Radiotracer method to study the transport of mercury(II)chloride from water to sediment and air

F. Karaca; I. Ölmez; N. K. Aras

doi:10.1023/B:JRNC.0000017292.55751.26

Radiotracer method to study the transport of mercury(II)chloride from water to sediment and air

F. Karaca, I. Ölmez, N. K. Aras

Research output: Contribution to journal › Article › peer-review

6 Citations (Scopus)

Abstract

The fate of dissolved Hg(II) in surface waters is an important component of the Hg cycle. A simple experimental methodology was used to understand and measure the transport of Hg(II) from water to air and sediment. The use of radioactive dissolved Hg tracer for the determination of evasion and deposition is found to be a very useful technique. The evasion of mercury was investigated during a 140-hour period. It was observed that about a quarter of mercury chloride remained in the water phase, the other quarter was emitted via the evasion process and half of it deposited in sediment.

Original language	English
Pages (from-to)	223-226
Number of pages	4
Journal	Journal of Radioanalytical and Nuclear Chemistry
Volume	259
Issue number	2
DOIs	https://doi.org/10.1023/B:JRNC.0000017292.55751.26
Publication status	Published - Feb 1 2004
Externally published	Yes

ASJC Scopus subject areas

Analytical Chemistry
Nuclear Energy and Engineering
Radiology Nuclear Medicine and imaging
Pollution
Spectroscopy
Public Health, Environmental and Occupational Health
Health, Toxicology and Mutagenesis

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title = "Radiotracer method to study the transport of mercury(II)chloride from water to sediment and air",

abstract = "The fate of dissolved Hg(II) in surface waters is an important component of the Hg cycle. A simple experimental methodology was used to understand and measure the transport of Hg(II) from water to air and sediment. The use of radioactive dissolved Hg tracer for the determination of evasion and deposition is found to be a very useful technique. The evasion of mercury was investigated during a 140-hour period. It was observed that about a quarter of mercury chloride remained in the water phase, the other quarter was emitted via the evasion process and half of it deposited in sediment.",

author = "F. Karaca and I. {\"O}lmez and Aras, {N. K.}",

note = "Funding Information: One of us (NKA) thanks to Turkish Academy of Sciences for their partial support of this work.",

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AU - Karaca, F.

AU - Ölmez, I.

AU - Aras, N. K.

N1 - Funding Information: One of us (NKA) thanks to Turkish Academy of Sciences for their partial support of this work.

PY - 2004/2/1

Y1 - 2004/2/1

N2 - The fate of dissolved Hg(II) in surface waters is an important component of the Hg cycle. A simple experimental methodology was used to understand and measure the transport of Hg(II) from water to air and sediment. The use of radioactive dissolved Hg tracer for the determination of evasion and deposition is found to be a very useful technique. The evasion of mercury was investigated during a 140-hour period. It was observed that about a quarter of mercury chloride remained in the water phase, the other quarter was emitted via the evasion process and half of it deposited in sediment.

AB - The fate of dissolved Hg(II) in surface waters is an important component of the Hg cycle. A simple experimental methodology was used to understand and measure the transport of Hg(II) from water to air and sediment. The use of radioactive dissolved Hg tracer for the determination of evasion and deposition is found to be a very useful technique. The evasion of mercury was investigated during a 140-hour period. It was observed that about a quarter of mercury chloride remained in the water phase, the other quarter was emitted via the evasion process and half of it deposited in sediment.

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