Australian Natural Resources Atlas

Groundwater Management Unit

Location map of Bungaree

Groundwater Management Unit: Bungaree

Introduction

The groundwater resource characteristics for the Bungaree groundwater managment unit are presented below. This includes technical detail on aquifer properties and water level change for key monitoring bores.

What is the character of Bungaree's groundwater resource?

Vital Statistics:

Area200 km2
Total Water Allocated5,870 ML/yr
Total Water Used3,325 ML/yr
Average Salinity640 mg/L
Sustainable Yield4,400 ML/yr
Depth to top of aquifer5 m

Unconfined fractured Newer Volcanics basalt aquifer. Need explanation of fracture flow and anisotropy

Method used for determining sustainable yield:

The PAV developed for the Bungaree GMA has been estimated at 4,436 ML/year. This figure has been calculated using the rainfall recharge method with limited information and has low confidence limits.

Comparison of a number of aquifer recharge determination methods were used to calculate this figure. The Bungaree GMA has shown considerable variation between these methods. The method of rainfall infiltration was favoured over hydrograph fluctuation as the availability of water level data for analysis was very poor.

Discharge at the margins of the lava flows to the underlying Tertiary sediments and basement rock, as well as to streams, springs and lakes was considered.

It should be noted that the PAV specified above applies to a large area and localised intensive extraction is likely to cause local interference effects between bores through local drawdown in water level.

Assumptions used for allocating development categories:

Groundwater categorisation was assessed in terms of the requirements of the audit documentation. Information applied to the categorisation of both abstractions and allocations was based on the best information available from a combination of information supplied by the responsible Rural Water Authority and information from the Groundwater Database.

Forward projections of abstraction were based on a combined surface and groundwater demand evaluation model. This model projected potential demand for water based on predictions of population growth, industry development, agricultural development and water consumption trends.

Are groundwater levels changing?

Technical information on the key groundwater bores and monitoring stations is presented below, including hydrographs where available. Link to a discussion on groundwater levels and trends at a State level as it relates to dryland salinity.

Bore IDStart recordEnd recordDepth of bore (m)Reduced level (m)
VIC11933026-Oct-9423-Sep-9930523
VIC11933726-Oct-9423-Sep-9966378
VIC11934126-Oct-9424-Sep-9980597

The following groundwater management units also occur in Lachlan Province:

Further information

Key

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