Abstract
The geographical pattern of human dialects is a result of history. Here, we formulate a simple spatial model of language change which shows that the final result of this historical evolution may, to some extent, be predictable. The model shows that the boundaries of language dialect regions are controlled by a length minimizing effect analogous to surface tension, mediated by variations in population density which can induce curvature, and by the shape of coastline or similar borders. The predictability of dialect regions arises because these effects will drive many complex, randomized early states toward one of a smaller number of stable final configurations. The model is able to reproduce observations and predictions of dialectologists. These include dialect continua, isogloss bundling, fanning, the wavelike spread of dialect features from cities, and the impact of human movement on the number of dialects that an area can support. The model also provides an analytical form for Séguy’s curve giving the relationship between geographical and linguistic distance, and a generalization of the curve to account for the presence of a population center. A simple modification allows us to analytically characterize the variation of language use by age in an area undergoing linguistic change.
15 More- Received 28 February 2017
DOI:https://doi.org/10.1103/PhysRevX.7.031008
Published by the American Physical Society under the terms of the Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI.
Published by the American Physical Society
Physics Subject Headings (PhySH)
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Language Boundaries Driven by Surface Tension
Published 17 July 2017
A new model of language evolution assumes that changes in the spatial boundaries between dialects are controlled by a surface tension effect.
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Popular Summary
A “dialect” is defined as a set of linguistic idiosyncrasies shared by speakers of a particular geographical region, and language surveys can be used to define dialect regions and measure dialect differences. Here, we claim that regional dialects are driven by individuals’ tendency to conform. We show that the evolution of isoglosses—geographic boundaries between dialects—is driven by two opposing forces: An effect analogous to surface tension renders isoglosses smoother over time, but variations in population density create curvature. These two effects, encapsulated in a single equation drawing on ideas from statistical mechanics, allow us to predict the spatial distribution of dialects.
Using population density census data from the United Kingdom, we predict the most likely pattern of English dialects assuming that people living within roughly 10 to 20 kilometers of one another come into linguistic contact. We consider these interactions between individual speakers and model the geographical distribution of dialects throughout the United Kingdom. We find that many isoglosses follow similar patterns, which results in “isogloss bundling” despite initial differences in language use. Our model also reproduces several observed phenomena, including the expansion of urban dialects—such as those in the London area—and the relation between linguistic distance and geographical distance, which is of long-standing interest to dialectologists.
Our model is deliberately simple in its assumptions yet still yields predictive power. It lays a theoretical foundation to investigate patterns in other countries and in other cultural or natural processes that involve copying, such as technology, art, and possibly evolution.