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Pedogenesis on volcanic rocks in protected landscape areas in Central and North Bohemia

机译:中波希米亚州和北波西米亚受保护景观区火山岩成岩作用

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The development of soil cover on volcanic rocks in Central and North Bohemia was analyzed. The study was performed in the protected landscape areas on basalt, andesite, and dolerite. Parent material was characterized on the basis of thin-section study. Petrography of the parent material makes it possible to document the differences in the texture, character, and amount of rock-forming minerals. All the studied sequences exhibit the same configuration of soil profiles but various thicknesses. The soil profiles were evaluated on the basis of particle size distribution, chemical properties, soil organic matter parameters, and mineral composition of clay fraction. The major specific pedogenic process in soils developed on volcanic rocks is weathering of parent material and development of the Bw horizon with the formation of mainly smectite from the group of swelling clay minerals. The results revealed differences in the formation of the Bw horizon which is significantly affected by the petrography of the parent material and local geological conditions. According to the type of volcanic rocks, the intensity of the developmental process of the Bw horizon is as follows: andesite (Ty?ovické skály) > dolerite (Záhrabská) > basalt (B?ezina).
机译:分析了中波希米亚州和北波西米亚州火山岩上的土壤覆盖变化。这项研究是在受保护的风景区上使用玄武岩,安山岩和白云石进行的。根据薄层研究对母体材料进行了表征。母体材料的岩相学可以记录成岩矿物的质地,特征和数量上的差异。所有研究的序列都显示出相同的土壤剖面构造,但厚度不同。根据粒度分布,化学性质,土壤有机质参数和粘土级分的矿物组成评估土壤剖面。在火山岩上发育的土壤中,主要的特定成岩过程是母体材料的风化和Bw层的发育,主要是由溶胀性粘土矿物组成的蒙脱石的形成。结果表明,Bw层位的形成差异受母体岩石学和当地地质条件的影响很大。根据火山岩的类型,Bw层的发育过程强度如下:安山岩(Ty?ovickéskály)>白云岩(Záhrabská)>玄武岩(Bezezina)。

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