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| 1 | Measurements of dihadron correlations relative to the event plane in Au+Au collisions at√^(S)NN=200 GeV显示文摘Dihadron azimuthal correlations containing a high transverse momentum(pr)trigger particle are sensit-ive to the properties of the nuclear medium created at RHIC through the strong interactions occurring between the traversing parton and the medium,ie.jet-quenching.Previous measurements revealed a strong modification to di-hadron azimuthal correlations in Au+Au collisions with respect to ptp and d+Au collisions.The modification in-creases with the collision centrality,suggesting a path-length or energy density dependence to the je-quenching ef-fect.This paper reports STAR measurements of dihadron azimuthal correlations in mid-central(20%-60%)Au+Au collisions at√^(S)NN=200 GeV as a function of the trigger particle's azimuthal angle relative to the event plane,Ф_(s)=|Ф_(t)-ψ_(Ep)|.The azimuthal correlation is studied as a function of both the trigger and associated particle pr.The subtractions of the combinatorial background and anisotropic flow,assuming Zero Yield At Minimum(ZYAM),are described.The correlation results are first discussed with subtraction of the even harmonic(elliptic and quadrangu-lar)flow backgrounds.The away-side correlation is strongly modifed,and the modification varies withФ_(s),with a double-peak structure for out-of-plane trigger particles.The near-side ridge(long range pseudo-rapidity△_(η)correla-tion)appears to drop with increasingФ_(s)while the jet-like component remains approximately constant.The correla-tion functions are further studied with the subtraction of odd harmonic triangular flow background arising from fluc-tuations.It is found that the triangular flow,while responsible for the majority of the amplitudes,is not sufficient to explain theφs-dependence of the ridge or the away-side double-peak structure.The dropping ridge withФ_(s)could be attributed to aФ_(s)-dependent lliptie anisotropy;however,the physics mechanism of the ridge remains an open ques-tion.Even with aФ_(s)-dependent elliptic flow,the away-side correlation structure is robust.These results,with extens-ive systematic studies of the dihadron correlations as a function ofФ_(s),trigger and associated particle pT,and the pseudo-rapidity range△_(η),should provide stringent inputs to help understand the underlying physics mechanisms of jet-medium interactions in high energy nuclear collisions. | H.Agakishiev M.M.Aggarwal Z.Ahammed A.V.Alakhverdyants I.Alekseev J.Alford B.D.Anderson C.D.Anson D.Arkhipkin G.S.Averichev J.Balewski D.R.Beavis N.K.Behera R.Bellwied M.J.Betancourt R.R.Betts A.Bhasin A.K.Bhat H.Bichsel J.Bieleik J.Bielcikova B.Biritz L.C.Bland W.Borowski J.Bouchet E.Braidot A.V.Brandin A.Bridgeman S.G.Brovko E.Bruna S.Bueltmann I.Bunzarov T.P.Burton X.Z.Cai H.Caines M.Calderon de la Barca Sanchez D.Cebra R.Cendejas M.C.Cervantes Z.Chajecki P.Chaloupka S.Chattopadhyay H.F.Chen J.H.Chen J.Y.Chen L.Chen J.Cheng M.Cherney A.Chikanian K.E.Choi W.Christie P.Chung M.J.M.Codrington R.Corliss J.G.Cramer H.J.Crawford S.Dash A.Davila Leyva L.C.De Silvat R.R.Debbe T.G.Dedovich A.A.Derevschikov R.Derradi de Souza L.Didenko P.Djawotho S.M.Dogra X.Dong J.L.Drachenberg J.E.Draper J.C.Dunlop L.G Efimov M.Elnim J.Engelage G Eppley M.Estienne L.Eun O.Evdokimov R.Fatemi J.Fedorisin