BioReGen project expands: greening brownfield sites with energy crops and biofuels
Entitled BioReGen ('Biomass, Remediation, reGeneration'), the project began in 2004 with test planting at several small brownfield sites, the first being a former enamel works at Fylands Bridge, near Bishop Auckland, County Durham. The willow trees and the miscanthus, reed canary and switch grasses cleaned up the soil by absorbing contaminants such as zinc, copper, cadmium and heavy metals in coal ash. Plants break these pollutants down into harmless byproducts and either incorporate them into their roots, stems and leaves or release the clean substances into the air (schematic, click to enlarge).
BioReGen believes the method can work on bigger sites and planting has now been carried out on five larger areas, each covering a hectare and all with a history of heavy industrial use. The five full-scale demonstration sites are at: (1) the former Haverton Hill shipyard on the River Tees, near the Transporter Bridge; (2) part of the old Head Wrightson engineering site, at the Tees Barrage, made famous by Margaret Thatcher’s Walk in the Wilderness during a visit to Teesside two decades ago; (3) a former colliery and coal yard at Binchester, near Bishop Auckland, County Durham; (4) Warden Law, a landfill site, and former gravel pit, near Sunderland; (5) a former sewage treatment works at Rainton Bridge, near Houghton-le-Spring, Wearside.
CLEMANCE believes the work, supported by a €1.2 million grant from the European Union’s LIFE-Environment research programme, has major implications for greening the industrial landscape of the past.
When we started this project, we did not know if we could grow plants on such contaminated land but it has been a success everywhere we have tried it. We have proved that phytoremediation works and what works on a small site can also do so on much larger sites as well. It is also much cheaper than having to clean up a site or remove contaminated soils to landfill sites. Developers looking to do that spend millions of pounds per hectare, whereas our method costs only tens of thousands of pounds. - Dr Richard Lord, CLEMANCE’s Programme Leader for Contaminated Land and WaterThe potential of the project is described as 'huge', because there are 1,155 hectares of brownfield land in the Tees Valley alone. However, the old dirty industrial past stretches across the entire industrialised world and has transformed much of its landscape into sites that need to be cleaned up.
Phytoremediation is not a quick fix, though. To get a site ready for development through this method could take years but BioReGen thinks it is on the right track (however, recently scientists designed an energy crop with a vastly improved phytoremediation capacity, speeding up the process considerably - more here). CLEMANCE researchers regard their activity as a holding operation until the sites are needed for industry again. In the meantime, the greened sites are made attractive again, and good wildlife habitats, rather than visions of unsightly dereliction which blight the image of the North-East. The project is helping to turn the Tees Valley - the ultimate symbol of a polluted landscape - into a 'Trees Valley' instead.
But then the story gets even better. CLEMANCE has been negotiating with energy provider SembCorp about providing willow to the company’s recently-opened Wilton 10 biomass power station, on the Wilton International site near Redcar, east Cleveland:
energy :: sustainability :: biomass :: bioenergy :: biofuels :: climate change :: brownfield :: pollution :: energy crops :: phytoremediation :: EU ::
Wilton 10 is a £60m biomass power station, the first of its type in the UK, which began generating this summer and is capable of producing energy for 30,000 properties. Operated by SembCorp Utilities UK, it burns wood, a classic example of an infinitely renewable fuel which is also ‘carbon neutral’.
Wilton 10 is helping to sustain the planting and harvesting of woodland and is a development which neatly ties in with the pioneering phytoremediation project.
When the willow has been coppiced, or cut back, the resulting timber could help feed Wilton 10’s voracious appetite for 300,000 tonnes of wood a year. Forty per cent of the station’s required timber will be recycled and a similar amount will eventually be sourced from energy crops, such as those planted by CLEMANCE.
According to Dr Lord, Wilton 10 has a huge appetite for timber and BioReGen can help provide it, particularly if it expands its planting over larger areas. What started as a research project has thus found a commercial application.
Wilton 10 could provide a real opportunity to commercialise our work by using willow trees as an energy crop. This is as sustainable as it gets. Wilton 10 has already generated national and international interest. - Dr LordIt doesn't come as a surprise that other researchers, both in the EU and the US, are looking at creating similar win-win situations.
Recently, scientists led by the University of Washington's Sharon Doty reported that they succeeded in genetically engineering poplar plants with a dramatically improved capacity to clean up contaminated sites. Doty, an assistant professor of forest resources, told Biopact that the ideal end of phytoremediation projects based on the trees would be to use the plants as a bioenergy feedstock. After all, poplar has been identified as a promising, fast-growing energy crop (previous post).
Other scientists in France looked at miscanthus, an energy crop, to clean up brown fields (more here); Michigan State University researchers are working on a similar project and are examining the possibility that some oilseed crops like soybeans, sunflower and canola, and other crops such as corn and switchgrass, can be grown on abandoned industrial sites for use in ethanol or biodiesel fuel production (previous post). Finally, scientists have identified hybrid poplars as good candidates for soaking up and cleaning polluted water from coal mining sites (earlier post).
BioReGen is short for "Biomass, Remediation reGeneration: Re-using brownfield sites for renewable energy crops". It is a 4-5 year project funded by the EU's Life III Environment Programme to investigate whether brownfield sites can be used to grow plants for fuel.
Photo: University of Teesside researchers planting energy crops to phytoremediate a polluted site under an EU-sponsored project called BioReGen. Credit: BioReGen.
References:
AlphaGalileo: Pioneering project helps to transform brownfield sites into the ‘Trees Valley' - December 10.
John Dean, "Green Revolution", Research & Enterprise, a University of Teesside Magazine, Issue Six, pp. 34-35 (December 2007).
