Australian Natural Resources Atlas

Natural Resource Topics

Water resources - Quality

National overview of surface water quality issues

Deteriorating water quality increases the cost of treating water for domestic and commercial use. It affects industries as diverse as tourism, fishing and agriculture. Ecologically, poor water quality affects the variety and abundance of plant, fish and other animal life in our rivers, wetlands and estuaries.

Management is best based on knowledge of existing water quality. Getting and processing data to define surface water quality issues in Australia has been one of the tasks of the National Land and Water Resources Audit in partnership with the State of the Environment Reporting section of Environment Australia and State and Territory agencies.

Using information supplied by State and Territory Agencies, the Audit has for the first time compiled an Australia wide overview of catchments with major salinity, nutrient, turbidity and acidity / alkalinity water quality problems. Where data was available, assessments of blue-green algal blooms and faecal coliform contamination have also been completed.

Other important surface water quality issues in Australia include toxic chemical and heavy metal pollution, organic carbon loading, oxygen depletion, thermal pollution and biological pathogens. Information on these issues is limited and localised and is not part of this Audit.

The Summary of Surface Water Quality Issues map provides an Australia-wide overview of four water quality variables: turbidity, nutrients (total nitrogen and total phosphorus), salinity and acidity/alkalinity (pH).

These four issues are significant across much of Australia including most of the intensive land use areas. Assessing water quality issues was nevertheless constrained by monitoring coverage in each river basin. For much of Australia there is no water quality monitoring. Water quality monitoring is one input into an overall assessment of Australia's natural resources. Other supporting information is also being drawn from the Audit's assessments of river basin water use, sediment and nutrient exports, estuary and waterway condition.

This assessment is a snapshot based on records of water quality guidelines being exceeded. Of the four major water quality issues, nutrient exceedances affected the greatest number of river basins followed by turbidity, salinity and acidity / alkalinity (pH). Data for trend analyses was limited but where available generally indicated the absence of obvious trends for most basins. In basins where trends were detected, increases in turbidity and total phosphorus, and decreases in pH (increasing acidity) predominated. The trends for total nitrogen and salinity were split, with an approximate equivalent number of basins showing decreases and increases. Some of this variation may be associated with climatic events (high and low rainfall) during the record period. However, dryland and irrigation associated soil salinity, both key contributors to surface water salinity, are expanding, therefore the number of river basins affected by surface water salinity is expected to increase.

Map of surface water quality issues

Turbidity

Findings

Turbidity is a major surface water quality issue in Australia. The affected areas included most inland and lower rainfall basins of the North East drainage division, most of the Murray-Darling drainage division and the more intensively developed basins of the southern South-East Coast drainage division. Turbidity was not an issue in the relatively well vegetated, less developed and higher rainfall coastal basins within the North-East Coast, South-East Coast and South West Coast drainage Divisions,

While constrained by data availability, most observed turbidity trends were of increasing turbidity:

This assessment was constrained by data availability and the monitoring coverage within individual river basins. The ability to assess whether turbidity was associated with extensive land use in the Indian Ocean, Timor Sea, Gulf of Carpentaria and Lake Eyre Drainage Divisions was also prevented by lack of data.

Context

Australia is a dry continent with variable rainfall and stream flow with large areas of highly erodable soil types. These factors often combine to create naturally high levels of turbidity in Australian surface waters. They also make the Australian landscape vulnerable to soil erosion. For this assessment, the Audit used State and Territory based water quality guidelines that reflect to varying degrees, regional distinctions in 'natural' water quality. However, more information on the natural characteristics of river basins may support the establishment of more lenient turbidity guidelines. This would allow for better water quality assessments where soil and flow conditions generate naturally high levels of turbidity.

Impacts

Turbidity affects water clarity and consequently light penetration. This in turn affects ecological processes that depend on sunlight including primary production by aquatic plants and plankton growth. Light penetration also affects the temperature regime of surface waters. Suspended sediments clog gills and filter feeders and smother sedentary aquatic plants, animals and their eggs. In extreme cases, catchment erosion, high turbidity and consequent sedimentation within watercourses can significantly alter the physical habitat of instream environments. This produces shallowing of pools and buries coarse bottom sediments leading to a loss of habitat and spawning sites for gravel bed dependent fish. In an aquatic ecosystem these impacts can generate flow on effects through food chain linkages.

