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Artículos de revistas sobre el tema "Pedogenesis"

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Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 29 de enero de 2023

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1

Medeiros, Edgardo Ramos, Fabrício De Araújo Pedron y Anderson Augusto Volpato Sccoti. "EVIDÊNCIAS DE PEDOGÊNESE ALÓCTONE SOBRE ARENITOS BOTUCATU NO SUDOESTE GAÚCHO". Ciência e Natura 35, n.º 1 (22 de octubre de 2013): 43. http://dx.doi.org/10.5902/2179460x9600.

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The southwestern region of Rio Grande do Sul (RS) is characterized by large portions of sandy soils that have high environmental vulnerability, due to their low fertility and high susceptibility to erosion. Some of these soils have increased clay, suggesting allochtonous pedogenesis. In this case, the aims of this study were to determine evidence of allochtonous pedogenesis on sandstones Botucatu Formation in the southwestern region of the RS. A profile of Argissolo Vermelho and other of Neossolos Quartzarênico were analyzed, both formed on quartz sandstones of the Botucatu formation. Through morphological, physical, chemical and mineralogical analysis was possible to verify the process of allochthonous pedogenesis by higher clay content in the B horizon of the Argissolo profile and confirmed by the absence of clay forming minerals in the rock and in the presence of ilmenite in the pedogenetic horizons and its absence in the rock matrix. The environmental conditions suggest that the ilmenite originates from alteration of the surrounding volcanic rocks.

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2

UGOLINI, F. C., M. G. STONER y D. J. MARRETT. "ARCTIC PEDOGENESIS". Soil Science 144, n.º 2 (agosto de 1987): 90–100. http://dx.doi.org/10.1097/00010694-198708000-00002.

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3

STONER, M. G. y F. C. UGOLINI. "ARCTIC PEDOGENESIS". Soil Science 145, n.º 1 (enero de 1988): 46–51. http://dx.doi.org/10.1097/00010694-198801000-00006.

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4

Cunha, 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.º 3/4 (2016): 110–25. http://dx.doi.org/10.1097/ss.0000000000000144.

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5

Phillips, Jonathan D. "Soil Complexity and Pedogenesis". Soil Science 182, n.º 4 (abril de 2017): 117–27. http://dx.doi.org/10.1097/ss.0000000000000204.

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6

JOHNSON, D. L. y D. WATSON-STEGNER. "EVOLUTION MODEL OF PEDOGENESIS". Soil Science 143, n.º 5 (mayo de 1987): 349–66. http://dx.doi.org/10.1097/00010694-198705000-00005.

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7

Chesworth, Ward. "Pedogenesis and soil taxonomy". Geochimica et Cosmochimica Acta 49, n.º 1 (enero de 1985): 309. http://dx.doi.org/10.1016/0016-7037(85)90214-5.

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8

Leguédois, Sophie, Geoffroy Séré, Apolline Auclerc, Jérôme Cortet, Hermine Huot, Stéphanie Ouvrard, Françoise Watteau, Christophe Schwartz y Jean Louis Morel. "Modelling pedogenesis of Technosols". Geoderma 262 (enero de 2016): 199–212. http://dx.doi.org/10.1016/j.geoderma.2015.08.008.

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9

Rodriguez, Victoria, Lisa-Marie Moskwa, Rómulo Oses, Peter Kühn, Nicolás Riveras-Muñoz, Oscar Seguel, Thomas Scholten y 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.º 5 (20 de abril de 2022): 847. http://dx.doi.org/10.3390/microorganisms10050847.

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Soil bacteria play a fundamental role in pedogenesis. However, knowledge about both the impact of climate and slope aspects on microbial communities and the consequences of these items in pedogenesis is lacking. Therefore, soil-bacterial communities from four sites and two different aspects along the climate gradient of the Chilean Coastal Cordillera were investigated. Using a combination of microbiological and physicochemical methods, soils that developed in arid, semi-arid, mediterranean, and humid climates were analyzed. Proteobacteria, Acidobacteria, Chloroflexi, Verrucomicrobia, and Planctomycetes were found to increase in abundance from arid to humid climates, while Actinobacteria and Gemmatimonadetes decreased along the transect. Bacterial-community structure varied with climate and aspect and was influenced by pH, bulk density, plant-available phosphorus, clay, and total organic-matter content. Higher bacterial specialization was found in arid and humid climates and on the south-facing slope and was likely promoted by stable microclimatic conditions. The presence of specialists was associated with ecosystem-functional traits, which shifted from pioneers that accumulated organic matter in arid climates to organic decomposers in humid climates. These findings provide new perspectives on how climate and slope aspects influence the composition and functional capabilities of bacteria, with most of these capabilities being involved in pedogenetic processes.

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10

Jigău, Gheorghe, Liviu Apostol, Ana Barsan y 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.º 1 (1 de mayo de 2015): 111–27. http://dx.doi.org/10.1515/pesd-2015-0007.

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Abstract Component part of the Carpathian-Danubian-Pontic space, the interfluve area between Prut and Dniester is subject to the regional process of climate evolution and change. In what regards the concept of human-influenced pedogenesis, the role of the biological factor is significantly reduced. As a consequence the direction and intensity of the elementary landscape and pedogenetic processes are determined by the relations between climate and the geomorphological factor. In the conditions of a relative stability of the geomorphological factor, the determining role is held by climate. To this is added soil vulnerability to the implications of climate changes, determined by the degree of soil physical degradation but also by a series of intrinsic and external (drainage) factors. This implies the idea of the control and management of the landscape and pedogenetic implications of climate changes by improving soil physical characteristics.

