Waterways of the Merri Catchment flowing slowly through emergent vegetation; and the lower 30% is a slow, non-uniformly flowing stream.
3.3.2 Summaries of the Significant Tributaries
This summary is based on the work of N.M. Craigie & Associates (Craigie, 1994). They divide each stream into a series of reaches based on generally similar features such as channel, bank and verge characteristics. This section deals with the channel origin and the flow character alone and lists the creeks as they join the Merri Creek from its headwaters to its mouth.
It is worth noting that N.M. Craigie & Associates acknowledge that the classification of the catchment in this manner is quite broad and can be refined by more detailed study. However, this is the best available work that covers the whole watershed.
Mittagong Creek
This creek is the northernmost headwaters of the Merri Creek system but joins Wallan Creek before the Merri Creek near the Hume Freeway. Craigie classed it as having only one reach. From its beginnings to its confluence with Wallan Creek, Mittagong Creek is 5 km long.
Although the channel is essentially natural in origin, there has been extensive modification to it. There are several large on-stream dams and the stream from William Street in Wallan to its confluence with Wallan Creek has been straightened somewhat.
The flow is generally negligible but there are disconnected but relatively permanent pools. The dams constructed obviously control the flow.
Wallan Creek
This creek in the headwaters of the Merri Catchment arises on the south side of Pretty Sally on the Great Dividing Range. It flows south then east through the township of Wallan into the Merri Creek near Wallan East, a total distance of nearly six kilometres. The creek has been divided into four reaches.
The uppermost reach, which has not been described by Craigie, flows through farmland and the urban fringe a distance of 1.2 km. It is likely that the form has not been altered much. The sections of the creek downstream of the township, 65% of the total length (5.35 km), have been substantially altered. These alterations include channel enlargement, installation of a low-flow pipe, channel straightening, channelisation and de-snagging.
The uppermost reach is characterised by a stream flowing slowly through emergent vegetation. The middle reach has not been classified as it has a low-flow pipe. The section from the Hume Freeway to the Merri Creek does not normally flow but has disconnected and semi-permanent pools.
Page 50 State of the Environment Report - Introduction
Strathaird Creek (Airfield Drain)
This creek has its origins in the hills to the west of Wallan, from which it flows southward until it reaches Rowe's Lane where it turns east and flows into the Merri Creek. The point at which it is joined by Taylor's Creek it is termed the Airfield Drain. Craigie divided the creek-drain system into two reaches and the total length of the system is approximately nine kilometres.
Of the total length of the system (8.6 km), 56% has been drastically modified to an unlined artificial drain while the upper 3.8 is in a close to natural state.
The flow regime of the upper part of the creek is likely to be discontinuous but relatively permanent pools with negligible flow. Downstream of Rowe's Lane the creek-drain system is characterised as a slow flowing stream filtered through emergent vegetation.
Taylor's Creek
Taylor's Creek arises on the southern side of Pretty Sally on the Great Dividing Range and flows southwards past Wallan before joining the east flowing Airfield Drain at Macsfield Road and then uniting with the Merri Creek at Herne's Swamp south of Wallan, total length of approximately eight kilometres. The creek has been divided into four reaches.
Of the total length of the creek to the Airfield Drain (5.6 km), 23% is highly modified (straightened and de-snagged), 14% has slightly less modification (de-snagging) and 63% is largely unmodified.
The flow character of each of the three reaches is slow and filtered through emergent vegetation.
Unnamed Western Tributary
This minor tributary drains a small area northeast of Mt Fraser. Although Craigie described the lower two kilometres only as one reach, the upper one kilometre of the stream appears (from the topographic map) to be in a largely natural state. The reach described by Craigie is an artificial unlined drain. Therefore 66% of the creek has been highly modified.
The flow in the lower section is slow and filtered by emergent vegetation.
Bald Hill Drain
This small tributary drains an area northeast of Bald Hill. Again Craigie has described the lower 1.5 km only (as one reach), although the drain begins another 2 km further upstream. The reach described by Craigie is a natural channel that has been extensively modified by straightening and de-snagging. It appears that the remainder could be classed similarly.
The flow has been characterised as slow and filtered through emergent vegetation.
Kalkallo Creek System
This system of drains and creeks draws water off the hills west of Beveridge flowing southward to join Merri Creek near Donnybrook Road. Five drains unite west of Kalkallo to
Page 51 Waterways of the Merri Catchment form Kalkallo Creek proper. Craigie has described three of these drains and termed them Kalkallo Creek West Leg, Kalkallo Creek Centre Leg and Kalkallo Creek East Leg.
The state of the channels of this drainage network is that nearly 36 km of channel length, 14.6 km (41%) is in nearly natural (with only slight modifications) whilst 20.7 km (59%) is unlined channel.
Except for the East Leg which flows only after rainfall, the flow character of all the streams is one of discontinuous but semi-permanent pools of water with negligible flow.
Malcolm Creek
This western tributary joins the Merri Creek a little north of Craigieburn. The creek has its headwaters in an area of open forest between Mickleham and Mt Ridley from which it flows southwards through open pasture until it reaches Craigieburn whereupon the creek turns eastward and flows into the Merri Creek a total distance of approximately 8.3 km. Craigie divided the creek into just two different reaches - that above the Hume Freeway and that below.
The two reaches are in a close to natural state with only minor de-snagging, however the lower reach has greater inputs of rubbish.
The whole of the stream flow is very slow to non-existent and is characterised by disconnected but relatively permanent pools.
Aitken Creek
Another western tributary, this creek joins the Merri Creek just south of Craigieburn. The headwaters of this creek are near the Old Sydney Road about 5 km west of Craigieburn from which it flows in a southeasterly direction through open pasture and then the township of Craigieburn until it joins the Merri Creek a total distance of approximately eight kilometres. Neil Craigie divided the creek into three reaches; that above the Craigieburn Golf Course, the section through the golf course and the section through the township to the Merri Creek.
As a percentage of the total, over 81% of the creek is kept in a nearly natural state and the character of the remainder, whilst extensively modified, is not completely destroyed.
From the headwaters to the golf course the flow is almost non-existent and is characterised by disconnected but relatively permanent pools. There are also many on-stream dams, which in times of storm activity must disrupt the natural flow of the creek. The flow through the golf course is slow and filtered through emergent vegetation. Through the township the flow is slow and non-uniform having runs, glides and pools.
Curly Sedge Creek
This medium-sized tributary arises northeast of Summer Hill and joins the Merri Creek near O'Hern's Road, a distance of around 7.5 km. Craigie has classed the whole creek as one reach. The creek is in a basically natural state with only minor de-snagging.
The natural flow of the creek is negligible with the stream consisting of discontinuous but relatively permanent pools.
Page 52 State of the Environment Report - Introduction
Campbellfield Creek
This small creek is a tributary of Merlynston Creek that runs parallel and adjacent to the Hume Highway. It begins at Mahoney's Road and enters Merlynston Creek in the Fawkner Crematorium, a length of 2.2 km.
Although Craigie has not examined this creek, it is apparent from the topographic maps that the section below the retarding basin to Box Tree Road (a distance of 0.5 km) has been straightened and is probably channelised.
It appears that the creek is an intermittent stream. Surrounding urban development has probably caused an increase in the flow during storm events.
