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Статті в журналах з теми "Natural peatlands"
Poulin, Monique, Line Rochefort, François Quinty, and Claude Lavoie. "Spontaneous revegetation of mined peatlands in eastern Canada." Canadian Journal of Botany 83, no. 5 (May 1, 2005): 539–57. http://dx.doi.org/10.1139/b05-025.
Повний текст джерелаRoganda, M. S., Sigit Heru Murti, and Wirastuti Widyatmanti. "Mapping the distribution of natural ecosystems on peatlands through vegetation using the object-based image analysis (obia) method in bangko district, rokan hilir regency, riau." IOP Conference Series: Earth and Environmental Science 1047, no. 1 (July 1, 2022): 012017. http://dx.doi.org/10.1088/1755-1315/1047/1/012017.
Повний текст джерелаSasmito, Sigit D., Pierre Taillardat, Letisha S. Fong, Jonathan W. F. Ren, Hanna Sundahl, Lahiru Wijedasa, Aditya Bandla, et al. "Terrestrial and Aquatic Carbon Dynamics in Tropical Peatlands under Different Land Use Types: A Systematic Review Protocol." Forests 12, no. 10 (September 23, 2021): 1298. http://dx.doi.org/10.3390/f12101298.
Повний текст джерелаSakuntaladewi, N., Y. Rochmayanto, Ramawati, M. Iqbal, and V. B. Arifanti. "Strategies of the village community to survive in a changing environment: survive or change." IOP Conference Series: Earth and Environmental Science 917, no. 1 (November 1, 2021): 012026. http://dx.doi.org/10.1088/1755-1315/917/1/012026.
Повний текст джерелаPellerin, Stéphanie, and Claude Lavoie. "Peatland fragments of southern Quebec: recent evolution of their vegetation structure." Canadian Journal of Botany 78, no. 2 (April 7, 2000): 255–65. http://dx.doi.org/10.1139/b99-186.
Повний текст джерелаDeane, Patrick Jeffrey, Sophie Louise Wilkinson, Paul Adrian Moore, and James Michael Waddington. "Seismic Lines in Treed Boreal Peatlands as Analogs for Wildfire Fuel Modification Treatments." Fire 3, no. 2 (June 6, 2020): 21. http://dx.doi.org/10.3390/fire3020021.
Повний текст джерелаPertiwi, N., T. W. Tsusaka, N. Sasaki, and E. Gunawan. "Peatland conservation strategies and carbon pricing possibilities for climate change mitigation in Indonesia: a review." IOP Conference Series: Earth and Environmental Science 892, no. 1 (November 1, 2021): 012061. http://dx.doi.org/10.1088/1755-1315/892/1/012061.
Повний текст джерелаYi, Boli, Fan Lu, and Zhao-Jun Bu. "Nitrogen addition turns a temperate peatland from a near-zero source into a strong sink of nitrous oxide." Plant, Soil and Environment 68, No. 1 (January 12, 2022): 49–58. http://dx.doi.org/10.17221/411/2021-pse.
Повний текст джерелаCharman, D. J., D. W. Beilman, M. Blaauw, R. K. Booth, S. Brewer, F. M. Chambers, J. A. Christen, et al. "Climate-related changes in peatland carbon accumulation during the last millennium." Biogeosciences Discussions 9, no. 10 (October 17, 2012): 14327–64. http://dx.doi.org/10.5194/bgd-9-14327-2012.
Повний текст джерелаCharman, D. J., D. W. Beilman, M. Blaauw, R. K. Booth, S. Brewer, F. M. Chambers, J. A. Christen, et al. "Climate-related changes in peatland carbon accumulation during the last millennium." Biogeosciences 10, no. 2 (February 8, 2013): 929–44. http://dx.doi.org/10.5194/bg-10-929-2013.
Повний текст джерелаДисертації з теми "Natural peatlands"
Wind-Mulder, Heather Lynne. "Towards the restoration of harvested peatlands, comparisons of harvested and natural peatlands and examination of revegetation techniques." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ29126.pdf.
Повний текст джерелаMorrison, Ross David. "Land/atmosphere carbon dioxide exchange at semi-natural and regenerating peatlands in East Anglia, UK." Thesis, University of Leicester, 2013. http://hdl.handle.net/2381/27972.
