1998
DOI: 10.2965/jswe.21.421
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Study on Purification Ability for Water Quality in Tidal Flats in Hiroshima Bay-Evaluation for the Characteristics of Organic Matter Decomposition.

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Cited by 8 publications
(6 citation statements)
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“…A similar seasonal change in sediment respiration has been reported previously for other estuarine intertidal flats (van Es 1982;Middelburg et al 1995Middelburg et al , 1996. At our study site, the Therkildsen and Lomstein (1993) Tidally dominated bay Northern Waddesn Sea, Germany 2.7-4.3 b Kristensen et al (1997) Intertidal estuary Westerschelde Estuary, The Netherlands 2.2-6.3 b Middelburg et al (1996) Intertidal flat Hiroshima Bay, Japan 2.4-2.8 a Seiki et al (1998) Sublittoral area Sapelo Island, Georgia, USA 1.26-2.16 a Smith (1973) Intertidal esutary Kurose River Estuary, Japan 1.8 b Present study a Value was determined under submerged conditions b Value was determined under air-exposed conditions Landscape Ecol Eng (2012) 8:107-114 111 monthly respiration was minimum in February (4.7 g CO 2 -C m -2 ) and maximum in August (11.5 g CO 2 -C m -2 ). In terrestrial habitats, extremely low soil respiration in winter is common (e.g., Mariko et al 2000;Rayment and Jarvis 2000;Mo et al 2005).…”
Section: Resultssupporting
confidence: 67%
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“…A similar seasonal change in sediment respiration has been reported previously for other estuarine intertidal flats (van Es 1982;Middelburg et al 1995Middelburg et al , 1996. At our study site, the Therkildsen and Lomstein (1993) Tidally dominated bay Northern Waddesn Sea, Germany 2.7-4.3 b Kristensen et al (1997) Intertidal estuary Westerschelde Estuary, The Netherlands 2.2-6.3 b Middelburg et al (1996) Intertidal flat Hiroshima Bay, Japan 2.4-2.8 a Seiki et al (1998) Sublittoral area Sapelo Island, Georgia, USA 1.26-2.16 a Smith (1973) Intertidal esutary Kurose River Estuary, Japan 1.8 b Present study a Value was determined under submerged conditions b Value was determined under air-exposed conditions Landscape Ecol Eng (2012) 8:107-114 111 monthly respiration was minimum in February (4.7 g CO 2 -C m -2 ) and maximum in August (11.5 g CO 2 -C m -2 ). In terrestrial habitats, extremely low soil respiration in winter is common (e.g., Mariko et al 2000;Rayment and Jarvis 2000;Mo et al 2005).…”
Section: Resultssupporting
confidence: 67%
“…Our results indicate that the estuarine intertidal flats contribute considerably to organic matter mineralization at the interfaces between terrestrial and marine White and black column shows sediment respiration under air-exposed and submerged conditions, respectively systems, although its area is only 0.2% of the terrestrial river basin area. Seiki et al (1998) Intertidal sandy flats at coast Island Sylt, Germany 500-767 a de Beer et al (2005) Intertidal sandy beach Eastern English Channel, France 15 b Spilmont et al (2005) Estuarine intertidal flats Ems-Dollard Estuary, The Netherlands 66-298 a van Es (1982) Estuarine intertidal flats Scheldt Estuary, The Netherlands 252 b Middelburg et al (1995) Estuarine intertidal flats Kurose River Estuary, Japan 92 c Present study a Measurement was conducted under submerged conditions; O 2 consumption rates were converted to CO 2 emission rates assuming the respiratory quotient was 1 b Measurement was conducted under air-exposed conditions c Value considering the variation of sediment respiration rates with temperature and tide Landscape Ecol Eng (2012) 8:107-114 113…”
Section: Resultsmentioning
confidence: 97%
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“…Although some authors have reported CO 2 emission rates under air-exposed conditions (Middelburg et al 1996;Migne´et al 2002;Spilmont et al 2005), most investigations of benthic respiration in intertidal estuaries, including organic carbon mineralization rate, were conducted under submerged conditions (e.g., van Es 1982;Cammen 1991;Seiki et al 1998). Therefore, the amount of mineralized organic carbon in intertidal estuaries likely has been underestimated.…”
Section: Resultsmentioning
confidence: 99%
“…During the measurements, water temperature was kept at 20°C. Changes in O 2 concentration in the seawater were monitored with a dissolved oxygen meter (model 52, YSI Nanotech Inc.) for at least 5 h. For comparison with CO 2 emission rates, O 2 consumption rates were converted to CO 2 emission rates assuming a molar ratio of 1:1 (Seiki et al 1998).…”
Section: Laboratory Experimentsmentioning
confidence: 99%