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| 1 | Model on L-to H-Mode Transition Driven with Lower-Hybrid Wave显示文摘In this letter,a model for active suppressing tokamak edge turbulence and hence inducing the L-mode to H-mode transition with lower-hybrid wave(LHW)is proposed.The model includes the two contents:(a)The poloidal sheared flow of plasma is generated by the ponderomotive potential and induced magnetization acting on a tokamak plasma resulting from the oscillating electric field of the injected LHW.(b)During the time the LHW is injected into tokamak edge,the edge turbulence and the LHW-generated plasma poloidal flow compete with each other;if the shear of plasma poloidal flow is large enough to suppress the edge turbulence,the confinement will be remarkably improved and hence the system will enter the H operating mode.This model leads us to find that the threshold LHW power required for edge-turbulence suppression is proportional to A(ω)≡(ω/ωLH)^(2)|(ω/ωLH)^(2)-1|,which enables us to explain the experiment in the JT-60 tokamak with lower-hybrid current drive. | QIU Xiaoming(X.M.Qiu) BAI Lin(L.Bai) | 1994 | Chinese Physics Letters1994，11，11： | 3 |
| 2 | TiO显示文摘 | Y.‐G.Guo J.‐S.Hu H.‐P.Liang C.‐L.Bai | 2005 | Adv Funct Mater2005，，2： | 1 |
| 3 | Model on Inducing H-Mode by Biased Electrode in Tokamaks显示文摘In this letter,a model on inducing H-mode by biased electrode in tokamaks is put forward,it successfully explains the experiments in CCT,TEXTOR,and HL-1 with bias. | X.M.Qiu L.Bai L.B.Ran | 1992 | Chinese Physics Letters1992，9，10： | 0 |
| 4 | 主喜马拉雅逆冲断裂的横向变化控制2015年尼泊尔廓尔喀地震的破裂长度显示文摘喜马拉雅造山带大地震活动频繁,影响着长达2500km的人口密集地带。2015年尼泊尔廓尔喀地震(MW7.8)发生在主喜马拉雅逆冲断裂(MHT)上,为陆陆碰撞带断裂活动特征的研究提供了最直接的观测资料。我们使用覆盖整个余震区的近震台站地震波形数据对MHT进行研究。结果表明,MHT沿构造走向呈现清晰的横向变化,在主震区存在低喜马拉雅断坡,而在余震区东部变得更深且倾角更加平缓。余震区以东MHT界面上的地震波速表现为高速异常,可能与印度板块基底隆起的俯冲结构有关,余震区以西同样存在地震波速异常。MHT的总体形态结构变化控制了廓尔喀地震的破裂长度。 | L.Bai S.L.Klemperer J.Mori M.S.Karplus L.Ding H.B.Liu G.H.Li B.W.Song S.Dhakal 江勇(译) 李国辉(译) 白玲(校) | 2020 | 世界地震译丛2020，51，1： | 0 |
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