Merlynston Creek
This creek is one of the western tributaries of the Merri Creek and has its headwaters a little north of Barry Road near the Upfield railway station. It flows southward for approximately seven kilometres through the suburbs of Broadmeadows and Glenroy and then through the Fawkner Crematorium, finally entering the Merri Creek two hundred metres above Coburg Lake. The creek has been radically altered by the industrial and urban development. Neil Craigie has divided the creek into five reaches.
Of the total length of the stream (some 6.75 km), 43% is either a pipeline or an open concrete channel and a further 27% has had major modifications. Only 30% of the stream remains relatively unmodified.
For the most part the flow in Merlynston Creek is either very slow or negligible. In the first unconcreted section (the second reach), the flow is almost non-existent, the stream characterised by discontinuous but permanent pools. The next two reaches are distinguished by slow but reasonably steady and uniformly flowing water. The lowest reach has not been classified as it is a pipe.
Edgar’s Creek
Edgar's Creek is the largest tributary of the Merri Creek, flowing from near Wollert on the eastern edge of the catchment through the suburbs of Epping, Thomastown and Reservoir to join the Merri Creek just below Coburg Lake, a distance of almost 17 kilometres. Neil Craigie has split the creek into ten different reaches.
The total length of the creek is 16.9 km, 11% of which is concrete lined. Another 34% of the channel is artificial but unlined. This leaves around 55% of the stream length in near original condition, however, these reaches are at the head and lower end of the stream and are separated by 7.6 km of artificial channel.
The uppermost reach is a mostly dry bed with the occasional semi-permanent pool. The second reach is characterised by a non-flowing stream of disconnected but relatively permanent pools. The section through Huskisson Avenue Reserve is a slow flowing stream
Page 53 Waterways of the Merri Catchment through emergent vegetation. The fourth reach is not classified being a concrete channel. The fifth reach is distinguished by a stream of slow and non-uniformly flowing water passing though runs, pools and glides. The sixth reach is not classified. The seventh reach is distinguished by a stream of slow and non-uniformly flowing water passing though runs, pools and glides. The eighth reach has not been classified. The ninth reach is classed as slow but reasonably uniform and steady flow. The final reach is characterised by fast but non-uniformly flowing water, passing through pools, glides, runs and rapids.
3.3.3 Wetlands
Wetlands are an important landform for both their capacity to temporarily store water “in- catchment” and as habitat for many species of plants and animals. Oates (1994) identifies a number of different types of wetland morphology, of which five are currently found, or were historically present, in the Merri Catchment. These types are: • floodplain/river flats • volcanic plains • alluvial fan/plains • foothills • along drainage lines
At present the main natural wetland area is Hernes Swamp near Wallan. This volcanic plains type used to be an area of approximately 1 km2 but this has been significantly reduced. The swamp at Beveridge (a volcanic plains/alluvial plains type) used to be approximately 1 km2 but is much less than this today. Wetlands along drainage lines are still found throughout the catchment, for example those along Aitken Creek, but they are disappearing due to increased channelisation. Restricted floodplain type wetlands still occur in various locations along the Merri Creek (eg. around Mahoneys Road).
A number of wetlands that were marked on a geological map of the catchment produced in the early 1970s by Earl (1974), but have since been drained. The swampy alluvial fan area around Wallan East used to be some 5-6 km2 but is no longer wetland. Maps show an area (1 x 0.5 km) two kilometres west of Hernes Swamp as a foothills type wetland but it does not appear on recent maps. An area (1.2 x 0.7 km) on the west bank of the Merri Creek between Merriang and Merri Creek Park was an example of the alluvial plains wetland. A swampy area (1 km2) north of Cooper Street was a volcanic plains wetland but is now the site of the Cooper Street Landfill. No doubt many other wetlands were found in both the urban and rural parts of the catchment and have long since disappeared.
The main wetlands that remain in the Merri Catchment (refer to Map 8 in Aquatic Ecology) are: • an unnamed swamp east of Dunlop factory at Campbellfield • Hernes Swamp (S4) • Beveridge Swamp (R6 on east side of Spring Street, Beveridge)
Page 54 State of the Environment Report - Introduction
3.3.4 Water Harvesting
Water harvesting is the extraction of water from a catchment for human uses, such as agriculture and industry. In the Yarra Catchment this has been split into two categories (c.f. Haydon, 1994); Major Diversions (e.g. the Water Storage Reservoirs) and Minor Diversions (eg. Private diverters). In the Merri Catchment there are no Major Diversions.
The Minor Diversions are attributed mainly to private diverters for irrigation or domestic use and as the data is not accurate its true impact has not been investigated. Private diverters are issued licences to extract water administered by Melbourne Water and the amounts allowable vary depending upon the area to be irrigated or the capacity of the licensee's storage. There is no actual measurement of this amount but past studies show that the amount allocated and the amount used is roughly the same. For the Merri Catchment the amount allocated 52 Megalitres (ML) per year.
Another form of harvesting exists for property owners who have waterways on their properties. This "Riparian Right" allows farmers to divert 2.2 ML/year of water for the whole catchment without need for a permit. There is no information as to how many owners exercise this right for the Merri Catchment.
The total extractable water in the catchment is 54.2 ML/year. Based on an average annual flow of 17000 ML, this is approximately 0.32% of the average total contribution of Merri Creek flow to the Yarra River. Whilst this appears to be very small, it could be significant to stream flows in the areas from where it is taken (mainly in the rural segment of the catchment). The allowable extractions also do not take into account periods of low flow in the creek and indeed may be exercised to their full extent during these times of drought, thus increasing pressures on the creek ecosystems.
3.3.5 Stormwater
Although stormwater runoff is a natural process, in the urban environment it is increased due to large areas of land being sealed and paved with an impervious layer that does not allow the ground to soak up excess runoff. Many studies, including Jovanovic (1986), have shown that the process of urbanisation decreases the amount of infiltration. The most obvious impact is an increase in the volume of stormwater entering the stormwater drainage system. The impact of this on the increase in volume on the creek system is best illustrated in Figure 1. This shows how the peak volume and velocity of water flowing in the creeks is raised with increasing urbanisation and how, generally, the peak flows are reached much earlier. Rankin (1994) outlines the process that occurs in the northern tributaries of the Yarra River suggesting that creeks such as the Merri Creek are more sensitive to rainfall with increased development and display an increased “peakiness” of water level, meaning that waterways rise more quickly to a high level - a level higher than pre-development flows - and maintain that level for a longer period.
Page 55 Waterways of the Merri Catchment
Figure 1 Runoff hydrographs for different percentages of urbanisation of a catchment (from Jovanovic, 1986).
The increased runoff in urban areas gives rise to the need for a stormwater drainage system. This extensive network of pipes and drains draws water from the roads and house roofs and directs it into the natural watercourses such as the Merri Creek. The responsibility for this network is currently split between Melbourne Water Corporation (main drains) and the local councils. The following is a list of the main drains that flow into the Merri Creek, their location is shown on Map 5.
