Occasional Flooding Impact On Heavy Metals Content In The Soil Of Polder Beša

B. Šoltysová, J. Hecl, L. Kováč, M. Danilovič
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Abstract

Abstract Three plots in Dry Polder Beša in Slovakia (E) and 3 plots in no flooded area (R) were chosen to assess the Cd, Pb and Ni contamination in the soil by using geo-accumulation index (Igeo) and anthropogenic contribution rate (ACR). Heavy metals content was measured at three depths (0‒0.2 m, 0.2‒0.4 m and 0.4‒0.6 m). It was found that the average content of Pb was 1.4 times higher and content of Ni 2.3 times higher at experimental area than at reference area. The average content of Cd were on the same level (E - 0.040 mg/kg, R - 0.041 mg/kg). The variability of heavy metals content in the soil was significantly influenced by soil depth and sampling plot and concentrations significantly correlated with soil organic carbon content (r - in the range of 0.41 to 0.65, p < 0.05). Geo-accumulation index indicates that the soils in the all of studied plots were polluted with respect to Ni, while were unpolluted with respect to Cd and Pb. Cd and Pb occurrence in these soils may be associated to the geochemical weathering. The value of the ACR indicate that anthropogenic input of Ni was 1.331 times higher in flooded area than in reference no flooded area. Different soil types can be arranged in descending Igeo values for Ni as follows: Luvisols ˃ Regosols ˃ Gleysols ˃ Chernozems. It was found that the content of Ni and Pb exceeded the critical values, in relation to transfer of contaminants from the soil to the plant , only at flooded area.
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偶尔洪水对圩田土壤重金属含量的影响Beša
选取斯洛伐克干旱区Beša 3个样地(E)和无水患区3个样地(R),采用地累积指数(Igeo)和人为贡献率(ACR)对土壤Cd、Pb和Ni污染进行评价。在0 ~ 0.2 m、0.2 ~ 0.4 m和0.4 ~ 0.6 m 3个深度测量重金属含量,发现试验区Pb平均含量比对照区高1.4倍,Ni平均含量比对照区高2.3倍。Cd的平均含量E - 0.040 mg/kg, R - 0.041 mg/kg。土壤重金属含量变异性受土壤深度和样地影响显著,与土壤有机碳含量呈显著相关(r -在0.41 ~ 0.65范围内,p < 0.05)。地积指数表明,所有研究样地的土壤Ni均受到污染,Cd和Pb未受污染。这些土壤中Cd和Pb的赋存可能与地球化学风化有关。ACR值表明,洪涝区人为输入的Ni是参考无洪涝区人为输入的1.331倍。不同土壤类型的Ni依Igeo值降序排列为:露壤型、雷土型、灰壤型、黑钙土型。研究发现,仅在淹水地区,土壤中Ni和Pb的含量超过了污染物向植物转移的临界值。
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