Повний текст джерелаHjelm, Axel. "From forest to open bog : A status report from a forest-to-open bog-restoration, 8 years later." Thesis, Uppsala universitet, Institutionen för biologisk grundutbildning, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-451054.
Повний текст джерелаScheffer, Clemens von. "Holocene human impact, climate and environment in the northern Central Alps : a geochemical approach on mountain peatlands." Thesis, Toulouse, INPT, 2019. http://www.theses.fr/2019INPT0057.
Повний текст джерелаSince the last deglaciation the European Alps have experienced several phases of human colonisation from different directions and societies. However, the interaction of climate, human impact and environment is still not fully understood in this high mountain region. In particular, information on the time and scale of human impact in the northern Central Alps (NCA) during the Holocene is missing. This study fills this gap by using geochemical, pollen and radiocarbon analyses in comparison to regional archaeological and historical data. Mires in three areas of the NCA were selected as study sites: Kleinwalser Valley (Vorarlberg, Austria), Piller Mire (Tyrol, Austria) and upper Fimba Valley (Grisons, Switzerland), situated in an altitudinal range of 1100 to 2400 m a.s.l. These mires were cored and analysed. The use of geochemical proxies (lithogenic elements, trace metals) in peat is a well-established method to detect mineral input, erosion or metallurgical activities. Despite an advantage of a fast sample preparation and measurement, applying portable X-Ray-Fluorescence analysis (pXRF) on mountain mires is an uncommon approach, mainly due to limitations by low count rates, matrix effects or lacking calibrations for organic materials. By calibrating pXRF with measurements of quantitative Inductively Coupled Plasma – Mass Spectrometry (ICP-MS), these issues could be overcome, showing that, Ti, Pb, Sr, Zn, K, S, Fe, V, Zr, and - to some extent - Rb, Ca and Mn, can be successfully calibrated and used as palaeoenvironmental proxies in peat. These proxies allow the following conclusions: At high elevations, periglacial processes influence the deposition processes in the mires. Around 8200 and in the late 7th millennium BP, wetter and colder climate conditions prevail in the region. The earliest land use is recorded in the Kleinwalser Valley around 5500 cal BP, with fire clearings, pastoralism and hints at previously undetected regional metallurgy. Just before the Bronze Age (c. 4300 cal BP), centuries before mining districts in the Eastern Alps boomed, metallurgy around the Piller Mire is detected. The possibly strongest human land use in prehistoric times affects all sites from the Mid to Late Bronze Age (3500-3000 cal BP), as shown by elevated erosion and significant landscape alteration – from forests to agro-pastoral systems. Potential metal enrichments are, however, masked by high mineral inputs. This period is followed by a phase of lower land use, reaching well into the late Roman period (2800 cal BP to 250 cal CE). However, a strong Pb enrichment factor (Pb EF) in the Kleinwalser Valley is recorded around 2700 cal BP. Human impact increases in north-western Tyrol around 2400 cal BP. Periods of mining and metallurgy are indicated by increased Pb EF in all mires during the Roman Empire but also right after its collapse. Intensive human activities rise again with the fading Roman power after 250 cal CE in the Kleinwalser Valley but are interrupted by a climate deterioration after 500 cal CE (Late Antique Little Ice Age). At the sites in higher elevations, land use intensification does not take place before the High Middle Ages and is accompanied by rising Pb EF, indicating mining activities after 1000 cal CE. While Pb EF keeps rising due to mining, industrialisation and leaded fuel until 1980 cal CE, fluctuating human impact (deforestation, pasture management, drainage) can be linked to a varying impact of climatic, cultural and demographic factors. Over the last century, growing tourism and infrastructure construction increase erosion, but land use change leads to a recovery of the studied mires in Kleinwalser Valley and Tyrol. The results of this study add a new dimension to archaeological and historical data, by showing the wider extent of human land use and its links to climate. Moreover, previously unknown periods of prehistoric mining or metallurgy in the NCA are revealed, encouraging further interdisciplinary research
Tolkkinen, M. (Mari). "Multi-stressor effects in boreal streams:disentangling the roles of natural and land use disturbance to stream communities." Doctoral thesis, Oulun yliopisto, 2016. http://urn.fi/urn:isbn:9789526211220.