• Alexandra Parade Main Drain • Chauvel Street Main Drain • Alexandra Parade Relief Main Drain • Merlynston Main Drain (see Merlynston Ck) • North Fitzroy Main Drain • South Street Main Drain • Lygon Street Main Drain • Middle Street Main Drain • Dover Street Main Drain • Fawkner East Drain • Green Street Main Drain • Campbellfield Creek Diversion Drain • Glenlyon Road Main Drain • Lynch Road Main Drain • Sumner Avenue Main Drain • Major Road Main Drain • Albert Street Main Drain • Fawkner North Drain • Preston Main Drain • Maffra Street Drain • The Avenue Main Drain • Somerset Road Drain • Spring Street Main Drain • Augusta Avenue Drain • Elizabeth Street Main Drain • Jesica Street Drain • Merrilands Drain • Ainslie Road Drain • Harding Street Main Drain
It should be noted that although this is the full list of main drains, there are also numerous smaller drains which carry water off each suburban street before feeding into the main drain system. These smaller street drains are the responsibility of the local councils. The increased runoff carries many sorts of pollutants into the waterways and the increased volume can also cause a loss of in-stream sediments due to erosion.
Page 56 State of the Environment Report - Introduction
Map 5 Drains to the urban waterways of the Merri Catchment
Page 57 Waterways of the Merri Catchment
3.3.6 Floods
One of the more important aspects of stream flow is flooding. Floods are important both in terms of their intimate association with the ecology of the waterways and in terms of impacts on human communities.
Floods and the Human Landscape
In May of 1974 the Merri Creek flooded. This event was, and still is, the worst of the 19 floods since records began in 1894 and caused serious damage to several hundred properties built on the lower Merri Creek floodplain (Earl, 1974). In their Merri Creek Plan, the MMBW (1987) mapped out the 1% (or 100 year) flood levels based on environmental conditions and data current for the mid 1980s and which are subject to change. The most important of these changes are new urban developments that are constantly going outward from the city. There can be little doubt that such urban expansion will, if certain measures are not taken, increase the risk of flood damage to those who live in the lower portions of the catchment. This very view was expressed after the 1974 floods (Earl, 1974).
Current Flood Control Mechanisms
Weirs and Retarding Basins are perhaps the most obvious means by which the management authorities have attempted to mitigate flood events. These are situated at:
• Weir at Coburg Lake: A structure that has no low-flow outlet and relies on the principle of flow in = flow out and the lake remains at a constant level. However, if the level should drop below the weir height (due to groundwater recharge in times of prolonged drought), no flow could be released downstream of the weir until the level recovered sufficiently.
• Weir at Edwardes Lake: A similar structure to that at Coburg Lake (with the same restrictions).
• Retarding Basins on Merlynston Creek: There are three of these structures on this creek designed to protect residents from flooding as the downstream portion is an enclosed drain.
Other dams on the minor tributaries include:
• Retarding basin on Campbellfield Creek • Dam on Strathaird Creek - 5.1 km upstream of confluence with Merri Creek. • Retarding basin on Kalkallo Creek Central Leg - 7 km upstream of confluence with Merri Creek. • Dam on Mittagong Creek - 2.8 km upstream of confluence with Merri Creek
There are also a number of small illegal dams on the creeks in the upper part of the catchment which will have some influence on flooding.
Page 58 State of the Environment Report - Introduction
Other engineered structures that control floods are levee banks on the Merri Creek between Normanby Avenue and Anderson’s Street, Sumner Avenue and Winifred Street. A retarding basin on the Merri Creek has been proposed at Campbellfield but has not been constructed to date.
Other methods engineers have used to reduce the impacts of floods are channel straightening, de-snagging and in some cases lining the channel with rocks or concrete. These all have the effect of removing water swiftly from one area but this can cause more flooding problems further downstream. The parts of the creeks with such works are outlined in more detail above.
In his report on the floods of May 1974, Earl (1974) acknowledges the role that wetlands play in flood prevention. He said then “...that if further relatively minor drainage works are undertaken to drain the natural rural swamps, flood flows downstream of these areas will increase greatly...” At the time the Shire of Whittlesea planned to establish a Drainage Trust to oversee the draining of rural lands. MMBW strongly opposed this for the reasons outlined above but it seems the draining has continued. Since 1974 the community has not experienced such a damaging flood and it is more than likely that if and when one occurs, the damage will be more extensive than that disaster.
3.3.7 Groundwater
Groundwater in the Yarra Catchment is important as it contributes about 50% of the total flow of the water into the Yarra River. Groundwater is also a significant source of water supply within the catchment with the annual licensed diversion to irrigators and others being around 7000 megalitres per year. Groundwater is a major source of soluble salt load carried by the river contributing somewhere between 50-80% of the total (Shugg & O’Rourke, 1994).
Groundwater catchment boundaries generally coincide with their surface counterparts, however aquifers may cross catchment boundaries. This means that activities in one catchment may affect the water quality and quantity in another.
The Department of Natural Resources and Environment monitors groundwater in the Merri Catchment and their results are outlined in the discussion of groundwater quality in Section 4.4.3.
Groundwater use
The authorised yield for the Merri Catchment is not specified but the amount from the "Basalt Plains" as the authors refer to it (which includes the Merri Creek) is 269 megalitres and there are 1027 registered bores in this region (Shugg & O’Rourke, 1994).
Groundwater Hydrology
Groundwater recharge on the basalt plains is around or below 10 mm per year (Shugg & O’Rourke, 1994). The fracture permeability throughout the basalt plains of the northern part
Page 59 Waterways of the Merri Catchment of the Yarra catchment is usually high and groundwater flow is likely to occur over large distances. Indications point to several local recharge areas which, if they inject saline waters into the aquifers, have the potential to produce augmented salinity concentrations (Thomas & Cummings, 1994).
3.4 Conclusions
Very little of the Merri Creek or its tributaries escape the affect of morphology and flow changes brought about by post-European settlement landuse practices. In the rural reaches these changes are most pronounced where the channel is least incised. In the headwaters, the swampy alluvial fan and the chain-of-ponds settings, agricultural practices have, in places, drastically altered stream form by channel straightening, drainage of wetlands and snag removal. Natural flows are reduced by both on- and off-stream dams.
The encroachment of urban development up the valley of the Merri Creek has brought with it the almost inevitable changes to morphology and flow. These are most severe in the long- established inner urban areas of Northcote and Brunswick. It is here that channel modifications, designed to limit the impacts of floods are most extensive. However, the problems which flooding causes to the people living near the creek are exacerbated by landuse practices further up the catchment such as paving and associated stormwater drainage, the channelisation of streams and drainage of in-catchment water storage wetlands.
The portion of the Merri Creek least altered by landuse changes since the arrival of Europeans is a stretch a few kilometres either side of Craigieburn. In these reaches, the incised valley protects the creek from destructive farming practices. Flows here are somewhat restricted by dams.
The understanding of groundwater, which is normally a significant contributor to streamflow, is very limited in this catchment. More work needs to be done to determine the effects of landuse practices on rates and volumes of discharge to the catchment streams.
Page 60 State of the Environment - Water Quality
Summary: Water Quality
Over the last twenty years there have been 11 studies examining water quality. Some of these have been one off “snapshots” while others have been over a period of a few years and still others are even longer term. Most of these investigations examine only physico-chemical aspects of water quality but four studies consider biological aspects (shown in Table 6). Much of the monitoring has taken place as a part of a larger sampling program for the Yarra Catchment, so the number of sites monitored in the Merri Catchment has been limited. As a result, there is a lack of data for tributaries of the Merri Creek. Edgars Creek has been the subject of some research but this amounts to, at most, two sites per study. Other tributaries receive no attention whatsoever.
