Monitoring of the current state of peatlands of the Western Polissia

Authors

DOI:

https://doi.org/10.33730/2310-4678.3.2024.314923

Keywords:

peatland, deposit CO2, degree of decomposition, ash content, West Polissia Wetland, Ukraine

Abstract

Among the minerals that our country is rich in, peat deposits are of significant importance. The latter are a complex multi-component and unique natural system that significantly affects the ecological state of the environment, especially in recent times of global warming. The article provides statistical data on peat reserves of Western Polissia (the northern part of the Volyn, Rivne oblast) in deposits of Ukraine and their properties are considered. Swamps and peat of the Western Polissia are a great natural resource, a center of carbon (carbon) deposition, a hydrological regulator, biotopes for the spread of rare species of biota, in particular with regard to marginal, boreal, postglacial species. The group composition of organic matter of upland and lowland type peat in the regions of Western Polissia was studied. Peat contains approximately 60% carbon and 40% oxygen, depending on composition and ash content, which was proven in the publication. Peat sediments primarily components and structural fragments, organic compounds from swamp plants. On the one hand, peat retains a certain ratio of fragments of varying degrees of preservation of the original plant phytogroup that form the macrostructure, and on the other hand, in the process of biotransformation, mineralization occurs at the same time — the breakdown of the most biodiversity components of plant tissues (proteins, fats, and carbohydrates) into simple substances (carbon dioxide and water), and humification — the formation of new high-molecular compounds — humic acids (HA). The materials provide data on the yield of humic acids from the investigated peat samples. The presence of HA in peat, which have valuable agrochemical properties and physiological activity, determine its use in agriculture. The conducted research confirms that preparations of peat humic acids can be used as a promising material for obtaining natural medicines for balneological, medical and veterinary purposes. Currently, peat resources are recognized as a unique natural potential of organic origin, which affects the sustainable development of the environment. With the development of science, it has become a reliable source in biotechnology, nature conservation, paleoecology, etc. It is important to note that peat resources are conditionally renewable, but it is advisable not to use peat as fuel, and it is better to do it in organic agriculture, bioenergy and resource production (palud culture — cranberry, blueberry, miscanthus; bioenergy species such as willow, paulownia, etc.) etc.

References

Konishchuk, V.V. (2015). Torfovi bolota [Peat swamps]. Kyiv: DIA [in Ukrainian].

Lishchenko, L.P., & Pazynych, N.V. (2016). Monitorynh stanu torfovyshch dlia vyiavlennia pozhezhonebezpechnykh dilianok za dopomohoiu dystantsiinykh metodiv [Monitoring the state of peatlands to identify fire-prone areas using remote methods]. Ukrainskyi zhurnal dystantsiinoho zonduvannia Zemli — Ukrainian Journal of Earth Remote Sensing, 8, 29–39 [in Ukrainian].

Pyavchenko, N.Y. (1985). Torfyanye bolota, ikh prirodnoe i khozyaystvennoe znachenie [Peat bogs, their natural and economic significance]. Moskva: Science [in Russian].

Siviy, M. (2012). Torfovi resursy Ukrayiny: suchasnyy stan, perspektyvy, vykorystannia [Peat resources of Ukraine: current state, prospects, use]. Naukovi zapysky — Proceedings, 1, 81–86 [in Ukrainian].

Derzhavna sluzhba statystyky Ukrainy (2008). Derzhavnyy balans zapasiv korysnykh kopalyn Ukrayiny na 01.01.2008 r. [State balance of mineral reserves of Ukraine as of January 1, 2008]. Kyiv [in Ukrainian].

Perminova, I.V. (2000). Analiz, klassifikatsiya i prognoz svoystv guminovykh kislot [Analysis, classification and prediction of the properties of humic acid]. Doctor’s thesis [in Russian].

Lopatin, V.D. (1949). O gidrologicheskom znachenii verkhovykh bolot [On the hydrological significance of raised bogs]. Vestnik Leningradskogo Gosudarstvennogo Universiteta — Bulletin of Leningrad State University, 2, 37–49. [in Russian].

Laichuk, O.V. (Ed.). (2000). Analiz stanu mineralno-syrovynnoi bazy Ukrayiny, oblik rodovyshch i skladannia Derzhavnykh balansiv zapasiv torfu ta sapropeliu za stanom na 1997–1999 rr.: zvit [Analysis of the state of the mineral and raw material base of Ukraine, accounting of deposits and compilation of state balances of peat and sapropel reserves as of 1997–1999: report]. Kyiv [in Ukrainian].

Truskavetskyi, R.S. (2010). Torfovi grunty i torfovyshcha Ukrainy [Peat soils and peatlands of Ukraine]. Kharkiv: Miskdruk [in Ukrainian].

Konishchuk, V.V. (Ed.), Pronevich, V.A., Yehorova, T.M., & Shumyhai, I.V. (2015). Ekolohichni osnovy zbalan sovanoho rozvytku landshaftiv vodno-bolotnykh uhid i torfovyshch: monohrafіiа [Ecological foundations of balanced development of wetlands and peatland landscapes: monograph]. Kyiv: DIA [in Ukrainian].

