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Concept
Pragmatics
Summary
In linguistics and related fields, pragmatics is the study of how context contributes to meaning. The field of study evaluates how human language is utilized in social interactions, as well as the relationship between the interpreter and the interpreted. Linguists who specialize in pragmatics are called pragmaticians. The field has been represented since 1986 by the International Pragmatics Association (IPrA).
Pragmatics encompasses phenomena including implicature, speech acts, relevance and conversation, as well as nonverbal communication. Theories of pragmatics go hand-in-hand with theories of semantics, which studies aspects of meaning, and syntax which examines sentence structures, principles, and relationships. The ability to understand another speaker's intended meaning is called pragmatic competence. Pragmatics emerged as its own subfield in the 1950s after the pioneering work of J.L. Austin and Paul Grice.
Pragmatics was a reaction to structuralist linguistics as outlined by Ferdinand de Saussure. In many cases, it expanded upon his idea that language has an analyzable structure, composed of parts that can be defined in relation to others. Pragmatics first engaged only in synchronic study, as opposed to examining the historical development of language. However, it rejected the notion that all meaning comes from signs existing purely in the abstract space of langue. Meanwhile, historical pragmatics has also come into being. The field did not gain linguists' attention until the 1970s, when two different schools emerged: the Anglo-American pragmatic thought and the European continental pragmatic thought (also called the perspective view).
The study of the speaker's meaning focusing not on the phonetic or grammatical form of an utterance but on what the speaker's intentions and beliefs are.
The study of the meaning in context and the influence that a given context can have on the message. It requires knowledge of the speaker's identities, and the place and time of the utterance.
Official source
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