{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"为预测注塑成型中短纤维取向分布,提出了在模拟分析中采用RSC纤维取向预测模型对纤维取向分布进行预测的方法.基于RSC取向模型,通过第二顺序张量aij对三维取向分辨率进行描述,采用Orthotropic闭合近似模型对RSC模型进行求解.采用MoldFlow软件对RSC模型的纤维取向分布进行了模拟,分析了相互作用系数Ci及标量因子k对纤维取向的影响.并获得了纤维取向随空间、时间的取向规律——沿宽度方向,两端面的取向要大于中心层,并且端面在开始阶段就能达到很高的纤维取向;沿流动方向,在浇口及充填末端,纤维取向都呈下降趋势,而中间部分则有所增加.","authors":[{"authorName":"王梦寒","id":"5aa717dd-6075-48a5-9a6b-e0a2e32aaab5","originalAuthorName":"王梦寒"},{"authorName":"<span style=\"color:red\">杨</span>海","id":"dce934fb-9d53-46dc-8dc6-4a272778d100","originalAuthorName":"杨海"},{"authorName":"董晶晶","id":"7185b5c9-62f2-4ba1-99bc-984dc05ee763","originalAuthorName":"董晶晶"},{"authorName":"周杰","id":"c6d9d4ff-5481-43c0-8bab-0cdb345024c9","originalAuthorName":"周杰"},{"authorName":"<span style=\"color:red\">杨</span><span style=\"color:red\">运</span><span style=\"color:red\">成</span>","id":"2cbd0160-7c1e-403a-9dff-e90764e91092","originalAuthorName":"杨运成"},{"authorName":"姚小兵","id":"1425e2a8-282b-48da-a36d-fa36919c2aa8","originalAuthorName":"姚小兵"}],"doi":"","fpage":"105","id":"239ef5d1-c202-46e0-b28f-5e22eec254b7","issue":"3","journal":{"abbrevTitle":"GFZCLKXYGC","coverImgSrc":"journal/img/cover/GFZCLKXYGC.jpg","id":"31","issnPpub":"1000-7555","publisherId":"GFZCLKXYGC","title":"高分子材料科学与工程"},"keywords":[{"id":"ad511958-f0fa-413c-bed7-a42747c54c68","keyword":"纤维取向","originalKeyword":"纤维取向"},{"id":"4627f6af-94b0-46bf-a4c3-1dfee2e0218d","keyword":"RSC模型","originalKeyword":"RSC模型"},{"id":"d1d5a6ab-7105-43ef-bc43-636fbf36a38f","keyword":"Orthotropic闭合近似","originalKeyword":"Orthotropic闭合近似"},{"id":"e5cf0118-f298-410e-98fb-f2985e839d3c","keyword":"相互作用系数","originalKeyword":"相互作用系数"},{"id":"83aecaec-0ee8-49d1-a0ac-7c6eaff9d074","keyword":"标量因子","originalKeyword":"标量因子"}],"language":"zh","publisherId":"gfzclkxygc201403023","title":"RSC模型中相互作用系数和标量因子对短纤维取向的影响","volume":"30","year":"2014"},{"abstractinfo":"本文以深部咸水层二氧化碳地质封存为背景，针对超临界压力二氧化碳和水在岩心中的驱替过程和<span style=\"color:red\">运</span>移规律进行了可视化研究。本文主要通过实验方法，利用核磁共振设备，得到了岩心的孔隙率、岩心中超临界压力二氧化碳水相对渗透率随饱和度变化曲线及不同时刻岩心中水的分布特征等。研究表明，用核磁测量得到的岩心孔隙率具有很高精确度，利用核磁共振得到横向弛豫时间乃图谱，可以有效分析有效孔隙率和可流动流体所占比例。通过观察不同注入比例时的切层图像，发现在注入比例为CO2：H2O=3：1（体积比）时在入口处出现了较显著的浮升力作用。","authors":[{"authorName":"马瑾","id":"24737854-58b8-4aa2-8b4c-333011f99b7a","originalAuthorName":"马瑾"},{"authorName":"胥蕊娜","id":"3cd95e41-f40b-403c-a0ac-108539e135d8","originalAuthorName":"胥蕊娜"},{"authorName":"罗庶","id":"67ed5c7c-0d86-453c-b771-393ffee84b27","originalAuthorName":"罗庶"},{"authorName":"姜培学","id":"7851283d-fe83-4e02-8337-7cf612b35197","originalAuthorName":"姜培学"}],"doi":"","fpage":"1971","id":"9ede31f3-36f2-442f-9f3c-20459e356ed3","issue":"11","journal":{"abbrevTitle":"GCRWLXB","coverImgSrc":"journal/img/cover/GCRWLXB.jpg","id":"32","issnPpub":"0253-231X","publisherId":"GCRWLXB","title":"工程热物理学报   "},"keywords":[{"id":"2b4671d9-6fd6-4fbb-af22-2565ed0465a6","keyword":"二氧化碳","originalKeyword":"二氧化碳"},{"id":"6b4f6558-8e0c-452f-ac75-1c3c67c9da39","keyword":"深部咸水层","originalKeyword":"深部咸水层"},{"id":"3365e65d-d2c9-4cdb-b0be-519703d7017e","keyword":"相对渗透率","originalKeyword":"相对渗透率"},{"id":"81aed073-7b34-4016-bb76-035685b9b166","keyword":"饱和度","originalKeyword":"饱和度"}],"language":"zh","publisherId":"gcrwlxb201211035","title":"超临界压力CO2在深部<span style=\"color:red\">成</span>水层中<span style=\"color:red\">运</span>移规律研究","volume":"33","year":"2012"},{"abstractinfo":"采用Woods-Saxon形成的密度函数，按照<span style=\"color:red\">杨</span>立铭方法以及稍微修改的方法进行估算都得出，紧接126的幻数应该接近于184．","authors":[{"authorName":"李先卉","id":"de0a8216-5ace-4a39-a9c2-dc0e4635868d","originalAuthorName":"李先卉"},{"authorName":"周治宁","id":"fb0bee5a-b978-479d-a348-7cfeb81683ff","originalAuthorName":"周治宁"},{"authorName":"钟毓澍","id":"7e1c646a-9dd6-4099-a1dd-48a38d24785c","originalAuthorName":"钟毓澍"},{"authorName":"<span style=\"color:red\">杨</span>泽森","id":"dac8f638-c051-480c-899f-55daa616b078","originalAuthorName":"杨泽森"}],"doi":"10.3969/j.issn.1007-4627.2000.01.009","fpage":"39","id":"24ab9145-669e-473f-940c-46aafa41541e","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":"a56c609f-1561-4216-adb0-fc937f323b42","keyword":"超重核幻数","originalKeyword":"超重核幻数"},{"id":"bc154b1b-0f42-4d6f-9e65-64cf1cf70b5f","keyword":"<span style=\"color:red\">杨</span>立铭方法","originalKeyword":"杨立铭方法"},{"id":"913e281b-2cf2-4469-99de-7758f327a0c2","keyword":"Thomas-Fermi近似","originalKeyword":"Thomas-Fermi近似"}],"language":"zh","publisherId":"yzhwlpl200001009","title":"用<span style=\"color:red\">杨</span>立铭方法估算大于126的幻数","volume":"17","year":"2000"},{"abstractinfo":"倾斜、厚矿体应用爆力<span style=\"color:red\">运</span>矿采矿法回采,可以很好地解决矿房内的<span style=\"color:red\">运</span>矿问题.文中详述了中深孔爆力<span style=\"color:red\">运</span>矿采矿法回采工艺及应用技术要求,应用实践表明,该采矿法采准比小、成本低、工艺简单、便于管理.","authors":[{"authorName":"李景利","id":"6a934420-57fb-4e0d-b1fe-941bbd002707","originalAuthorName":"李景利"}],"doi":"10.3969/j.issn.1001-1277.2007.08.008","fpage":"28","id":"2b2db1e8-b9bd-42e5-8bfe-8e62c94766f2","issue":"8","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"35f6eade-a720-484c-8266-dfe8a0ca7663","keyword":"倾斜厚矿体","originalKeyword":"倾斜厚矿体"},{"id":"6a84044a-f32f-438b-9be3-c84c24aeff8e","keyword":"爆力<span