Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater
Abstract We observed the initial release rate of metals from four fresh (i.e., without long time exposure to the atmosphere) hydrothermal sulfide cores into artificial seawater. The sulfide samples were collected by seafloor drilling from the Okinawa Trough by D/V Chikyu, powdered under inert gas, a...
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doaj-9b8d2efa4ecb4d648511801931c367a02020-11-25T00:53:44ZengBMCGeochemical Transactions1467-48662018-12-0119111510.1186/s12932-018-0060-9Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawaterShigeshi Fuchida0Jun-ichiro Ishibashi1Kazuhiko Shimada2Tatsuo Nozaki3Hidenori Kumagai4Masanobu Kawachi5Yoshitaka Matsushita6Hiroshi Koshikawa7Marine Environment Section, Center for Regional Environmental Research, National Institute for Environmental Studies (NIES)Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu UniversityDepartment of Earth and Planetary Sciences, Faculty of Sciences, Kyushu UniversityResearch and Development (R&D) Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)Research and Development (R&D) Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)Biodiversity Resource Conservation Office, Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies (NIES)Research Network and Facility Services Division, The National Institute for Materials Science (NIMS)Marine Environment Section, Center for Regional Environmental Research, National Institute for Environmental Studies (NIES)Abstract We observed the initial release rate of metals from four fresh (i.e., without long time exposure to the atmosphere) hydrothermal sulfide cores into artificial seawater. The sulfide samples were collected by seafloor drilling from the Okinawa Trough by D/V Chikyu, powdered under inert gas, and immediately subjected to onboard metal-leaching experiments at different temperatures (5 °C and 20 °C), and under different redox conditions (oxic and anoxic), for 1–30 h. Zinc and Pb were preferentially released from sulfide samples containing various metals (i.e., Mn, Fe, Cu, Zn, Cd, and Pb) into seawater. Under oxic experimental conditions, Zn and Pb dissolution rates from two sulfide samples composed mainly of iron disulfide minerals (pyrite and marcasite) were higher than those from two other sulfide samples with abundant sphalerite, galena, and/or silicate minerals. Scanning electron microscopy confirmed that the high metal-releasing sample contained several galvanic couples of iron disulfide with other sulfide minerals, whereas the low metal-releasing sample contained fewer galvanic couples or were coated by a silicate mineral. The experiments overall confirmed that the galvanic effects with iron disulfide minerals greatly induce the initial release of Zn and Pb from hydrothermal sulfides into seawater, especially under warm oxic conditions.http://link.springer.com/article/10.1186/s12932-018-0060-9Onboard leaching experimentHydrothermal sulfidesMetal contaminationSMS-miningMarine environmental impacts assessment |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Shigeshi Fuchida Jun-ichiro Ishibashi Kazuhiko Shimada Tatsuo Nozaki Hidenori Kumagai Masanobu Kawachi Yoshitaka Matsushita Hiroshi Koshikawa |
spellingShingle |
Shigeshi Fuchida Jun-ichiro Ishibashi Kazuhiko Shimada Tatsuo Nozaki Hidenori Kumagai Masanobu Kawachi Yoshitaka Matsushita Hiroshi Koshikawa Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater Geochemical Transactions Onboard leaching experiment Hydrothermal sulfides Metal contamination SMS-mining Marine environmental impacts assessment |
author_facet |
Shigeshi Fuchida Jun-ichiro Ishibashi Kazuhiko Shimada Tatsuo Nozaki Hidenori Kumagai Masanobu Kawachi Yoshitaka Matsushita Hiroshi Koshikawa |
author_sort |
Shigeshi Fuchida |
title |
Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
title_short |
Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
title_full |
Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
title_fullStr |
Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
title_full_unstemmed |
Onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
title_sort |
onboard experiment investigating metal leaching of fresh hydrothermal sulfide cores into seawater |
publisher |
BMC |
series |
Geochemical Transactions |
issn |
1467-4866 |
publishDate |
2018-12-01 |
description |
Abstract We observed the initial release rate of metals from four fresh (i.e., without long time exposure to the atmosphere) hydrothermal sulfide cores into artificial seawater. The sulfide samples were collected by seafloor drilling from the Okinawa Trough by D/V Chikyu, powdered under inert gas, and immediately subjected to onboard metal-leaching experiments at different temperatures (5 °C and 20 °C), and under different redox conditions (oxic and anoxic), for 1–30 h. Zinc and Pb were preferentially released from sulfide samples containing various metals (i.e., Mn, Fe, Cu, Zn, Cd, and Pb) into seawater. Under oxic experimental conditions, Zn and Pb dissolution rates from two sulfide samples composed mainly of iron disulfide minerals (pyrite and marcasite) were higher than those from two other sulfide samples with abundant sphalerite, galena, and/or silicate minerals. Scanning electron microscopy confirmed that the high metal-releasing sample contained several galvanic couples of iron disulfide with other sulfide minerals, whereas the low metal-releasing sample contained fewer galvanic couples or were coated by a silicate mineral. The experiments overall confirmed that the galvanic effects with iron disulfide minerals greatly induce the initial release of Zn and Pb from hydrothermal sulfides into seawater, especially under warm oxic conditions. |
topic |
Onboard leaching experiment Hydrothermal sulfides Metal contamination SMS-mining Marine environmental impacts assessment |
url |
http://link.springer.com/article/10.1186/s12932-018-0060-9 |
work_keys_str_mv |
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