Повний текст джерелаTiivistelmä Ihmistoiminnan vaikuttaessa yhä enemmän luonnon elinympäristöihin eliöyhteisöihin kohdistuu usein samanaikaisesti monenlaisia paineita. Ekosysteemien tehokas hoitaminen ja suojelu edellyttävät tarkkaa tietoa siitä, miten luonnollinen stressi ja ihmistoiminta yhdessä ja erikseen vaikuttavat ekosysteemeihin. Väitöskirjassani tutkin, kuinka geologiasta johtuva luonnollinen happamuus ja metsäojitus vaikuttavat boreaalisten purojen eliöyhteisöihin ja lehtikarikkeen hajotukseen. Tarkastelin myös eliöryhmien yhdenmukaisuutta ihmistoimintagradientilla ja luonnollisella stressigradientilla. Malliorganismeinani olivat piilevät, vesisammalet, pohjaeläimet ja hajottajasienet. Väitöskirjassani osoitan, että geologiasta johtuva puroveden happamuus toimii merkittävänä ympäristösuodattimena purojen eliöyhteisöille vähentäen lajirunsautta ja muokaten lajistoa. Myös eliöryhmien lajistovaihtelu oli yhdenmukaisinta luonnollisella happamuusgradientilla. Toisaalta luonnollinen happamuus ei vaikuttanut merkittävästi lehtikarikkeen hajotukseen tai purojen väliseen sieniyhteisöjen monimuotoisuuteen. Metsäojituksen fysikaalis-kemiallinen vaikutus erosi purotyypeittäin: pH-neutraaleissa puroissa ojitus pääosin lisäsi pohjan hiekoittumista, kun taas happamissa puroissa veden metallipitoisuudet kasvoivat entisestään. Yleisesti ottaen sekä luonnollisen happamuuden että metsäojituksen vaikutukset näkyivät parhaiten muutoksina eliöyhteisöjen lajikoostumuksessa. Lisäksi ojitetuissa happamissa puroissa hajottajasieniyhteisöjen lajistot olivat keskenään samankaltaisempia ja lehtikarikkeen hajotus hitaampaa kuin muissa purotyypeissä. Metsäojituksen aikaansaama muutos luonnollisesti happamien purojen vesikemiassa näyttää siis olevan jopa merkittävämpi ympäristösuodatin kuin pohjan hiekoittuminen. Luonnollisesti stressattujen elinympäristöjen herkkyys maankäytön muutoksille tulisikin huomioida ympäristön hoidon suunnittelussa nykyistä paremmin
Wendel, Dirk. "Autogene Regenerationserscheinungen in erzgebirgischen Moorwäldern und deren Bedeutung für Schutz und Entwicklung der Moore." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2011. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-67943.
Повний текст джерела- Objectives - The objective of this work is to analyse and to assess to which extent autogenous peatland regeneration occurs after anthropogenic disturbances, what preconditions it requires and what processes are important. Relevance of the findings for forestry and nature conservation is to be examined. - Experimental set-up and methods - The experimental set-up comprises various spatial scale levels and time periods. Five study sites are located in the study area Saxon Erzgebirge Mountains. Historical aspects are analysed based on investigations, the actual condition of the peatland is determined by ground surveys focusing on the vegetation and the site. Long-term observations serve to prove succession processes and the environmental factors influencing them. Regeneration processes are localized by means of regeneration characteristics, which were elaborated just for this purpose, localized, and interpreted in the context of the actual peatland condition and of the requirements of nature conservation and forestry. - Results and conclusions - - The material under survey allows distinguishing between 28 vegetation types which are characterised by means of species groups and indicator values and which are used as mapping units for evaluating the peatlands. The peatland area in the study area comprises an estimated 8500 ha. Each investigated peatland has a specific combination of abiotic and biotic characteristics and therefore needs to be evaluated individually. Drainage and peat cuttings lead to strong degeneration, dominance of forest, rarity of plants species typical of peatland, open-land associations, wetness-coined hydromorphological structures as well as ecosystem-relevant key species. In addition, the tree and moss layer had been damaged by SO2-pollution up to the 1990ies and a succeeding regeneration. - Recurring wetting due to filling-up of ditches and peat cuttings by sedimentation are verifiable by time sequences and actual regeneration characteristics. Autogenous peatland regeneration occurs even in heavily degenerated peatlands. Regeneration areas are frequent, accounting, however, only for a small share at the peatland area (study area: 1 %, study sites: 12 %). Often they are of mesotrophic nature. An increased disposition to regeneration is found, among others, in case of convergent water flows and slight inclinations. Local processes like the formation of obstacles for the flowing may cause ditches to become ineffective. Establishing of peat-forming vegetation is a crucial phenomenon. Various stages of a discontinuous regeneration progress can be differentiated