Results 21 to 30 of about 232,915 (212)
Chemistry Teacher International, 2023 In this paper, the cooling effect of alternative ice cubes made of granite, soapstone and ceramic is experimentally examined with the help of a digital temperature sensor and compared with that of a conventional ice cube.
Fleischer Timo +3 more
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Glaciochemistry of Cave Ice: Paradana and Snežna Caves, Slovenia
Geosciences, 2019 Cave ice samples collected within karstic terrain have major ion and nutrient concentrations showing that the ice originates from local precipitation modified by the addition of Ca2+ and HCO3− from the dissolution of the local bedrock.
Anne E. Carey +7 more
doaj +1 more source
Variability in sea ice carbonate chemistry: a case study comparing the importance of ikaite precipitation, bottom-ice algae, and currents across an invisible polynya [PDF]
The Cryosphere, 2022 The carbonate chemistry of sea ice is known to play a role in global carbon cycles, but its importance is uncertain in part due to disparities in reported results.
B. G. T. Else +11 more
doaj +1 more source
Ice core chemistry of Vestfonna Ice Cap in Svalbard, Norway [PDF]
Journal of Geophysical Research: Atmospheres, 2002 Chemical analyses were done on samples from a 2.2‐m deep snow pit and a 211‐m deep ice core that came from the top of the Vestfonna Ice Cap in Nordaustlandet, Svalbard, Norway. The snow pit samples showed that the temperature increased during the winter owing to advection of warm air from the south, and δ18O did not show a seasonal cycle. Chronology of
Sumito Matoba +4 more
openaire +1 more source
, 2020 Ice III is a hydrogen-disordered phase of ice that is stable between about 0.2 and 0.35 GPa. Upon cooling, it transforms to its hydrogen-ordered counterpart ice IX within the stability region of ice II.
Craig L., Bull +4 more
core +1 more source
Atmospheric impact of the 1783-1784 Laki eruption: Part I Chemistry modelling. [PDF]
, 2003 Results from the first chemistry-transport model study of the impact of the 1783–1784 Laki fissure eruption (Iceland: 64°N, 17°W) upon atmospheric composition are presented.
Stevenson, D. S.; id_orcid +17 more
core +1 more source
ICE CHEMISTRY IN STARLESS MOLECULAR CORES [PDF]
The Astrophysical Journal, 2015 Starless molecular cores are natural laboratories for interstellar molecular chemistry research. The chemistry of ices in such objects was investigated with a three-phase (gas, surface, and mantle) model. We considered the center part of five starless cores, with their physical conditions derived from observations. The ice chemistry of oxygen, nitrogen,
openaire +2 more sources
Development of a Bioaerosol single particle detector (BIO IN) for the Fast Ice Nucleus CHamber FINCH [PDF]
, 2010 In this work we present the setup and first tests of our new BIO IN detector. This detector was constructed to classify atmospheric ice nuclei (IN) for their biological content. It is designed to be coupled to the Fast Ice Nucleus CHamber FINCH.
U. Bundke +9 more
core +1 more source
The anomalous pressure drop behaviour of ice slurries flowing through constrictions [PDF]
, 2008 The effective ‘viscosity’ for ice slurry containing more than say 30 to 40% ice fraction is many orders of magnitude higher than that for water. However, this work suggests that such slurries, when flowing through constrictions, can incur lower pressure ...
Rhys, T. D. L. +3 more
core +1 more source
Journal of Glaciology, 2018 Past atmospheric pollution can be reconstructed from ice core trace element records retrieved from mountain glaciers. However, the current global temperature increase can result in post-depositional melt processes, significantly altering the originally ...
SVEN ERIK AVAK +2 more
doaj +1 more source