Water resources - Availability - Northern Territory
Northern Territory
Northern Territory Overview
With a comparatively small population base and low intensity of land use, there has been relatively little pressure on the Northern Territory's (NT) water resources to date. This, however, is changing, and increasingly the NT's largely intact water resources are becoming subject, generally locally, to a complex range of needs and demands.
As demand on the NT's water resources grows, along with increased awareness in the community of environmental issues, so to do the demands on assessment, planning and sustainable development of the water resources. The NT has an extreme range of climatic zones, limited data across most areas and a resource knowledge base limited to areas of current demand. Much assessment work is still required to better understand issues like environmental flow requirements and surface water - groundwater interaction in order to enable effective management of the water resources.
Surface Water Reporting Units
Forty Surface Water Management Areas (SWMAs) have been defined, and 38 of them are same as the respective basins designated by the Agriculture and Resource Management Council of Australia and New Zealand (ARMCANZ) within NT, and are shown in Figure 1. This includes nine management areas (001.NT, 005.NT, 007.NT, 023.NT, 026.NT, 809.NT, 810.NT, 910.NT and 912.NT) which represents the NT portion of the respective basins. The Finniss River basin has been further subdivided to distinguish between developed and undeveloped river systems.
Groundwater Reporting Units
Groundwater information has been reported at two levels - Groundwater Management Units (GMUs) and Unincorporated Areas (UAs). Eight GMUs have been reported and these are selected major aquifer systems within gazetted Water Control Districts. The UAs comprise the majority of the NT and these are classified according to Groundwater Sub-Province (major aquifer) and typical bore yield. Some 46 Unincorporated Areas have been defined. Both GMUs and UAs are sub-areas of Groundwater Provinces which are the hydrogeological basins within the NT and the unit of reporting for the 85 Review.
For further information, contact the Northern Territory Department of Natural Resources, Environment and The Arts www.nreta.nt.gov.au.
How much surface water does Northern Territory have?
Hydrology
The mean annual flow (MAF) of all NT SWMAs is 75,400 GL. The NT can be considered to have two climatic zones, humid and arid. The boundary of these two zones approximates the catchment boundary of the streams that flow to the north (to the Timor Sea and Gulf of Carpentaria) and the streams that flow to the south (to inland ephemeral lakes and floodouts).
River flows in the humid zone have a distinct seasonal pattern and moderately low year to year variability. About 90% of the average annual discharge occur in the four month period from December to March and mean annual runoff(MAFSWMA /AREASWMA) from SWMAs vary from 70 mm to 470 mm. In the arid zone the yearly variability is high to very high. The mean annual runoff from SWMAs is very small, and varies between 0.1 and 5 mm.
Available Resource
The total annual divertible yield of the 40 SWMAs is approximately 55,900 GL or approximately 74% of the total mean annual flow. It should be noted that divertible Yield was based on median annual flow, which is generally lower than the mean annual flow. The remaining 26%, has limited development potential due to salinity (tidal) or environmental flow requirements for National Parks (eg. SWMAs 819, 820 and 821). Quoted annual divertible yield does not account for environmental water requirements outside National Parks.
Sustainable yield is defined as the maximum volume of water that can be diverted after taking account of all environmental water requirements. In the NT this requirement has been set, for the interim, at 80% of the Divertible Yield in the humid zone, and 95% in the arid zone. The total sustainable yield is approximately 11,100,000 ML or approximately 15% of the total mean annual flow.
The SWMA with the most highly developed surface water resource is 815.A (Darwin / Blackmore Rivers), with a developed yield of 38.2 GL. This represents about 72% of the total developed yield in the NT.
