• Title/Summary/Keyword: Rising contour

Search Result 15, Processing Time 0.02 seconds

The Perception and Production of Vietnamese Tones by Japanese, Lao and Taiwanese Second Language Speakers

  • Dao, Muc Dich;Anh, Thu T. Nguyen
    • SUVANNABHUMI
    • /
    • v.14 no.1
    • /
    • pp.193-228
    • /
    • 2022
  • This study investigates the production and perception of Vietnamese tones by Japanese, Lao, and Taiwanese second language (L2) learners [n=30], comparing their performance in an Imitation task to that of Identification and Read-Aloud tasks. The results show that the Imitation task is generally easier for L2 speakers than the Identification and Read-Aloud tasks, suggesting that imitation is performed without some of the skills required by the other two tasks. It is also found that Lao and Taiwanese speakers outperform Japanese speakers, suggesting that prior experience with one tone language facilitates the acquisition of tone in another language. The result on speakers' tonal range show that L2 leaners have significantly narrower tonal F0 range than control Vietnamese speakers [n=11]. The results of error pattern analysis and tonal transcription also suggest that non-modal voice (glottal stop and creakiness) and contour tones (bidirectional fall-rise) are more difficult for L2 learners than modal voice tones (e.g., unidirectional contours: rising, falling, and level).

Intonation Patterns of Korean Spontaneous Speech (한국어 자유 발화 음성의 억양 패턴)

  • Kim, Sun-Hee
    • Phonetics and Speech Sciences
    • /
    • v.1 no.4
    • /
    • pp.85-94
    • /
    • 2009
  • This paper investigates the intonation patterns of Korean spontaneous speech through an analysis of four dialogues in the domain of travel planning. The speech corpus, which is a subset of spontaneous speech database recorded and distributed by ETRI, is labeled in APs and IPs based on K-ToBI system using Momel, an intonation stylization algorithm. It was found that unlike in English, a significant number of APs and IPs include hesitation lengthening, which is known to be a disfluency phenomenon due to speech planning. This paper also claims that the hesitation lengthening is different from the IP-final lengthening and that it should be categorized as a new category, as it greatly affects the intonation patterns of the language. Except for the fact that 19.09% of APs show hesitation lengthening, the spontaneous speech shows the same AP patterns as in read speech with higher frequency of falling patterns such as LHL in comparison with read speech which show more LH and LHLH patterns. The IP boundary tones of spontaneous speech, showing the same five patterns such as L%, HL%, LHL%, H%, LH% as in read speech, show higher frequency of rising patterns (H% and LH%) and contour tones (HL%, LH%, LHL%) while read speech on the contrary shows higher frequency of falling patterns and simple tones at the end of IPs.

  • PDF

A Comparative Study on the Characteristics of the Prosodic Phrases between Autism Spectrum Disorder and Normal Children in the Reading of Korean Read Sentences (자폐 범주성 장애아동과 정상아동의 평서문 읽기에서의 운율구 특성 비교)

  • Jung, Kum-Soo;Seong, Cheol-Jae
    • MALSORI
    • /
    • no.65
    • /
    • pp.51-65
    • /
    • 2008
  • The aim of this study is to compare ASD (Autism Spectrum Disorder) children with normal children in terms of the prosodic features. Materials are collected by the reading of Korean read sentences. They are composed of 10 declarative sentences, each of which was consisted of 5-6 words. Subjects are consisted of 10 ASD and 10 normal male children with a receptive vocabulary age of 5;0-6;5 years. We found out that both groups showed the differences not only in the tonal patterns at the end of the prosodic phrases, but also in both the degree of rising and falling slope related to pitch contour. While HL% and HLH% were highly emerged in sentence final position in normal group, HL% and HLH% were prominent in ASD group in the same position. LH% and LHL% IP types were observed only in ASD group in sentence medial position. The slope showing the variation in the fundamental frequency at the end of the prosodic phrase was twice as steep in the group of ASD children as in the group of normal children.

  • PDF

A Study on Risk Assessment and Risk Mitigation Measures of Liquefied Chlorine Leak (액화염소 누출의 위험도 분석 및 위험경감조치에 대한 연구)

  • Lee, Ju-Youn;Chon, Young-Woo;Hwang, Yong-Woo;Lee, Ik-Mo
    • Journal of the Korea Safety Management & Science
    • /
    • v.20 no.1
    • /
    • pp.1-9
    • /
    • 2018
  • As the chemical industry becomes more advanced, the awareness of chemical accidents is rising, and legal systems for chemical safety management are strengthened. In this study, quantitative risk assessment of liquid chlorine leak was conducted. Risk assessment was performed in the order of frequency analysis, consequence analysis, and risk calculation. The individual risk was presented in the form of contour lines. The social risk was expressed by the FN curve. The risk of day and night was in an unacceptable area, so it was required to mitigate risk. Therefore in-building, which could trap the pool, was selected as a risk mitigation measure. As a result of the cost benefit analysis, it was concluded that this measure should be reasonably implemented.

Submarine Layer Structure By Seismic Reflection Survey Between Geoje Island And Namhae Island (탄성파 탐사로 본 거제도 남해도간의 해저지층 구조)

  • Song, Moo-Young;Jo, Kyu Chang
    • 한국해양학회지
    • /
    • v.13 no.1
    • /
    • pp.1-8
    • /
    • 1978
  • A seismic reflection Survey was carried out in the offshere area between Geoje Island and Namhae Island, utilizing the echosounder with the frequency 28KHz and thd Uniboom with the filter band 800∼2000Hz. The results show the submarine topography, sedimentary layer structure and the depth distribution of the base rock. The water depth of the sea in the survey area is less than 80m; up to 40m contour line the sea bottom surface has a slight dip(about 1/1000), while in the zone deeper than 40m the bottom topography has a irregular relief. The thickness of the whole sedimentary deposit is about 20∼70m and divided into 3 layers: Upper layer(A layer) with horizontal laminae, intermediate layer(B layer) with cross-bedding and groove structure, and lower layer(C layer) not showing any sedimentary structure on the seismic reflection profile. The surface of the base rock is deeper gradually in the south-eastern part of the survey area and extends to 140m depth. The vertical sediments sequences, composed of B layer and A layer, show the type of transgressive sequences. It is interpreted that B layer was formed at one period when the sea level was lower 40∼60 than the present and ince then, following the rising of the sea level, A layer was deposited.

  • PDF