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Artykuły w czasopismach na temat "Arid zone plants"
Jain, Satish C., B. Pancholi, R. Singh i R. Jain. "Pharmacognostical studies of important arid zone plants". Revista Brasileira de Farmacognosia 20, nr 5 (listopad 2010): 659–65. http://dx.doi.org/10.1590/s0102-695x2010005000023.
Pełny tekst źródłaFrancois, L. E. "Salinity effects on four arid zone plants". Journal of Arid Environments 11, nr 1 (lipiec 1986): 103–9. http://dx.doi.org/10.1016/s0140-1963(18)31315-6.
Pełny tekst źródłaLewis, Megan. "Spectral characterization of Australian arid zone plants". Canadian Journal of Remote Sensing 28, nr 2 (styczeń 2002): 219–30. http://dx.doi.org/10.5589/m02-023.
Pełny tekst źródłaSimpson, B. S., V. Bulone, S. J. Semple, G. W. Booker, R. A. McKinnon i P. Weinstein. "Arid awakening: new opportunities for Australian plant natural product research". Rangeland Journal 38, nr 5 (2016): 467. http://dx.doi.org/10.1071/rj16004.
Pełny tekst źródłaJain, SC, B. Pancholi, R. Singh i R. Jain. "Antibacterial and antifungal potential of some arid zone plants". Indian Journal of Pharmaceutical Sciences 72, nr 4 (2010): 510. http://dx.doi.org/10.4103/0250-474x.73939.
Pełny tekst źródłaBona, Elisa, Nadia Massa, Omrane Toumatia, Giorgia Novello, Patrizia Cesaro, Valeria Todeschini, Lara Boatti i in. "Climatic Zone and Soil Properties Determine the Biodiversity of the Soil Bacterial Communities Associated to Native Plants from Desert Areas of North-Central Algeria". Microorganisms 9, nr 7 (23.06.2021): 1359. http://dx.doi.org/10.3390/microorganisms9071359.
Pełny tekst źródłaRathore, Mala. "Leaf Protein Concentrate as Food Supplement from Arid Zone Plants". Journal of Dietary Supplements 7, nr 2 (maj 2010): 97–103. http://dx.doi.org/10.3109/19390211003766777.
Pełny tekst źródłaBIDINGER, F. R., O. P. YADAV i E. WELTZIEN RATTUNDE. "GENETIC IMPROVEMENT OF PEARL MILLET FOR THE ARID ZONE OF NORTHWESTERN INDIA: LESSONS FROM TWO DECADES OF COLLABORATIVE ICRISAT-ICAR RESEARCH". Experimental Agriculture 45, nr 1 (styczeń 2009): 107–15. http://dx.doi.org/10.1017/s0014479708007059.
Pełny tekst źródłaRakhimov, Tulkin, Ikram Yusupov i Zafar Boirov. "Influence of Industrial Emissions on Morphological Signs of Leaves of Greening Plants". Natural Systems and Resources, nr 2 (październik 2020): 26–32. http://dx.doi.org/10.15688/nsr.jvolsu.2020.2.3.
Pełny tekst źródłaSchweingruber, Fritz Hans. "Anatomical Characteristics and Ecological Trends in the Xylem and Phloem of Brassicaceae and Resedacae". IAWA Journal 27, nr 4 (2006): 419–42. http://dx.doi.org/10.1163/22941932-90000164.
Pełny tekst źródłaRozprawy doktorskie na temat "Arid zone plants"
McGee, P. A. "Role of mycorrhizas in the regeneration of arid zone plants /". Title page, contents and summary only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phm1448.pdf.
Pełny tekst źródłaEaston, Lyndlee Carol, i lyndlee easton@flinders edu au. "LIFE HISTORY STRATEGIES OF AUSTRALIAN SPECIES OF THE HALOPHYTE AND ARID ZONE GENUS FRANKENIA L. (FRANKENIACEAE)". Flinders University. Biological Sciences, 2008. http://catalogue.flinders.edu.au./local/adt/public/adt-SFU20081124.105244.
