Interactions Between Sediments and Fresh Water 1976
DOI: 10.1007/978-94-011-9802-8_53
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Importance of the Denitrification Process for the Rate of Degradation of Organic Matter in Lake Sediments

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Cited by 21 publications
(15 citation statements)
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“…Methods of denitrification measurement: advantages and disadvantages Different methods for measuring denitrification have been developed: the acetylene inhibition technique (Sørensen 1978), the measurement of nitrate disappearance (Andersen 1977), the calculation of nitrate flux between sediment and water (Mengis et al 1997), the nitrogen mass balance approach (Ahlgren 1967), the direct measurement of N 2 production (Seitzinger et al 1980), the 15 N isotope pairing technique (IPT, Nielsen 1992), the determination of N 2 /Ar ratio via Membrane Introduction Mass Spectrometry (MIMS) (Kana et al 1998) and the whole-system scale of 15 N addition (Mulholland et al 2004). In recent years, there has been considerable discussion regarding the reliability of all these techniques, because they all show advantages but also potential problems, doubtful underlying assumptions and limitations that have been dealt with in some studies (Seitzinger et al 1993;Cornwell et al 1999;Steingruber et al 2001, Final Report of the Workshop on Denitrification 2004), why they will not be repeated here.…”
Section: Methodsmentioning
confidence: 99%
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“…Methods of denitrification measurement: advantages and disadvantages Different methods for measuring denitrification have been developed: the acetylene inhibition technique (Sørensen 1978), the measurement of nitrate disappearance (Andersen 1977), the calculation of nitrate flux between sediment and water (Mengis et al 1997), the nitrogen mass balance approach (Ahlgren 1967), the direct measurement of N 2 production (Seitzinger et al 1980), the 15 N isotope pairing technique (IPT, Nielsen 1992), the determination of N 2 /Ar ratio via Membrane Introduction Mass Spectrometry (MIMS) (Kana et al 1998) and the whole-system scale of 15 N addition (Mulholland et al 2004). In recent years, there has been considerable discussion regarding the reliability of all these techniques, because they all show advantages but also potential problems, doubtful underlying assumptions and limitations that have been dealt with in some studies (Seitzinger et al 1993;Cornwell et al 1999;Steingruber et al 2001, Final Report of the Workshop on Denitrification 2004), why they will not be repeated here.…”
Section: Methodsmentioning
confidence: 99%
“…3, 6). Andersen 1977 showed that anaerobic water conditions resulted in a high rate of denitrification in six Danish lakes compared with conditions with oxygenated water overlying in the sediment. With oxygen present, the uppermost sediment will be maintained at a high redox level as denitrification will occur below this oxidized zone, a longer diffusion pathway for the nitrate will result in lower denitrification rates.…”
Section: Environmental Controls Of Denitrificationmentioning
confidence: 98%
“…Greater oxygen availability may enhance nitrification in the oxic sediment zone while higher N03 supply to the suboxic sediment zone will enhance denitrification and N03 ammonification (Pelegri et al 1994) . Various authors have reported a significant increase in oxygen consumption and N03 uptake rates in sediments inhabited by chironomid species (Andersen 1977 ;Edwards & Rolley 1965 ;Granelli 1979 ;Hargrave 1975 ;Tatrai 1982) relative to non-inhabited sediments . Production of NH4 by chironomid larvae appears to be an important mechanism contributing to nitrogen regeneration from lake sediments (Fukuhara & Yasuda 1989 ;Gardner et al .…”
Section: Introductionmentioning
confidence: 99%
“…Edwards (1958) found that chironomids increased ammonia and decreased oxidized nitrogen in water overlying settled activated sludge. Anderson (1977) also observed an increase of denitrification in overlying water after addition of chironomids. In the Live microcosms, nitrification of ammonia may have contributed to the increase in sediment nitrate (Chatarpaul et al 1979).…”
Section: Nitrogen Componentsmentioning
confidence: 81%
“…Sulfur, in the form of sulfuric acid, is also a major contributor to acid precipitation (Likens et al 1976), and lake acidification . Nitrogen chemistry has been studied in freshwater by various investigators (Anderson 1977;Chen et al 1972;Hill 1979), while sulfur has been investigated in much less detail (Stuiver 1967;King & Klug 1980). In addition, little work has been done on the effect of benthic invertebrates on nitrogen and sulfur in freshwater sediments.…”
Section: Introductionmentioning
confidence: 99%