Turbidity generated within a catchment can be exported to estuarine and coastal marine environments. Turbid water exported from catchments during floods has been implicated in the demise of coastal sea grass beds and fringing coral reefs. In addition to impacts associated with reduced water clarity and sediment smothering, turbid water can carry significant amounts of nutrients into estuaries and coastal waters, because nutrients such as phosphorus bind to the suspended soil particles.

Increased turbidity can directly impact on social and economic values. It reduces recreational opportunities and can affect industries such as fishing, aquaculture and tourism. Turbidity can also increase the cost of treating water for industrial and domestic use, affect pumps and irrigation infrastructure, increase flooding (due to reduced channel capacity) and lead to sedimentation of reservoirs and other water stores.

Map of Turbidity

Managing surface water turbidity

Common characteristics of river basins affected by turbidity often include climate and intensity of land use. They usually contain areas largely cleared of native vegetation, support high levels of agriculture and/or pastoral development and have seasonally dry climates with generally variable rainfall. In contrast, river basins in which turbidity was assessed as not being significant have greater natural vegetation cover, and higher, and more even rainfall.

In the basins in which turbidity is a major water quality issue, management efforts need to counter practices that contribute to soil erosion that ultimately finds its way to surface waters through catchment run off. Management also needs to be directed at identifying means of intercepting soil mobilised by erosion before it reaches surface waters.

Catchment management seeking to reduce surface water turbidity needs to consider a range of initiatives under two strategic approaches that are not mutually exclusive, including:

Reducing soil erosion

Intercepting water born suspended solids

There are two key challenges to combating turbidity problems. (1) the problem usually originates from a range of diffuse sources rather than a specific point, and (2) the impacts upon common property resources are often due to cumulative actions upon private property.

In some instances the potential for downstream impacts on nationally valuable resources such as Ramsar wetlands and protected marine areas such as the Great Barrier Reef Marine Park, provide some statutory capacity and impetus for Commonwealth government policy initiatives to support State and territory activities.

Salinity

Findings

Salinity is a major surface water quality issue in much of temperate southern Australia. It affects basins in most of the South-West Coast, the southern South-East Coast and southern Murray-Darling drainage divisions. Four basins in western New South Wales within the Murray Darling Drainage Division, one east coast basin in the South Coast Drainage Division (Hawkesbury) and three basins in the South Australian Gulf also recorded major and significant salinity exceedances. Assessments also revealed that two tropical and several sub-tropical Queensland basins in the North-East Coast Drainage Division had basin scale salinity exceedances. In at least three of these basins, however, tidal influences in the lower river monitoring stations, may have skewed the results.

In contrast most coastal river basins in the North East Coast and South East Coast Drainage Division, many of the upper and lower basins in the Murray Darling Drainage Division and four near coastal basins in the South-West Coast Drainage Division indicated no major of significant exceedances of salinity guidelines.

Surface water quality in terms of salinity refers to salt concentration and should not be confused with salt loads. Stream flow can dilute salt concentration, so that basins may export high salt loads but not exceed surface water salinity guidelines. This is the case of some basins such as the Murrumbidgee, which recorded good salinity levels (salt concentration), but is know to export significant salt loads downstream (Murray Darling Basin Ministerial Council 1999).

Trend analyses were constrained by available data, but where available, the data indicated both increasing and decreasing trends:

The Murray Darling Basin's Salinity Audit (Murray Darling Basin Ministerial Council 1999) predicts increased salinity for almost all river basins within the Murray Darling Drainage Division through to 2020, 2050 and 2100. The trends identified in this assessment are based on observed river salinity values over a proceeding 8-10 year period. While such trend assessments are important for tracking changes in river salinity they have a limited capacity to predict salinity values. This is because of the non linear nature of salinity trends which are driven by climate, water diversion patterns and complex interactions with groundwater levels and salt stores. In comparison the predictive method used in the MDBMC (1999) study incorporates modeling of groundwater rise and salt load mobilsation processes and highlights the complexity of developing a predictive capacity for surface water quality.

