LANDUSE FEATURES IN A MOUNTAIN AREA AND THEIR EFFECTS ON THE PROCESS OF SYLVATISATION (STRYY DISTRICT LVIV REGION)

O. Lenevych, Z. Pankiv
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Harsh weather conditions and low soil fertility significantly impacted the further agricultural land uses in the mountainous region. However, wide-scale decline of agricultural lands occurred in the period of the collapse of the former USSR due to decline of collective and state farms. As a result of denationalization with subsequent privatization of agricultural lands there are nowadays 31 303 land owners and land users in the study area, 97,54 % of which are physical persons. At the same time, despite such remarkable figures citizens share less than a half of total lands for agriculture, residential and construction purposes, whilst the state forestry enterprises are using 51,11 % (75 173,50 ha) in total. In contrast to lowlands, animal farming and husbandry in the Skole District is held exclusively by households. In recent years local animal husbandry is experiencing the livestock decline that leads to certain reduction in the share of both hay meadows and pasturelands. Thus, from 2009 to 2016 the total area of fodder lands in the district decreased by 65 ha (ca. 0,2 % of total privately owned agricultural lands). I assume that ongoing land reform will cause further increase in fallows in the Skole District.\nIn order to better comprehend the processes of spontaneous reforestation (sylvatisation) in a mountain region (the Pohartsi boundary, Koziova village, Stryi district, Lviv regionthe ) four study plots were selected representing the successional sequence: forest → pasture → hay meadow → arable lands. The study showed that areas that were previously used for pasture and were not plowed, are restored to their natural state much faster. These areas are characterized by satisfactory physical, physico-chemical and biotic properties. The decrease in acidity towards the neutral side is explained by an increase in the activity of catalase and urease by approximately 1.5 times. In connection with the developed grass cover, slightly higher nitrogen values were recorded in the upper soil horizon. Due to the absence of a regular annual supply to the base and replenishment of its nutrient reserves due to precipitation and waste of dead phytomass, the content of humus in the upper horizon of the base is half as much as under forest biogeocenoses. Plowing (overturning the lower horizons to the mountain, and vice versa) is a very strong anthropogenic factor, which leads to the almost complete destruction of natural vegetation on the cultivated area and a radical change in the main properties of the soil cover. According to some indicators: physical (total sparability), physico-chemical (nitrogen nitrate and ammonia), biotic (urease, catalase, biomass of microorganisms) in the upper humus horizons were even somewhat close to anthropogenically unaltered ecosystems. 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Moench., Rosa canina L., Bеtula and others\nKey words: land use; land owners and land users; fallows; agricultural lands; mountainous region; Skolivski Beskydy.","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"98 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-12-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.30970/gpc.2022.1.3861","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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Abstract

The Skole District that is nowadays a part of newly established Stryy District (Lviv Region) is entirely situated within the range of the Ukrainian Carpathians. Its area encompasses the Skolivsli Beskydy and the Stryy-San Highland physiographic regions featuring a dominance of considerably high altitudes above sea level, terrain disarticulation, and afforestation. Establishing new villages alongside rural population’s natural increase and land reforms (the capitalist stage of land use (after the abolition of serfdom in 1848) and Soviet stage of land use) called for respective increase in agricultural lands. Forested lands in the Ukrainian Carpathians were the source for such an increase therefore cropland and pasture lands were emerging from deforestation. Harsh weather conditions and low soil fertility significantly impacted the further agricultural land uses in the mountainous region. However, wide-scale decline of agricultural lands occurred in the period of the