在波兰北部的粘土-淤泥质土壤中作为附带过程的锈蚀

IF 1.4 Q4 SOIL SCIENCE Soil Science Annual Pub Date : 2021-12-31 DOI:10.37501/soilsa/143444
M. Świtoniak
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引用次数: 3

摘要

在波兰的土壤覆盖中,土蚀和锈蚀是两种最常见的土壤形成过程。粘土组分的积积层位在近似上被观察到。占波兰土壤的50%,而锈土约占14%,几乎占该国所有沙质土壤的一半。由于这两个过程的不同条件-主要是岩性-它们通常被认为是可分离的现象,导致形成两种不同类型的土壤-粘土-积土(WRB - Luvisols)和锈土(Brunic Arenosols)。然而,在某些土壤剖面中,特别是在覆盖冰川垄的沙子中形成的土壤剖面中,可以观察到这两种土壤形成过程的影响。该研究的目的是表征土壤的特征,其特征与粘土部分的光照(减少)和铁半氧化物的积累有关,这些铁半氧化物以铁涂层的形式在沙质材料中原位形成(锈化)。为了检查这些过程同时发生的频率,分析了波兰北部年轻冰川地区29个土壤剖面,其质地使这两个过程同时发生。在多达66%的病例中,发现了与这两个过程相关的特征。缺乏锈蚀的情况主要发生在可耕土壤中,这些土壤往往因侵蚀而变浅,或在残积层中有明显的水停滞。所研究的土壤大部分被分类为结构对比锈质粘土-淤泥质土(WRB - Abruptic Luvisols (Brunic))或层状锈质粘土-淤泥质土(WRB - lamellic Luvisols (Brunic))。因此,由冰碛下的覆盖砂形成的土壤中的这两个过程是相互补充的,A-Bv-Et-2Bt-2Ck形态(根据波兰土壤分类(PSC, 2019)指定的层位)的剖面应被视为完全形成且未受人类活动干扰。关键字
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Rustification as a collateral process in clay-illuvial soils of northern Poland
The lessivage (clay-illuviation) and rustifi cation are among the two most common soil-forming processes in soil cover of Poland. The horizons of illuvial accumulation of the clay fraction are observed in approx. 50% of Polish soils, while rusty soils constitute about 14% – that is almost half of all sandy soils in the country. Due to the different conditions of both processes – mainly lithological in nature – they are generally perceived as separable phenomena leading to the formation of two different types of soils – clay-illuvial soils (WRB – Luvisols) and rusty soils (Brunic Arenosols). However, in some soil profi les, especially those formed in sands covering glacial tills, the effects of both of these soil-forming processes are observed. The aim of the study was to characterize the soils with the features related to the illuviation (lessivage) of the clay fraction and the accumulation of iron sesquioxides in the form of iron coatings formed in-situ in the sandy material (rustifi cation). In order to check how often these processes take place simultaneously, 29 soil profi les with a texture enabling the simultaneous acting of both processes in the young glacial areas of northern Poland were analyzed. In as many as 66% of cases, the presence of features related to both processes were found. The lack of the rustifi cation was recorded predominantly in arable soils – often shallowed by erosion or with a clear stagnation of water in the eluvial horizons. Most of the studied soils were classifi ed as texturally contrasted rusty clay-illuvial soils (WRB – Abruptic Luvisols (Brunic)) or lamellic rusty clay-illuvial soils (WRB – Lamellic Luvisols (Brunic)). Thus, both processes in soils developed from cover sands underlying by glacial tills are complementary to each other, and the profi les of A-Bv-Et-2Bt-2Ck morphology (designation of horizons according to Polish Soil Classifi cation (PSC, 2019)) should be perceived as fully formed and undisturbed by human activity. Keywords
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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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