1995
DOI: 10.1007/bf01569945
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Cation-exchange capacity of algae and cyanobacteria: A parameter of their metal sorption abilities

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Cited by 22 publications
(8 citation statements)
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“…In soils above pH 7 (true for most desert soils), cation exchange capacity is significantly increased by all microbial species (Gadd, 1990a;Pirszel et al, 1995). Polysaccharide production can be simulated by soil Mg, K, and Ca.…”
Section: Discussionmentioning
confidence: 98%
“…In soils above pH 7 (true for most desert soils), cation exchange capacity is significantly increased by all microbial species (Gadd, 1990a;Pirszel et al, 1995). Polysaccharide production can be simulated by soil Mg, K, and Ca.…”
Section: Discussionmentioning
confidence: 98%
“…Initial binding may also be followed by inorganic deposition of an increased amount of metal. Particulate material can bind to crustal organisms (e.g., sulfides of copper, Zn, Pb, zinc dust, magnesic oxide, and ferric hydroxide ;Lange 1974;Gadd 1990a,b;McLean and Beveridge 1990;Pirszel et al 1995). Most adsorbed metals stay on or within the extracellular sheath, and are not absorbed by the cells, thus remaining available to plants (Geesey and Jang 1990).…”
Section: Carbon C:n Ratios and Organic Mattermentioning
confidence: 98%
“…The Cu(II) adsorption capacity at pH 7.0 was 10.77 mol m Ϫ2 , equivalent to 0.829 mmol per g of dried spores, which is the same order of magnitude as the Cu(II) adsorption capacities of various biomasses, such as bacteria, algae, fungi (20). Pirszel et al (26) reported that the ionexchange capacities were 0.825 mmol g of dry weight Ϫ1 for cells for Anacystis nidulans (a cyanobacterium), 0.205 mmol g Ϫ for Synechocystis aquatilis (a cyanobacterium), 0.260 mmol g Ϫ1 for Stichococcus bacillaris (a green alga), and 0.041 mmol g Ϫ1 for Vaucheria sp. (a macroalga).…”
Section: Resultsmentioning
confidence: 86%