泥炭化效应对不同粒度分布冻土中水相组成的实验评估

IF 0.3 Q4 GEOLOGY

Moscow University Geology Bulletin Pub Date : 2024-07-17 DOI:10.3103/s0145875224700303

R. G. Motenko, R. R. Davletova, E. S. Grechishcheva, A. G. Alekseev

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引用次数: 0

摘要

摘要本文介绍了对泥炭化程度在 3% 到 100% 之间（以 10% 为增量）、具有不同粒度分布的冻土中未冻结含水量（Ww）的实验研究结果。本文讨论了所获得的 Ww = f(t °C) 模式。估计了有机质含量在 0 至 -18°C 温度范围内形成水分相组成中的作用。研究主要考虑了泥炭化程度超过 50%（根据 GOST 25 100-2020 标准，土壤属于泥炭）的未冻水导致的水分变化规律。研究给出了在固定温度下，Ww 随泥炭化程度变化的规律。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Experimental Evaluation of the Peatification Effect on the Phase Composition of Water in Frozen Soils of with Different Grain Size Distributions

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Experimental Evaluation of the Peatification Effect on the Phase Composition of Water in Frozen Soils of with Different Grain Size Distributions

Abstract

The article presents the results of experimental studies of the unfrozen water content (W_w) in frozen soils with different grain size distributions with a degree of peatification from 3 to 100% (in increments of 10%). The obtained patterns W_w = f(t °C) are discussed. The role of the organic matter content in the formation of the phase composition of moisture in the temperature range from 0 to –18°C is estimated. The study primarily considers the patterns of moisture changes due to unfrozen water with a degree of peatification above 50%, when soils are referred to peat according to GOST 25 100–2020. The patterns of the change in W_w from the degree of peatification at fixed temperatures are given.

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来源期刊

Moscow University Geology Bulletin GEOLOGY-

CiteScore

0.60

自引率

25.00%

发文量

期刊介绍： Moscow University Geology Bulletin is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.