,000 mg/L at Peake Crossing Waterhole. The saline waterholes are found typically in the mid and lower reaches of both rivers.
Although there are no volumetric flow data collected in the Arckaringa subregion, stage data of varying quality and length have been collected for all waterholes over the period 2000 to 2013 for the Neales-Peake catchment. There is little consistency in the data collected across waterholes and no single waterhole has continuous data for that period, however the data collected are invaluable and are currently being used to inform hydrologic modelling that is being undertaken for the region.
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- 1.1.1 Bioregion
- 1.1.2 Geography
- 1.1.3 Geology
- 1.1.4 Hydrogeology and groundwater quality
- 1.1.5 Surface water hydrology and surface water quality
- 1.1.6 Surface water – groundwater interactions
- 1.1.7 Ecology
- Contributors from the Government of South Australia
- Contributors to the Technical Programme
- About this technical product