and allocated to the processes that are known so far. Frequency and the area ratio of initial and progressed regeneration suggest that regeneration processes take place on a larger area, but that they are not recognised. Regeneration leads to site drifting and the distribution of peatland species. The regeneration potential is given by abiotic conditions. Irreversible changes of the hydro-morphological structure due to drainage or peat cutting are limiting factors for the regeneration. Anthropogenic input of matter and lack of key species bring about other restrictions. - If a profitable timber production is aimed at, autogenously regenerated peatlands are sites difficult to manage or that cannot be managed at all, involving a high production risk due to site drifting and partly inadequacy for woody plants. For nature conservation, regeneration processes are a chance and an important asset worth of protection, as they lead to high-grade peatland habitats. In the case of advanced regeneration cost-intensive operations are not necessary. A protection of static nature is inadequate for the process character. Initial stages and zones not yet under regeneration, implying, however, a high potential, can be promoted efficiently. Heavy degeneration of the peatlands in the study area, given a low proportion of actual regeneration zones, justifies a strong call for action, including a shielding protection as well as efficient control mechanisms. - An appropriate data basis for localisation of areas, having a high regeneration potential, is largely missing. Remedying this deficit is possible
Bootsma, Antoinette Alexandra. "Natural mechanisms of erosion prevention and stabilisation in a Marakele Peatland ; implications for conservation management." Diss., 2016. http://hdl.handle.net/10500/23115.
Повний текст джерелаEnvironmental Sciences
M. Sc. (Environmental Management)
Hapsari, Kartika Anggi. "Indonesian coastal wetlands." Doctoral thesis, 2018. http://hdl.handle.net/11858/00-1735-0000-002E-E5C9-A.
Повний текст джерелаWendel, Dirk. "Autogene Regenerationserscheinungen in erzgebirgischen Moorwäldern und deren Bedeutung für Schutz und Entwicklung der Moore." Doctoral thesis, 2010. https://tud.qucosa.de/id/qucosa%3A25564.
Повний текст джерела- Objectives - The objective of this work is to analyse and to assess to which extent autogenous peatland regeneration occurs after anthropogenic disturbances, what preconditions it requires and what processes are important. Relevance of the findings for forestry and nature conservation is to be examined. - Experimental set-up and methods - The experimental set-up comprises various spatial scale levels and time periods. Five study sites are located in the study area Saxon Erzgebirge Mountains. Historical aspects are analysed based on investigations, the actual condition of the peatland is determined by ground surveys focusing on the vegetation and the site. Long-term observations serve to prove succession processes and the environmental factors influencing them. Regeneration processes are localized by means of regeneration characteristics, which were elaborated just for this purpose, localized, and interpreted in the context of the actual peatland condition and of the requirements of nature conservation and forestry. - Results and conclusions - - The material under survey allows distinguishing between 28 vegetation types which are characterised by means of species groups and indicator values and which are used as mapping units for evaluating the peatlands. The peatland area in the study area comprises an estimated 8500 ha. Each investigated peatland has a specific combination of abiotic and biotic characteristics and therefore needs to be evaluated individually. Drainage and peat cuttings lead to strong degeneration, dominance of forest, rarity of plants species typical of peatland, open-land associations, wetness-coined hydromorphological structures as well as ecosystem-relevant key species. In addition, the tree and moss layer had been damaged by SO2-pollution up to the 1990ies and a succeeding regeneration. - Recurring wetting due to filling-up of ditches and peat cuttings by sedimentation are verifiable by time sequences and actual regeneration characteristics. Autogenous peatland regeneration occurs even in heavily degenerated peatlands. Regeneration areas are frequent, accounting, however, only for a small share at the peatland area (study area: 1 %, study sites: 12 %). Often they are of mesotrophic nature. An increased disposition to regeneration is found, among others, in case of convergent water flows and slight inclinations. Local processes like the formation of obstacles for the flowing may cause ditches to become ineffective. Establishing of peat-forming vegetation is a crucial phenomenon. Various stages of a discontinuous regeneration progress