Permeability is a measure of how fast water will flow through connected openings in soil or rock
L. K. Wenzel has written: 'Methods for determining permeability of water-bearing materials with special reference to discharging-well methods' -- subject(s): Groundwater, Bibliography, Soil percolation
Magnetic field strength is measured using a device called a magnetometer. There are different methods for determining magnetic field strength, including using a Hall effect sensor, a fluxgate magnetometer, or a SQUID (Superconducting Quantum Interference Device). These devices can accurately measure the strength of a magnetic field in a given area.
All materials are magnetized when placed in the magnetic field . The material magnetized by the effect of a magnetic field is called magnetic permeability.
1. The permeability results might be localized due to excavation. 2. Lateral permeability not considered which may lead to erroneous estimate of field permeability.
Two common indirect methods to determine the diameter of a hair in a microscope are by measuring the diameter of the field of view and the number of hairs across the field, and by using a calibration slide with known dimensions for comparison.
Permeability
Permeability is the measure of the ability of a material to support the formation of a magnetic field within itself.(Degree of magnetization that a material obtains in response to an applied magnetic field.) It is represented by the Greek letter μ.
The relative permeability of 10,000 means that the material can support a magnetic field 10,000 times more dense than than a magnetic field in free space.
The magnetic field of a wire can be increased by increasing the current flowing through the wire, increasing the number of turns in the wire to create a coil, or by using a material with higher permeability around the wire, such as an iron core. All of these methods increase the strength of the magnetic field produced by the wire.
The slope of the magnetic force vs. magnetic field graph represents the magnetic permeability of the material. A steeper slope indicates a higher magnetic permeability, meaning the material is more easily magnetized by an applied magnetic field. Conversely, a shallower slope indicates lower magnetic permeability.
Soil permeability is a measure of how easily water can flow through soil. It is an important factor in determining the ability of soil to absorb and drain water, which can impact plant growth and soil erosion.
Permeability of a nonmagnetic medium is defined as being equal to the permeability of a vacuum, which is approximately 4π x 10^-7 H/m. This means that nonmagnetic materials do not enhance or diminish the magnetic field passing through them.