{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"采用基板生长工艺对各种影响气相生长碳纤维的因素进行分析.结果表明,选择硫化亚铁作为催化剂,氩气为载气,丙烯为碳源,炉内压力4200Pa左右,是气相生长碳纤维的最佳条件,可制备出直径均匀、表面光洁的碳纤维.","authors":[{"authorName":"<span style=\"color:red\">付</span><span style=\"color:red\">铁</span><span style=\"color:red\">岩</span>","id":"6ddcb12e-c82d-43f0-b73a-507188660f26","originalAuthorName":"付铁岩"},{"authorName":"孙晋良","id":"4b09f2d5-105f-468a-ae62-fd2ae1dc20f2","originalAuthorName":"孙晋良"},{"authorName":"任慕苏","id":"9f8964ae-06fb-4e9e-989f-2e83eb392d3c","originalAuthorName":"任慕苏"},{"authorName":"陈来","id":"3b34ad26-e3b1-4355-aa82-ba355dbd09cd","originalAuthorName":"陈来"},{"authorName":"周春节","id":"bef4aa18-b64a-4901-9d03-8d36127d0804","originalAuthorName":"周春节"},{"authorName":"张家宝","id":"1eb5c8dd-d3ff-4206-85da-12e918404a34","originalAuthorName":"张家宝"},{"authorName":"潘剑峰","id":"b07c7343-3e20-4759-9b78-0e8e732ae625","originalAuthorName":"潘剑峰"}],"doi":"10.3969/j.issn.1001-7208.2005.03.001","fpage":"1","id":"8c8b1db2-a499-4998-aad3-0542cf7ce7c2","issue":"3","journal":{"abbrevTitle":"SHJS","coverImgSrc":"journal/img/cover/SHJS.jpg","id":"59","issnPpub":"1001-7208","publisherId":"SHJS","title":"上海金属"},"keywords":[{"id":"de372623-f073-45dd-b61d-df1708bc3c75","keyword":"气相生长碳纤维","originalKeyword":"气相生长碳纤维"},{"id":"168117b9-baec-40db-9127-d3908f34d65e","keyword":"基板生长法","originalKeyword":"基板生长法"},{"id":"6dbe57d9-cac5-4c5d-a4d7-a3f7e1164912","keyword":"影响因素","originalKeyword":"影响因素"}],"language":"zh","publisherId":"shjs200503001","title":"气相生长碳纤维影响因素的研究","volume":"27","year":"2005"},{"abstractinfo":"采用超声均相沉淀法,以硫代乙酰胺和硫酸亚铁铵为原料,通过调整溶液pH值,并借助表面活性剂防止颗粒团聚,在常温下合成了均匀分散的FeS纳米颗粒.X射线衍射和透射电镜(TEM)分析表明颗粒直径为40～50nm.将制备的FeS溶液涂在陶瓷板上进行化学气相沉积,得到了大量直径为5～8μm的气相生长碳纤维.","authors":[{"authorName":"<span style=\"color:red\">付</span><span style=\"color:red\">铁</span><span style=\"color:red\">岩</span>","id":"21958642-0b54-4147-b706-8895822d4f6b","originalAuthorName":"付铁岩"},{"authorName":"孙晋良","id":"f9df599a-e8b6-4f35-8ef9-1c912e161d94","originalAuthorName":"孙晋良"},{"authorName":"陈来","id":"8c088bd6-4230-4179-9de9-26496bc0df36","originalAuthorName":"陈来"},{"authorName":"任慕苏","id":"b6729f1d-e6c9-49cc-853a-a98bb39e7623","originalAuthorName":"任慕苏"}],"doi":"10.3969/j.issn.1673-2812.2005.05.019","fpage":"549","id":"8a07e7a2-f245-45cf-a981-c6d02c0c0b38","issue":"5","journal":{"abbrevTitle":"CLKXYGCXB","coverImgSrc":"journal/img/cover/CLKXYGCXB.jpg","id":"13","issnPpub":"1673-2812","publisherId":"CLKXYGCXB","title":"材料科学与工程学报"},"keywords":[{"id":"9aa30109-5226-4dd7-9cfd-45477909e0e9","keyword":"气相生长碳纤维","originalKeyword":"气相生长碳纤维"},{"id":"2b90f8d2-f05c-4b62-b9e3-25b0680f6262","keyword":"硫化亚铁","originalKeyword":"硫化亚铁"},{"id":"c9db1a8b-82f1-44ee-a0cd-6f0745451642","keyword":"均相沉淀","originalKeyword":"均相沉淀"},{"id":"6c5b0c95-d332-4e2f-9dce-76ef3d06592e","keyword":"超声技术","originalKeyword":"超声技术"}],"language":"zh","publisherId":"clkxygc200505019","title":"纳米催化剂FeS的制备及其在气相生长碳纤维中的应用","volume":"23","year":"2005"},{"abstractinfo":"采用低浓度NaCN、低pH值堆浸工艺条件,处理含铜、呈酸性的<span