Letteratura scientifica selezionata sul tema "Pedogenesis"
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Articoli di riviste sul tema "Pedogenesis"
Medeiros, Edgardo Ramos, Fabrício De Araújo Pedron e Anderson Augusto Volpato Sccoti. "EVIDÊNCIAS DE PEDOGÊNESE ALÓCTONE SOBRE ARENITOS BOTUCATU NO SUDOESTE GAÚCHO". Ciência e Natura 35, n. 1 (22 ottobre 2013): 43. http://dx.doi.org/10.5902/2179460x9600.
Testo completoUGOLINI, F. C., M. G. STONER e D. J. MARRETT. "ARCTIC PEDOGENESIS". Soil Science 144, n. 2 (agosto 1987): 90–100. http://dx.doi.org/10.1097/00010694-198708000-00002.
Testo completoSTONER, M. G., e F. C. UGOLINI. "ARCTIC PEDOGENESIS". Soil Science 145, n. 1 (gennaio 1988): 46–51. http://dx.doi.org/10.1097/00010694-198801000-00006.
Testo completoCunha, Luis, George G. Brown, David W. G. Stanton, Elodie Da Silva, Fabricio A. Hansel, Gabriella Jorge, Doyle McKey et al. "Soil Animals and Pedogenesis". Soil Science 181, n. 3/4 (2016): 110–25. http://dx.doi.org/10.1097/ss.0000000000000144.
Testo completoPhillips, Jonathan D. "Soil Complexity and Pedogenesis". Soil Science 182, n. 4 (aprile 2017): 117–27. http://dx.doi.org/10.1097/ss.0000000000000204.
Testo completoJOHNSON, D. L., e D. WATSON-STEGNER. "EVOLUTION MODEL OF PEDOGENESIS". Soil Science 143, n. 5 (maggio 1987): 349–66. http://dx.doi.org/10.1097/00010694-198705000-00005.
Testo completoChesworth, Ward. "Pedogenesis and soil taxonomy". Geochimica et Cosmochimica Acta 49, n. 1 (gennaio 1985): 309. http://dx.doi.org/10.1016/0016-7037(85)90214-5.
Testo completoLeguédois, Sophie, Geoffroy Séré, Apolline Auclerc, Jérôme Cortet, Hermine Huot, Stéphanie Ouvrard, Françoise Watteau, Christophe Schwartz e Jean Louis Morel. "Modelling pedogenesis of Technosols". Geoderma 262 (gennaio 2016): 199–212. http://dx.doi.org/10.1016/j.geoderma.2015.08.008.
Testo completoRodriguez, Victoria, Lisa-Marie Moskwa, Rómulo Oses, Peter Kühn, Nicolás Riveras-Muñoz, Oscar Seguel, Thomas Scholten e Dirk Wagner. "Impact of Climate and Slope Aspects on the Composition of Soil Bacterial Communities Involved in Pedogenetic Processes along the Chilean Coastal Cordillera". Microorganisms 10, n. 5 (20 aprile 2022): 847. http://dx.doi.org/10.3390/microorganisms10050847.
Testo completoJigău, Gheorghe, Liviu Apostol, Ana Barsan e Elena Tofan. "Elements of Climate Evolution in yhe Area Between Prut and Dniester Rivers. Landscape and Pedogenetic Implications". Present Environment and Sustainable Development 9, n. 1 (1 maggio 2015): 111–27. http://dx.doi.org/10.1515/pesd-2015-0007.
Testo completoTesi sul tema "Pedogenesis"
Millington, Jennifer A. "Pedogenesis on the Sefton Coastal Dunes, NW England". Thesis, University of Wolverhampton, 2010. http://hdl.handle.net/2436/116327.
Testo completoAlbuquerque, Antonia Gislaine Brito Marques. "Pedogenesis and evolution of Apicum soils in tropical semiarid". Universidade Federal do CearÃ, 2015. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=14874.
