{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":1,"startPagecode":1},"records":[{"abstractinfo":"分析了TP2铜盘管在Junker炉中退火的传热过程,利用有限元软件MSC.Mare模拟了铜盘管退火过程的温度变化,研究了退火过程中铜盘管\"热点\"和\"冷点\"温度变化的规律.模拟结果表明:退火过程中铜盘管的温度分布是不均匀的,铜盘管中出现表面\"热点\"和中心\"冷点\";在退火时间上,\"冷点\"比\"热点\"要滞后一段时间.实测了TP2铜盘管在Junker炉中退火的温度场,测量结果与数值模拟结果一致.","authors":[{"authorName":"<span style=\"color:red\">潘</span><span style=\"color:red\">进兵</span>","id":"47b8439f-93cb-4bbe-9372-32f044a56635","originalAuthorName":"潘进兵"},{"authorName":"张士宏","id":"01c30ce8-98fa-4aad-bd64-0c65b712256e","originalAuthorName":"张士宏"},{"authorName":"张立文","id":"7d6090ff-117b-4218-8a95-d1ce32ae4fa4","originalAuthorName":"张立文"},{"authorName":"刘劲松","id":"58377fee-a227-4090-86ea-2aac552c20da","originalAuthorName":"刘劲松"},{"authorName":"张海渠","id":"cc649a3b-cb56-4805-9694-71183f991a16","originalAuthorName":"张海渠"}],"doi":"","fpage":"171","id":"224457da-4ee8-4d02-979f-07f547c7155e","issue":"2","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":"fa35680b-5bc3-4078-9f33-e45ebf1bfac0","keyword":"铜盘管","originalKeyword":"铜盘管"},{"id":"05c19062-2276-4587-a148-e9c24f3c3c2c","keyword":"Junker炉","originalKeyword":"Junker炉"},{"id":"2e1d475c-ac4e-4885-b573-c43dbcb12c81","keyword":"温度场","originalKeyword":"温度场"},{"id":"e2b3d87f-92f4-410a-9136-211718e0d110","keyword":"有限元","originalKeyword":"有限元"}],"language":"zh","publisherId":"jsrclxb200802039","title":"TP2铜盘管Junker炉退火温度场的有限元模拟","volume":"29","year":"2008"},{"abstractinfo":"基于构造逐级控制理论,以江苏泗洪县褶皱区的区域地质为背景,运用地质构造解析和物化探等手段研究矿区构造.结果表明,区域构造控制矿区构造,矿区构造反映区域构造.宿迁市泗洪县<span style=\"color:red\">潘</span>赵庄铜镍矿区处于构造有利区,岩石化学特征对形成铜镍硫化物矿床较为有利,具备铜镍硫化物矿床的找矿前提,确定有利靶区受构造控制作用明显,存在于岩体中下部熔离型矿体及岩体边贯入式矿体两处.","authors":[{"authorName":"罗跃","id":"744127b8-7fa6-4807-96bc-8226affe3bff","originalAuthorName":"罗跃"},{"authorName":"周贤金","id":"074c8c12-ab87-4459-9d53-f08320a80ca8","originalAuthorName":"周贤金"},{"authorName":"施建斌","id":"e7efc5f3-3467-429c-a26b-986b5b37f807","originalAuthorName":"施建斌"},{"authorName":"冯学知","id":"c4d96ab0-cf41-4f0a-aea3-6042ba5a1bdf","originalAuthorName":"冯学知"},{"authorName":"刘正疆","id":"6b5ad79e-3d4c-4e3f-b65a-78778d2f5430","originalAuthorName":"刘正疆"},{"authorName":"张琪","id":"69cc55d7-64c9-4bcb-8cad-a9d676dd0962","originalAuthorName":"张琪"}],"doi":"10.3969/j.issn.2095-1744.2013.06.010","fpage":"48","id":"139b4e79-0f29-4c56-ac61-41753022d73d","issue":"6","journal":{"abbrevTitle":"YSJSGC","coverImgSrc":"journal/img/cover/YSJSGC.jpg","id":"76","issnPpub":"2095-1744","publisherId":"YSJSGC","title":"有色金属工程"},"keywords":[{"id":"c20e5d56-689a-40aa-9a63-796dac006db7","keyword":"铜-镍硫化矿","originalKeyword":"铜-镍硫化矿"},{"id":"5a907ae9-825e-4737-a764-797201503314","keyword":"构造逐级控制","originalKeyword":"构造逐级控制"},{"id":"c138a0de-cc7e-440c-8177-b76cf229ee27","keyword":"构造指示矿","originalKeyword":"构造指示矿"},{"id":"36755356-60f4-4d84-90e5-ab2910d6c12a","keyword":"靶区","originalKeyword":"靶区"},{"id":"44cad5bd-df83-4450-97f6-9b6e490ab7c9","keyword":"泗洪县","originalKeyword":"泗洪县"}],"language":"zh","publisherId":"ysjs201306015","title":"<span style=\"color:red\">潘</span>赵庄铜镍矿区构造逐级控制及构造指示矿特征探讨","volume":"3","year":"2013"},{"abstractinfo":"试样于<span style=\"color:red\">潘</span>菲氏管中加入还原铁粉,加热使汞与基体及共存元素分离;试验了氢化物-原子荧光光谱法测定汞的最佳条件.