To evaluate the effects of long-term applications of phosphorus fertilizers on mobility of dissolved organic matter(DOM) and heavy metals in agricultural soils,a sandy soil and a loamy soil were spiked with ammonium phosphate at application rates of 0,25,50,100,250,and 500 mg P per kilogram of soil.A series of 15-cm long soil columns were constructed by packing incubated soils of varying concentrations of P.The soil columns were consecutively leached by simulated rainfalls for six cycles.The contents of water extractable organic carbon in both sandy and loamy soils increased significantly with increasing rates of P applications.Relatively high rates of P applications could induce a marked increase in DOM concentrations in the leachates,the effects were larger with the sandy soil rather than with the loamy soil.Applications of P changed the partitioning of trace metals in the soil solids and the soil solutions.The increased P application rates also seemed to elevate the leaching of Cu,Cd,and Zn from soils.The concentrations of Cu,Cd,and Zn in the leachates were positively correlated with DOM,probably due to the formation of metal-DOM complexes.In contrast,Pb concentrations in the leachates were negatively correlated with DOM,and decreased with increasing rates of P applications.The boosted leaching of DOM induced by high rates of P applications was probably due to the added phosphate ions competing for adsorption sites in the soil solids with the indigenous DOM.
Soils can often be contaminated simultaneously by more than one heavy metal. The sorption-desorption behavior of a metal in a soil will be affected by the presence of other metals. Therefore, selective retention and competitive adsorption of the soils to heavy metals can affect their availability and movement through the soils. In this study, the simultaneous competitive adsorption of four heavy metals (Cd, Cu, Hg, and Pb) on ten agricultural soils collected from the Changjiang and Zhujiang deltas, China was assessed. The results showed that the competition affected the behavior of heavy metal cations in such a way that the soils adsorbed less Cd and Hg, and more Pb and Cu with increasing total metal concentrations, regardless of the molar concen- tration applied. As the applied concentrations increased, Pb and Cu adsorption increased, while Cd and Hg adsorption decreased. The adsorption sequence most found was Pb>Cu>Hg>Cd. The maximum adsorption capacity for the heavy metal cations was calculated, and affected markedly by soil properties. The results suggest that Hg and Cd have higher mobility associated to the lower adsorption and that Pb and Cu present the opposite behavior. Significant correlations were found between the maximum adsorption capacity of the metals and pH value and exchangeable acid, suggesting that soil pH and exchangeable acid were key factors controlling the solubility and mobility of the metals in the agricultural soils.
The soil factors influencing the potential migration of dissolved and particulate phosphorus(P) from structurally-weak sandy subsoils were evaluated by means of soil column leaching experiments. Soil colloids were extracted from two types of soils to make the colloid-bound forms of P solution. Eight sandy soils with diverse properties were collected for packing soil columns. The effects of influent solutions varying in concentrations of colloids,P,and electrolyte,on the transport of P and quality of leachates were characterized. P migration in the soils was soil property-dependent. High soil electrical conductivity values retarded the mobility of colloids and transportability of colloid-associated P(particulate P) . Soil electrical conductivity was negatively correlated with colloids and reactive particulate P(RPP) concentrations in the leachates,whereas,the total reactive P(TRP) and dissolved reactive P(DRP) concentrations in the leachates were mainly controlled by the P adsorption capacity and the P levels in the subsoil. The reactive particulate P in the leachates was positively correlated with the colloidal concentration. Increased colloidal concentration in the influent could significantly increase the colloidal concentration in the leachates. Elevated P concentration in the influent had little effect on P recovery in the leachates,but it resulted in significant increases in the absolute P concentration in the leachates.