Testo completoCoordenaÃÃo de AperfeÃoamento de Pessoal de NÃvel Superior
The last eustatic events, coupled with the intense amount of sediments in the coastal plain gave rise to a set of geo-environmental units, such as the marine fluvial plains, home to the apicuns. This subunit is an area for the expansion of mangroves in periods of increase in the average sea level. Moreover, it is a environment related with the reproduction, protection and development of mangrove fauna as well as assists in the socio-economic and cultural aspects of local people. However, despite its important ecological function, there are few research involving the genesis of its soils. In this sense, this study aimed to contribute to the understanding of the dynamics of this coastal system under the pedological view. Apicuns located southeast and northwest of Cearà were selected and were held morphological, physical, chemical, geochemical, morphoscopic and micromorphological analyzes. The results showed that the fluctuation of the water table allowed the intense iron oxide precipitation and the incipient structuring of the soil. The contribuition of sandy material with nature thin to very thin and well selected grain from dunes has been verified. Furthermore, it was found that the northwest apicum have a lower degree of development as compared with the other soils, since the morphology and mineralogy support this fact. Also, there is differentiation in iron content between the two estuaries and disfavoring in the genesis of pyrites. In this case, the presence of pyrite in conditions not conducive to their formation indicates that apicum has its genesis correlated with areas of mangroves and should be considered, before the law, member of the mangrove ecosystem.
Os Ãltimos eventos eustÃticos, aliado ao intenso aporte de sedimentos na planÃcie costeira deram origem a um conjunto de unidades geoambientais, como por exemplo, as planÃcies fluviomarinhas, que abrigam os apicuns. Essa subunidade à uma Ãrea para a expansÃo do manguezal em perÃodos de aumento do nÃvel mÃdio do mar. AlÃm disso, à um ambiente relacionado com a reproduÃÃo, proteÃÃo e desenvolvimento da fauna do manguezal, bem como auxilia nos aspectos sÃcioeconÃmico- cultural da populaÃÃo local. No entanto, apesar da sua importante funÃÃo ecolÃgica, poucas sÃo as pesquisas que envolvam a gÃnese de seus solos. Neste sentido, esse estudo teve por finalidade contribuir para o entendimento da dinÃmica deste sistema costeiro sob a visÃo pedolÃgica. Para tanto, foram selecionados apicuns situados a sudeste e a noroeste do Estado do CearÃ, onde foram realizadas anÃlises morfolÃgicas, fÃsicas, quÃmicas, geoquÃmicas, morfoscÃpicas e micromorfolÃgicas. Os resultados encontrados mostraram que a flutuaÃÃo do lenÃol freÃtico permitiu a intensa formaÃÃo de mosquedos e a incipiente estruturaÃÃo do solo. Foi verificada a contribuiÃÃo de material arenoso de natureza fina a muito fina e de grÃos bem selecionados proveniente de dunas. AlÃm disso, verificou-se que os solos do apicum a noroeste possuem menor grau de desenvolvimento, em comparaÃÃo com os demais solos estudados, visto que a mineralogia e a micromorfologia suportam este fato. AlÃm disso, hà diferenciaÃÃo nos teores de ferro entre os dois estuÃrios e desfavorecimento na gÃnese de piritas. Neste caso, a presenÃa de pirita em condiÃÃes nÃo propÃcias à sua formaÃÃo indica que o apicum possui sua gÃnese correlacionada com os domÃnios de mangues, devendo ser considerado, diante das leis, integrante do ecossistema manguezal.
Heckman, Katherine Ann. "Pedogenesis & Carbon Dynamics Across a Lithosequence Under Ponderosa Pine". Diss., The University of Arizona, 2010. http://hdl.handle.net/10150/196016.
Testo completoGirÃo, Rodrigo de Oliveira. "Pedogenesis in a semiarid carstic environment at Limoeiro do Norte - CearÃ". Universidade Federal do CearÃ, 2011. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=9401.
Testo completoThe soils formed on limestone rocks in semiarid climate of the Apodi Plateau show distinct characteristics of the rest of the state of CearÃ. In Apodi Plateau soils factors of soil formation are homogeneous, what suggests that this geomorphological formation sat up so the exposure time of the parent material of different soils is the same, the relief is homogeneous, the vegetation is caatinga across the Plateau and the distance between different profiles is small to suggest a possible change in climate, so it is supposed that the strong variations in soil classes are closely related to lithological variations. The Apodi Plateau in its Cearense portion covers four municipalities: QuixerÃ, Tabuleiro do Norte, Alto Santo and Limoeiro do Norte, the latter being the search location. The lithological constitution is predominantly limestone with different facies. It was established a transect with approximately 300 m, where observations were made by auger evaluations that allowed to select the locations of the five profiles. Morphological descriptions of the profiles were made and samples collection for physical analysis: granulometry, particle and soil density,determination of the gravel fraction, clay dispersed in water, quantity of nodules, and these were divided into five classes C1, C2, C3, C4 and C5, with diameter from 0.053 to 0.25 mm, 0.25 to 2 mm, 2 to 4.76 mm, 4.76 to 7.9 mm, 7.9 to 19.1 mm, respectively . Chemical analysis were to determine cation exchange capacity - CEC, phosphorus, total organic carbon - TOC, pH in water and KCl, selective dissolution of Fe in Citrate Dithionite Bicarbonate - DCB, Ammonium Oxalate and Sulfuric acid to determine the levels of total Fe, Al and Si in the clay fraction, and determine the molecular indices Ki and Kr. Three profiles were classified as Argissolos and two as Cambissolos. All the profiles showed significative quantity of nodules, which decreased in diameter yet increasing mechanical resistance as they neared the surface, where it had an aspect similar to "chumbo de caÃa." The data showed variations within and between profiles, such as the amount of gravel, which in one of the profiles of Cambissolos fell in the order of 780 g.kg-1 for 30 g.kg-1, a fact corroborated by the levels of Titanium, which indicate that such variations are due to different lithogenic origins. This allows us to conclude that among the factors of soil formation, parent material prints its characteristics as reflected in the different soil classes within a few meters between soil profiles and even a few inches of soil horizons.
