Soil permeability determines the water flow characterises in soil, that is, a soil’s ability to allow water to pass through it. The permeability is calculated as coefficient of permeability (k) - also known as hydraulic conductivity- and is based on Darcy’s law for laminar flow in sediment. The coefficient is defined as the rate of flow through a cross section of soil. Depending on the type of soil, either a constant-head or falling-head permeameter can be used to measure the permeability.
Ons bedrijf is gesloten van 21 december t/m 3 januari 2021!
Dear visitor,
We will be closed from December 24 to January 8.
Happy Holidays!
