15.1 Surface
water quality
CICL’s surface water quality program is aimed at monitoring
supply and drainage water quality within CICL’s operational area, including at
the licensed discharge points. The program
monitors flow, turbidity, dissolved oxygen, pH, salinity and chemical levels at
various points in compliance with licence conditions. CICL’s water quality monitoring sites are shown in Figure 15.1.

Figure 15.1 Water quality monitoring sites
There are three licensed drainage discharge points and one
licensed monitoring point; Coleambally Outfall Drain monitoring site A
(CODA). It has been agreed that the
CODA site will no longer be a licensed monitoring point after 2000/2001. At the licensed sites the flow, salinity and
physical parameters of the drainage water are monitored continuously. Monthly water samples are collected from
these sites and are analysed for chemicals as required by the Environment
Protection Licence (EPL).
From October to December each year samples are collected
from 22 sites and are analysed for molinate levels as part of the Rice Chemical
Management Program (RCMP). Molinate
levels are used as an indicator of the presence of other rice chemicals in the
drainage water.
The Salinity Management Program involves weekly monitoring
of drainage and supply water salinity within CICL’s operational area. Fifty-six sites are monitored once a
week.
15.1.1 Drainage
flows, salinity and salt load
Drainage flow and salinity data are monitored continuously
at three licensed discharge points and one licensed monitoring point. The data from the licensed discharge sites
is transmitted to the DLWC offices at Leeton and Deniliquin in real-time
through radio signals. At the licensed
monitoring site, CODA, the data is stored in dataloggers and is downloaded
regularly by DLWC, Leeton.
Data recovery has not been consistent at these sites since
logging started in 1993. Due to various
problems, the logger may cut out at times, causing a loss of data. Table 15.1 shows that the
data recovery at the licensed discharge sites has been relatively good this
year with only Drainage Channel 800 monitoring site A (DC800A) falling below
the average for the last seven years. Table
15.2 shows that at CODA, data recovery has improved considerably this
season and is slightly better than the long-term average.
Table 15.1
Data Recovery Summary for CCD, DC800A and CODD
Table 15.2
Data Recovery Summary for CODA
For the purpose of this report, monthly flows and salt loads
were calculated by multiplying average daily flows and salt loads with the
number of days in the month. If no data
is available for a month the eight-year average of the data for the month is
used. Therefore only limited comments
are made and analysis of drainage data should be assessed carefully. Brief statistics on the drainage data at
licensed sites are attached as Appendix
B of the Reference Document.
Drainage flows at the licensed discharge points are shown in
Table 15.3 and drainage flows
at the licensed monitoring site, CODA, are shown in Table 15.4. These tables show the total monthly flow for
each site as well as the average monthly flows since 1993/94. All calculations have been made using the
monthly average multiplied by the number of days in each month. Calculations were carried out in this manner
as total monthly figures were not considered accurate as some daily readings
were absent. The licensed discharge
sites have been totalled to show the entire amount of drainage flows leaving
CICL’s operational area. The average
value for the month of September for site Coleambally Outfall Drain monitoring
site D (CODD) has been used because the data that was provided is currently
under investigation.
Table 15.3 Drainage flows (ML) at licensed discharge
points
Table 15.4 Drainage flows (ML) at CODA
The total average flow from CICL’s operational area since
1993/1994 is 94,323 ML per year. In
2000/2001 the total drainage flows were 98,961 ML, which is 105 percent of the
average figure. This total drainage
figure for 2000/2001 includes 55,808 ML of flows diverted for DLWC through the
CCD and DC800. Table
15.5 is a monthly summary of total drainage minus DLWC drainage
credits, which gives the total flows of actual drainage water from CICL’s
operational area. 1993/1994 drainage
flow do not include any flow for DLWC.
This change indicates a drainage efficiency improvement of around 50,000
ML since 1993/1994.
Table 15.5 Total drainage, DLWC drainage credits and
CICL drainage flows (ML)
Average monthly drainage water salinity readings at
the licensed discharge points are shown in Table 15.6. Salinity readings at the CODA site are shown
in Table 15.7. The
average salinity values in 2000/2001 were greater than the eight-year average
figures shown. However, the median
salinity was less. This is due to the
fact that winter salinity readings have increased and irrigation season
salinity readings have decreased.
Table 15.6 Monthly salinity readings (mS/cm) at licensed
discharge points
Table 15.7 Monthly salinity readings (mS/cm) at CODA
The salt loads at the licensed discharge points are shown in
Table 15.8. Salt loads at CODA are shown in Table
15.9. All calculations have
been carried out by multiplying the monthly average by the number of days in
each month. This was carried out
because some daily readings are absent, and total monthly figures are therefore
not considered accurate. Figure
15.2 shows
the trends in drainage flow and salt load at the licensed discharge points for
the last five years. The data for this
figure was calculated by working out the difference between the total flow for
the licensed discharge points and the DLWC credits. This data shows the true trends for drainage flow and salt load.