Os solos formados sobre rochas calcÃrias no clima semiÃrido da Chapada do Apodi apresentam caracterÃsticas distintas da grande maioria do restante do estado do CearÃ. Nos solos da Chapada, os fatores de formaÃÃo sÃo homogÃneos, ou seja, esta formaÃÃo geomorfolÃgica soergueu e o tempo de exposiÃÃo do material de origem de diferentes solos à o mesmo, o relevo à plano, a vegetaÃÃo à caatinga em toda a extensÃo e a distÃncia entre perfis diferentes à pequena para sugerir uma possÃvel variaÃÃo no clima. Desta maneira, suspeita-se que as fortes variaÃÃes nas classes de solos estÃo intimamente ligadas a variaÃÃes litolÃgicas. A Chapada do Apodi na sua porÃÃo cearense abrange quatro municÃpios, QuixerÃ, Tabuleiro do Norte, Alto Santo e Limoeiro do Norte, sendo neste Ãltimo o local da pesquisa. A constituiÃÃo litolÃgica à predominantemente carbonÃtica, com diferentes fÃcies. No local foi definido um transecto de aproximadamente 300 m, onde foram feitas observaÃÃes por tradagens, que permitiram selecionar os locais dos cinco perfis. Foram feitas as descriÃÃes morfolÃgicas dos perfis e coletas das amostras para anÃlises fÃsicas: granulomÃtrica, densidade das partÃculas e do solo, determinaÃÃo da fraÃÃo cascalho, argila dispersa em Ãgua quantidade de nÃdulos, sendo que estes foram divididos em cinco classes, C1, C2, C3, C4 e C5, com os seguintes diÃmetros 0,053 a 0,25 mm, 0,25 a 2 mm, 2 a 4,76 mm, 4,76 a 7,9 mm, 7,9 a 19,1 mm, respectivamente. As anÃlises quÃmicas foram para determinar capacidade de troca de cÃtions - CTC, fÃsforo, carbono orgÃnico total â COT, pH em Ãgua e KCl, dissoluÃÃes seletivas do Fe em Ditionito Citrato Bicarbonato de SÃdio â DCB, Oxalato de AmÃnio e Ataque SulfÃrico para determinaÃÃo dos teores de totais de Fe, Al e Si na fraÃÃo argila, alÃm de determinar os Ãndices moleculares Ki e Kr. Foram encontrados trÃs perfis de Argissolos e dois Cambissolos. Em todos estes perfis foi encontrada significativa quantidade de nÃdulos, que diminuÃam de diÃmetro, porÃm aumentavam sua resistÃncia mecÃnica à medida que se aproximavam da superfÃcie do solo, onde tinha um aspecto semelhante a âchumbo de caÃaâ. Os dados obtidos mostraram variaÃÃes intra e inter perfis, tais como o teor de cascalho, que em um dos perfis de Cambissolos caiu da ordem de 780 g.kg-1, para 30 g.kg-1 fato corroborado pelos teores de TitÃnio, que sugerem que tais variaÃÃes se devam a diferentes origens litogÃnicas. Isso nos permite concluir que dentre os fatores de formaÃÃo destes solos, o material de origem imprime suas caracterÃsticas de forma que isso se reflete nas diferentes classes de solos distanciados de poucos metros entre perfis e mesmo em poucos centÃmetros entre horizontes de solos.
