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

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Sites Affected by Long-Range <strong>Lead</strong> Transport<br />

Because the effects <strong>of</strong> anthropogenic Pb emissions tend to be restricted in geographic<br />

extent, most natural terrestrial ecosystems in the U.S. sites have Pb burdens derived primarily<br />

from long-range atmospheric transport. Pollutant Pb represents a large fraction <strong>of</strong> the Pb in<br />

many <strong>of</strong> these ecosystems. In particular, many <strong>of</strong> these sites have accumulated large amounts <strong>of</strong><br />

Pb in soils. For example, at the Hubbard Brook Experimental Forest in New Hampshire, the<br />

amount <strong>of</strong> Pb in the <strong>for</strong>est floor was estimated to have increased from about 1.35 kg ha !1 in 1926<br />

(be<strong>for</strong>e the introduction <strong>of</strong> alkyl-Pb additives in gasoline) to 10.5 kg ha !1 in 1977 (Johnson et al.,<br />

1995a). They also estimated the atmospheric Pb deposition from 1926 to 1987 to be 8.7 kg ha !1 ,<br />

an amount that could account <strong>for</strong> nearly all <strong>of</strong> the increase in Pb in the <strong>for</strong>est floor during the<br />

period. The input <strong>of</strong> precipitation Pb to the Hubbard Brook ecosystem in the six decades<br />

spanning 1926 to 1987 was more than half <strong>of</strong> the total Pb estimated to have been released by<br />

mineral weathering in the entire 12,000- to 14,000-year post-glacial period (14.1 kg ha !1 :<br />

[Johnson et al., 2004]). Other studies employing Pb budgets (Miller and Friedland, 1994;<br />

Watmough et al., 2004), and Pb isotopes (Bacon et al., 1995, 1996; Watmough et al., 1998;<br />

Bindler et al., 1999; Hansmann and Köppel, 2000; Kaste et al., 2003), have also shown that<br />

pollutant Pb, primarily from gasoline combustion, represents a quantitatively significant fraction<br />

<strong>of</strong> labile Pb in temperate soils, especially in the upper, organic-rich horizons.<br />

Despite years <strong>of</strong> elevated atmospheric Pb inputs and elevated concentrations in soils, there<br />

is little evidence that sites affected primarily by long-range Pb transport have experienced<br />

significant effects on ecosystem structure or function. Low concentrations <strong>of</strong> Pb in soil<br />

solutions, the result <strong>of</strong> strong complexation <strong>of</strong> Pb by soil organic matter, may explain why few<br />

ecological effects have been observed. At Hubbard Brook, <strong>for</strong> example, the concentration <strong>of</strong> Pb<br />

in soil solutions draining the Oa horizon is

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