CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA
Diamond crystals from Siberian, Arkhangelsk, South African, Canadian and South American deposits were analyzed for structurally bound nitrogen, hydrogen and “platelet ” defects using infrared (IR) absorption spectroscopy. Wide variations in total nitrogen and hydrogen contents and in the state of ni...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.535.9921 2023-05-15T15:23:52+02:00 CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA Felix V. Kaminsky Galina K. Khachatryan The Pennsylvania State University CiteSeerX Archives 1733 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.9921 http://rruff.info/doclib/cm/vol39/CM39_1733.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.9921 http://rruff.info/doclib/cm/vol39/CM39_1733.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://rruff.info/doclib/cm/vol39/CM39_1733.pdf diamond nitrogen hydrogen infrared absorption. SOMMAIRE text 1733 ftciteseerx 2020-02-23T01:14:28Z Diamond crystals from Siberian, Arkhangelsk, South African, Canadian and South American deposits were analyzed for structurally bound nitrogen, hydrogen and “platelet ” defects using infrared (IR) absorption spectroscopy. Wide variations in total nitrogen and hydrogen contents and in the state of nitrogen aggregation were established in diamond crystals from different areas and deposits. On this basis, three groups were distinguished: (1) low-nitrogen, highly-aggregated-nitrogen diamond, (2) intermediate diamond crystals, and (3) high-nitrogen, poorly-aggregated-nitrogen diamond (occasionally with high concentrations of hydrogen and “platelets”). They represent, in general terms, three major stages of diamond formation: (1) the initial stage at high P–T conditions, which occasionally occurs in super-deep areas (e.g., lower mantle and transition zone), (2) the main stage, and (3) the final stage, which represents the latest episodes of magmatic evolution and is characterized by high oversaturation of the crystallization medium and high internal temperature-gradients. These data may be used for “fingerprinting ” of diamond, in prospecting for new deposits in diamondiferous areas, and in the evaluation of diamond crystals from newly discovered deposits. Text Arkhangelsk Unknown |
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English |
topic |
diamond nitrogen hydrogen infrared absorption. SOMMAIRE |
spellingShingle |
diamond nitrogen hydrogen infrared absorption. SOMMAIRE Felix V. Kaminsky Galina K. Khachatryan CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
topic_facet |
diamond nitrogen hydrogen infrared absorption. SOMMAIRE |
description |
Diamond crystals from Siberian, Arkhangelsk, South African, Canadian and South American deposits were analyzed for structurally bound nitrogen, hydrogen and “platelet ” defects using infrared (IR) absorption spectroscopy. Wide variations in total nitrogen and hydrogen contents and in the state of nitrogen aggregation were established in diamond crystals from different areas and deposits. On this basis, three groups were distinguished: (1) low-nitrogen, highly-aggregated-nitrogen diamond, (2) intermediate diamond crystals, and (3) high-nitrogen, poorly-aggregated-nitrogen diamond (occasionally with high concentrations of hydrogen and “platelets”). They represent, in general terms, three major stages of diamond formation: (1) the initial stage at high P–T conditions, which occasionally occurs in super-deep areas (e.g., lower mantle and transition zone), (2) the main stage, and (3) the final stage, which represents the latest episodes of magmatic evolution and is characterized by high oversaturation of the crystallization medium and high internal temperature-gradients. These data may be used for “fingerprinting ” of diamond, in prospecting for new deposits in diamondiferous areas, and in the evaluation of diamond crystals from newly discovered deposits. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Felix V. Kaminsky Galina K. Khachatryan |
author_facet |
Felix V. Kaminsky Galina K. Khachatryan |
author_sort |
Felix V. Kaminsky |
title |
CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
title_short |
CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
title_full |
CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
title_fullStr |
CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
title_full_unstemmed |
CHARACTERISTICS OF NITROGEN AND OTHER IMPURITIES IN DIAMOND, AS REVEALED BY INFRARED ABSORPTION DATA |
title_sort |
characteristics of nitrogen and other impurities in diamond, as revealed by infrared absorption data |
publishDate |
1733 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.9921 http://rruff.info/doclib/cm/vol39/CM39_1733.pdf |
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Arkhangelsk |
genre_facet |
Arkhangelsk |
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http://rruff.info/doclib/cm/vol39/CM39_1733.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.9921 http://rruff.info/doclib/cm/vol39/CM39_1733.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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