东欧平原森林草原和草原带的土壤覆盖格局

IF 1.4 Q4 SOIL SCIENCE Soil Science Annual Pub Date : 2019-09-01 DOI:10.2478/ssa-2019-0018
N. Khitrov, M. Smirnova, N. Lozbenev, E. Levchenko, V. Gribov, D. Kozlov, D. Rukhovich, N. Kalinina, P. Koroleva
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引用次数: 11

摘要

东欧平原森林草原和草原带的土壤覆盖特征是在传统的自同构土壤地带性序列从北向南交替的背景下,通过大尺度和详细的土壤制图显示出不同的土壤组合,并在小尺度土壤图上清晰地显示出来。特定土壤覆盖形态的组成、形态和功能是由特定区域内的土壤形成因素决定的。通过传统和数字土壤制图方法,绘制了俄罗斯中部、卡拉什和伏尔加高地的基本土壤面积(详细比例尺)和基本土壤覆盖格局图(大比例尺)。在厚粘土质母质和自由排水条件下,以低对比土壤组合为主,背景为单粒黑钙土(壤质或粘土质,泛绿质),微地形凸元素为单粒黑钙土(壤质或粘土质,泛绿质),微地形凹元素为双粒黑钙土(壤质或粘土质,泛绿质)。在低渗透粘土沉积物浅埋条件下,土壤覆盖层包括黑钙土或部分剖面具有静止特征的Chernic Phaeozems,甚至包括Mollic Stagnosols。不同年龄的收缩膨胀粘土的存在导致了深埋黑钙土、垂直黑钙土、垂直黑钙土和(或)盆状黑钙土的形成。母质中可溶性盐的存在导致了由原生黑钙土或钠黑钙土和不同类型的黑钙土组成的土壤复合体的发育。
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Soil cover patterns in the forest-steppe and steppe zones of the East European Plain
Abstract The soil cover of the forest-steppe and steppe zones of the East European Plain is characterized by diverse soil combinations revealed during large-scale and detailed soil mapping against the background of a traditional zonal sequence of dominant automorphic soils alternating from the north to the south and clearly displayed on small-scale soil maps. The composition, configuration and functioning of particular soil cover patterns are determined by the soil forming factors acting within a given area. The elementary soil areas (detailed scale) and elementary soil cover patterns maps (large scale) of the Central Russian, Kalach, and Volga Uplands are created by both traditional and digital soil mapping methods. Low-contrasting soil combinations with the background Haplic Chernozems (Loamic or Clayic, Pachic) alternating with zooturbated Haplic Chernozems (Loamic or Clayic, Pachic) on convex elements of the microtopography and Luvic Chernozems (Loamic or Clayic, Pachic) on concave elements of the microtopography prevails under conditions of thick clay loamy parent materials and free drainage. Under conditions of shallow embedding by low-permeable clayey sediments, the soil cover includes Chernozems or Chernic Phaeozems with stagnic features in some part of the soil profile or even Mollic Stagnosols. The presence of shrink-swell clays of different ages leads to the formation of Bathyvertic Chernozems, Vertic Chernozems, Vertic Chernic Phaeozems and/or Pellic Vertisols. The presence of soluble salts in the parent material leads to the development of solonetzic soil complexes consisting of Protosodic or Sodic Chernozems and different types of Solonetzes.
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来源期刊
Soil Science Annual
Soil Science Annual SOIL SCIENCE-
CiteScore
2.50
自引率
6.70%
发文量
0
审稿时长
29 weeks
期刊介绍: Soil Science Annual journal is a continuation of the “Roczniki Gleboznawcze” – the journal of the Polish Society of Soil Science first published in 1950. Soil Science Annual is a quarterly devoted to a broad spectrum of issues relating to the soil environment. From 2012, the journal is published in the open access system by the Sciendo (De Gruyter).
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