style=\"color:red\">运</span>矿","originalKeyword":"爆力运矿"},{"id":"20623978-005a-4fa5-9dc8-204bbcee5d07","keyword":"乌拉嘎金矿","originalKeyword":"乌拉嘎金矿"}],"language":"zh","publisherId":"huangj200708008","title":"中深孔爆力<span style=\"color:red\">运</span>矿采矿法在乌拉嘎金矿的应用","volume":"28","year":"2007"},{"abstractinfo":"基于中国科学院近代物理研究所正在研制的兰州重离子治疗专用装置（HITFiL）的参数和指标,对从回旋加速器到同步加速器之间中能传输段的纵向束流匹配过程进行了模拟分析。根据主加速器的注入要求,在束<span style=\"color:red\">运</span>线上采用了散束器以降低束流动量分散,从理论上分析了中能传输段末端可能实现的最小动量分散和达到最小动量分散的条件,讨论了散束效果与初始动量分散、束团相宽和漂移长度的关系。并利用MathCAD程序对束团在束<span style=\"color:red\">运</span>线上的纵向运动进行了跟踪模拟,使用PBO-Lab程序进行了验算,得到了当散束器射频电压为102kV时,末端动量分散为最小值2.764×10-4。进一步提出了中能传输段的基本参数,也为下一步的优化设计提供了基础。","authors":[{"authorName":"谢修璀","id":"6c639d00-c5af-4e55-9eb4-b316217e086f","originalAuthorName":"谢修璀"},{"authorName":"宋明涛","id":"4bed1e29-fca1-44da-98c6-3c9da61aa129","originalAuthorName":"宋明涛"},{"authorName":"郝焕锋","id":"f3b4fba0-227f-4ede-b7f4-920f0157b1e8","originalAuthorName":"郝焕锋"},{"authorName":"王贤武","id":"46e5ed29-dfeb-4dfc-aac0-421cae49fd37","originalAuthorName":"王贤武"}],"doi":"","fpage":"62","id":"a5600d80-23aa-4304-aab3-ea914e84d31b","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":"a868b012-946a-4971-bda6-7c99c10a7a49","keyword":"HITFiL","originalKeyword":"HITFiL"},{"id":"97d474bd-21df-4072-8d62-3e6751d85964","keyword":"散束器","originalKeyword":"散束器"},{"id":"57322204-4c68-48e4-9ed0-ad2f33c4e58a","keyword":"能散","originalKeyword":"能散"},{"id":"cb151bd0-aff2-45a3-8c0a-a83e015b514c","keyword":"纵向运动","originalKeyword":"纵向运动"},{"id":"f0f6ff99-4401-4c3b-8c84-1e28e4efd603","keyword":"束流匹配","originalKeyword":"束流匹配"}],"language":"zh","publisherId":"yzhwlpl201201009","title":"HITFiL中能束<span style=\"color:red\">运</span>线的纵向匹配","volume":"29","year":"2012"},{"abstractinfo":"<span style=\"color:red\">杨</span>坪金矿床赋存于下古生界丹凤群大草坝组变火山—沉积建造中,金矿化严格受层间挤压破碎(片理化)带控制,赋矿岩性为蚀变的二云石英片岩、绢云母石英片岩、绿泥石英片岩等变质岩及黄铁矿化石英脉,金矿化受变质、构造及次生氧化三重作用控制.对<span style=\"color:red\">杨</span>坪金矿床的地质特征及控矿特征进行了系统的研究,总结了找矿标志,并指出了找矿方向.","authors":[{"authorName":"张银斗","id":"8764fff0-6afd-4f47-8cbb-a0bc3aebc5e3","originalAuthorName":"张银斗"}],"doi":"","fpage":"24","id":"7c98a968-7112-4917-9271-e00b77970427","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"5034aee0-cb40-4bd0-b883-2eb1d15eac4b","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"5f6b6235-c284-4a52-a713-e0bb3ac50aa3","keyword":"控矿特征","originalKeyword":"控矿特征"},{"id":"1e4733d3-52c3-4c63-9072-ff2e17cf002e","keyword":"找矿标志","originalKeyword":"找矿标志"},{"id":"f0b2ed2b-45f9-4bad-aba9-8b696a60102b","keyword":"找矿方向","originalKeyword":"找矿方向"},{"id":"abe0bc7e-b8e2-4095-a867-8c7cbb45a24f","keyword":"<span