書誌事項
- タイトル別名
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- Studies on the Thermal Production of Magnesium
- カンシキ マグネシウム セイレン ノ ケンキュウ
- 原料物質および反応生成物の検討
- Investigations of the reacting materials by X-ray diffraction method
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抄録
The reacting materials in the thermal production of magnesium-dolomite, ferrosilicon and reduction residue-were investigated by X-ray diffraction method. The following results were obtained.<BR>1) The thermal decomposition of dolomite takes place according to the following formula.<BR>CaMg (CO3) 2→CaCO3+MgCO3→CaCO3+MgO+CO2↑CaO+MgO+CO2↑<BR>2) The reduction of MgO is influenced by the growth of MgO and CaO crystals caused by the excess heating of dolomite<BR>3) The reduction of MgO is influenced by the growth of MgO and CaO crystals caused by the excess heating of dolomite<BR>Si 98% and 85%...Si only<BR>Si 75%...Si and FeSi2<BR>Si 45%...FeSi2 and FeSi<BR>Si 25%...FeSi only<BR>4) The reduction residue consists of 2CaO·SiO2, CaO and MgO. Therefore, the reacting formula is as follows.<BR>2CaO+2MgO+Si (Fe) =2CaO·SiO2+2Mg↑+(Fe)
収録刊行物
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- 日本鑛業會誌
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日本鑛業會誌 78 (884), 113-118, 1962
一般社団法人 資源・素材学会
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詳細情報 詳細情報について
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- CRID
- 1390282680959025280
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- NII論文ID
- 130007256297
- 40018292998
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- NII書誌ID
- AN00188932
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- ISSN
- 21856729
- 03694194
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- NDL書誌ID
- 9158335
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- データソース種別
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- JaLC
- NDL
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- 抄録ライセンスフラグ
- 使用不可