Water

Was it former Soviet President Mikhail Gorbachev, Australian Democrat Senator Andrew Bartlett or Parliamentary Secretary to the Prime Minister Malcolm Turnbull?

Who convinced Queensland’s Premier Beattie to change his mind on recycling sewage as a source of drinking water?

They have each visited my home town of Brisbane over the last week and each publicly announced their support for the concept.

Now the Premier says he’s going to put the idea to the people of Brisbane.

That is quite a back flip.

Until recently Peter Beattie had been promising new dams, desalination plants and even piping water over 1,000 kms from the Burdekin to fix Brisbane’s water shortage, but had ruled out waste water recycling. Now he says recycling is a possibility – that he will make it an election issue.

You can read about Andrew Bartlett’s petition in favor of recycling at his website and Mikhail Gorbachev and Malcolm Turnbull’s comments in The Australian here, here and here.

I attended the Brisbane Institute last night to hear Malcolm Turnbull speak and he really was eloquent. On the subject of recycled water he suggested that:

“We must learn to judge water by its quality, not its history”.

He also commented that permanent water restrictions in Brisbane make no more sense than would permanent electricity restrictions. He indicated that the current water restrictions reflected a lack of investment in infrastructure by state governments and spoke about the referendum on waste water recycling in Toowoomba this Saturday.

I wrote in support of sipping sewage in last week’s The Land and blogged on the issue last August.

Ian Mackay [1] has just returned from visiting south east Queensland’s many water storages. He clocked up 1,800 kilometres over the four days and this is what he found:

1. In pictures: http://www.stoppress.com.au/ .

2. In words:

“Dam after dam, dams well away from areas of population pressure, were well below critical level. Several were even at zero.

It was seeing the two and a half metre tree growing just a little above the waterline at Moogerah Dam, though, that really drove it home.

Plainly the dam hadn’t been filled beyond this level for years.

Dates scrawled at the side of the spillway wall, indicating when the dam had overflowed only confirmed it. There was the mark for the memorable Australia Day floods of 1974, but nothing after 1976. The towering, impressively curved dam wall, tightly wedged between two massive hills, had been touted as something of an engineering feat when completed in the early sixties.

Despite all the hopes behind its construction, it was clear that it had been holding back a dwindling water reserve for years.

Moogerah Dam — the name means either “place of storms” or “meeting place of storms” depending who you ask — is currently holding only 7% of its capacity.

The water ski cottages hugging what was once its shore line and the twice-extended boat ramp tell the tale of a water level that has receded over a much longer time period than just the last few years.

One friend tells me of watching enormous eels thunder over the spillway back in the early seventies. Another speaks wistfully of water skiing over the top of what is now a great isthmus jutting into the dwindling pond. Tall grass now covers the spillway area and fishermen drive the considerable length of the isthmus to cast a line. Pelicans, stilts and cormorants share the receding shoreline with grazing cattle in scenes that wouldn’t be out of place around a drying billabong much further inland.

But Moogerah is far from alone.

Most of the Sunwater storages throughout the southeast are well under a third full [2].

Nearby Maroon Dam, which also drains the impressive towering peaks of the Border Ranges stands at 21%; Bjelke-Petersen Dam collecting water from a wide catchment in the South Burnett, including the Bunya Mountains holds just 3% of its 125 000 megalitre capacity.

Atkinson Dam, near Lowood is at 0%; its picnic grounds understandably deserted, its remaining water puddle far off in the distance behind the water skiing signs.

All these dams share a common thread of optimism, the hope that the provision of a dependable water supply would somehow “drought-proof” the state and facilitate enhanced agriculture and easier living. To many who share this dream that dams equate to a certainty of water supply, the present crisis is wholly attributable to our not having added to our portfolio of existing dams.

Now, four decades on, it might be as well to reflect on the reality.

South East Queensland gets nightly updates of the levels of the major domestic storages. Somerset, Wivenhoe and North Pine Dams are collectively at around 29%. These figures look almost respectable compared to those previously mentioned, but anxiety about their low levels has lead to severe restrictions.

Property owners on the shores of Somerset Dam speak of having to regularly extend their fences out into what had been dam, of their cattle now grazing on land recently exposed and now covered in grass.

The simple fact is that our dams are failing us.

It’s not the engineers’ fault. They built dams that held back water when it rained, but there’s that other variable that is well out of the control of every engineer, and also, as he has repeatedly rued, our Premier.

“I can’t make it rain,” says Peter Beattie.

What he could do, though, is recognize that our water crisis comes from an almost total reliance on dams for water supply. Dams in the area of greatest population growth aren’t in fact the lowest. Changing rainfall patterns mean that Moogerah is getting fewer of the storms that gave it both its name and its desirability as a dam-site.

