강원․경북 동해안 접경 지역의 w 반모음화 관련 현상

Abstract

The purpose of this article is to examine the phenomena related to w Glide Formation by targeting the Samcheok and Uljin regional dialects, which are bordering regions of the east coast of Gangwon-do and the east coast of Gyeongsangbuk-do. Since the phenomenon related to w Glide Formation shows various appearances depending on the phonological environment(① the presence or absence of a consonant in the stem syllable of a verb, ② the type of consonant if there is a consonant, ③ the number of syllables in the stem of the verb, ④ whether the stem ending is an open syllable or a closed syllable), the application aspect of the phonological rule was examined. In the case where onsets of the stem-final syllable is other consonants, w glide formation occurs in the Samcheok regional dialect, but in the Uljin regional dialect, w glide formation followed by w deletion or w glide formation followed by ‘wə → o’ vowel coalescence occurs. In the case where onsets of the stem-final syllable is labial consonants, the necessary w deletion following w glide formation occurred in both regional dialects. In the case where onsets of the stem-final syllable is ∅, w glide formation occurs in both regional dialects, and w deletion occurred additionally in the Uljin regional dialect. Lastly, in the case of s irregular conjugation, In the case where onsets of the stem-final syllable is labial consonants, w glide formation occurs in both regional dialects, and ‘wə → o’ vowel coalescence occurred additionally in Uljin regional dialect. in the case of p irregular conjugation, w glide formation occur actively in the Samcheok regional dialect, but it is occur partly in the Uljin regional dialect.