directional permeability measurement - meaning and definition. What is directional permeability measurement
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What (who) is directional permeability measurement - definition

MEASURE OF THE ABILITY OF A POROUS MATERIAL TO ALLOW FLUIDS TO PASS THROUGH IT
Pervious; Permeability (soil science); Permeability (geology); Fluid permeability; Permeability tensor; Permeability (fluid); Intrinsic permeability; Permeable rock; Impervious; Soil permeability; Permeability (earth science); Gas permeability; Permeability (earth sciences)
  • Symbol used to represent ''in situ'' permeability tests in geotechnical drawings

Magnetic Permeability         
MEASURE OF THE ABILITY OF A MATERIAL TO SUPPORT THE FORMATION OF A MAGNETIC FIELD WITHIN ITSELF
Magnetic permeability; Permeability(electromagnetics); Vacuum Permeability; Magnetic Permeability; Relative Permeability; Magnetic permittivity; Μi; Relative magnetic permeability
The specific susceptibility of any substance, existing in a mass, for magnetic induction. (See Magnetic Induction, Coefficient of, synonym for Magnetic Permeability and Magnetization, Coefficient of Induced.) Synonyms--Magnetic Inductive Capacity--Multiplying Power--Coefficient of Magnetic Induction.
Permeability (electromagnetism)         
MEASURE OF THE ABILITY OF A MATERIAL TO SUPPORT THE FORMATION OF A MAGNETIC FIELD WITHIN ITSELF
Magnetic permeability; Permeability(electromagnetics); Vacuum Permeability; Magnetic Permeability; Relative Permeability; Magnetic permittivity; Μi; Relative magnetic permeability
In electromagnetism, permeability is the measure of magnetization that a material obtains in response to an applied magnetic field. Permeability is typically represented by the (italicized) Greek letter μ.
Páramo Directional Clothing         
BRITISH CLOTHING COMPANY
Paramo Directional Clothing
Páramo Directional Clothing is a British outdoor clothing company. It was founded by Nick Brown, who also started the Nikwax waterproofing products company.

Wikipedia

Permeability (Earth sciences)

Permeability in fluid mechanics and the Earth sciences (commonly symbolized as k) is a measure of the ability of a porous material (often, a rock or an unconsolidated material) to allow fluids to pass through it.