Relevant bibliographies by topics / Soil profiles Soil formation Bodenentwicklung

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Soil profiles Soil formation Bodenentwicklung'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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Journal articles on the topic "Soil profiles Soil formation Bodenentwicklung"

1

Heusch, Karl, Johannes Botschek, and Armin Skowronek. "Zur jungholozänen Oberflächen- und Bodenentwicklung der Siegaue im Hennefer Mäanderbogen." E&G Quaternary Science Journal 46, no. 1 (1996): 18–31. http://dx.doi.org/10.3285/eg.46.1.02.

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Abstract. The flood loams in the Sieg valley near Hennef were investigated with geomorphological, sedimentological and pedological methods. They are free of carbonate. Four late Holocene floodplain terraces can be seperated and dated. On the Upper Floodplain Terrace an Auenparabraunerde-Auenbraunerde (Fluvi-Luvic Cambisol) of early Iron Age was found. The pedogenesis on the older Middle Floodplain Terrace lead to a Typische Auenbraunerde (Fluvi-Eutric Cambisol) of Latene Age. The younger part of this terrace is covered by a Braunauenboden (Eutric Fluvisol) of late Middle Ages/modern times. The
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2

Suresh, P. O., A. Dosseto, P. P. Hesse, and H. K. Handley. "Soil formation rates determined from Uranium-series isotope disequilibria in soil profiles from the southeastern Australian highlands." Earth and Planetary Science Letters 379 (October 2013): 26–37. http://dx.doi.org/10.1016/j.epsl.2013.08.004.

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3

Gavrilov, Denis, Sergey Loiko, and Nina Klimova. "Holocene Soil Evolution in South Siberia Based on Phytolith Records and Genetic Soil Analysis (Russia)." Geosciences 8, no. 11 (2018): 402. http://dx.doi.org/10.3390/geosciences8110402.

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Dark, coniferous hemiboreal forests in the south of West Siberia are located in the Holocene forest-steppe ecotone, where natural environmental conditions have been quite dynamic. This dynamic environment resulted in the contrasting evolution of regional soil cover and the development of unique soil profiles with the second humus horizon. The second humus horizon is assumed to be a relic from the dark-humus soil formation stage in the mid-Holocene. This article draws conclusions about changes in regional environmental conditions by analysing data from a geochemically interrelated coevolutionar
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Bobrovskii, M. V. "The role of windfall pedoturbations in the formation of forest soil profiles." Eurasian Soil Science 41, no. 13 (2008): 1366–70. http://dx.doi.org/10.1134/s1064229308130036.

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Liebmann, Patrick, Patrick Wordell-Dietrich, Karsten Kalbitz, et al. "Relevance of aboveground litter for soil organic matter formation – a soil profile perspective." Biogeosciences 17, no. 12 (2020): 3099–113. http://dx.doi.org/10.5194/bg-17-3099-2020.

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Abstract. In contrast to mineral topsoils, in subsoils the origin and processes leading to the formation and stabilization of organic matter (OM) are still not well known. This study addresses the fate of litter-derived carbon (C) in whole soil profiles with regard to the conceptual cascade model, which proposes that OM formation in subsoils is linked to sorption–microbial processing–remobilization cycles during the downward migration of dissolved organic carbon (DOC). Our main objectives were to quantify the contribution of recent litter to subsoil C stocks via DOC translocation and to evalua
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6

Németh, Tibor, and P. Sipos. "Characterization of Clay Minerals in Brown Forest Soil Profiles (Luvisols) of the Cserhát Mountains (North Hungary)." Agrokémia és Talajtan 55, no. 1 (2006): 39–48. http://dx.doi.org/10.1556/agrokem.55.2006.1.5.

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The clay mineral composition of four brown forest soil profiles (Luvisols) developed on different parent rocks was studied in detail to determine the major clay mineral alteration processes. In the studied profiles a siltstone bedrock weathered to chlorite/vermiculite and vermiculite in a less developed, shallow soil profile, while the major product of soil formation in a clayey, well-developed deep soil is a typical soil montmorillonite with heterogeneous charge distribution. The most possible pathway of clay alteration is illite smectitization via charge reduction, and considerable degradati
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7

Becker-Heidmann, Peter, та Hans-Wilhelm Scharpenseel. "Thin Layer δ13C and D14C Monitoring of “Lessive” Soil Profiles". Radiocarbon 28, № 2A (1986): 383–90. http://dx.doi.org/10.1017/s0033822200007499.

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The natural 14C and 13C content of soil organic matter and their dependence on depth for two Alfisols are presented. This soil type which covers a large area of the earth's surface is characterized by clay migration processes (“Lessivé”). The samples were taken as successive horizontal layers of 2cm depth from an area of ca lm2 size as deep as the C content allows 14C analysis. The minima of the D14C distribution decrease with depth, while the maxima increase in the upper, leached horizon (A1) due to bomb 14C and decrease in the lower, clay illuviated (Bt). δ13C indicates proceeding decomposit
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8

Iavid, Elizaveta Iaroslavovna, Veronika Nikolaevna Kondakova, Vyacheslav Igorevich Polyakov, and Evgeny Vasilyevic Abakumov. "Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago)." Czech Polar Reports 8, no. 1 (2018): 43–59. http://dx.doi.org/10.5817/cpr2018-1-4.

