学术文献库

The mass physical and dynamic properties of marine mud deposits are a function of the interaction among a maximum of four sediment Phases as follows: (1) clay mineral solids that often include silt and sand size particles of different mineralogy, (2) semisolid hydrated organic matter, (3) free pore water, and (4) free gas when present. Historically, the total water was removed by oven drying which includes the seawater of hydration of the organic matter (OM); thus, the total water content was considered free pore water in several research disciplines. The semisolid hydrated OM resists transport through the mud pore space and the water that is bound to the OM is not free pore water. Calculations of marine mud mass-physical properties without consideration and correction for the presence of hydrated organic matter can introduce significant error in the amount of free water content of the pore space in the mud and the quantitative differences in both porosity and void ratio. Simulations reveal absolute relative differences due to the presence of hydrated OM that can reach meaningful values even when the %TOC values are below ~3%. Relevance is determined by comparing the differences due to the hydrated OM Phase with the differences in the fluid saturation Phase at 100% and at 90%. Understanding the presence and characteristics of hydrated OM is expected to engage important future research in several sciences and in geotechnical engineering of terrestrial and marine mud deposits.