| Basin/Surface Water Management Area | Mean Annual Run-off (GL/yr) | % of state | Natural mean annual out-flow (GL/yr) | In-flow (GL/yr) |
|---|---|---|---|---|
| Adelaide River | 1,880 | 2.49 | 1,880 | 0 |
| Barkly | 600 | .8 | 0 | 0 |
| Bathurst and Melville Islands | 3,100 | 4.11 | 3,100 | 0 |
| Blyth River | 1,840 | 2.44 | 1,840 | 0 |
| Buckingham River | 2,800 | 3.71 | 2,800 | 0 |
| Burt | 20 | .03 | 0 | 0 |
| Calvert River | 940 | 1.25 | 940 | 0 |
| Daly River | 6,740 | 8.94 | 6,740 | 0 |
| Darwin / Blackmore Rivers | 440 | .58 | 340 | 0 |
| East Alligator River | 6,870 | 9.11 | 6,870 | 0 |
| Finke River (NT) | 164 | .22 | no data | 0 |
| Finniss / Elizabeth / Howard Rivers | 2,680 | 3.55 | 2,680 | 0 |
| Fitzmaurice River | 1,500 | 1.99 | 1,500 | 0 |
| Georgina River (NT) | 2,487 | 3.3 | 2,487 | 0 |
| Goomadeer River | 1,300 | 1.72 | 1,300 | 0 |
| Goyder River | 1,685 | 2.23 | 1,685 | 0 |
| Groote Eylandt | 680 | .9 | 680 | 0 |
| Hay River (NT) | 146 | .19 | no data | 0 |
| Keep River (NT) | 510 | .68 | 720 | 210 |
| Koolatong River | 1,760 | 2.33 | 1,760 | 0 |
| Limmen Bight River | 1,570 | 2.08 | 1,570 | 0 |
| Liverpool River | 4,260 | 5.65 | 4,260 | 0 |
| Mackay (NT) | 22 | .03 | 0 | 0 |
| Mary River | 2,180 | 2.89 | 2,180 | 0 |
| McArthur River | 3,270 | 4.34 | 3,270 | 0 |
| Moyle River | 600 | .8 | 600 | 0 |
| Nicholson River (NT) | 674 | .89 | 674 | 0 |
| Ord River (NT) | 830 | 1.1 | 830 | 0 |
| Robinson River | 960 | 1.27 | 960 | 0 |
| Roper River | 5,540 | 7.34 | 5,540 | 0 |
| Rosie River | 500 | .66 | 500 | 0 |
| Settlement Creek (NT) | 830 | 1.1 | 830 | 0 |
| South Alligator River | 5,750 | 7.62 | 5,750 | 0 |
| Todd River | 86 | .11 | 0 | 0 |
| Towns River | 540 | .72 | 540 | 0 |
| Victoria River | 4,540 | 6.02 | 4,540 | 0 |
| Walker River | 3,500 | 4.64 | 3,500 | 0 |
| Warburton (NT) | no data | no data | 0 | |
| Wildman River | 815 | 1.08 | 815 | 0 |
| Wiso | 820 | 1.09 | 0 | 0 |
How saline are Northern Territory's surface water resources?
Table: Surface water resource by salinity class for divertible yield (GL)
| Surface Water Managemnet Area | <500 mg/l (GL/yr) | 500 - 1500 mg/l (GL/yr) | 1500 - 5000 mg/l (GL/yr) | 5000 -14000 mg/l (GL/yr) | >14000 mg/l (GL/yr) | Total volume (GL/yr) |
|---|---|---|---|---|---|---|
| Northern Territory | 111,827 | no data | no data | no data | no data | no data |
| Adelaide River | 2,960 | no data | no data | no data | no data | 1,480 |
| Barkly | 1,200 | no data | no data | no data | no data | 600 |
| Bathurst and Melville Islands | 5,400 | no data | no data | no data | no data | 2,700 |
| Blyth River | 2,600 | no data | no data | no data | no data | 1,300 |
| Buckingham River | 4,400 | no data | no data | no data | no data | 2,200 |
| Burt | 39 | no data | no data | no data | no data | 20 |
| Calvert River | 1,780 | no data | no data | no data | no data | 890 |
| Daly River | 11,120 | no data | no data | no data | no data | 5,560 |
| Darwin / Blackmore Rivers | 704 | no data | no data | no data | no data | 352 |
| East Alligator River | 5,720 | no data | no data | no data | no data | 2,860 |
| Finke River (NT) | 328 | no data | no data | no data | no data | 164 |
| Finniss / Elizabeth / Howard Rivers | 4,800 | no data | no data | no data | no data | 2,400 |
| Fitzmaurice River | 2,840 | no data | no data | no data | no data | 1,420 |
| Georgina River (NT) | 4,974 | no data | no data | no data | no data | 2,487 |