Table 6 Overview of surveys examining water quality in the Merri Catchment. Study Type Date Location Type of # of parameter sites MMBW period Apr1971Mar.1984 Merri&Edgar physico-chemical 10 EPA longterm 1972-1981 Merri Creek physico-chemical 1,2 PIRG snapshot Dec. 1974-JanMerri Creek physico-chemical 13 1975 & biological Campbell period Nov. 1979-Ma Merri Creek physico-chemical 2 1980 & biological Mitchell & Clark snapshot March 1990 Merri &physico-chemical 12 Edgars & biological VWQMN longterm Jan. 1991- Merri Creek physico-chemical 2 Mitchell & Dunn snapshot 26-28October1992Merri&Edgar physico-chemical 10 Gaal period 1993-1994 Edwardes physico-chemical 1 Lake & biological Ellett & Kingsley snapshot 1994 Merri Creek physico-chemical 5 Roy snapshot April, August 199 Merri&Edgar physico-chemical 8,4 Melbourne Water snapshot Feb.-March 1995 Merri&Edgar biological 16
The Merri Creek
The studies of physico-chemical and biological parameters show broad changes down the length of the Merri Creek. These changes in water quality are indicative of changes in the surrounding land use over time and along the length of the waterways. In general, the level of alteration to the surrounding land reflects the level of degradation of the aquatic ecosystem, with the rural sections of the waterways being healthier than the industrial and urban sections. However, each broad land use has its own distinctive problems and these are described downstream along the creek. This is based on available monitoring information but it should be noted that other polluting substances such as surfactants, pesticides, petroleum products are potential problems based on current catchment activities, but they have not been recorded. The quality of the water is, in most cases, measured against SEPP guidelines, however where these standards are inadequate other more relevant guidelines are used (eg. ANZECC and Ontario guidelines).
Page 61 Waterways of the Merri Catchment
The rural section The main problem in the rural sector (ie from the headwaters to Craigieburn) is nutrient (and suspended solids) levels, the main source of which is runoff from agricultural land. Concentrations of nutrients measured occasionally fail the ANZECC guideline objectives.
Heavy metals are not generally a problem in this segment. However two recent studies have noted high levels (one of 27 ppm in sediments) of arsenic from Summerhill Road to Craigieburn (maybe from pesticides). Currently there are no objectives set for heavy metals in sediments. All studies of macroinvertebrate communities reveal good diversity and abundance indicative of fairly low pollution levels.
The industrial section Water declines in quality after the creek enters the industrial zone (from Craigieburn to Mahoneys Road). Poor water quality is evident in all studies of macroinvertebrates. Populations of these organisms experience a major decline between O’Herns and Mahoneys roads.
The upper portion of this section is dominated by treated effluent discharges from the Craigieburn Sewage Treatment Plant. Invariably the high concentrations of nutrients measured downstream of Craigieburn fail the ANZECC guideline objectives. Of particular concern is the jump in levels of reactive phosphorus at Craigieburn (up two orders of magnitude). More recent surveys show that suspended solids also have high levels from Craigieburn to O’Herns Road. Although the lack of data makes comparison difficult, results suggest levels exceed the SEPP objectives. Nutrient levels, after decreasing downstream of Craigieburn, rise again just below Cooper Street before again decreasing downstream.
A number of studies point out that heavy metals in the water column and in stream sediments increase markedly upon reaching the industrialised region. This is recognised as a potentially serious threat to the aquatic life of the creek. Of the two forms of contamination, it is thought that those in the sediments may offer the best means of gaining a long-term account of the importance of heavy metals in the creek.
The three studies that have tested the sediments show that concentrations of copper, lead and zinc (and to a lesser extent cadmium and chromium) increase by at least one order of magnitude around Barry Road in Campbellfield. These high levels decrease slightly on progression downstream but not very significantly. Inputs of heavy metals to stream sediments may be from historical effluent prior to sewer connection of this area, as well as the continued diffuse inputs from catchment activities via stormwater drains.
The residential section Some indicators show that the water quality improves in some parts of the residential area (downstream of Mahoneys Road), but generally it deteriorates further. Studies show that the macroinvertebrate community recovers downstream of Mahoneys Road indicating a slight improvement in overall water quality.
Nutrient levels (although they do not return to their pre-Craigieburn levels), salinity and suspended solids show some improvement. Heavy metals, on the other hand, generally maintain their high levels in sediments. Litter levels increase markedly downstream through
Page 62 State of the Environment - Water Quality the urban area. Dissolved oxygen levels display a deterioration downstream and are close to the limits below which aquatic fauna may not survive. This could be a result of organic pollution and high levels of algae.
Edgars Creek
Edgars Creek is the only other creek in the catchment that is monitored, and there have been a limited number of monitoring sites. The available data show that it generally shares the same problems as the Merri Creek, however it differs in some respects.
Levels of turbidity are generally lower in Edgars Creek as are levels of suspended solids and salinity. Nutrients do not display a consistent pattern downstream, but lower than the Merri Creek. Heavy metals are generally lower than those of the Merri Creek, however Mitchell & Dunn (1993) found the highest levels of metals in sediments for their whole study were on Edgars Creek at Mahoneys Road. Their study of heavy metals in the water column did not display these high levels. On a positive note, levels of dissolved oxygen are well in excess of those recommended by the SEPP and appear to have improved from 1990 (Mitchell & Clark, 1991) to 1992 (Mitchell & Dunn, 1993).
Conclusions
The water quality in the Merri Creek and Edgars Creek generally declines downstream along the waterways. Much of this decline is associated with changes in the surrounding landuse, from rural to urban. However, each landuse has its own particular problem.
In agricultural areas, high nutrient levels are a problem. From the industrial region, there is a rise in heavy metal pollution. The main problems in the urban area are the result of inadequate sewage disposal and diffuse source pollution via the stormwater drainage system.
Page 63 Waterways of the Merri Catchment
Page 64 State of the Environment - Water Quality
4. Water Quality
4.1 Introduction
The quality of the water in which plants and animals live is of vital importance for their survival. Therefore it is important to consider water quality when assessing aquatic ecosystem health. A number of key indicators, such as dissolved oxygen or suspended solids, have traditionally been used to determine water quality. This section assesses past and present water quality based on the information available on various water quality indicators. This section then examines the polluting sources, both diffuse and point, to enable appropriate management of the degradation.
4.1.1 Previous Work
This section is a review of the state of water quality based on a number of studies. It attempts to draw together all of the relevant pieces of work into one coherent document. What follows is a brief description of the scope of the important research efforts. The outline below highlights the great amount of information about water quality so one of the tasks of this section is to underline the most important aspects and the areas where the research fails in its efforts to pin-point the nature of the problem. The following list shows how water quality monitoring has moved away from using purely physico-chemical assessments to using biological monitoring as well.
The Public Interest Research Group (1975) study of December 1974 through to January 1975. This group sampled 10 sites along the Merri Creek from Craigieburn to Clifton Hill. They analysed the water for Biological Oxygen Demand (BOD), Dissolved Oxygen (DO) and acidity (as pH). They also collected aquatic fauna at 13 sites (see Section 5).
