Nutrient distribution in the Bosphorus and surrounding areas

As part of a five years monitoring project "Water Quality Monitoring of the Strait of Istanbul", February-December 1999 nutrient dynamics of the Black Sea-the Sea of Marmara transect are studied to evaluate the effect of discharges given by deep disposals. Through a one-year study, upper l...

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Veröffentlicht in:Water science and technology 2002-01, Vol.46 (8), p.59-66
Hauptverfasser: OKUS, E, ASLAN-YILMAZ, A, YÜKSEK, A, TAS, S, TÜFEKCI, V
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creator OKUS, E
ASLAN-YILMAZ, A
YÜKSEK, A
TAS, S
TÜFEKCI, V
description As part of a five years monitoring project "Water Quality Monitoring of the Strait of Istanbul", February-December 1999 nutrient dynamics of the Black Sea-the Sea of Marmara transect are studied to evaluate the effect of discharges given by deep disposals. Through a one-year study, upper layer nutrient concentrations were generally under the effect of northwestern-shelf Black Sea originated waters. This effect was strictly observed in July, when the upper layer flow was the thickest. On the other hand, partly in November but especially in December the northwestern-shelf Black Sea originated water flow was a minimum resulting in similar concentrations in both layers. Nutrient fluctuations also affected the chlorophyll a and POC concentrations as parameters of productivity. The nutrient concentrations decreased with the effect of spring bloom and highest chlorophyll a values were detected in November at Strait stations that did not match to the Sea of Marmara values. This fact represents the time-scale difference between the Black Sea and the Sea of Marmara. On the contrary, high nutrient concentrations in the lower layer (especially inorganic phosphate), and therefore low N:P ratios reflect the effect of deep discharge. Vertical mixing caused by meteorological conditions of the shallow station (M3) under the effect of surface discharges resulted in homogenous distribution of nutrients. Nutrient concentrations of the stations affected by deep discharge showed that the two-layer stratification of the system did not permit the discharge mix to the upper layer.
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Vertical mixing caused by meteorological conditions of the shallow station (M3) under the effect of surface discharges resulted in homogenous distribution of nutrients. Nutrient concentrations of the stations affected by deep discharge showed that the two-layer stratification of the system did not permit the discharge mix to the upper layer.</abstract><cop>London</cop><pub>IWA</pub><pmid>12420966</pmid><doi>10.2166/wst.2002.0145</doi><tpages>8</tpages></addata></record>
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subjects Animal, plant and microbial ecology
Applied ecology
Applied sciences
Baltic States
Biological and medical sciences
Chlorophyll
Discharge
Earth sciences
Earth, ocean, space
Ecotoxicology, biological effects of pollution
Engineering and environment geology. Geothermics
Environmental Monitoring
Eutrophication
Exact sciences and technology
Fundamental and applied biological sciences. Psychology
Marine
Marine and brackish environment
Natural water pollution
Nitrogen - analysis
Nutrient concentrations
Nutrient dynamics
Nutrients
Phosphorus - analysis
Pollution
Pollution, environment geology
Seawaters, estuaries
Stations
Straits
Turkey, Bosphorus Strait
Water flow
Water monitoring
Water Movements
Water Pollutants - analysis
Water quality
Water quality management
Water treatment and pollution
title Nutrient distribution in the Bosphorus and surrounding areas
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