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MONITORING OF ACTUAL STATUS AND DEVELOPMENT OF ACTIVE ALUMINIUM IN SOILS IN SLOVAKIA

机译:斯洛伐克土壤的实际状况监测和活性铝的发育

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Active aluminium contents in agricultural soils of Slovakia were evaluated in the frame of partial-monitoring system - soil. The soil samples were taken in 5 years regular intervals from depths of 0-0.10 and 0.35-0.45 m. In the dry homogenised samples, soil reaction (pH in CaCl2), exchangeable cation Ca2+ and active Al content by Sokolov (soil is extracted with 1 N KCl and Al is precipitated with NaF) in the samples with pH value lower than 6.0 were measured. Active Al content was in the range 0.10-684.0 mg/kg with the average value 59.28 mg/kg and median value 8.30 mg/kg in the depth 0-0.10 m. In the depth 0.35-0.45 m, the average value was 59.30 mg/kg and the median value was 9.00 mg/kg. Significant differences in average and median values between the arable land and permanent grassland are determined as a consequence of the relationship between soil quality and its use. The increase in the active aluminium content (between first and last monitoring cycles) was determined in the group Podzols, Lithic Leptosols used as the permanent grassland as well as in the group Cambisols on the crystalline rocks and in the group Fluvisols used as arable land.
机译:在部分监测系统-土壤框架下,评估了斯洛伐克农业土壤中的活性铝含量。在5年内定期从0-0.10和0.35-0.45 m深度采集土壤样品。在干燥的均质样品中,测量pH值低于6.0的样品中的土壤反应(CaCl2中的pH),可交换阳离子Ca2 +和活性物质的含量(用1 N KCl萃取土壤,并用NaF沉淀铝)。活性Al含量在0.10-684.0 mg / kg的范围内,在0-0.10 m深度处的平均值为59.28 mg / kg,中值为8.30 mg / kg。在0.35-0.45 m深度处,平均值为59.30 mg / kg,中值为9.00 mg / kg。由于土壤质量及其用途之间的关系,确定了耕地和永久草地之间的平均值和中位数存在显着差异。在Podzols组,用作永久草地的锂瘦小白溶胶以及在结晶岩石上的Cambisols组以及在用作耕地的Fluvisols组中确定了活性铝含量的增加(在第一个监测周期和最后一个监测周期之间)。

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