汞的检出限为0.05ng/mL,线性范围为0.5～250ng/mL,汞的回收率为94%～101%.方法应用于锌精矿中汞的测定,取得满意结果.","authors":[{"authorName":"钟勇","id":"28126a39-4461-43d5-85c3-fe3a51b87f74","originalAuthorName":"钟勇"}],"doi":"10.3969/j.issn.1000-7571.2002.01.012","fpage":"38","id":"d43ad448-87f6-4c0c-9651-93da5de3aadf","issue":"1","journal":{"abbrevTitle":"YJFX","coverImgSrc":"journal/img/cover/YJFX.jpg","id":"71","issnPpub":"1000-7571","publisherId":"YJFX","title":"冶金分析   "},"keywords":[{"id":"a2e8e9c0-5aab-4736-9937-982056210857","keyword":"<span style=\"color:red\">潘</span>菲氏管","originalKeyword":"潘菲氏管"},{"id":"c3888355-ef2a-44c7-91ef-2b4d70031e81","keyword":"氢化物","originalKeyword":"氢化物"},{"id":"805c6bb7-c5dc-489d-9e0c-37dc385c05f8","keyword":"冷原子荧光光谱法","originalKeyword":"冷原子荧光光谱法"},{"id":"e2805568-4e3c-4b8f-bf78-31f522e2f76d","keyword":"锌精矿","originalKeyword":"锌精矿"},{"id":"536aae8f-f0d4-4aff-a0b7-256b6e58239f","keyword":"汞","originalKeyword":"汞"}],"language":"zh","publisherId":"yjfx200201012","title":"<span style=\"color:red\">潘</span>菲氏管分离氢化物-冷原子荧光光谱法测定锌精矿中微量汞","volume":"22","year":"2002"},{"abstractinfo":"介绍了美国、独联体、日本、比利时和以色列用于8～12 μm红外系的锗晶体的生产方法, 包括CZ法、定向结晶法、铸造法、斯捷<span style=\"color:red\">潘</span>诺夫法、旋转晶片法、斯拉克巴杰法和籽晶垂直梯度凝固法. 国外已分别用CZ法和定向凝固法生产出Φ300 mm和Φ520 mm的大直径锗单晶.","authors":[{"authorName":"李贺成","id":"110f9244-1f03-4ef5-9a8f-3bb28de99dcd","originalAuthorName":"李贺成"},{"authorName":"王铁艳","id":"6d5c4b09-aef8-456b-b82f-6cb65013c8a1","originalAuthorName":"王铁艳"}],"doi":"10.3969/j.issn.0258-7076.2000.03.010","fpage":"203","id":"7c31e131-f312-4ed3-b19c-689bd11af622","issue":"3","journal":{"abbrevTitle":"XYJS","coverImgSrc":"journal/img/cover/XYJS.jpg","id":"67","issnPpub":"0258-7076","publisherId":"XYJS","title":"稀有金属"},"keywords":[{"id":"bdcad738-4678-4f75-9a92-145da9f63935","keyword":"红外用锗晶体","originalKeyword":"红外用锗晶体"},{"id":"eae6c049-42b3-4655-bacd-cef86c895edc","keyword":"CZ法","originalKeyword":"CZ法"},{"id":"f61bc3dd-5af2-46f8-bd46-d855c03043ff","keyword":"定向凝固法","originalKeyword":"定向凝固法"},{"id":"d6d88a2a-0318-4d83-a326-d56d4545961d","keyword":"斯捷<span style=\"color:red\">潘</span>诺夫法","originalKeyword":"斯捷潘诺夫法"},{"id":"44e426b2-58ac-4829-b780-6b83d2d9964e","keyword":"铸造法","originalKeyword":"铸造法"}],"language":"zh","publisherId":"xyjs200003010","title":"国外红外用大尺寸锗晶体的生产方法及水平","volume":"24","year":"2000"},{"abstractinfo":"光栅式自由立体显示设备由于存在重影问题而限制了它们在商业上的应用,文章从<span style=\"color:red\">潘</span>弄区和可视区域两个角度分析了光栅式自由立体显示设备产生重影问题的理论原因,并建立一个光学结构模型,推导出人眼所看到的实际像素强度公式.给出一种定义重影度的方法,经软件仿真得到重影度与人眼到显示屏幕距离的关系曲线,基于上述模型和定义对重影问题的改善进行了探讨.