Loading…

蘇州方言連讀變調的共時層面和歴史層次

蘇州方言有兩種連讀變調:(1)以後字爲基字的語音變調,(2)以前字爲基字的音義變調。音義變調的後字高度中和,連調式廣泛漂移並導致單字調竄調,連調規則跟語音變調截然不同。兩種連調分屬不同的共時層面,又是發生於不同時期的歷史層次。語音變調早期是主層,音義變調則是從語音變調中衍生的創新變層。音義變調最初產生於動詞體貌結構、動詞重疊式、數量結構等語法單位,然後向其他語法、詞彙單位擴散,目前已成爲蘇州方言連調式的主層,語音變調則降爲滯後的變層。音義變調的衍生過程類似詞彙單位的語法化。...

Full description

Saved in:
Bibliographic Details
Published in:Journal of Chinese Linguistics Monograph Series 2010-12 (24), p.21-32
Main Author: 李小凡(Xiaofan Li)
Format: Article
Language:Chinese
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites
container_end_page 32
container_issue 24
container_start_page 21
container_title Journal of Chinese Linguistics Monograph Series
container_volume
creator 李小凡(Xiaofan Li)
description 蘇州方言有兩種連讀變調:(1)以後字爲基字的語音變調,(2)以前字爲基字的音義變調。音義變調的後字高度中和,連調式廣泛漂移並導致單字調竄調,連調規則跟語音變調截然不同。兩種連調分屬不同的共時層面,又是發生於不同時期的歷史層次。語音變調早期是主層,音義變調則是從語音變調中衍生的創新變層。音義變調最初產生於動詞體貌結構、動詞重疊式、數量結構等語法單位,然後向其他語法、詞彙單位擴散,目前已成爲蘇州方言連調式的主層,語音變調則降爲滯後的變層。音義變調的衍生過程類似詞彙單位的語法化。
format article
fullrecord <record><control><sourceid>airiti</sourceid><recordid>TN_cdi_airiti_journals_P20181128001_201012_201811290012_201811290012_21_32</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><airiti_id>P20181128001_201012_201811290012_201811290012_21_32</airiti_id><sourcerecordid>P20181128001_201012_201811290012_201811290012_21_32</sourcerecordid><originalsourceid>FETCH-airiti_journals_P20181128001_201012_201811290012_201811290012_21_323</originalsourceid><addsrcrecordid>eNpjYeA0MjGw1DWyMLfgYOAtLs4yMDAwNjCwtDQ34GQwezGj_en2ec-m7XyxouFlw-IX6xperOt6sWr_81ktT1s3PpvZ9HTjkpdzFz2d1PNs7Zan_ZuA3GdrFvIwsKYl5hSn8kJpbgYvN9cQZw_dxMyizJLM-Kz80qI8oER8gJGBoYWhoZGFgYFhPJBtYGgUDxWyNMDkGMYbGxlT1TAA-XBXvQ</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>蘇州方言連讀變調的共時層面和歴史層次</title><source>JSTOR</source><creator>李小凡(Xiaofan Li)</creator><creatorcontrib>李小凡(Xiaofan Li)</creatorcontrib><description>蘇州方言有兩種連讀變調:(1)以後字爲基字的語音變調,(2)以前字爲基字的音義變調。音義變調的後字高度中和,連調式廣泛漂移並導致單字調竄調,連調規則跟語音變調截然不同。兩種連調分屬不同的共時層面,又是發生於不同時期的歷史層次。語音變調早期是主層,音義變調則是從語音變調中衍生的創新變層。音義變調最初產生於動詞體貌結構、動詞重疊式、數量結構等語法單位,然後向其他語法、詞彙單位擴散,目前已成爲蘇州方言連調式的主層,語音變調則降爲滯後的變層。音義變調的衍生過程類似詞彙單位的語法化。</description><identifier>ISSN: 2409-2878</identifier><language>chi</language><publisher>Journal of Chinese Linguistics Publication Office</publisher><ispartof>Journal of Chinese Linguistics Monograph Series, 2010-12 (24), p.21-32</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781</link.rule.ids></links><search><creatorcontrib>李小凡(Xiaofan Li)</creatorcontrib><title>蘇州方言連讀變調的共時層面和歴史層次</title><title>Journal of Chinese Linguistics Monograph Series</title><description>蘇州方言有兩種連讀變調:(1)以後字爲基字的語音變調,(2)以前字爲基字的音義變調。音義變調的後字高度中和,連調式廣泛漂移並導致單字調竄調,連調規則跟語音變調截然不同。兩種連調分屬不同的共時層面,又是發生於不同時期的歷史層次。語音變調早期是主層,音義變調則是從語音變調中衍生的創新變層。音義變調最初產生於動詞體貌結構、動詞重疊式、數量結構等語法單位,然後向其他語法、詞彙單位擴散,目前已成爲蘇州方言連調式的主層,語音變調則降爲滯後的變層。音義變調的衍生過程類似詞彙單位的語法化。