'American Institute of Aeronautics and Astronautics (AIAA)'
Abstract
Reliable prediction of the high heat transfer rates experienced
during the hypersonic portion of planetary entry and descent is
critical to vehicle survival. Two types of sensors that can be used to
measure surface heat flux are coaxial thermocouple gages and thin
film resistance thermometers. Individually, both types of gages have
been used successfully in a number of studies [1–19]. Both
thermocouple and thin film gages measure surface temperature from
which heat transfer can be calculated. Both have µs response times,
and can be flush-mounted in models. Coaxial thermocouples are
robust, can survive challenging experimental conditions, and are
typically used in higher enthalpy flows. Thin film resistance gages
typically provide improved signal levels, but are less robust, have to
be individually calibrated, and are typically used in lower enthalpy
flows. As a result, there are few studies which directly compare
measurements from the two types of gages. In the present work, we
perform experimental measurements at a range of intermediate
enthalpies in hypervelocity flow and make direct comparisons
between temperature histories and heat flux data obtained from
thermocouple and thin film gages