Agbenin John O
Department of Soil Science, Ahmadu Bello University, Zaria, Nigeria.
Sci Total Environ. 2002 Mar 8;286(1-3):1-14. doi: 10.1016/s0048-9697(01)00917-2.
Concern about heavy metal accumulation in agricultural soils under long-term application of phosphate fertilizers and organic wastes makes investigation of heavy metals in agricultural soils imperative. This study examines the total, available and chemical forms of lead (Pb) in a savanna soil after 50 years of continuous cultivation and application of NPK fertilizers and farmyard manure (FYM). Total Pb concentration ranged from 28 to 42 mg kg(-1) over 2-3 times more than the average Pb concentration of non-polluted soils worldwide. Available Pb was, however, less than 2 mg kg(-1) indicating that Pb in the soils was largely insoluble. There were no detectable concentrations of water soluble and organically-bound Pb fractions. On average, residual Pb accounted for over 80% of total Pb. Compared to the natural site, cultivation and fertilization with NPK and FYM increased total Pb concentration by 19 and 17%, respectively, or, on mass basis, by 10 and 35 kg ha(-1), respectively, after 50 years. Soil Pb showed strong linear relations with sand fraction and inorganic phosphorus in the soils. Thermodynamic equilibrium relations provided some indirect evidence that the control on soluble Pb appeared to be chloropyromorphite [Pb5(PO4)3Cl], an insoluble lead phosphate mineral.
长期施用磷肥和有机废弃物导致人们担忧重金属在农业土壤中的积累,因此对农业土壤中的重金属进行调查势在必行。本研究考察了在连续种植50年并施用氮磷钾肥料和农家肥(FYM)后,稀树草原土壤中铅(Pb)的总量、有效态和化学形态。总铅浓度在28至42毫克/千克之间,比全球无污染土壤的平均铅浓度高出2至3倍多。然而,有效态铅含量低于2毫克/千克,这表明土壤中的铅大部分不溶。水溶性和有机结合态铅组分的浓度未被检测到。平均而言,残留铅占总铅的80%以上。与天然场地相比,连续50年施用氮磷钾肥料和农家肥后,总铅浓度分别增加了19%和17%,按质量计算,分别增加了10和35千克/公顷。土壤铅与土壤中的砂粒组分和无机磷呈强线性关系。热力学平衡关系提供了一些间接证据,表明对可溶性铅的控制似乎是氯磷灰石[Pb5(PO4)3Cl],一种不溶性磷酸铅矿物。