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绿河组油页岩中的氨态氮。

Ammonium-nitrogen in green river formation oil shale.

出版信息

Science. 1983 Feb 4;219(4584):492-3. doi: 10.1126/science.219.4584.492.

Abstract

It has been assumed that all of the nitrogen in oil shale from the Green River Formation is present as organic nitrogen and that the nitrogen in spent shale from retorting is present in the char or coke. In fact, from 41 to 84 percent of the nitrogen is present as ammonium fixed within silicate minerals in five samples of raw oil shale and between 46 and 69 percent of the nitrogen is similarly fixed in two samples of spent shale. Both organic nitrogen and fixed ammonium-nitrogen are lost during retorting by the Fischer assay procedure; the loss of organic nitrogen is greater.

摘要

人们曾假定绿河组油页岩中的所有氮都以有机氮的形式存在,并且油页岩干馏后的残渣中的氮都存在于焦炭或焦煤中。实际上,在五个原始油页岩样本和两个干馏油页岩样本中,有 41%至 84%的氮是以固定在硅酸盐矿物中的铵态氮的形式存在的。在费歇尔分析过程中,无论是有机氮还是固定的铵态氮都会在干馏过程中流失,而且有机氮的流失量更大。

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