Temporal Fluctuation of Backscattered Field Due to Bioturbation in Marine Sediments
Abstract
Biological activity in marine sediments creates a time-varying, randomly fluctuating medium. A bio-diffusive model is proposed for predicting the temporal and spatial spectrum of sediment density fluctuations. Perturbation theory is used to model sediment volume scattering and the temporal correlation of the scattered field. These models are compared with field data recorded in a biologically active shallow water environment, and sediment blo-diffusion parameters are estimated.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jan 01, 1998
- Accession Number
- AD1114089
Entities
People
- Christopher D. Jones
- Darrell R. Jackson
Organizations
- University of Washington