Week 5: Water Retention and Movement in Soil and Solute Transport Flashcards
Volumetric water content
Volume of water in the sample over the volume of the wet material.
Gravimetric water content
Mass of water over the mass of the substance.
Porosity
Volume of pore space by total volume – is dimensionless.
Porosity = specific yield (Sy) + specific retention (Sr)
Tension
The elastic-like force existing in the surface of a liquid caused by the attraction of the particles in the surface layer by the bulk of the liquid. Minimises surface area.
Available water
The water available for plants to use.
Given as a fraction between field capacity and the permanent wilting point.
As plants use this water the stress on the plant increases and growth diminishes.
Field capacity
The moisture content of the soil after the excess water has drained, often taken 1-3 after drainage from saturation has occurred. Taken when the pressure head is -10kPa.
Pousille’s Law
In the case of laminar flow, the volume flowrate is given by the pressure difference divided by the viscous resistance.
Hydraulic conductivity
Describes the ease with which a fluid (usually water) can move through pore spaces or fractures. Given by permeability x fluidity.
Water retention
An equation to describe the relationship between soil water pressure (ψ) and water content (θ).
Solute transport
The movement of solutes through the catchment.
Advection
A transport mechanism of water due to a fluids bulk motion. E.g. the transportation of pollutants or silt in a river by water flow downstream.
Dispersion
Distribution of particles over a wide area.
Retardation
The process of delaying or impeding.