软件仿真结果显示通过改善边缘光栅结构能在一定程度上增大可视区域,减小人眼看到重影的几率.","authors":[{"authorName":"文江涛","id":"a9b97380-4085-41ae-917e-355f2f266f27","originalAuthorName":"文江涛"},{"authorName":"胡跃辉","id":"5c2b5969-7332-47cc-b386-53e4ef6511dc","originalAuthorName":"胡跃辉"},{"authorName":"吕国强","id":"262c69b6-fc82-47b2-a2c8-eeafb381e658","originalAuthorName":"吕国强"},{"authorName":"钱鑫","id":"b7b8995c-3d66-4595-9cd6-393e6f486baa","originalAuthorName":"钱鑫"},{"authorName":"宋志成","id":"b7967906-e098-4a2a-a2ba-6c440b3ce2d0","originalAuthorName":"宋志成"}],"doi":"10.3969/j.issn.1007-2780.2007.03.015","fpage":"310","id":"87ababb6-8311-4965-9dfd-885c5be5a079","issue":"3","journal":{"abbrevTitle":"YJYXS","coverImgSrc":"journal/img/cover/YJYXS.jpg","id":"72","issnPpub":"1007-2780","publisherId":"YJYXS","title":"液晶与显示   "},"keywords":[{"id":"ce0a0954-384f-49f4-b69d-c7f0bd24e9ab","keyword":"自由立体显示","originalKeyword":"自由立体显示"},{"id":"89a72c4f-02d6-4aa1-9ecf-2b929d201710","keyword":"视差光栅","originalKeyword":"视差光栅"},{"id":"00972ae3-d1a7-4ddc-80f0-3e71279c72b3","keyword":"重影","originalKeyword":"重影"},{"id":"536a13d5-90ab-40d6-a58f-3660b02a9017","keyword":"<span style=\"color:red\">潘</span>弄区","originalKeyword":"潘弄区"},{"id":"b038b26d-ada2-49ce-aafe-d5f014957edd","keyword":"立体图像对","originalKeyword":"立体图像对"}],"language":"zh","publisherId":"yjyxs200703015","title":"光栅式立体显示器重影问题的研究","volume":"22","year":"2007"},{"abstractinfo":"根据2012年11月至2013年9月的9次监测数据，分析了淮南<span style=\"color:red\">潘</span>集开放型和封闭型沉陷区地表水与浅层地下水中氮、磷时间分布特征；通过相关性分析揭示了各类水体内氮、磷之间的响应关系和运移特征；通过各形态氮、磷比对研究区水体营养状态进行了限制性分析。结果表明，两类沉陷积水区内氮、磷时间分布存在一定差异，主要影响因素有降雨、周围农业面源输入、外部河流的互相补给等；各类水体内氮、磷之间均存在不同程度的响应，封闭型沉陷区地表水与浅层地下水中氮、磷响应关系更强；两类沉陷积水区均属磷限制性水体。","authors":[{"authorName":"范廷玉","id":"bc34a974-dbc8-4190-8504-87227fef3956","originalAuthorName":"范廷玉"},{"authorName":"谷得明","id":"6b11f20b-2de3-4580-8334-ee7511fdec6f","originalAuthorName":"谷得明"},{"authorName":"严家平","id":"ea8e3e33-022a-4c3b-8962-448469f84b72","originalAuthorName":"严家平"},{"authorName":"王顺","id":"e7eedc97-eaaf-43aa-9c6f-ca19049e096b","originalAuthorName":"王顺"},{"authorName":"程方奎","id":"379a06e1-c2e1-44f7-90db-65c4177d1801","originalAuthorName":"程方奎"},{"authorName":"陈永春","id":"0a2b040a-0eb2-40ee-8512-9428b5312746","originalAuthorName":"陈永春"},{"authorName":"陆春辉","id":"ff86f9f8-4ff9-43c8-9939-ebc7a624dcb4","originalAuthorName":"陆春辉"},{"authorName":"李国瑞","id":"c56860f6-ec6e-41e7-84ee-e320f150e2bd","originalAuthorName":"李国瑞"},{"authorName":"陈威","id":"18a822d8-a7ac-4a15-983b-cbd5cb226b22","originalAuthorName":"陈威"}],"doi":"10.7524/j.issn.0254-6108.2015.06.2015020501","fpage":"1158","id":"a45f4584-184a-452b-b050-3663ccdd75cf","issue":"6","journal":{"abbrevTitle":"HJHX","coverImgSrc":"journal/img/cover/HJHX.jpg","id":"43","issnPpub":"0254-6108","publisherId":"HJHX","title":"环境化学   "},"keywords":[{"id":"d15ffa94-96cd-4307-931a-7de053ce4df7","keyword":"采煤沉陷积水区","originalKeyword":"采煤沉陷积水区"},{"id":"a263ac95-93de-4122-bc9d-7cd10c2e1860","keyword":"地表水","originalKeyword":"地表水"},{"id":"ae62d918-f61b-420b-8746-cb4fca7fda3a","keyword":"浅层地下水","originalKeyword":"浅层地下水"},{"id":"a63a868a-a776-4c41-886b-04ddf52a04eb","keyword":"氮磷","originalKeyword":"氮磷"}],"language":"zh","publisherId":"hjhx201506018","title":"采煤沉陷积水区地表水与浅层地下水的氮、磷动态及相关性?","volume":"","year":"2015"}],"totalpage":1,"totalrecord":6}