{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"利用硅藻土比表面积大、孔洞多因而吸附性好的特点,吸附正十八烷,制备出形态稳定、高相变焓的硅藻土/正十八烷复合相变材料.利用扫描电镜(SEM)观察其表面形貌,采用红外光谱法(FTIR)分析材料的微观结构,用热重分析仪(TG)及受热形态变化对其热稳定性进行了表征,用示差扫描量热法(DSC)对其相变温度及相变焓进行了测定.结果表明:制得的复合相变材料的分解温度在240℃以上,当正十八烷的吸附量不超过40%时,在高于相变温度时未泄漏,相变温度在26~31℃之间,并且具有很高的相变焓(131.6~163.3 J/g),是一类形态稳定、相变焓高、热性能良好、应用前景广泛的节能环保材料.","authors":[{"authorName":"","id":"4794e873-4b19-4dd6-a897-16d2db61603d","originalAuthorName":"宋秀龙"},{"authorName":"康虹","id":"e8c6948f-140f-49b7-a142-36eecb54187b","originalAuthorName":"康虹"},{"authorName":"高向华","id":"1c19f2ee-4ad9-4e5d-bdf2-807b4416ee7b","originalAuthorName":"高向华"},{"authorName":"许并社","id":"1419b5ca-7146-457b-a0ae-ef9e493b68ba","originalAuthorName":"许并社"},{"authorName":"魏丽乔","id":"67e74fd9-c4e1-426e-88e5-acaa868d2d3b","originalAuthorName":"魏丽乔"},{"authorName":"马森源","id":"871e70b2-5d44-43e1-870a-79f49f232bd3","originalAuthorName":"马森源"}],"doi":"10.11896/j.issn.1005-023X.2015.18.010","fpage":"40","id":"051ef9ae-4248-4810-9178-c9acaf45b746","issue":"18","journal":{"abbrevTitle":"CLDB","coverImgSrc":"journal/img/cover/CLDB.jpg","id":"8","issnPpub":"1005-023X","publisherId":"CLDB","title":"材料导报"},"keywords":[{"id":"74032fbe-5666-4ddc-9a89-6d507c3eef3c","keyword":"相变材料","originalKeyword":"相变材料"},{"id":"2c74ca82-30cb-44c5-80b4-93a8f812db5e","keyword":"硅藻土","originalKeyword":"硅藻土"},{"id":"16820b4f-7f8c-4696-a0d3-29e7ec74610e","keyword":"正十八烷","originalKeyword":"正十八烷"},{"id":"24489483-003a-4ded-bcde-f1b1d9f72521","keyword":"吸附","originalKeyword":"吸附"}],"language":"zh","publisherId":"cldb201518010","title":"硅藻土吸附正十八烷高相变焓复合相变材料的制备及其性能研究","volume":"29","year":"2015"},{"abstractinfo":"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":"中国钧官瓷釉的实验与研究","volume":"31","year":"2012"},{"abstractinfo":"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,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":"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":"山东牟平家沟金矿床流体包裹体研究","volume":"36","year":"2015"},{"abstractinfo":"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":"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":"山东省牟平家沟金矿床地质特征","volume":"22","year":"2001"},{"abstractinfo":"脖河铜矿达矿段Ⅲ1-4号矿群共有5个矿体。通过研究达矿段的地质特征,基本查明了Ⅲ1-4号矿群5个矿体的形态、产状、空间位置及厚度、品位的变化情况;基于地质块段法在探矿区范围内对Ⅲ1-4号矿群进行了资源/储量的估算,获得了5个铜矿体332+333总金属量18559.57 t,为脖河铜矿今后的进一步资源开发规划提供了依据。","authors":[{"authorName":"江训普","id":"19d78a9a-d7ed-4d75-ae30-22c3124cbcd9","originalAuthorName":"江训普"},{"authorName":"黄德镛","id":"9586c9ec-f096-46ac-9105-4051be6f0762","originalAuthorName":"黄德镛"},{"authorName":"陈雷","id":"403534a5-72d1-4c30-acf1-9990026bcff6","originalAuthorName":"陈雷"},{"authorName":"钟彩彩","id":"e0a2748a-df4a-48e8-b084-96921aede099","originalAuthorName":"钟彩彩"}],"doi":"10.11792/hj20160306","fpage":"28","id":"335a09ff-2baa-4931-af6f-eda180ade851","issue":"3","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"3b5e26a4-08b1-4b6f-8ade-417f1e760e8f","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"c72f5f24-e79b-4d2e-8712-eddc5f7e71b8","keyword":"Ⅲ1-4号矿群","originalKeyword":"Ⅲ1-4号矿群"},{"id":"55b17b4f-698e-4498-9162-269897357830","keyword":"资源/储量","originalKeyword":"资源/储量"},{"id":"87c3d4a9-db92-493a-acab-8b9d92e5c776","keyword":"估算","originalKeyword":"估算"},{"id":"137407be-8948-4058-a57d-7be4024eaece","keyword":"脖河铜矿达矿段","originalKeyword":"龙脖河铜矿龙达矿段"}],"language":"zh","publisherId":"huangj201603006","title":"脖河铜矿达矿段地质特征及资源/储量估算","volume":"37","year":"2016"},{"abstractinfo":"介绍了塘金矿多层堆浸的大规模、永久性堆浸场、采用一堆多区、交叉喷淋、逆流浸出、二次吸附和无氰解吸工艺的特点,及生产中取得的技术经济指标.","authors":