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Comparison of methods for soil acidity measurement in Nyirlugos (Hungary) long-term field expriment

机译:NYIR​​ Lugos(匈牙利)长期田间实验中土壤酸度测量方法的比较

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Soil acidification and the amelioration of acidic soils is a world wide problem. Acid soils occupy approximately 30% of the world's ice free land area. The knowledge of the exact value of soil acidity is important because of lime requirement estimation, thus the amelioration and protection of soils. In Hungary and in some other countries the CaCO_3 amount needed to ameliorate acid soils is calculated by considering their hydrolytic acidity (y1). In the measurement suggested by Kappen (1929) the acidity of the equilibrium solution of the soil's Ca-acetate extract is quantified. The amount of acidity titrated in the equilibrium solution depends on the acidity of the soil and on the suspension pH. To determine the total releasable surface acidity the soil must be continuously percolated or the soil/extractant ratio must be changed. For the elimination of this principle error of Kappen's method the soil acidity can be determined by the pH-stat titration of the soil suspension. Our results show that thenew method can characterise quantitatively soil acidity thus it can give the basis for the lime requirement calculation.
机译:土壤酸化和酸性土壤的改善是世界各地的问题。酸性土壤占据世界冰块地区的约30%。由于石灰要求估算,土壤酸度确切值的知识是重要的,因此土壤的改善和保护。在匈牙利和其他一些国家,通过考虑其水解酸度(Y1)来计算改变酸性土壤所需的CaCO_3。在Kappen(1929)建议的测量中,量化了土壤的Ca-乙酸盐提取物的平衡溶液的酸度。在平衡溶液中滴定的酸度的量​​取决于土壤和悬浮液pH的酸度。为了确定总可释放的表面酸度,必须连续渗滤土壤或者必须改变土壤/萃取液比。为了消除κ的方法的这种原理误差,土壤酸度可以通过土壤悬浮液的pH-统计滴定来确定。我们的结果表明,此方法可以在定量的土壤酸度表征定量土壤酸度,因此它可以赋予石灰要求计算的基础。

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