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应用扁平溶度计考察了一个水青冈林 (Fageta paupera)的重力土壤溶液 ,该森林位于克里尼奇克·沃奇山脉 (斯洛伐克中部 )的生态实验站 (EES)。逐月采集土壤表层以及 10 cm和 15 cm土壤矿质层的土壤渗透液化学特征的样品。同时 ,采集各层的土壤样品 ,并分析其中的 Ca,Mg,K和 Na等 4个化学元素 ,并测定 p H值和传导力。一年中矿质土层中阳离子积累量如下 :Ca分别为 2 .6 kg· hm- 2 和 14.2 kg· hm- 2 ,Mg分别为 2 .1kg· hm- 2 和1.1kg· hm- 2 ,K分别为 42 .1kg· hm- 2 和 2 .3 kg· hm- 2 ,Na分别为 5 .5 kg· hm- 2 和 2 .0 kg· hm- 2 。
A gravimetric solver was used to examine a gravity soil solution from the Fageta paupera located at the Ecological Experiment Station (EES) in the Krynichk Vori mountains (central Slovakia). Samples of the soil surface chemistry as well as the chemical characteristics of soil permeate from the 10 cm and 15 cm soil mineral layers were collected monthly. At the same time, the soil samples of each layer were collected and analyzed for four chemical elements, Ca, Mg, K and Na, and the p H value and conductivity were measured. The accumulation of cations in mineralized soil in a year was as follows: Ca2.6kg · hm-2 and 14.2kg · hm-2, respectively, with Mg1.2kg · hm-2 and1.1kg · hm-2, respectively Respectively, 42.1kg · hm -2 and 2.3kg · hm -2, and Na were 5.5 kg · hm -2 and 2.0 kg · hm -2, respectively.