can be differentiated and allocated to the processes that are known so far. Frequency and the area ratio of initial and progressed regeneration suggest that regeneration processes take place on a larger area, but that they are not recognised. Regeneration leads to site drifting and the distribution of peatland species. The regeneration potential is given by abiotic conditions. Irreversible changes of the hydro-morphological structure due to drainage or peat cutting are limiting factors for the regeneration. Anthropogenic input of matter and lack of key species bring about other restrictions. - If a profitable timber production is aimed at, autogenously regenerated peatlands are sites difficult to manage or that cannot be managed at all, involving a high production risk due to site drifting and partly inadequacy for woody plants. For nature conservation, regeneration processes are a chance and an important asset worth of protection, as they lead to high-grade peatland habitats. In the case of advanced regeneration cost-intensive operations are not necessary. A protection of static nature is inadequate for the process character. Initial stages and zones not yet under regeneration, implying, however, a high potential, can be promoted efficiently. Heavy degeneration of the peatlands in the study area, given a low proportion of actual regeneration zones, justifies a strong call for action, including a shielding protection as well as efficient control mechanisms. - An appropriate data basis for localisation of areas, having a high regeneration potential, is largely missing. Remedying this deficit is possible.
Pereira, Dinis Manuel Teixeira. "Avaliação do valor dos ecossistemas de turfeiras dos Açores, com recurso a modelação em sistemas de informação geográfica." Doctoral thesis, 2015. http://hdl.handle.net/10400.3/3924.
Повний текст джерелаO panorama mundial tem-se debatido com os problemas inerentes às alterações climáticas, bem como os decorrentes das alterações aos usos do solo, propondo soluções que passam, em grande parte, pelo recurso a sistemas florestais. Recentemente tem-se assistido ao dealbar de vozes que reclamam as zonas húmidas como uma solução mais promissora, assistindo-se a um avanço do conhecimento caracterizador dos diferentes impactos ambientais resultantes das acções antrópicas. As turfeiras são zonas húmidas particulares, nas quais se têm centrado grandes esforços de obtenção de conhecimento, revelando-se como ecossistemas prioritários a inserir nas preocupações de entidades internacionais, tais como a FAO, ou a Comissão Europeia (e. g.: European Comission 2013; Borges et al. 2010; Joosten et al. 2012; McInnes 2007; Wood & Halsema 2008). No caso específico de Portugal as turfeiras não assumiram ainda um papel de destaque, encontrando-se uma grande área de turfeiras, perturbadas e/ou em bom estado de conservação no arquipélago dos Açores e só recentemente surgiu no debate científico como área relevante (Mendes 2009, 2010, 2013) e no plano político como área de investimento prioritário para recuperação ecológica (Decreto Legislativo Regional n.º 15/2010/A). Estas, na Região açoriana, ocupam cerca de 40% da superfície das áreas protegidas, sendo esta emergente relevância reconhecida pelas funções que as mesmas desempenham como elementos estruturadores da paisagem, na capacidade das ilhas para serem ecologicamente equilibradas, como sistema tamponizante/retentor de eventos climáticos, atuando como regularizadores do mesmo nas partes mais altas das ilhas e, consequentemente, das linhas de água a jusante. São um sistema retentor de metano e sequestrador de carbono; promotores de biodiversidade zonal e azonal (Dias et al. 2004); são ainda promotores da estabilidade física das zonas mais altas das ilhas, limitando a possibilidade de derrocadas e deslizamentos. São ecossistemas produtivos, que, nos Açores sofrem pressões antrópicas, as quais limitam as funções ecológicas desempenhadas pelos mesmos. Existem trabalhos caracterizadores das turfeiras nos Açores, porém o desconhecimento ainda é considerável, pelo que se torna premente desenvolver um estudo que quantifique os impactos que as mesmas têm na regulação do ciclo hídrico e no processo de crescimento e acumulativo de turfa (com as consequências inerentes), bem como da distribuição potencial no território açoriano. Pretende-se assim colmatar esta falta de conhecimento, estimando estes impactos, recorrendo a técnicas de modelação tridimensional em Sistemas de Informação Geográfica (SIG), com recurso a dados cartográficos, modelação da distribuição potencial de diversos tipos de turfeiras, secções transversais das mesmas, medições de matéria orgânica, uso de radares de penetração no solo e dados da quantidade de água retida pelas turfeiras, bem como uma avaliação do seu potencial futuro sob diferentes modelos de gestão.
