Publication Date:
2024-02-07
Description:
Highlights
• Mercury fulminate dissolves rapidly when it comes in contact with seawater
• Dissolution rates are highly temperature dependent
• Dissolution rates are salinity dependent only at lower temperatures
• Historical munitions with mercury fulminate could be a mercury pollution source
• Warming environments will aid mercury fulminate release from relic munitions
Abstract
Mercury fulminate (HgFu) was used as an initial detonator for World War I and II munitions. Its presence in previously discarded and dumped munitions could potentially supply mercury pollution into coastal ecosystems where bygone weaponries reside. There is evidence that historical munitions have already contributed mercury pollution in coastal environments, and millions remain embedded in sediments and subjected to further weakening via corrosion under environmental conditions. Experiments were undertaken assessing HgFu dissolution under varying temperature and salinity conditions to constrain controls on mercury release into marine environments. Our results show that HgFu discharge is strongly temperature dependent, with dissolution rate constants increasing from ∼0.4 mg cm−2 d−1 at 5 °C to ∼2.7 mg cm−2 d−1 at 30 °C. No significant differences were observed between freshwater and seawaters up to 36 psu, except at 5 °C. These experiments provide a basis for modeling HgFu release from underwater munitions and its dynamics in coastal environments.
Type:
Article
,
PeerReviewed
Format:
text
Format:
text
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