Balduff, Danielle Marie. "Pedogenesis, inventory, and utilization of subaqueous soils in Chincoteague Bay, Maryland". College Park, Md.: University of Maryland, 2007. http://hdl.handle.net/1903/7732.
Testo completoThesis research directed by: Dept. of Natural Resource Sciences and Landscape Architecture. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
Girmay, Berhane. "Criteria for recognising pedogenesis in buried Quaternary deposits in north-west Wales". Thesis, Bangor University, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261729.
Testo completoDuarte, Lilian Rafaelly de Sousa. "Pedogenesis horizons with character in two toposequences cohesion in tray of coastal CearÃ". Universidade Federal do CearÃ, 2015. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=15108.
Testo completoThe Coastal Tablelands are a geomorphological unit associated with sediments of Barreiras Formation and feature great interest to farm. However, some soils of this region have subsurface horizons with cohesive character, which can cause physical impediments to the development of the root system and the dynamics of water. The genesis of the cohesive character has not yet been fully elucidated, but it is known that occurs naturally. However, some studies have linked the genesis of these horizons to several factors such as particle size of the soil, clay translocation processes and the action of organic and inorganic cementing agents. Thus, this study was conducted in order to obtain greater insight into the characteristics and the genesis of soils with this character. Therefore, soils were studied presenting horizons with cohesive character, seeking to identify and characterize processes that govern the genesis horizons with cohesive character in soils of Coastal Tablelands of CearÃ. The study was conducted in two areas of the Coastal Plains of the state of Cearà (Pacajus and Trairi), where soils are arranged in topossequence and present cohesive character. The samples were subjected to physical fractionation of the sand fraction and morphoscopic analysis. Sequential extraction was carried out on Si surface and subsurface horizons, as well as chemical fractionation of humic substances. The results show that the two areas of study have different processes associated with the genesis of cohesive. In Pacajus soils showed moderate degree of selection, however the high concentration of clay subsurface influences the density of these soils. The cohesive soils of Trairi have a poor degree of selection, which facilitates the adjustment of these particles and the action of low crystalline compounds as cementing agent.
Os Tabuleiros Costeiros constituem uma unidade geomorfolÃgica associada aos sedimentos da FormaÃÃo Barreiras e apresentam grande interesse para exploraÃÃo agrÃcola. No entanto, alguns solos dessa regiÃo apresentam horizontes subsuperficiais com carÃter coeso, os quais podem causar impedimentos fÃsicos ao desenvolvimento do sistema radicular e à dinÃmica da Ãgua. A gÃnese do carÃter coeso ainda nÃo foi completamente esclarecida, apenas sabe-se que ocorre de forma natural. No entanto, alguns trabalhos tÃm associado a gÃnese desses horizontes a diversos fatores como a granulometria dos solos, processos de translocaÃÃo de argila e a aÃÃo de agentes cimentantes orgÃnicos e inorgÃnicos. Dessa forma, este trabalho foi desenvolvido com o intuito de obter maior conhecimento sobre as caracterÃsticas e a gÃnese de solos que apresentam esse carÃter. Para tanto, foram estudados solos que apresentem horizontes com carÃter coeso, procurando-se identificar e caracterizar processos que regem a gÃnese de horizontes com carÃter coeso nos solos dos Tabuleiros Costeiros do CearÃ. O estudo foi realizado em duas Ãreas dos Tabuleiros Costeiros do estado do Cearà (Pacajus e Trairi), nas quais os solos estÃo dispostos em topossequÃncia e apresentam carÃter coeso. As amostras foram submetidas a fracionamento fÃsico da fraÃÃo areia e anÃlise morfoscÃpica. A extraÃÃo sequencial de Si foi realizada em horizontes de superfÃcie e subsuperfÃcie, assim como o fracionamento quÃmico das substÃncias hÃmicas. Os resultados apontam que, as duas Ãreas de estudos apresentam diferentes processos associados à gÃnese do coeso. Em Pacajus os solos apresentaram moderado grau de seleÃÃo, no entanto a elevada concentraÃÃo de argila em subsuperfÃcie influencia o adensamento desses solos. Os solos coesos de Trairi apresentam um pobre grau de seleÃÃo, o que facilita o ajuste dessas partÃculas e a aÃÃo de compostos de baixa cristalinidade como agente cimentante. Os fracionamentos horizontes com carÃter coeso e sem carÃter coeso, entretanto os compostos de baixa cristalinidade apresentam Al com teores mais altos e Si em menor proporÃÃo.