</description><issn>2409-2878</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNpjYeA0MjGw1DWyMLfgYOAtLs4yMDAwNjCwtDQ34GQwezGj_en2ec-m7XyxouFlw-IX6xperOt6sWr_81ktT1s3PpvZ9HTjkpdzFz2d1PNs7Zan_ZuA3GdrFvIwsKYl5hSn8kJpbgYvN9cQZw_dxMyizJLM-Kz80qI8oER8gJGBoYWhoZGFgYFhPJBtYGgUDxWyNMDkGMYbGxlT1TAA-XBXvQ</recordid><startdate>20101201</startdate><enddate>20101201</enddate><creator>李小凡(Xiaofan Li)</creator><general>Journal of Chinese Linguistics Publication Office</general><scope>188</scope></search><sort><creationdate>20101201</creationdate><title>蘇州方言連讀變調的共時層面和歴史層次</title><author>李小凡(Xiaofan Li)</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-airiti_journals_P20181128001_201012_201811290012_201811290012_21_323</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2010</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>李小凡(Xiaofan Li)</creatorcontrib><collection>Airiti Library</collection><jtitle>Journal of Chinese Linguistics Monograph Series</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>李小凡(Xiaofan Li)</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>蘇州方言連讀變調的共時層面和歴史層次</atitle><jtitle>Journal of Chinese Linguistics Monograph Series</jtitle><date>2010-12-01</date><risdate>2010</risdate><issue>24</issue><spage>21</spage><epage>32</epage><pages>21-32</pages><issn>2409-2878</issn><abstract>蘇州方言有兩種連讀變調:(1)以後字爲基字的語音變調,(2)以前字爲基字的音義變調。音義變調的後字高度中和,連調式廣泛漂移並導致單字調竄調,連調規則跟語音變調截然不同。兩種連調分屬不同的共時層面,又是發生於不同時期的歷史層次。語音變調早期是主層,音義變調則是從語音變調中衍生的創新變層。音義變調最初產生於動詞體貌結構、動詞重疊式、數量結構等語法單位,然後向其他語法、詞彙單位擴散,目前已成爲蘇州方言連調式的主層,語音變調則降爲滯後的變層。音義變調的衍生過程類似詞彙單位的語法化。</abstract><pub>Journal of Chinese Linguistics Publication Office</pub><tpages>12</tpages></addata></record>
fulltext fulltext
identifier ISSN: 2409-2878
ispartof Journal of Chinese Linguistics Monograph Series, 2010-12 (24), p.21-32
issn 2409-2878
language chi
recordid cdi_airiti_journals_P20181128001_201012_201811290012_201811290012_21_32
source JSTOR
title 蘇州方言連讀變調的共時層面和歴史層次
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-20T08%3A02%3A00IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-airiti&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=%E8%98%87%E5%B7%9E%E6%96%B9%E8%A8%80%E9%80%A3%E8%AE%80%E8%AE%8A%E8%AA%BF%E7%9A%84%E5%85%B1%E6%99%82%E5%B1%A4%E9%9D%A2%E5%92%8C%E6%AD%B4%E5%8F%B2%E5%B1%A4%E6%AC%A1&rft.jtitle=Journal%20of%20Chinese%20Linguistics%20Monograph%20Series&rft.au=%E6%9D%8E%E5%B0%8F%E5%87%A1(Xiaofan%20Li)&rft.date=2010-12-01&rft.issue=24&rft.spage=21&rft.epage=32&rft.pages=21-32&rft.issn=2409-2878&rft_id=info:doi/&rft_dat=%3Cairiti%3EP20181128001_201012_201811290012_201811290012_21_32%3C/airiti%3E%3Cgrp_id%3Ecdi_FETCH-airiti_journals_P20181128001_201012_201811290012_201811290012_21_323%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rft_airiti_id=P20181128001_201012_201811290012_201811290012_21_32&rfr_iscdi=true