The availability of data and the intensity of monitoring coverage limited the assessment. Salinity guideline exceedances could also be expected in some basins with insufficient monitoring coverage in the South-Australian Gulf, the southern South-East Coast and the Murray Darling Drainage Divisions, as all these areas have significant soil salinisation.

Context 

Australia's dry climate and ancient weathered landscape result in naturally high stores of salt being present within a range of soil types. These factors often combine to create relatively high 'natural' salinity levels in Australian surface waters. State and Territory based water quality guidelines reflecting regional distinctions in 'natural' water quality were used for the Audit.

Impacts

For most freshwater organisms high levels of salinity cause major physiological stress resulting in changes in aquatic biotic communities and a significant loss of diversity. Salinity inhibits or prevents the growth of many aquatic plants affecting primary production and causing the loss of important microhabitats. Salinity impacts upon riparian vegetation further reducing habitat and increasing the potential for bank erosion.

High surface water salinity also has economic and social impacts. Salinity increases the cost of treating water for drinking, reduces the suitability / availability of water for irrigation and other industrial applications, and contributes to the loss of productive land (through the use of unsuitable irrigation supplies) and impacts on public infrastructure. Other social impacts include reduced recreational opportunities and aesthetic impacts.

Map of Surface Water Quality 2000 Exceedence - Salinity Guidelines.

Managing surface water salinity

Management actions required to address surface water salinity are often linked to those needed to address soil salinisation which is one of the key drivers behind increasing surface water salinity.

River basins with major salinity water quality issues are commonly characterised by similar land use patterns and climate. Most have low levels of natural vegetation cover, and a seasonally dry climate with generally low rainfall. Irrigated agriculture is also a significant land use in many of the affected basins.

In such situations there is often a high risk of soil salinisation due to accumulated salt stores within the (unflushed) soil profile and the prospect of rising water tables associated with changes in the landscape water balance. These changes in the landscape water balance are usually associated with the replacement of deep-rooted native vegetation with shallow rooted crops and pastures, and/or the contribution of deep drainage 'leakages' from irrigated agriculture. Rising water tables mobilise salts stored in the soil profile which find their way to surface waters though saline groundwater discharges or via surface catchment run off.

Management of both soil and surface water salinity is therefore associated with restoring the water balance within the landscape. However some of the management options promoted to address soil salinisation for example engineering solutions such as deep drainage or groundwater de-watering, can increase salinity levels in receiving surface waters.

The nature of groundwater systems ie, whether they are local or regional in magnitude, will affect the likely success and response times of potential management options. Regional groundwater systems may accommodate more than 100 years of rising groundwater before the water table approaches the surface. Consequently, response times in terms of reducing groundwater levels are of an equivalent duration. Local groundwater systems fill and respond more rapidly to intervention. The Audit's mapping of regional, intermediate and local groundwater systems provides an appropriate operational framework for planning restorative and preventative management actions to address bother surface water and soil salinity. These include but are not limited to:

Nutrients

Findings

Nutrients (total phosphorus and total nitrogen) are a major surface water quality issue in Australia affecting most of the more intensively developed basins in the North-East Coast, Murray-Darling, South-East Coast and South-West Coast drainage divisions. Basins assessed to have nutrient levels within guidelines include the relatively well vegetated and less developed basins in areas such as north Queensland, north eastern Victoria and south western Australia.

Nutrient trend analyses were more constrained by the availability of data than analysis of exceedances. The available trend data indicated that:

Data availability and monitoring coverage within individual river basins limited this assessment. Monitoring coverage for total nitrogen was more limited than for total phosphorus and was not available for some states - see map below. Major or significant nutrient issues may not be detected where monitoring coverage is insufficient or non-existent. This could particularly apply to river basins with poor monitoring coverage in the North-East Coast, South-East Coast, South Australian Gulf and South-West Coast Drainage Divisions, which are characterised by more intensive land use, recognised to pose risks to surface water quality in terms of nutrient loading.