Environment Protection Authority (EPA, 1975, 1981, 1982, 1983a) long-term study from 1972 to 1981. These surveys sampled the Merri Creek at Heidelberg Road and Roseneath Street (1972-1974), Roseneath Street (1974-1975), Roseneath Street and St Georges Road (1976-1978), numerous sites on the Merri Creek and a number of tributaries (May-July 1977; May 1979-April 1981). Physico-chemical parameters measured include turbidity, suspended solids, pH, E. coli, heavy metals in the water (copper, zinc), DO, salinity (Total Dissolved Solids-TDS) and nutrients.
The Ministry of Conservation (Campbell, et al., 1982) study from November 1979 to October 1980. This group measured BOD, DO, nutrients, heavy metals (lead, zinc, copper, chromium and mercury) and benthic macroinvertebrates at two sites (Summerhill Road and Heidelberg Road) on the Merri Creek as part of a Yarra Catchment-wide project.
Melbourne & Metropolitan Board of Works (unpublished) study from April 1971 to March 1984. This agency conducted a six-site survey on the Merri Creek (simultaneously with the EPA) between Craigieburn and St Georges roads, on Edgars Creek at Boyne and Leamington streets and Mahoneys Road and at Merlynston Main Drain. Sample analysis was for nutrients (total phosphorus and nitrogen, orthophosphate and nitrate),
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Mitchell & Clark (1991) study in March 1990. This report is based on physico-chemical and biological monitoring from 10 sites on the Merri Creek between Beveridge and Heidelberg roads and on Edgars Creek at Broadhurst Avenue and Leamington Street. Samples were analysed for temperature, pH, salinity (Electrical Conductivity-E.C.), DO, BOD, suspended solids, nutrients (oxidised nitrogen, total kjeldahl nitrogen and reactive and total phosphorus), E. coli, heavy metals in water (arsenic, cadmium, chromium, copper, zinc, iron, lead, manganese and nickel), heavy metals in sediment (cadmium, chromium, copper, zinc, iron and lead) and surfactants. Macroinvertebrates and diatoms were the biological parameters measured.
Mitchell & Dunn (1993) study in October 1992. This survey over three weeks was carried out at eight sites on the Merri Creek (between Summerhill Road and Broadhurst Ave) and two sites on Edgars Creek (at Mahoneys Road and upstream of the Merri Creek confluence). Parameters measured include turbidity, suspended solids, nutrients (oxidised nitrogen, kjeldahl total nitrogen and reactive and total phosphorus), DO, pH, E.C. and heavy metals in water and sediment (arsenic, cadmium, chromium, copper, zinc and lead).
Victorian Water Quality Monitoring Network (Hunter & Zampatti, 1994a, 1994b) study since January 1991. This study measures physico-chemical aspects at two sites on the Merri Creek (Cooper Street and Roseneath St). Monitoring at Cooper Street recently stopped. They are measuring parameters such as temperature, pH, E.C., DO, turbidity, suspended solids and nutrients (oxidised nitrogen, total kjeldahl nitrogen and reactive and total phosphorus).
Gaal (1994) study of Edwardes Lake during 1993 and 1994. This study examined the physico-chemical parameters of Edwardes Lake such as turbidity and nutrients (total nitrogen and total phosphorus). Macroinvertebrates were the biological parameters measured.
Ellett & Kingsley (1994) study of 1994. This study examined the chemistry of a number of drains entering the Merri Creek between Barry and Mahoneys roads. Five sites were sampled and measurements taken for velocity, temperature, pH, E.C., total suspended solids, TDS, DO, chemical oxygen demand (COD), metals (chromium, zinc, copper, manganese iron) and nutrients.
Melbourne Water (unpublished) study from February to March 1995. This study, conducted in conjunction with a survey of Platypus numbers, sampled 15 locations on the Merri Creek and two on Edgars Creek (one site doubled up) for macroinvertebrates.
Victorian Water Quality Monitoring Network (VWQMN), 1995. Victorian Water Quality Monitoring Network Database, Water EcoScience. While not a study, water quality data for the Merri Creek from the VWQMN database has been analysed for use in this section.
Roy (1996) study in April and August 1995. This study assessed the level of heavy metals in sediments of Merri and Edgars creeks. In April, eight sites on the Merri Creek from Summerhill Road to Rushall Station along with one at Edgars Creek below the Epping Trade Waste disposal site were studied in the first stage. The second stage in August reduced the
Page 66 State of the Environment - Water Quality number of sites to four (all on the Merri Creek). Metals analysed include arsenic, chromium, cadmium, copper, lead, zinc, nickel and mercury. Selenium was added to the list for the second stage. Other parameters measured include DO, E.C., pH and temperature.
4.1.2 Scope of this section
This section seeks to establish the current state of knowledge of water quality of streams in the Merri Catchment. It reviews previous work in which physico-chemical and biological parameters were monitored and assessed in an attempt to determine what state the creek system is in, while being aware of the limitations of this information. It also includes results from specific studies undertaken for this report, to assess heavy metal contamination in creek sediments and the impact of landfill leachate on the Merri Creek.
4.2 ‘Natural’ states
To understand the level of degradation or the level of health of the aquatic environment of the Merri Creek, it is important to try to determine the 'natural’ state of the Merri Creek before human interference.
However, this is not an easy task. Much of the Merri Catchment lies in the Volcanic Plains Grasslands. This is prime grazing land and has been utilised from the earliest days of settlement. This land was so quickly and thoroughly used, that in 1916 it was written of the plains, north and west of Melbourne that '...it has been put so thoroughly to pastoral and agricultural uses that hardly any part now remains in the virgin state' (OCE, 1988). These settlers did not make many detailed accounts of the early state of this environment. If there were any records, they do not remain today.
As a result of such activities, it is difficult to determine the natural water quality of the Merri Creek. High levels of salinity in the Merri Creek may be a result of the clearing of vegetation within the catchment, or may be naturally high due to mineral deposits or a natural lack of vegetation with deep root systems. Determining the natural degree of vegetation cover in the area is also difficult. Since the catchment is part of the west Victorian Volcanic Plains morphology (Jenkin, 1988), it is likely that the degree of tree cover to begin with was small. In addition, aboriginal hunters may have played some part in the clearing of forest cover to open up areas for more accessible hunting. The extent of management undertaken by the aboriginal people before European settlement is often overlooked, especially when trying to predict so-called 'natural’ states.
Determining baseline levels of heavy metals in the sediments is also difficult to determine. It is possible that these baseline levels may be quite naturally high due to the large amount of volcanic activity in the region. An indication of background levels based on the Rock Shale Standard is in given in Appendix 7.
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4.3 Water quality parameters as indicators of stream health Traditionally, a number of physical, chemical and biological indicators are used to monitor the health of streams. These indicators are the basis of the monitoring programs beginning in the 1970s to ascertain the condition of the Merri Creek. The following section outlines these, and the reasons for using each as an indicator of stream health.
Box 9 Water Quality Indicators
One of the main means of measuring the health of aquatic ecosystems is the use of water quality indicators. These indicators may be divided into two broad categories, key indicators and secondary indicators.
Key indicators are most sensitive indicators for providing information on aquatic ecosystem health These include:
• Physical & chemical indicators • Biological indicators
Secondary indicators provide information relating to human activities which impact on the environment and provide clues to the state of the environment if key indicators are absent. Examples of secondary indicators include such things as:
• Indigenous vegetation cover • Land use • Sewage & waste discharges.
