skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Ion temperature measurements in the Maryland Spheromak

Thesis/Dissertation ·
DOI:https://doi.org/10.2172/10140798· OSTI ID:10140798
 [1]
  1. Univ. of Maryland, College Park, MD (United States)

Initial spectroscopic data from MS showed evidence of ion heating as deduced from the line widths of different ion species. Detailed measurements of OIV spectral emission line profiles in space and time revealed that heating takes place at early time, before spheromak formation and is occurring within the current discharge. The measured ion temperature is several times the electron temperature and cannot be explained by classical (Spitzer) resistivity. Classically, ions are expected to have lower temperatures than the electrons and therefore, lower temperatures than observed. High ion temperatures have been observed in different RFP`s and Spheromaks but are usually associated with relaxation to the Taylor state and occur in the sustainment phase. During formation, the current delivered to start the discharge is not axisymmetric and as a consequence, X-points appear in the magnetic flux. A two dimensional analysis predicts that magnetic reconnection occurring at an X-point can give rise to high ion heating rates. A simple 0-dimensional calculation showed that within the first 20 μs, a conversion of mass flow kinetic energy into ion temperature could take place due to viscosity.

Research Organization:
Univ. of Maryland, College Park, MD (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
FG05-86ER53241
OSTI ID:
10140798
Report Number(s):
DOE/ER/53241-7-Pt.3; ON: DE94009604; BR: AT051011C/AT051011E; TRN: 94:007563
Resource Relation:
Other Information: TH: Thesis (Ph.D.); PBD: 1992
Country of Publication:
United States
Language:
English