{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":2,"startPagecode":1},"records":[{"abstractinfo":"纯低温余热发电技术开始应用于钢铁、玻璃等行业,给企业带来巨大的环保和经济效益.对信义玻璃厂的热工标定数据分析,信义公司各玻璃生产线出窑废气温度较水泥窑废气温度高100℃以上,总余热发电量可达1.4万kW.从余热发电的效益评估来看增加余热发电系统,只需两到三年多就可回收成本.并能有效充分地利用能源,减少SO2等有毒粉尘和CO2排放量.","authors":[{"authorName":"冠军","id":"a87a07eb-17f1-4d85-98f2-7d59ed24509b","originalAuthorName":"宋冠军"},{"authorName":"孙士华","id":"7df279e1-caca-41ae-b528-b06d3b138b86","originalAuthorName":"孙士华"},{"authorName":"李昌勇","id":"715ae289-0200-494c-bcfb-b2b3903664a2","originalAuthorName":"李昌勇"}],"doi":"","fpage":"1208","id":"56823666-d6b6-42bb-8426-5ad37064582d","issue":"5","journal":{"abbrevTitle":"GSYTB","coverImgSrc":"journal/img/cover/GSYTB.jpg","id":"36","issnPpub":"1001-1625","publisherId":"GSYTB","title":"硅酸盐通报 "},"keywords":[{"id":"b45abed1-4cbb-475a-8fd8-9a4c5caed47a","keyword":"热工检测","originalKeyword":"热工检测"},{"id":"4cfe89b2-8d16-4ece-9c13-307fee83a8d5","keyword":"余热发电","originalKeyword":"余热发电"},{"id":"d7383ae6-c27e-4958-85f2-1a59fb9742af","keyword":"效益评估","originalKeyword":"效益评估"}],"language":"zh","publisherId":"gsytb201205034","title":"余热发电在玻璃厂中的应用及节能分析","volume":"31","year":"2012"},{"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":"","authors":[{"authorName":"米文权","id":"c0ded1b5-46db-47ee-a75f-b458d7bf8376","originalAuthorName":"米文权"}],"doi":"10.3969/j.issn.1000-6826.2004.04.020","fpage":"48","id":"dca703f6-f3db-4d39-b2b1-503179353970","issue":"4","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":"f14238da-eb67-4194-9e5e-a531d0504c83","keyword":"","originalKeyword":""}],"language":"zh","publisherId":"jssj200404020","title":"小小纤维,虽貌不惊人,却前途无量世界跳高冠军的秘密武器","volume":"","year":"2004"},{"abstractinfo":"","authors":[{"authorName":"林昆勇","id":"125c9b8d-d115-4a18-83c5-e7fb6db76372","originalAuthorName":"林昆勇"}],"doi":"10.3969/j.issn.1000-6826.2008.05.026","fpage":"63","id":"4d32e81a-4290-4950-8281-71be62c203fb","issue":"5","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":"77990c78-4472-4cd7-a01c-b9b6493da031","keyword":"","originalKeyword":""}],"language":"zh","publisherId":"jssj200805026","title":"明代应星《天工开物》记载广西产锡及其意义——我国锡矿资源的供给保障与开发战略研究之一","volume":"","year":"2008"},{"abstractinfo":"","authors":[],"doi":"","fpage":"52","id":"88d02802-635f-4302-a930-1eaf14ab619c","issue":"5","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"b4d21286-b321-460c-96a5-1ee920b4d33a","keyword":"","originalKeyword":""}],"language":"zh","publisherId":"huangj200905017","title":"中国共产党中国黄金集团公司第二次代表大会在北京召开创新党建工作推动公司科学发展大会选举产生公司新一届党的委员会和纪律检查委员会孙兆学当选党委书记权礼当选党委副书记、纪委书记","volume":"30","year":"2009"},{"abstractinfo":"用仪器中子活化分析研究了陕西立地坡明代地层和陕西西岳庙、元、明、清早期、清晚期4个地层出土的古琉璃胎中的主量和微量元素, 并对实验数据进行多元统计分析.