When Penn State decided to convert its two power plants from their historic use of coal as a source of energy to natural gas, there was concern about radon emissions. Although radon is known to exist in natural gas, now Penn State research indicates that it does not escape from these two power plants in harmful amounts.

By converting the West Campus Steam Plant on the University Park Campus, Penn State reduced its greenhouse gas emissions at the plant by nearly 40 percent, but the University wanted to make sure that the conversion was not causing a significant increase of radon levels in the atmosphere. Penn State also operates a second power plant on the East end of campus near its football stadium.

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With new methods of reconstruction, climate researchers in Bern have been able to demonstrate that some 9,000 to 5,000 years ago, the Mediterranean climate was considerably warmer than previous studies had suggested. Among other things, previous concerns regarding the reliability of climate models could thus be dispelled.

Climate reconstructions are necessary because reliable measurement data are only available for the last 150 years. For this reason, research on past climate change uses so-called ‘proxies’. These are indicators with which it is possible to reconstruct temperatures in the past. A widespread reconstruction method examines pollen which is embedded in lake sediments. From the composition of this pollen, it is possible to determine the plant species which occurred at a particular location in the past – and since the temperatures that the individual species require are also known, it is possible to reconstruct the temperature conditions for the period in question.

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The development of agriculture is universally believed to underpin some of the most significant advances made by humans worldwide. In New Guinea, where one of the earliest human experiments with tropical forest agriculture occurred, researchers have cast doubt on two views about the origins of agriculture.

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A University of Wyoming researcher contributed to a paper that determined a “Snowball Earth” event actually took place 100 million years earlier than previously projected, and a rise in the planet’s oxidation resulted from a number of different continents -- including what is now Wyoming -- that were once connected.

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