Carbonscape and the new Victorians

Buried among the emails which accumulated while I was in hospital was one from Carbonscape, the NZ company working on biochar, drawing my attention to an article in the UK Sunday Times. It missed proper attention until I tidied up my inbox yesterday, but even a few weeks late I think it’s worth reporting, especially as Hot Topic has posted on Carbonscape previously (here, here and here).

The Sunday Times article contained interviews with a number of people it described as the new Victorians, meaning modern-day heroes of science and technology. Among them, as the new David Livingstone, was Carbonscape director Chris Turney, paleoclimatologist and author of Ice, Mud and Blood (reviewed here). In the interview he speaks of how 125,000 years ago the temperature was 1.7 degrees warmer than before industrialisation got going and the sea levels were 4-6 metres higher than today, suggesting a large number of the ice sheets had melted. Now our stated goal is to keep temperatures less than 2 degrees higher than at the start of industrialisation. The possible implications for ice sheets and sea levels are obvious.

We talk about reducing emissions in the future, but we’ve already got 200 billion tons of carbon in the atmosphere that shouldn’t be there, and that’s what’s driving the changes we see today. We need to get this carbon out of the atmosphere, and fast. This is where Carbonscape’s technology has a part to play. Turney describes it as effectively an enormous microwave with a few tweaks. It turns plants, including waste, into charcoal, which is stable and locks the carbon away permanently. The charcoal can be put in the soil or – and this was a new thought for me – go back down and refill coal mines.

Opinions vary, sometimes fiercely, on the feasibility of charcoal as a means of CO2 sequestration, but there are some well-known names among its supporters, including James Lovelock and Tim Flannery, the latter having joined the Carbonscape Board. It’s still largely unexplored territory, which I presume is why the Sunday Times suggested David Livingstone as Turney’s progenitor. Surely territory worth investigating.

Carbonscape update

As we mentioned in a recent post New Zealand company Carbonscape was shortlisted in the Financial Times competition to find the most innovative solution to the effects of climate change. It went into the final as judges’ favourite, but the nearly 15,000 visitors to the website chose another entry, the Kyoto Box from Kenya, a cheap, solar-powered cardboard cooker able to be made in existing cardboard factories, flat-packed and easily distributed. It could much reduce firewood use, saving trees and preventing carbon emissions.

So Carbonscape has the kudos of the judges’ approval, but not the money. However 15,000 people now know about it, and it is continuing to attract attention elsewhere. I notice Eric Steig on Real Climate gave it the thumbs up in a comment response the other day. And there was an article in the Australian last month. We’ll keep an eye on its development with interest.

Blenheim biochar gets global attention

carbonscape.jpgCarbonscape, the New Zealand company working on making charcoal from a microwaving process discussed here and here on Hot Topic, has just announced that they are one of only five companies to make the shortlist in a global competition, the Financial Times’ Climate Change Challenge.

The competition seeks the most innovative solution to the effects of climate change. The winner, to be chosen by Financial Times readers and a panel of judges will receive a US$75,000 prize, sponsored by Hewlett Packard, to help bring their service to market. I notice Richard Branson, IPCC Chair Rajendra Pachauri and Jonathon Porritt among the eight judges.

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Carbonscape and the charred potato

This column was published in the Waikato Times on 20 January

A couple of months ago a young company called Carbonscape opened a new plant in Marlborough. It makes charcoal from wood waste, hardly an exciting matter one might think. But beyond its traditional use as a fuel, charcoal may hold enormous potential for a sustainable future, for several reasons.

Soil fertility is one. Charcoal added by humans to the soil in pre-European times in the Amazon region has produced a much higher level of fertility than normal in the relatively poor soils of the region.  Modern experiments indicate that at least some soils benefit greatly from having porous charcoal added to them. Our neighbour Australia is finding this in soils which are lower in carbon content than optimal. The biochar, as it is called, seems to act as a catalyst to increase soil fertility. Less fertiliser is required. Microbial and fungal activity is increased. Water retention is improved. Leaching of nitrate and phosphate to waterways is reduced. Crop growth is greater, sometimes considerably so. And the biochar itself lasts for many centuries, being a very stable form of carbon.

