Volume 15, Issue 10 pp. 1771-1789
Research Article

Hydrobiogeochemistry of forest ecosystems in Japan: major themes and research issues

Nobuhito Ohte

Corresponding Author

Nobuhito Ohte

Graduate School of Agricultural Sciences, Kyoto University, Kyoto, Japan

Division of Environmental Science and Technology, Graduate School of Agricultural Sciences, Kyoto University, Kyoto 606-8502, Japan===Search for more papers by this author
Naoko Tokuchi

Naoko Tokuchi

Graduate School of Agricultural Sciences, Kyoto University, Kyoto, Japan

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Hideaki Shibata

Hideaki Shibata

North Research Station, Hokkaido University Forests, Faculty of Agriculture, Hokkaido University, Hokkaido, Japan

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Maki Tsujimura

Maki Tsujimura

Institute of Geoscience, University of Tsukuba, Tsukuba, Japan

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Tadashi Tanaka

Tadashi Tanaka

Institute of Geoscience, University of Tsukuba, Tsukuba, Japan

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Myron J. Mitchell

Myron J. Mitchell

College of Environmental Science and Forestry, State University of New York, New York, USA

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First published: 11 July 2001
Citations: 43

Abstract

Hydrobiogeochemical information on forested watersheds in the Japanese archipelago is reviewed to qualitatively summarize the major factors affecting the hydrology and biogeochemistry of this region. Major features that distinguish Japanese forest watersheds from those of north central Europe and the northeast United States generally include higher temperature, greater precipitation and steeper topography. There have been three major themes in hydrobiogeochemistry research on Japanese forest ecosystems: (1) investigations of nutrient cycles with particular emphasis on the establishment and maintenance of forest ecosystems; (2) evaluations of streamwater chemistry as an output from the forest ecosystem; and (3) hydrological studies using biogeochemical tracers. High precipitation inputs during the growing season affect the seasonality of the streamwater NO3 concentration, resulting in different temporal patterns than those generally found in north central Europe and the northeast United States. The high alkalinity and pH of Japanese surface waters is due to the rapid weathering of relatively young soils that are generated by steep hillslopes. Warm temperatures and elevated soil moisture enhance high rates of mineral weathering. Hydrological studies using biogeochemical tracers have shown that the steep topography contributes to the highly heterogeneous movement of water within Japanese catchments. Copyright © 2001 John Wiley & Sons, Ltd.

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