(Askeri) GEÇİRİMLİ KORUYUCU GAZ ELBİSESİ: Yakıcı gazların buhar ve zerrelerine karşı nötrleştirme ile temin için, bazı kimya maddeleriyle emprenge edilmiş özel elbise
Pervious; a permeable rock is a rock, either porous or cracked, that allows water to soak into and pass through it freely
In geology, refers to a rock that due to its structure permits liquid or gasses to pass through it
Describes material or soil that allows the movement or passage of water through it Compare impermeable
Permeability is a measure of the ease with which a fluid will move through a porous material (e g , sand and gravel or rock) A geologic unit is permeable if ground water moves easily through it
Capable of being permeated, or passed through; yielding passage; passable; penetrable; used especially of substances which allow the passage of fluids; as, wood is permeable to oil; glass is permeable to light
If a substance is permeable, something such as water or gas can pass through it or soak into it. A number of products have been developed which are permeable to air and water. impermeable. material that is permeable allows water, gas etc to pass through it impermeable
a quantitative measure of the degree of magnetization of a material in the presence of an applied magnetic field (measured in Newtons per Ampere squared in SI units)
A semipermeable membrane, also termed a selectively permeable membrane, a partially permeable membrane or a differentially permeable membrane, is a membrane which will allow certain molecules or ions to pass through it by diffusion and occasionally specialized "facilitated diffusion". The rate of passage depends on the pressure, concentration and temperature of the molecules or solutes on either side, as well as the permeability of the membrane to each solute.Depending on the membrane and the solute, permeability may depend on solute size, solubility, properties, or chemistry. An example of a semi-permeable membrane is a lipid bilayer, on which is based the plasma membrane that surrounds all biological cells. Many natural and synthetic materials thicker than a membrane are also semipermeable. An example of this is the thin film on the inside of an egg
A semipermeable membrane, also termed a selectively permeable membrane, a partially permeable membrane or a differentially permeable membrane, is a membrane which will allow certain molecules or ions to pass through it by diffusion and occasionally specialized "facilitated diffusion". The rate of passage depends on the pressure, concentration and temperature of the molecules or solutes on either side, as well as the permeability of the membrane to each solute.Depending on the membrane and the solute, permeability may depend on solute size, solubility, properties, or chemistry. An example of a semi-permeable membrane is a lipid bilayer, on which is based the plasma membrane that surrounds all biological cells. Many natural and synthetic materials thicker than a membrane are also semipermeable. An example of this is the thin film on the inside of an egg
A semipermeable membrane, also termed a selectively permeable membrane, a partially permeable membrane or a differentially permeable membrane, is a membrane which will allow certain molecules or ions to pass through it by diffusion and occasionally specialized "facilitated diffusion". The rate of passage depends on the pressure, concentration and temperature of the molecules or solutes on either side, as well as the permeability of the membrane to each solute.Depending on the membrane and the solute, permeability may depend on solute size, solubility, properties, or chemistry. An example of a semi-permeable membrane is a lipid bilayer, on which is based the plasma membrane that surrounds all biological cells. Many natural and synthetic materials thicker than a membrane are also semipermeable. An example of this is the thin film on the inside of an egg
The ability of a material to allow the passage of liquid, such as water, through rocks Permeable materials, such as gravel and sand, allow water to move quickly through them, whereas unpermeable materials, such as clay, don't allow water to flow freely
the ability of a material to allow the passage of a liquid, such as water through rocks Permeable materials, such as gravel and sand, allow water to move quickly through them, whereas unpermeable material, such as clay, don't allow water to flow freely
The capability of a given substance to allow the passage of a fluid Permeability depends on the size of and the degree of connection among a substance's pores
The measure of the flow of water through soil The ease (or measurable rate) with which gasses, liquids, or plant roots penetrate or pass through a layer of soil or porous media The capacity or ability of a porous rock, sediment, or soil to allow the movement of water through its pores
(1) Ability of a material (generally an earth material) to transmit fluids (water) through its pores when subjected to pressure or a difference in head Expressed in units of volume of fluid (water) per unit time per cross section area of material for a given hydraulic head; (2) description of the ease with which a fluid may move through a porous medium; abbreviation of intrinsic permeability It is a property of the porous medium only, in contrast to hydraulic conductivity, which is a property of both the porous medium and the fluid content of the medium
The property of rock or soil permitting water to pass through it Primary permeability depends on pores between the grains of material Secondary Permeability depends on solutional widening of joints & bedding planes & on other solution cavities Hydrology terms Ref JJ
The capacity or ability of a porous medium, such as rock or soil, to transmit fluid; the rate of diffusion of a fluid under unequal pressure The common unit of measure is the millidarcy (mD)
a quantitative measure of the degree of magnetization of a material in the presence of an applied magnetic field (in terms of for instance, Newtons per square Amperes in SI units)
A soil characteristic that enables water or air to move through the profile, measured as the number of inches per hour that water moves down ward through the saturated soil The rate at which water moves through the least permeable layer governs soil permeability
(1) passage or diffusion of a gas, vapor, liquid, or solid through a material without physically or chemically affecting it; (2) term used to express various relationships between magnetic induction and magnetizing force; either absolute permeability or specific (relative) permeability
The ability of an aquifer or water-bearing formation to allow water to pass through it Permeability is also known as effective porosity because it is a function of interconnected saturated pore spaces
The capacity of a substance (such as rock) to transmit a fluid The degree of permeability depends on the number, size, and shape of the pores and/or fractures in the rock and their interconnections It is measured by the time it takes a fluid of standard viscosity to move a given distance The unit of permeability is the Darcy
A measure of the ability of soil, sediments, and rock to transport water horizontally and vertically Permeability is dependent on the porosity of the medium the water is flowing through Some rocks like granite have very poor permeability, while rocks like shale are actually quite pervious As for soils, sand is the most pervious, while clay has the lowest permeability Silt usually is somewhere in the middle