2011
DOI: 10.1016/j.jhydrol.2011.02.015
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Hydrological and chemical budgets of a mire pool formed on alluvial lowland of Hokkaido, northern Japan

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Cited by 8 publications
(3 citation statements)
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“…Lake Akanuma has a surface area of 95,280 m 2 , a maximum depth of 2.1 m, and a mean depth (volume of the water body divided by its surface area) of 1.8 m (Kizuka et al 2011). The hydrological budget of Lake Akanuma is dominated by surface water inflow (18.3 mm day -1 ) and surface water outflow (20.2 mm day -1 ).…”
Section: Study Sites and Samplingmentioning
confidence: 99%
See 1 more Smart Citation
“…Lake Akanuma has a surface area of 95,280 m 2 , a maximum depth of 2.1 m, and a mean depth (volume of the water body divided by its surface area) of 1.8 m (Kizuka et al 2011). The hydrological budget of Lake Akanuma is dominated by surface water inflow (18.3 mm day -1 ) and surface water outflow (20.2 mm day -1 ).…”
Section: Study Sites and Samplingmentioning
confidence: 99%
“…The hydrological budget of Lake Akanuma is dominated by surface water inflow (18.3 mm day -1 ) and surface water outflow (20.2 mm day -1 ). The wetland around Lake Akanuma consists mainly of bogs with hummock-hollow microtopographies, with vegetation dominated by peat moss and vascular plants, as described in detail by Kizuka et al (2011). The vertical soil type profiles and microbial activity profiles in the Kushiro Wetland have been described by Senga et al (2015).…”
Section: Study Sites and Samplingmentioning
confidence: 99%
“…Joosten 1999 km marsh Kizuka et al 2008;Chaichana et al 2011 km Kizuka et al 2008Yamada et al unpublished National Research Council 1992Heino 2000Watanabe et al 2000;Kilroy et al 2008Ferone & Devito 2004Kizuka et al 2011Calder et al 1995Legesse et al 2004Ito et al 2009Vanni et al 2011 TN TP km Concentrations for inflow ditch water, bottom pore water, and groundwater respectively stand for the flow-rate-weighted average of all inflow ditches, the average of groundwater located 5 m distant from east and west shorelines, and the value of pore water sampled at 1.5 m depth under the lake bottom. DTN and DTP data are used for rain water, bottom pore water, and ground water in TN-TP plot.…”
Section: Kmmentioning
confidence: 99%