Abstract
In the Dicke-Brans-Jordan theory of gravity, far away from a bounded system, orbiting test particles measure the total, active gravitational mass M while orbiting test black holes measure the "tensor" mass MT. Their difference (MMT) is the scalar mass MS. In this paper, conservation laws for MS, MT, and M are delineated and are used to show the following: (i) A spin-2 gravitational plane wave carries tensor mass, but does not carry scalar mass; the flux of tensor mass is proportional to the square of the time-integrated amplitude of the Riemann tensor |Ψ4dt|2. (ii) A spin-0 gravitational plane wave carries both tensor mass (flux proportional to the square of the time-integrated Riemann amplitude |Φ22dt|2) and scalar mass (flux proportional to the Riemann amplitude Φ22—or, equivalently, proportional to the second time derivatives of the amplitude of the scalar field 2φt2). (iii) The tensor mass in a gravitational wave curves up the background spacetime through which the wave propagates; the scalar mass does not. (iv) The tensor mass in a wave is positive-definite; the scalar mass is not. (v) If a dynamical spherical system emits gravitational waves that change its scalar mass by ΔMS in time τ (ΔMS may be positive or negative), then these waves will also reduce its tensor mass by an amount (ΔMS)2τ. The response of gravitational-wave antennas to scalar waves is discussed. It is shown that, whereas antennas of negligible self-gravity respond only to the tidal forces of the wave (Φ22), antennas with significant self-gravity respond about equally to the tidal forces Φ22 and the oscillating Cavendish gravitation constant φ. Because of the unique phase and amplitude relations of Φ22 and φ, the two responses are coherent—and can even cancel each other perfectly for a "carefully designed" detector.