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Air Quality Criteria for Lead Volume II of II - (NEPIS)(EPA) - US ...

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varies from 4:1 in rural streams to 27:1 in urban streams (Getz et al., 1977). In still waters, Pb is<br />

removed through sedimentation at a rate determined by temperature, pH, oxidation-reduction<br />

(redox) potential, organic content, grain size, and chemical <strong>for</strong>m <strong>of</strong> Pb in the water and<br />

biological activities (Jenne and Luoma, 1977). Since the publication <strong>of</strong> the 1986 <strong>Lead</strong> AQCD<br />

(U.S. Environmental Protection Agency, 1986a), knowledge <strong>of</strong> the properties <strong>of</strong> Pb in aquatic<br />

ecosystems has expanded. This section will provide further detail on the chemical species and<br />

the environmental factors affecting speciation <strong>of</strong> Pb in the aquatic environment. In addition,<br />

quantitative distributions <strong>of</strong> Pb in water, sediment, and biological tissues will be presented <strong>for</strong><br />

aquatic ecosystems throughout the United States. Finally, recent studies discussing the tracing <strong>of</strong><br />

Pb in aquatic systems will be summarized.<br />

AX7.2.2.1 Speciation <strong>of</strong> <strong>Lead</strong> in Aquatic Ecosystems<br />

The speciation <strong>of</strong> Pb in the aquatic environment is controlled by many factors. The<br />

primary <strong>for</strong>m <strong>of</strong> Pb in aquatic environments is divalent (Pb 2+ ), while Pb 4+ exists only under<br />

extreme oxidizing conditions (Rickard and Nriagu, 1978). Labile <strong>for</strong>ms <strong>of</strong> Pb (e.g., Pb 2+ ,<br />

PbOH + , PbCO3) are a significant portion <strong>of</strong> the Pb inputs to aquatic systems from atmospheric<br />

washout. <strong>Lead</strong> is typically present in acidic aquatic environments as PbSO4, PbCl4, ionic Pb,<br />

cationic <strong>for</strong>ms <strong>of</strong> Pb-hydroxide, and ordinary Pb-hydroxide (Pb(OH)2). In alkaline waters,<br />

common species <strong>of</strong> Pb include anionic <strong>for</strong>ms <strong>of</strong> Pb-carbonate (Pb(CO3)) and Pb(OH)2.<br />

Speciation models have been developed based on the chemical equilibrium model developed by<br />

Tipping (1994) to assist in examining metal speciation. The <strong>EPA</strong> MINTEQA2 computer model<br />

(http://www.epa.gov/ceampubl/mmedia/minteq/) is one such equilibrium speciation model that<br />

can be used to calculate the equilibrium composition <strong>of</strong> dilute aqueous solutions in the laboratory<br />

or in natural aqueous systems. The model is useful <strong>for</strong> calculating the equilibrium mass<br />

distribution among dissolved species, adsorbed species, and multiple solid phases under a variety<br />

<strong>of</strong> conditions, including a gas phase with constant partial pressures. In addition to chemical<br />

equilibrium models, the speciation <strong>of</strong> metals is important from a toxicological perspective.<br />

The BLM was developed to study the toxicity <strong>of</strong> metal ions in aquatic biota and was previously<br />

described in Section AX7.2.1.3. Further detail on speciation models is not provided herein,<br />

rather a general overview <strong>of</strong> major speciation principles are characterized in the following<br />

sections.<br />

AX7-118

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