Context

Australia has a wide variety of soil and vegetation types and climatic regimes, all of which affect the natural nutrient status of surface waters. State and Territory based water quality guidelines reflecting regional distinctions in 'natural' water quality were used for the Audit. However, further research concerning the natural characteristics of river basins and the capacity of their aquatic ecosystems to assimilate nutrients may support the establishment of more site-specific nutrient guidelines.

Impacts

Surface waters nutrients are essential for aquatic ecosystem food chains. However, excessive inputs lead to nutrient pollution known as eutrophication. The impacts of eutrophication include excessive growth of nuisance aquatic plants including algae that can smother bottom habitats and choke waterways and estuaries. Flow on ecological effects include the loss of important feeding and breeding habitats such as sea grass, and impacts on benthic animals such as corals. Decomposing organic matter produced by excessive aquatic weed and algal growth can lead to oxygen depletion and in some cases, fish kills. High nutrient levels in surface waters also promote blue-green algae blooms, which can contain compounds toxic to humans and stock. Eutrophic waters also provide an ideal environment for pathogens that can increase the incidence of infections and disease in exposed wildlife and people.

Nutrient loads generated within a catchment are usually exported to estuarine and coastal marine environments. Nutrients derived from upper catchment land uses exported from catchments during floods have been implicated in the demise of coastal sea grass beds and fringing coral reefs.

Ecological impacts can lead to a loss of biodiversity within affected aquatic ecosystems. Social and economic impacts include increased costs of water treatment, public health risks, loss of amenity values (fishing, swimming, boating, aesthetics), reduced fisheries productivity and impacts on tourism.

Map of Surface Water Quality 2000 Exceedence - Nutrient Guidelines.

The national overview of surface water exceedances of total phosphorus guidelines indicates that phosphorus was the main driver of recorded nutrient exceedances.

The similarity between basins with phosphorus exceedances and those with turbidity exceedances highlights the recognised role of suspended sediment as a transporter of bound phosphorus.

Basins that did not have phosphorus exceedances ie, smaller coastal basins with better vegetation cover and more even rainfall, also tended to not have turbidity exceedances.

Map of Surface Water Quality 2000 Exceedence - Total Phosphorus Guidelines.

The national overview of surface water exceedances of total nitrogen guidelines shows the more limited data available for total nitrogen. Some assessments revealed exceedance patterns for nitrogen were distinct from those observed for total phosphorus. Some larger inland basins ie, the Mallee, Murrumbidgee, Burnett, Fitzroy, that recorded major exceedances for total phosphorus, recorded only significant exceedances for total nitrogen. In contrast, some smaller more coastal basins ie, the Preston, Thomson, and Herbert that did not record exceedances for total phosphorus, recorded significant exceedances for total nitrogen.

These differences in exceedance patterns between the two main classes of nutrient indicate different nutrient sources. This highlights the need for specific management initiatives to deal with nutrient loads generated from different catchment activities and land uses.

Map of Surface Water Quality 2000 Exceedence - Total Nitrogen Guidelines.

Managing surface water nutrients

Most of the assessed river basins within the more intensive land use areas of Australia have significant or major exceedances of nutrient water quality guidelines.

Two nutrients are the main contributors to the eutrophication of Australian surface waters: phosphorus and nitrogen (see separate maps below). Both nutrients occur in a number of chemical and physical forms and are derived from a range of diffuse and point sources. Organic carbon is also implicated in the nutrient loading of surface waters but due to limited data availability was not part of the Audit.

Phosphorus and nitrogen loading within surface waters comes from natural sources such as soil, organic matter and rainfall, and land uses sources including domestic animal waste, fertilisers, storm water run off, sewage and industrial discharges. Knowing the source and relative contribution of nutrient types from different land uses within a catchment is fundamental to any catchment strategy seeking to manage nutrient loading. At a local and sub-catchment scale, nutrient loading from point sources such as sewage plants and diffuse sources such as fertiliser used in intensive agriculture and horticulture, both contribute significantly to surface water nutrient loads. However, nutrient budgets for entire river basins often point to a more significant contribution from other diffuse sources such as soil erosion and domestic animal wastes.