4.4 Existing states
A number of studies have analysed the water quality of the Merri Creek since the 1970s (outlined above), using physical, chemical and biological parameters. A brief summary of their specific aims and results is provided in Appendix 4. The following section is an overview of the state of the water quality in the Merri Creek.
4.4.1 Physical and chemical parameters
Physical and chemical tests are highly specific measurements of water quality. Their purpose is to determine the health of a stream based on the quantitative or qualitative measurement of a specific physical or chemical parameter of the water. For example, it is possible to measure the level of dissolved oxygen in the water, and use that information to determine if aquatic fauna can survive in the stream. Dissolved oxygen is essential for the for the respiration of aquatic organisms. If levels of dissolved oxygen are low, more sensitive species will not be able to survive and aquatic biodiversity will be diminished.
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Table 7 summarises the main purposes behind the use of a number of physical and chemical parameters that have been monitored in the Merri Catchment. However, there are limitations in their use, which has prompted the recent introduction of biological indicators. Table 13 evaluates the performance of the Merri Creek with respect to pollution issues against EPA State Environment Protection Policy guidelines.
Turbidity
Turbidity in the Merri Creek has been a consistent problem over the monitoring period. The Public Interest Research Group (PIRG, 1975) study noted high level of turbidity in 1974, as did the EPA 1974-75 study. More recently, data from the Victorian Water Quality Monitoring Network from 1992 to 1994 also recorded intermittently high levels. While turbidity levels are not always high, there are periods (often associated with high flow) when turbidity exceeds the level recommended by the EPA State Environment Protection Policy (SEPP). Mitchell & Dunn (1993) noted that turbidity increases downstream along the Merri Creek and is generally higher in the Merri Creek than in Edgars Creek.
A water quality study of Edwardes Lake (Gaal, 1994) found that the levels of turbidity in the lake may also be high from time to time. With the reduction of stream flow as Edgars Creek enters Edwardes Lake, the lake is acting as a sink for the fine suspended particles and is gradually becoming shallower requiring periodic dredging. An artificial wetland is being constructed directly upstream of the lake to act as a silt and litter trap. This will improve the water quality of Edwardes Lake for recreational activities.
Suspended Solids
Like turbidity, suspended solids have consistently been a problem in the Merri Catchment. EPA data from 1974-75 noted high levels of suspended solids, as did the data from 1976-78. This later report noted that there were significant peak loads during high flows, but that levels had decreased since the earlier study (EPA; 1975, 1982). This corresponded with the connection to sewer of previously unsewered areas. Mitchell & Clark (1991) noted increased suspended solid levels downstream of the Craigieburn Sewage Treatment Plant and again between Mahoneys Road and Broadhurst Avenue. This indicates that the sewage treatment plant and urban stormwater are causing an increase in suspended solids in the creek. The VWQMN data from Campbellfield and Fitzroy North from 1992-1995 indicated that levels of suspended solids are intermittently high in the creek, with the upstream site being in excess of the SEPP 90th percentile level.
Temperature
Based on recent cumulative water quality data from the Victorian Water Quality Monitoring Network, the temperature of the Merri Creek fluctuates seasonally from a minimum of about 8OC to a maximum of 24OC with a mean of 15.6OC at St Georges Road in Fitzroy and 5OC to 22OC with a mean of 13.5OC at Coopers Street in Somerton. Fluctuation may occur as a result of natural conditions or events such as the amount of shade or the climate. The major anthropogenic effect on water quality is likely to be from discharges of industrial cooling water or urban stormwater. The temperature of the water will have some effect on the suitability of the creek for certain aquatic fauna and flora. Temperature also affects other parameters. For example, cooler water is able to hold more dissolved oxygen, whereas
Page 69 Waterways of the Merri Catchment warmer water will increase the metabolic activity of certain aquatic organisms such as bacteria and algae, which in turn may affect levels of dissolved oxygen.
Salinity (Electrical Conductivity)
Salinity levels in the Merri Creek have generally been high. It is uncertain if these high levels are natural to some extent, or the result of anthropogenic impacts. Based on measurements of total dissolved solids, the EPA report noted significant salinity in the Merri Creek in 1976-78, and occasional failure to comply with the EPA SEPP in the 1979-81 data. More recently, the Victorian Water Quality Monitoring Network data (Hunter & Zampatti, 1994a; VWQMN, 1995) showed levels of salinity that often exceeded the EPA SEPP, particularly at Campbellfield where more of the flow originates from the groundwater. Mitchell & Dunn (1993) reported an increase in salinity downstream along the Merri Creek with highest levels between Barry Road and Mahoneys Road, and higher levels in the Merri Creek than in Edgars Creek.
Litter
According to community consultation, litter is one of the most serious problems facing the Merri Creek (Jan Bruce & Assoc. Pty Ltd, 1993). For aesthetic reasons, litter is one factor that may limit peoples' appreciation of the creek corridor and ultimately their level of commitment to its preservation and restoration.
An EPA report from 1979-1981 (EPA, 1981), noted that the Merri Creek fails to meet the EPA SEPP draft guidelines for litter.
A 1987 study "Litter Control in Urban Waterways" carried out a quantitative study of the litter problem in the Merri Creek, and is believed to be the first study of its type in Australia. It involved the identification of litter types and sources, assessment of a variety of simple litter trap devices and the development of recommendations arising from these investigations and associated recommendations. An analysis of the litter caught in the traps classified 66% as general plastics. Further classification of the trapped litter into 56 categories found that 59% of this litter was made up of 5 types of item; plastic bags, plastic sheeting and film, plastic confectionery and crisp wrappers, take away food containers and free distribution items. This study produced eleven recommendations and an action plan. While a number of the actions have been implemented, litter in the Merri Creek is still a major problem.
The Water Quality Concept Plan (Mitchell & Dunn, 1993) again noted that the Merri Creek "would be likely to fail the 'no visible floating matter' criteria for floatable matter". The great amount of litter remaining caught on riparian vegetation during periods of high flow is a problem that needs addressing, if creek restoration is to be realised.
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Table 7 Water Quality Parameters as Indicators a. Physical Parameters Parameter Indicator of Potential impact Possible cause
Suspended Plant Matter, sand, May smother benthic • Catchment erosion; Solids silt and clay. Is a organisms, plants, & • Inappropriate land measurement of fish, habitat, eggs, & use coupled with concentration or respiration. A inadequate stream- load, and doesn’t transport medium for side vegetation. indicate ‘cloudiness’. phosphorus and heavy metals. Turbidity Water ‘cloudiness’, Reduces light As above indicating the penetration & limits presence of photosynthesis. This suspended or limits animal food colloidal matter sources. Temperature Temperature Fauna and flora have • Seasonal fluctuations specific temperature fluctuations; tolerances. May • Stormwater; effect other • Industrial waste; parameters. eg • Sewage effluent. dissolved oxygen. Electrical Salinity Important • Clearing of trees; Conductivity determinant of fauna • Irrigation. and flora distribution. b. Chemical Parameters Parameter Indicator of: Potential impact Possible cause
Phosphorus Nutrients; Promotion of • Pastures of N-fixing Nitrogen Algal growth. excessive plant legumes; growth, leading to: • Fertilisers; • toxic algal • Treated sewage; blooms, making • Plant debris. water unsafe for human and animal consumption • alteration of the macroinvertebrate community structure. pH Acidity/alkalinity May alter toxicity of • Alkalinity-HCO3, other pollutants. ammonia (natural); eg acidity increases • Acid rain. metal toxicity
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E. coli Faecal Restrict use of water • Sewerage leaks and contamination; for recreation, due to overflows; Human pathogens. health risks. Increase • Diffuse source BOD and are harmful inputs of animal to aquatic life faeces. Biological oxygen required by Affects levels of • See causes for Oxygen biological processes dissolved oxygen nutrients and E. Demand (BOD) in water coli.