Instead, his assessment of the situation is that if our existing dams aren’t holding enough water, then plainly we need more of them……… if your wallet doesn’t contain much money, then obviously you need more wallets.

His newly announced additions include a mega-dam at Traveston across the Mary River, a smaller dam at Wyaralong across Teviot Brook near Boonah and raising of both Borumba and Hinze dams and a few other storages as well.

It’s an assessment he hopes will be shared by voters, at least those who still share that axiomatic “dam equals more water” connection. Many though, are questioning how dams that can’t possibly begin to fill until at least 2011 will be any use at all in a crisis that could well crunch in just two years time if significant rains don’t fall.

The Beattie government’s newest, the Paradise Dam that drowns the Burnett River, northwest of Childers, was recently named in an international list of failed dams. It was hoped that after the wall was completed last year, the dam would fill quickly but it is currently at only 15%. It is an expensive fulfillment (no pun intended) of an electoral promise for which we’ll still be paying years hence.

You can understand why there’s far more outcry about the Mary and Wyaralong Dams than from just those who stand to be displaced. Councils the length of the Mary have spoken out in opposition, and rural groups, environmentalists and church groups have added a long list of concerns.

Many are comparing Premier Beattie’s approach and vision to that of Joh Bjelke-Petersen.

Making the long walk, down through the cracked mud toward the receding shoreline of Bjelke-Petersen Dam, you can almost feel the vision splendid evaporating as surely as the dam’s contents.

While many farmers we encountered were making the most of the opportunity to excavate and deepen their dams in anticipation of eventual rain, no such activity was taking place in the bigger dams. It seemed it was simply easier to just build a new one.

At a time when most water authorities are diversifying their supply options, shouldn’t a first priority be reflecting on the success of the status quo?

The red dots tell the story.

Without good run-off rain, a dam is just an expensive wall.

It’s time we faced the fact that our dams aren’t working.“

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[1] Ian Mackay is a teacher, poet and environmentalist from the Mary Valley. For the last ten years he has been President of the Conondale Range Committee, one of the Sunshine Coast’s longest serving environment groups.

[2] Sunwater information comes from www.sunwater.com.au click on lower left hand information option.

The Macquarie Marshes is a large non-terminal wetland in central western New South Wales (Australia) recognised internationally as an important breeding site for migratory birds. The marshes are degraded and the popular perception is that upstream irrigators are to blame.

Most of marsh lands are privately owned and used for cattle grazing. There is a southern and northern nature reserve which together comprise 12 percent of the Macquarie Marshes and the only areas where grazing is excluded.

In my last blog post on the Macquarie Marshes entitled ‘Three Pressing Issues for the Macquarie Marshes’ I showed how a levy bank running across the southern boundary of the southern nature reserve is stopping water flooding into the nature reserve.

Some water does flow through the southern nature reserve by way of Monkeygar Creek.

Monkeygar Creek then flows through more private land before flowing into the Macquarie River and then the northern nature reserve.

Up stream of the northern nature reserve there are more levy banks and a rock wall across Monkeygar Creek, diverting more water to private grazing land.

It’s all much easier to understand on a map, which is exactly what Chris Hogendyk has sent me today in the following pdf file, CLICK HERE [3 MB file].

The pdf file includes pictures, published for the first time here today, of the illegal system of levy banks upstream of the northern nature reserve.

Chris Hogendyk was mentioned in the Sydney Morning Herald article of two Saturday’s ago entitled ‘Fat Ducks, Fat Cattle – Fat Change’. The article included the following comment:

“Hogandyk is chairman of the 600-strong Macquarie irrigator collective and a man who says saving the marshes is his great passion – “I think this is the one thing in my life where I can really make a difference to history.

… Hogandyk says the marshes still receive an average annual inflow that has only decreased by 15 per cent since Burrendong was built.

“A lot of the marshes were actually lost pre-dam due to grazing and channelisation. We are in danger of losing the marshes because the wrong solutions are being advocated.“

It’s easier to understand on a map and with pictures so CLICK HERE.

Its a 3 MB file, scroll down beyond the map to see the many aerial shots of the levy banks.

It was good to see Professor John Quiggin drawing attention to the problems with the Macquarie Marshes in his post of last Sunday titled ‘Macquarie Marshes again’.

But it’s a pity he can’t get beyond ad hominem attacks [1] and a pitch for his ARC fellowship, which is about trading water in the Murray Darling Basin. And it really is naive to suggest, as Professor Quiggin does, that we can “restore the Murray-Darling Basin to a sustainable balance” simply by taking water from irrigators.