Table 15.8 Monthly salt load (tonnes) at licensed
discharge points
Table 15.9 Monthly salt load (tonnes) at CODA
Figure 15.2
Total flow and salt load from CICL after adjusting DLWC drainage credits
In total 50,540 tonnes of salt was imported into CICL’s
operational area
(see Table 15.10). However, this figure also
includes the salt load contained in diversions for Tombullen Storage. Table 15.11 shows the flows
and salt loads diverted to Tombullen Storage.
In 2000/2001 CICL’s operational area imported a net salt load of 31,039
tonnes of salt. This is calculated by subtracting
the total salt load diverted to Tombullen Storage and the total salt load
measured at the three licensed discharge points from the total salt load
entering the area through the supply system.
Table 15.10 Monthly diversions, salinity and salt loads of water entering
CICL's operational area in 2000/2001
Table 15.11 Salt loads diverted to Tombullen Storage in
2000/2001
15.1.2 Drainage water salinity within the CIA
CICL’s internal Salinity Management Program involves
salinity monitoring at 56 sites once a week.
Each site is located at the bottom of a sub-catchment, enabling
management to focus on particular catchments showing continuously high salinity
readings. Table 15.12
is a summary of the program since 1997/1998.
The data has been separated into irrigation and non-irrigation
seasons. It is important to split the
data in this way due to the large decrease in flow during non-irrigation. This leads to higher salt concentrations due
to the intrusion of groundwater and the increased presence of stagnant water.
Table 15.12 Salinity management program summary
The table shows that there has been a decrease in the
proportion of samples exceeding 1,000 mS/cm
during the 2000/2001 irrigation season.
The proportion of samples less than 400mS/cm have increased during
2000/2001 irrigation season. This is
also illustrated in Figure 15.3, which shows overall improvement
in salinity management within the CIA.
This data is also consistent with the decrease in the median salinity
values at the licensed discharge points.
Figure 15.3
Proportion of samples less than 400 mS/cm and greater than 1000
mS/cm
(irrigation season)
15.1.3 Indicative
water balance
Indicative
water balance shows that there has been significant improvement in water
availability and its management. Total
diversions and deliveries increased from last season. The conveyance efficiency also increased from last season and was
higher than the average of the five seasons from 1996/97 to 2000/2001. Escape flows, system losses and gains were
close to the five-year average.
Table 15.13 Indicative summary water balance
15.1.4 Nutrients, turbidity and pH
Measurements of nutrient load, turbidity and pH have been
taken at six sites in the drainage and supply systems. These sites are for drainage; CODA, CODD,
DC800A and CCD; and for supply; CCS and CE260-2.
Total phosphate and nitrogen have been measured and graphed
for both the supply and drainage systems.
Figure 15.4 and Figure 15.5 show the
total phosphate at the drainage and supply sites respectively. Total nitrogen has also been graphed for the
drainage (Figure 15.6) and the supply (Figure
15.7) systems. In all four of
these figures the Australian and New Zealand Environment and Conservation
Council (ANZECC) recommended guidelines for each parameter have also been
included. The recommended guidelines
show concentrations that are provided as an indication of levels at or above
which problems have been known to occur, depending upon a range of other
factors (ANZECC, 1992).
Figure 15.4 Total phosphate at drainage sites
Figure 15.5 Total phosphate at supply sites
Figure 15.6 Total nitrogen at drainage sites

Figure 15.7 Total nitrogen at supply sites
The recommended guideline is an indication only of nutrient
levels. It is recommended that more
site-specific analysis should be carried out before a guideline is strictly
enforced. For this reason a seasonal
comparison of total phosphate and total nitrogen has been carried out. Table 15.14 is a summary of
total phosphate at the various sites from the years 1998/1999 to 2000/2001. Table 15.15 is a summary of
total nitrogen for the same sites.
Table 15.14
Total phosphate summary (mg/L)
Table 15.15
Total nitrogen summary (mg/L)
Turbidity has been measured at each of the six sites using a
field meter. Figure
15.8 and Figure 15.9 are graphical representations of
the turbidity within the drainage and supply systems. These charts show that the turbidity in the supply system remains
fairly constant throughout the year whereas the turbidity in the drainage system
varies considerably. Table
15.16 also shows the large variation that occurs within the drainage
system compared to the supply system.
ANZECC guidelines for turbidity recommend that seasonal mean
nephelometric turbidity units (NTU) should not change by more than 10 percent
(ANZECC, 1992).
Figure 15.8 Turbidity at drainage sites
Figure 15.9 Turbidity at supply sites
Table 15.16
Turbidity summary (NTU)
The alkalinity or pH of the supply and drainage water is
also measured at each of the six sites using a field meter. Figure 15.10 and Figure
15.11 present the pH readings at the drainage and supply sites since
July 1997. Both systems exhibit similar
trends, with pH rarely exceeding nine or falling below seven. This can also be seen in Table
15.17, which summarises the data from the years 1998/1999 to
2000/2001.
Figure 15.10 pH at drainage sites
Figure 15.11 pH at supply sites
Table 15.17
pH summary