中国有色金属学报, 2008, 18(1): 163-170.
Zn在FetO-CaO-SiO2-Al2O3渣系中的挥发行为
张延玲 1, , 李士琦 宋博强","id":"dc8937cc-f043-44cf-89f6-835ea4ae2384","originalAuthorName":"宋博强"},{"authorName":"陈旭","id":"b801dc34-c12c-46a2-9928-f4d924876316","originalAuthorName":"陈旭"},{"authorName":"马贵阳","id":"9f04e610-5fe5-4060-8d7e-027532adf615","originalAuthorName":"马贵阳"},{"authorName":"刘睿","id":"94b5d7c7-e2c9-4f3b-b2f8-a4df9069f79e","originalAuthorName":"刘睿"}],"doi":"","fpage":"122","id":"e20a4e61-e2e0-425e-8c10-529a01e0843d","issue":"4","journal":{"abbrevTitle":"CLRCLXB","coverImgSrc":"journal/img/cover/CLRCLXB.jpg","id":"15","issnPpub":"1009-6264","publisherId":"CLRCLXB","title":"材料热处理学报"},"keywords":[{"id":"3c567095-bda9-47d1-b8e0-30c233ee8076","keyword":"X70管线钢","originalKeyword":"X70管线钢"},{"id":"34c3d911-dca9-43f1-8ac0-1f8ba955f7f1","keyword":"焊缝","originalKeyword":"焊缝"},{"id":"ddadea7a-6a6c-4748-b222-dfb0406bc688","keyword":"硫酸盐还原菌","originalKeyword":"硫酸盐还原菌"},{"id":"bddcb5ff-85a2-4ad4-bb5a-19633dd78e53","keyword":"慢应变速率拉伸","originalKeyword":"慢应变速率拉伸"},{"id":"d650cdaf-de2e-446b-8be6-54f72a7149fe","keyword":"近中性pH溶液","originalKeyword":"近中性pH溶液"},{"id":"aef9777c-21be-43c3-b265-10bd83f806b8","keyword":"应力腐蚀开裂","originalKeyword":"应力腐蚀开裂"}],"language":"zh","publisherId":"jsrclxb201604022","title":"SRB对X70钢及其焊缝在近中性pH溶液中SCC行为的影响","volume":"37","year":"2016"},{"abstractinfo":"宋钧官瓷作为中国钧瓷领域中的最高水平,它不仅仅是唐钧瓷釉和早期宋钧瓷釉的扩展和延续,更是一个时代的创造.在给世人留下宝贵财富的同时,也留下一些需待解决的问题.诸如,菟丝纹、蚯蚓走泥纹的产生原因,乳光、分相、窑变的形成机理等等,是本文探讨的主要问题.本文在研究唐钧花釉、宋代天青、天蓝釉的基础上,采用了当地及周边地域原料,并分别采用了现代及传统的制作工艺以及柴烧、煤烧和气烧的烧成方法最终成功烧制出完美的宋钧官瓷艺术效果.实验结果表明,利用当地及周边地域原料和不同的制作工艺,采用不同的烧成方式恢复钧官瓷釉的艺术效果是切实可行的,通过实验证实了钧官瓷釉不同特征的形成原因与工艺过程的相应关系,为钧官瓷的进一步研究提供了可借鉴的科学依据,并从不同角度论述了钧官瓷菟丝纹、蚯蚓走泥纹的形成原理及其乳光、分相、窑变的形成原因及相关问题.","authors":[{"authorName":"张义","id":"909d4353-1cd0-4eee-a44b-3ec77b34500d","originalAuthorName":"张义"},{"authorName":"宁建新","id":"9a0f77bd-2260-4c1b-bde8-80b3290c1f04","originalAuthorName":"宁建新"},{"authorName":"王洪伟","id":"43a25014-afc3-4461-a428-ea03eee7d0d2","originalAuthorName":"王洪伟"},{"authorName":"孙晓岗","id":"0401d67c-3dbd-4010-9516-ba9a9b368e97","originalAuthorName":"孙晓岗"}],"doi":"","fpage":"1580","id":"f8c4c852-1c5a-4313-976c-cafa12ebc6fd","issue":"6","journal":{"abbrevTitle":"GSYTB","coverImgSrc":"journal/img/cover/GSYTB.jpg","id":"36","issnPpub":"1001-1625","publisherId":"GSYTB","title":"硅酸盐通报 "},"keywords":[{"id":"0aa1d7a6-7395-435b-9181-1b28805d06d6","keyword":"钧官瓷","originalKeyword":"钧官瓷"},{"id":"0b13b908-8d98-452b-b15e-ca0566602fe5","keyword":"菟丝纹","originalKeyword":"菟丝纹"},{"id":"4e16e888-70a0-45d2-8f77-0129b5c5c850","keyword":"蚯蚓走泥纹","originalKeyword":"蚯蚓走泥纹"},{"id":"e127e381-fb75-4815-a63c-728d5fc1a78d","keyword":"分相","originalKeyword":"分相"},{"id":"c4d7fc92-502c-4e58-9eaf-04931ed8f0e1","keyword":"乳光","originalKeyword":"乳光"}],"language":"zh","publisherId":"gsytb201206048","title":"中国宋钧官瓷釉的实验与研究","volume":"31","year":"2012"},{"abstractinfo":"宋家沟金矿床位于胶莱盆地东北缘,牟平—即墨断裂带内,控矿构造为陡倾断裂和裂隙密集带,赋矿围岩为莱阳群的灰白色砾岩,共出露4个矿体. 对区内主成矿阶段石英中的流体包裹体进行了岩相学、显微测温及单个包裹体成分激光拉曼光谱分析. 研究表明,矿石中的包裹体主要有纯CO2包裹体、气液二相包裹体和含CO2三相包裹体3种类型;矿石中的包裹体普遍富含CO2 ,成矿流体为CO2 -NaCl -H2 O 体系,成矿流体具有低盐度(5.0 %~14.42 %)、低密度(0.64 ~0.96 g/cm3 )的特点. 主成矿温度集中在220~240 ℃,成矿压力范围为40~62 MPa,对应的成矿深度为5 .01~6 .34 km. 结合前人研究的流体包裹体氢氧同位素分析认为,宋家沟金矿床的成矿流体以幔源流体为主,后期有少量的岩浆流体参与. 确定其矿床成因类型为受陡倾断裂和裂隙密集带联合控制的中温热液脉型金矿床.","authors":[{"authorName":"王铎融","id":"57db05a3-f351-4858-a91f-dc5e55d76d91","originalAuthorName":"王铎融"},{"authorName":"王力","id":"6ae5d5ab-dc31-4d55-b277-66c26e917c3e","originalAuthorName":"王力"},{"authorName":"陈扬","id":"b51e2de7-08f0-4113-9bb3-bf03d3fefde3","originalAuthorName":"陈扬"}],"doi":"10.11792/hj20150506","fpage":"21","id":"d6faaeb1-ea85-4d3e-8b4e-f2c5112bb635","issue":"5","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"9677e386-9d38-41b1-b464-5fb2c9f59529","keyword":"流体包裹体","originalKeyword":"流体包裹体"},{"id":"2714d8e0-3e4e-4c95-9799-2de2bf03eb4c","keyword":"矿床成因","originalKeyword":"矿床成因"},{"id":"d5357e7b-0f4c-4361-9eba-171958c313fa","keyword":"宋家沟金矿床","originalKeyword":"宋家沟金矿床"},{"id":"538316f1-7869-438a-b887-682bb8771dd3","keyword":"山东牟平","originalKeyword":"山东牟平"},{"id":"6798c4a0-d1d0-492a-bf71-fb99d7ce85ce","keyword":"胶莱盆地","originalKeyword":"胶莱盆地"}],"language":"zh","publisherId":"huangj201505006","title":"山东牟平宋家沟金矿床流体包裹体研究","volume":"36","year":"2015"},{"abstractinfo":"宋家沟金矿床位于山东省牟平,为胶莱盆地中发现的颇具工业规模的金矿床.含矿地层为下白垩统莱阳群下段砾岩,矿床由多个矿体组成,矿石为含金砾岩.含矿地层富金(Au=100.2×10-9).围岩矿石稀土总量232.87×10-6～352.2×10-6,LREE/HREE=1.88～12.71,稀土元素分布模式相似、同步.