| Goomadeer River | 2,300 | no data | no data | no data | no data | 1,150 |
| Goyder River | 3,028 | no data | no data | no data | no data | 1,514 |
| Groote Eylandt | 1,300 | no data | no data | no data | no data | 650 |
| Hay River (NT) | 292 | no data | no data | no data | no data | 146 |
| Keep River (NT) | 780 | no data | no data | no data | no data | 390 |
| Koolatong River | 3,160 | no data | no data | no data | no data | 1,580 |
| Limmen Bight River | 2,980 | no data | no data | no data | no data | 1,490 |
| Liverpool River | 5,680 | no data | no data | no data | no data | 2,840 |
| Mackay (NT) | 44 | no data | no data | no data | no data | 22 |
| Mary River | 3,880 | no data | no data | no data | no data | 1,940 |
| McArthur River | 6,340 | no data | no data | no data | no data | 3,170 |
| Moyle River | 1,080 | no data | no data | no data | no data | 540 |
| Nicholson River (NT) | 1,348 | no data | no data | no data | no data | 674 |
| Ord River (NT) | 1,660 | no data | no data | no data | no data | 830 |
| Robinson River | 1,800 | no data | no data | no data | no data | 900 |
| Roper River | 9,560 | no data | no data | no data | no data | 4,780 |
| Rosie River | 900 | no data | no data | no data | no data | 450 |
| Settlement Creek (NT) | 1,620 | no data | no data | no data | no data | 810 |
| South Alligator River | no data | no data | no data | no data | no data | no data |
| Todd River | 172 | no data | no data | no data | no data | 86 |
| Towns River | 1,020 | no data | no data | no data | no data | 510 |
| Victoria River | 5,600 | no data | no data | no data | no data | 2,800 |
| Walker River | 6,600 | no data | no data | no data | no data | 3,300 |
| Warburton (NT) | no data | no data | no data | no data | no data | no data |
| Wildman River | 178 | no data | no data | no data | no data | 89 |
| Wiso | 1,640 | no data | no data | no data | no data | 820 |
How much of Northern Territory's surface water resource has been developed?
Currently only two major water-supply systems use surface water in the NT. Darwin is supplied from Darwin River Dam (259 GL capacity). The town of Katherine is supplied from a weir on Katherine River.
How committed are Northern Territory's surface water resources?
All the Surface Water Management Areas are in development category 1, except for the Darwin / Blackmore River Management Area (815.A), which is in category 2. There are no over-developed management areas in the Territory. About 99% of the sustainable yield is undeveloped.
| Basin/SWMA | Volume diverted (GL/yr) | Sustainable (GL/yr) | Diversion Development class |
|---|---|---|---|
| Adelaide River | 2 | 290 | LOW DEVELOPMENT |
| Barkly | 1 | 30 | LOW DEVELOPMENT |
| Bathurst and Melville Islands | 1 | 588 | LOW DEVELOPMENT |
| Blyth River | 0 | 220 | LOW DEVELOPMENT |
| Buckingham River | 0 | 440 | LOW DEVELOPMENT |
| Burt | 1 | 4 | LOW DEVELOPMENT |
| Calvert River | 1 | 180 | LOW DEVELOPMENT |
| Daly River | 8 | 1,110 | LOW DEVELOPMENT |
| Darwin / Blackmore Rivers | 36 | 70 | MEDIUM DEVELOPMENT |
| East Alligator River | 0 | 900 | LOW DEVELOPMENT |
| Finke River (NT) | 1 | 8 | LOW DEVELOPMENT |
| Finniss / Elizabeth / Howard Rivers | 1 | 480 | LOW DEVELOPMENT |
| Fitzmaurice River | 1 | 280 | LOW DEVELOPMENT |
| Georgina River (NT) | 1 | 125 | LOW DEVELOPMENT |
| Goomadeer River | 0 | 490 | LOW DEVELOPMENT |
| Goyder River | 0 | 303 | LOW DEVELOPMENT |
| Groote Eylandt | 3 | 130 | LOW DEVELOPMENT |
| Hay River (NT) | 1 | 7 | LOW DEVELOPMENT |
