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326 G.M. Gadd<br />

cases, microbial activities can result in remobilization of metals from other<br />

wastes and transfer into aquatic systems. It is commonly accepted that toxic<br />

metals, and their chemical derivatives, metalloids, and organometals can<br />

have significant effects on microbial populations and almost every index<br />

of microbial activity can be affected, depending on the particular situation.<br />

However, metal toxicity is greatly affected by the physico-chemical<br />

nature of the environment and the chemical behaviour of the particular<br />

metal species in question (Gadd and Griffiths 1978). The degree of metal<br />

toxicity reduction can be quantitatively related to adsorption capacity and<br />

selectivity of adsorbents for example (Malakul et al. 1998). Further, unlike<br />

certain xenobiotics perhaps, not always is there a link between bioavailability<br />

and toxicity, a good example being the frequent amelioration of<br />

metal fungitoxicity by acidic pH (Gadd 1993a). Despite apparent toxicity,<br />

many microorganisms survive, grow and even flourish in apparently<br />

metal-polluted locations and a variety of mechanisms, both active and incidental,<br />

contribute to tolerance. All mechanisms depend on some change<br />

in metal speciation leading to decreased or increased mobility. Such metal<br />

transformations between soluble and insoluble phases are also at the heart<br />

of metal biogeochemistry, thus providing a direct link between microbial<br />

responses and element cycles. Thus, interactions of microorganisms with<br />

metals are extremely important and underpin many aspects of soil biology.<br />

The objective of this chapter is to detail major interactions of microorganisms<br />

with metals with particular reference to effects on speciation,<br />

toxicity, and biogeochemical cycling. In addition, attention is drawn to<br />

their significance in plant nutrition and in environmental biotechnology<br />

where certain microbial processes have application in metal recovery or<br />

detoxification.<br />

2<br />

Metals in Soils<br />

All soils contain metals, the concentrations in uncontaminated soil being related<br />

to the geology of the parental material. ‘Normal’ total concentrations<br />

may be high with speciation and bioavailability determining any effects<br />

on microbial populations. Metal release by environmental disturbance,<br />

weathering processes and biological activities may result in toxic effects<br />

on indigenous microbial populations, as well as metal transfer to aquatic<br />

habitats. However, effects on microbial populations are more commonly<br />

associated with pollution events, where concentrations of introduced toxic<br />

metals may greatly exceed indigenous levels. To appreciate and understand<br />

possible effects on microbial populations, it is necessary to consider some<br />

aspects of metal chemistry in soil since this determines speciation, bioavail-

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