Chemical Munitions Search and Assessment Project—Towards Creating Risk Assessment Tools for the Baltic Sea

2012 ◽  
Vol 46 (1) ◽  
pp. 28-36 ◽  
Author(s):  
Jacek Beldowski ◽  
Terrance P. Long

AbstractVast quantities of German chemical warfare agents (CWA) were stored in Wolgast, on the Baltic shore, at the end of World War II. Those munitions, together with others collected by allies after the war, were disposed in the Baltic Sea. Altogether, an estimated 50,000 tonnes of chemical weapons were sunk in the Baltic Sea. Official dumpsites are located in the Bornholm Deep, Gotland Deep, Little Belt, and Skagerrak. According to previous studies, several unofficial dumping sites exist on the transport routes from Wolgast to dumping areas and in the Gdańsk Deep (cold war dump).In the years 2005‐2008, the interdisciplinary “Modeling of Environmental Risks related to sea-dumped Chemical Weapons” (MERCW) project performed mapping, (ca. 20% of dumping areas) and addressed some possible ecological risks in official dumpsites in the Bornholm Deep, Gotland Deep, and Skagerrak. The Chemical Munitions Search and Assessment (CHEMSEA) project aims to fill the gaps in MERCW research (mapping using new techniques, sediment contamination study, corrosion estimation), observing temporal trends in the ecosystem (compare present CWA and degradation products to that observed in MERCW), and extend this research to the largest unofficial dumpsite (Gdańsk Deep). Moreover, CHEMSEA will provide a number of guidelines for affected groups and stakeholders regarding operations in bottom areas contaminated with CWA and assess the probability, range, and ecological consequences of CWA release from dumped munitions in the Baltic Sea. The results of the project will be shared with the Helsinki Commission and the project’s partners and associated partners. The CHEMSEA is planned for years 2011‐2014.

2009 ◽  
Vol 282 (2) ◽  
pp. 419-425 ◽  
Author(s):  
Tarja Katri Ikäheimonen ◽  
Iisa Outola ◽  
Vesa-Pekka Vartti ◽  
Pekka Kotilainen

2013 ◽  
Vol 10 (4) ◽  
pp. 2725-2735 ◽  
Author(s):  
M. Blumenberg ◽  
C. Berndmeyer ◽  
M. Moros ◽  
M. Muschalla ◽  
O. Schmale ◽  
...  

Abstract. The Baltic Sea, one of the world's largest brackish-marine basins, established after deglaciation of Scandinavia about 17 000 to 15 000 yr ago. In the changeable history of the Baltic Sea, the initial freshwater system was connected to the North Sea about 8000 yr ago and the modern brackish-marine setting (Littorina Sea) was established. Today, a relatively stable stratification has developed in the water column of the deep basins due to salinity differences. Stratification is only occasionally interrupted by mixing events, and it controls nutrient availability and growth of specifically adapted microorganisms and algae. We studied bacteriohopanepolyols (BHPs), lipids of specific bacterial groups, in a sediment core from the central Baltic Sea (Gotland Deep) and found considerable differences between the distinct stages of the Baltic Sea's history. Some individual BHP structures indicate contributions from as yet unknown redoxcline-specific bacteria (bacteriohopanetetrol isomer), methanotrophic bacteria (35-aminobacteriohopanetetrol), cyanobacteria (bacteriohopanetetrol cyclitol ether isomer) and from soil bacteria (adenosylhopane) through allochthonous input after the Littorina transgression, whereas the origin of other BHPs in the core has still to be identified. Notably high BHP abundances were observed in the deposits of the brackish-marine Littorina phase, particularly in laminated sediment layers. Because these sediments record periods of stable water column stratification, bacteria specifically adapted to these conditions may account for the high portions of BHPs. An additional and/or accompanying source may be nitrogen-fixing (cyano)bacteria, which is indicated by a positive correlation of BHP abundances with Corg and δ15N.


2012 ◽  
Vol 46 (1) ◽  
pp. 37-50 ◽  
Author(s):  
Victor Zhurbas ◽  
Vadim Paka

AbstractResults of modeling of the migration of chemical warfare agents (CWAs) and their decay products from the initial chemical weapons dump site are presented. The aim was to find idealized sediment redistribution schemes in deep basins of the Baltic Sea corresponding to different wind conditions and to model the concentration of dissolved CWA in a continuous release scenario in the Bornholm dump site corresponding to real wind statistics.


2020 ◽  
Vol 161 ◽  
pp. 105036 ◽  
Author(s):  
Anu Lastumäki ◽  
Raisa Turja ◽  
Matthias Brenner ◽  
Paula Vanninen ◽  
Hanna Niemikoski ◽  
...  