Pełny tekst źródłaMagagi, Ramata D. "Étude de synergie optique et micro-onde active : estimation des paramètres de surface en zone semi-aride : cas du Sahel". Toulouse, INPT, 1995. http://www.theses.fr/1995INPT101H.
Pełny tekst źródłaChaieb, Mohamed. "Influence des réserves hydriques du sol sur le comportement comparé de quelques espèces végétales de la zone aride tunisienne". Montpellier 2, 1989. http://www.theses.fr/1989MON20126.
Pełny tekst źródłaHeshmatti, Gholam Ali. "Plant and soil indicators for detecting zones around water points in arid perennial chenopod shrublands of South Australia /". Title page, contents and summary only, 1997. http://web4.library.adelaide.edu.au/theses/09PH/09phh584.pdf.
Pełny tekst źródłaErrata page is behind title page (p. i). Copies of author's previously published articles inserted. Includes bibliographical references (leaves 121-156).
Monroy, Ata Arcadio. "Installation de plantes pérennes de la zone aride soumises à des contraintes hydriques contrôlées et à des coupes". Montpellier 2, 1989. http://www.theses.fr/1989MON20025.
Pełny tekst źródłaPierre, Caroline. "Variabilité interannuelle des émissions d'aérosols minéraux en zone semi-aride sahélienne". Phd thesis, Université Pierre et Marie Curie - Paris VI, 2010. http://tel.archives-ouvertes.fr/tel-00921688.
Pełny tekst źródłaKarimi, Rachid. "Hydrogéologie et aménagement des eaux en zône aride exemple des plaines de Tagmoute et Tata (sud marocain) /". Grenoble 2 : ANRT, 1988. http://catalogue.bnf.fr/ark:/12148/cb37614694c.
Pełny tekst źródłaCosta, Carlos Alexandre Gomes. "Umidade do solo e disponibilidade hídrica na zona das raízes em condições naturais de caatinga preservada". reponame:Repositório Institucional da UFC, 2012. http://www.repositorio.ufc.br/handle/riufc/18822.
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Regarding ecohydrology, the catchment water is distributed over several important compartments. Many studies in semiarid re gions indicate the surface reservoirs as the main water compartments. However, the watershed has greater scope than the water reservoirs contained therein, and water resources in compartments distributed in the watershed (like in soil) should be analyzed not only with regard to ecological uses, but also as spaces of water availability. Therefore, the object ive of this work was to analyze, based on measurements and modeling, the water dynamics in th e soils of a semi-arid basin in preserved Caatinga, and its impact on water availability. Wit h this in mind, it was measured, among others, the soil moisture, every hour, from 2003 to 2010 (2923 days) in the Aiuaba Experimental Basin (AEB, 12 km ²), fully preserved and with average annual rainfall of 560 mm. Monitoring was carried out through three TDR se nsors, one installed in each of the three soil and vegetation associations (SVA) identified in the basin. The research method considered six main steps: i) assessment of the eff ective root depth of preserved Caatinga ii) calibration of humidity TDR sensors iii) space-time representation of soil moisture in each SVA unit iv) analysis of soil water availability in the root zone, v) parameterization of the WASA-SED hydrological model, and vi) parameterizati on of the DiCaSM hydrological model. The results of this research indicate the importance of addressing the temporal analysis of soil moisture and soil water availability in the root zone to maintain the Caatinga biome. More specifically, it was observed that the effecti ve depth of the root system on AEB ranged between 70 and 80 cm in areas with deep soils, but in areas with shallow soils, it was observed that the effective depth of the roots had adapted to the constraints, having been reduced to less than 40 cm. Furthermore, the season al analysis showed that in the dry season, the roots have lengths up to 11 cm smaller, openin g, therefore, secondary pores that facilitate the penetration of what little rain water falls in the dry months (June-December), as well as in the first rains of the wet season. In the two SVAs whose soils are deep and the vegetation is dense, the soil water is 'not available' (ie below the permanent wilting point - WP) during nearly nine months a year (72% of the time), and on ly during three months of the year (25% of the time) the soil water is available. In the re maining 3% of the year (about 10 