Using Mercury Stable Isotopes to Quantify Bidirectional Water-Atmosphere Hg(0) Exchange Fluxes and Explore Controlling Factors
In this study, exchange fluxes and Hg isotope fractionation during water-atmosphere Hg(0) exchange were investigated at three lakes in China. Water-atmosphere exchange was overall characterized by net Hg(0) emissions, with lake-specific mean exchange fluxes ranging from 0.9 to 1.8 ng m-2 h-1, which produced negative δ202Hg (mean: -1.61 to -0.03‰) and Δ199Hg (-0.34 to -0.16‰) values. Emission-controlled experiments conducted using Hg-free air over the water surface at Hongfeng lake (HFL) showed negative δ202Hg and Δ199Hg in Hg(0) emitted from water, and similar values were observed between daytime (mean δ202Hg: -0.95‰, Δ199Hg: -0.25‰) and nighttime (δ202Hg: -1.00‰, Δ199Hg: -0.26‰). Results of the Hg isotope suggest that Hg(0) emission from water is mainly controlled by photochemical Hg(0) production in water. Deposition-controlled experiments at HFL showed that heavier Hg(0) isotopes (mean ε202Hg: -0.38‰) preferentially deposited to water, likely indicating an important role of aqueous Hg(0) oxidation played during the deposition process. A Δ200Hg mixing model showed that lake-specific mean emission fluxes from water surfaces were 2.1-4.1 ng m-2 h-1 and deposition fluxes to water surfaces were 1.2-2.3 ng m-2 h-1 at the three lakes. Results from the this study indicate that atmospheric Hg(0) deposition to water surfaces indeed plays an important role in Hg cycling between atmosphere and water bodies.
Medienart: |
E-Artikel |
---|
Erscheinungsjahr: |
2023 |
---|---|
Erschienen: |
2023 |
Enthalten in: |
Zur Gesamtaufnahme - volume:57 |
---|---|
Enthalten in: |
Environmental science & technology - 57(2023), 29 vom: 25. Juli, Seite 10673-10685 |
Sprache: |
Englisch |
---|
Beteiligte Personen: |
Zhang, Hui [VerfasserIn] |
---|
Links: |
---|
Themen: |
− |
---|
Anmerkungen: |
Date Completed 26.07.2023 Date Revised 26.07.2023 published: Print-Electronic Citation Status MEDLINE |
---|
doi: |
10.1021/acs.est.3c01273 |
---|
funding: |
|
---|---|
Förderinstitution / Projekttitel: |
|
PPN (Katalog-ID): |
NLM358799570 |
---|
LEADER | 01000naa a22002652 4500 | ||
---|---|---|---|
001 | NLM358799570 | ||
003 | DE-627 | ||
005 | 20231226075516.0 | ||
007 | cr uuu---uuuuu | ||
008 | 231226s2023 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.1021/acs.est.3c01273 |2 doi | |
028 | 5 | 2 | |a pubmed24n1195.xml |
035 | |a (DE-627)NLM358799570 | ||
035 | |a (NLM)37378655 | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
100 | 1 | |a Zhang, Hui |e verfasserin |4 aut | |
245 | 1 | 0 | |a Using Mercury Stable Isotopes to Quantify Bidirectional Water-Atmosphere Hg(0) Exchange Fluxes and Explore Controlling Factors |
264 | 1 | |c 2023 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ƒaComputermedien |b c |2 rdamedia | ||
338 | |a ƒa Online-Ressource |b cr |2 rdacarrier | ||
500 | |a Date Completed 26.07.2023 | ||
500 | |a Date Revised 26.07.2023 | ||
500 | |a published: Print-Electronic | ||
500 | |a Citation Status MEDLINE | ||
520 | |a In this study, exchange fluxes and Hg isotope fractionation during water-atmosphere Hg(0) exchange were investigated at three lakes in China. Water-atmosphere exchange was overall characterized by net Hg(0) emissions, with lake-specific mean exchange fluxes ranging from 0.9 to 1.8 ng m-2 h-1, which produced negative δ202Hg (mean: -1.61 to -0.03‰) and Δ199Hg (-0.34 to -0.16‰) values. Emission-controlled experiments conducted using Hg-free air over the water surface at Hongfeng lake (HFL) showed negative δ202Hg and Δ199Hg in Hg(0) emitted from water, and similar values were observed between daytime (mean δ202Hg: -0.95‰, Δ199Hg: -0.25‰) and nighttime (δ202Hg: -1.00‰, Δ199Hg: -0.26‰). Results of the Hg isotope suggest that Hg(0) emission from water is mainly controlled by photochemical Hg(0) production in water. Deposition-controlled experiments at HFL showed that heavier Hg(0) isotopes (mean ε202Hg: -0.38‰) preferentially deposited to water, likely indicating an important role of aqueous Hg(0) oxidation played during the deposition process. A Δ200Hg mixing model showed that lake-specific mean emission fluxes from water surfaces were 2.1-4.1 ng m-2 h-1 and deposition fluxes to water surfaces were 1.2-2.3 ng m-2 h-1 at the three lakes. Results from the this study indicate that atmospheric Hg(0) deposition to water surfaces indeed plays an important role in Hg cycling between atmosphere and water bodies | ||
650 | 4 | |a Journal Article | |
650 | 4 | |a Research Support, Non-U.S. Gov't | |
650 | 4 | |a MDF | |
650 | 4 | |a MIF | |
650 | 4 | |a atmosphere Hg(0) exchange | |
650 | 4 | |a deposition | |
650 | 4 | |a emission | |
650 | 4 | |a lakes | |
650 | 4 | |a stable Hg isotope | |
650 | 4 | |a water | |
650 | 4 | |a − | |
650 | 7 | |a Mercury Isotopes |2 NLM | |
650 | 7 | |a Water |2 NLM | |
650 | 7 | |a 059QF0KO0R |2 NLM | |
650 | 7 | |a Mercury |2 NLM | |
650 | 7 | |a FXS1BY2PGL |2 NLM | |
650 | 7 | |a Isotopes |2 NLM | |
700 | 1 | |a Fu, Xuewu |e verfasserin |4 aut | |
700 | 1 | |a Wu, Xian |e verfasserin |4 aut | |
700 | 1 | |a Deng, Qianwen |e verfasserin |4 aut | |
700 | 1 | |a Tang, Kaihui |e verfasserin |4 aut | |
700 | 1 | |a Zhang, Leiming |e verfasserin |4 aut | |
700 | 1 | |a Sommar, Jonas |e verfasserin |4 aut | |
700 | 1 | |a Sun, Guangyi |e verfasserin |4 aut | |
700 | 1 | |a Feng, Xinbin |e verfasserin |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Environmental science & technology |d 1967 |g 57(2023), 29 vom: 25. Juli, Seite 10673-10685 |w (DE-627)NLM112374735 |x 1520-5851 |7 nnns |
773 | 1 | 8 | |g volume:57 |g year:2023 |g number:29 |g day:25 |g month:07 |g pages:10673-10685 |
856 | 4 | 0 | |u http://dx.doi.org/10.1021/acs.est.3c01273 |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a GBV_NLM | ||
951 | |a AR | ||
952 | |d 57 |j 2023 |e 29 |b 25 |c 07 |h 10673-10685 |