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法国国家科研中心的Gleb S.Pokrovski、德国拜罗伊特大学的Leonid S.Dubrovinsky等在溶液中首次发现了硫元素的离子形式S3-,这一成果将有助于他们对地质结构进行深入研究。相关研究成果发表在2011年2月25日出版的《Science》杂志。此前普遍认为,硫元素在地壳中只以硫化物和硫酸盐两种形式存在。一些地质学家推测,地壳深处流动的热液中可能存在硫元素的其他形式,但由
Gleb S.Pokrovski of the National Center for Research in France and Leonid S. Dubrovinsky of Bayreuth University in Germany first discovered the ionic form S3- of elemental sulfur in solution, which will help them to further study the geological structure . Relevant research results published in the February 25, 2011 “Science” magazine. It was generally accepted that sulfur exists only in the crust as both sulphide and sulphate. Some geologists speculate that other forms of elemental sulfur may be present in the hydrothermal fluid flowing deep into the crust,