style=\"color:red\">铁</span>帽型金矿石,可降低NaCN和碱的消耗,同时也有利于炭吸附,可提高炭吸附率和载金炭品位.","authors":[{"authorName":"巫汉泉","id":"574ee559-b829-4747-9e18-277171820fea","originalAuthorName":"巫汉泉"}],"doi":"10.3969/j.issn.1001-1277.2001.09.009","fpage":"32","id":"49d030f5-fed4-4b5a-8661-7211afd98374","issue":"9","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"7d61b8bf-c2f4-4bf1-9dc6-5a20735cb58a","keyword":"NaCN浓度","originalKeyword":"NaCN浓度"},{"id":"b66e8d32-a934-4148-8bfa-46d6656c2ecd","keyword":"pH值","originalKeyword":"pH值"},{"id":"4bdccc19-39e4-49df-9d24-214a72cd42af","keyword":"<span style=\"color:red\">铁</span>帽型金矿石","originalKeyword":"铁帽型金矿石"},{"id":"c3c6e355-3e1b-42a7-8585-9b15a565d3b9","keyword":"堆浸","originalKeyword":"堆浸"}],"language":"zh","publisherId":"huangj200109009","title":"矽卡<span style=\"color:red\">岩</span><span style=\"color:red\">铁</span>帽型金矿石堆浸提金工艺特性","volume":"22","year":"2001"},{"abstractinfo":"以乙二胺四乙酸二钠(EDTA)、柠檬酸、草酸、酒石酸改性制备了H-BEA,并根据XRD和NH3-TPD对沸石H-BEA进行表征.采用上述改性沸石催化4-苯基丁酸分子内<span style=\"color:red\">付</span>克反应合成1-萘满酮进行催化剂反应活性评价.实验结果表明,以柠檬酸改性沸石H-BEA具有较高的催化活性.进一步对催化剂用量、反应温度、反应时间等工艺条件优化得到最佳工艺条件,在最佳工艺条件下,产物1-萘满酮产率达到94.3%.","authors":[{"authorName":"邱俊","id":"70aef54d-1698-4072-ade6-5aece137f1d3","originalAuthorName":"邱俊"},{"authorName":"王建刚","id":"249030d9-483f-4e98-8b62-8ef1f7c30e18","originalAuthorName":"王建刚"},{"authorName":"孙杰","id":"a428191e-8a87-41d9-bed9-7882614d4ee6","originalAuthorName":"孙杰"}],"doi":"10.3724/SP.J.1095.2011.00367","fpage":"194","id":"a36cd46b-50c2-464d-a5a4-bfdd989a48d6","issue":"2","journal":{"abbrevTitle":"YYHX","coverImgSrc":"journal/img/cover/YYHX.jpg","id":"73","issnPpub":"1000-0518","publisherId":"YYHX","title":"应用化学"},"keywords":[{"id":"a72fe36f-275b-48e6-9ebb-7f00a617dc9d","keyword":"苯基丁酸","originalKeyword":"苯基丁酸"},{"id":"a4a44539-8c88-4346-91a4-019d6c951751","keyword":"萘满酮","originalKeyword":"萘满酮"},{"id":"9abf5898-6838-4059-844d-2a2a86e9bb13","keyword":"分子内Friedel-Crafts","originalKeyword":"分子内Friedel-Crafts"},{"id":"8d055735-2308-49a3-9862-cb9f5c7a9841","keyword":"沸石H-BEA","originalKeyword":"沸石H-BEA"}],"language":"zh","publisherId":"yyhx201102013","title":"改性沸石H-BEA催化4-苯基丁酸分子内<span style=\"color:red\">付</span>克反应合成1-萘满酮","volume":"28","year":"2011"},{"abstractinfo":"<span style=\"color:red\">岩</span>爆是一种世界性的地质灾害,极大地威胁着矿山施工人员和设备的安全.目前,国内外在<span style=\"color:red\">岩</span>爆方面做了大量的研究工作,但是,由于<span style=\"color:red\">岩</span>爆问题极为复杂,还没有成熟的理论和方法.