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Svalbard archipelago is characterized by specific climate conditions, high air temperature and relative air humidity, which are not typical for high latitudes. Such conditions affect soil-forming processes. Classification and morphological structure of the soil cover on the Spitsbergen archipelago are still poorly understood. The aim of current research was to reveal diverse soil taxons in the Gronfjord area and characterize framework of its formation. As the results of this work, the authors provide the description of the investigated soils and their taxonomy in accordance with World Referenc
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9

Medvedev, V. V. "Agrizem as a new 4-dimensional polygenetic formation." Fundamental and Applied Soil Science 17, no. 1-2 (2016): 5–21. http://dx.doi.org/10.15421/041601.

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Morphological (horizontal and vertical profiles of soils), micromorphological (mainly, anisotropism of aggregates and pores), physical properties (structure, density, differential porosity and their transformation for an appreciable length of time – time profiles), features of formation of descending (preferential) and ascending waterstreams were investigated. Chernozems (typical, ordinary, southern) were objects of the research. In the article the results of comparative researches of the soils which are in various conditions of use – from absolutely reserved virgin soil to variants in industr
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10

Farias, Phâmella Kalliny Pereira, Carolina Malala Martins Souza, Jeane Cruz Portela, Isadora Nayara Bandeira Medeiros de Moura, and Ana Carla Rodrigues da Silva. "GENESIS AND CHARACTERISTICS OF SOILS OF THE SANTANAMOUNTAIN RANGE IN THE SERIDÓ REGION, RIO GRANDE DO NORTE, BRAZIL." Revista Caatinga 31, no. 4 (2018): 1017–26. http://dx.doi.org/10.1590/1983-21252018v31n425rc.

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ABSTRACT Rio Grande do Norte has mountain formations with edaphoclimatic conditions different from those predominating in the state, presenting deeper,acid soils, and milder climate. Among these formations, is the Santana mountain range, which is part of the Serra do Martins Formation. The objective of this work was to interpret the pedogenesis of the representative soils of the Santana mountain range through morphological, physical, and chemical characterizations of soil profiles and evaluate the effect of these attributes on the distribution of pedological forms along the landscape using mul
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Dissertations / Theses on the topic "Soil profiles Soil formation Bodenentwicklung"

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Lorz, C. "Ein substratorientiertes Boden-Evolutions-Konzept für geschichtete Bodenprofile : Genese und Eigenschaften von lithologisch diskontinuierlichen Böden /." Berlin : Gebrüder Borntraeger, 2008. http://d-nb.info/987000470/04.

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Taha, Ammar. "Etude expérimentale et numérique de la contribution des eaux infiltrées à la formation des débits des crues en zone méditerranéenne : application à un versant du Real Collobrier." Université Joseph Fourier (Grenoble), 1995. http://www.theses.fr/1995GRE10052.

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L'objectif de ce travail est de contribuer a la comprehension du fonctionnement hydrologique d'un bassin versant mediterraneen, notamment a l'occasion de ses crues. Il est compose d'un premier volet experimental destine a l'observation du comportement des eaux souterraines. Ce volet inclut des mesures de pression de l'eau dans le sol et de niveaux des nappes (fugitives ou perennes) sous un versant (ligne de plus grande pente perpendiculaire a la riviere), et une analyse approfondie des sols du versant: granulometries, conductivites hydrauliques in situ mesurees a l'aide de differents appareill
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3

Zomeni, Zomenia. "Quaternary marine terraces on Cyprus : constraints on uplift and pedogenesis, and the geoarchaeology of Palaipafos." Thesis, 2012. http://hdl.handle.net/1957/30355.

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Numerous flights of Quaternary marine terraces are present around the island of Cyprus, in the Eastern Mediterranean. These terraces are a result of the global eustatic sea-level curve and local tectonism. Marine Isotope Stage (MIS) 5 through MIS 13 terraces are identified, mapped and dated. Palaeoshoreline elevation, an excellent indicator for a past sea–level, and new numerical geochronology are used to calculate an Upper Pleistocene uplift rate for various coastal sectors. Southwestern Cyprus presents the highest uplift rates of 0.35-0.65 mm/year with other sections suggesting uplift of 0.0
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Books on the topic "Soil profiles Soil formation Bodenentwicklung"

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Buol, S. W. Soil genesis and classification. 3rd ed. Iowa State University Press, 1989.

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2

Franco, E. P. Cardoso. Aplicação de métodos de análise multivariante no teste da uniformidade, intrapédones e interpédones, do material originario do solo. Ministério do Planeamento e da Administração do Território, Secretaria de Estado da Ciência e Tecnologia, 1994.

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3

Soil Genesis and Classification. 5th ed. Iowa State Press, 2002.

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4

Genesis and residence times of soil and weathering profiles on residual and transported parent materials in the Pine Mountain area of west-central Georgia. U.S. G.P.O., 1994.