A.Feng R.G.Fersch P.Filip E.Finch V.Fine Y.Fisyak C.A.Gagliardi D.R.Gangadharan A.Geromitsos F.Geurts P.Ghosh Y.N.Gorbunov A.Gordon O.Grebenyuk D.Grosnick S.M.Guertin A.Gupta W.Guryn B.Haag O.Hajkova A.Hamed L-X.Han J.W.Harris J.P.Hays-Wehle M.Heinz S.Heppelmann A.Hirsch E.Hjort G.W.Hoffmann D.J.Hofiman B.Huang H.Z.Huang T.J.Humanic L.Huo G.Igo P.Jacobs W.W.Jacobs C.Jena F.Jin J.Joseph E.G.Judd S.Kabana K.Kang J.Kapitan K.Kauder H.Ke D.Keane A.Kechechyan D.Kettler D.P.Kikola J.Kiryluk A.Kisiel V.Kizka A.G.Knospe D.D.Koetke T.Kollegger J.Konzer I.Koralt L.Koroleva W.Korsch L.Kotchenda V.Kouchpil P.Kravtsov K.Krueger M.Krus L.Kumar P.Kurnadi M.A.C.Lamont J.M.Landgraf S.LaPointe J.Lauret A.Lebedev R.Lednicky J.H.Lee W.Leight M.J.LeVine C.Lil L.Li N.Li W.Li X.Li X.Li Y.Li Z.M.Li M.A.Lisa F.Liu H.Liu J.Liu T.Ljubicic W.J.Llope R.S.Longacre W.A.Love Y.Lu E.V.Lukashov X.Luo G.L.Ma Y.G.Mai D.P.Mahapatra R.Majka O.I.Mall L.K.Mangotra R.Manweiler S.Margetis C.Markert H.Masui H.S.Matis Yu.A.Matulenko D.MeDonald T.S.McShane A.Meschanin R.Milner N.G.Minaev S.Mioduszewski A.Mischke M.K.Mitrovski B.Mohanty M.M.Mondal B.Morozov D.A.Morozov M.G.Munhoz M.Naglis B.K.Nandi T.K.Nayak P.K.Netrakanti L.V.Nogach S.B.Nurushev G.Odyniec A.Ogawa Oh Ohlson V.Okorokov E.W.Oldag D.Olsont M.Pachr B.S.Page S.K.Pal Y.Pandit Y.Panebratsev T.Pawlak H.Pei T.Peitzmann C.Perkins W.Peryt S.C.Phatak P.Pile M.Planinic M.A.Ploskon J.Pluta D.Plyku N.Poljak A.M.Poskanzer B.V.K.S.Potukuchi C.B.Powell D.Prindle N.K.Pruthi A.M.Poskanzer B.V.K.S.Potukuchi B.Powell D.Prindle N.K.Pruthi P.R.Pujahar J.Putschke H.Qiu R.Raniwala S.Raniwala R.L.Ray R.Redwine R.Reed H.G.Riter J.B.Roberts O.V.Rogachevskiy J.L.Romero A.Rose L.Ruan J.Rusnak N.R.Sahoo S.Sakai I.Sakrejda T.Sakuma S.Salur J.Sandweiss E.Sangaline A.Sarkar J.Schambach R.P.Scharenberg A.M.Schmah N.Schmitz T.R.Schuster J.Seele J.Seger I.Selyuzhenkov P.Seyboth E.Shahaliev M.Shao M.Sharma S.S.Shi Q.Y.Shou E.P.Sichtermann F.Simon R.N.Singaraju M.J.Skoby N.Smirnov H.M.Spinka B.Srivastava T.D.S.Stanislaus D.Staszak S.G.Steadman J.R.Stevens R.Stock M.Strikhanov B.Stringfellow A.A.P.Suaide M.C.Suarez N.L.Subba M.Sumbera X.M.Sun Y.Sun Z.Sun B.Surrow D.N.Svirida T.J.M.Symons A.Szanto de Toledo J.Takahashi A.H.Tang Z.Tang L.H.Tarini T.Tarnowsky D.Thein J.H.Thomas J.Tian A.R.Timmins D.Tlusty M.Tokarev V.N.Tram S.Trentalange R.E.Tribble Tribedy O.D.Tsai T.Ullrich D.G.Underwood G.Van Buren G.van Nieuwenhuizen J.A.Vanfossen R.Varma G.M.S.Vasconcelos A.N.Vasiliev F.Videbaek Y.P.Viyogi S.Vokal M.Wadat M.Walker F.Wang G.Wang H.Wang J.S.Wang Q.Wang X.L.Wang Y.Wang G.Webb J.C.Webb G.D.Westfall C.Whitten H.Wieman S.W.Wissink R.Witt W.Witzke Y.F.Wu Xiao W.Xie H.Xu N.Xu Q.H.Xu W.Xu Y.Xu Z.Xu L.Xue Y.Yang P.Yepes K.Yip I-K.Yoo M.Zawisza H.Zbroszczyk W.Zhan J.B.Zhang S.Zhang W.M.Zhang X.P.Zhang Y.Zhang Z.P.Zhang J.Zhao C.Zhong W.Zhou X.Zhu Y.H.Zhu R.Zoulkarneev Y.Zoulkarneeva | 2021 | Chinese Physics C2021，45，4： | 351 |
| 2 | New aspects in the oxidative stabilization of PAN-basedcarbonfibers显示文摘 | A.Gupta IR.Harrison | | 0，，11： | 1 |
| 3 | Packet caches on routers:the implications of universal redundant traffic elimination显示文摘 | A.Anand A.Gupta A.Akella S.Seshan S.Shenker | | 0，，04： | 1 |
| 4 | 查看详情显示文摘 | N.Bao L.Shen G.Srinivasan K.Yanagisawa and A.Gupta | | 0，，23： | 1 |
| 5 | 查看详情显示文摘 | D.Mazumdar V.Shelke M.Iliev S.Jesse A.Kumar S.V.Kalinin A.P.Baddorf and A.Gupta | | 0，，07： | 1 |