Ogg, Charles Morgan. "Pedogenesis and geomorphic implications of soils developed on Blue Ridge alluvial fans, Virginia". Diss., This resource online, 1995. http://scholar.lib.vt.edu/theses/available/etd-08272007-163709/.
Testo completoNash, Whitney Laine. "Long-Term Effects of Rock Type, Weathering and Amendments on Southwest Virginia Mine Soils". Thesis, Virginia Tech, 2012. http://hdl.handle.net/10919/42657.
Testo completoMaster of Science
Rasmussen, Craig. "Pedogenesis, soil mineralogy, and soil carbon dynamics in Sierra Nevada conifer systems of California /". For electronic version search Digital dissertations database. Restricted to UC campuses. Access is free to UC campus dissertations, 2004. http://uclibs.org/PID/11984.
Testo completoLibri sul tema "Pedogenesis"
Varma, Ajit, e Devendra K. Choudhary, a cura di. Mycorrhizosphere and Pedogenesis. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8.
Testo completoSandler, Amir. A Turonian subaerial event in Israel: Karst, sandstone, and pedogenesis. Jerusalem: Geological Survey of Israel, 1996.
Cerca il testo completoA. K. M. Eakubul Islam. Pedogenesis and mineralogy of some typical deep water rice growing soils of Bangladesh. Uppsala: Swedish University of Agricultural Sciences, Division of Soil Science and Ecochemistry, 1987.
Cerca il testo completoHaryanto, Rachmat. Karakterisasi sifat-sifat mineral, kimia, fisika, pedogenesis dan klasifikasi tanah di kebun percobaan Fakultas Pertanian, Universitas Padjadjaran, Jatinangor: Laporan penelitian. [Jatinangor]: Fakultas Pertanian, Universitas Padjadjaran, 1997.
Cerca il testo completoPérez, Xosé Luis Otero, e Felipe Macías Vazquez. Biogeochemistry and pedogenetic process in saltmarsh and mangrove systems. New York: Nova Science Publishers, 2010.
Cerca il testo completoKubiniok, Jochen. Reliefentwicklung, Pedogenese und geoökologische Probleme agrarischer Nutzung eines tropischen Berglandes: Das Beispiel Nordthailand. Berlin: Gebrüder Borntraeger, 1999.
Cerca il testo completoMahr, Andrea. Lockerbraunerden und periglaziale Hangsedimente im Bayerischen Wald: Untersuchungen zu Paläoumwelt und Geomorphodynamik im Spätglazial und ihrem Einfluss auf die Pedogenese. [Regensburg]: Institut für Geographie an der Universität Regensburg Selbstverlag, 1998.
Cerca il testo completoVarma, Ajit, e Devendra K. Choudhary. Mycorrhizosphere and Pedogenesis. Springer Singapore Pte. Limited, 2020.
Cerca il testo completoVarma, Ajit, e Devendra K. Choudhary. Mycorrhizosphere and Pedogenesis. Springer, 2019.
Cerca il testo completoDuchaufour, P. Pedology: Pedogenesis and Classification. Springer, 2012.
Cerca il testo completoCapitoli di libri sul tema "Pedogenesis"
Blake, George R., Gary C. Steinhardt, X. Pontevedra Pombal, J. C. Nóvoa Muñoz, A. Martínez Cortizas e R. W. Arnold. "Pedology and Pedogenesis". In Encyclopedia of Soil Science, 512–16. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_414.
Testo completoUpadhayay, Viabhav K., Jyoti Singh, Amir Khan, Swati Lohani e Ajay Veer Singh. "Mycorrhizal Mediated Micronutrients Transportation in Food Based Plants: A Biofortification Strategy". In Mycorrhizosphere and Pedogenesis, 1–24. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_1.
Testo completoSharma, Palika, e Gaurav Bhakri. "Role of Bacteria in Pedogenesis". In Mycorrhizosphere and Pedogenesis, 167–79. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_10.
Testo completoBhatt, Pankaj, Divya Joshi, Nitin Kumar e Narendra Kumar. "Recent Trends to Study the Functional Analysis of Mycorrhizosphere". In Mycorrhizosphere and Pedogenesis, 181–90. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_11.
Testo completoVats, Siddharth, Neeraj Gupta e Prachi Bhargava. "Vulnerability of Soil Micro Biota Towards Natural and Anthropogenic Induced Changes and Loss of Pedospheric Functionality". In Mycorrhizosphere and Pedogenesis, 191–205. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_12.