days) there is gravitational water in these SVAs. In the SVAs whose soil is shallow and whose vegetation is sparse, the dynamics of soil water are different : the time when there is gravitational water, available and unavailable, is practically the same (four months a year). This is due to, among other things, the low soil moisture at the permanen t wilting point of the Udorthent, and to its limited thickness, generating saturation much more frequently than in others that - unlike this one - have deep drainage. The depletion of soil wat er under conditions of moisture below the wilting point was another important result of this research. In the two associations with deep soils and thick vegetation, it was observed – throu ghout the observation period – continuous fall of moisture level until it approached asymptot ically the residual moisture. More detailed analysis showed that the reduction of soil moisture between the WP and the residual moisture level always followed the exponential decay. It was observed, in the association of shallow soil and sparse vegetation, that the moisture did not fall to below the WP, even subjected to the same rigorous climate of the other associations . Considering: (i) that in such a dry soil, the drainage is unlikely, and (ii) that the associated processes of percolation and evaporation should not be responsible for the removal of soil w ater either (since the phenomenon is not observed in SVAs whose soil is shallow and therefor e warmer) , it is raised the hypothesis that the soil drying under these conditions must be caused by water extraction by vegetation. This would strengthen the argument that the Caating a has adapted to survive under water stress. The hydrological models WASA-SED and DiCaSM failed to adequately represent the temporal dynamics of soil water in the AEB. However , the models did satisfactorily reproduce the retention curves of soil moisture, al lowing the representation of the water availability in the root zone for planning purposes . Finally, we managed to evaluate - quantitatively, spatially and temporally – the soil water availability. This availability is of the same order of magnitude of the availability of an o ptimal surface reservoir. The availability in the soil, in quantitative terms, can be almost five times higher than that of the surface reservoir. However, the security associated with su rface water (90%) is much higher than the water permanence available in the AEB: just 28% in areas with deep soils and 65% in areas with shallow soils.
A água na bacia hidrográfica está distribuída em diversos compartimentos importantes no que se refere à ecohidrologia. Muitos estudos em regiões semiáridas apontam os reservatórios superficiais como principais compartimentos de água. Entretanto, a bacia hidrográfica tem maior abrangência que as bacias hidráulicas nela contida, e os recursos hídricos nos compartimentos distribuídos na bacia hidrográfica (como no solo) devem ser analisados não somente no que se refere aos usos ecológicos, mas também como espaço de disponibilidade hídrica. Portanto, o objetivo do trabalho foi analisar, com base em medidas e modelagem, a dinâmica da água nos solos de uma bacia semiárida de Caatinga preservada e seu impacto sobre a disponibilidade hídrica. Para isso foi medida, entre outros, a umidade do solo a cada hora, de 2003 a 2010 (2923 dias) na Bacia Experimental de Aiuaba (BEA, 12 km²), totalmente preservada e com precipitação média anual de 560 mm. O monitoramento foi realizado através de três sensores TDR, um instalado em cada uma das três associações entre solo e vegetação (SVA) identificadas na bacia. O método de investigação considerou seis etapas principais: i) determinação da profundidade efetiva das raízes da Caatinga preservada; ii) calibração dos sensores de umidade tipo TDR; iii) representação espaço-temporal da umidade do solo em cada unidade de SVA; iv) análise da disponibilidade hídrica do solo na zona das raízes; v) parametrização do modelo hidrológico WASA-SED; e vi) parametrização do modelo hidrológico DiCaSM. Os resultados obtidos nesta pesquisa indicam a importância da abordagem da análise temporal da umidade do solo e da disponibilidade hídrica do solo na zona das raízes para a manutenção do bioma Caatinga. Mais especificamente, foi observado que a profundidade efetiva do sistema radicular na BEA