СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ

Introduction The problem of forest fires is extremely relevant for Ukraine and for the world. Successful prediction of the occurrence and development of fires is possible only with a clear assessment of the structure of the forest litter and duff, which are among the main components of forest fuels....

Повний опис

Збережено в:
Бібліографічні деталі
Дата:2018
Автори: Voron, V. P., Sydorenko, S. H., Tkach, O. M.
Формат: Стаття
Мова:Українська
Опубліковано: Ukrainian Research Institute of Forestry and Forest Melioration named after G. M. Vysotsky (URIFFM) 2018
Теми:
Онлайн доступ:https://forestry-forestmelioration.org.ua/index.php/journal/article/view/15
Теги: Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
Назва журналу:Forestry and Forest Melioration

Репозитарії

Forestry and Forest Melioration
_version_ 1856543331682615296
author Voron, V. P.
Sydorenko, S. H.
Tkach, O. M.
author_facet Voron, V. P.
Sydorenko, S. H.
Tkach, O. M.
author_sort Voron, V. P.
baseUrl_str
collection OJS
datestamp_date 2019-04-22T11:36:56Z
description Introduction The problem of forest fires is extremely relevant for Ukraine and for the world. Successful prediction of the occurrence and development of fires is possible only with a clear assessment of the structure of the forest litter and duff, which are among the main components of forest fuels. The study of characteristics and features of forest litter formation will enable to predict more accurately its ability to combustion. Materials and Methods The object of the study was the litter in Scots pine forests in Ukrainian Polissya. The stocks of the litter were determined in pine stands not damaged by fires in northern and southern parts of the Rivne Polissya. In general, 11 sample plots (SP) were investigated in pure pine plantations of different ages. The stocks of the litter were estimated by fractions according to Rodin's method (Rodin & Bazievich 1965) in three organic horizons: the upper, litter – L; the middle, fermented – F and the lower, humic – H. The litter layer density was determined according to Kurbatsky's method, as the ratio of the stock of litter to the thickness of its layer. Results The stock of the litter increased with age of planting (r = 0.87; p = 0.05). Regression analysis revealed that 76 % of the litter stock was determined by its thickness (R? = 0.76; p = 0.05). Humidity in different layers of forest litter varied considerably. The lowest humidity was observed in the litter horizon L, which dries out the fastest. Layers F and H were wetter; it is characteristic that the bottom layer did not always have the highest humidity. One can assume that, on the one hand, for a small amount of precipitation due to the high density of the middle layer F moisture does not enter the deeper horizons. On the other hand, in this type of forest, horizon H was strongly permeated with roots of Scots pine and roots of the ground cover, which actively absorb moisture retained in this layer. Correlation dependence between the litter density and the age of the forest stand, which has the coefficient r = 0.73, was revealed. During the regression analysis, it was found that this dependence is approximated by the equation of y = 0.7458x + 15.47. The difference in litter density between different age classes may be significant. So, if in pine stands of 2nd–3rd age class the average density of the litter was 30.6–36.2 g·dm-3, then in 6th–7th age class the value was 74.8–97.3 g·dm-3, that is, it grew by 2.1–3.2 times. It has been established that there was a significant increase in the stocks of the middle and lower layers in pine stands after 50 years, which, in the conditions of prolonged drought and the occurrence of a surface fire, would pose a serious threat to the stand. Conclusions The Scots pine stands of Rivne Polissya have accumulated significant stocks of litter (from 11,700 to 86,200 kg·ha-1). In the pine forest, the distribution of the litter was found to be uneven: the largest volumes were registered near the tree trunk, and they decreased with the increase in distance from it. With increasing age of pine plantations, both the volumes and the density of the litter increased. The density of forest litter increased from 30.6 to 97.3 g·dm-3 for age classes from 2nd to 8th. Up to 50–60 years, the maximum density value was usually registered on the edge of the crown canopy, and in the older pine stands, near the trunk. During ontogenesis of pine forest stands, the ratio of forest litter stocks between the organic horizons has changed significantly. After 50 years, the proportion of F and H sharply increased. 6 Figs., 5 Tables, 15 Refs.
first_indexed 2026-02-08T08:01:32Z
format Article
id oai:ojs2.forestry-forestmelioration.org.ua:article-15
institution Forestry and Forest Melioration
language Ukrainian
last_indexed 2026-02-08T08:01:32Z
publishDate 2018
publisher Ukrainian Research Institute of Forestry and Forest Melioration named after G. M. Vysotsky (URIFFM)
record_format ojs
spelling oai:ojs2.forestry-forestmelioration.org.ua:article-152019-04-22T11:36:56Z STRUCTURE OF FOREST LITTER AS AN INDICATOR OF POTENTIAL FIRE RISK IN THE PINE FORESTS OF POLISSYA, UKRAINE СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ Voron, V. P. Sydorenko, S. H. Tkach, O. M. surface fires, forest litter, mineralization layers, litter moisture, litter volumetric weight низові пожежі, лісова підстилка, шари мінералізації, вологість підстилки, об’ємна маса підстилки Introduction The problem of forest fires is extremely relevant for Ukraine and for the world. Successful prediction of the occurrence and development of fires is possible only with a clear assessment of the structure of the forest litter and duff, which are among the main components of forest fuels. The study of characteristics and features of forest litter formation will enable to predict more accurately its ability to combustion. Materials and Methods The object of the study was the litter in Scots pine forests