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首页> 外文期刊>Zeitschrift fur Arznei- und Gewurzpflanzen >CONTENT OF SELECTED ELEMENTS AND EXCHANGEABLE CATIONS IN SOILS DEVELOPED FROM GLACIO-LACUSTRINE SEDIMENTS OF SEPOPOLSKA PLAIN (NE POLAND)
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CONTENT OF SELECTED ELEMENTS AND EXCHANGEABLE CATIONS IN SOILS DEVELOPED FROM GLACIO-LACUSTRINE SEDIMENTS OF SEPOPOLSKA PLAIN (NE POLAND)

机译：从Sepopolska Plain的Glacio-Lapustine沉积物中产生的选定元素和可交换阳离子（Ne Poland）

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There are soils in northern part of the Masurian Lakeland and the Sepopolska Lowland that developed from fine-grained, glacio-lacustrine sediments and are now used as arable land. The purpose of this study was to determine the content of macro- and microelements, exchangeable cations and cation exchange capacity of the soils in a catenary sequence. The following soil properties were determined: particle-size distribution, pH, content of total organic carbon and total nitrogen, total content of Ca, Mg, K, P, Na, Fe, Mn, Zn and Cu and that of exchangeable cations (Ca2+, Mg2+, K+, H+, Na+). According to the Polish Soil Classification (2019), the soils on the top and in the upper parts of the slope in the studied catena were Humic vertisols, while the middle and lover parts of the slope comprised proper humic colluvial soils, and in the depression there were Murshic soils. According to the IUSS Working Group WRB (2015), the identified soils are Haplic Vertisols (Aric, Hypereutric, Endostagnic), Haplic Phaeozems (Aric, Colluvic) and Haplic Phaeozems (Aric, Colluvic, Pachic), Histosols (Hemic, Murshic, Eutric) and Histosols (Hemic, Murshic, Eutric, Mineralic). In the analysed soil catena, the soil texture as well as the distribution of macro- and microelements (except sodium and phosphorus) showed small variability between soil units. The soil's particle-size distribution in the catenary sequence hardly varied. Contrary to moraine areas, there was no significant enrichment of colluvial soils with the clay and silt granulometric fractions. The main factors determining the distribution of macro- and microelements in the surface horizons of soils developed from clay is the process of vertilization and homogenization of soil material by mixing it during plowing. The amounts of exchangeable cations follow the order: Ca2+ > Mg2+ > H+ > K+ > Na+, with the highest content of base cations, cation exchange capacity and the highest base saturation in hemi-murshic soils. The research has confirmed the validity of distinguishing soils covered with mineral or mineral-organic sediments in the taxonomy of Polish soils.
机译：Masurian Lakeland的北部有土壤，以及从细粒度，冰川曲线沉积物开发的Sepopolska低地，现在用作耕地。本研究的目的是确定脉链序列中土壤的宏观和微量元素，可交换阳离子和阳离子交换能力的含量。测定以下土壤性质：粒度分布，pH值，总有机碳的总含量和总氮气，Ca，Mg，K，P，Na，Fe，Mn，Zn和Cu的总含量和可交换阳离子（Ca2 + ，mg2 +，k +，h +，na +）。根据波兰土壤分类（2019年），上面的土壤和研究的坡度上部的土壤是腐殖质的转甾醇，而坡度的中间和情人部分组成了适当的腐殖伞抗菌土壤，并且在抑郁症有误解的土壤。根据IUSS工作组WRB（2015），所识别的土壤是单级转溶胶（ARIC，SHOPEREC，ENDOSTAGNIC），单位氏植物（ARIC，Colaruvic）和单片鼠（ARIC，Colluvic，Pachic），组织醇（Hemic，Murshic，Eutric） ）和组织溶胶（Hemic，Murshic，Eutric，Mineralic）。在分析的土壤中，土壤纹理以及宏观和微量元素的分布（钠和磷除外）在土壤单元之间显示出小的变化。土壤在凸状序列中的粒度分布几乎不变。与冰碛地区相反，粘土和淤泥粒状分数没有明显富集的血管泥土。确定从粘土中产生的土壤表面视野中宏观和微量元素分布的主要因素是通过在耕作期间将土壤材料垂直和均质化的过程。可更换阳离子的量遵循顺序：Ca2 +> Mg2 +> H +> K +> Na +，具有最高含量的基阳离子，阳离子交换能力和半误差土壤中的最高基础饱和度。该研究证实了区分土壤覆盖着矿物质或矿物质 - 有机沉积物在波兰土壤的分类中的有效性。

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