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Book chapters on the topic "Soil profiles Soil formation Bodenentwicklung"

1

Cline, Marlin G. "Major Kinds of Profiles and Their Relationships in New York." In Selected Papers in Soil Formation and Classification. Soil Science Society of America, Inc., 2015. http://dx.doi.org/10.2136/sssaspecpub1.c2.

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2

St. Arnaud, R. J., and E. P. Whiteside. "Morphology and Genesis of a Chernozemic to Podzolic Sequence of Soil Profiles in Saskatchewan." In Selected Papers in Soil Formation and Classification. Soil Science Society of America, Inc., 2015. http://dx.doi.org/10.2136/sssaspecpub1.c29.

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3

"Studying Soil Profiles." In Soil Formation. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-0-585-31788-5_5.

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"Studying Soil Profiles." In Soil Formation. Springer Netherlands, 2003. http://dx.doi.org/10.1007/0-306-48163-4_5.

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5

"SOIL FORMATION—PROCESSES AND PROFILES." In Soils and Environment. Routledge, 2002. http://dx.doi.org/10.4324/9780203415245-14.

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6

Deutscher, M. S., J. M. Gasmo, H. Rahardjo, E. C. Leong, and S. K. Tang. "Field measurements of pore-water pressure profiles in residual soil slopes of the Bukit Timah Granite Formation, Singapore." In Unsaturated Soils for Asia. CRC Press, 2020. http://dx.doi.org/10.1201/9781003078616-139.

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7

Holliday, Vance T. "Conceptual Approaches to Pedogenesis." In Soils in Archaeological Research. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195149654.003.0006.

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To fully appreciate and apply pedologic principals in archaeology, some of the theoretical underpinnings of pedology and especially soil geomorphology must be outlined. Pedologists and soil geomorphologists have attempted to describe, if not model, the processes of soil formation, the factors that drive the processes, and the evolution of soils as landscapes evolve (summarized by Smeck et al., 1983; Johnson and Watson-Stegner, 1987; and Gerrard, 1992, pp. 1–50, 217–220). The task is a difficult one, however, because of the complex and variable sets of processes responsible for soil development. Several of the resulting approaches have proven useful for conceptualizing pedogenesis and, more important, for interpreting soils. In addition to understanding soil-forming processes for interpreting soil profiles, understanding soil formation is important for understanding site formation. The conceptual approaches particularly useful in soil geomorphic and geoarchaeological research are summarized below. Soil-forming processes as components of site formation are discussed more fully in chapter 10. The following discussions of conceptual approaches to pedogenesis are roughly arranged in order of increasing complexity. The “multiple-process model” is essentially a categorization of soil-forming processes. It does not explain pedogenesis but is a useful way to sort and group the many soil-forming processes. The “state factor” approach and the “K-cycle” concept do not deal directly with soil formation, but instead focus on important external factors and processes that drive or affect pedogenesis such as climate and geomorphic evolution. The “soil evolution” model and the “new global view of soils” attempt to integrate pedogenic process with landscape evolution, climate, and other factors. This section closes with discussion of two important aspects of pedogenesis and pedogenic pathways that offer caveats in the use of soils for reconstructing the past. Soils are the result of biogeochemical processes determined and driven by the ecosystem (following Buol et al., 1997). This relationship is more simply described as “internal soil-forming processes” driven by “external soil-forming factors” (fig. 3.1; after Buol et al., 1984). A useful approach to categorizing the many and varied internal soil-forming processes responsible for pedogenesis is the multiple-process model of Simonson (1959, 1978).
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Conference papers on the topic "Soil profiles Soil formation Bodenentwicklung"

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Spirina, V. Z., L. V. Khotskova, and E. A. Zharikova. "PROPERTIES AND ELEMENT COMPOSITION OF SOILS OF THE DENDROLOGICAL TERRITORY OF THE SIBERIAN BOTANICAL GARDEN." In Prirodopol'zovanie i ohrana prirody: Ohrana pamjatnikov prirody, biologicheskogo i landshaftnogo raznoobrazija Tomskogo Priob'ja i drugih regionov Rossii. Izdatel'stvo Tomskogo gosudarstvennogo universiteta, 2020. http://dx.doi.org/10.17223/978-5-94621-954-9-2020-55.

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The properties, content and profile distribution of macroelements in the soils of the dendrological territory of the Siberian Botanical Garden were studied. The nature of the distribution of chemical elements in soil profiles is revealed depending on the intensity of sod, podzolic and glue soil formation processes.
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Haghighi, Ali, Jitender Rai, Yann Le Maout, and John Oliphant. "An Improved Approach for Modelling Reliability of Buckle Formation for Subsea Pipelines." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61377.

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Lateral buckling (LB) design for subsea pipelines generally requires reliability analysis to evaluate the probability that a lateral buckling mitigation system will behave as expected, which means that the engineered initiators will trigger buckles sequentially before any uncontrolled buckle can form in between. As various parameters involved in the buckle formation process are uncertain (soil characteristics, residual horizontal and vertical Out of Straightness (OOS) after pipelay), a probabilistic approach is used to assess the likelihood that the pipeline will buckle at the intended locatio
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