| Keep River (NT) | 1 | 78 | LOW DEVELOPMENT |
| Koolatong River | 0 | 310 | LOW DEVELOPMENT |
| Limmen Bight River | 1 | 300 | LOW DEVELOPMENT |
| Liverpool River | 0 | 570 | LOW DEVELOPMENT |
| Mackay (NT) | 1 | 2 | LOW DEVELOPMENT |
| Mary River | 1 | 400 | LOW DEVELOPMENT |
| McArthur River | 1 | 630 | LOW DEVELOPMENT |
| Moyle River | 0 | 110 | LOW DEVELOPMENT |
| Nicholson River (NT) | 1 | 134 | LOW DEVELOPMENT |
| Ord River (NT) | 1 | 166 | LOW DEVELOPMENT |
| Robinson River | 1 | 180 | LOW DEVELOPMENT |
| Roper River | 1 | 950 | LOW DEVELOPMENT |
| Rosie River | 1 | 90 | LOW DEVELOPMENT |
| Settlement Creek (NT) | 1 | 160 | LOW DEVELOPMENT |
| South Alligator River | 0 | no data | LOW DEVELOPMENT |
| Todd River | 1 | 4 | LOW DEVELOPMENT |
| Towns River | 0 | 100 | LOW DEVELOPMENT |
| Victoria River | 2 | 560 | LOW DEVELOPMENT |
| Walker River | 0 | 660 | LOW DEVELOPMENT |
| Warburton (NT) | 0 | no data | LOW DEVELOPMENT |
| Wildman River | 0 | 60 | LOW DEVELOPMENT |
| Wiso | 1 | 40 | LOW DEVELOPMENT |
The volume diverted is the total volume of the SWMA's surface water resources diverted for use both within the management area and for export to other management areas.
A four-class classification system was developed to provide a simple method to communicate the status of the use and allocation of Australia's water resources in relation to sustainable water management.
It is important to recognise that adequately quantifying a sustainable flow regime or sustainable yield and consequent operating rules is a complex matter. State, Territory and scientific agencies continue to develop and apply methods and measures for determining sustainable flow regimes and sustainable yields.
This categorisation provides a general guide only. Please refer to the State and Territory Overview and Technical reports for detail on the analysis methods used.
| Category | Development status | |
|---|---|---|
| 1 | <30% | Low development |
| 2 | 30 - 70% | Moderate development |
| 3 | 70 - 100% | Highly developed |
| 4 | 100% | Overdeveloped |
* Water use as a percentage of sustainable flow regime (surface water) and sustainable yield (groundwater)
How much groundwater does Northern Territory have?
Hydrology
The principal groundwater resources in the NT are contained in fractured rock aquifers of Palaeozoic and Pre Cambrian age and porous Tertiary/Cretaceous sediments. Bore yields are typically less than 2 L/s but higher yields occur in several provinces. Of note in this regard are the widespread fractured and cavernous Cambrian limestones of the Daly, Wiso and Georgina Basins and the porous and fractured Palaeozoic sandstones of the Amadeus Basin.
Recharge is generally related to the north to south rainfall distribution across the NT. In the higher rainfall areas of the north (>800mm/year), recharge is relatively high and occurs regularly each year. In the low rainfall areas of the south recharge are very low and occur infrequently. This is obviously the major influence on reliability and long term sustainability of groundwater supplies.
Available Resources
The available groundwater resource is defined to be the amount of groundwater that is renewable or recharging the systems. Across the different aquifer systems of the NT this volume totals approximately 13,000 GL annually.
Generally to determine aquifer recharge, the NT was subdivided into 4 zones based on the likely dominant mechanism of recharge.
