2012
DOI: 10.1134/s009780781201006x
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Seasonal biogeochemical and microbiological studies of small lakes in taiga zone of northwestern Russian (Arkhangelsk Province)

Abstract: Abatract-The results of biogeochemical and microbiological studies of three small lakes in southwestern Arkhangelsk province are presented. The lakes differ in their morphometric characteristics, thermal and oxy gen regimes, and the extent of anthropogenic impact they experience. In the periods of summer and winter stratification, anaerobic water layers with higher phosphates, ammonium, and sulfide sulfur (hydrogen sul fide) are found to form in the bottom horizon of deep water zones of the lakes. The highest … Show more

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Cited by 9 publications
(6 citation statements)
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“…5a). Note that the probable contribution of thioarsenic species (as evidenced in sulfidic environments by Wilkin et al 2003) to the observed colloidal As in the bottom water and sediment of lake Maselga could not be tested in this work, although the concentration of thiosulfate in the water column is comparable to that of sulfide (Kokryatskaya et al 2012). However, the independence of colloidal As proportion on depth during most studied season and even its decrease in March, during the maximal anoxy in the hypolimnion (cf.…”
Section: Colloidal Speciation Of Trace Elementsmentioning
confidence: 55%
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“…5a). Note that the probable contribution of thioarsenic species (as evidenced in sulfidic environments by Wilkin et al 2003) to the observed colloidal As in the bottom water and sediment of lake Maselga could not be tested in this work, although the concentration of thiosulfate in the water column is comparable to that of sulfide (Kokryatskaya et al 2012). However, the independence of colloidal As proportion on depth during most studied season and even its decrease in March, during the maximal anoxy in the hypolimnion (cf.…”
Section: Colloidal Speciation Of Trace Elementsmentioning
confidence: 55%
“…Typical biogenic elements (Si, P, and N) and Ba are not associated with colloids; however, they exhibit significant stratification, as they probably originated from degrading sinking plankton debris and/or reflux from the sediments to the water column. The presence of the anoxic zone below 15-18 m, which is especially notable in winter and contains up to 0.67 lmol/L H 2 S (Kokryatskaya et al 2012), may be responsible for the increase in the bottom water concentrations of Cr, V, Mo, and As ( Fig. EA-2-1, E-H).…”
Section: Stratification Of Trace Elementsmentioning
confidence: 94%
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“…These FeS nanoparticles are capable of scavenging some trace metals [34,35]. Given elevated sulfide concentrations in the hypolimnion of Lake Svyatoe (from 0.24 µM at the surface to 1.18 µM at the bottom [36]), colloidal iron sulfide may be potentially important and deserves special investigation using size fractionation techniques.…”
Section: Trace Metal Speciation and Cycling In The Water Columnmentioning
confidence: 99%