结果表明, 陕西西岳庙从到清早期古琉璃胎料很稳定, 其原料可能来自本地; 清晚期古琉璃胎料与到清早期的古琉璃之间存在明显的区别, 明代3个样品和清晚期的古琉璃制造原料与立地坡出土的古琉璃其成分相近, 西岳庙清晚期的古琉璃可能来自陕西立地坡窑烧制.","authors":[{"authorName":"程琳","id":"346d8ac0-f1f3-4288-8b83-cf846cdeae3b","originalAuthorName":"程琳"},{"authorName":"冯松林","id":"b5f2de6e-5095-40a4-9ef0-c714b975666b","originalAuthorName":"冯松林"},{"authorName":"吕智荣","id":"ca7086b8-3f39-4955-92c9-57156131d841","originalAuthorName":"吕智荣"}],"doi":"10.3969/j.issn.1007-4627.2005.01.041","fpage":"135","id":"b97de8ad-7714-4b41-a397-cb49135e51aa","issue":"1","journal":{"abbrevTitle":"YZHWLPL","coverImgSrc":"journal/img/cover/YZHWLPL.jpg","id":"78","issnPpub":"1007-4627","publisherId":"YZHWLPL","title":"原子核物理评论 "},"keywords":[{"id":"4a654b0f-0a63-4416-a372-c4326f0153b5","keyword":"古琉璃","originalKeyword":"古琉璃"},{"id":"76f6e7fb-9a67-426e-8669-a147b5ac107d","keyword":"仪器中子活化分析","originalKeyword":"仪器中子活化分析"},{"id":"1ba93e9f-2f8e-4cdf-89f0-e04dfd3b1766","keyword":"多元统计分析","originalKeyword":"多元统计分析"}],"language":"zh","publisherId":"yzhwlpl200501041","title":"陕西西岳庙古琉璃胎料来源的INAA研究及多元统计分析","volume":"22","year":"2005"},{"abstractinfo":"$lP海水腐蚀导致铜镍合金的沿晶析出…………………………………………………………… .林乐耘 刘少峰 朱,]、龙门)阵列电极法测量聚合物/金属界面电位分布……………………… ..林昌健 卓向东 陈纪东 王 辉(7)叫义钢管桩阴极保护时的电位分布…………………… 邱 枫 徐乃欣卜)钠筋在混凝土模拟液中腐蚀行为的*IS特证… ,……….刘晓敏 史志明 林海潮 光铃 曹楚南(19)磁场和 C厂对铁在中性 Na:SOa溶液中阳极极化行为?...","authors":[],"categoryName":"|","doi":"","fpage":"314","id":"0cf605d4-95c1-4062-8fa7-a74fc5609696","issue":"4","journal":{"abbrevTitle":"ZGFSYFHXB","coverImgSrc":"journal/img/cover/中国腐蚀封面19-3期-01.jpg","id":"81","issnPpub":"1005-4537","publisherId":"ZGFSYFHXB","title":"中国腐蚀与防护学报"},"keywords":[],"language":"zh","publisherId":"1005-4537_1997_4_6","title":"1997年总目录","volume":"17","year":"1997"},{"abstractinfo":"钢在厦门海域飞溅带腐蚀数学模型分析林志坚,文桑(中国船舶工业总公司七二五研究所厦门分部,厦门361002)根据暴露在厦门试验平台飞溅带几种钢8年的腐蚀数据,按大气腐蚀常用的数字模型:F=KT”(。进行曲线拟合,并进行二次回归分析,获得相关系数大于0.95的回归方程:F-A+BT’+C/T’(2,讨论和分析回归系数与耐蚀性的关系,从而了解不同钢种腐蚀变化规律.TablelLnF—Lnk+nLnt,F—A+BTZ+C/TZ(F:mm,T:a)国家自然科学基金重大项目选用的....","authors":[{"authorName":"林志坚","id":"d9359627-d8f1-4a66-a425-71ace34fa247","originalAuthorName":"林志坚"},{"authorName":"文桑","id":"4586ebf6-1605-4254-834f-65947fd5ba0d","originalAuthorName":"宋文桑"}],"categoryName":"|","doi":"","fpage":"256","id":"27de5284-1a0d-49c2-a0c3-0c799776902d","issue":"3","journal":{"abbrevTitle":"FSKXYFHJS","coverImgSrc":"journal/img/cover/FSKXYFHJS.jpg","id":"24","issnPpub":"1002-6495","publisherId":"FSKXYFHJS","title":"腐蚀科学与防护技术"},"keywords":[],"language":"zh","publisherId":"1002-6495_1995_3_21","title":"钢在厦门海域飞溅带腐蚀数学模型分析","volume":"7","year":"1995"}],"totalpage":2,"totalrecord":12}