Mr Dutton has chosen Callide in Central Queensland as one of his putative 'locations' to build Federal Government nuclear power stations. Since I personally designed a number of the surface facilities on this site, thought you might be interested in a run-through.
It's a congested, hilltop site. There are three power stations, two of which still operate, sometimes -- Callide B and Callide C. Despite being separately owned, the generators for those two are actually co-located in the same extended shed.
I suppose you could find a place there somewhere to put a 500-1000 MW nuclear unit -- perhaps up near the old Callide A site, which plant has still not been demolished and rehabilitated, many years after it closed. (It was for a time used for abortive carbon capture experiments.)
This power station cluster is located where it is because it's beside the Callide coal mine, now run by a little private operator called Batchfire Resources. The site has no other major advantages. google.com.au/maps/@-24.3212…
Actually it had significant disadvantages that needed to be overcome in the original design: 1. It's a long way from the load centre in South East Queensland. Solved with strong grid connections -- to Gladstone PS (then existing), Boyne Smelter, later Stanwell PS (Rockhampton).
Dutton is correct to view those as a current *advantage* of the site. 2. It's in an important agricultural area, Callide Valley, with the available irrigation water supply (from two existing dams, Callide and Kroombit, and from groundwater) heavily overcommitted.
These are thirsty evaporatively cooled power stations (note the cooling towers above). They need lots of fresh water. That was solved, for Callide B and C at least, by a part-distance pipeline over the Great Dividing Range from Awoonga Dam near Gladstone:
A nuclear power station on this site would also be evaporatively cooled, and at least as thirsty. 3. The site is hard-adjacent to the upstream edge of the agriculturally important Callide Aquifer. Protecting it was a significant concern, and would also be for any nuclear unit.
It's not widely appreciated that evaporatively cooled thermal power stations, coal-fired or nuclear, are significant generators of wastewater -- not especially toxic wastewater, but *salty* (technically, 'cooling tower blowdown'). That is generally just discharged, under licence.
At Callide that was not acceptable, because the downstream aquifer is already salty -- too salty to irrigate some crops. So, unlike (then) every other power station in Australia, Callide was design for on-site salty wastewater disposal, via extensive hillside evaporation ponds.
There are now other ways to do that (reverse osmosis with brine crystallisation), which might be used for an evaporatively-cooled nuclear unit here.
Is this a good site for a nuclear power station (leaving aside that other question)? Not imo. This is the driest lived-on continent on Earth. Inland evaporatively-cooled thermal power stations (nuclear!) are immensely thirsty machines. That's not a wise use of scarce fresh water.
(Correction: That's not actually the Great Dividing Range mentioned above; it's much further west. But it is a helluva big hill.)
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Why is it so? To get far there you'd first have to admit that the misfit is real, and the modelling community is still clutching it's 'uncertainty band' pearls, and denying the appropriateness of non-linear observational models.
It's correct that the IPCC 'middle projections' carry substantial uncertainty, but those are the numbers, right there in the great big report (Table SPM.1, below). It's odd that no one much bothers to refer to them.
Here's the two graphs to the same scale, for direct comparison:
What about this, for the whole planet? Properly interpreting and understanding this dataset is tricky.
This is actually seasonally adjusted (not anomaly from an adopted climatology, which is what is labelled 'deseasonalised' on the CERES site):
Rocky planets everywhere are radiation balance engines. Their surface temperature – or atmosphere temperature, if they have one – depends on a fine balance between incoming radiation from their star(s) and outgoing heat radiation to space, mostly in infrared ('longwave').
Around the world, most valley glacier terminal lakes like this have appeared in the last ~half-century of heating (since ~1970), as the glaciers retreated. Here's the largest such glacier in our region -- Tasman Glacier in NZ:
Its large terminal lake was completely absent in 1970. We know because the New Zealand Department of Lands and Survey made an excellent topographic map of the glacier snout, as it was then:
1. It's not particularly small. At 200 MWe, this is about one-fifth the size of the last conventional reactor commissioned in the world -- Vogtle 3 in the US, in July (1100 MWe). That was 7 years late and ~ x5 over budget.
2. It's not particularly modular. The reinforced concrete containment building is being constructed on-site, in situ, as is conventional. Yes the reactor pressure vessel was fabricated in a factory, delivered on a special transporter and is being craned in; they always are.
This is quite an interesting read. Have to admit to never looking much at #SMR's (why would you; it's a deliberate distraction, probably run by the same fossil-industry misinformation team). But, as may know, cannot resist things technical, especially in a field I've worked in...
...Power engineering -- coal-fired, not nuclear -- though have had some long-term interest there too. The link is to a 2019 design parameters summary for one proposed design, Rolls-Royce's 'UK SMR', which may or may not be typical of the 'class': aris.iaea.org/PDF/UK-SMR_202…
That has had a long gestation (commencing 2015), largely funded by the UK government. It's reportedly one of at least 3 likely candidates for the UK's recently announced SMR design competition, which might be more about an election next year than much else...