Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C

<p/> <p>We conducted reversed deliquescence experiments in saturated NaCl–NaNO<sub>3</sub>–H<sub>2</sub>O, KNO<sub>3</sub>–NaNO<sub>3</sub>–H<sub>2</sub>O, and NaCl–KNO<sub>3</sub>–H<sub>2</sub>O systems...

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Main Authors: Wolery Thomas J, Craig Laura, Carroll Susan
Format: Article
Language:English
Published: BMC 2005-04-01
Series:Geochemical Transactions
Online Access:http://dx.doi.org/10.1186/1467-4866-6-19
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author Wolery Thomas J
Craig Laura
Carroll Susan
author_facet Wolery Thomas J
Craig Laura
Carroll Susan
author_sort Wolery Thomas J
collection DOAJ
description <p/> <p>We conducted reversed deliquescence experiments in saturated NaCl–NaNO<sub>3</sub>–H<sub>2</sub>O, KNO<sub>3</sub>–NaNO<sub>3</sub>–H<sub>2</sub>O, and NaCl–KNO<sub>3</sub>–H<sub>2</sub>O systems from 90 to 120°C as a function of relative humidity and solution composition. NaCl, NaNO<sub>3</sub>, and KNO<sub>3 </sub>represent members of dust salt assemblages that are likely to deliquesce and form concentrated brines on high-level radioactive waste package surfaces in a repository environment at Yucca Mountain, NV. Discrepancy between model prediction and experiment can be as high as 8% for relative humidity and 50% for dissolved ion concentration. The discrepancy is attributed primarily to the use of 25°C models for Cl–NO<sub>3 </sub>and K–NO<sub>3 </sub>ion interactions in the current Yucca Mountain Project high-temperature Pitzer model to describe the nonideal behavior of these highly concentrated solutions.</p>
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spelling doaj.art-a0ee803ddd7c4b7693e1b4b5b46159932022-12-22T02:58:02ZengBMCGeochemical Transactions1467-48662005-04-01621910.1186/1467-4866-6-19Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°CWolery Thomas JCraig LauraCarroll Susan<p/> <p>We conducted reversed deliquescence experiments in saturated NaCl–NaNO<sub>3</sub>–H<sub>2</sub>O, KNO<sub>3</sub>–NaNO<sub>3</sub>–H<sub>2</sub>O, and NaCl–KNO<sub>3</sub>–H<sub>2</sub>O systems from 90 to 120°C as a function of relative humidity and solution composition. NaCl, NaNO<sub>3</sub>, and KNO<sub>3 </sub>represent members of dust salt assemblages that are likely to deliquesce and form concentrated brines on high-level radioactive waste package surfaces in a repository environment at Yucca Mountain, NV. Discrepancy between model prediction and experiment can be as high as 8% for relative humidity and 50% for dissolved ion concentration. The discrepancy is attributed primarily to the use of 25°C models for Cl–NO<sub>3 </sub>and K–NO<sub>3 </sub>ion interactions in the current Yucca Mountain Project high-temperature Pitzer model to describe the nonideal behavior of these highly concentrated solutions.</p>http://dx.doi.org/10.1186/1467-4866-6-19
spellingShingle Wolery Thomas J
Craig Laura
Carroll Susan
Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
Geochemical Transactions
title Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
title_full Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
title_fullStr Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
title_full_unstemmed Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
title_short Deliquescence of NaCl–NaNO<sub>3</sub>, KNO<sub>3</sub>–NaNO<sub>3</sub>, and NaCl–KNO<sub>3 </sub>salt mixtures from 90 to 120°C
title_sort deliquescence of nacl nano sub 3 sub kno sub 3 sub nano sub 3 sub and nacl kno sub 3 sub salt mixtures from 90 to 120°c
url http://dx.doi.org/10.1186/1467-4866-6-19
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