Please use this identifier to cite or link to this item: https://ptsldigital.ukm.my/jspui/handle/123456789/778481
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dc.contributor.authorStig H. Fonselius-
dc.date.accessioned2025-03-20T05:07:27Z-
dc.date.available2025-03-20T05:07:27Z-
dc.identifier.urihttps://ptsldigital.ukm.my/jspui/handle/123456789/778481-
dc.description.abstractThe water exchange of the Baltic is restricted through the narrow and shallow entrance area. The positive water balance causes stagnant conditions in the deep water. In such semi-enclosed basins the oxygen content of the deep water is depleted and nutrients are accumulated there. The oxygen deficiency is caused by oxidation of organic matter in the water. Nutrient salts are formed through transformation into inorganic form of organically bound nutrient elements. Therefore the supply of organic matter and the oxidation rate are the main factors which regulate the oxygen conditions in deep water, beside the water exchange ratio in the Danish sounds.en_US
dc.language.isoenen_US
dc.publisherNational Swedish Environment Protection Boarden_US
dc.subjectBalticen_US
dc.subjectWater exchangeen_US
dc.subjectHydrographicen_US
dc.subjectBiogenic elementsen_US
dc.titleOn biogenic elements and organic matter in the Balticen_US
dc.typeSeminar Papersen_US
dc.format.pages29-36en_US
dc.identifier.callnoGC1271.S68 1971 semen_US
dc.contributor.conferencenameSoviet-Swedish Symposium on the Pollution of the Baltic-
dc.coverage.conferencelocationStockholm, Sweden-
dc.date.conferencedate1971-09-08-
Appears in Collections:Seminar Papers/ Proceedings / Kertas Kerja Seminar/ Prosiding

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