Suffice to say it was a wonderful Test Match accompanied by
some tremendous hospitality from my South Australian Cricket Association (and
wool industry) friends.
To summarise my day at the Lower Lakes, I can only say I come home greatly enthused by the beauty of the area, enthused by the history and its preservation, and the wonderful water body; yet aghast at the waste of fresh water when it is so obvious that even better environmental outcomes could be achieved with the judicial use of healthy, oxygenated seawater with a concomitant reduction on the demand for upstream fresh water.
When you consider this in the context of the Murray Darling
Basin Plan it is simply outrageous that the issue of better management (and
upgrading) of the Barrages has not even been properly debated. It is not
overstating the “final” position of the Plan to say that it has the supply of fresh
water to the Lower Lakes as its prime objective.
There is absolutely no reason why the objectives for the
environment and recreation, with irrigation needs and Adelaide water needs
covered from upstream fresh water extractions, can’t be achieved with
downstream seawater. Studies of tidal inflow movements, even when 80 gigalitres
a day had been flowing to the Southern Ocean, have demonstrated the capacity,
with Barrage manipulation, to use seawater to continue to hold the Lake level
at the usual .75 metres above sea level and thus achieve the basic objective.
Furthermore, such a return to a more estuarine situation would have the added
environmental benefit of re-introducing the marine biota which contributes so
much to the character of estuaries. An additional Lock would almost certainly
be necessary to prevent sea water intrusion, in low flow conditions, up the
main stem of the river.
Clearly the Barrages need to be “upgraded” to allow more cost
effective management including the capacity to make it possible to periodically
release substantial surges from the elevated Lake so as to keep the mouth to
the ocean open. It will probably also be necessary to excavate much of Bird
Island which has built up since the building of the Barrages in the 1930’s. I
was surprised to discover that the Barrages are managed by the Murray Darling
Basin Authority. I had always assumed that they were managed by the South
Australians.
My ‘Australian Little Oxford Dictionary’ defines a “barrage”
as “an artificial barrier in a river”. A “weir” is generally accepted to be a barrier
which can be over-topped by water flows e.g Hume Weir. The term “dam” is
usually used to describe a blockage in a water course to hold back water. It
may be overtopped by big flows or have other means of allowing big flows to
pass-pipes or spillways. In many areas the word “dam” is used to describe what
is also called a “tank” (earthen) which is an excavated hole in the ground to
capture water where there is no natural watercourse. The term “sea dyke” has
also been used to describe the Barrages. A ‘sea dyke’ is usually used to
describe a barrier to seawater intruding over land wanted for other purposes eg
in low lying countries like Holland. On the Murray we also have a series of
‘locks’. These may also play the role of a dam, but always with the capacity to
allow boats to get through.
So what is the right word to describe the Barrages? They were
originally designed to store fresh water, principally for irrigation. A purpose
since replaced by the piping of fresh water from upstream. They were built with
a beautiful flexibility to change their height as desired by the lifting or
adding of concrete panels (Goolwa Barrage). Their construction brought with it
the secondary impact of keeping seawater out so in that sense they are ‘sea
dykes’. So when one considers all that, the word “barrage” will do me.
To my mind, the two most important principles in water
management to deal with Australia’s notorious climate variability are conservation (ie to conserve water from
big flows) and flexibility. The
Barrages with their modular construction strike me as meeting these principles
perfectly, albeit the purpose of conserving water is somewhat different to the
usual objective.
One further important factor that my Goolwa visit brought to
mind was the huge impact that wind can have on water movement. When the south
westerly winds get up, particularly at high tides, they can drive seawater into
the Lakes even when there are substantial flows of fresh water coming from
upstream. Providing the Barrages can be lowered and raised quickly this water can be
captured to maintain the elevated level. In very low flow times it might be
difficult to maintain the full .75metre elevation, but with the use of seawater
at least the emergence of acid-sulfate soils could be avoided by keeping the
lake bed inundated.