主催: 社団法人 日本エネルギー学会
会議名: 第29回石炭科学会議
回次: 29
開催地: 東京
開催日: 1992/11/05 - 1992/11/06
p. 1-4
Plagioclase, analcime, paragonite and illite/smectite mixed layer are found as Na-bearing minerals in the Ikeshima coals. Analcime and paragonite are formed in the fissures and pores in relatively low ash coals. Na content is well correlated with ash content. Na in high ash coals and related sediments mainly depends on plagioclase and Na in low ash coals on analcime, paragonite and plagioclase.