[{"authorName":"巫汉泉","id":"dde9e2f7-5ecb-461d-8389-17fe5bfc9fb1","originalAuthorName":"巫汉泉"},{"authorName":"林源","id":"8e9a3f1a-211a-4fda-8dc9-6400b5e92531","originalAuthorName":"林源"}],"doi":"10.3969/j.issn.1001-1277.2002.10.010","fpage":"34","id":"1e3013c0-81e2-44c8-a834-23c297f6cf73","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"f01e8896-b973-487a-a564-ca1204fcb752","keyword":"堆浸","originalKeyword":"堆浸"},{"id":"7beb3211-c29b-4d24-ab0f-31058aa9b802","keyword":"喷淋","originalKeyword":"喷淋"},{"id":"3a7a5db4-08f6-48be-a846-14ea9b831665","keyword":"工艺特点","originalKeyword":"工艺特点"},{"id":"c346c25f-9fa0-4352-adcb-6b43d1ee9754","keyword":"指标","originalKeyword":"指标"}],"language":"zh","publisherId":"huangj200210010","title":"塘金矿堆浸工艺特点","volume":"23","year":"2002"},{"abstractinfo":"鸡公岩矿段位于高金矿区东部,为高金矿区的重要矿段.详细阐述了高金矿区鸡公岩矿段地质特征,并对矿床成因进行了分析,为进一步勘查开发高金矿区各矿段提供了依据.","authors":[{"authorName":"肖振","id":"e3b4a333-966b-4151-bbc5-1c3898302d64","originalAuthorName":"肖振"},{"authorName":"王广南","id":"84073893-b6b9-41a2-b3f6-1a24bac7f435","originalAuthorName":"王广南"}],"doi":"10.3969/j.issn.1001-1277.2011.11.005","fpage":"24","id":"82a39593-7e1f-4699-b5f9-6f3375666987","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"db2b844f-640a-47f0-a321-0cbfa14eee8a","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"e56de525-a0df-48fb-b363-8ce206589e1f","keyword":"矿床成因","originalKeyword":"矿床成因"},{"id":"b1e1ad41-9ea6-4cbb-b09f-468034e8b923","keyword":"高金矿区","originalKeyword":"高龙金矿区"}],"language":"zh","publisherId":"huangj201111005","title":"广西高金矿区鸡公岩矿段地质特征及矿床成因","volume":"32","year":"2011"},{"abstractinfo":"介绍了建钢铁烧结烟气脱硫工艺抉择过程中重点关注的原料特点、烟气参数、选择的原则、选择的依据等因素,较详细地介绍了建钢铁石灰-石膏法湿式脱硫工艺流程,并从工程建设角度,对选择该工艺后可能出现的腐蚀和磨损问题进行了应对策略分析.","authors":[{"authorName":"芮义斌","id":"7e6f7537-1190-450f-b712-0daea3f79f78","originalAuthorName":"芮义斌"},{"authorName":"赵宏","id":"ed80e639-fd34-4da6-b597-d3cbc01d986b","originalAuthorName":"赵宏"}],"doi":"10.3969/j.issn.1000-6826.2010.01.017","fpage":"39","id":"bac2fe71-756b-485c-b983-118325c8c6fe","issue":"1","journal":{"abbrevTitle":"JSSJ","coverImgSrc":"journal/img/cover/3abe017a-2574-4821-8152-4ae974ef0471.jpg","id":"47","issnPpub":"1000-6826","publisherId":"JSSJ","title":"金属世界"},"keywords":[{"id":"6d9408a7-41ff-4af6-8933-87226c1411b8","keyword":"烧结机","originalKeyword":"烧结机"},{"id":"749c272e-fa1f-4079-af32-e7887bc283fd","keyword":"烟气","originalKeyword":"烟气"},{"id":"ee3945cb-20c9-4847-8872-a779deca0d2a","keyword":"脱硫","originalKeyword":"脱硫"},{"id":"093e7a7c-4e78-4041-9552-d7162b694458","keyword":"磨损","originalKeyword":"磨损"},{"id":"01e87954-8644-42dd-a1d6-13a34b686ed0","keyword":"腐蚀","originalKeyword":"腐蚀"}],"language":"zh","publisherId":"jssj201001017","title":"建钢铁烧结烟气脱硫工艺抉择实践","volume":"","year":"2010"},{"abstractinfo":"赛材料作为一种新型水润滑轴承材料,在海洋工程中有广阔的应用前景,但目前有关海水介质对赛材料吸湿性及摩擦学性能的影响研究还不够深入.研究了赛材料在海水环境中的吸湿行为和摩擦磨损性能,分析了摩擦工况参数如润滑介质、载荷、转速等对赛材料润滑性能的影响规律.结果表明,在各测试条件下,海水均比纯水对赛材料有更好的润滑效果,其原因之一为赛在海水介质中浸泡后,基体-填料间的结合力更强.","authors":[{"authorName":"杨薇","id":"1afdcd27-ec68-4cbf-8103-4357b305f9f1","originalAuthorName":"杨薇"},{"authorName":"蒲晓妮","id":"aebae157-83d8-48f2-ae7f-64c3f5965305","originalAuthorName":"蒲晓妮"},{"authorName":"文光平","id":"a0e86df1-3492-4fd2-96f1-bd3fb3b7284a","originalAuthorName":"文光平"},{"authorName":"刘昊","id":"1eec66bd-8e36-4b26-8420-9b0358dc2be8","originalAuthorName":"刘昊"},{"authorName":"王建章","id":"de2e6eb8-a3af-4446-8acc-746c2e9733f7","originalAuthorName":"王建章"},{"authorName":"阎逢元","id":"5bb6bd47-5e9b-48fd-a79b-49321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