Konishchuk, V.V. (2012). Kontseptsiia i stratehiia zbalansovanoho rozvytku landshaftiv vodno-bolotnykh uhid i torfovykh ekosystem Ukrainy [Concept and strategy of balanced development of landscapes of wetlands and peat ecosystems of Ukraine]. Kyiv: DIA [in Ukrainian].

Lupinovich, I.S., & Golub, T.F. (1958). Torfyano-bolotnye pochvy BSSR i ikh plodorodie [Peat-bog soils of the BSSR and their fertility]. Minsk [in Russian].

Chambers, F.M. et al. (2012). Development and refinement of proxy-climate indicators from peats. Quaternary International, 268, 21–33 [in English].

Schellekens, J., & Buurman, P. (2011). n-Alkane distributions as palaeoclimatic proxies in ombrotrophic peat: The role of decomposition and dominant vegetation. Geoderma, 164, 112–121 [in English].

Izart, A. et al. (2012). Palaeoclimate reconstruction from biomarker geochemistry and stable isotopes of n-alkanes from Carboniferous and Early Permian humic coals and limnic sediments in western and eastern Europe. Organic Geochemistry, 43, 125–149 [in English].

Konishchuk, V.V. (2012). Metodyka paleoekolohichnykh doslidzhen vodno-bolotnykh, torfovykh vidkladiv [Methodology of paleoecological studies of wetlands and peat deposits]. Kyiv: Hlobus [in Ukrainian].

Yakist gruntu. Vyznachennia zolnosti torfu i torfovoho gruntu [Soil quality. Determination of ash content of peat and peat soil]. (2016). DSTU 7942:2015 from 22nd June 2002. Kyiv: DP “UkrNDNTS” [in Ukrainian].

Dombrovskaya, A.V., Koreneva, M.I., & Tyuremnov, S.N. (1959). Atlas rastitelnykh ostatkov, vstrechayemykh v torfe [Atlas of plant residues found in peat]. Gosenergoizdat [in Russian].

Konishchuk, V.V. (2012). Metodychni rekomendatsii z vyznachennia ekolohichnoi entropii, hemerobii, enerhetyky bolit i torfovyshch [Methodical recommendations for determining ecological entropy, hemeroby, energetics of swamps and peatlands]. Kyiv: DIA [in Ukrainian].

Losev, N.X., & Smagunova, A.N. (1982). Osnovy rentgenospektralnogo fluorestsentnogo analiza [Fundamentals of X-ray fluorescence analysis]. Moskva: Khimiya [in Russian].

Konishchuk, V.V. (2015). Entsyklopedychnyi dovidnyk: ekolohiia vodno-bolotnykh uhid i torfovyshch [Encyclopedic reference: ecology of wetlands and peatlands]. Kyiv: DIA [in Ukrainian].

Konishchuk, V.V. (2012). Ekoloho-henetychna klasyfikatsiia u vyznachenni rozvytku ta okhorony torfovyshch [Ecological and genetic classification in determining the development and protection of peatlands]. Naukovyi visnyk Natsionalnoho universytetu bioresursiv i pryrodokorystuvannia Ukrainy. Seriia: Lisivnytstvo ta dekoratyvne sadivnytstvo — Scientific Bulletin of the National University of Bioresources and Nature Management of Ukraine. Series: Forestry and decorative horticulture, 171, 1, 95–100 [in Ukrainian].

Bondar, O.I., & Konishchuk, V.V. (2011). Helolohiia: kontseptsiia rozvytku, metodolohiia, suchasna paradyhma vyvchennia bolit, torfovyshch ta yikh ekolohichna pasportyzatsiia [Helology: concept of development, methodology, modern paradigm of study of swamps, peatlands and their ecological certification]. Ahroekolohichnyi zhurnal — Agroecological journal, 2, 25–30 [in Ukrainian].

Haskevych, V. & Netsyk, M. (2013). Henetyko-heohrafichni osoblyvosti torfovykh gruntiv Maloho Polissia [Genetic and geographical features of the peat soils of Maly Polissia]. Visnyk Lvivskoho Universytetu — Bulletin of Lviv University, 42, 64–77 [in Ukrainian].

Inisheva, L.I., Shaydak, L. (2013). Geoekologiya i geokhimiya landshaftov. Nauka o zemle [Geoecology and geochemistry of landscapes. Geoscience]. Vestnik Tyumenskogo gosudarstvennogo universiteta — Bulletin of Tyumen State University, 4, 95–104 [in Russian].

Pereverzev, V.N. (1999). Khimicheskiy sostav i organicheskoe veshchestvo okulturennykh torfyanykh pochv Kolskogo poluostrova [Chemical composition and organic matter of cultivated peat soils of the Kola Peninsula]. Agrokhimiya — Agrochemistry, 11, 8–15 [in Russian].

Palamarchuk, I.K., Hrysiuk, M.M., & Hurin, I.I. (1986). Torfiano-bolotnyi fond: ratsionalne vykorystannia i okhorona [Peat-swamp fund: rational use and protection]. Kyiv: Urozhai [in Ukrainian].

Published

2024-08-22

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Articles