Catchment management efforts seeking to reduce the nutrient loading of surface waters need to identify methods of reducing the number and contribution of catchment nutrient sources. This includes recognising the fundamental link between nutrients and turbidity. Because nutrients bind to suspended sediments in the water, soil erosion contributes to both turbidity and nutrient pollution. Management also needs to consider ways of intercepting and assimilating within catchments the nutrient loads that result from soil erosion and land use activities to ensure that catchment nutrient exports remain within ecologically sustainable limits.

Catchment management planning for nutrients should consider a range of initiatives under these two strategic approaches which are not mutually exclusive. These include but are not limited to:

Reducing nutrient sources

Intercepting and assimilating nutrients

pH

Findings

The monitoring coverage for pH is limited primarily to Queensland and Victoria. The main affected areas were tropical Queensland coastal basins within the North-East Coast Drainage Division and the Campaspe basin within the southern Murray-Darling Drainage Division. Several other basins within the southern Murray-Darling Drainage Division and one each within the, South-East Coast, South-West Coast and North-East Coast Drainage Divisions also significantly exceeded pH guidelines. Problems were well documented but not necessarily well monitored in other basins. For example, acid-drainage water quality problems have been detailed for a number of north coast NSW catchments (NSW EPA 1997).

Both low pH (acidic) and high pH (alkaline) exceedances were recorded, sometimes from the same basin. The weighting of lower basin, floodplain/coastal sampling sites may bias the exceedance records in some coastal catchments.

Data to support trend analyses were limited to Victoria, Queensland and South Australia. In the Victorian section of the Murray Darling Drainage Division, trend analyses identified increasing pH in one basin and decreasing pH (increasing acidity) in six basins, only one of which was recognised to currently exceed pH guidelines. In the South-East Coast Drainage Division, decreasing pH was recorded in four basins and increasing in three basins, all of which did not have existing pH guideline exceedances. Two Queensland basins in the North-East Coast Drainage Division also exhibited pH trends: the Brisbane (increasing pH) and the Fitzroy (decreasing pH).

Map of Surface Water Quality 2000 Exceedence - ph Guidelines.

Managing surface water pH

The natural pH of Australian surface waters is highly variable and is driven by a range of factors including underlying geology, organic loading, flow characteristics and climate. State and Territory based water quality guidelines for pH reflect some of this variability, with some states such as Victoria setting specific guideline for individual basins under State Environment Protection Policies. Queensland uses national ANZECC guidelines but has recognised that naturally acidic floodplain wetlands may sometimes record exceedances. Australia-wide, the development of more site, and regionally specific pH guidelines could be warranted in order to accommodate natural surface water conditions outside the existing guidelines.

The predominance of decreasing pH (increasing acidity) trends in Victoria, highlights the need for further investigation. The relationship between surface water acidity and a range of drivers including land degradation processes such as soil acidification is recognised (Harris 2000)

Many of the pH exceedances were located in coastal basins perhaps reflecting natural floodplain conditions or the disturbance (oxidisation) of insitu acid-sulphate soils. Increasing pH in non-coastal areas could be associated with land degradation (ie. soil acidification) and may indicate an emerging surface water quality issue. Other potential causes of surface water pH exceedances include acid rain (a major issue in the Northern Hemisphere), acid mine drainage, industrial discharges, and organic loading of slow flowing or still waters.

Catchment management plans to address pH exceedances first needs to identify the source of the problem. Appropriate management initiatives could include:

Surface water quality monitoring in Australia

In Australia, monitoring of surface water quality is undertaken to provide information for a range of purposes including to:

Australia spends $142 - 168 M per year monitoring water quality (Atech 2000). This is undertaken by:

To assess surface water quality guideline exceedances and trends, data was obtained from all the major State and Territory agency water quality monitoring programs. However, data was not obtained from other sources because:

Where available, data was obtained for six water quality variables including, salinity, turbidity, total nitrogen, total phosphorus, pH and faecal coliforms. Data for other important water quality variables was limited and localised and was not part of the Audit.

To enable defensible exceedance and trend analyses to be conducted, stringent data quality and length of record requirements had to be met. This reduced the amount of available water quality data.

Map of number of measuring station per basin

Where is surface water quality being monitored?

