Silver in Tokyo Bay Estuarine Waters and Japanese Rivers
スポンサーリンク
概要
- 論文の詳細を見る
- Oceanographic Society of Japanの論文
- 2008-04-01
著者
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Gamo Toshitaka
Ocean Research Institute The University Of Tokyo
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Gamo Toshitaka
Ocean Research Institute University Of Tokyo
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Obata Hajime
Ocean Research Institute (ori) The University Of Tokyo
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Zhang Yan
Legos
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Gamo Toshitaka
Ocean Research Institute (ORI), The University of Tokyo
関連論文
- Onboard Determination of Submicromolar Nitrate in Seawater by Anion-Exchange Chromatography with Lithium Chloride Eluent
- Evidence for the Grazing Hypothesis : Grazing Reduces Phytoplankton Responses of the HNLC Ecosystem to Iron Enrichment in the Western Subarctic Pacific (SEEDS II)
- Tectonic pumping: earthquake-induced chemical flux detected in situ by a submarine cable experiment in Sagami Bay, Japan
- Discovery of a new hydrothermal venting site in the southernmost Mariana Arc: Al-rich hydrothermal plumes and white smoker activity associated with biogenic methane
- In-situ Survey of Nanomolar Manganese in Seawater Using an Autonomous Underwater Vehicle around a Volcanic Crater at Teishi Knoll, Sagami Bay, Japan
- Contribution of heat outputs from high- and low-temperature hydrothermal sources to the neutrally buoyant plume at the TAG hydrothermal mound, Mid-Atlantic Ridge
- Iron, Manganese and Aluminum in Upper Waters of the Western South Pacific Ocean and Its Adjacent Seas
- Helium Isotopes of Seawater in the Japan Sea
- Stability of Amino Acids in Simulated Hydrothermal Vent Environments
- Helium isotopes in South Pacific deep seawater
- Hydrogen Effect on the δ^C Value of CO_2 Measured by Mass Spectrometry with Electron-Impact Ionization
- Spatial Variations of Rare Earth Elements in North Pacific Surface Water
- Gas geochemical characteristics of hydrothermal plumes at the HAKUREI and JADE vent sites, the Izena Cauldron, Okinawa Trough
- Rare Earth Elements in the hydrothermal system at Okinawa Trough back-arc basin
- Hydrothermal fluid geochemistry at the Iheya North field in the mid-Okinawa Trough : Implication for origin of methane in subseafloor fluid circulation systems
- Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough
- O_2 Consumption Rate and Its Isotopic Fractionation Factor in the Deep Water of the Philippine Sea
- Silver in Tokyo Bay Estuarine Waters and Japanese Rivers