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In social science, mass communication is related to communication studies, but has its roots in sociology.Mass communication is "the process by which a person, group of people or organization creates a message and transmits it through some type of medium to a large, anonymous, heterogeneous audience."
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Copy of a newspaper (El Universo), an example of mass media. Mass media include the diverse arrays of media that reach a large audience via mass communication.. Broadcast media transmit information electronically via media such as films, radio, recorded music, or television.
Mass mobilization (also known as social mobilization or popular mobilization) refers to mobilization of civilian population as part of contentious politics.Mass mobilization is defined as a process that engages and motivates a wide range of partners and allies at national and local levels to raise awareness of and demand for a particular development objective through face-to-face dialogue.
Various acoustic devices in a Greek radio studio Deep, pulsating digital sound effect Voice saying "Ja", followed by the same recording with a massive digital reverb A blackbird singing, followed by the same recording with the blackbird singing with 5 voices
The x-axis of a mass spectrum represents a relationship between the mass of a given ion and the number of elementary charges that it carries. This is written as the IUPAC standard m/z to denote the quantity formed by dividing the mass of an ion (in daltons) by the dalton unit and by its charge number (positive absolute value).
Edmund Gustav Albrecht Husserl (/ ˈ h ʊ s ɜːr l / HUUSS-url, [14] US also / ˈ h ʊ s ər əl / HUUSS-ər-əl; [15] German: [ˈɛtmʊnt ˈhʊsɐl]; [16] 8 April 1859 – 27 April 1938 [17]) was an Austrian-German philosopher and mathematician who established the school of phenomenology.
Mathematically, mass flux is defined as the limit =, where = = is the mass current (flow of mass m per unit time t) and A is the area through which the mass flows.. For mass flux as a vector j m, the surface integral of it over a surface S, followed by an integral over the time duration t 1 to t 2, gives the total amount of mass flowing through the surface in that time (t 2 − t 1): = ^.