Книги з теми "Natural peatlands"
International, Conference and Workshop on Tropical Peat Swamps (1999 George Town Pinang). Tropical peat swamps: Safe-guarding a global natural resource. [Minden], Pulau Pinang: Penerbit Universiti Sains Malaysia, 2004.
Знайти повний текст джерелаUrban, Noel R. Sulfur metabolism and organic acids: Implications for the natural and anthropogenic acidification of peatlands and colored lakes. St. Paul, MN: Water Resources Research Center, University of Minnesota, 1989.
Знайти повний текст джерелаDavis, Ronald B. A numeric method and supporting database for evaluation of Maine peatlands as candidate natural areas. Orono, ME: Dept. of Biological Sciences, University of Maine, 1999.
Знайти повний текст джерелаSymposium '87: Wetlands/Peatlands (1987 Edmonton, Alta.). Symposium '87, Wetlands-Peatlands: Proceedings, Edmonton Convention Centre, Edmonton, Alberta, Canada, August 23-27, 1987. S.l: S.n., 1987.
Знайти повний текст джерелаGrace, O'Donovan, and University College, Dublin. Environmental Institute., eds. The bogs of Ireland: An introduction to the natural, cultural and industrial heritage of Irish peatlands. Dublin: University College, Dublin, Environmental Institute, 1996.
Знайти повний текст джерелаForysiak, Jacek. Zapis zmian środowiska przyrodniczego późnego vistulianu i holocenu w osadach torfowisk regionu łódzkiego: Record of changes in the natural environment of the late Weichselian and Holocene preserved in the sediments of peatlands of the Łódź Region. Łódź: Łódzkie Towarzystwo Naukowe, 2012.
Знайти повний текст джерелаA, Spigarelli S., and Bemidji State University. Center for Environmental Studies., eds. International Symposium on Peat/Peatland Characteristics and Uses: Bemidji State University, May 16-19, 1989. Bemidji, Minn: Center for Environmental Studies, Bemidji State University, 1990.
Знайти повний текст джерелаRobertson, Kevin. Management of peatland shrub- and forest-dominated communities for threatened and endangered species. [Champaign, IL]: US Army Corps of Engineers, Construction Engineering Research Laboratories, 1998.
Знайти повний текст джерелаPingmư̄ang, Ranidā. Khrōngkān wičhai kānsưksā læ phatthanā lǣng rīanrū thāng thammachāt læ khwāmlāklāi thāng chīwaphāp pā phru nam čhư̄t pā chumchon Bān Mǣ Khāo Lūang, Tambon San Klāng, ʻAmphœ̄ Phān, Čhangwat Chīang Rai =: The study and development of nature and biodiversity learning resources center of peat swamp forest in Mae Khaow Luang Community Forest, San Klang Sub-District, Phan District, Chiangrai Province. [Chiang Rai]: Mahāwitthayālai Rātchaphat Chīang Rai, 2007.
Знайти повний текст джерелаQuane, Michael Timothy. The isolation and characterisation of humic substances from peatland soils subjected to natural rainfall and acidified waters. Birmingham: University of Birmingham, 1997.
Знайти повний текст джерелаЧастини книг з теми "Natural peatlands"
Gorham, E., J. A. Janssens, G. A. Wheeler, and P. H. Glaser. "The Natural and Anthropogenic Acidification of Peatlands." In Effects of Atmospheric Pollutants on Forests, Wetlands and Agricultural Ecosystems, 493–512. Berlin, Heidelberg: Springer Berlin Heidelberg, 1987. http://dx.doi.org/10.1007/978-3-642-70874-9_36.
Повний текст джерелаHolden, J., R. P. Smart, P. J. Chapman, A. J. Baird, and M. F. Billett. "The Role of Natural Soil Pipes in Water and Carbon Transfer in and from Peatlands." In Carbon Cycling in Northern Peatlands, 251–64. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000804.
