{"title":"Compressibility of distilled water and seawater","authors":"Alvin Bradshaw , Karl Schleicher","doi":"10.1016/0011-7471(76)90002-4","DOIUrl":null,"url":null,"abstract":"<div><p>The compressions of distilled water and of seawater of approximately 31, 35, and 39% salinity were measured at 10°C for pressures up to 1000 bars. The data were summarized by a ‘best’ least-square fit polynomial in pressure and salinity. The summary formula was combined with<span>Bryden's</span> (<em>Deep-Sea Research</em>,<strong>20</strong>, 401–408, 1973) similar type fit to our earlier thermal expansion data (<span>Bradshaw</span> and<span>Schleicher</span>, <em>Deep-Sea Research</em>,<strong>17</strong>, 691–706, 1970) and<span>Fofonoff</span> and<span>Bryden's</span> (<em>Journal of Marine Research</em>, in press) recent empirical formula for sigma-0 of seawater to give an expression for the specific volume of seawater as a function of temperature, pressure and salinity in the salinity range 31 to 39%. At 35% specific volumes from this expression in the oceanographic range of temperature and pressure agree within 15 × 10<sup>−6</sup>cm<sup>3</sup>g<sup>−1</sup> with those computed using sound velocities (<span>Wang</span> and<span>Millero</span>, <em>Journal of Geophysical and Research</em>,<strong>78</strong>, 7122–7128, 1973). Our mean compressibilities for distilled water at 10°C also agree with those from sound velocities (to within 0·05%) but disagree with those of<span>Kell</span> and<span>Whalley</span> (<em>Philosophical Transactions of the Royal Society of London</em>, A,<strong>258</strong>, 565–614, 1965) by about 0·3%.</p></div>","PeriodicalId":11253,"journal":{"name":"Deep Sea Research and Oceanographic Abstracts","volume":"23 7","pages":"Pages 583-593"},"PeriodicalIF":0.0000,"publicationDate":"1976-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0011-7471(76)90002-4","citationCount":"24","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep Sea Research and Oceanographic Abstracts","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0011747176900024","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 24
Abstract
The compressions of distilled water and of seawater of approximately 31, 35, and 39% salinity were measured at 10°C for pressures up to 1000 bars. The data were summarized by a ‘best’ least-square fit polynomial in pressure and salinity. The summary formula was combined withBryden's (Deep-Sea Research,20, 401–408, 1973) similar type fit to our earlier thermal expansion data (Bradshaw andSchleicher, Deep-Sea Research,17, 691–706, 1970) andFofonoff andBryden's (Journal of Marine Research, in press) recent empirical formula for sigma-0 of seawater to give an expression for the specific volume of seawater as a function of temperature, pressure and salinity in the salinity range 31 to 39%. At 35% specific volumes from this expression in the oceanographic range of temperature and pressure agree within 15 × 10−6cm3g−1 with those computed using sound velocities (Wang andMillero, Journal of Geophysical and Research,78, 7122–7128, 1973). Our mean compressibilities for distilled water at 10°C also agree with those from sound velocities (to within 0·05%) but disagree with those ofKell andWhalley (Philosophical Transactions of the Royal Society of London, A,258, 565–614, 1965) by about 0·3%.