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Ice, Mud and Blood

Ice, Mud and Blood: Lessons from Climates Past

In the recently published Ice, Mud and Blood: Lessons from Climates Past British geologist Chris Turney describes how scientists are building up knowledge of the earth’s climate in the past and what it might mean for our future.  He describes attending a showing of The Great Warming Swindle in Australia in 2007. He remarks on the panel discussion which followed when questions were taken from the audience: “…I suddenly realised that many of my companions were either loonies or had been very badly informed. It struck home just how poor a job we’ve done as scientists in communicating our work.”

I’m not sure that the scientists are altogether to blame, but certainly his book makes amends if they are required.

He selects various periods in the past when the climate changed and reports on the current thinking about what caused those changes. Along the way he provides fascinating stories of how the jigsaws have been assembled from a great variety of pieces of scientific investigation.

His first two periods are very distant. One 55 million years ago, the drastic warming over a period of 160,000 years, known as the Peleocene-Eocene Thermal Maximum (PETM), on which Gareth had a recent post. The second from 540 million to 1000 million years ago when it appears that the globe was almost covered in ice during at least three ice ages. Acknowledging that these events happened when the patchwork of continents was different from our time he moves closer to the present in the remainder of the book. He begins a mere 2.5 million years ago when the earth became locked into the bout of ice ages and inter-glacials which continue to the present. His subsequent chapters narrow the focus to episodes within that period: a warm stretch in the last interglacial from 130,000 to 116,000 years ago; the up and down progression from then  towards the Last Glacial Maximum 21,000 years ago; the tumultuous time which marked the end of that last ice age from 21,000 to 11,700 years ago; and what it has meant to the conditions of life for humans to be in the comparatively settled, but by no means uniformly even, climate of recent millenia.

The book carries intrinsic interest in its accounts of how the changes in the past are reconstructed. The evidence gained from ice cores and ocean bed cores is always astonishing in its detail and complexity. The range of information that can be prised from the shells of foraminifera, ancient ocean-dwelling organisms, is extraordinary.  The sheer excitement of discoveries which confirm other discoveries carries a drama which the author is well capable of communicating. Clearly paleoclimate is an absorbing and rewarding area in which to work.

But Turney is much concerned with its lessons for the present. Understandably, considering the likely causes of past changes. Greenhouse gases are always an important part of his picture. For example the PETM was probably triggered by the release of a vast amount of carbon into the ocean and atmosphere over less than 2000 years, likely to have been methane from ocean sources. This was enough to drive a massive warming over 30,000 years or so.  The warm conditions persisted for another 60,000 years.It then took another 70,000 years before temperatures started to drop and return to what they were before, with the oceans playing a different part at this stage in gradually sucking greenhouse gases out of the air. The implications for us today?  If we exhaust the available fossil fuels we will release more carbon than was released at the beginning of the PETM.

Another lesson from the past is the importance of positive feedbacks in the climate system, when the changes that have occurred trigger new and greater changes than the original cause on its own would account for. There is a warning for us that a cascade of unintended consequences can follow from apparently small beginnings. “A little more greenhouse gas in the air does not cause a little change in climate.”

A further lesson is the rapidity with which changes have sometimes happened in the past as tipping points were reached. Abrupt shifts in the climate system are quite possible, as is illustrated, for example, in his account of the sudden reversals which marked the progress towards the Last Glacial Maximum.

Summaries like this unfortunately obscure the pleasure and interest of the book which lies in the wealth of detail it contains and the cheerful clarity with which it is ordered and conveyed to the reader. The underlying earnestness of the author’s concern about the direction we are headed is unmistakable but there is nothing ponderous about his narrative.

Incidentally the author has spent time in New Zealand and describes being able to correct a faulty carbon-dating of wood in the Franz Josef glacier’s Waiho Loop moraine to show that the glacier surge was 13,100 years old and thus contributory evidence of a southern hemisphere cooling at a time when the northern hemisphere was warming. This phenomenon he discusses in the context of his account of the abrupt veerings which marked the end of the last ice age.  His connection with New Zealand includes a directorship in the new young company Carbonscape which is using a world-first microwaving technology to make charcoal.  I expect to post about that soon.