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Freezing-induced acidification of sea ice brine

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985904%3A_____%2F24%3A00587907" target="_blank" >RIV/67985904:_____/24:00587907 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/24:00137406

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0048969724043420?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0048969724043420?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.scitotenv.2024.174194" target="_blank" >10.1016/j.scitotenv.2024.174194</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Freezing-induced acidification of sea ice brine

  • Original language description

    The acidity of sea ice and snow plays a key role in the chemistry of the cryosphere, an important example lies in the photochemical catalytic release of reactive bromine in polar regions, facilitated at pHs below 6.5. We apply in-situ acid-base indicators to probe the microscopic acidity of the brine within the ice matrix in artificial sea water at a range of concentrations (0.35-70 PPT) and initial pHs (6-9). The results are supported by analogous measurements of the most abundant salts in seawater: NaCl, Na2SO4, and CaCO3. In the research herein, the acidity is expressed in terms of the Hammett acidity function, H2- . The obtained results show a pronounced acidity increase in sea water after freezing at -15 degrees C and during the subsequent cooling down to -50 degrees C. Importantly, we did not observe any significant hysteresis, the values of acidity upon warming markedly resembled those at the corresponding temperatures at cooling. The acidity increase is attributed to the minerals' crystallization, which is accompanied by a loss of the buffering capacity. Our observations show that lower salinity sea water samples (<= 3.5 PPT) reach pH values below 6.5 at the temperature of -15 degrees C, whereas higher salinity ices attain such values only at -30 degrees C. The ensuing implications for polar chemistry and the relevance to the field measurements are discussed.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10613 - Zoology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Science of the Total Environment

  • ISSN

    0048-9697

  • e-ISSN

    1879-1026

  • Volume of the periodical

    946

  • Issue of the periodical within the volume

    OCT 10

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    14

  • Pages from-to

    174194

  • UT code for WoS article

    001266508700001

  • EID of the result in the Scopus database

    2-s2.0-85196803827