collapse of the former USSR due to decline of collective and state farms. As a result of denationalization with subsequent privatization of agricultural lands there are nowadays 31 303 land owners and land users in the study area, 97,54 % of which are physical persons. At the same time, despite such remarkable figures citizens share less than a half of total lands for agriculture, residential and construction purposes, whilst the state forestry enterprises are using 51,11 % (75 173,50 ha) in total. In contrast to lowlands, animal farming and husbandry in the Skole District is held exclusively by households. In recent years local animal husbandry is experiencing the livestock decline that leads to certain reduction in the share of both hay meadows and pasturelands. Thus, from 2009 to 2016 the total area of fodder lands in the district decreased by 65 ha (ca. 0,2 % of total privately owned agricultural lands). I assume that ongoing land reform will cause further increase in fallows in the Skole District. In order to better comprehend the processes of spontaneous reforestation (sylvatisation) in a mountain region (the Pohartsi boundary, Koziova village, Stryi district, Lviv regionthe ) four study plots were selected representing the successional sequence: forest → pasture → hay meadow → arable lands. The study showed that areas that were previously used for pasture and were not plowed, are restored to their natural state much faster. These areas are characterized by satisfactory physical, physico-chemical and biotic properties. The decrease in acidity towards the neutral side is explained by an increase in the activity of catalase and urease by approximately 1.5 times. In connection with the developed grass cover, slightly higher nitrogen values were recorded in the upper soil horizon. Due to the absence of a regular annual supply to the base and replenishment of its nutrient reserves due to precipitation and waste of dead phytomass, the content of humus in the upper horizon of the base is half as much as under forest biogeocenoses. Plowing (overturning the lower horizons to the mountain, and vice versa) is a very strong anthropogenic factor, which leads to the almost complete destruction of natural vegetation on the cultivated area and a radical change in the main properties of the soil cover. According to some indicators: physical (total sparability), physico-chemical (nitrogen nitrate and ammonia), biotic (urease, catalase, biomass of microorganisms) in the upper humus horizons were even somewhat close to anthropogenically unaltered ecosystems. However, the changes in the indicators of the density of the soil structure and its solid phase corresponded to the depth of plowing. And the humus content was several times lower than under forest biogeocenoses. Areas that were not plowed in the past are restored due to the main rock of the region Picea abies (L.) Karst.. Areas that were devastated in the past are recovering much more slowly. Such areas begin to overgrow with Alnus incana (L.) Moench., Rosa canina L., Bеtula and others Key words: land use; land owners and land users; fallows; agricultural lands; mountainous region; Skolivski Beskydy.
山区土地利用特征及其对森林化过程的影响(斯特里区利沃夫地区)
Skole区现在是新成立的Stryy区(利沃夫地区)的一部分,完全位于乌克兰喀尔巴阡山脉的范围内。它的区域包括Skolivsli Beskydy和Stryy-San高地地理区域,具有相当高的海拔,地形分离和植树造林的优势。随着农村人口的自然增长和土地改革(土地利用的资本主义阶段(1848年废除农奴制后)和土地利用的苏维埃阶段),建立新的村庄要求分别增加农业用地。乌克兰喀尔巴阡山脉的林地是这种增长的来源,因此农田和牧场正在从森林砍伐中出现。恶劣的气候条件和较低的土壤肥力显著影响了山区农业用地的进一步利用。然而,在前苏联解体期间,由于集体农场和国营农场的衰落,农业用地大规模减少。由于非国有化和随后的农业土地私有化,目前在研究地区有31 303名土地所有者和土地使用者,其中97,54%是自然人。与此同时,尽管有如此显著的数字,但公民用于农业、住宅和建筑目的的土地还不到总土地的一半,而国有林业企业总共使用了51.11%(75 173,50公顷)的土地。与低地不同,斯科勒区的畜牧业完全由家庭经营。近年来,当地畜牧业正在经历牲畜数量的减少,导致干草草地和牧场的份额有所减少。因此,从2009年到2016年,该地区的饲料用地总面积减少了65公顷(约占私有农业用地总面积的0.2%)。我认为正在进行的土地改革将导致斯科勒区的休耕面积进一步增加。为了更好地理解一个山区(Pohartsi边界,Koziova村,Stryi区,利沃夫地区)的自发再造林(造林)过程,选择了四个代表演替顺序的研究样地:森林→牧场→干草草甸→耕地。该研究表明,以前用作牧场而没有耕种的地区恢复到自然状态的速度要快得多。这些地区具有令人满意的物理、物理化学和生物特性。酸度向中性侧降低的原因是过氧化氢酶和脲酶的活性增加了约1.5倍。与发达的草被有关,上层土壤的氮值略高。由于基地没有每年定期的补给,也没有因降水和枯死植物质的浪费而补充其营养储备,因此基地上层的腐殖质含量只有森林生物地球群落的一半。翻耕(将较低的地平线翻到山上,反之亦然)是一个非常强烈的人为因素,它导致耕地上的自然植被几乎完全被破坏,土壤覆盖的主要性质发生了根本性的变化。根据一些指标:上层腐殖质层的物理(总疏疏性)、物理化学(硝酸氮和氨)、生物(脲酶、过氧化氢酶、微生物生物量)甚至在某种程度上接近于未受人为改变的生态系统。土壤结构密度和固相密度等指标的变化与耕深相关。腐殖质含量比森林生物地沼低几倍。由于该地区的主要岩石云杉(Picea abies) (L.),过去没有耕种的地区得以恢复。岩溶. .过去遭受破坏的地区恢复得要慢得多。这些地区开始长满白桤木(Alnus incana)。Moench。关键词:土地利用;土地所有人和土地使用者;法洛斯;农业用地;山区;Skolivski Beskydy。
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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