Effect of forest site types on the exchangeable and water-soluble cations distribution in the soil profiles

G. Porębska, A. Ostrowska
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Abstract

Abstract The aim of this research was to assess the impact of forest site types on the ionic composition of the soil sorption complex and soil water extracts in a soil profile. Three forest site types: coniferous forest (CF), coniferous-deciduous forest (CDF), and deciduousconiferous forest (DCF), were selected for the studies. Three dominant soil types were distinguished on the studied plots: Haplic Podzol, Dystric Arenosol, and Dystric Cambisol. Calcium (Ca), magnesium (Mg), potassium (K), sodium (Na), and aluminium (Al) in the soil sorption complex and soil water extracts were determined. Ca is a dominant cation in the soil sorption complex in organic horizon, while Al in mineral soil horizons. The differences between forest site types in ionic composition of soil water extracts were observed, mainly in the organic horizon and the horizons below the rooting zone. The vegetation affected the Ca/Al and base cations to Al molar (BC/Al) ratios. The Ca/Al and the BC/Al molar ratios increased in the sequence of sites: CF < CDF < DCF.
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不同立地类型对土壤剖面交换性和水溶性阳离子分布的影响
摘要本研究的目的是评估不同立地类型对土壤剖面中土壤吸附复合物和土壤水提取物离子组成的影响。选取针叶林(CF)、针叶林-落叶林(CDF)和落叶针叶林(DCF) 3种立地类型进行研究。研究样地的优势土壤类型分为三种:单灰壤、单砂壤和单砂壤。测定了土壤吸附络合物和土壤水提取物中的钙(Ca)、镁(Mg)、钾(K)、钠(Na)和铝(Al)。钙离子是有机层土壤吸附复合物的优势阳离子,而铝离子是矿物层土壤吸附复合物的优势阳离子。不同立地类型土壤水提物离子组成存在差异,主要表现在有机层和生根区以下层。植被对Ca/Al和碱离子/Al摩尔比(BC/Al)有影响。Ca/Al摩尔比和BC/Al摩尔比的增大顺序为:CF < CDF < DCF。
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