Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest

To clarify the effect of vegetation and surface soil removal on dissolved inorganic nitrogen (N) dynamics in a snow-dominated forest soil in northern Japan, the seasonal fluctuation of N concentrations in soil solution and the annual flux of N in soil were investigated at a treated site (in which su...

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Main Authors: M. Ozawa, H. Shibata, F. Satoh, K. Sasa
Format: Article
Language:English
Published: Hindawi Limited 2001-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2001.311
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spelling doaj-68439cbb46b940a899c385f29f79cb502020-11-25T00:50:43ZengHindawi LimitedThe Scientific World Journal1537-744X2001-01-01152753310.1100/tsw.2001.311Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated ForestM. Ozawa0H. Shibata1F. Satoh2K. Sasa3Graduate School of Agriculture, Hokkaido University, Sapporo, JapanGraduate School of Agriculture, Hokkaido University, Sapporo, JapanGraduate School of Agriculture, Hokkaido University, Sapporo, JapanGraduate School of Agriculture, Hokkaido University, Sapporo, JapanTo clarify the effect of vegetation and surface soil removal on dissolved inorganic nitrogen (N) dynamics in a snow-dominated forest soil in northern Japan, the seasonal fluctuation of N concentrations in soil solution and the annual flux of N in soil were investigated at a treated site (in which surface soil, including understory vegetation and organic and A horizons, was removed) and control sites from July 1998 to June 2000. Nitrate (NO3–) concentration in soil solution at the treated site was significantly higher than that of the control in the no-snow period, and it was decreased by dilution from melting snow. The annual net outputs of NO3– from soil at the treated site and control sites were 257 and –12 mmol m–2 year–1, and about 57% of the net output at the treated site occurred during the snowmelt period. NO3– was transported from the upper level to the lower level of soil via water movement during late autumn and winter, and it was retained in soil and leached by melt water in early spring. Removing vegetation and surface soil resulted in an increase in NO3– concentration of soil solution, and snowmelt strongly affected the NO3– leaching from treated soil and the NO3– restoration process in a snow-dominated region.http://dx.doi.org/10.1100/tsw.2001.311
collection DOAJ
language English
format Article
sources DOAJ
author M. Ozawa
H. Shibata
F. Satoh
K. Sasa
spellingShingle M. Ozawa
H. Shibata
F. Satoh
K. Sasa
Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
The Scientific World Journal
author_facet M. Ozawa
H. Shibata
F. Satoh
K. Sasa
author_sort M. Ozawa
title Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
title_short Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
title_full Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
title_fullStr Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
title_full_unstemmed Effects of Surface Soil Removal on Dynamics of Dissolved Inorganic Nitrogen in a Snow-Dominated Forest
title_sort effects of surface soil removal on dynamics of dissolved inorganic nitrogen in a snow-dominated forest
publisher Hindawi Limited
series The Scientific World Journal
issn 1537-744X
publishDate 2001-01-01
description To clarify the effect of vegetation and surface soil removal on dissolved inorganic nitrogen (N) dynamics in a snow-dominated forest soil in northern Japan, the seasonal fluctuation of N concentrations in soil solution and the annual flux of N in soil were investigated at a treated site (in which surface soil, including understory vegetation and organic and A horizons, was removed) and control sites from July 1998 to June 2000. Nitrate (NO3–) concentration in soil solution at the treated site was significantly higher than that of the control in the no-snow period, and it was decreased by dilution from melting snow. The annual net outputs of NO3– from soil at the treated site and control sites were 257 and –12 mmol m–2 year–1, and about 57% of the net output at the treated site occurred during the snowmelt period. NO3– was transported from the upper level to the lower level of soil via water movement during late autumn and winter, and it was retained in soil and leached by melt water in early spring. Removing vegetation and surface soil resulted in an increase in NO3– concentration of soil solution, and snowmelt strongly affected the NO3– leaching from treated soil and the NO3– restoration process in a snow-dominated region.
url http://dx.doi.org/10.1100/tsw.2001.311
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