首页> 外文期刊>Journal of soil & sediments >The impact of restoration processes on the selected soil properties and organic matter transformation of mountain fens under Caltho-Alnetum community in the Babiogorski National Park in Outer Flysch Carpathians, Poland
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The impact of restoration processes on the selected soil properties and organic matter transformation of mountain fens under Caltho-Alnetum community in the Babiogorski National Park in Outer Flysch Carpathians, Poland

机译:恢复过程对波兰外弗希施喀尔巴阡山脉巴比戈尔斯基国家公园Caltho-Alnetum群落下山fen选定土壤特性和有机质转化的影响

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Purpose The objective of this study was to determine the impact of restoration processes on the selected soil properties and organic matter transformation of mountain fens under the Caltho-Alnetum community in the Babiogórski National Park in Outer Flysch Carpathians. Materials and methods Restoration processes were conducted on three degraded mountain fens in the Babiogórski National Park in Outer Flysch Carpathians, Poland. The degradation degree of soils was the criterion for the selection of habitats for further studies. To determine the influence of restoration processes on mountain fen soil properties and organic matter transformation, samples were collected in 2011 and 2013. The soil samples were assayed for pH, base cation concentration, hydrolytic acidity, organic carbon and total nitrogen content, total exchangeable base cation concentration, cation exchange capacity, and base saturation. Organic matter fractions were extracted by IHSS method. Quantitative and qualitative study of organic matter was based on fraction composition analysis and the ratio of humic acid carbon to fulvic acid carbon. The research results were statistically verified. Results and discussion Based on morphological and chemical properties, the studied mountain fen soils can be classified as Sapric Dranic Eutric Histosols and Sapric Dranic Dystric Histosols according to WRB guidelines (2015). Before restoration processes, the mountain fen soils subjected to a different water regime showed various contents of total nitrogen and organic carbon. The decreasing of the groundwater level was reflected in pH, calcium ion content, exchangeable base cation concentration, and base saturation. The increase of the groundwater level had influence on chemical properties of mountain fen soils such as pH, total exchangeable base cation concentration, hydrolytic acidity, cation exchange capacity, and base saturation. Three-year restoration processes did not cause significant changes in the composition of humic substance fractions. Conclusions Mountain fens under Caltho-Alnetum community are priority habitats in Babiogórski National Park in Outer Flysch Carpathians, Poland. These habitats responded to restoration processes in varying degrees depending on the extent of their degradation. The least degraded mountain fen was characterized by a short response time on the restoration processes. The reaction of higher degraded habitats was weaker.
机译:目的这项研究的目的是确定恢复过程对外部Flysch喀尔巴阡山脉Babiogrrski国家公园Caltho-Alnetum社区下山的选定土壤特性和有机物质转化的影响。材料和方法在波兰外弗希施喀尔巴阡山脉的巴比奥戈尔斯基国家公园,对三个退化的山进行了恢复过程。土壤的降解程度是选择生境进行进一步研究的标准。为确定恢复过程对山fen土壤性质和有机质转化的影响,于2011年和2013年收集了样品。对土壤样品进行了pH,碱阳离子浓度,水解酸度,有机碳和总氮含量,总可交换碱含量的测定。阳离子浓度,阳离子交换容量和碱饱和度。通过IHSS方法提取有机物馏分。对有机物的定量和定性研究是基于馏分组成分析和腐殖酸碳与富里酸碳的比率。研究结果经过统计学验证。结果与讨论根据WRB指南(2015年),根据形态和化学性质,所研究的山土壤可分为Sapric Dranic Eutric组织溶胶和Sapric Dranic Dystric组织溶胶。在恢复过程之前,经过不同水处理的山土壤显示出不同的总氮和有机碳含量。地下水位的降低反映在pH,钙离子含量,可交换的碱性阳离子浓度和碱性饱和度方面。地下水水位的升高对山土壤的化学性质如pH,总交换性阳离子浓度,水解酸度,阳离子交换能力和碱饱和度都有影响。三年的修复过程并未引起腐殖质组分组成的重大变化。结论Caltho-Alnetum群落下的山是波兰外弗希施喀尔巴阡山脉的Babiogrrski国家公园的优先栖息地。这些栖息地对退化过程的反应程度不同,具体取决于退化程度。退化最少的山的特征是对恢复过程的响应时间短。退化程度较高的生境的反应较弱。

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