oscilou entre 70 e 80 cm nas regiões com solos profundos, porém, em regiões com solos rasos, observou-se que a profundidade efetiva das raízes adaptou-se às restrições, ficando reduzida a menos de 40 cm. Além disso, a análise sazonal demonstrou que, na estação de estio, as raízes têm comprimentos até 11 cm menores, abrindo, portanto, poros secundários que facilitarão a penetração da água nas eventuais chuvas dos meses secos (junho a dezembro), assim como nas primeiras chuvas da estação úmida. Nas duas SVAs cujos solos são profundos e cuja vegetação é densa, a água no solo encontra-se ‘não-disponível’ (isto é, abaixo do ponto de murcha permanente – WP) em quase nove meses ao ano (72% do tempo); e somente durante três meses ao ano (25%) a água no solo encontra-se disponível. Nos 3% restantes do ano (cerca de 10 dias) há água gravitacional nessas SVAs. Na SVA cujo solo é raso e cuja vegetação é esparsa, a dinâmica da água no solo é diferente: o tempo em que há água gravitacional, disponível e não disponível é praticamente o mesmo (quatro meses ao ano). Isso se deve, entre outros, à baixa umidade do solo no ponto de murcha permanente do neossolo litólico; e à sua restrita espessura, gerando saturação muito mais frequentemente que nos demais solos que – ao contrário deste – dispõem de drenagem profunda. A depleção da água no solo sob condições de umidade abaixo do ponto de murcha foi outro resultado importante desta pesquisa. Nas duas associações com solos profundos e vegetação densa, observou-se – ao longo de todo o período investigado – decaimento contínuo da umidade até que a mesma se aproximasse assintoticamente da umidade residual. Análise mais detalhada demonstrou que a redução da umidade do solo entre o WP e a umidade residual sempre obedecia ao decaimento exponencial. Na associação com solo raso e vegetação esparsa observou-se que a umidade não caía para valores inferiores ao WP, mesmo sujeita ao mesmo rigor climático das demais associações. Considerando-se: (i) que em solo tão seco, a drenagem é improvável; e (ii) que os processos associados de percolação e evaporação tampouco devam ser os responsáveis pela retirada de água do solo (posto que o fenômeno não se observa na SVA cujo solo é raso e, portanto, mais quente); levanta-se a hipótese que o secamento do solo nessas condições deva ser causado por extração de água pela vegetação. Isso reforçaria a tese de que a Caatinga dispõe de adaptação para sobreviver mesmo em condições de estresse hídrico. Os modelos hidrológicos WASA-SED e DiCaSM não conseguiram representar adequadamente a dinâmica temporal da água nos solos da BEA. No entanto, os modelos reproduziram satisfatoriamente as curvas de permanência da umidade dos solos, permitindo representar a disponibilidade hídrica na zona das raízes para fins de planejamento. Por fim, logrou-se avaliar – quantitativa, espacial e temporalmente – a disponibilidade hídrica do solo. Esta é da mesma ordem de grandeza da disponibilidade de um reservatório superficial ótimo. Em termos quantitativos, a disponibilidade no solo chega a ser quase cinco vezes superior à do reservatório superficial, entretanto, a garantia associada da água superficial (90%) é bem superior à permanência da água disponível na BEA: apenas 28% nas áreas com solos profundos e 65% nas áreas com solos rasos.
Osorio, Barahona Rodomiro. "Conséquences biologiques des variations du climat, de l'intensité de la coupe mécanique et du pâturage sur deux espèces arbustives de la région aride du Chili". Montpellier 2, 1989. http://www.theses.fr/1989MON20089.
Pełny tekst źródłaKsiążki na temat "Arid zone plants"
Booth, F. E. M. Non-timber uses of selected arid zone trees and shrubs in Africa. Rome: Food and Agriculture Organization of the United Nations, 1988.
Znajdź pełny tekst źródłaHouérou, H. N. Le. Les plantations sylvo-pastorales dans la zone aride de Tunisie. Paris: Unesco, 1987.
Znajdź pełny tekst źródłaLalymenko, N. K. Vozdelyvanie kormovykh kulʹtur v aridnoĭ zone na oroshenii khozi͡a︡ĭstvenno-bytovymi stochnymi vodami: Na primere g. Nebitdaga. Ashgabat: Ylym, 1992.
Znajdź pełny tekst źródłaGintzburger, Gustave. Rangelands of the arid and semi-arid zones in Uzbekistan. Montpellier, France: CIRAD, 2003.
Znajdź pełny tekst źródłaKhamdamov, I. Kh. Morfologo-biologicheskie osobennosti kormovykh rasteniĭ aridnoĭ zony Uzbekistana. Tashkent: "Mekhnat", 1987.
