These
significant depths suggest that Ceres» subsurface is no more than 40 percent ice by
volume, and the rest may be a mixture
of rock and low - density
materials such as salts or chemical compounds called clathrates.
These characteristics included morphometric, geographic, and historical properties
of study reservoirs (i.e., depth, residence time,
volume, surface area, age, and latitude), biologically
significant water column solute concentrations (i.e., NO3 — , total phosphorus, and dissolved organic carbon), and metrics
of ecosystem primary productivity (i.e., trophic status and mean or modeled surface water chlorophyll a concentrations; see the supplemental
materials for a complete list
of the tested variables).