Water resources - Management and Development - Queensland
Groundwater Management Unit: Unincorporated Area - Clarence Moreton
Introduction
Management Context:
Performance of bores is directly related to recharge to aquifers from rainfall and streambed infiltration which are determined by seasonal conditions. Hence, during drought conditions water levels in bores can drop up to 15 m significantly affecting bore performance.
Priority issues
Declining Water Levels | YES |
Salt Water Intrusion | NO |
SALINISATION |
|
Dryland | NO |
Irrigation | NO |
Groundwater | NO |
Surface Water | NO |
Urban | NO |
Point Source Pollution | NO |
Diffuse Source Pollution | NO |
Subsidence | NO |
Artificial Recharge (ML/yr) | no data |
Ecosystems Protection | NO |
Surface Water Interaction | NO |
Management Plans | NO |
Defined Minimum Water Level | NO |
Comment: Groundwater levels are highly susceptible to local climate and are currently recovering from a long term decline in response to below average rainfall and increased use.
Comments on Management Responses
2020 Management Response:
No forecast use estimate is reported for the Clarence Moreton Unincorporated Area in 2020.
2050 Management Response:
No forecast use estimate is reported for the Clarence Moreton Unincorporated Area in 2050.
See QLD Water Resources Assessment 2000 Technical Report for a review of management responses.
Assessment of monitoring in Unincorporated Area - Clarence Moreton
Efficacy of the network:
The Clarence Moreton UA contains no formal monitoring network and has general reported information for the majority of the catchments within the area.
Data management requirements:
Queensland groundwater monitoring data, including water level and water quality, is stored within the Groundwater Database (GWDB) system. The new GWDB system uses web technology and is available through the department's intranet.
Allocation and use data is obtained through the Water Entitlements Registration Database (WERD) which is an electronic database for water licences. However the GMU has no groundwater allocations.
Both databases are managed locally at district level, with respect to the collection and entering of water monitoring, allocation and use data; and are accessed statewide.
Protective management:
Over exploitation of small fractured rock aquifers is a concern to local users. These often recharge vertically and replenish quickly during good rainfall events. Reduction in availability seems to be seasonal, and can therefore be anticipated.
Options for monitoring:
No options for Commonwealth, State, industry or community groups to address data gaps are identified or reported for the Clarence Moreton Unincorporated Area.
See QLD Water Resources Assessment 2000 Technical Report for a review of monitoring.
What is the estimated demand for groundwater?
| Sustainable Yield | |
|---|---|
Comment about sustainable yield figure: | No global sustainable yield has been assessed for the Clarence Moreton UA. Estimated yields for several areas and aquifer types indicate that there is at least 79000 Ml/yr available from aquifer exclusively within the UA area. This figure comprises 43000 Ml/yr from alluvial aquifers in the east of the UA; and about 36000 Ml/yr from basalt and sandstone aquifers in the west of the UA. |
Sustainable yield: | ML/yr |
Threshold year for sustainable year: | no data |
Abstraction Volume 1996/1997: | 50,000 ML |
Current Resource development categorisation: |
|
| Estimated Use in 2020 | |
|---|---|
Comment: |
|
Estimated use in 2020: | 79,000 ML |
% change from 1996/1997: | 58 |
Resource development categorisation: |
|
| Estimated in 2050 | |
|---|---|
Comment: |
|
Estimated use in 2050: | no data ML |
% change from 1996/1997: | no data |
Resource development categorisation: |
|
What assumptions were used in this assessment
Development Potential:
Groundwater in the Clarence Moreton Unincorporated Area aquifers is utilised mostly for stock, irrigation and private domestic farm supply. Current demand is not anticipated to increase significantly before the year 2020 but is difficult to gauge without knowledge of a regional sustainable yield and current and historical groundwater use data.
Estimate of Use:
No forecast use estimates are reported for the Clarence Moreton Unincorporated Area.
Data Availability,Gaps and Recommendations
Data Availablility:
Data on the Clarence Moreton UA groundwater resources is limited outside of company and investigative reports. Salinity data is available for over 2800 bores within the UA but ranges significantly in age rendering much of the data out of date. There are groundwater allocations for bores within the Eastern Downs Declared Sub-Artesian Area in the far west of the UA and there is no groundwater metering.
Current Gaps and Recommendations:
Data Gaps: There is no bore network dedicated to monitoring the regional groundwater resources of the Clarence Moreton UA. Although 153 Monitoring Network Bores are exclusively within the UA area their purpose is aimed at monitoring the basalt outside of the GMU resources and local alluvial groundwater resources. The UA is also without regional groundwater level data, quantification of the resource and groundwater abstraction data.
Recommendations: As a low priority area there are no recommendations made to address data gaps. Local town and shire council groups should continue monitoring groundwater in their respective areas within the Clarence Moreton UA.
Future Gaps:
There is no bore network dedicated to monitoring the regional groundwater resources of the Clarence Moreton UA. Although the UA is without groundwater level data, assessment of aquifer properties, quantification of the resource and groundwater abstraction data, there is no strategy to establish monitoring to assess these.
Further information
- The following groundwater management units also occur in Clarence-Morton Province.
- Alstonville Basalt (NSW)
- Central Lockyer Valley (QLD)
- Condamine - Condamine Groundwater Management Area Sub-Area 4 (QLD)
- Condamine River Alluvium (Cunningham to Ellangowan) (QLD)
- Condamine River Alluvium (Killarney to Murrays Bridge) (QLD)
- Condamine River Alluvium (Murrays Bridge to Cunningham) (QLD)
- Dalrymple Creek Alluvium (QLD)
- Flagstone Creek (QLD)
- Glengallan Creek (QLD)
- Kings Creek Alluvium (QLD)
- Laidley Creek (Upper Reach) (QLD)
- Lockyer - Helidon (QLD)
- Logan / Albert Rivers (QLD)
- Lower Lockyer Creek (QLD)
- Lower Oakey Creek Alluvium (QLD)
- Ma Ma Creek (QLD)
- Myall / Moola Creek North (QLD)
- Myall Creek (QLD)
- Nobby Basalts (QLD)
- North Coast Fractured Rocks (NSW)
- Oakey Creek Management Area (QLD)
- Richmond Coastal Sands (NSW)
- Richmond River Alluvium (NSW)
- Sandy Creek (QLD)
- Swan Creek Alluvium (QLD)
- Tenthill Creek (QLD)
- Toowoomba City Basalt (QLD)
- Unincorporated Area - Clarence-Morton Basin (NSW)
- Upper Hodgson Creek (QLD)
- Upper Lockyer Creek (QLD)
- Queensland Water Resources Assessment 2000 Report
- Queensland Water Resources Assessment 2000 Technical Report
- For more information about water and other natural resource issues link to www.nrm.qld.gov.au.
- Link to data available for download on the Groundwater management units and provinces - ARC/INFO export
- Link to Map maker to make a map using this information.
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