针对<span style=\"color:red\">岩</span>爆定义、<span style=\"color:red\">岩</span>爆发生机理、<span style=\"color:red\">岩</span>爆预测预报、<span style=\"color:red\">岩</span>爆控制的研究现状,进行了归纳分析与评述,并在某些方面提出了新的见解.","authors":[{"authorName":"刘卫东","id":"794ba667-c65f-4c14-b674-50fade3015cf","originalAuthorName":"刘卫东"},{"authorName":"李角群","id":"8bcda317-9c89-476f-8470-3587db468039","originalAuthorName":"李角群"},{"authorName":"李磊","id":"1b0c079f-b622-4e5b-97a0-d99194ea9bbc","originalAuthorName":"李磊"}],"doi":"10.3969/j.issn.1001-1277.2010.01.007","fpage":"26","id":"78c9471a-2a55-422d-92bd-0ac6fa7b4868","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"4c195465-ed84-4338-8160-9b3d95ce6d76","keyword":"<span style=\"color:red\">岩</span>爆","originalKeyword":"岩爆"},{"id":"671204bc-3f7f-49c4-8181-b104fd4732c3","keyword":"<span style=\"color:red\">岩</span>爆发生机理","originalKeyword":"岩爆发生机理"},{"id":"ce1fcc6b-a971-4208-a83b-9eba548f108c","keyword":"<span style=\"color:red\">岩</span>爆预测预报","originalKeyword":"岩爆预测预报"},{"id":"3dfac183-ad8c-41fd-b37a-42ca3a8f6ac9","keyword":"<span style=\"color:red\">岩</span>爆控制","originalKeyword":"岩爆控制"}],"language":"zh","publisherId":"huangj201001007","title":"<span style=\"color:red\">岩</span>爆研究现状综述","volume":"31","year":"2010"},{"abstractinfo":"郭家埠地区位于招平断裂中段，该地区围岩蚀变发育，蚀变分带明显。选取切穿该区蚀变带的1012剖面，分析其围岩蚀变特征，自断裂中心向两侧蚀变<span style=\"color:red\">岩</span>依次为：黄<span style=\"color:red\">铁</span>绢英<span style=\"color:red\">岩</span>、绢英<span style=\"color:red\">岩</span>和钾化花岗岩，蚀变强度依次减弱。蚀变<span style=\"color:red\">岩</span>地球化学分析显示：随着蚀变的增强， Si、K、Fe增加， Na减少，说明蚀变是一种硅化、钾化、而去Na的过程；稀土元素总量整体呈降低的趋势。钾化花岗岩轻重稀土元素分异程度较强，轻稀土相对富集，而绢英<span style=\"color:red\">岩</span>重稀土富集；Rb、Ba含量总体随着矿化强度的增强而增加，高场强元素含量在钾化蚀变阶段和黄<span style=\"color:red\">铁</span>绢英<span style=\"color:red\">岩</span>化阶段减少，在绢英<span style=\"color:red\">岩</span>化阶段增加。通过探讨蚀变<span style=\"color:red\">岩</span>与找矿的关系，认为黄铁矿化、绢云母化、钾长石化等蚀变是找矿的直接标志。郭家埠地区蚀变<span style=\"color:red\">岩</span>带规模大，蚀变强，钻孔资料表明深部蚀变<span style=\"color:red\">岩</span>Au含量已达边界品位，加之周边地区成矿条件较好，初步推测郭家埠地区成矿前景良好。","authors":[{"authorName":"王玺","id":"f13be2d9-186a-4e51-9faa-5bdfaab06829","originalAuthorName":"王玺"},{"authorName":"胡宝群","id":"c331c4b7-25cf-44eb-8976-6ed26ef4ac19","originalAuthorName":"胡宝群"},{"authorName":"张志航","id":"fa25c980-39d9-4e60-8b9c-b678452b8022","originalAuthorName":"张志航"},{"authorName":"王志强","id":"19d38f08-66d5-40e8-95a0-09927b137f85","originalAuthorName":"王志强"},{"authorName":"顾延景","id":"81daa1b1-12d9-4927-afef-ca381852978f","originalAuthorName":"顾延景"},{"authorName":"申玉科","id":"f425c023-7421-4125-9f9e-77ed1c0c529f","originalAuthorName":"申玉科"},{"authorName":"郭涛","id":"85163ded-3a81-4095-951c-5629a8e88bb3","originalAuthorName":"郭涛"},{"authorName":"吕古贤","id":"3ab1be77-a2d7-4060-95a0-bbedf7d6aeed","originalAuthorName":"吕古贤"}],"doi":"10.11792/hj20141104","fpage":"14","id":"f5e83ab5-d009-4999-8ace-3c068657a3e0","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"c1a1169a-4b51-40d9-9957-2ad254c05758","keyword":"郭家埠地区","originalKeyword":"郭家埠地区"},{"id":"cb274d57-aba9-4441-aec2-d5ab85d9e5a1","keyword":"招平断裂","originalKeyword":"招平断裂"},{"id":"2f926037-55ed-4a2b-a9ac-77a49110e4a0","keyword":"蚀变<span style=\"color:red\">岩</span>带","originalKeyword":"蚀变岩带"},{"id":"7693266c-2f93-4de9-99fb-87942c75ef01","keyword":"地球化学","originalKeyword":"地球化学"},{"id":"78e94c23-bb7b-4ce0-9291-bf3610e78c88","keyword":"找矿意义","originalKeyword":"找矿意义"}],"language":"zh","publisherId":"huangj201411004","title":"招平断裂郭家埠地区蚀变<span style=\"color:red\">岩</span>特征及找矿意义","volume":"","year":"2014"},{"abstractinfo":"为了解释山西石英<span style=\"color:red\">岩</span>并非所谓的胶结硅石,采用场发射扫描电镜-能谱仪和XRD研究了原矿石的石英晶体大小、分布和杂质特征以及煅烧后的显微结构.结果表明,山西石英<span style=\"color:red\">岩</span>系显晶和微晶石英构成的复合型石英<span style=\"color:red\">岩</span>,白色区域为自形石英晶体;红色区域含有纳米尺度的石英晶体、伴生矿物球状和针状<span style=\"color:red\">铁</span>、锰氧化物.经1 450℃保温3h煅烧后的试样约有30％转化为方石英和产生液相分离现象.","authors":[{"authorName":"高振昕","id":"1294aae2-dea0-412e-8543-64c73b25dd27","originalAuthorName":"高振昕"},{"authorName":"张巍","id":"172dfe48-fdc0-4bbd-8b29-ecc81a60fcad","originalAuthorName":"张巍"},{"authorName":"郑小平","id":"d11741bb-41a8-45eb-9248-a2c7031f89f4","originalAuthorName":"郑小平"},{"authorName":"李君霞","id":"e52a950b-d759-4385-8027-964b83e4bf2b","originalAuthorName":"李君霞"},{"authorName":"傅秋华","id":"2fe0a536-437b-4308-ad31-714247754e8d","originalAuthorName":"傅秋华"}],"doi":"10.3969/j.issn.1001-1935.2016.04.020","fpage":"315","id":"f1fcd7ae-bbdd-48fd-930d-2f8c25d803da","issue":"4","journal":{"abbrevTitle":"NHCL","coverImgSrc":"journal/img/cover/NHCL.jpg","id":"55","issnPpub":"1001-1935","publisherId":"NHCL","title":"耐火材料   "},"keywords":[{"id":"1fec2e05-0910-4aae-89f9-5063c7499f30","keyword":"微晶石英","originalKeyword":"微晶石英"},{"id":"7bc9b179-a994-4475-8796-d77336bdbbac","keyword":"石英自形晶","originalKeyword":"石英自形晶"},{"id":"f4edf320-a251-499b-8de4-88bcf26d55d9","keyword":"复合型石英<span style=\"color:red\">岩</span>","originalKeyword":"复合型石英岩"},{"id":"acf71a71-d5a3-4fa0-ad13-ce6396b910c0","keyword":"相变","originalKeyword":"相变"},{"id":"2d182227-22b6-4bba-81c9-23a80217aac7","keyword":"液相分离","originalKeyword":"液相分离"}],"language":"zh","publisherId":"nhcl201604020","title":"山西石英<span style=\"color:red\">岩</span>的结晶特征与加热相变","volume":"50","year":"2016"},{"abstractinfo":"中国深井<span style=\"color:red\">岩</span>爆课题研究已经有近30年的历史,但一般都停留在理论性研究方面,解决<span style=\"color:red\">岩</span>爆防治的实用性研究工作却没有太多成果.