Recharge Zone 1 was considered to have distributed recharge over the catchment. Recharge Zone 2 - recharge from upper catchment rivers and creeks with some distributed recharge over parts of the catchment. Recharge Zone 3 - recharge from ephemeral lakes, floodouts, creeks and rivers. Recharge Zone 4 - recharge from floodouts, creeks and rivers.
Within the zones the probable recharge rates (ML/Ha/year) ranged from 0.2 to 5 ML/Ha/year in the northern most zone to 0.02 to 2.5 ML/Ha/year in the southern most zone. The range of recharge mechanisms and rates combine to reflect relatively higher annual recharge in the north to lower and infrequent recharge in the south. The rate applied to the GMUs and UAs was based upon the level of understanding of the GMU/UA.
An estimate of the percentage of the total GMU/UA area that receives recharge was also made again based on the level of understanding of the GMU/UA. The annual GMU/UA groundwater recharge volume, or available groundwater resource, was determined by multiplying the probable recharge rate by the estimated recharge area.
The areas of greatest potential for use, if considered only with respect to the amount of available groundwater, are those with the highest estimated recharge rates. These areas are naturally in the northern most part of the NT where the rainfall is highest and where the rock types are favourable for recharge. They include limestone aquifers of the Pine Creek Groundwater Province, the Daly River Groundwater Province and the McArthur Groundwater Province and sedimentary aquifers of the McArthur Groundwater Province , the Melville Groundwater Province , the Bonaparte Groundwater Province , the Pine Creek Groundwater Province and the Arafura Groundwater Province.
Across the NT the average depth to the aquifer varies from 5 to 80m. Predominantly across the northern region the depth is less than 20m. In the Wiso, Amadeus, Ngalia, Georgina and Great Artesian Groundwater Provinces, which comprise approximately 30% of the NT, the depth is greater than 50m. Through the west-southwest of the NT the depth is predominantly between 20 and 50m. No relationship exists between the depth to the aquifer and the usage of groundwater because most groundwater is used for public or pastoral water supplies.
Sustainable Yield and Environmental Allocation
In the humid zone, the Sustainable Yield is estimated as 20% of the Divertible Yield, and in the arid zone it is estimated as 5%.
The sustainable yield of an aquifer system in the NT for the Audit has been defined by DLPE as 50% of the average annual aquifer recharge. Effectively this is stating that of the available groundwater resources, 50% is required to be allocated to sustain groundwater dependent ecosystems. The sustainable yield of the NT's groundwater resources is approximately 6,500 GL/year. Considering the annual use of groundwater, approximately 2% of the sustainable yield is being utilised.
Currently, without further scientific knowledge, the groundwater requirements of the environment can not be determined with greater confidence or accuracy. To narrow this gap in knowledge, the NT is undertaking 5 projects as part of the National River Health Program - Environmental Flows Initiative. The details of these projects are mentioned in the Environmental Water Requirements section.
How committed are Northern Territory's groundwater resources?
Table: Allocation volumes (GL/yr in each development category)
Note: "GMU"=Groundwater Management Unit "UA"=Unallocated Area
| Province | Over | High | Med | Low | Total (GL/yr) | |
|---|---|---|---|---|---|---|
| Amadeus | GMU | 14 | no data | no data | 0 | 14 |
| UA | no data | no data | no data | 2 | 2 | |
| Arafura | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | no data | 1 | 1 | |
| Arunta | GMU | 1 | 4 | no data | 0 | 5 |
| UA | no data | no data | no data | 3 | 3 | |
| Bonaparte | GMU | no data | no data | no data | 2 | 2 |
| UA | no data | no data | no data | 1 | 1 | |
| Daly River | GMU | no data | no data | no data | 1 | 1 |
| UA | no data | no data | no data | 1 | 1 | |
| Georgina | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | no data | 9 | 9 | |
| Great Artesian | GMU | 919 | 2 | 9 | 1 | 1,017 |
| UA | no data | no data | no data | no data | no data | |
| Halls Creek | GMU | no data | no data | no data | 7 | 7 |
| UA | no data | no data | no data | no data | 0 | |
| Mcarthur | GMU | no data | 12 | no data | no data | 12 |
| UA | no data | no data | no data | 2 | 2 | |
| Melville | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | no data | no data | 0 | |
| Musgrave | GMU | no data | no data | no data | 0 | 0 |
| UA | no data | no data | no data | 1 | 1 | |
| Ngalia | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | no data | 1 | 1 | |
| Ord-Victoria | GMU | no data | no data | no data | 0 | 0 |
| UA | no data | no data | no data | 6 | 6 | |
| Pine Creek | GMU | no data | no data | no data | 12 | 12 |
| UA | no data | no data | no data | 5 | 5 | |
| Tanami | GMU | no data | no data | no data | 0 | 0 |
| UA | no data | no data | no data | 1 | 1 | |
| Tennant Creek | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | no data | 1 | 1 | |
| Wiso | GMU | no data | no data | 3 | no data | 3 |
| UA | no data | no data | no data | 2 | 2 |
A four-class classification system was developed to provide a simple method to communicate the status of the use and allocation of Australia's water resources in relation to sustainable water management.
