Mountain recreation impact on changes in soil penetration resistance of spruce forests

Y. Ivanenko, Lobchenko Ganna, V. Yukhnovskyi
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Abstract

The uniqueness of the Carpathian Mountain Forest ecosystems, a large part of which belongs to nature conservation areas, attracts a significant number of visitors annually. Intensive tourist flow on popular hiking trails leads to recreational digression, topsoil compaction, development of erosion processes and deterioration of forests. The research aims to determine the impact of recreation as an external mechanical impact on soil compaction by determining the soil penetration resistance under the canopy of predominant spruce stands. For this purpose, soil penetration resistance was measured with a penetrometer along two hiking trails within the root layer of the soil at four measuring sites at different distances from the hiking trail. In general, under the canopy of a forest stand, the soil cover is not homogeneous and the obtained penetration resistance values are characterised by considerable variability. It was revealed that for the “Zelene village – Uhorski skeli rocks” hiking trail in the areas close to the path (up to 20 m) there is a significant increase in soil penetration resistance compared to remote areas: at a depth of 10 cm it doubles, at a depth of 20 cm – by 20-40%, but with further deepening, the penetration resistance level off. At the same time, for the more popular “To Mount Pip Ivan Chornohirskyi” hiking trail, in the area adjacent to the trailbed, the penetration resistance reaches 19.6 kg·cm-2 in the upper 10 cm layer, and at a depth of 30 cm, it peaks at 37.8 kg·cm-2 (over 3 MPa), which affects the root spatial distribution of spruce forests. Intensive erosion processes due to soil compaction with an increase in soil penetration resistance above 60 kg·cm-2 (~6 MPa) are observed on the trailbed. The practical significance of the results obtained, and the established patterns is to complement existing methods for assessing the degree of recreational digression in mountainous conditions and can be the basis for designing measures to regulate tourist flows and restore affected areas
山地游憩对云杉林土壤穿透性变化的影响
喀尔巴阡山脉森林生态系统的独特性,其中很大一部分属于自然保护区,每年吸引大量游客。热门徒步路线上密集的游客流量导致休闲偏离、表土压实、侵蚀过程的发展和森林的退化。本研究旨在通过测定优势云杉林分冠层下土壤渗透阻力,确定游憩作为外部机械影响对土壤压实的影响。为此,在距离徒步旅行路线不同距离的4个测量点,沿着两条徒步旅行路线在土壤根层内用渗透计测量土壤渗透阻力。一般来说,在林分冠层下,土壤覆盖物是不均匀的,所获得的渗透阻力值具有相当大的变异性。结果显示,对于“泽莱内村-乌尔斯基骷髅岩”徒步路线,在接近路径的区域(高达20米),与偏远地区相比,土壤渗透阻力显著增加:在深度为10厘米时,土壤渗透阻力增加一倍,在深度为20厘米时,土壤渗透阻力增加20-40%,但随着深度的进一步加深,渗透阻力趋于平稳。与此同时,对于比较受欢迎的“To Mount Pip Ivan Chornohirskyi”徒步路线,在步道相邻区域,10 cm以上的穿透阻力达到19.6 kg·cm-2, 30 cm深度的穿透阻力峰值为37.8 kg·cm-2(大于3 MPa),影响了云杉林根系的空间分布。由于土壤压实,土壤侵蚀过程剧烈,土壤渗透阻力增加到60 kg·cm-2 (~6 MPa)以上。所获得的结果和所建立的模式的实际意义是补充现有的山地条件下游憩偏离程度的评估方法,并可作为设计调节旅游流量和恢复受影响地区的措施的基础
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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