Arsenic Behavior in Paddy Fields during the Cycle of Flooded and Non-flooded Periods

The behavior of As in paddy fields is of great interest considering high As contents of groundwater in several Asian countries where rice is the main staple. We determined the concentrations of Fe, Mn, and As in soil, soil water, and groundwater samples collected at different depths down to 2 m in a...

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Veröffentlicht in:Environmental science & technology 2004-02, Vol.38 (4), p.1038-1044
Hauptverfasser: Takahashi, Yoshio, Minamikawa, Reiko, Hattori, Kéiko H, Kurishima, Katsuaki, Kihou, Nobuharu, Yuita, Kouichi
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container_issue 4
container_start_page 1038
container_title Environmental science & technology
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creator Takahashi, Yoshio
Minamikawa, Reiko
Hattori, Kéiko H
Kurishima, Katsuaki
Kihou, Nobuharu
Yuita, Kouichi
description The behavior of As in paddy fields is of great interest considering high As contents of groundwater in several Asian countries where rice is the main staple. We determined the concentrations of Fe, Mn, and As in soil, soil water, and groundwater samples collected at different depths down to 2 m in an experimental paddy field in Japan during the cycle of flooded and non-flooded periods. In addition, we measured the oxidation states of Fe, Mn, and As in situ in soil samples using X-ray absorption near-edge structure (XANES) and conducted sequential extraction of the soil samples. The results show that Fe (hydr)oxide hosts As in soil. Arsenic in irrigation waters is incorporated in Fe (hydr)oxide in soil during the non-flooded period, and the As is quickly released from soil to water during the flooded period because of reductive dissolution of the Fe (hydr)oxide phase and reduction of As from As(V) to As(III). The enhancement of As dissolution by the reduction of As is supported by high As/Fe ratios of soil water during the flooded period and our laboratory experiments where As(III) concentrations and As(III)/As(V) ratios in submerged soil were monitored. Our work, primarily based on data from an actual paddy field, suggests that rice plants are enriched in As because the rice grows in flooded paddy fields when mobile As(III) is released to soil water.
doi_str_mv 10.1021/es034383n
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Sci. Technol</addtitle><date>2004-02-15</date><risdate>2004</risdate><volume>38</volume><issue>4</issue><spage>1038</spage><epage>1044</epage><pages>1038-1044</pages><issn>0013-936X</issn><eissn>1520-5851</eissn><coden>ESTHAG</coden><abstract>The behavior of As in paddy fields is of great interest considering high As contents of groundwater in several Asian countries where rice is the main staple. We determined the concentrations of Fe, Mn, and As in soil, soil water, and groundwater samples collected at different depths down to 2 m in an experimental paddy field in Japan during the cycle of flooded and non-flooded periods. In addition, we measured the oxidation states of Fe, Mn, and As in situ in soil samples using X-ray absorption near-edge structure (XANES) and conducted sequential extraction of the soil samples. The results show that Fe (hydr)oxide hosts As in soil. Arsenic in irrigation waters is incorporated in Fe (hydr)oxide in soil during the non-flooded period, and the As is quickly released from soil to water during the flooded period because of reductive dissolution of the Fe (hydr)oxide phase and reduction of As from As(V) to As(III). The enhancement of As dissolution by the reduction of As is supported by high As/Fe ratios of soil water during the flooded period and our laboratory experiments where As(III) concentrations and As(III)/As(V) ratios in submerged soil were monitored. Our work, primarily based on data from an actual paddy field, suggests that rice plants are enriched in As because the rice grows in flooded paddy fields when mobile As(III) is released to soil water.</abstract><cop>Washington, DC</cop><pub>American Chemical Society</pub><pmid>14998016</pmid><doi>10.1021/es034383n</doi><tpages>7</tpages></addata></record>
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subjects Agriculture
Agronomy. Soil science and plant productions
Applied sciences
Arsenic
Arsenic - analysis
Arsenic - pharmacokinetics
Biological and medical sciences
Biological and physicochemical phenomena
Biological and physicochemical properties of pollutants. Interaction in the soil
Contamination
Disasters
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Environmental Monitoring
Exact sciences and technology
Freshwater
Fundamental and applied biological sciences. Psychology
Groundwater
Irrigation
Natural water pollution
Oryza - chemistry
Oryza sativa
Oxidation-Reduction
Pollution
Pollution, environment geology
Rice
Soil and sediments pollution
Soil and water pollution
Soil Pollutants - analysis
Soil Pollutants - pharmacokinetics
Soil science
Solubility
Water Pollutants - analysis
Water Pollutants - pharmacokinetics
Water Supply
Water treatment and pollution
title Arsenic Behavior in Paddy Fields during the Cycle of Flooded and Non-flooded Periods
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