It is important to recognise that adequately quantifying a sustainable flow regime or sustainable yield and consequent operating rules is a complex matter. State, Territory and scientific agencies continue to develop and apply methods and measures for determining sustainable flow regimes and sustainable yields.
This categorisation provides a general guide only. Please refer to the State and Territory Overview and Technical reports for detail on the analysis methods used.
| Category | Development status | |
| 1 | <30% | Low development |
| 2 | 30 - 70% | Moderate development |
| 3 | 70 - 100% | Highly developed |
| 4 | 100% | Overdeveloped |
Table: Groundwater resource by salinity class
| Province | <1500 mg/l (GL/yr) | 5000 mg/l (GL/yr) | 14000 mg/l (GL/yr) | >14000 mg/l (GL/yr) | Total volume (GL/yr) | |
|---|---|---|---|---|---|---|
| Northern Territory | GMU | 105173 | 9818 | 820 | 84254 | |
| UA | 5691918 | 176759 | 324135 | 140709 | 2009369 | |
| Amadeus | GMU | 13,848 | no data | 30 | no data | no data |
| UA | no data | no data | 79 | 20 | no data | |
| Arafura | GMU | no data | no data | no data | no data | no data |
| UA | 121 | no data | no data | no data | no data | |
| Arunta | GMU | no data | 5 | 11 | no data | no data |
| UA | no data | no data | 28 | 117 | no data | |
| Bonaparte | GMU | no data | no data | 123 | no data | no data |
| UA | 1,140 | no data | no data | 2 | no data | |
| Daly River | GMU | 27,053 | no data | no data | no data | no data |
| UA | 623 | no data | no data | no data | no data | |
| Georgina | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | 172 | no data | no data | |
| Great Artesian | GMU | 187,400 | 327 | 90 | 41 | 30 |
| UA | no data | no data | no data | no data | no data | |
| Halls Creek | GMU | no data | 218 | no data | no data | no data |
| UA | no data | 1 | no data | no data | no data | |
| Mcarthur | GMU | 12,150 | no data | no data | no data | no data |
| UA | 2,349 | no data | no data | no data | no data | |
| Melville | GMU | no data | no data | no data | no data | no data |
| UA | 246 | no data | no data | no data | no data | |
| Musgrave | GMU | no data | no data | 1 | 39 | no data |
| UA | no data | no data | 25 | no data | no data | |
| Ngalia | GMU | no data | no data | no data | no data | no data |
| UA | no data | no data | 8 | 4 | no data | |
| Ord-Victoria | GMU | no data | 102 | 91 | no data | no data |
| UA | 351 | 19 | no data | no data | no data | |
| Pine Creek | GMU | 52,122 | no data | no data | no data | no data |
| UA | 866 | no data | no data | no data | 6 | |
| Tanami | GMU | no data | no data | 25 | no data | 95 |
| UA | no data | 19 | 15 | no data | no data | |
| Tennant Creek | GMU | no data | no data | no data | no data | no data |
| UA | no data | 29 | no data | no data | no data | |
| Wiso | GMU | no data | 6 | no data | no data | no data |
| UA | no data | 111 | no data | no data | no data |
How much water does Northern Territory trade?
