Breuer K, Melzer A
Limnologische Station, D-8127, Iffeldorf, Federal Republic of Germany.
Institut für Botanik und Mikrobiologie der Technischen Universität München, Arcisstr. 21, D-8000, München 2.
Oecologia. 1990 Apr;82(4):468-473. doi: 10.1007/BF00319787.
Chemical equilibrium of ion exchange reactions of Sphagnum mosses was investigated for four different combinations of ions. These combinations were: Pb/Ca; Cd/Ca; Pb/K; Cd/K. Based on the law of mass action one can find mathematical descriptions of ion exchange reactions which permit one to calculate a state of equilibrium. As a measure of ion selectivity a rational coefficient of selectivity can be used. For culture experiments three different species of Sphagnum originating from a bog ("Hochmoor") in southern Bavaria were used. With these species coefficients of selectivity of the mentioned heavy metals were determined in solutions of different total ion content. Furthermore for each test solution of fixed total concentration the portions of the ions were altered. The Sphagnum material shows the behaviour of a relative ideal ion exchanger, whose states of equilibrium can be well described by the mathematical equations. The coefficients of selectivity are independent of Sphagnum species. In all cases they reflect the preferred binding of lead to the exchanger. Cadmium and calcium are adsorbed in approximately equivalent amounts. Representative limit isotherms permit an estimation of the errors caused by variation of the rational coefficients of selectivity. The applicability of the determined interactions and regularities on heavy metal monitoring programs is discussed.
针对四种不同的离子组合,研究了泥炭藓离子交换反应的化学平衡。这些组合分别是:铅/钙;镉/钙;铅/钾;镉/钾。根据质量作用定律,可以找到离子交换反应的数学描述,从而能够计算平衡状态。作为离子选择性的一种度量,可以使用合理的选择性系数。在培养实验中,使用了源自巴伐利亚南部一个沼泽(“高位沼泽”)的三种不同泥炭藓物种。利用这些物种,在不同总离子含量的溶液中测定了上述重金属的选择性系数。此外,对于每种固定总浓度的测试溶液,改变离子的比例。泥炭藓材料表现出相对理想离子交换剂的行为,其平衡状态可以用数学方程很好地描述。选择性系数与泥炭藓物种无关。在所有情况下,它们都反映了铅优先与交换剂结合。镉和钙的吸附量大致相当。代表性的极限等温线允许估计由合理选择性系数变化引起的误差。讨论了所确定的相互作用和规律在重金属监测计划中的适用性。