BioReGen project website.
Biopact: Scientists dramatically improve poplar's capacity to clean up polluted sites - potential to couple phytoremediation to bioenergy - October 17, 2007
Biopact: Turning brownfields into greenfields with the help of biofuels - August 09, 2006
Biopact: Energy crops may soak up methane water - August 15, 2006
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Monday, December 10, 2007
Scientists find global warming intensified El Niño in the past; provides clues for the future
El Niño ('Child Jesus') got its name because it generally occurs at the time of Christmas along the Peruvian coasts. This mode of variability of the climate, also called ENSO (El Niño-Southern Oscillation), results from a series of interactions between the atmosphere and the tropical ocean. Its effects are drought in otherwise humid areas and, vice versa, precipitation and even floods in arid zones (schematic, click to enlarge).
Scientists qualify this phenomenon as 'quasi-cyclical' because its periodicity, which varies from 2 to 7 years, does not have a strict regularity. Drawing on research carried out for over 25 years by oceanographers, climatologists and meteorologists, the mechanisms driving El Niño events are becoming known better and better. However, it has been difficult to include and understand the influence of other modes of climate variability on the ENSO subsystem. More precisely, until now it was not known whether the intensity and the frequency of the phenomenon is undergoing changes because of planetary global warming.
Now a team made up of Chilean scientists and researchers from France's Institut de Recherche pour le Développement (IRD) sheds new light on the question. The researchers took sediment cores, going 80 metres deep, in the bay of Mejillones, located in the north of Chile, and analysed the geochemical data contained in the samples. In particular they zoomed in on the by-products of the decomposition of diatoms - unicellular planktonic algae - which allowed for a precise determination of the changes of ocean surface temperatures in this area between 1650 and 2000.
The researchers found a sea temperature drop of more than 2°C between 1820 and 1878. The same decrease was detected in two samples collected near the South American coast more than one thousand kilometers north and south of Mejillones. The findings prove the ocean temperatures observed since 1820 affected the entire coastline of western South America, from central Chile to the north of Peru. The entire stretch of ocean where the Humboldt current can be found was thus the theatre of a significant cooling during this period.
However, this conclusion is paradoxical because the beginning of the 19th century coincides with the end of the 'Small Ice Age' which was accompanied by a reheating of the planet. In order to supplement and double check the data, the scientists studied minerals contained in the sediment samples, which made it possible to confirm that these minerals were transported by the winds from the continent. From this they concluded that the dominant trade winds in the region were strengthened at the time, pushing back the layer of warm surface water towards the west, resulting in an upwelling of cold water found usually in the deep along the Pacific coasts of South America:
energy :: sustainability :: biomass :: bioenergy :: agriculture :: El Niño :: ENSO :: climate change :: global warming ::
The assumption was confirmed by the measurement of the organic carbon flow which is directly related to an increase in the concentration of nutrients in the surface water. The increase in this flow, consistent with the observation of a 'cold phase' between 1820 and 1878, proves that the rise in the concentration in nutrients is the consequence of an upwelling of cold water.
The researchers then put forth the assumption that, in a climatic context of warming like the one which followed the end of the Small Ice Age, the important variation in temperature between the continent's land mass and that of the ocean would be responsible for this strengthening of the trade winds.
Whereas the coastal desert of Atacama was heated quickly during this period, the temperature of sea water would have increased much more slowly. Because this difference persisted and even grew, dominant winds intensified. By pushing back surface waters towards the west, these winds would thus have allowed the cooling of coastal water, modifying the normal mode of El Niño, which is usually characterized by a heating of the water.
Between the end of the Small Ice Age and the onset of the warming effects caused by anthropogenic climate change, the ENSO changed its mode.
These historical climatology studies also explain the observations made by chroniclers at the time who describe floods and an abrupt change in El Niño's behavior, occuring around 1820, along the peaceful coasts of South America.
Since the beginning of the 19th century, from the end of the Small Ice Age onwards, the ENSO has been characterized by abnormal rains occuring at in central Chile during the southern winter and on the northern coast of Peru during the next southern summer.
The new results underline the complexity of the interactions between global changes in the climate, the particularities of the El Niño-Southern Oscillation and regional climatic changes.
Now it remains to be determined whether the very strong intensity of the two extreme El Niño events occuring at the end of the 20th century, in 1982-1983 and again in 1997-1998, are also related to the recent intensification of the warming of the land mass caused by global warming. If that were indeed the case, El Niño could then become increasingly intense and have destructive impacts on the coasts of South America, but also in other areas of the planet.
The research was undertaken by the Institut de Recherche pour le Développement in collaboration with the Universities of Chile and Concepción. They follow upon the doctoral thesis of Gabriel Vargas supported at the University of Bordeaux I and financed by the IRD.
(Note, Chilean universities recently launched a bioenergy program based on drought-tolerant energy crops to be planted in the arid zones along the coast. The project will have to take into account potential for more extreme El Niño events in the future.)
Translated for Biopact by Laurens Rademakers, 2007, CC.
References:
Vargas G., Pantoja S., Rutllant J. A., Lange C. B., Ortlieb L. "Enhancement of coastal upwelling and interdecadal ENSO-like variability in the Peru-Chile Current since late 19th century", Geophysical Research Letters, 2007, 34 (13), doi:10.1029/2006GL028812
AlphaGalileo: El Niño affecté par le réchauffement de la planète - December 10, 2007.
IRD: Les recherches sur le climat à l'IRD - dossier [*.pdf] - 2007.
Biopact: Chile and the U.S. to cooperate on biofuels development - July 14, 2007
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