An ANSI standard FORTRAN-77 numerical model is provided. The model pre
dicts the spatial and temporal change in seafloor particle size seawar
d of a river mouth. The model needs the input files generated by a sis
ter program DELTA2, a 2-D model that simulates the progradation of a r
iver delta and the resultant fill of one or more marine basins. GRAIN2
tracks four size fractions in the mud-size range: coarse silt, medium
silt, fine silt, and clay. Their spatial distribution is determined u
sing (1) a velocity distribution developed from a buoyancy-dominated,
free, 2-D jet flowing into a highly stratified marine basin; and (2) a
particle-scavenging model that takes into account the biogeochemical
affects of settling of particles in a marine environment (i.e. floccul
ation). This hemipelagic component is predicted seasonally (four times
a year) based on fluctuations in river velocity and river mouth shape
, and on the suspended load discharged into the sea. Sand deposition i
s predicted from the seasonal rate of turbidity current deposition, an
d from DELTA2. The model is sensitive to changes in river mouth positi
on and thus sediment supply and sea level fluctuations.