Landscapes of loessial islands in high Novgorod-Siversky Polissia

S. Kanivets, Yu. V. Zalavskiy, V. Lebed
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Abstract

The territory of Novgorod-Siversky Polissia is characterized by natural conditions as a province of mixed forests, where soddy-podzolic soils of low fertility have formed on loamy sandy and sandy deposits. However, on the high plateau the Desna River valley right bank, there are Novgorod-Siversky and Ponornitsky loessial islands with fertile dark-colored soils (Opillia). They were formed in rather damp and cool conditions, which is natural for the forest zone. However, their landscapes by the property of the components have a forest-steppe nature. On the plateau, in the Novgorod-Siversky Opillia, eolian loessial is located, which led to the formation of dark gray podzolized soils and chernozems leached and podzolized mainly with a humus-degraded arable layer. On sufficiently large areas near localities Pontornytsya, Pokoshychi and Desnianske there was happened loessivation and silt-loam sandy. Fertile gray forest soils were formed here – a kind of Opillia region. During the large-scale survey and mapping of Ukraine's soils in 1957–1961, dark-colored soils of loessial islands were defined predominantly as dark gray podzolized. However, our recent studies have proved the widespread distribution of leached chernozems and podzolized opіlsky chernozems. On strongly eroded slopes of the right-bank native shores, we have remnants of the suboak forest, which indicate the forest-steppe nature of the landscapes. In virgin areas, unlike sandy areas, a thick bean-grass-mixed grass cover, including indicators of forest-steppe. The Opillia area with chernozems and other dark-colored soils is a major agrarian resource of the region. But gray forest soils also belong to the most valuable land in Polissia. On gray forest soils, cereal crops are grown by 4–5 centners per hectare higher than those on typical of the Polissia sod-podzolic soils. Loessial islands are common in southern part of Novgorod-Siversky Polissia, in particular, on the Desna River valley right bank. Landscapes are diverse in properties of components – the nature of loessial species, geological foundations, features of soil cover and relief. They are united by forest-steppe features of soil cover, the presence in the central part of Opilia – fertile dark-colored soils, including chernozems with signs of relic steppe phase in their development, meadow-steppe composition of herbaceous cover on virgin areas and the presence of remnants of the suboak forest. These are large fragments of the Forest-Steppe in Polissia, which have a high natural resource.
高诺夫哥罗德-西沃斯基波兰的黄土岛屿景观
诺夫哥罗德-西沃斯基波兰境内的自然条件是一个混交林省,在那里,低肥力的钠灰化土在壤土和沙质沉积物上形成。然而,在德斯纳河河谷右岸的高原上,有诺夫哥罗德-西沃斯基和波诺尼茨基黄土岛,具有肥沃的深色土壤(Opillia)。它们是在相当潮湿和凉爽的条件下形成的,这对森林地区来说是很自然的。然而,它们的景观由组成部分的性质具有森林草原的性质。在高原上,诺夫哥罗德-西沃斯基盆地为风成黄土,形成深灰色灰化土,黑钙土以腐殖质退化的可耕地层为主。在Pontornytsya, Pokoshychi和Desnianske附近足够大的地区发生了黄土化和粉砂质壤土。这里形成了肥沃的灰色森林土壤——一种奥菲利亚地区。在1957-1961年乌克兰土壤大尺度测绘中,黄土岛深色土壤主要被定义为深灰色灰化土。然而,我们最近的研究表明,淋溶黑钙土和灰化黑钙土分布广泛。在右岸原生海岸被严重侵蚀的斜坡上,我们有水下森林的遗迹,这表明了森林草原的景观性质。在原始地区,与沙质地区不同,有一层厚厚的豆草混合草覆盖,包括森林草原的指标。奥菲利亚地区黑钙土和其他深色土壤是该地区的主要农业资源。但是灰色的森林土壤也属于波兰最有价值的土地。在灰色森林土壤上,谷类作物每公顷的生长比在典型的波兰草灰土壤上高出4-5个中心。黄土岛在诺夫哥罗德-西沃斯基波兰南部很常见,特别是在德斯纳河谷右岸。景观在组成部分的性质上是多种多样的——黄土物种的性质、地质基础、土壤覆盖和地形的特征。它们是由森林-草原的土壤覆盖特征,在Opilia -肥沃的深色土壤的中心部分的存在,包括黑钙土,在其发展过程中有遗迹草原阶段的迹象,在原始地区草本覆盖的草甸-草原组成,以及亚速林的残余存在。这些是波兰森林草原的大片,拥有丰富的自然资源。
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