Heavy Metals Lead, zinc, copper, Occurs naturally but • Mining; arsenic, cadmium, high levels from • Industrial waste; chromium, mercury, human activities • Urban runoff; etc. accumulate over time • Sewage effluent. and are toxic to human and aquatic life Toxicant Summation of effects Toxicants present As above. Mixture Ratio of various toxicants together often have additive toxic effects
Dissolved Oxygen
Levels of dissolved oxygen in the creek are an area of possible concern. While recorded levels have generally been within the EPA SEPP recommended levels, there is some indication that this may not always be the case. Dissolved oxygen levels fluctuate throughout the day, with highest levels usually occurring in the afternoon and lowest levels occurring at night. Assuming that monitoring usually occurs during daylight hours, actual levels may fall below acceptable levels at night and therefore may not be sufficient for fish survival.
The PIRG study noted extremely low dissolved oxygen levels in the creek at Mahoneys Road in 1974. The EPA study from 1976-1978 (EPA 1982) recorded high levels in summer, indicating excessive algal photosynthesis. This indicates potentially low DO levels at night (when photosynthesis stops and algal respiration starts). Recently, Ellett & Kingsley (1994) noted occasionally low levels of dissolved oxygen in the creek at Campbellfield.
Edwardes Lake has levels of dissolved oxygen below SEPP recommended values, especially below a depth of 1.5 metres (Gaal, 1994). This is probably due to the low levels of oxygen in the water feeding the lake from Edgars Creek, and a high oxygen demand due to the lake's organic sediments and algal activity.
Nutrients
A high level of nutrients in the Merri Catchment is likely to be one of the most serious problems facing the aquatic health of the creek. The PIRG study in 1974 noted eutrophication at Craigieburn Road East. The EPA data consistently recorded high levels of nutrients in the creek. The 1976-1978 EPA study noted significant levels of nutrients, with high levels of phosphorus associated with the Somerset Road drain. For the 1979-1981 EPA
Page 72 State of the Environment - Water Quality study, the Merri Creek failed to comply with the EPA draft SEPP for phosphorus, nitrogen and macrophyte growth levels. More recently, Mitchell & Clark (1991) noted high levels of nutrients at all sites, both from chemical measurements and according to biological indicators (diatoms). Mitchell & Dunn (1993) indicated that the Craigieburn Sewage Treatment Plant was an important source of nutrient pollution of the Merri Creek, but that levels 'assimilated' to some degree further downstream. Levels again increased downstream of Ainslie Road drain and Central Creek, indicating these as potential sources. A study on levels of pollution in urban stormwater (Weeks, 1982) indicates that stormwater is a significant source of nutrient pollution. Ellett & Kingsley (1994) recorded high phosphorus levels, but noted a slight improvement since the 1990 data. However, care must be taken when making such comparisons given the different sampling times, techniques and sites. VWQMN data from the period 1992-1994 (Hunter & Zampatti, 1994a) indicated that total phosphorus levels at both the upstream and downstream sites, exceeded the Australian Water Quality Guidelines and the quantitative levels outlined in the new draft SEPP for the Yarra Catchment on all occasions. Likewise, the levels of nitrates from the upstream site (Campbellfield) exceed the new SEPP levels set for total nitrogen for 50% of the samples, whereas the downstream site (North Fitzroy) exceeds these levels on one occasion.
Toxic algal blooms are recognised as a problem in Edwardes Lake. In summer, the high nutrient levels and the right temperature and flow conditions provide favourable conditions for algal growth. The levels of total phosphorus and total nitrogen measured in a 1993/1994 study (Gaal, 1994) often were close to or exceeded the values at which eutrophication may be expected to occur. While drains within the lake are a source of nutrients, the major input appeared to be from Edgars Creek. High phosphorus levels were also recorded in the Lake sediments and may also be a potential source of nutrients to aquatic plants and algae. pH
Most studies of the Merri Creek have noted that the pH of the water is neutral to basic, and generally within the EPA SEPP acceptable levels. EPA data from 1973-1974 (EPA 1975) recorded pH levels of 5.0 (acidic) in June and July 1973, outside the now acceptable SEPP range of 5.5 - 9.5, and noted that pH levels were occasionally unacceptable. Mitchell & Dunn (1993) noted a pH of 9.3 (basic) in Edgars Creek in 1992, a level just within the EPA’s upper limit of 9.5. Acidity is an important factor affecting the mobility of heavy metals in stream sediments and changes to the pH could release contaminants into the water column.
BOD
BOD was not measured in all the monitoring studies in the Merri Catchment. The PIRG report recorded BOD levels in 1974 and recorded high levels at Craigieburn and very high levels at Mahoneys Road. At this time, the creek passed through several unsewered areas, and organic pollution (and therefore oxygen demanding substances) within the creek was high. The EPA data from 1976-1978 noted high levels of BOD from the Somerset Road drain, but also noted that levels of E. coli were acceptable. Recent reports (Mitchell & Dunn, 1993) note that organic pollution in the creek has decreased to some extent since the 1970s, possibly due to most of the catchment being connected to sewer. However, the problem still exists.
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Heavy Metals
Heavy metal contamination has been the subject of a detailed study as a part of this report. This section is therefore more detailed than for the other indicators of water quality.
Background: Heavy metals occur naturally in the environment, but high levels resulting from human activities are toxic to aquatic life. Monitoring heavy metals in the water may detect recent pollution events, but if sampling does not take place soon after the time of the polluting event, these high levels may not be detected. Heavy metals bind to fine particulate matter in the water and settle to the bottom of the stream, becoming incorporated in the stream sediment. Monitoring stream sediments therefore gives a more long term view of the levels of heavy metal pollution in the creek
Once bound in the stream sediments, the heavy metal contaminants may become less available to impact on aquatic life. However, there is a threat that these toxic metals may still have the potential to impact on the aquatic ecosystem by remobilisation into the water column in a number of physical, chemical and biological processes.
Metals in the water column: A number of surveys have recorded high levels of heavy metals in the waters of the Merri Creek. EPA data from 1979-1981 (EPA, 1981) noted that there was poor compliance with the toxicant mixture ratio (a measure of the cumulative effect of several heavy metals and other toxic pollutants), and high levels of zinc and copper. Campbell (1982) recorded high levels of lead, zinc, copper, chromium and mercury. More recently, Mitchell & Clark (1991) recorded high levels of arsenic, chromium, iron and zinc in the waters of the Merri Creek. Arsenic levels were much higher than had previously been recorded. Mitchell & Dunn (1993) noted high levels of chromium and zinc in the water column on the one sampling occasion.