Повний текст джерелаZubkova, Ksenya A., Lyudmila N. Shikhova, and Eugene M. Lisitsyn. "Paleopalinology Studies of Conditions of Peatlands Formation on European Northeast of Russia." In Biological Assessment of Natural and Anthropogenic Ecosystems, 27–47. New York: Apple Academic Press, 2021. http://dx.doi.org/10.1201/9781003145424-3.
Повний текст джерелаCraft, Christopher, Chad Washburn, and Amanda Parker. "Latitudinal Trends in Organic Carbon Accumulation in Temperate Freshwater Peatlands." In Wastewater Treatment, Plant Dynamics and Management in Constructed and Natural Wetlands, 23–31. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-8235-1_3.
Повний текст джерелаPärn, Jaan, Anto Aasa, Sergey Egorov, Ilya Filippov, Geofrey Gabiri, Iuliana Gheorghe, Järvi Järveoja, et al. "Global Boundary Lines of N2O and CH4 Emission in Peatlands." In The Role of Natural and Constructed Wetlands in Nutrient Cycling and Retention on the Landscape, 87–102. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-08177-9_7.
Повний текст джерелаCooper, William T., Malak M. Tfaily, Jane E. Corbet, and Jeffrey P. Chanton. "Correlating Bulk Optical Spectroscopy and Ultrahigh-Resolution Mass Spectrometry to Determine the Molecular Composition of Dissolved Organic Matter in Northern Peatlands." In Functions of Natural Organic Matter in Changing Environment, 19–23. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5634-2_4.
Повний текст джерелаPereira, Dinis, Cândida Mendes, and Eduardo Dias. "The Importance of Land Cover Planning on Climatic Events: Evaluation of Peatlands’ Buffer Impact on Terceira and Flores Islands (Azores, Portugal)." In Advances in Natural Hazards and Hydrological Risks: Meeting the Challenge, 91–95. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-34397-2_18.
Повний текст джерелаVávrová, Petra, Bo Stenberg, Marjut Karsisto, Veikko Kitunen, Tarja Tapanila, and Raija Laiho. "Near Infrared Reflectance Spectroscopy for Characterization of Plant Litter Quality: Towards a Simpler Way of Predicting Carbon Turnover in Peatlands?" In Wastewater Treatment, Plant Dynamics and Management in Constructed and Natural Wetlands, 65–87. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-8235-1_7.
Повний текст джерелаOsaki, Mitsuru, Nobuyuki Tsuji, Tsuyoshi Kato, Manabu D. Yamanaka, Albertus Sulaiman, Sisva Silsigia, and Rahmawati I. Wetadewi. "Natural Capital-Based Societies in the Tropics." In Tropical Peatland Eco-management, 197–245. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4654-3_6.
Повний текст джерелаTampubolon, Agustinus P., Maman Turjaman, and Mitsuru Osaki. "Sago Palm Practice as Natural AeroHydro Culture." In Tropical Peatland Eco-management, 363–77. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4654-3_12.
Повний текст джерелаТези доповідей конференцій з теми "Natural peatlands"
Georgiev, Georgi. "BIOLOGICAL DIVERSITY OF WETLANDS AND RAMSAR PLACES IN THE CROSS-BORDER REGION OF BULGARIA, NORTHERN MACEDONIA, ALBANIA AND GREECE AND DEVELOPMENT." In TOURISM AND CONNECTIVITY 2020. University publishing house "Science and Economics", University of Economics - Varna, 2020. http://dx.doi.org/10.36997/tc2020.97.
Повний текст джерелаHutbarat, S. "Challenges on Peatland Restoration: From Oil Palm Plantation to Sustainable Peatland Ecosystem." In International Conference on Natural Resources and Sustainable Development. SCITEPRESS - Science and Technology Publications, 2018. http://dx.doi.org/10.5220/0009905400002480.
Повний текст джерелаUlanov, Nikolay. "INFLUENCE OF ATMOSPHERIC PRECIPITATION ON THE EFFICIENCY OF SLUICING IN THE CONDITIONS OF DEPLETED PEATLANDS." In Multifunctional adaptive fodder production. ru: Federal Williams Research Center of Forage Production and Agroecology, 2020. http://dx.doi.org/10.33814/mak-2020-24-72-44-48.
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