Abstract
{sup 240}Pu/{sup 239}Pu atom ratios in seawater and surface sediment collected from the northwest (NW) Pacific Ocean from 1992 to 1997 were determined using ICP-sector field mass spectrometry (ICP-MS). In whole water columns, the atom ratios of {sup 240}Pu/{sup 239}Pu were higher than the global fallout ratio (0.18). It is noted that the atom ratios of {sup 240}Pu/2{sup 39}Pu in the seawater increase with depth. Such elevated {sup 240}Pu/{sup 239}Pu atom ratios indicate that the close-in fallout plutonium isotopes originating from the Pacific Proving Grounds (PPGs) due to the U.S. tests are prevailing in the seawater in the NW Pacific Ocean. However, the {sup 240}Pu/{sup 239}Pu atom ratios in the surface sediment from the NW Pacific Ocean varied with the sampling locations. As a consequence, this study will provide the information that the water mass along with the current plays a key role in driving the distribution of Pu and in transporting Pu from the PPGs to the far eastern marginal sea in the NW Pacific Ocean. (author)
Lee, Sang-Han;
[1]
Hong, Gi-Hoon;
Suk, Moon-Sik;
[2]
Gastaud, J.;
[3]
La Rosa, J.;
[4]
Kim, Chul-Soo;
[5]
Wyse, E.;
[6]
Povinec, P. P.
[7]
- Korea Research Institute of Standards and Science, Daejeon (Korea, Republic of)
- Korea Ocean Research and Development Institute, Seoul (Korea, Republic of)
- International Atomic Energy Agency, Marine Environment Laboratory (Monaco)
- National Institute of Standards and Technology, Ionizing Radiation Division, Gaithersburg, Maryland (United States)
- Environmental Laboratories, International Atomic Energy Agency, Seibersdorf (Austria)
- New Brunswick Laboratory Argonne, IL (United States)
- Comenius University, Faculty of Mathematics and Physics, Bratislava (Slovakia)
Citation Formats
Lee, Sang-Han, Hong, Gi-Hoon, Suk, Moon-Sik, Gastaud, J., La Rosa, J., Kim, Chul-Soo, Wyse, E., and Povinec, P. P.
The Transport of Close-In Fallout Plutonium in the Northwest Pacific Ocean: Tracing the Water Mass Movement Using {sup 240}Pu/{sup 239}Pu Atom Ratio.
IAEA: N. p.,
2013.
Web.
Lee, Sang-Han, Hong, Gi-Hoon, Suk, Moon-Sik, Gastaud, J., La Rosa, J., Kim, Chul-Soo, Wyse, E., & Povinec, P. P.
The Transport of Close-In Fallout Plutonium in the Northwest Pacific Ocean: Tracing the Water Mass Movement Using {sup 240}Pu/{sup 239}Pu Atom Ratio.
IAEA.
Lee, Sang-Han, Hong, Gi-Hoon, Suk, Moon-Sik, Gastaud, J., La Rosa, J., Kim, Chul-Soo, Wyse, E., and Povinec, P. P.
2013.
"The Transport of Close-In Fallout Plutonium in the Northwest Pacific Ocean: Tracing the Water Mass Movement Using {sup 240}Pu/{sup 239}Pu Atom Ratio."
IAEA.
@misc{etde_22122105,
title = {The Transport of Close-In Fallout Plutonium in the Northwest Pacific Ocean: Tracing the Water Mass Movement Using {sup 240}Pu/{sup 239}Pu Atom Ratio}
author = {Lee, Sang-Han, Hong, Gi-Hoon, Suk, Moon-Sik, Gastaud, J., La Rosa, J., Kim, Chul-Soo, Wyse, E., and Povinec, P. P.}
abstractNote = {{sup 240}Pu/{sup 239}Pu atom ratios in seawater and surface sediment collected from the northwest (NW) Pacific Ocean from 1992 to 1997 were determined using ICP-sector field mass spectrometry (ICP-MS). In whole water columns, the atom ratios of {sup 240}Pu/{sup 239}Pu were higher than the global fallout ratio (0.18). It is noted that the atom ratios of {sup 240}Pu/2{sup 39}Pu in the seawater increase with depth. Such elevated {sup 240}Pu/{sup 239}Pu atom ratios indicate that the close-in fallout plutonium isotopes originating from the Pacific Proving Grounds (PPGs) due to the U.S. tests are prevailing in the seawater in the NW Pacific Ocean. However, the {sup 240}Pu/{sup 239}Pu atom ratios in the surface sediment from the NW Pacific Ocean varied with the sampling locations. As a consequence, this study will provide the information that the water mass along with the current plays a key role in driving the distribution of Pu and in transporting Pu from the PPGs to the far eastern marginal sea in the NW Pacific Ocean. (author)}
place = {IAEA}
year = {2013}
month = {Jul}
}
title = {The Transport of Close-In Fallout Plutonium in the Northwest Pacific Ocean: Tracing the Water Mass Movement Using {sup 240}Pu/{sup 239}Pu Atom Ratio}
author = {Lee, Sang-Han, Hong, Gi-Hoon, Suk, Moon-Sik, Gastaud, J., La Rosa, J., Kim, Chul-Soo, Wyse, E., and Povinec, P. P.}
abstractNote = {{sup 240}Pu/{sup 239}Pu atom ratios in seawater and surface sediment collected from the northwest (NW) Pacific Ocean from 1992 to 1997 were determined using ICP-sector field mass spectrometry (ICP-MS). In whole water columns, the atom ratios of {sup 240}Pu/{sup 239}Pu were higher than the global fallout ratio (0.18). It is noted that the atom ratios of {sup 240}Pu/2{sup 39}Pu in the seawater increase with depth. Such elevated {sup 240}Pu/{sup 239}Pu atom ratios indicate that the close-in fallout plutonium isotopes originating from the Pacific Proving Grounds (PPGs) due to the U.S. tests are prevailing in the seawater in the NW Pacific Ocean. However, the {sup 240}Pu/{sup 239}Pu atom ratios in the surface sediment from the NW Pacific Ocean varied with the sampling locations. As a consequence, this study will provide the information that the water mass along with the current plays a key role in driving the distribution of Pu and in transporting Pu from the PPGs to the far eastern marginal sea in the NW Pacific Ocean. (author)}
place = {IAEA}
year = {2013}
month = {Jul}
}