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Title: [Anomalous ion transport and feedback control]

Technical Report ·
DOI:https://doi.org/10.2172/10169878· OSTI ID:10169878

The slab branch of the ITG mode was produced by a d.c. ion acceleration heating scheme and definitively identified in CLM under the previous DOE grant. A transit-time rf heating scheme was used to produce a more Maxwellian ion population to produce and identify a more predictable slab ITG mode. These experiments are partly based on some theoretical work on the substantial effects of anisotropy in {eta}{sub i} on the slab mode. The progress under the present DOE grant are described below.

Research Organization:
Columbia Univ., New York, NY (United States)
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
FG02-87ER53257
OSTI ID:
10169878
Report Number(s):
DOE/ER/53257-6; ON: DE93018324; TRN: 93:016788
Resource Relation:
Other Information: PBD: [1993]
Country of Publication:
United States
Language:
English

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