The Total reported Volume Traded in Northern Territory is 0 GL; in 0 transactions.
The State and Territory water management agencies continue to consider water use efficiency and optimisation strategies within existing infrastructure (e.g. water supply efficiency, precision irrigation and scheduling, water recycling, trading and pricing) as part of water resource development planning.
Recognising that water is a finite resource, the States and Territories have developed water allocation systems where security and reliability are assigned to entitlement, trading is provided so water can be moved to high value uses and the choices of individuals are maximised.
Part of the decision-making framework to enable and facilitate water trading, changes in water allocation and definition of rights to water is the need for water use monitoring. Water use monitoring will assist decision-making and provide an opportunity over time to evaluate the effectiveness of allocation policies.
Environmental water requirements
In the absence of rigorous scientific assessment basis, environmental flow requirement is assumed to be 80% of the Divertible Yield (median annual flow) in the Humid Zone and 95% in the Arid Zone.
Catchment wide management decisions impacting on flow regimes can lead to unintended consequences for the environment. The provision of water for existing and potential water resource demands, both surface and groundwater, and associated infrastructure should be implemented in a manner consistent with nationally agreed policy frameworks relating to the ecologically sustainable management of water resources.
Underpinning ecologically sustainable management is scientific knowledge on water requirements of ecosystems (ie timing, quantity and quality). Across the humid, arid and semi-arid regions of the NT the paucity of scientific knowledge on water requirements of ecosystems is acknowledged.
As part of the National River Health Program - Environmental Flows Initiative, the NT is undertaking 5 projects to assist in the establishment of environmental flow requirements for aquatic ecosystems (including flood plains and ecosystems). These projects are concentrated in the Daly River Basin and their title and aims are detailed below:
Modelling Dry-season Flows and Predicting the Impact of Water Extraction on a Flagship Species
The aim of this project is to provide recommendations on environmental flows consistent with maintaining the biota of the Daly River, given the competing demands of agriculture, recreation and tourism, conservation and Aboriginal culture.
Inventory and Risk Assessment of Water Dependent Ecosystems in the Daly Basin
The aim of this project is to provide a mapping-base for further assessment of water-dependent ecosystems in the Daly basin. This will be done through remote sensing and GIS and will allow overlaying of further information sets, such as land use and water management structures that may affect the water dependent ecosystems. Threats to these ecosystems from forecast and existing water use and land management practices will be established and those ecosystems most at risk will be identified.
Environmental Flow Requirements of Vallisneria nana
This project will map the distribution, dimensions and performance of key habitat patches of Vallisneria nana and record and analyse associated hydraulic parameters. The habitat preferences of Vallisneria and dependent macroinvertebrate fauna will allow predictions of the response of these species to altered flow. Importantly, the interaction between these two ecological components will be investigated as part of furthering environmental flow assessment methods and understanding of the requirements of different biota.
Water requirements for riparian vegetation
Effect of reduced dry season flow on phytoplankton and periphyton
For the Daly catchment, the projects will develop information to increase the understanding of the need to maintain environmental flows and for a rational basis for the determination of sustainable water use, considering all commercial and non-commercial values of the region. This will include a well-supported example of the consequential effects of flow alteration on the biology of a key element of the Daly River's fauna.
At the NT level, the project outcomes will assist to improve the scientific basis for decisions underpinning the move to sustainable management of water resources under the principles set out by the COAG Water Reform Framework, National Principles for the Provision of Water for Ecosystems (ARMCANZ and the Australian and New Zealand Environment Conservation Council) and the National River Health Program Strategy - Environmental Flows Initiative.
Further information
- Northern Territory Water Resources Assessment 2000 Report
- Northern Territory Water Resources Assessment 2000 Technical Report
- report from the study of Streamflow data and modelled streamflow
- Link to data available for download on the:
- extension of unimpaired monthly streamflow data and regionalisation of parameter values to estimate streamflow in ungauged catchments (NLWRA 2000)
- Surface Water Management Areas
- Groundwater management units and provinces - ARC/INFO export
- Link to the Map Maker to make a map using this information.
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