Influence of snow on iron release from soil

Mayumi Seto, Tasuku Akagi

研究成果: ジャーナルへの寄稿記事

1 引用 (Scopus)

抄録

The concentration of Fe in stream water and groundwater was measured monthly during a whole year. The study fields were Ozenuma lake and Senjougahara peatland, which snow covers for more than 5 months in winter. Iron concentration in water increased during snow-covered and thaw seasons with the synchronized decrease in Eh and pH for both stream water and groundwater. In snow-covered seasons, it is hypothesized that supply of melt water and/or coverage with ice layers during this period could cause the development of an anaerobic zone in underlying soil. This study suggests that change in the amount of snowfall or in the length of snow season may influence the geochemical cycle of iron.

元の言語英語
ページ(範囲)173-183
ページ数11
ジャーナルGEOCHEMICAL JOURNAL
39
発行部数2
DOI
出版物ステータス出版済み - 1 1 2005
外部発表Yes

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snow
Snow
soils
Iron
Soils
iron
ground water
Water
water
geochemical cycle
groundwater
soil
Groundwater
snow cover
meltwater
peatland
lakes
winter
ice
Ice

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

これを引用

Influence of snow on iron release from soil. / Seto, Mayumi; Akagi, Tasuku.

:: GEOCHEMICAL JOURNAL, 巻 39, 番号 2, 01.01.2005, p. 173-183.

研究成果: ジャーナルへの寄稿記事

Seto, Mayumi ; Akagi, Tasuku. / Influence of snow on iron release from soil. :: GEOCHEMICAL JOURNAL. 2005 ; 巻 39, 番号 2. pp. 173-183.
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