Estudio de la intensidad en el marco de la prosodia de Canarias

  1. Carolina Jorge Trujillo 1
  2. Josefa Dorta 1
  3. Moisés Betancort 1
  1. 1 Universidad de La Laguna
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    Universidad de La Laguna

    San Cristobal de La Laguna, España

    ROR https://ror.org/01r9z8p25

    Geographic location of the organization Universidad de La Laguna
Journal:
Onomázein: Revista de lingüística, filología y traducción de la Pontificia Universidad Católica de Chile

ISSN: 0717-1285 0718-5758

Year of publication: 2017

Issue: 35

Pages: 145-172

Type: Article

DOI: 10.7764/ONOMAZEIN.35.09 DIALNET GOOGLE SCHOLAR lock_openDialnet editor

More publications in: Onomázein: Revista de lingüística, filología y traducción de la Pontificia Universidad Católica de Chile

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SDG classification obtained using Aurora SDG artificial intelligence model.

Abstract

This work aims at determining the importance of intensity within the research framework of Canarian prosody, by taking into account an acoustic and statistical study from a corpus of 648 sentences uttered in a formal speech style by Canarian informants from two diatopically opposed islands: El Hierro, which belongs to the western region of the Canarian Archipelago, and Fuerteventura, which belongs to the eastern region. With the obtained acoustic results, we have labelled the tonic vowels according to their intensity, by taking into account a differential threshold of 4 dB, which has been recently determined in a perceptive-type study (Dorta, Martín Gómez and Jorge Trujillo, in press). Furthermore, a statistical analysis has been carried out in R (R Core Team, 2015) and ULLRToolbox (Hernández-Cabrera, 2012). From the acoustic results obtained, the amplitude of the accentuated is found to be higher in the following circumstances: in the nuclear accent, the acute accent and the plain accent, the contrast tonic/ post-tonic, the declarative modality and pertaining to Fuerteventura. From the statistical results we highlight the importance of the contrast tonic/ post-tonic in the SPrep, which reflects the acoustically registered final descent in intensity.