论文标题
逐步的压力平衡,流量松弛,并在反向场捏中应用
Stepped pressure equilibrium with relaxed flow and applications in reversed-field pinch plasmas
论文作者
论文摘要
多区域放松的MHD(MRXMHD)在三维(3D)构型以均衡的构建方面取得了成功。在MRXMHD中,等离子体被切成由理想界面分离的子体积,每个界面都会放松,从而形成了岛屿和混乱。所得的平衡在跨亚卷的范围内具有逐步的压力曲线。阶梯压力平衡代码(规格)[S.R. Hudson等人,物理学。等离子体19,112502(2012)]开发了以数值计算MRXMHD平衡。在这项工作中,我们扩展了规格代码,以计算出具有场对齐的流量和旋转的MRXMHD平衡,并遵循理论发展,以结合交叉热度和角动量约束。该代码已经过验证以进行收敛,并将其与2D中的毕业生shafranov求解器进行了比较。我们应用新工具来研究反向场捏置放电的锯齿崩溃之前和之后的流量变化,其中可用的平行流量数据可用。我们发现有希望的结果是,在交叉旋转和角动量的限制下,裂纹后特定平衡中的平行流量图在等离子体核心中是平坦的,而流动幅度与实验观察匹配。最后,我们提供了一个示例平衡,具有3D螺旋场结构作为偏爱的较低能量状态。这将是第一个3D数值平衡,其中流动效应是自吻的。
The Multi-region Relaxed MHD (MRxMHD) has been successful in the construction of equilibria in three-dimensional (3D) configurations. In MRxMHD, the plasma is sliced into sub-volumes separated by ideal interfaces, each undergoing relaxation, allowing the formation of islands and chaos. The resulting equilibrium has a stepped pressure profile across sub-volumes. The Stepped Pressure Equilibrium Code (SPEC) [S.R. Hudson et al., Phys. Plasmas 19, 112502 (2012)] was developed to calculate MRxMHD equilibria numerically. In this work, we have extended the SPEC code to compute MRxMHD equilibria with field-aligned flow and rotation, following the theoretical development to incorporate cross-helicity and angular momentum constraints. The code has been verified for convergence and compared to a Grad-Shafranov solver in 2D. We apply our new tool to study the flow profile change before and after the sawtooth crash of a reversed-field pinch discharge, in which data of the parallel flow is available. We find the promising result that under the constraints of cross-helicity and angular momentum, the parallel flow profile in post-crash SPEC equilibrium is flat in the plasma core and the amplitude of the flow matches experimental observations. Finally, we provide an example equilibrium with a 3D helical field structure as the favoured lower energy state. This will be the first 3D numerical equilibrium in which the flow effects are self-consistently calculated.