Znajdź pełny tekst źródłaRoy, M. M. Status of plant genetic resources at Central Arid Zone Research Institute. Jodhpur: Central Arid Zone Research Institute, 2012.
Znajdź pełny tekst źródłaP, Gupta J. Biomass production and rehabilitation of degraded lands in arid zone. Jodhpur: Division of Integrated Landuse Management and Farming System, Central Arid Zone Research Institute, 2002.
Znajdź pełny tekst źródłaArbonnier, Michel. Trees, shrubs and lianas of West African dry zones. Paris: CIRAD, 2004.
Znajdź pełny tekst źródłaSevertoka, Iosif Iosifovich. Dekorativnye formy khvoĭnykh rasteniĭ dli͡a︡ ozelenenii͡a︡: Umerennye i aridnye zony. Ashgabat: Ylym, 1993.
Znajdź pełny tekst źródłaPlisak, R. P. Vlii͡a︡nie vodokhranilishch aridnoĭ zony na rastitelʹnostʹ. Alma-Ata: "Gylym", 1992.
Znajdź pełny tekst źródłaCzęści książek na temat "Arid zone plants"
Maconochie, J. R. "Plants of the Australian arid zone — an undeveloped potential". W Plants for Arid Lands, 289–301. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-011-6830-4_21.
Pełny tekst źródłaLe Houérou, H. N. "Forage and fuel plants in the arid zone of North Africa, the Near and Middle East". W Plants for Arid Lands, 117–41. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-011-6830-4_10.
Pełny tekst źródłaHe, Honghua, David J. Eldridge i Hans Lambers. "Mineral Nutrition of Plants in Australia’s Arid Zone". W On the Ecology of Australia’s Arid Zone, 77–102. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-93943-8_4.
Pełny tekst źródłaBhansali, R. Raj, i Manjit Singh. "Somatic Embryogenesis in Fruit and Forest Trees of Arid Zone". W Somatic Embryogenesis in Woody Plants, 141–67. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-3030-3_5.
Pełny tekst źródłaPathak, Rakesh, Praveen Gehlot i S. K. Singh. "Seed Priming-Mediated Induced Disease Resistance in Arid Zone Plants". W Microbial-mediated Induced Systemic Resistance in Plants, 57–67. Singapore: Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-0388-2_5.
Pełny tekst źródłaPathak, Rakesh, S. K. Singh i Praveen Gehlot. "Diversity, Nitrogen fixation, and Biotechnology of Rhizobia from Arid Zone Plants". W Soil Biology, 61–81. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-64982-5_5.
Pełny tekst źródłaLe Houérou, H. N. "Salt-tolerant plants for the arid regions of the Mediterranean isoclimatic zone". W Towards the rational use of high salinity tolerant plants, 403–22. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1858-3_42.
Pełny tekst źródłaBhansali, Rikhab Raj. "Ganoderma Diseases of Woody Plants of Indian Arid Zone and their Biological Control". W Plant Defence: Biological Control, 209–39. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1933-0_9.
Pełny tekst źródłaNajjaa, Hanen, Abdelkarim Ben Arfa, Ákos Máthé i Mohamed Neffati. "Aromatic and Medicinal Plants of Tunisian Arid and Desert Zone Used in Traditional Medicine, for Drug Discovery and Biotechnological Applications". W Medicinal and Aromatic Plants of the World, 157–230. Dordrecht: Springer Netherlands, 2017. http://dx.doi.org/10.1007/978-94-024-1120-1_8.
Pełny tekst źródłaBouwer, H. "Water Conservation in Arid Zones". W Water Saving Techniques for Plant Growth, 21–31. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2767-7_4.
Pełny tekst źródłaStreszczenia konferencji na temat "Arid zone plants"
Davlatova, D. М., M. В. Niyzmuhamedova, D. Berdiev, M. М. Rahimov, F. Kosumbekova i N. Kamolov. "WATER CONTENT IN LEAVES OF HALOPHYTES AND XEROPHYTES GROWING IN ARID ZONE OF TAJIKISTAN". W The All-Russian Scientific Conference with International Participation and Schools of Young Scientists "Mechanisms of resistance of plants and microorganisms to unfavorable environmental". SIPPB SB RAS, 2018. http://dx.doi.org/10.31255/978-5-94797-319-8-256-258.