针对<span style=\"color:red\">岩</span>爆类型划分、形成机理、发生判据、<span style=\"color:red\">岩</span>爆预测与防治的研究现状,进行了归纳分析和评述.","authors":[{"authorName":"郭树林","id":"ba9d6e81-9ca4-43dd-932f-30c0ea7a39d5","originalAuthorName":"郭树林"},{"authorName":"姚香","id":"d7bb5964-1475-4972-9f58-7c63d288a12f","originalAuthorName":"姚香"},{"authorName":"严鹏","id":"248d6530-7986-4e7f-a6b9-cddb7caa16ce","originalAuthorName":"严鹏"},{"authorName":"许卫军","id":"da7521b5-9292-45a9-908b-fc1a8b8d0708","originalAuthorName":"许卫军"},{"authorName":"李晓明","id":"c3a5a75d-b1d0-46a4-b096-00a7ab66d5a1","originalAuthorName":"李晓明"}],"doi":"10.3969/j.issn.1001-1277.2009.01.006","fpage":"18","id":"d9f96b61-377f-4835-80a6-1fabbbefa351","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"52cc1191-a273-4c1e-b380-257a43021987","keyword":"深井<span style=\"color:red\">岩</span>爆","originalKeyword":"深井岩爆"},{"id":"0877954d-415f-4604-947a-bffbbfe9291d","keyword":"<span style=\"color:red\">岩</span>爆类型","originalKeyword":"岩爆类型"},{"id":"874390c5-195d-492c-b648-b7f073dd4159","keyword":"<span style=\"color:red\">岩</span>爆判据","originalKeyword":"岩爆判据"},{"id":"41c5f135-0051-465a-9344-f9f4130af1ca","keyword":"<span style=\"color:red\">岩</span>爆预测与防治","originalKeyword":"岩爆预测与防治"}],"language":"zh","publisherId":"huangj200901006","title":"中国深井<span style=\"color:red\">岩</span>爆研究现状评述","volume":"30","year":"2009"},{"abstractinfo":"以乌江流域石灰<span style=\"color:red\">岩</span>、白云质灰<span style=\"color:red\">岩</span>、白云<span style=\"color:red\">岩</span>、硅质<span style=\"color:red\">岩</span>、页岩和砂岩等沉积<span style=\"color:red\">岩</span>的13条风化剖面为对象,运用R型分层聚类分析和质量平衡计算方法,研究了这些岩石风化过程中稀土元素(REE)的富集与释放及其对植物生长和河水REE分布的影响,目的是为河水物质来源研究和为农业生产提供依据. 结果表明: (1) 乌江流域石灰土中REE的富集程度显著高于各自母<span style=\"color:red\">岩</span>、黄壤、上陆壳(UCC)、中国土壤(CS)和世界土壤(WS);(2) 沉积<span style=\"color:red\">岩</span>风化过程中REE的富集特征和机制可能与母<span style=\"color:red\">岩</span>中REE分布特征以及风化剖面中有机质、<span style=\"color:red\">铁</span>(氢)氧化物和粘土矿物的吸附有关;(3) 沉积<span style=\"color:red\">岩</span>风化过程中释放的REE可为植物吸收利用;(4) 石灰<span style=\"color:red\">岩</span>等沉积<span style=\"color:red\">岩</span>风化过程中REE和Fe等元素的释放对河水溶解态REE的分布有重要影响.","authors":[{"authorName":"宋照亮","id":"0968332d-805b-4cf3-ade1-0b1e618673d0","originalAuthorName":"宋照亮"},{"authorName":"刘丛强","id":"b8cb46dc-710a-4ddc-b35a-4fab20c53f5c","originalAuthorName":"刘丛强"},{"authorName":"韩贵琳","id":"6e7c20d1-583a-46d5-aab7-a2a27fc7872b","originalAuthorName":"韩贵琳"},{"authorName":"王中良","id":"332f3deb-9de1-44b2-93ea-a033dbb86a6b","originalAuthorName":"王中良"},{"authorName":"朱兆洲","id":"ba860b4f-c087-48db-8c5c-368436706b8b","originalAuthorName":"朱兆洲"},{"authorName":"杨成","id":"cb81a7e4-2a51-4310-a68a-80cc6363cb27","originalAuthorName":"杨成"}],"doi":"","fpage":"344","id":"ebe622da-7242-4595-b121-f9398