Meridianiite detected in ice

F. Elif Genceli; Shinichirou Horikawa; Yoshinori Iizuka; Toshimitsu Sakurai; Takeo Hondoh; Toshiyuki Kawamura; Geert Jan Witkamp

doi:10.3189/002214309788608921

Meridianiite detected in ice

F. Elif Genceli^*
, Shinichirou Horikawa
, Yoshinori Iizuka
, Toshimitsu Sakurai
, Takeo Hondoh
, Toshiyuki Kawamura
, Geert Jan Witkamp

^*Bu çalışma için yazışmadan sorumlu yazar

Delft University of Technology
Hokkaido University

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

15 Atıf (Scopus)

Özet

Inclusions affect the behavior of ice, and their characteristics help us understand the formation history of the ice. Recently, a low-temperature magnesium sulfate salt was discovered. This paper describes this naturally occurring MgSO₄· 11H₂O mineral, meridianiite, derived from salt inclusions in sea ice of Lake Saroma, Japan and in Antarctic continental core ice. Its occurrence is confirmed by using micro-Raman spectroscopy to compare Raman spectra of synthetic MgSO _{4 ·}-11H₂O with those of the inclusions.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	117-122
Sayfa sayısı	6
Dergi	Journal of Glaciology
Hacim	55
Basın numarası	189
DOI'lar	https://doi.org/10.3189/002214309788608921
Yayın durumu	Yayınlandı - 2009
Harici olarak yayınlandı	Evet

Belgeye Erişim

10.3189/002214309788608921

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Link to publication in Scopus

Alıntı Yap

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title = "Meridianiite detected in ice",

abstract = "Inclusions affect the behavior of ice, and their characteristics help us understand the formation history of the ice. Recently, a low-temperature magnesium sulfate salt was discovered. This paper describes this naturally occurring MgSO4· 11H2O mineral, meridianiite, derived from salt inclusions in sea ice of Lake Saroma, Japan and in Antarctic continental core ice. Its occurrence is confirmed by using micro-Raman spectroscopy to compare Raman spectra of synthetic MgSO 4 ·-11H2O with those of the inclusions.",

author = "\{Elif Genceli\}, F. and Shinichirou Horikawa and Yoshinori Iizuka and Toshimitsu Sakurai and Takeo Hondoh and Toshiyuki Kawamura and Witkamp, \{Geert Jan\}",

year = "2009",

doi = "10.3189/002214309788608921",

language = "English",

volume = "55",

pages = "117--122",

journal = "Journal of Glaciology",

issn = "0022-1430",

publisher = "Cambridge University Press",

number = "189",

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TY - JOUR

T1 - Meridianiite detected in ice

AU - Elif Genceli, F.

AU - Horikawa, Shinichirou

AU - Iizuka, Yoshinori

AU - Sakurai, Toshimitsu

AU - Hondoh, Takeo

AU - Kawamura, Toshiyuki

AU - Witkamp, Geert Jan

PY - 2009

Y1 - 2009

N2 - Inclusions affect the behavior of ice, and their characteristics help us understand the formation history of the ice. Recently, a low-temperature magnesium sulfate salt was discovered. This paper describes this naturally occurring MgSO4· 11H2O mineral, meridianiite, derived from salt inclusions in sea ice of Lake Saroma, Japan and in Antarctic continental core ice. Its occurrence is confirmed by using micro-Raman spectroscopy to compare Raman spectra of synthetic MgSO 4 ·-11H2O with those of the inclusions.

AB - Inclusions affect the behavior of ice, and their characteristics help us understand the formation history of the ice. Recently, a low-temperature magnesium sulfate salt was discovered. This paper describes this naturally occurring MgSO4· 11H2O mineral, meridianiite, derived from salt inclusions in sea ice of Lake Saroma, Japan and in Antarctic continental core ice. Its occurrence is confirmed by using micro-Raman spectroscopy to compare Raman spectra of synthetic MgSO 4 ·-11H2O with those of the inclusions.

UR - https://www.scopus.com/pages/publications/67651171561

U2 - 10.3189/002214309788608921

DO - 10.3189/002214309788608921

M3 - Article

AN - SCOPUS:67651171561

SN - 0022-1430

VL - 55

SP - 117

EP - 122

JO - Journal of Glaciology

JF - Journal of Glaciology

IS - 189

ER -

Meridianiite detected in ice

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