2020 ◽  
Vol 98 (37) ◽  
pp. 12-12
Author(s):  
Joshua Rapp Learn, special to C&EN

Author(s):  
Silvija Ozola

The port city Liepaja had gained recognition in Europe and the world by World War I. On the coast of the Baltic Sea a resort developed, to which around 1880 a wide promenade – Kurhaus Avenue provided a functional link between the finance and trade centre in Old Liepaja. On November 8, 1890 the building conditions for Liepaja, developed according to the sample of Riga building regulations, were partly confirmed: the construction territory was divided into districts of wooden and stone buildings. In 1888 after the reconstruction of the trade canal Liepaja became the third most significant port in the Russian Empire. The railway (engineer Gavriil Semikolenov; 1879) and metal bridges (engineers Huten and Ruktesel; 1881) across the trade canal provided the link between Old Liepaja and the industrial territory in New Liepaja, where industrial companies and building of houses developed in the neighbourhood of the railway hub, but in spring 1899 the construction of a ten-kilometre long street electric railway line and power station was commenced. Since September 25 the tram movement provided a regular traffic between Naval Port (Latvian: Karosta), the residential and industrial districts in New Liepaja and the city centre in Old Liepaja. In 1907 the construction of the ambitious “Emperor Alexander’s III Military Port” and maritime fortress was completed, but already in the following year the fortress was closed. In the new military port there were based not only the navy squadrons of the Baltic Sea, but also the Pacific Ocean before sending them off in the war against Japan. The development of Liepaja continued: promenades, surrounded by Dutch linden trees, joined squares and parks in one united plantation system. On September 20, 1910 Liepaja City Council made a decision to close the New Market and start modernization of the city centre. In 1911 Liepaja obtained its symbol – the Rose Square. In the independent Republic of Latvia the implementation of the agrarian reform was started and the task to provide inhabitants with flats was set. Around 1927 in the Technical Department of Liepaja City the development of the master-plan was started: the territory of the city was divided into the industrial, commercial, residential and resort zone, which was greened. It was planned to lengthen Lord’s (Latvian: Kungu) Street with a dam, partly filling up Lake Liepaja in order to build the water-main and provide traffic with the eastern bank. The passed “Law of City Lands” and “Regulations for City Construction and Development of Construction Plans and Development Procedure” in Latvia Republic in 1928 promoted a gradual development of cities. In 1932 Liepaja received the radio transmitter. On the northern outskirts a sugar factory was built (architect Kārlis Bikše; 1933). The construction of the city centre was supplemented with the Latvian Society House (architect Kārlis Blauss and Valdis Zebauers; 1934-1935) and Army Economical Shop (architect Aleksandrs Racenis), as well as the building of a pawnshop and saving bank (architect Valdis Zebauers; 1936-1937). The hotel “Pēterpils”, which became the property of the municipality in 1936, was renamed as the “City Hotel” and it was rebuilt in 1938. In New Liepaja the Friendly Appeal Elementary school was built (architect Karlis Bikše), but in the Naval Officers Meeting House was restored and it was adapted for the needs of the Red Cross Bone Tuberculosis Sanatorium (architect Aleksandrs Klinklāvs; 1930-1939). The Soviet military power was restored in Latvia and it was included in the Union of Soviet Socialist Republics. During the World War II buildings in the city centre around the Rose Square and Great (Latvian: Lielā) Street were razed. When the war finished, the “Building Complex Scheme for 1946-1950” was developed for Liepaja. In August 1950 the city was announced as closed: the trade port was adapted to military needs. Neglecting the historical planning of the city, in 1952 the restoration of the city centre building was started, applying standard projects. The restoration of Liepaja City centre building carried out during the post-war period has not been studied. Research goal: analyse restoration proposals for Liepaja City centre building, destroyed during World War II, and the conception appropriate to the socialism ideology and further development of construction.


Chemosphere ◽  
2011 ◽  
Vol 85 (2) ◽  
pp. 253-261 ◽  
Author(s):  
Johanna Kratzer ◽  
Lutz Ahrens ◽  
Anna Roos ◽  
Britt-Marie Bäcklin ◽  
Ralf Ebinghaus

2010 ◽  
Vol 7 (8) ◽  
pp. 2489-2508 ◽  
Author(s):  
J. Gelting ◽  
E. Breitbarth ◽  
B. Stolpe ◽  
M. Hassellöv ◽  
J. Ingri

Abstract. To indentify sources and transport mechanisms of iron in a coastal marine environment, we conducted measurements of the physiochemical speciation of Fe in the euphotic zone at three different locations in the Baltic Sea. In addition to sampling across a salinity gradient, we conducted this study over the spring and summer season. Moving from the riverine input characterized low salinity Bothnian Sea, via the Landsort Deep near Stockholm, towards the Gotland Deep in the Baltic Proper, total Fe concentrations averaged 114, 44, and 15 nM, respectively. At all three locations, a decrease in total Fe of 80–90% from early spring to summer was observed. Particulate Fe (PFe) was the dominating phase at all stations and accounted for 75–85% of the total Fe pool on average. The Fe isotope composition (δ 56Fe) of the PFe showed constant positive values in the Bothnian Sea surface waters (+0.08 to +0.20‰). Enrichment of heavy Fe in the Bothnian Sea PFe is possibly associated to input of aggregated land derived Fe-oxyhydroxides and oxidation of dissolved Fe(II). At the Landsort Deep the isotopic fractionation of PFe changed between −0.08‰ to +0.28‰ over the sampling period. The negative values in early spring indicate transport of PFe from the oxic-anoxic boundary at ∼80 m depth. The average colloidal iron fraction (CFe) showed decreasing concentrations along the salinity gradient; Bothnian Sea 15 nM; Landsort Deep 1 nM, and Gotland Deep 0.5 nM. Field Flow Fractionation data indicate that the main colloidal carrier phase for Fe in the Baltic Sea is a carbon-rich fulvic acid associated compound, likely of riverine origin. A strong positive correlation between PFe and chl-a indicates that cycling of suspended Fe is at least partially controlled by primary production. However, this relationship may not be dominated by active uptake of Fe into phytoplankton, but instead may reflect scavenging and removal of PFe during phytoplankton sedimentation.


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