Putting aside the question of whether environments are ever in ‘balance’, there are three particularly pressing issues for the Macquarie Marshes:
1. Getting water to the nature reserve including for the reed beds,
2. Preventing the trampling of bird nesting sites by cattle, and
3. Addressing the general issues of overgrazing.

The Macquarie Marshes is a large non-termial wetland in central western New South Wales covering about 200,000 hectares. Most of this area (88 percent) is privately owned and grazed. There are two publicly-owned nature reserves where cattle are excluded and which are Ramsar-listed, meaning they are considered of international importance for migratory bird species.

It is reasonable to assume that water taken from irrigators for environmental flow purposes will be directed first to these nature reserves. Yet both local graziers and upstream irrigators have sent me photographs and letters complaining that water is being directed away from the nature reserves to private land.

Following is a satellite photograph with the green area showing where the marshes flooded in December 1999. The yellow line shows the boundary of the southern nature reserve. It is evident from this photograph that something is blocking water from flowing into the reserve. This something is a levy bank on private land that according to the NSW government has been in place for approximately 15 years [2].

As I explained in an article recently published by On Line Opinion: “The only real monitoring of the biodiversity of the marshes has been the breeding of water birds. Bird-breeding sites were first mapped in the late 1970s. At this time the major breeding colonies were along the Macquarie River and most within the nature reserve. But over the past 30 years there has been a migration east to the Terrigal-Gum Cowal wetland, which is all on private land. The last big waterbird breeding event in the marshes was in 2000, and ten of the 12 main breeding colonies were located on private land with only two in the nature reserve.”

Local graziers tell me that when the birds breed in the nature reserve they are protected from the cattle, but when they are forced to breed on heavily grazed marsh lands their nests are often trampled. Fifty years ago there were restrictions on grazing on the private land in the marshes, in particular there was a regulation stating that all rookeries for bird nesting and breeding had be completely enclosed with a sheep and cattle proof fence. There are nolonger any such conditions.

Water has apparently even been redirected from the adjacent Marra Creek system through the recent construction of an additional weir, all on the pretext the water was needed for the marshes. Marra Creek graziers have subsequently watched the water directed not to the nature reserve, but to heavily grazed private land.

Not all of the private land within the marshes is overgrazed. But there was evidence of overgrazing when I visited the marshes last October and I have been sent photographs and emails from some upstream irrigators and some local graziers explaining to me that many areas, including areas that have received recent environmental flow allocations, are severely overgrazed. Here’s one of those photographs:

The evidence would seem overwhelming that all is not well in the Macquarie Marshes and that simply taking water from upstream irrigators, as suggested by Professor Quiggin, is not going to fix the problem.

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[1] It is also somewhat amusing that Professor Quiggin could suggest I’m against the grazing industry. I grew up with buffalo and cattle at Coomalie Creek in the Northern Territory and charolais at Conondale in south east Queensland. I was awarded the Cattleman’s Union Industry Research Medal in 1991 for my work in Madagascar, and was recently invited to speak at the annual Australian Beef Industry Dinner on 11th August.

[2] The levy is pictured at my blog post of 12 April 2005 titled ‘But Reed Beds Need Water’ along with comment from government officers, click here.

The following comments by Australian forester Frank McKinnell are based on three visits to the Aral Sea region between 2004 and 2006, including trips out onto the Dry Aral Seabed (DAS) on both the Kazakhstan and Uzbekistan sides of the border:

“The Dry Aral Sea (DRA) is one of two serious environmental problems that Kazakhstan inherited from the former Soviet Union, the other being the Polygon nuclear test site, near the city of Semey, where about 600 nuclear weapons were set off.

The Aral Sea lies roughly half and half in Kazakhstan and Uzbekistan, and in a region of largely flat topography, covered by shrubby steppe vegetation. At the present time (2006) it is about half the area it was in 1960 and the rate of drying up is continuing, at least in the southern portion. In some places the edge of the Sea is said to now be 200 km away from where it was in 1960. One can go to what were formerly seaside fishing villages and see marooned ex-fishing boats many kilometres out of sight of the water.

The Aral is fed by two major rivers, the Amur Darya (formerly known as the Oxus) and the Syr Darya. Since 1960 the rate of inflow into the Aral has been greatly reduced by diversion of the water into a series of ill-conceived irrigation schemes in Uzbekistan and Kazakhstan.