含矿地层是矿源层,燕山晚期(110～125Ma)构造岩浆活动导致该矿床形成定位,该矿床为沉积改造层控矿床.南地口、大崮头是此类矿床的新的找矿地段.","authors":[{"authorName":"张竹如","id":"6cf30b8d-d9ff-4426-9aa7-5675fbac8f07","originalAuthorName":"张竹如"},{"authorName":"唐波","id":"6192e8e9-037f-4f13-8945-3e83050e2c13","originalAuthorName":"唐波"},{"authorName":"聂爱国","id":"d12eb366-0068-4670-90ec-aaa6a418d49e","originalAuthorName":"聂爱国"},{"authorName":"李明琴","id":"d94f6b0c-4dc5-48f7-8b29-28597a76ee89","originalAuthorName":"李明琴"}],"doi":"10.3969/j.issn.1001-1277.2001.07.001","fpage":"1","id":"39b0ce24-99cf-46a0-8349-681635319935","issue":"7","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"a8a75b24-78aa-456b-9ef9-d2733c1418ce","keyword":"宋家沟金矿","originalKeyword":"宋家沟金矿"},{"id":"fde93d52-1bdf-479b-b2c9-bf65c404a974","keyword":"胶莱盆地","originalKeyword":"胶莱盆地"},{"id":"f41fbe9e-7dff-40f0-8f62-421df075703e","keyword":"含金砾岩","originalKeyword":"含金砾岩"},{"id":"c2d4dbe7-3f51-446a-aafa-b42febdd9686","keyword":"稀土配分","originalKeyword":"稀土配分"},{"id":"4a07d8e5-7a61-44bb-8985-1f6b2140d9c4","keyword":"改造成矿","originalKeyword":"改造成矿"},{"id":"d6aa28a7-2f0a-4391-ace4-44ae4bfc8c53","keyword":"层控矿床","originalKeyword":"层控矿床"}],"language":"zh","publisherId":"huangj200107001","title":"山东省牟平宋家沟金矿床地质特征","volume":"22","year":"2001"},{"abstractinfo":"通过对白云鄂博矿中稀土赋存情况的分析,选取随铁开采的稀土作为主要研究对象,通过对粒度、药剂作用以及温度、浓度、pH值等因素对稀土选别的影响,总体分析白云鄂博矿稀土的分选特性,并以此为基础对白云鄂博矿的稀土选别工艺与因素控制提出科学的见解.最终确定,粒度20 μm～ 50 μm、温度不低于60℃、粗选浓度55％ ～65％时,白云鄂博矿稀土浮选作业条件最好.","authors":[{"authorName":"陈宏超","id":"98ea382e-dd87-416a-84fd-c063a3f27baf","originalAuthorName":"陈宏超"}],"doi":"","fpage":"78","id":"cef2dead-9654-462b-8f36-964b77439f45","issue":"4","journal":{"abbrevTitle":"XT","coverImgSrc":"journal/img/cover/XT.jpg","id":"65","issnPpub":"1004-0277","publisherId":"XT","title":"稀土"},"keywords":[{"id":"0df43db5-1bc0-4d7f-87bc-d1a3c0e53a4d","keyword":"白云鄂博矿","originalKeyword":"白云鄂博矿"},{"id":"0507ed0e-f5d9-493e-952c-5612594b5a44","keyword":"稀土","originalKeyword":"稀土"},{"id":"094e7107-b399-44a3-80a2-c2242df6446d","keyword":"因素","originalKeyword":"因素"},{"id":"0e83e9e5-f416-47bd-9aa9-494af550eb35","keyword":"选别","originalKeyword":"选别"}],"language":"zh","publisherId":"xitu201404015","title":"白云鄂博矿稀土选别研究","volume":"35","year":"2014"},{"abstractinfo":"通过可视流化床研究不同温度和氢气流速下对还原白云鄂博铁精矿的影响.