2020
DOI: 10.1088/1361-6552/ab9480
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The anomalous thermal expansion of water

Abstract: The anomalous thermal expansion of water in the 0 °C–4 °C range is extremely important to life on Earth, but it is normally not presented experimentally in educational settings. This paper presents a simple experiment to explore the anomalous thermal expansion of water in the 0 °C–4 °C range and the heat exchange processes in natural bodies of water in the winter and spring.

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Cited by 3 publications
(6 citation statements)
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“…to form soils. [101] The detailed mechanism of this anomalous temperature dependence of water density remains still a matter of debate. [102] This water anomaly at 4 °C also has observable effects on luminescent materials.…”
Section: Water Anomaliesmentioning
confidence: 99%
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“…to form soils. [101] The detailed mechanism of this anomalous temperature dependence of water density remains still a matter of debate. [102] This water anomaly at 4 °C also has observable effects on luminescent materials.…”
Section: Water Anomaliesmentioning
confidence: 99%
“…This anomaly alters the convection mechanism of water at low temperatures and has significant effects in nature, for example, it influences the preservation of ecosystems in frozen lakes and promotes erosion of porous rocks to form soils. [ 101 ] The detailed mechanism of this anomalous temperature dependence of water density remains still a matter of debate. [ 102 ] This water anomaly at 4 °C also has observable effects on luminescent materials.…”
Section: Water Anomaliesmentioning
confidence: 99%
“…In this case seawater heated near its freezing point becomes lighter than the surroundings and hence rises. In contrast, at lower salinities, heating of water close to freezing temperatures, actually makes water denser, due to the anomalous expansion of near-freezing water (Ede, 1956;Ivanov & Nikolov, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…With this assumption, seawater heated near its freezing point becomes lighter than the surroundings and hence rises. In contrast, at lower salinities (about half of Earth's ocean salinity), heating of water close to freezing temperatures, actually makes water denser, due to the anomalous expansion of near‐freezing water (Ede, 1956; Ivanov & Nikolov, 2020). As first discussed by Melosh et al.…”
Section: Introductionmentioning
confidence: 99%
“…With this assumption, seawater heated near its freezing point becomes lighter than the surroundings and hence rises. In contrast, at lower salinities (about half of Earth's ocean salinity), heating of water close to freezing temperatures, actually makes water denser, due to the anomalous expansion of near-freezing water (Ede, 1956;Ivanov & Nikolov, 2020). As first discussed by Melosh et al (2004), if the ocean is sufficiently fresh a pool of increasingly warm but dense water can form at the base of the ocean and inhibit convection from directly reaching the upper light layer.…”
mentioning
confidence: 99%