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Gyrokinetic simulation of low-n Alfvénic modes in tokamak HL-2A plasmas
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作者 林文浩 李继全 +1 位作者 J Garcia S Mazzi 《Chinese Physics B》 SCIE EI CAS CSCD 2023年第2期358-365,共8页
The turbulence characteristics of plasmas with internal transport barriers in the HL-2A tokamak are analyzed by means of linear gyrokinetic simulations. It is found that turbulence is dominated by the ion temperature ... The turbulence characteristics of plasmas with internal transport barriers in the HL-2A tokamak are analyzed by means of linear gyrokinetic simulations. It is found that turbulence is dominated by the ion temperature gradient(ITG)mode together with large-scale modes characterized by high-frequency electromagnetic fluctuation, which are destabilized by the steep ion temperature gradient in the weak magnetic shear regime. Comparison with solutions of analytical dispersion relations shows that their linear features match well with the beta-induced Alfvén eigenmode branch of the shear Alfvénic spectrum. It is further clarified that the large population of fast ions in these plasmas plays a stabilization role through the dilution mechanism in high-n ITG mode regimes. 展开更多
关键词 low-n alfvénic modes fast ions gyrokinetic simulation TOKAMAK
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基于行星际磁场阿尔芬特性的星载磁通门磁强计在轨标定新方法 被引量:4
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作者 孟立飞 王国强 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2023年第5期1847-1855,共9页
准确的磁场测量对深入研究空间等离子体环境具有重要意义.星载磁通门磁强计的磁补偿随时间缓慢变化,因此,需要对其进行常规的在轨标定.现有的在轨标定方法都依赖于磁扰动或磁结构事件的筛选,导致标定结果的频次受限于事件的筛选,且差的... 准确的磁场测量对深入研究空间等离子体环境具有重要意义.星载磁通门磁强计的磁补偿随时间缓慢变化,因此,需要对其进行常规的在轨标定.现有的在轨标定方法都依赖于磁扰动或磁结构事件的筛选,导致标定结果的频次受限于事件的筛选,且差的事件还会增大计算误差.为此,本文研发出一种不依赖于磁场事件筛选的在轨标定新方法.根据行星际磁场强度的取值范围,我们可建构一个磁补偿取值空间.不同的磁补偿值会影响行星际磁场的阿尔芬特性;于是,我们通过在磁补偿空间中找到使被调整之后的行星际磁场的阿尔芬特性最强的点作为磁补偿值的最优解.测试结果表明,我们的新方法可以利用1~4 h时长的行星际磁场数据获得误差小于0.1 nT的标定结果. 展开更多
关键词 磁通门磁强计 磁补偿 在轨标定 行星际磁场 阿尔芬特性
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Automatic calculation of the magnetometer zero offset using the interplanetary magnetic field based on the Wang-Pan method 被引量:5
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作者 XiaoWen Hu GuoQiang Wang ZongHao Pan 《Earth and Planetary Physics》 CSCD 2022年第1期52-60,共9页
The space-borne fluxgate magnetometer(FGM)requires regular in-flight calibration to obtain its zero offset.Recently,Wang GQ and Pan ZH(2021a)developed a new method for the zero offset calibration based on the properti... The space-borne fluxgate magnetometer(FGM)requires regular in-flight calibration to obtain its zero offset.Recently,Wang GQ and Pan ZH(2021a)developed a new method for the zero offset calibration based on the properties of Alfvén waves.They found that an optimal offset line(OOL)exists in the offset cube for a pure Alfvén wave and that the zero offset can be determined by the intersection of at least two nonparallel OOLs.Because no pure Alfvén waves exist in the interplanetary magnetic field,calculation of the zero offset relies on the selection of highly Alfvénic fluctuation events.Here,we propose an automatic procedure to find highly Alfvénic fluctuations in the solar wind and calculate the zero offset.This procedure includes three parts:(1)selecting potential Alfvénic fluctuation events,(2)obtaining the OOL,and(3)determining the zero offset.We tested our automatic procedure by applying it to the magnetic field data measured by the FGM onboard the Venus Express.The tests revealed that our automatic procedure was able to achieve results as good as those determined by the Davis-Smith method.One advantage of our procedure is that the selection criteria and the process for selecting the highly Alfvénic fluctuation events are simpler.Our automatic procedure could also be applied to find fluctuation events for the Davis-Smith method. 展开更多
关键词 fluxgate magnetometer in-flight calibration zero offset highly alfvénic fluctuations automatic procedure
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慢太阳风中的小冕洞风和阿尔芬波 被引量:2
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作者 齐兆辉 刘勇 刘若炎 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2021年第11期3837-3845,共9页
慢太阳风的起源是一个困扰空间物理领域多年的问题,一些研究人员认为慢太阳风中阿尔芬度比较高的部分起源于小冕洞或者是冕洞的边界,不过另外一些研究者发现高阿尔芬度慢太阳风在成分上和低阿尔芬度的慢太阳风并无显著差别.最近的一项... 慢太阳风的起源是一个困扰空间物理领域多年的问题,一些研究人员认为慢太阳风中阿尔芬度比较高的部分起源于小冕洞或者是冕洞的边界,不过另外一些研究者发现高阿尔芬度慢太阳风在成分上和低阿尔芬度的慢太阳风并无显著差别.最近的一项研究中发现的慢太阳风中的小冕洞风并没有特别高的阿尔芬度.我们利用一个简单的二维太阳风模型计算了阿尔芬波和小冕洞风的传播;计算结果显示,由于阿尔芬波的传播特性,从小冕洞出发的等离子体和阿尔芬波动在传播到1AU的过程中会发生分离,形成了低阿尔芬度的小冕洞风和高阿尔芬度的普通慢风.这个结果定性地解释了慢太阳风中观测到的小冕洞风和高阿尔芬度慢风的特性,也为解开慢太阳风的起源之谜提供了新的思路. 展开更多
关键词 太阳风 小冕洞风 阿尔芬波 阿尔芬度
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