在可持续管理的背景下提取泥炭地的泥炭特性特征

IF 2.6 Q1 GEOGRAPHY Folia Geographica Pub Date : 2019-01-01 DOI:10.22364/fg.17.6
Reinis Bitenieks, L. Kalniņa, Ingrīda Krīgere, J. Dreimanis
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引用次数: 0

摘要

提取泥炭地的退化程度和重新耕作的可能性通常是利用来自植被研究的数据和部分来自水文测量的数据来评价的。对剩余泥炭层性质的关注很少;然而,这对于规划和选择复育方案是很重要的。本研究的目的是研究剩余泥炭部分的性质,特别关注顶层。本研究项目包括以下实验室方法:燃失法、pH值、泥炭分解程度、植物组成和天然泥炭密度分析。这项研究的结果指出,由于提取过程,泥炭的性质正在发生变化。研究结果表明,受影响泥炭地的泥炭性质存在差异。泥炭剖面的顶层具有较高的自然密度和增加的矿物质量。观察到的主要变化是泥炭的自然水分、pH值、矿物质含量、降解率和灰分含量,在提取的泥炭田中,这些变化与水文制度的改变有关。
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Characteristics of peat properties from extracted peatlands in the context of sustainable management
The degradation level and re-cultivation possibilities of extracted peat fields have usually been evaluated using data from vegetation studies, and partly from hydrological measurements. Very little attention has been paid to the remaining peat layer properties; however, this is important for the planning and choice of scenario for re-cultivation. The aim of this study has been to investigate the properties of the remaining peat section with special attention to the top layer. This research project included the following laboratory methods: loss – on ignition method, pH, degree of peat decomposition botanical composition and natural peat density analysis. The results of this study point to those peat properties that are changing due to extraction processes. The obtained results suggest that peat properties in the studied affected peatlands vary differently. The top layers of the peat section have a higher natural density and increased amount of mineral matter. The main changes observed were in the peat natural moisture, pH, mineral content, degradation rates, and ash content, which in the extracted peat field were associated with hydrological regime modification.
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来源期刊
Folia Geographica
Folia Geographica GEOGRAPHY-
CiteScore
4.60
自引率
30.80%
发文量
0
审稿时长
18 weeks
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