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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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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
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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