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Simulation of plectoneme formation: Final Report
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Executive Summary
This final report summarizes an INFUSE-funded collaboration between Los Alamos National Laboratory and Helicity Space Corporation to simulate plectoneme formation and stable magnetized plasma jets using the LA-COMPASS 3D MHD code. The study successfully reproduced key characteristics of the MOCHI experiment, demonstrating that nested electrodes and specific injection conditions drive stabilizing helical shear flows essential to the Helicity Drive fusion concept. The findings provide quantitative scaling insights and validate the physical feasibility of creating long, stable plasma jets for advanced magneto-inertial fusion applications.
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ST_CODE: MATION
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DOC-HELICITY
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Page 1 of 6
Project Overview & Section 1.1 Problem Statement
Simulation of plectoneme formation
Final Report
National Laboratory: Los Alamos National Laboratory
Principal Investigator: Dr. Hui Li ([email protected]), Dr. Shengtai Li ([email protected])
Company: Helicity Space Corporation
Principal Investigator: Dr. Setthivoine You ([email protected])
Award: INFUSE 2019
Period of Performance: June 2020 – June 2021
Final Report Submission Date: April 6th, 2022
Note: Report may be posted publicly. Do not include proprietary information.
1 Technical Overview
1.1 Problem Statement
Describe the company challenges this program is meant to address. Should be adapted from original application, noting any departures / evolutions from that original application.
The challenge facing the company is developing some predictive capability for a key ingredient of the Helicity Drive fusion concept in a cost-effective and timely manner.
The key ingredient is a novel, magnetized, plasma configuration called a plectoneme for short.
A plectoneme is a non-axisymmetric m = 1 Taylor state. It is a cousin of the spheromak which is the axisymmetric m = 0 Taylor state. The name plectoneme is taken from the mathematics of twisted ribbons and frequently used in the description of DNA double-helix "supercoil" strands.
Open plectonemes can be thought of as cables or ropes that are sufficiently twisted to develop tight intertwined strands that emerge between the cable ends; and closed plectonemes can be thought of as tightly twisted rubber band loops inside a long closed cylinder. Magnetic plectoneme configurations were first predicted theoretically almost forty years ago [1, 2], and recently discovered in the SSX experiment with close-fitting flux conserving walls [3, 4] and in the MOCHI experiment within a stable magnetized jet without close-fitting walls [5-7].
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This final report summarizes an INFUSE-funded collaboration between Los Alamos National Laboratory and Helicity Space Corporation to simulate plectoneme formation and stable magnetized plasma jets using the LA-COMPASS 3D MHD code. The study successfully reproduced key characteristics of the MOCHI ex...