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Field soil pore water monitoring was applied in a highly heavy-metal contaminated area in SW Sardinia, Italy, as a direct, realistic measure of heavy metal mobility. The main chemistry of pore waters well reflects the local characteristics of soils, ranging from Ca–SO4 to (Ca)Mg–HCO3 to Ca(Na)–SO4(Cl), with a wide range of conductivity. The mobility of Zn and Pb is apparently controlled by equilibrium...
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