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Reacidification Effects on Water Chemistry and Plankton in a Limed Lake in Sweden
Water chemistry and plankton has been monitored in three Lakes in Tyresta National park SE of Stockholm since 1977. Liming operations started in Lake Långsjön and Lake Trehörningen in 1978 and were repeated every 3-5 years, while Lake Årsjön is an unlimed reference Lake. During 1991-1999, the annual...
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Published in: | Water, air, and soil pollution air, and soil pollution, 2001-08, Vol.130 (1-4), p.1763-1768 |
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description | Water chemistry and plankton has been monitored in three Lakes in Tyresta National park SE of Stockholm since 1977. Liming operations started in Lake Långsjön and Lake Trehörningen in 1978 and were repeated every 3-5 years, while Lake Årsjön is an unlimed reference Lake. During 1991-1999, the annual pH median in Lake Långsjön and Lake Årsjön ranged between 6.6-7.1 and 5.2-5.8, respectively, and the composition of phyto- and zooplankton in these lakes did not change markedly. After a final treatment in 1991, the liming of Lake Trehörningen was terminated intentionally. As a result, pH decreased from an annual median 7.1 in 1991, to 6.1 in 1999 (5.8 in 1998). Total organic carbon (TOC) did not change markedly during this period, while the levels of calcium decreased. Metals, known to be influenced by acidification, especially cadmium, manganese and aluminium (Al), increased. The labile-inorganic forms of Al also reached higher levels, especially in 1998. Following the decreasing pH, the total number of phytoplankton taxa decreased by ca 40%. Among zooplankton, the cladocerans Holopedium gibberum, Diaphanosoma brachyurum and Daphnia longispina, common during the limed period, became rare.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1023/A:1013964123524 |
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Liming operations started in Lake Långsjön and Lake Trehörningen in 1978 and were repeated every 3-5 years, while Lake Årsjön is an unlimed reference Lake. During 1991-1999, the annual pH median in Lake Långsjön and Lake Årsjön ranged between 6.6-7.1 and 5.2-5.8, respectively, and the composition of phyto- and zooplankton in these lakes did not change markedly. After a final treatment in 1991, the liming of Lake Trehörningen was terminated intentionally. As a result, pH decreased from an annual median 7.1 in 1991, to 6.1 in 1999 (5.8 in 1998). Total organic carbon (TOC) did not change markedly during this period, while the levels of calcium decreased. Metals, known to be influenced by acidification, especially cadmium, manganese and aluminium (Al), increased. The labile-inorganic forms of Al also reached higher levels, especially in 1998. Following the decreasing pH, the total number of phytoplankton taxa decreased by ca 40%. Among zooplankton, the cladocerans Holopedium gibberum, Diaphanosoma brachyurum and Daphnia longispina, common during the limed period, became rare.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0049-6979</identifier><identifier>EISSN: 1573-2932</identifier><identifier>DOI: 10.1023/A:1013964123524</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Acidification ; Aluminum ; Cadmium ; Cladocera ; Daphnia longispina ; Diaphanosoma brachyurum ; Environmental monitoring ; Freshwater ; Heavy metals ; Holopedium gibberum ; Lakes ; Liming ; Manganese ; National parks ; Organic carbon ; pH effects ; Phytoplankton ; Plankton ; Sweden, Aarsjoen L ; Sweden, Laangsjoen L ; Sweden, Trehoerningen L ; Total organic carbon ; Water chemistry ; Zooplankton</subject><ispartof>Water, air, and soil pollution, 2001-08, Vol.130 (1-4), p.1763-1768</ispartof><rights>Kluwer Academic Publishers 2001</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c289t-b4a5f74e144af9545451b69ecb74c92d56441179528e6c28c58c6c92c450ce2f3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/746646625/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/746646625?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,11688,27924,27925,36060,36061,44363,74895</link.rule.ids></links><search><creatorcontrib>Edberg, Frida</creatorcontrib><creatorcontrib>Andersson, Paul</creatorcontrib><creatorcontrib>Borg, Hans</creatorcontrib><creatorcontrib>Ekström, Christina</creatorcontrib><creatorcontrib>Hörnström, Einar</creatorcontrib><title>Reacidification Effects on Water Chemistry and Plankton in a Limed Lake in Sweden</title><title>Water, air, and soil pollution</title><description>Water chemistry and plankton has been monitored in three Lakes in Tyresta National park SE of Stockholm since 1977. Liming operations started in Lake Långsjön and Lake Trehörningen in 1978 and were repeated every 3-5 years, while Lake Årsjön is an unlimed reference Lake. During 1991-1999, the annual pH median in Lake Långsjön and Lake Årsjön ranged between 6.6-7.1 and 5.2-5.8, respectively, and the composition of phyto- and zooplankton in these lakes did not change markedly. After a final treatment in 1991, the liming of Lake Trehörningen was terminated intentionally. As a result, pH decreased from an annual median 7.1 in 1991, to 6.1 in 1999 (5.8 in 1998). Total organic carbon (TOC) did not change markedly during this period, while the levels of calcium decreased. Metals, known to be influenced by acidification, especially cadmium, manganese and aluminium (Al), increased. The labile-inorganic forms of Al also reached higher levels, especially in 1998. Following the decreasing pH, the total number of phytoplankton taxa decreased by ca 40%. 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Liming operations started in Lake Långsjön and Lake Trehörningen in 1978 and were repeated every 3-5 years, while Lake Årsjön is an unlimed reference Lake. During 1991-1999, the annual pH median in Lake Långsjön and Lake Årsjön ranged between 6.6-7.1 and 5.2-5.8, respectively, and the composition of phyto- and zooplankton in these lakes did not change markedly. After a final treatment in 1991, the liming of Lake Trehörningen was terminated intentionally. As a result, pH decreased from an annual median 7.1 in 1991, to 6.1 in 1999 (5.8 in 1998). Total organic carbon (TOC) did not change markedly during this period, while the levels of calcium decreased. Metals, known to be influenced by acidification, especially cadmium, manganese and aluminium (Al), increased. The labile-inorganic forms of Al also reached higher levels, especially in 1998. Following the decreasing pH, the total number of phytoplankton taxa decreased by ca 40%. 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subjects | Acidification Aluminum Cadmium Cladocera Daphnia longispina Diaphanosoma brachyurum Environmental monitoring Freshwater Heavy metals Holopedium gibberum Lakes Liming Manganese National parks Organic carbon pH effects Phytoplankton Plankton Sweden, Aarsjoen L Sweden, Laangsjoen L Sweden, Trehoerningen L Total organic carbon Water chemistry Zooplankton |
title | Reacidification Effects on Water Chemistry and Plankton in a Limed Lake in Sweden |
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