in Ukrainian Polissya. The stocks of the litter were determined in pine stands not damaged by fires in northern and southern parts of the Rivne Polissya. In general, 11 sample plots (SP) were investigated in pure pine plantations of different ages. The stocks of the litter were estimated by fractions according to Rodin's method (Rodin & Bazievich 1965) in three organic horizons: the upper, litter – L; the middle, fermented – F and the lower, humic – H. The litter layer density was determined according to Kurbatsky's method, as the ratio of the stock of litter to the thickness of its layer. Results The stock of the litter increased with age of planting (r = 0.87; p = 0.05). Regression analysis revealed that 76 % of the litter stock was determined by its thickness (R? = 0.76; p = 0.05). Humidity in different layers of forest litter varied considerably. The lowest humidity was observed in the litter horizon L, which dries out the fastest. Layers F and H were wetter; it is characteristic that the bottom layer did not always have the highest humidity. One can assume that, on the one hand, for a small amount of precipitation due to the high density of the middle layer F moisture does not enter the deeper horizons. On the other hand, in this type of forest, horizon H was strongly permeated with roots of Scots pine and roots of the ground cover, which actively absorb moisture retained in this layer. Correlation dependence between the litter density and the age of the forest stand, which has the coefficient r = 0.73, was revealed. During the regression analysis, it was found that this dependence is approximated by the equation of y = 0.7458x + 15.47. The difference in litter density between different age classes may be significant. So, if in pine stands of 2nd–3rd age class the average density of the litter was 30.6–36.2 g·dm-3, then in 6th–7th age class the value was 74.8–97.3 g·dm-3, that is, it grew by 2.1–3.2 times. It has been established that there was a significant increase in the stocks of the middle and lower layers in pine stands after 50 years, which, in the conditions of prolonged drought and the occurrence of a surface fire, would pose a serious threat to the stand. Conclusions The Scots pine stands of Rivne Polissya have accumulated significant stocks of litter (from 11,700 to 86,200 kg·ha-1). In the pine forest, the distribution of the litter was found to be uneven: the largest volumes were registered near the tree trunk, and they decreased with the increase in distance from it. With increasing age of pine plantations, both the volumes and the density of the litter increased. The density of forest litter increased from 30.6 to 97.3 g·dm-3 for age classes from 2nd to 8th. Up to 50–60 years, the maximum density value was usually registered on the edge of the crown canopy, and in the older pine stands, near the trunk. During ontogenesis of pine forest stands, the ratio of forest litter stocks between the organic horizons has changed significantly. After 50 years, the proportion of F and H sharply increased. 6 Figs., 5 Tables, 15 Refs. У соснових лісостанах північної та південної частин Рівненського Полісся поряд із визначенням запасів вивчали вологість та щільність (об’ємну масу) підстилки. Виявлено, що у міру зростання віку соснових насаджень збільшуються як запаси, так і щільність підстилки. У разі збільшення запасів підстилки зростають тривалість і максимальна температура горіння; збільшення щільності, навпаки, вповільнює швидкість горіння або унеможливлює його. Встановлено, що щільність підстилки зростає углиб профілю зі збільшенням частки безструктурної мортмаси. Таким чином коли структура підстилки стає менш пористою, зменшується доступ повітря і збільшується тривалість горіння. Ukrainian Research Institute of Forestry and Forest Melioration named after G. M. Vysotsky (URIFFM) 2018-02-05 Article Article application/pdf https://forestry-forestmelioration.org.ua/index.php/journal/article/view/15 10.33220/1026-3365.132.2018.115 Forestry and Forest Melioration; No. 132 (2018): Forestry and Forest Melioration; 115-123 Лісівництво і Агролісомеліорація; № 132 (2018): Лісівництво і Агролісомеліорація; 115-123 2663-4147 1026-3365 10.33220/1026-3365.132.2018 uk https://forestry-forestmelioration.org.ua/index.php/journal/article/view/15/16 Copyright (c) 2018 Forestry and Forest Melioration
spellingShingle низові пожежі
лісова підстилка
шари мінералізації
вологість підстилки
об’ємна маса підстилки
Voron, V. P.
Sydorenko, S. H.
Tkach, O. M.
СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title_alt STRUCTURE OF FOREST LITTER AS AN INDICATOR OF POTENTIAL FIRE RISK IN THE PINE FORESTS OF POLISSYA, UKRAINE
title_full СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title_fullStr СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title_full_unstemmed СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title_short СТРУКТУРА ПІДСТИЛКИ ЯК ПОКАЗНИК ПОТЕНЦІЙНОГО ПОЖЕЖНОГО РИЗИКУ В СОСНОВИХ ЛІСАХ ПОЛІССЯ
title_sort структура підстилки як показник потенційного пожежного ризику в соснових лісах полісся
topic низові пожежі
лісова підстилка
шари мінералізації
вологість підстилки
об’ємна маса підстилки
topic_facet surface fires
forest litter
mineralization layers
litter moisture
litter volumetric weight
низові пожежі
лісова підстилка
шари мінералізації
вологість підстилки
об’ємна маса підстилки
url https://forestry-forestmelioration.org.ua/index.php/journal/article/view/15
work_keys_str_mv AT voronvp structureofforestlitterasanindicatorofpotentialfireriskinthepineforestsofpolissyaukraine
AT sydorenkosh structureofforestlitterasanindicatorofpotentialfireriskinthepineforestsofpolissyaukraine
AT tkachom structureofforestlitterasanindicatorofpotentialfireriskinthepineforestsofpolissyaukraine
AT voronvp strukturapídstilkiâkpokaznikpotencíjnogopožežnogorizikuvsosnovihlísahpolíssâ
AT sydorenkosh strukturapídstilkiâkpokaznikpotencíjnogopožežnogorizikuvsosnovihlísahpolíssâ
AT tkachom strukturapídstilkiâkpokaznikpotencíjnogopožežnogorizikuvsosnovihlísahpolíssâ