1992
DOI: 10.1002/iroh.19920770108
|View full text |Cite
|
Sign up to set email alerts
|

Chemical and Microbial Binding Forms of Phosphorus Considering the Availability of Nitrate in Sediment‐Water Systems

Abstract: An analytical registration of P-transport processes in intact sediment cores from the shallow reservoir Radeburg I1 (near Dresden, Saxonia, Germany) was possible by application of KH232P04 and followed by sequential P-fractionation (PSENNER et al. 1984). Under oxygen free conditions and sufficient nitrate supply an activity accumulation was found in the uppermost sediment horizon. Nitrate influences above all the BD-fraction (reductant soluble P), so that an interaction between nitrate and the iron binding sys… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

1996
1996
2008
2008

Publication Types

Select...
3
3

Relationship

0
6

Authors

Journals

citations
Cited by 9 publications
(3 citation statements)
references
References 19 publications
0
3
0
Order By: Relevance
“…The remarkably low nitrate concentration in the deep hypolimnetic water of station E in February 2006 illustrates the high reductive power of the sediment at this point. The nitrate concentrations measured in 2005 in the upper 0.5 cm sediment layer of the main basin may point to the absence of a concurrent phosphate release from the sediment into the water body (Andrusch et al, 1992;Hupfer and Uhlmann, 1991;Maaßen et al, 2005). The low concentration or absence of nitrate in the sediment of all sampling points in 2006 could be explained by long winter stagnation (97 days) and an extremely short spring circulation (6 days).…”
Section: Chemical Componentsmentioning
confidence: 90%
“…The remarkably low nitrate concentration in the deep hypolimnetic water of station E in February 2006 illustrates the high reductive power of the sediment at this point. The nitrate concentrations measured in 2005 in the upper 0.5 cm sediment layer of the main basin may point to the absence of a concurrent phosphate release from the sediment into the water body (Andrusch et al, 1992;Hupfer and Uhlmann, 1991;Maaßen et al, 2005). The low concentration or absence of nitrate in the sediment of all sampling points in 2006 could be explained by long winter stagnation (97 days) and an extremely short spring circulation (6 days).…”
Section: Chemical Componentsmentioning
confidence: 90%
“…Usually, as long as the presence of nitrate keeps a sediment aerobic and enough aerobic sorption capacity is provided, P release is prevented or reduced [5][6][7][8]. A threshold value in the range of 1 mg L -1 NO 3 --N in stratified and 0.5 mg L -1 NO 3 --N in non stratified lakes was proposed to be sufficient to inhibit P release [9].…”
Section: Influence Of Nitratementioning
confidence: 99%
“…Struwe and Kjoller retention in Viiratsi. Also, some investigations (1991) found up to 100 times higher denitrifying suggest that permanently high N concentration in activity in slurry incubations than in the black alder soil can cause P leaching (Andrusch et al 1992). On forest.…”
Section: S ]42 Porij6gi Test Sitementioning
confidence: 99%