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Environmental record of layers of bubbles in natural pond ice

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F18%3A10381774" target="_blank" >RIV/00216208:11310/18:10381774 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/18:00501241

  • Result on the web

    <a href="https://doi.org/10.1017/jog.2018.73" target="_blank" >https://doi.org/10.1017/jog.2018.73</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1017/jog.2018.73" target="_blank" >10.1017/jog.2018.73</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Environmental record of layers of bubbles in natural pond ice

  • Original language description

    Autonomous temperature data loggers were used to measure the temperature profile within a growing ice cover and in the water below. The ice formed under natural conditions over the pond. We observed the presence of distinct layers of gas bubbles throughout the ice thickness. Temperature measurements allowed us to determine growth rates (μm s-1) and cooling rates (°C s-1) of the ice and demonstrated that these bubble layers formed during the peak ice growth rates from 0.58 to 0.92 μm s-1. The growth rates, leading to the formation of layers of bubbles, were more than an order of magnitude lower than for bubbles produced in controlled laboratory conditions (from 3 to 80 μm s-1). This observation introduces the possibility that solid impurities play a role in natural waters and that they must lower the limit of growth rates required for bubble occurrence. Data revealed a decrease in ice growth rates while cooling rates increased. We interpret this observation as an effect of the heat flux from the water to the ice (8.34-34.11 W m-2), and of gas concentration changes in the water below. Calculations of the ice thickness using traditional methods showed the necessity to include the heat flux from the water to the ice and the effect of gas bubbles within the ice and near the ice-water interface.

  • 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

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GA17-05935S" target="_blank" >GA17-05935S: Role of changes in environemntal chemistry on lake ecosystems at the Younger Dryas onset</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2018

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Journal of Glaciology

  • ISSN

    0022-1430

  • e-ISSN

  • Volume of the periodical

    64

  • Issue of the periodical within the volume

    248

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    26

  • Pages from-to

    866-876

  • UT code for WoS article

    000454427700002

  • EID of the result in the Scopus database

    2-s2.0-85054986051