| 6 | Content-Based Image Retrieval at the End of the Early Years显示文摘 | A.W.M.Smeulders M.Worring S.Santini A.Gupta R.Jain | | 0，，12： | 1 |
| 7 | 印度库茂恩喜马拉雅纳尼塔尔温带地区晚全新世古植被和古气候(英文)显示文摘根据从印度库茂恩(Kumaun)喜马拉雅纳尼塔尔(Naini Tal)温带地区获得的85 cm钻井的孢粉资料,恢复了1720+/-130年以来晚全新世古植被演变史,并推测了当地的古气候。当前孢粉资料说明了该地区当时发育有栎树混交林和波动的温暖湿润气候。孢粉组合序列的初始阶段,森林距沉积盆地较远。但是,由于气候变得更加温暖潮湿,森林也很快茂密起来。约1200年前,因气候恶化,森林变得稀疏。而在约124年前,气候再次转好。麦类及其他作物花粉资料证明农耕活动大约开始于1460年前左右。 | A.Gupta | 2002 | 古生物学报2002，41，4： | 1 |
| 8 | Adiponectin activation of AMPK disrupts leptin‐mediated hepatic fibrosis via suppressors of cytokine signaling (SOCS‐3)显示文摘 | Jeffrey A.Handy Neeraj K.Saxena PingpingFu SongbaiLin Jamie E.Mells Nitika A.Gupta Frank A.Anania | 2010 | J Cell Biochem2010，，5： | 1 |
| 9 | 利用可复用的知识创建灵活的商业系统显示文摘在21世纪的商务中,要想获得全面的卓越和客户价值,灵活与创新是必不可少的。但是现有的绝大多数对商业过程的研究为了运行效率及经济利益而牺性了创新。自动化及封装商业过程的IT系统是不灵活的,不能对不断变化的商业环境作出反应。 | A.Mitra A.Gupta 胡光华 | 2008 | 国外科技新书评介2008，，4： | 0 |
| 10 | 一款抗敏产品对缓解牙本质敏感的作用显示文摘在双盲、平行设计的三个组的随机对照临床试验(RCT)中,对一款抗敏产品在一次刷牙后的即刻抗敏效果,和在连续使用一周、四周和八周后的抗敏效果进行评价。招募有至少两颗敏感牙的受试者进行研究(筛选时要求Schiff指数达到2或者3),敏感牙源自:牙颈部酸蚀、磨损或是牙龈退缩所导致的牙根暴露。 | 孙佳凝 陶丹英 杨雯洁 S.Srinivasan A.Gupta 张琼 S.Bisignano M.Mantzourani | 2019 | 口腔护理用品工业2019，29，5： | 0 |
| 11 | 筛选钻进液配伍性的新方法显示文摘本文介绍了一种用岩屑筛来选择现场可用钻井液的新方法。该方法可帮助作业人员和泥浆公司选择和设计钻井液并鉴定所用钻井液的适配性。把保存完好的页岩样品浸入盐度变化的盐水(NaCl、KCl、CaCl2)以及典型油基泥浆中。通过热解重量分析法(TGA)试验表征岩石的结构和成分的变化。本文发表了浸泡试验的结果,说明了不同阳离子对不同页岩样品的影响。它表明不仅自由水,而且层间水、束缚水和结晶水以及方解石含量都可能随盐水溶液中的阳离子而改变。除TGA试验之处,还用提供评定物质削弱指数的透度计(penetrometer)测量了对比页岩层的强度。研究指出:即使改变页岩中的水含量分布,不同离子对岩石强度的影响也极小。本文描述了使用所推荐的方法的不同情况,从而设计钻井液,并连续检验钻井液与钻井地层的适配性。 | A.Gupta 廉抗利 | 2002 | 国外石油动态2002，，19： | 0 |
| 12 | Development of GIS-based environmental information system: an Indian scenario显示文摘Ideally,scientists should be able to format,explore,analyse,and visualise data in a simple,powerful and fast application that would seamlessly integrate georeferenced data from a variety of data sources into an intuitive visualisation.The focus of an Environmental Information System is providing environmental information to decision makers,policy planners,scientists and engineers,research workers,etc.which ensures integration of data collection,collation,storage,retrieval and dissemination to all concerned.All such queries should be responded to supplying substantive information in the form of reports.The paper presents an innovative way to utilise the geographic information associated with the environmental data.The stand-alone application is the integration of using ArcObjects Environmental System Research Institute ArcGIS Engine 9.1 and VB.Net.The geographic information system(GIS)-based application,a framework of digital earth in terms of environmental information system provides a user-friendly query interface,which gives information about various environmental parameters in tabular as well as on map display.It also provides the visual interpretation to make further analysis and future decisions at multiple scales,locations and extents.The facility for modifying the map attributes and corresponding databases is integrated to update the information system.Output spatial data are produced in the form of reports using selected fields with display on map. | R.Vijay D.R.Satapathy B.Nimje S.Nema S.Dhurve A.Gupta | 2009 | International Journal of Digital Earth2009，2，4： | 0 |
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