2008
DOI: 10.1007/978-3-540-70909-1_5
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Nutrient Dynamics in the Baltic Sea

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Cited by 7 publications
(27 citation statements)
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“…The Baltic Sea is the largest brackish water body in the world. The factors such as restricted water exchange, water stratification, oxygen deficiency in deep waters, shallow depths (mean depth = 53 m), and a large ratio of catchment area to the surface of the sea (4:1), cause the Baltic Sea to be sensitive to human pressure (Håkanson and Bryhn 2008 ; Wulff et al 2001 ). Agricultural and industrial catchment areas have led to considerable degradation of the sea.…”
Section: Introductionmentioning
confidence: 99%
“…The Baltic Sea is the largest brackish water body in the world. The factors such as restricted water exchange, water stratification, oxygen deficiency in deep waters, shallow depths (mean depth = 53 m), and a large ratio of catchment area to the surface of the sea (4:1), cause the Baltic Sea to be sensitive to human pressure (Håkanson and Bryhn 2008 ; Wulff et al 2001 ). Agricultural and industrial catchment areas have led to considerable degradation of the sea.…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, it is the share of these bioavailable nutrient forms that determine the eutrophication potential of wastewater discharged into receivers. Nitrates and ammonium are considered to be the most available N compounds (Nakajima et al 2006 ; Håkansson and Bryhn 2008 ), while orthophosphates (H 2 PO 4 − , HPO 4 2 − , or PO 4 3− ) are the only directly available P form for planktonic algae and bacteria (Warwick et al 2013 ; Venkiteshwaran et al 2018 ). Therefore, it should be emphasized, that not only total nutrient forms but mainly their inorganic compounds should be limited by legal regulations aimed at mitigating eutrophication.…”
Section: Methodsmentioning
confidence: 99%
“…The corresponding number for the sediments between 65 m and 100 m water depth would be around 100,000 tonnes, and the area equivalent to the expansion of laminated sediments between 1960 and 1990 according to Jonsson et al 9 Reducing the amount of phosphorus in the bottom waters by 100,000 tonnes corresponds to a decrease in phosphorus concentration around 30 mg/m 3 in the deep water (below 65 m), and the effect would possibly be felt also in the surface water although less dramatic. It is worth reflecting on the fact that the adjacent Bothnian Sea, where almost all sediment surfaces are oxic, 38 typically has total phosphorus concentrations in surface water around 10 mg/m 3 lower than the Baltic Proper, 6 keeping in mind that also the external P loading is lower to this basin. 3…”
Section: Discussionmentioning
confidence: 99%
“…According to the Baltic Sea Action Plan, the annual phosphorus load should be reduced with around 15,000 tonnes, including 12,500 tonnes to the Baltic Proper. 4 Budget calculations for the Baltic Proper indicate that the sediments annually release between 18,000 and 285,000 tonnes of phosphorus to the water column, 5,6 the latter including resuspension of old clays due to land uplift. Savchuk 7 found that a net flux of around 20,000 tonnes of phosphorus from the sediments of the Baltic Proper was required to sustain measured levels of phosphorus in the water column.…”
Section: Introductionmentioning
confidence: 99%