A neutrally buoyant, underwater acoustic intensity probe is constructed and
tested. This sensor measures the acoustic particle velocity at two closely
spaced locations, hence it is denoted a "u-u" intensity probe. A new theor
etical derivation infers the acoustic pressure from this one-dimensional ve
locity gradient, permitting the computation of one component of acoustic in
tensity. A calibration device, which produces a planar standing-wave field,
is constructed and tested. In this calibrator, the performance of the rc-r
r intensity probe compares favorably to that of an acoustic intensity probe
which measures both pressure and velocity directly. (C) 1999 Acoustical So
ciety of America. [S0001 -4966(99)05312-6].