style=\"color:red\">杨</span>坪金矿床","originalKeyword":"杨坪金矿床"}],"language":"zh","publisherId":"huangj201301006","title":"甘肃<span style=\"color:red\">杨</span>坪金矿床控矿特征及找矿方向","volume":"","year":"2013"},{"abstractinfo":"<span style=\"color:red\">杨</span>砦峪金矿床为河南灵宝小秦岭地区一重要大型石英脉型金矿床,矿床空间产出受太华群变质地层、岩浆岩及断裂构造控制,层间断裂为主要容矿构造.矿脉内矿体产出表现出\"尖灭再现\"、\"尖灭侧现\"规律.综合研究表明,小秦岭地区金矿床深部具有存在第二矿化富集段的可能性,在<span style=\"color:red\">杨</span>砦峪矿区,矿脉东段深部仍存在较好的成矿远景和找矿潜力.","authors":[{"authorName":"张庆超","id":"bab17d0e-bafb-4b0d-a46c-af63e0f92041","originalAuthorName":"张庆超"}],"doi":"10.3969/j.issn.1001-1277.2004.10.006","fpage":"19","id":"a5e01dd1-9aa0-45a0-bbfc-dc367c2a13db","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"96b81f72-8929-4e32-a794-35b0f3908133","keyword":"<span style=\"color:red\">杨</span>砦峪金矿床","originalKeyword":"杨砦峪金矿床"},{"id":"6027da23-6ddc-4696-b051-89c13227848a","keyword":"石英脉型","originalKeyword":"石英脉型"},{"id":"0cb416f8-b21f-4ff8-b599-e31978de5af7","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"1379a96f-cb9d-492f-9621-dd980419d399","keyword":"深部成矿远景","originalKeyword":"深部成矿远景"}],"language":"zh","publisherId":"huangj200410006","title":"<span style=\"color:red\">杨</span>砦峪金矿床地质特征及深部成矿远景评价","volume":"25","year":"2004"},{"abstractinfo":"本文研究了应用稀土保水剂对干旱地区新疆<span style=\"color:red\">杨</span>育苗的效应,结果表明:应用稀土保水剂能极大地提高苗木成活率,加速苗木的生长发育,根系数量、株高、地茎等生长量指标均明显高于对照.因此,应用稀土保水剂对育苗的成功率、培育壮苗都有一定的作用.","authors":[{"authorName":"王永刚","id":"38361a45-f110-4aeb-a580-2436cf6c6956","originalAuthorName":"王永刚"},{"authorName":"张宇生","id":"083931f0-09cd-4490-8ade-f310257d5949","originalAuthorName":"张宇生"},{"authorName":"张宏江","id":"22614210-1ed9-46b4-94f5-e83cfbf53d69","originalAuthorName":"张宏江"}],"doi":"10.3969/j.issn.1004-0277.2000.05.011","fpage":"38","id":"f2fb53ae-860a-4080-930b-25c1c781692f","issue":"5","journal":{"abbrevTitle":"XT","coverImgSrc":"journal/img/cover/XT.jpg","id":"65","issnPpub":"1004-0277","publisherId":"XT","title":"稀土"},"keywords":[{"id":"d6121fd6-2f0c-4b38-8415-0809dff7b660","keyword":"稀土保水剂","originalKeyword":"稀土保水剂"},{"id":"dbb6825d-5ea8-42fb-a3b7-faaa66286cd7","keyword":"育苗","originalKeyword":"育苗"},{"id":"5354a5b7-84ad-4b44-90af-4de66e718826","keyword":"成活率","originalKeyword":"成活率"},{"id":"9145b6d2-c58c-44ca-9db8-3924c802ab04","keyword":"生长量","originalKeyword":"生长量"}],"language":"zh","publisherId":"xitu200005011","title":"稀土保水剂在新疆<span style=\"color:red\">杨</span>育苗上的应用研究","volume":"21","year":"2000"},{"abstractinfo":"通过扫描电镜、能谱仪等手段对失效的<span style=\"color:red\">运</span>五飞机灭火瓶管嘴断裂进行断口形貌、化学成分和金相组织分析.