2017
DOI: 10.14494/jnrs.17.1
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Mössbauer Spectroscopic Characterization of Iron in Ashes Made from the Ancient Woods Excavated in the Foothills of Mt. Chokai

Abstract: 2. Experimental 2.1. Umoregi wood and soil samples. The sample ashes were made from umoregi woods excavated from Nikaho City in Akita Prefecture, Japan, located to the northwest of Mt. Chokai (Figure 1) in 2015. Umoregi wo ods were the stems of trees buried by large-scale landslides from Mt. Chokai ca. 2500 years ago. 9, 10 The material umoregi woods were Japanese oak (Quercus serrata or Quercus crispula), Japanese chestnut (Castanea crenata), Japanese cedar (Cryptomeria japonica), and Japanese zelkova (Zelkov… Show more

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Cited by 5 publications
(5 citation statements)
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“…The elements for which the molar percentage is less than 0.10% are omitted from the table. As is expected from the previous study [1], Fe was concentrated considerably in the three umoregi-wood ash samples compared with MA. The XRF elemental-analysis results could provide two important pieces of information about the Fe-containing species.…”
Section: Elements In Ash Samplessupporting
confidence: 88%
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“…The elements for which the molar percentage is less than 0.10% are omitted from the table. As is expected from the previous study [1], Fe was concentrated considerably in the three umoregi-wood ash samples compared with MA. The XRF elemental-analysis results could provide two important pieces of information about the Fe-containing species.…”
Section: Elements In Ash Samplessupporting
confidence: 88%
“…Furthermore, experts or advanced learners of the Japanese tea or traditional incense ceremonies rate the ash made from umoregi wood, which displays various unusual colors, as top-quality ash in an incense burner or a brazier. However, there have been no reports examining the ash made from umoregi wood other than our previous work [1]. We investigated the coloring mechanism of ash obtained from the combustion of four species of umoregi trees excavated from the foothills of Mt.…”
Section: Introductionmentioning
confidence: 97%
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“…The ratio of the area between octahedral and tetrahedral sites is around 1.8 and this value is related to the lower Mössbauer fraction in Fe 2+ /Fe 3+ (Site B) than in Fe 3+ (Site A) [19]. The last two sextets correspond to Ca 2 Fe 2 O 5 with octahedral and tetrahedral Fe 3+ sites with B hf =50.6 a 41.9 T [20,21].…”
Section: Methodsmentioning
confidence: 94%