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Humanity's emissions '100-times greater' than volcanoes By Patrick GALEY Paris (AFP) Oct 1, 2019 Human activity churns out up to 100 times more planet-warming carbon each year as all the volcanoes on Earth, says a decade-long study released Tuesday. The Deep Carbon Observatory (DCO), a 500-strong international team of scientists, released a series of papers outlining how carbon is stored, emitted and reabsorbed by natural and manmade processes. They found that manmade carbon dioxide emissions drastically outstrip the contribution of volcanoes -- which belch out gas and are often fingered as a major climate change contributor -- to current warming rates. The findings, published in the journal Elements, showed just two-tenths of 1 percent of Earth's total carbon -- around 43,500 gigatonnes -- is above the surface in oceans, the land, and in our atmosphere. The rest -- a staggering 1.85 billion gigatonnes -- is stored in our planet's crust, mantle and core, providing scientists with clues as to how Earth formed billions of years ago. One gigatonne is equivalent to around 3 million Boeing 747s. By measuring the prominence of certain carbon isotopes in rock samples around the world, the DCO were able to create a timeline stretching back 500 million years to map how carbon moved between land, sea and air. They found that in general the planet self-regulated atmospheric levels of carbon dioxide, a key greenhouse gas, over geological timeframes of hundreds of thousands of years. The exceptions to this came in the form of "catastrophic disturbances" to Earth's carbon cycle, such as immense volcanic eruptions or the meteor strike that killed off the dinosaurs. "In the past we see that these big carbon inputs to the atmosphere cause warming, cause huge changes in both the composition of the ocean and the availability of oxygen," said Marie Edmonds, Professor of Volcanology and Petrology and Ron Oxburgh Fellow in Earth Sciences at Queens' College, Cambridge. The team estimated that the Chicxulub impact 66 million years ago, which killed off three-quarters of all life on Earth, released between 425 and 1,400 gigatonnes of CO2. Manmade emissions in 2018 alone topped 37 gigatonnes. "The amount of CO2 pumped into the atmosphere by anthropogenic (manmade) activity in the last 10-12 years (is equvalent) to the catastrophic change during these events we've seen in Earth's past," Edmonds told AFP. Celina Suarez, Associate Professor of Geology at the University of Arkansas, said modern manmade emissions were the "same magnitude" as past carbon shocks that precipitated mass extinction. "We are on the same level of carbon catastrophe which is a bit sobering," she told AFP. - 'Not a human timescale' - By comparison, the CO2 released annually by volcanoes hovers around 0.3 and 0.4 gigatonnes -- roughly 100 times less than manmade emissions. "Climate sceptics really jump on volcanoes as a possible contender for top CO2 emissions but it's simply not the case," said Edmonds. "It's also the timescale." Whereas Earth's atmosphere has frequently contained higher concentrations of CO2 than the present day, outside of catastrophic eruptions it has taken hundreds of thousands of years for such levels to accumulate. In contrast, manmade carbon emissions have seen CO2 levels rise two thirds in a span of a few centuries. "Climate deniers always say that Earth always rebalances itself," said Suarez. "Well, yes it has. It will rebalance itself, but not on a timescale that is of signficance to humans."
Graphene is 3D as well as 2D London, UK (SPX) Sep 24, 2019 Graphene is actually a 3D material as well as a 2D material, according to a new study from Queen Mary University of London. Realising that it is a 3D material is important for understanding its mechanical properties and for developing novel graphene-based devices. Often hailed as a 'wonder material', graphene has the highest known thermal and electrical conductivity, is stronger than steel, light, flexible and transparent. Its uses are wide-ranging and recently it has been shown it could eve ... read more
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