SOILS OF THE EASTERN PRIOL’KHONYE ON THE COAST OF THE LAKE BAIKAL: CURRENT STATE AND USE

Q4 Agricultural and Biological Sciences
I. Belozertseva, D. N. Lopatina, N. Zvereva
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引用次数: 1

Abstract

In summer periods of 2015–2017 within the framework of complex expeditions in the eastern Priol’khonye soil geochemical researches were performed. More than 120 soil samples were collected for subsequent physical and chemical analyses. Ecological, chemical and physical properties of meadow and steppe soils of Ol’khon district were studied and the results are presented in the article. The research was conducted on the east coast of the Lake Baikal in its central basin, which is most visited by tourists. Several soil types can be found along the coast line and on gently sloped surface nearby, they are: castanozems, umbrisols, cambisols, gray soils, histic fluvisols gleyic, humic fluvisols gleyic, chernozems, umbric fluvisols, cambic fluvisols and other. Owing to a specific environmental conditions some original soil types (for example “chestnut soils”, “castanozems”) can be found nowhere else in the Irkutsk region but only here. The explored soil profiles are mainly thick and stony to various extent (from high to medium),these soils are sandy or sandy loams, rich in humus, predominantly with neutral and weakly alkaline reaction (pH), low content of nitrogen in relation to carbon content (C : N), that creates favorable conditions for preservation of the vegetable remains in meadow landscapes. The conducted research results revealed that soils near touristic tracks and also on the territory of the ancient settlement are polluted by heavy metals, and their content exceeds sanitary and hygienic standards. The ecological condition of soils at the present stage can be characterized as average degree of disturbance resulting from recreational activity. Geochemical barriers are represented by organic and alkaline ones. However, due to the sandy and sandy-loamy soil texture waters of the lake coastal zone can be polluted by heavy metals as well. Soils of meadow-boggy landscapes of the coastal area are not polluted by heavy metals as far as it is a hard-to-reach region for tourists using automobile transport.
贝加尔湖沿岸东部priol 'khonye的土壤:现状和利用
2015-2017年夏季,在普里奥尔孔耶东部复杂考察的框架下,开展了土壤地球化学研究。收集了120多个土壤样本,用于随后的物理和化学分析。本文对鄂尔多斯地区草甸和草原土壤的生态、化学和物理性质进行了研究。这项研究是在贝加尔湖中部盆地的东岸进行的,这里是游客最多的地方。沿海岸线及附近缓坡地表可发现几种土壤类型,分别为:甜壳土、伞状土、伞状土、灰土、块状土、腐殖质土、黑钙土、伞状土、形成质土等。由于特定的环境条件,一些原始的土壤类型(例如“栗子土”、“castanozems”)在伊尔库茨克地区其他地方找不到,只有在这里才有。所探索的土壤剖面以厚质、不同程度的石质(从高到中)为主,为砂质或砂质壤土,腐殖质丰富,pH值以中性和弱碱性为主,氮碳比(C: N)较低,为草甸景观中蔬菜残体的保存创造了有利条件。研究结果表明,旅游线路附近和古聚落境内的土壤受到重金属污染,其含量超过卫生标准。现阶段土壤的生态状况可以用娱乐活动造成的平均扰动程度来表征。地球化学屏障以有机屏障和碱性屏障为代表。然而,由于湖岸带砂质和砂质壤土的质地,水体也会受到重金属的污染。沿海地区草甸沼泽景观的土壤没有受到重金属的污染,因为这是一个游客使用汽车难以到达的地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.90
自引率
0.00%
发文量
15
审稿时长
8 weeks
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