The irrigation schemes were ill-conceived in two ways:

• Part of the irrigated area was located on land that had a saline subsoil, with the inevitable consequence that groundwater tables rose, the salt rose to the surface, and the surface soil became saline. This is now largely wasteland.
• The main crops grown on the irrigated land were cotton and rice, and both had disastrous effects. The rice cultivation required huge volumes of water, which had adverse effects on the river flow, and exacerbated the rise of the groundwater. The cotton required heavy applications of insecticide, some of which washed out in the irrigation tailwater and ended up in the Aral Sea. When the Sea dried up, the chemicals remained in the sediments and were subsequently blown about in duststorms. This is widely believed to have had adverse effects on the health of people living downwind of the Sea, although definitive scientific studies to demonstrate this are so far lacking. People living in the region that I spoke with are emphatic that the incidence and severity of duststorms has greatly increased as the Sea dried up and that their health problems have become worse.

Despite the land management problems, large scale irrigated agriculture continues, for economic and social reasons.

As the sea retreated, it exposed a large area, now some 4 million ha, of flat or slightly undulating land. In some places it is mobile sand dunes, and in others it is heavier textured silty soils. There is a large area of the solonchak soil type, which is particularly difficult to work with, being both alkaline and saline. The salts in this case are both sodium chloride and sodium carbonate.

Figure 1. Newly exposed seabed

Figure 2. After a time sand dunes develop, but the depressions usually have solonchak soils.

The prospects for improving the condition of the DAS are severely limited by the extreme climate of the region. The annual rainfall is about 300mm and the climate is an extreme continental type, with temperatures falling to as low as -40ºC in winter and rising to +40ºC in midsummer. Furthermore, the wind strengths are very high, and make working out in the open almost impossible in the late afternoon, especially in winter.

The DAS does develop a vegetative cover naturally, starting with salt tolerant plants such as Salicornia, but the process is slow. The soils are quite variable and some types are very difficult to vegetate. Nevertheless some research in the early 1980s indicated that it was possible to speed up the rate of revegetation and achieve a more diverse plant assembly.

Figure 3. Natural revegetation.

The duststorms have been recognised as a problem for many years. In an effort to reduce their effect, a revegetation program was commenced in the 1980s, but this ceased, due to lack of funds, after the breakup of the Soviet Union in 1990. In the last 5 years, an aid project funded by Germany has been working on revegetation of the DAS on the Uzbek side of the border. The World Bank and the Government of Kazakhstan are jointly developing a similar project on the Kazakh side.

There are two possible approaches to the addressing the environmental issues arising from the DAS: try to refill the Sea again, and develop a vegetative cover on the exposed sea bed and so reduce the amount of dust transported by wind. Both avenues are currently being tackled. I should add that there is now a good deal of cooperation between Kazakhstan and Uzbekistan on this issue. While the level of cooperation might not yet be ideal, it does exist and is improving.

1. Refilling the Sea
In Kazakhstan, a EU-funded project is promoting more efficient use of irrigation water and supporting river bed improvement schemes that will increase the flow into the northern Aral. Similar work is under way in the irrigation areas fed by the Amur Darya in Uzbekistan, although the emphasis there seems to be more on changing cropping away from water-hungry rice to more water-efficient crops.

An overall review of the prospects for the Aral has found that there is no chance whatever of refilling the entire Sea in the foreseeable future. However, there is a good chance of partially recovering the northern section of the Aral, if the inflow from the Syr Darya is prevented from moving into the southern section. It has been decided that, on balance, a partially recovered North Aral is better than a devastated whole Aral. To this end, a dam is being constructed across a narrow neck of the Aral west of the town of Kazalinsk. I have not seen this dam myself, but have been told that the dam will raise the level of the northern Aral by about 12 metres. If so, a large part of the northern section will be restored, although salinity will probably be higher than in the Aral before 1960. In April 2006, people at Aralsk told me that the northern Aral had started to rise again.

2. Developing a Vegetative Cover on the DAS
The philosophy lying behind active programs to develop vegetative cover is basically that, left to itself, nature will do the job, but not very well and it will take an inconveniently long time about it. Therefore, some assistance to the process is justified. Research in the mid 1980s was able to develop methods of establishment of salt tolerant species on some of the soil types. This research has been continued by the German GTZ project in Uzbekistan and is intended to be a major part of the new project in Kazakhstan.

Figure 4. Research trial of saxaul (Haloxylon sp) about 6 years old. The need for a variety of other species for revegetation is apparent.

The idea of the revegetation programs is to hasten the rehabilitation process, which will bring about relatively rapid environmental benefits for the region, and also produce a more diverse ecosystem.

The long term use of the DAS has not been decided, but the thinking in Kazakhstan at the present time seems to lean towards making the area some sort of nature reserve. This would certainly provide the best protection for the soil, and so minimise the dust problem, but it will require attention to be given to control of wildfire, so that the soil is not bared once again. A wildfire problem on a former sea bed must be a unique situation!”

Thanks Frank McKinnell for sharing this information with us.