{"title":"钛在硅铁熔体和 CaO-SiO2-Al2O3 熔渣之间的分布行为:热化学和结构评估","authors":"Min Joo Lee, Tae Sung Kim, Joo Hyun Park","doi":"10.1007/s11663-024-03200-4","DOIUrl":null,"url":null,"abstract":"<p>The titanium distribution ratio (<span>\\({L}_{Ti}\\)</span>) between ferrosilicon (FeSi) melt and the CaO-SiO<sub>2</sub>-Al<sub>2</sub>O<sub>3</sub> slag was measured at 1773 K (1500 °C). FeSi-slag equilibration was carried out using various slag compositions. The <span>\\({L}_{Ti}\\)</span> was presented against the <i>Vee ratio</i> (pct CaO/pct SiO<sub>2</sub> = C/S) between 0.3 and 1.2, and Al<sub>2</sub>O<sub>3</sub> content from 5 to 20 mass pct. The <span>\\({L}_{Ti}\\)</span> exhibited minima at about C/S=0.7(±0.1) at a fixed Al<sub>2</sub>O<sub>3</sub> content. In a C/S < 0.7 regime, i.e., relatively acidic melts, Ti<sup>4+</sup> ions were considered as network forming [TiO<sub>4</sub>]-tetrahedron unit in the aluminosilicate framework. However, in a C/S > 0.7 regime, i.e., relatively basic melts, Ti<sup>4+</sup> ions were considered to form the [TiO<sub>5</sub>]-pyramid structure unit compensated by Ca<sup>2+</sup>. When adding Al<sub>2</sub>O<sub>3</sub> into the basic melts over 10 mass pct, [AlO<sub>4</sub>]-tetrahedrons take Ca<sup>2+</sup> ions for charge compensation, resulting in a decrease of stability of [TiO<sub>5</sub>] unit because of Ca<sup>2+</sup> depletion. At a greater than 10 mass pct Al<sub>2</sub>O<sub>3</sub> content in the basic melts, Ti<sup>4+</sup> replaced Al<sup>3+</sup> to form the [TiO<sub>4</sub>]-tetrahedron unit, decreasing the activity coefficient of TiO<sub>2</sub> in the slag.</p>","PeriodicalId":18613,"journal":{"name":"Metallurgical and Materials Transactions B","volume":"46 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-07-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Distribution Behavior of Titanium Between Ferrosilicon Melt and CaO-SiO2-Al2O3 Slag: Thermochemical and Structural Assessments\",\"authors\":\"Min Joo Lee, Tae Sung Kim, Joo Hyun Park\",\"doi\":\"10.1007/s11663-024-03200-4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The titanium distribution ratio (<span>\\\\({L}_{Ti}\\\\)</span>) between ferrosilicon (FeSi) melt and the CaO-SiO<sub>2</sub>-Al<sub>2</sub>O<sub>3</sub> slag was measured at 1773 K (1500 °C). FeSi-slag equilibration was carried out using various slag compositions. The <span>\\\\({L}_{Ti}\\\\)</span> was presented against the <i>Vee ratio</i> (pct CaO/pct SiO<sub>2</sub> = C/S) between 0.3 and 1.2, and Al<sub>2</sub>O<sub>3</sub> content from 5 to 20 mass pct. The <span>\\\\({L}_{Ti}\\\\)</span> exhibited minima at about C/S=0.7(±0.1) at a fixed Al<sub>2</sub>O<sub>3</sub> content. In a C/S < 0.7 regime, i.e., relatively acidic melts, Ti<sup>4+</sup> ions were considered as network forming [TiO<sub>4</sub>]-tetrahedron unit in the aluminosilicate framework. However, in a C/S > 0.7 regime, i.e., relatively basic melts, Ti<sup>4+</sup> ions were considered to form the [TiO<sub>5</sub>]-pyramid structure unit compensated by Ca<sup>2+</sup>. When adding Al<sub>2</sub>O<sub>3</sub> into the basic melts over 10 mass pct, [AlO<sub>4</sub>]-tetrahedrons take Ca<sup>2+</sup> ions for charge compensation, resulting in a decrease of stability of [TiO<sub>5</sub>] unit because of Ca<sup>2+</sup> depletion. At a greater than 10 mass pct Al<sub>2</sub>O<sub>3</sub> content in the basic melts, Ti<sup>4+</sup> replaced Al<sup>3+</sup> to form the [TiO<sub>4</sub>]-tetrahedron unit, decreasing the activity coefficient of TiO<sub>2</sub> in the slag.</p>\",\"PeriodicalId\":18613,\"journal\":{\"name\":\"Metallurgical and Materials Transactions B\",\"volume\":\"46 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-07-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Metallurgical and Materials Transactions B\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1007/s11663-024-03200-4\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Metallurgical and Materials Transactions B","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1007/s11663-024-03200-4","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Distribution Behavior of Titanium Between Ferrosilicon Melt and CaO-SiO2-Al2O3 Slag: Thermochemical and Structural Assessments
The titanium distribution ratio (\({L}_{Ti}\)) between ferrosilicon (FeSi) melt and the CaO-SiO2-Al2O3 slag was measured at 1773 K (1500 °C). FeSi-slag equilibration was carried out using various slag compositions. The \({L}_{Ti}\) was presented against the Vee ratio (pct CaO/pct SiO2 = C/S) between 0.3 and 1.2, and Al2O3 content from 5 to 20 mass pct. The \({L}_{Ti}\) exhibited minima at about C/S=0.7(±0.1) at a fixed Al2O3 content. In a C/S < 0.7 regime, i.e., relatively acidic melts, Ti4+ ions were considered as network forming [TiO4]-tetrahedron unit in the aluminosilicate framework. However, in a C/S > 0.7 regime, i.e., relatively basic melts, Ti4+ ions were considered to form the [TiO5]-pyramid structure unit compensated by Ca2+. When adding Al2O3 into the basic melts over 10 mass pct, [AlO4]-tetrahedrons take Ca2+ ions for charge compensation, resulting in a decrease of stability of [TiO5] unit because of Ca2+ depletion. At a greater than 10 mass pct Al2O3 content in the basic melts, Ti4+ replaced Al3+ to form the [TiO4]-tetrahedron unit, decreasing the activity coefficient of TiO2 in the slag.