Appel Chip, Ma Lena Q, Rhue Roy D, Reve William
Earth and Soil Sciences Department, California Polytechnic State University, 1 Grand Avenue, San Luis Obispo, CA 93407, USA.
Environ Pollut. 2008 Sep;155(1):132-40. doi: 10.1016/j.envpol.2007.10.026. Epub 2007 Dec 11.
It is important to examine mechanisms of Pb and Cd sorption in soils to understand their bioavailability. The ability of three tropical soils to retain Pb, Cd, and Ca was evaluated. The objectives of this study were to (1) determine the extent to which soil sorption sites are metal specific, (2) investigate the nature of reactions between metals and soil surfaces, and (3) identify how metals compete for sorption sites when they are introduced to soils sequentially or concurrently. Lead was shown to be much less exchangeable than Cd and inhibited Cd sorption. Cadmium had little effect on Pb sorption, though both Ca and Cd inhibited the adsorption of Pb at exchange sites. Lead appears to more readily undergo inner-sphere surface complexation with soil surface functional groups than either Cd or Ca. Thus, regardless of when Pb is introduced to a soil, it should be less labile than Cd.
研究土壤中铅和镉的吸附机制对于了解它们的生物有效性很重要。评估了三种热带土壤对铅、镉和钙的保留能力。本研究的目的是:(1)确定土壤吸附位点对金属的特异性程度;(2)研究金属与土壤表面之间反应的性质;(3)确定当金属依次或同时引入土壤时,它们如何竞争吸附位点。结果表明,铅的可交换性远低于镉,并且会抑制镉的吸附。镉对铅的吸附影响较小,不过钙和镉都会抑制铅在交换位点的吸附。与镉或钙相比,铅似乎更容易与土壤表面官能团发生内层表面络合。因此,无论何时将铅引入土壤,它的活性都应低于镉。