水蚀对中部黑钙土结构团聚体中不稳定腐殖物质结构和含量的影响

I. Vasenev, N. Gorbunova, A. Gromovik, T. Devyatova
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引用次数: 0

摘要

研究了在侵蚀发展过程中,在斜坡型地形条件下,浸出黑钙土(Voronic chernozems Pachic,根据WRB-2014)的结构集料组成、有机化合物Corg和不稳定腐殖物质(LHS)在碳结构集料组分中的分布。这项工作是在沃罗涅日地区北部的悬链带上进行的,悬链带包括一段分水岭,平滑地变成了一个约1500米长、5˚陡的西南斜坡。对链状带以下部分的土壤进行了研究:1)分水岭部分;2) 斜坡的上部;3) 斜坡的中间部分。研究表明,在侵蚀的黑钙土中,结构聚集体状态发生退化,伴随着微观结构的恶化、中聚集体数量和结构系数的减少,以及防水结构的损失。结果表明,LHS在保持黑钙土水分稳定结构方面起着非常重要的作用。对Corg含量的最显著贡献是粒径为5-1mm的中聚集体,这些中聚集体在侵蚀发展过程中主动损失。
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Influence of water erosion on the structure and content of labile humic substances in the structural-aggregate fractions of leached chernozems of the Central Chernozem region
The structural-aggregate composition of leached chernozems (Voronic Chernozems Pachic according to WRB-2014), the distribution of organic compounds Corg and labile humic substances (LHS) in the structural-aggregate fractions of carbon in the conditions of a slope type of terrain during the development of erosion were studied. The work was carried out in the northern part of the Voronezh region on the catena, which included a section of the watershed, smoothly turning into a southwestern slope about 1500 m long and 5˚ steep. The soils of the following sections of the catena were studied: 1) the watershed part; 2) the upper part of the slope; 3) the middle part of the slope. It was shown that degradation of the structural-aggregate state occurs in eroded chernozems, accompanied by a deterioration in microstructurality, a decrease in the number of mesoaggregates and a structural coefficient, as well as a loss of a water-resistant structure. According to the results, LHS play a very important role in maintaining the water-stable structure of chernozems. The most significant contribution to the content of Corg contribute mesoaggregates 5-1 mm in size, which are actively lost during the development of erosion.
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