Pełny tekst źródłaUmarov, B. R. "Association of nitrogen-fixing microorganisms in the surface of nodules in wild perennial leguminous plants Onobrychis transcaucasica and Onobrychis chorassanica". W 2nd International Scientific Conference "Plants and Microbes: the Future of Biotechnology". PLAMIC2020 Organizing committee, 2020. http://dx.doi.org/10.28983/plamic2020.262.
Pełny tekst źródłaVelasco, I. "Growing vulnerability of the arid zones to drought and its impacts". W RAVAGE OF THE PLANET 2006. Southampton, UK: WIT Press, 2006. http://dx.doi.org/10.2495/rav060451.
Pełny tekst źródłaTan Yuen, P., A. Savchenko, N. Broit, G. Boyle, P. Parsons i C. Williams. "The First Plant Seco-Steroid and a New lignan from the Australian Arid Zone". W GA 2017 – Book of Abstracts. Georg Thieme Verlag KG, 2017. http://dx.doi.org/10.1055/s-0037-1608084.
Pełny tekst źródłaKostenkova, E. V., i A. S. Bushnev. "Improvement the technology of sunflower cultivation to increase the yield and oil collection". W CURRENT STATE, PROBLEMS AND PROSPECTS OF THE DEVELOPMENT OF AGRARIAN SCIENCE. Federal State Budget Scientific Institution “Research Institute of Agriculture of Crimea”, 2020. http://dx.doi.org/10.33952/2542-0720-20205-9-10-30.
Pełny tekst źródłaPalapin, I. V., M. V. Marchenko, S. A. Kiryachek i T. R. Toloraya. "Yields of maize hybrids depending on their early ripeness, usage of fertilizer and plant density in the central zone of the Krasnodar Territory". W CURRENT STATE, PROBLEMS AND PROSPECTS OF THE DEVELOPMENT OF AGRARIAN SCIENCE. Federal State Budget Scientific Institution “Research Institute of Agriculture of Crimea”, 2020. http://dx.doi.org/10.33952/2542-0720-2020-5-9-10-38.
Pełny tekst źródłaFaibish, R. S., T. Konishi i M. Gasparini. "Application of Nuclear Energy for Seawater Desalination: Design Concepts of Nuclear Desalination Plants". W 10th International Conference on Nuclear Engineering. ASMEDC, 2002. http://dx.doi.org/10.1115/icone10-22071.
Pełny tekst źródłaKazanbayeva, L. M. "ANTHROPOGENIC FACTORS AND THEIR INFLUENCE ON FORMATION AND DISTRIBUTION OF GROUNDWATER WITHIN THE PLATFORM DEN-UDATION PLAINS OF THE ARID ZONE OF KAZAKHSTAN (CENTRAL KAZAKHSTAN)". W 19th SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings. STEF92 Technology, 2019. http://dx.doi.org/10.5593/sgem2019/1.2/s02.009.
Pełny tekst źródłaDiaconu, Daniela, Kay Birdsell i George Zyvoloski. "Natural and Engineered Barriers in a Romanian Disposal Site for Low and Intermediate Level Waste". W ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4638.
Pełny tekst źródłaKruis, Nathanael J., i Matthew K. Heun. "Analysis of the Performance of Earthship Housing in Various Global Climates". W ASME 2007 Energy Sustainability Conference. ASMEDC, 2007. http://dx.doi.org/10.1115/es2007-36030.
Pełny tekst źródłaRaporty organizacyjne na temat "Arid zone plants"
Brandt, Leslie A., Cait Rottler, Wendy S. Gordon, Stacey L. Clark, Lisa O'Donnell, April Rose, Annamarie Rutledge i Emily King. Vulnerability of Austin’s urban forest and natural areas: A report from the Urban Forestry Climate Change Response Framework. U.S. Department of Agriculture, Northern Forests Climate Hub, październik 2020. http://dx.doi.org/10.32747/2020.7204069.ch.
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