i̇letirlik

listen to the pronunciation of i̇letirlik
Türkçe - İngilizce
transmissivity
A measure of the capacity of a material to transmit radiation (the ratio of the amounts of energy transmitted and received)
A measure of luminous flux remaining in a light beam after it has passed through a specified distance of the atmosphere
An intrinsic property of a material; the ratio of energy transmitted by a material to total incident radiation
the proportion of a flux of electromagnetic radiation which is transmitted through the atmosphere (or part of it)
Flow capacity of an aquifer measured in volume per unit time per unit width Equal to the product of hydraulic conductivity times the saturated thickness of the aquifer < back to top U
refers to the rate at which limestone allows the transmission of water Limestone can be highly porous, but not very transmissive if the pores are not connected to each other Technically speaking, it is the rate at which water is transmitted through a unit width of aquifer under unit hydraulic gradient Transmissivity is directly proportional to aquifer thickness, thus it is high where the Edwards is thick and low where it is thin, given the same hydraulic conductivity
The rate at which water is transmitted through a unit width of an aquifer under a unit hydraulic gradient In the English Engineering System, transmissivity values are given in gallons per minute through a vertical section of an aquifer one foot wide and extending the full saturated height of an aquifer under a hydraulic gradient of 1 In the International System, transmissivity is given in cubic metres per day through a vertical section of an aquifer one metre wide and extending the full saturated height of an aquifer under a hydraulic gradient of 1
the rate at which water passes through an aquifer
A measure of the ability of an aquifer to transmit water
The rate at which water of the prevailing kinematic viscosity is transmitted through a unit width under a unit hydraulic gradient
The ability of an aquifer to transmit water
A property that determines the fraction of the irradiation passes through the surface
the rate of flow of water through a vertical strip of aquifer which is one unit wide and which extends the full saturated depth of the aquifer Transmissivity is related to Hydraulic Conductivity by the relationship
Rate at which water is transmitted through a unit width of an aquifer under a unit hydraulic gradient Transmissivity values can be expressed as square metres per day (m2/day), or as square metres per second (m2/s)
The rate at which groundwater can flow through an aquifer section of unit width under a unit hydraulic gradient It is the average permeability of a section of the entire aquifer at a given location multiplied by the thickness of the formation
The rate at which water is transmitted through a unit width of an aquifer under a unit hydraulic gradient It equals the hydraulic conductivity multiplied by the aquifer thickness
  Obsolete   See transmittance
The rate at which water is passed through a unit width of rock under a unit hydraulic gradient
The fraction of light that passes through the interior of a glass pane at normal incidence This does not consider light lost to reflection by the front or back surface, or multiple internal reflections From the transmissivity and the index of refraction, total transmittance and reflectance can be computed for any incident angle via a simple formula (See the CD-ROM section on materials for details )
1) The ability of an aquifer to transmit water 2) The rate at which water of the prevailing kinematic velocity is transmitted through a unit width of the aquifer under a unit of hydraulic gradient Normally ranges from 1,000 to 1,000,000 gal/day/ft