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Bioindication of volcanic mercury (Hg) deposition around Mt. Etna (Sicily)
Language
English
Status
Published
JCR Journal
JCR Journal
Title of the book
Issue/vol(year)
/310-311 (2012)
ISSN
0009-2541
Publisher
Elsevier
Pages (printed)
12-22
Issued date
2012
Subjects
Abstract
Mt. Etna is a major natural source of Hg to the Mediterranean region. Total mercury concentrations, [Hg]tot,in
Castanea sativa (sweet chestnut) leaves sampled 7–13 km from Etna's vents (during six campaigns in
2005–2011) were determined using atomic absorption spectroscopy. [Hg]tot in C. sativa was greatest on
Etna's SE flank reflecting Hg deposition from the typically overhead volcanic plume. [Hg]tot also showed Hg
accumulation over the growing season, increasing with leaf age and recent eruptive activity. [Hg]tot in C.
sativa was not controlled by [Hg]tot in soils, which instead was greatest on Etna's NW flank, and was
correlated with the proportion of organic matter in the soil (% Org). An elevated [Hg]tot/% Org ratio in soils on
Etna's SE flank is indicative of increased Hg deposition. This ratio was also found to decrease with local soil
pH, suggesting that Hg deposited to the low pH and organic-poor soils on Etna's SE flank may not be retained
but will instead be released to groundwater or re-emitted to the atmosphere. These results show that the
deposition of volcanic Hg has clear impacts and confirm that Etna is an important source of Hg to the local
environment.
Castanea sativa (sweet chestnut) leaves sampled 7–13 km from Etna's vents (during six campaigns in
2005–2011) were determined using atomic absorption spectroscopy. [Hg]tot in C. sativa was greatest on
Etna's SE flank reflecting Hg deposition from the typically overhead volcanic plume. [Hg]tot also showed Hg
accumulation over the growing season, increasing with leaf age and recent eruptive activity. [Hg]tot in C.
sativa was not controlled by [Hg]tot in soils, which instead was greatest on Etna's NW flank, and was
correlated with the proportion of organic matter in the soil (% Org). An elevated [Hg]tot/% Org ratio in soils on
Etna's SE flank is indicative of increased Hg deposition. This ratio was also found to decrease with local soil
pH, suggesting that Hg deposited to the low pH and organic-poor soils on Etna's SE flank may not be retained
but will instead be released to groundwater or re-emitted to the atmosphere. These results show that the
deposition of volcanic Hg has clear impacts and confirm that Etna is an important source of Hg to the local
environment.
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article
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2012_Bioindication of volcanic mercury (Hg) deposition around Mt. Etna (Sicily)_Chemical Geology.pdf
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