c24880f","issue":"3","journal":{"abbrevTitle":"ZGXTXB","coverImgSrc":"journal/img/cover/ZGXTXB.jpg","id":"86","issnPpub":"1000-4343","publisherId":"ZGXTXB","title":"中国稀土学报"},"keywords":[{"id":"69521583-ba64-43ab-8fbc-f47da8111ffe","keyword":"富集","originalKeyword":"富集"},{"id":"10ad99aa-1cf4-449d-9ab6-25a6a8412b12","keyword":"释放","originalKeyword":"释放"},{"id":"d3d113ea-66ff-4dfd-9377-a56240745feb","keyword":"风化","originalKeyword":"风化"},{"id":"17c389f9-a249-431d-a2e7-3c38aeb122a5","keyword":"沉积<span style=\"color:red\">岩</span>","originalKeyword":"沉积岩"},{"id":"467ae3e5-afc3-47d6-8a1c-d0db45383c57","keyword":"稀土","originalKeyword":"稀土"}],"language":"zh","publisherId":"zgxtxb200603017","title":"乌江流域沉积<span style=\"color:red\">岩</span>风化过程中稀土元素的富集与释放","volume":"24","year":"2006"},{"abstractinfo":"为了改善软<span style=\"color:red\">岩</span>遇水软化的特性,采用化学改性、水泥改性以及复合改性的处理方法从微观上改变软<span style=\"color:red\">岩</span>的结构,通过静态水润湿角实验、膨胀率实验、崩解性实验和直接剪切实验得到了改性前后软<span style=\"color:red\">岩</span>物理力学性质变化规律,并从微观上分析改性机理.结果表明:复合改性相对单一改性能够更好的改善软<span style=\"color:red\">岩</span>遇水软化的特性;复合改性后软<span style=\"color:red\">岩</span>的润湿角由3.58°提高到109.48°,使软<span style=\"color:red\">岩</span>由亲水性转变为憎水性;膨胀率由改性前的16.61％降为2.42％;软<span style=\"color:red\">岩</span>由强崩解性转变为弱崩解性;复合改性后软<span style=\"color:red\">岩</span>的抗剪强度变化明显,粘聚力由117.2 kPa增加到363.8 kPa,内摩擦角由24.4°提高到44.3°,分别提高了210.4％、81.6％;复合改性从微观上改变了软<span style=\"color:red\">岩</span>的结构,提高了颗粒间的胶结作用力,并在颗粒表面形成一层憎水膜.","authors":[{"authorName":"王来贵","id":"5b9062c9-b331-4323-af56-9458958c7c73","originalAuthorName":"王来贵"},{"authorName":"张鹏","id":"3af14208-04b0-4a00-bfeb-e5d1beb5555f","originalAuthorName":"张鹏"},{"authorName":"杨建林","id":"0c7c2805-9397-432c-86ae-bb099d560240","originalAuthorName":"杨建林"},{"authorName":"李喜林","id":"072dd77b-f3f8-4ba0-bd54-99f853d07c36","originalAuthorName":"李喜林"}],"doi":"","fpage":"99","id":"d3d8875a-466b-4070-9b71-75e02f526d0e","issue":"1","journal":{"abbrevTitle":"GSYTB","coverImgSrc":"journal/img/cover/GSYTB.jpg","id":"36","issnPpub":"1001-1625","publisherId":"GSYTB","title":"硅酸盐通报   "},"keywords":[{"id":"68bfba8c-8b4e-4afe-b8cd-b4543371c320","keyword":"软<span style=\"color:red\">岩</span>","originalKeyword":"软岩"},{"id":"2a64a3f5-b3ed-4937-9349-21265dfac89e","keyword":"复合改性","originalKeyword":"复合改性"},{"id":"4292b1f8-70f9-4161-9791-021954e860a1","keyword":"润湿角","originalKeyword":"润湿角"},{"id":"31343226-103a-461e-a44b-82ad444f9280","keyword":"崩解性","originalKeyword":"崩解性"},{"id":"cda06295-ff5e-4e45-abc5-003884a1e8ce","keyword":"抗剪强度","originalKeyword":"抗剪强度"}],"language":"zh","publisherId":"gsytb201501018","title":"软<span style=\"color:red\">岩</span>改性及其微观机理研究","volume":"34","year":"2015"}],"totalpage":1173,"totalrecord":11725}