结果表明,该灭火瓶管嘴断裂是由于应力腐蚀开裂引起的;根据分析结果,提出了预防措施.","authors":[{"authorName":"王在俊","id":"920b09d5-04e7-49b9-8038-ffcea52e274c","originalAuthorName":"王在俊"},{"authorName":"刘显超","id":"a29b1b8a-f3f6-4777-8583-06c65650d5d0","originalAuthorName":"刘显超"}],"doi":"10.3969/j.issn.1002-6495.2007.05.019","fpage":"377","id":"132c8a6b-4f99-4f15-b6f2-d3782b754b90","issue":"5","journal":{"abbrevTitle":"FSXB","coverImgSrc":"journal/img/cover/腐蚀学报封面.jpg","id":"24","issnPpub":"2667-2669","publisherId":"FSXB","title":"腐蚀学报（英文）"},"keywords":[{"id":"3b153524-741f-4c9c-82a4-4d6274bd6249","keyword":"灭火瓶管嘴","originalKeyword":"灭火瓶管嘴"},{"id":"acd129a9-eda5-4b91-939a-a1201956db2d","keyword":"断裂","originalKeyword":"断裂"},{"id":"546a1e7e-0153-4833-8916-90311c1809db","keyword":"失效分析","originalKeyword":"失效分析"},{"id":"43d93b74-f472-4e8b-a6ee-8abffc8f139d","keyword":"应力腐蚀","originalKeyword":"应力腐蚀"}],"language":"zh","publisherId":"fskxyfhjs200705019","title":"<span style=\"color:red\">运</span>五飞机灭火瓶管嘴断裂的失效分析","volume":"19","year":"2007"},{"abstractinfo":"在野外调研基础上,通过对<span style=\"color:red\">杨</span>金沟金矿床地质特征的研究和包裹体显微测温的分析,讨论了成矿条件和矿床成因.结果表明,该矿床赋存于古生代变质岩系与华力西晚期花岗岩接触带附近,明显受断裂构造控制；金矿石主要有蚀变岩型和石英脉型两种,金矿物以细粒—微细粒的包体金、裂隙金和晶隙金形式赋存于石英、黄铁矿等矿物的内部、晶隙或裂隙中；石英中主要发育气液二相包裹体、C02包裹体和含C02三相包裹体,成矿流体为中温(230 ～ 270℃)、中低盐度(3.37％～15.65％)、低密度(0.78～0.91 g/cm3)的NaCl-H20-C02体系.结合区内铜金矿床对比分析认为,<span style=\"color:red\">杨</span>金沟金矿床形成于板块俯冲后的伸展环境,金矿化与燕山晚期中酸性侵入体具有密切的时空和成因联系.","authors":[{"authorName":"李晨辉","id":"5aea53a0-c9be-4402-aa16-7b76b92ab973","originalAuthorName":"李晨辉"}],"doi":"10.3969/j.issn.1001-1277.2011.12.006","fpage":"22","id":"0c921024-5b83-4ee5-b2b4-93a29adc8a04","issue":"12","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"bf599b86-a5f3-4782-bb4b-6986f6aaf40d","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"c704fbcb-90a4-4649-a013-d2fe792bc4ce","keyword":"流体包裹体","originalKeyword":"流体包裹体"},{"id":"497fe4ae-5730-4e04-ac5f-eb6eeb134b40","keyword":"<span style=\"color:red\">杨</span>金沟金矿床","originalKeyword":"杨金沟金矿床"},{"id":"e917f097-ebf6-46f6-9148-a8da63819178","keyword":"延边东部地区","originalKeyword":"延边东部地区"}],"language":"zh","publisherId":"huangj201112006","title":"延边东部<span style=\"color:red\">杨</span>金沟金矿床地质特征与成矿物理化学条件研究","volume":"32","year":"2011"}],"totalpage":594,"totalrecord":5938}