Metals in sediment (past studies): Toxic heavy metal pollution of the sediments of the Merri Creek and Edgars Creek has only recently been recognised as a serious threat to the aquatic health of these waterways (Mitchell & Clark, 1991). Measurements of heavy metal contamination of the sediments of the Merri Creek undertaken by Mitchell & Clark (1991) noted a large increase in the level of heavy metals between O'Herns Road and Barry Road, at the point where the creek enters the industrial area. Levels of cadmium, zinc and copper increased seven to eightfold, whereas lead increased by a factor of twenty-six. The 1991 report noted that this increase in the level of heavy metals coincided with the major decline in the abundance and diversity of the macroinvertebrate community and concluded that the heavy metal contamination was having a substantial impact. Mitchell & Dunn (1993) noted high levels of arsenic in sediments in the rural segment at Summerhill Road, and high levels of copper, lead and zinc further downstream in an industrial area. This 1992 study also recorded moderate to high levels of heavy metal contamination in Edwardes Lake for copper, lead, zinc and chromium. Due to the higher levels recorded upstream of this lake, it appears that Edwardes Lake is acting as a sink for heavy metal pollution of Edgars Creek.
Metals in sediment (1995 study): To further investigate the impact of heavy metal contamination on the aquatic health of the Merri Creek, some sediment sampling was undertaken in April and August 1995 the results of which are included as part of this report (c.f. Roy, 1996). The aim of this research was to identify the nature of the metal-sediment interactions in the Merri Creek in order to predict the potential availability of the heavy
Page 74 State of the Environment - Water Quality metals to act as contaminants. The information in past studies has only given information on the total concentration of metal contaminants in sediments, which is usually an over- prediction of the availability of the contaminant. This study identified the relative association of the contaminant heavy metals to different phases of the creek sediments, thereby giving some indication of their bio-availability and the factors most likely to cause remobilisation of the heavy metal contaminants to the water column. The creek sediments are described in terms of the type association that binds the metals to the sedimentary particules. Four different phases are found; organic, exchangeable, reducible and residual.
This research consisted of three stages; the first of which involved an analysis of the total heavy metal concentrations in sediments at seven sites on the Merri Creek and one site on Edgars Creek. The second stage involved an analysis of the partitioning of heavy metals within different phases of sediment whilst the third stage examined one element in order to develop a model that broadly predicts the heavy metal availability in the Merri Creek.
The findings of this study agreed with those of Mitchell & Dunn (1993), showing that metal concentrations generally increase downstream along the Merri Creek, with major increases in concentrations being recorded at Barry Road (site APR4, Map 6), the results of which are listed in Appendix 5. A comparison of heavy metal concentrations at each site along the Merri Creek is presented in Figure 2.
At present there are no Australian criteria to determine the acceptable levels of heavy metals in the stream sediments to protect environmental values, hence it is difficult to assess the importance of this contamination. A number of Australian sediment assessment studies (including Sinclair Knight & Partners, 1991; Mitchell & Dunn, 1993) have used the Ontario Limit of Tolerance Levels as the comparison levels. The Ontario sediment guidelines are listed in Appendix 6 along with the levels indicated in Figure 2 (when Ontario levels are exceeded) as a means of assessing the severity of heavy metal contamination of the Merri Creek sediments.
While it is understood that these guidelines may not be directly applicable to Australian conditions, they are well in excess of the levels set in the other existing criteria listed in Appendix 6 and are, therefore, probably a fair estimate of levels at which serious impacts on ecosystem health may occur. Of course, it is possible that these metals may affect ecosystem health at far lower levels than this, and caution must be used in managing toxic contaminants.
Results from the April 1995 study add further support to the data collected previously and show the consistently high level of the heavy metal contamination of the streambed sediments over a number of years. The metals with high concentrations in this study are the same as those of the previous studies and the recorded levels are similar. Copper, lead, zinc, and to a lesser extent, chromium, are consistently high in all studies of metal contamination in the sediments of the Merri Creek. The contamination in Edgars Creek is less consistent but very little monitoring has been done there, so it is difficult to make such comparisons. Insufficient information exists to determine trends in heavy metal levels from recent studies. A long term monitoring program with consistent sites and methods will be required if this is to be known.
Of particular interest in the April 1995 study is the high levels of mercury in the creek sediments, in particular at Barry Road (Site APR4) and Broadhurst Avenue (Site APR5).
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Map 6 Sediment sampling sites 1995 heavy metal study.
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Results from the sequential extraction analyses in August 1995 also noted high levels of mercury at Barry Road but levels at all other sites were below detection limits. The levels of mercury recorded at Barry Road in April and August were 2.9 and 18.3 mg/kg respectively. These are very much higher than the Ontario ‘severe effect’ level of 1.7 mg/kg. Barry Road was the site of severe increase in the levels of heavy metal contamination indicated in the 1990 and 1992 studies but neither of these studies analysed the sediments for mercury concentrations. The 1982 EPA study of the Merri Creek (along with other studies of urban waterways in Melbourne) indicated that mercury pollution was not a problem in these type of streams and so it was not monitored in the 1990 and 1992 studies (Mitchell P., pers. comm.). A more recent polluting event may be contributing to these high levels recorded by Roy (1996).
The second stage of the 1995 study involved a sequential extraction of the metals from the sediments sampled from four sites on the Merri Creek (Map 6). The sequential extraction technique gives some further insight into the bioavailability of the metal contaminants by using the sequential addition of specific reagents which are designed to selectively remove the metals bound to the different phases of the sediment. Each reagent theoretically removes metals from each of the sediment phases based on the type and strength of the interaction. The operationally-defined phases are exchangeable, reducible, organic and the tightly bound residual metal. The exchangeable phase represents those metals that are loosely bound to the sediment and in equilibrium with the water column. Changes in the concentration of metals in the water column will therefore affect the amount of uptake or remobilisation of metals from this phase. The reducible and organic phases of the sediment are approximately equal in their ability to bind heavy metals, but the strength of binding differs under varying environmental conditions. The metals associated with the reducible phase are most likely to be released if the redox potential is significantly reduced, such as when the dissolved oxygen content of the water/sediment is lowered to approximately <1mg/l. The metals associated with the organic phase are most likely to be released if the pH of the system is reduced. The metal bound in the residual phase are highly stable and unlikely to be remobilised under any environmental conditions likely to occur in the Merri Creek.
Sequential extraction results from the four sites sampled on the Merri Creek in August 1995 indicate that a number of the metals have considerable potential to be remobilised These results are listed in Appendix 8 and presented graphically in Appendix 9. The results for each element found in high concentrations in Merri Creek sediments (chromium, copper, lead, mercury and zinc) are discussed in detail below.
Chromium:The distribution of chromium was similar in the sediments from all four sites sampled. Approximately 50-70% was associated with the residual phase, 20-30% with the organic phase, and very little chromium associated with the exchangeable and reducible phases. Total chromium concentrations are fairly high in the Merri Creek sediments, and were above the Ontario ‘severe effect’ level in the 1992 study.
Copper: High levels of copper have been found in Merri Creek sediments in all studies. At the highly contaminated sites at Barry Road (AUG3) and Rushall Station (AUG4), there is an increase in the proportion of copper associated with the reducible and exchangeable phases compared to the less contaminated sites (AUG1, AUG2). Barry Road sediments had a total concentration of 135 mg/kg and 150 mg/kg recorded in August 1995 and April 1995 studies respectively. While the spatial variation in the sampling point may mean that these values are not significantly different, they both exceed the Ontario ‘severe
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Figure 2 Concentration of metal in sediments downstream along Merri Creek (April 1995)
8