Coverage

Water quality data that met the requirements for exceedance or trend analyses for at least one water quality variable were available for 113 of the 246 river basins in Australia. Data was primarily limited to the more developed areas, often in those basins where water quality has already been an issue. This includes most of the North-East Coast, South-East Coast, Murray Darling, South-West Coast and the South-Australian Gulf Drainage divisions. Victoria had the best coverage, followed by New South Wales, Queensland, Western Australia and South Australia.

Areas that lacked water quality data suitable for analysis included: all of the Northern Territory and Tasmania, most of the northern tropics, central and southern arid regions including the Indian Ocean, Timor Sea, Gulf of Carpentaria and Lake Eyre Drainage Divisions.

Table of River Basin Water Quality Data Analysis Coverage for Different Water Quality Variables

Water Quality VariableRiver basins with sufficient data for site exceedance assessment*River basins with sufficient data for site trend assessment**
Total Phosphorus101 (41%)64 (26%)
Total Nitrogen75 (30%)41 (17%)
Electrical Conductivity112 (46%)99 (40%)
Turbidity98 (40%)74 (30%)
pH73 (30%)61 (25%)
Faecal Coliforms<1%<1%

% Figures indicate proportion of Australia's 246 basins

* At least three years of monthly data collected since 1995

** 7-10 years of monthly data collected since 1990. Flow measurements must have also been undertaken.

Exceedance Analyses

The number of exceedance analyses assessed per river basin largely paralleled monitoring station density. Agency monitoring programs capable of assessing a wider range of water quality variables usually covered areas of greater land use intensity. Data coverage for each variable relates to the ease and cost of measurement. The variables with the greatest coverage were salinity, followed by turbidity, total phosphorus, total nitrogen and pH.

Faecal coliform data were only available for small number of sites within Qld and the ACT. However, the Audit did not obtain faecal coliform data, from local government sources or corporate service providers which have the prime responsibility for monitoring surface water from a human health perspective.

Trend Analyses

Due to the more stringent data demands for trend analyses, available data was better able to support guideline exceedance analyses than trend analyses. For water quality trend assessments, salinity had the greatest coverage followed by turbidity, total phosphorus, pH and total nitrogen. 

However, it is encouraging that generally sufficient salinity data existed to assess trends for most of the more intensively developed catchments. There was also relatively good coverage of turbidity data to support trend analyses in the intensive land use areas.

One apparent limitation in terms of trend data coverage for key water quality issues concerned nutrients. Only Victoria had statewide monitoring of both nitrogen and phosphorus with sufficient sampling frequency to provide data for good trend analyses. Australia-wide total phosphorus had much greater data coverage than total nitrogen. This probably reflects the view that phosphorus concentrations are the major limiting factor in algal blooms and eutrophication, and hence more important to monitor than total nitrogen concentration (a concept being challenged by new research findings).

Although pH is readily and cheaply measured in the field it was not widely reported, possibly because acidification of surface waters is yet to be identified as a significant issue for most inland waters. In fact, the low priority given to acidification might explain why much of the pH data already collected, is yet to be analysed.

Number of Water Quality attributes per basin for which exceedance analyses could be assessed.

Map of Number of Water Quality attributes per basin for which exceedance analyses could be assessed.

Number of Water Quality attributes per basin for which trend analyses could be determined.

Map of Water Quality attributes per basin for which trend analyses could be determined.

The following table lists the coverage of water quality monitoring in Australia by State:

StateNumber of stations used in water quality reporting% of drainage basins reporting water quality
Australia70749.19
Australian Capital Territory51
New South Wales10031
Northern Territory
Queensland24536
South Australia2212
Tasmania
Victoria18428
Western Australia15619

Click on the State name in the table to view a report for that State.

Future challenges for monitoring of Australia's surface water quality

Even with an annual investment of about $150m, water quality monitoring in Australia, has a limited ability to assess and report on the status of Australia's surface waters.

Progress

In terms of achievements, Australia has:

Challenges

To gain maximum return on Australia's investment in water quality monitoring areas of potential improvement that present challenges include:

Monitoring Practices and Activities

Institutional 

Management

Further Information

Key

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