试验表明,同一温度下,氢气流速的增加有利于提高流化还原反应的还原效率,但这种作用在低温下更为明显.随温度的升高,流化还原效率提高,但高温下流化效率增长幅度小于低温.应用热重分析研究了不同温度下氢气还原白云鄂博铁精矿的还原动力学,结果表明:其反应的限制性环节为内扩散,活化能随还原时间呈现先下降后上升的现象,而表观活化能的降低更有利于反应的加速进行.在试验条件下,5 ～ 10 min时的还原反应速度较快.","authors":[{"authorName":"裴晓宇","id":"d810f6ff-2fdc-4a94-9cb3-c464900fd5b0","originalAuthorName":"裴晓宇"},{"authorName":"赵文广","id":"430668d2-1cc3-4070-b53e-a92f0639784a","originalAuthorName":"赵文广"},{"authorName":"赵团","id":"1b88dccb-1f69-4e38-b1d1-6f003c357f85","originalAuthorName":"赵团"},{"authorName":"彭军","id":"b80e14ca-58cb-40a0-ba40-e46b51ae3a9a","originalAuthorName":"彭军"},{"authorName":"安胜利","id":"517fd316-96fc-4cfb-90c8-4893c7ee2565","originalAuthorName":"安胜利"}],"doi":"10.7513/j.issn.1004-7638.2017.01.023","fpage":"132","id":"aa711b81-5312-494f-99a5-f42aae2c2fae","issue":"1","journal":{"abbrevTitle":"GTFT","coverImgSrc":"journal/img/cover/gtft1.jpg","id":"28","issnPpub":"1004-7638","publisherId":"GTFT","title":"钢铁钒钛"},"keywords":[{"id":"532f9bd8-0531-4e30-aa51-a24cff3d7486","keyword":"白云鄂博铁精矿","originalKeyword":"白云鄂博铁精矿"},{"id":"aec4acb3-e986-4d78-86d3-4790d52a850a","keyword":"氢气还原","originalKeyword":"氢气还原"},{"id":"c78185c8-048b-49ec-9f36-02bbb06b7d10","keyword":"流态化","originalKeyword":"流态化"}],"language":"zh","publisherId":"gtft201701023","title":"白云鄂博铁精矿氢气流化还原试验","volume":"38","year":"2017"},{"abstractinfo":"介绍了基于六铝酸钙(CA6)矿物相的一种新型合成致密耐火骨料--博耐特(Bonite);讨论了博耐特原料以及由博耐特、板状刚玉或者二者复合制备的多种试验用浇注料的理化性能;并结合博耐特的相关应用领域进行了博耐特耐火材料抗铝液侵蚀、热机械性能、热导率和微气孔等较为前瞻性的试验和探索.","authors":[{"authorName":"刘新彧","id":"9158ab13-c2f1-4039-a97f-6fa306b02ce6","originalAuthorName":"刘新彧"},{"authorName":"","id":"5c128dd4-3880-4b17-9261-f95cb4bfb673","originalAuthorName":""},{"authorName":"","id":"064c8ea2-e4a5-446e-9797-7a6f23c81d10","originalAuthorName":""},{"authorName":"","id":"8126ac55-759b-4313-ac26-22ffa03e827c","originalAuthorName":""}],"doi":"10.3969/j.issn.1001-1935.2006.01.018","fpage":"60","id":"6caef4f8-03d8-4750-877c-90dc00205269","issue":"1","journal":{"abbrevTitle":"NHCL","coverImgSrc":"journal/img/cover/NHCL.jpg","id":"55","issnPpub":"1001-1935","publisherId":"NHCL","title":"耐火材料 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