Article(id=1325116777109266639, tenantId=1146029695717560320, journalId=1255847867265597444, issueId=1325115579346059524, articleNumber=null, orderNo=null, doi=null, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1328371200000, receivedDateStr=2012-02-05, revisedDate=1330876800000, revisedDateStr=2012-03-05, acceptedDate=null, acceptedDateStr=null, onlineDate=1793862059142, onlineDateStr=2026-11-05, pubDate=1376496000000, pubDateStr=2013-08-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793862059142, onlineIssueDateStr=2026-11-05, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793862059142, creator=13701087609, updateTime=1793862059142, updator=13701087609, issue=Issue{id=1325115579346059524, tenantId=1146029695717560320, journalId=1255847867265597444, year='2013', volume='27', issue='4', pageStart='473', pageEnd='632', issueExtLink='null', onlineDate='null', pubDate='1376496000000', pubDateStr='2013-08-15', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793861773573, creator='13701087609', updateTime=1793861773573, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=490, endPage=494, ext={EN=ArticleExt(id=1325116777495142608, articleId=1325116777109266639, tenantId=1146029695717560320, journalId=1255847867265597444, language=EN, title=Liquid-Liquid Phase Transition of Water at High Pressure and Ambient Temperature, columnId=null, journalTitle=Chinese Journal of High Pressure Physics, columnName=null, runingTitle=null, highlight=null, articleAbstract=

In-situ Raman measurement of water has been conducted at the temperature of 300 K and the pressure of 0.1-1 400 MPa using a SiC anvil cell. The experimental results show that the frequency of liquid water ν1 decreases with increase of pressure (p), and two discontinuities are observed at about 200 and 620 MPa. Therefore three states of water are recognized. From state Ⅰ to state Ⅱ then to state III, the value of |dν1/dp| reduces, indicating that the compressibility is related to the pressure, and it is becoming more difficult to compress as the pressure is increasing. The connection mode of a water molecule with its neighboring water molecules changes as the pressure increases. The discontinuous property of water suggests a possible liquid to liquid phase transition and structural change at 200 and 620 MPa.

, authors=Hui-Yuan WANG, Hai-Fei ZHENG, authorsList=Hui-Yuan WANG, Hai-Fei ZHENG, authorCompany=null, correspAuthors=Hai-Fei ZHENG, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1325116777918767313, articleId=1325116777109266639, tenantId=1146029695717560320, journalId=1255847867265597444, language=CN, title=常温高压下水的液-液相变, columnId=0, journalTitle=高压物理学报, columnName=, runingTitle=null, highlight=null, articleAbstract=

在300 K、0.1~1 400 MPa条件下,利用碳化硅压腔,进行了液态水的拉曼光谱测量和研究。实验结果表明:随着压力的增大,水的对称伸缩振动峰(ν1)整体向低频方向移动,但在约200和620 MPa处存在不连续,可明显分为3个区间(Ⅰ、Ⅱ、Ⅲ);水从状态Ⅰ到状态Ⅱ再到状态Ⅲ,其拉曼位移对压力p的变化率(|dν1/dp|)减小,表明水变得越来越难以压缩;随着压力的改变,相邻的五水分子聚合体之间的连接方式发生了变化。这些性质表明,液态水在约200和620 MPa处可能存在着液-液相转变。

, authors=王慧媛, 郑海飞, authorsList=王慧媛, 郑海飞, authorCompany=null, correspAuthors=郑海飞, authorNote=

王慧媛(1986-),女,博士研究生,主要从事实验地球化学研究. E-mail:

, correspAuthorsNote=
郑海飞(1952-),男,教授,主要从事实验地球化学研究. E-mail:
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常温高压下水的液-液相变
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王慧媛 , 郑海飞
高压物理学报 | 2013,27(4): 490-494
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高压物理学报 | 2013 , 27 (4) : 490 -494
常温高压下水的液-液相变
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王慧媛(1986-),女,博士研究生,主要从事实验地球化学研究. E-mail:

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王慧媛 , 郑海飞
作者信息
  • 北京大学地球与空间科学学院造山带与地壳演化教育部重点实验室,北京 100871
通讯作者:
郑海飞(1952-),男,教授,主要从事实验地球化学研究. E-mail:
作者简介:

王慧媛(1986-),女,博士研究生,主要从事实验地球化学研究. E-mail:

Liquid-Liquid Phase Transition of Water at High Pressure and Ambient Temperature
Hui-Yuan WANG , Hai-Fei ZHENG
Affiliations
  • Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijng 100871, China
出版时间: 2013-08-15
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在300 K、0.1~1 400 MPa条件下,利用碳化硅压腔,进行了液态水的拉曼光谱测量和研究。实验结果表明:随着压力的增大,水的对称伸缩振动峰(ν1)整体向低频方向移动,但在约200和620 MPa处存在不连续,可明显分为3个区间(Ⅰ、Ⅱ、Ⅲ);水从状态Ⅰ到状态Ⅱ再到状态Ⅲ,其拉曼位移对压力p的变化率(|dν1/dp|)减小,表明水变得越来越难以压缩;随着压力的改变,相邻的五水分子聚合体之间的连接方式发生了变化。这些性质表明,液态水在约200和620 MPa处可能存在着液-液相转变。

高压  /  不连续  /  拉曼光谱  /  连接方式  /  液-液相变

In-situ Raman measurement of water has been conducted at the temperature of 300 K and the pressure of 0.1-1 400 MPa using a SiC anvil cell. The experimental results show that the frequency of liquid water ν1 decreases with increase of pressure (p), and two discontinuities are observed at about 200 and 620 MPa. Therefore three states of water are recognized. From state Ⅰ to state Ⅱ then to state III, the value of |dν1/dp| reduces, indicating that the compressibility is related to the pressure, and it is becoming more difficult to compress as the pressure is increasing. The connection mode of a water molecule with its neighboring water molecules changes as the pressure increases. The discontinuous property of water suggests a possible liquid to liquid phase transition and structural change at 200 and 620 MPa.

high pressure  /  discontinuity  /  Raman spectra  /  mode of connection  /  liquid-liquid phase transition
王慧媛, 郑海飞. 常温高压下水的液-液相变. 高压物理学报, 2013 , 27 (4) : 490 -494 .
Hui-Yuan WANG, Hai-Fei ZHENG. Liquid-Liquid Phase Transition of Water at High Pressure and Ambient Temperature[J]. Chinese Journal of High Pressure Physics, 2013 , 27 (4) : 490 -494 .
  • 国家自然科学基金(40873047)
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  • 接收时间:2012-02-05
  • 首发时间:2026-11-05
  • 出版时间:2013-08-15
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  • 收稿日期:2012-02-05
  • 修回日期:2012-03-05
基金
国家自然科学基金(40873047)
作者信息
    北京大学地球与空间科学学院造山带与地壳演化教育部重点实验室,北京 100871

通讯作者:

郑海飞(1952-),男,教授,主要从事实验地球化学研究. E-mail:
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