Testo completoBhargava, Prachi, Siddharth Vats e Neeraj Gupta. "Metagenomics as a Tool to Explore Mycorrhizal Fungal Communities". In Mycorrhizosphere and Pedogenesis, 207–19. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_13.
Testo completoJain, Pranay, e Ram Kumar Pundir. "Biocontrol of Soil Phytopathogens by Arbuscular Mycorrhiza – A Review". In Mycorrhizosphere and Pedogenesis, 221–37. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_14.
Testo completoChandra, Prem, e Enespa. "Mycoremediation of Environmental Pollutants from Contaminated Soil". In Mycorrhizosphere and Pedogenesis, 239–74. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_15.
Testo completoDey, Sanjukta, e Rabindranath Bhattacharyya. "The Mycorrhizoshpere Effect on Pedogenesis and Terrestrial Biomes". In Mycorrhizosphere and Pedogenesis, 275–96. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_16.
Testo completoRam, Ratul Moni, Prakash Jyoti Kalita, Rahul Singh Rajput e H. B. Singh. "Mycorrhiza Based Approaches for Soil Remediation and Abiotic Stress Management". In Mycorrhizosphere and Pedogenesis, 297–320. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-6480-8_17.
Testo completoAtti di convegni sul tema "Pedogenesis"
van Deventer, Piet, Anton Bloem e J. Hattingh. "Pedogenesis in Mine Tailings". In First International Seminar on Mine Closure. Australian Centre for Geomechanics, Perth, 2006. http://dx.doi.org/10.36487/acg_repo/605_31.
Testo completoPett-Ridge, Julie, Makenzie Nord e Steven Perakis. "Pedogenesis via Rock-‘eating’ Trees". In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2073.
Testo completoPopov, Leonid, Aureliu Overcenco e Stela Curcubat. "Considerațiuni privind folosirea polipedonului în aprecierea răspîdirii spațiale a solurilor". In Starea actuală a componentelor de mediu. Institute of Ecology and Geography, Republic of Moldova, 2019. http://dx.doi.org/10.53380/9789975315593.11.
Testo completoTotsche, Kai, e Ingrid Koegel-Knabner. "Co-Evolution of Structure, Heterogeneity, and Function During Pedogenesis". In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11003.
Testo completoBerry, Margaret E., Sam Johnstone, Adam Hudson, Harrison J. Gray, Cal Ruleman e Juan-Marcel Campos. "ASPECT, HILLSLOPE PEDOGENESIS, AND THE EMERGENCE OF TOPOGRAPHIC ASYMMETRY". In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-378356.
Testo completoBenson, Craig, e William Albright. "Pedogenesis and soil hydraulic properties – a challenge for design and monitoring". In Seventh International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2012. http://dx.doi.org/10.36487/acg_rep/1208_31_albright.
Testo completoMatchavariani, Lia. "INTENSITY, DISTRIBUTION AND ROLE OF PROFILE-FORMING PROCESSES IN PEDOGENESIS OF GEORGIA". In 15th International Multidisciplinary Scientific GeoConference SGEM2015. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2015/b32/s13.027.
Testo completoChangli Liu, Chao Song, Yun Zhang, Hongbing Hou, Xiuyan Wang, Jianmei Jiang, Jingjing Wang e Lixin Pei. "The influence of farmyard manure utilization on the pedogenesis of carbonate rocks". In 2011 International Symposium on Water Resource and Environmental Protection (ISWREP). IEEE, 2011. http://dx.doi.org/10.1109/iswrep.2011.5893591.
Testo completoHobbs, Kevin M., Gage Richards Lamborn e April Renee Bates. "DUST-DOMINATED CUMULIC ARIDISOL PEDOGENESIS DOMINATED THE PLIOCENE TAOS PLATEAU, NEW MEXICO, USA". In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334721.
Testo completoKogler, Sarah, e Daniel I. Hembree. "INFLUENCES OF MODERN PEDOGENESIS ON PALEOCLIMATE ESTIMATES FROM PENNSYLVANIAN AND PERMIAN PALEOSOLS, SOUTHEAST OHIO". In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302577.
Testo completoRapporti di organizzazioni sul tema "Pedogenesis"
Савосько, Василь Миколайович, Юлія Бєлик e Юрій Васильович Лихолат. Ecological and Geological Determination of the Initial Pedogenesis on Devastated Lands in the Kryvyi Rih Iron Mining & Metallurgical District (Ukraine). Journ. Geol. Geograph. Geoecology, 2019. http://dx.doi.org/10.31812/123456789/3643.
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