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11

Brevik, Eric C. y Andreas G. Lazari. "Rates of Pedogenesis in Reclaimed Lands as Compared to Rates of Natural Pedogenesis". Soil Horizons 55, n.º 1 (2014): 0. http://dx.doi.org/10.2136/sh13-06-0017.

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12

Phillips, Jonathan D. "Progressive and Regressive Pedogenesis and Complex Soil Evolution". Quaternary Research 40, n.º 2 (septiembre de 1993): 169–76. http://dx.doi.org/10.1006/qres.1993.1069.

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AbstractThe simultaneous operation of regressive and progressive pedogenetic pathways raises the possibility that soil evolution may exhibit patterns far richer and more complex than increasing development over time. This possibility is explored via a numerical model incorporating the relative rates of progressive and regressive pedogenesis and feedbacks between these rates and the degree of soil development. This model may exhibit deterministic chaos and sensitive dependence on initial conditions with realistic parameter values. Variations in profile development in a region of the North Carolina Coastal Plain where soil-forming factors are relatively constant is consistent with deterministic chaos. Chaotic soil evolution suggests that soil development may reflect the interplay between progressive and regressive soil-forming processes in addition to—or instead of—the age of a surface or deposit. The former may produce a state of development which is unique to a particular time, sensitively dependent on the (unknown) initial conditions, and not simply related to age. Soils and their genetic signatures as indicators of relative ages and Quaternary environments may need to be reinterpreted in this light.

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13

PROTZ, R., M. J. SHIPITALO, G. J. ROSS y J. TERASMAE. "PODZOLIC SOIL DEVELOPMENT IN THE SOUTHERN JAMES BAY LOWLANDS, ONTARIO". Canadian Journal of Soil Science 68, n.º 2 (1 de mayo de 1988): 287–305. http://dx.doi.org/10.4141/cjss88-028.

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Nine soil profiles from a 52-km-long transect orthogonal to the coast of Southern James Bay range in age from 1000 to 3000 yr. The depth of carbonate leaching, mass of vermiculite clay formation, profile organic matter and amorphous material (Fe, Al and Si) accumulation were determined. Rates of these pedogenetic processes were calculated, and compared to rates in a cooler, drier area on the Hudson Bay Coast. The rates are about twice as rapid in the southern James Bay area as in the Hudson Bay Coastal zone. These differences in rates are explained on the basis of mean annual temperature and precipitation. Key words: Vermiculite, carbonate leaching, rates of pedogenesis

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14

Delgado-Baquerizo, Manuel, Richard D. Bardgett, Peter M. Vitousek, Fernando T. Maestre, Mark A. Williams, David J. Eldridge, Hans Lambers et al. "Changes in belowground biodiversity during ecosystem development". Proceedings of the National Academy of Sciences 116, n.º 14 (15 de marzo de 2019): 6891–96. http://dx.doi.org/10.1073/pnas.1818400116.

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Belowground organisms play critical roles in maintaining multiple ecosystem processes, including plant productivity, decomposition, and nutrient cycling. Despite their importance, however, we have a limited understanding of how and why belowground biodiversity (bacteria, fungi, protists, and invertebrates) may change as soils develop over centuries to millennia (pedogenesis). Moreover, it is unclear whether belowground biodiversity changes during pedogenesis are similar to the patterns observed for aboveground plant diversity. Here we evaluated the roles of resource availability, nutrient stoichiometry, and soil abiotic factors in driving belowground biodiversity across 16 soil chronosequences (from centuries to millennia) spanning a wide range of globally distributed ecosystem types. Changes in belowground biodiversity during pedogenesis followed two main patterns. In lower-productivity ecosystems (i.e., drier and colder), increases in belowground biodiversity tracked increases in plant cover. In more productive ecosystems (i.e., wetter and warmer), increased acidification during pedogenesis was associated with declines in belowground biodiversity. Changes in the diversity of bacteria, fungi, protists, and invertebrates with pedogenesis were strongly and positively correlated worldwide, highlighting that belowground biodiversity shares similar ecological drivers as soils and ecosystems develop. In general, temporal changes in aboveground plant diversity and belowground biodiversity were not correlated, challenging the common perception that belowground biodiversity should follow similar patterns to those of plant diversity during ecosystem development. Taken together, our findings provide evidence that ecological patterns in belowground biodiversity are predictable across major globally distributed ecosystem types and suggest that shifts in plant cover and soil acidification during ecosystem development are associated with changes in belowground biodiversity over centuries to millennia.

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15

Lisetskii, F. "Biogeochemical features of soil formation without parent rock in natural conditions and in an urban environment". IOP Conference Series: Earth and Environmental Science 1010, n.º 1 (1 de abril de 2022): 012018. http://dx.doi.org/10.1088/1755-1315/1010/1/012018.

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Abstract The aim of the present study is to establish the biogeochemical characteristics of the primary soil formation, separately for natural conditions (protected areas) and urban environment (with incoming technogenic aerosols) for pedogenesis models when there is no parent rock (“upward soil growth”). This makes it possible to assess the contribution of the still poorly studied pedogenesis factors that can form the specific geochemical features of the material composition of soils non-inherited from the parent rock, and without the involvement of biogenic bottom-up migration of elements. We have studied two contrasting regions to perform a comparative analysis of pedogenesis conditions. We have compared embryonic soils on megalithic gabbro-diabase blocks in a 17th century defence wall located on the territory of a natural reserve, 1 km away from the Black Sea coast (ecologically clean area) and a 45-year solid bitumen cover between a thermal power plant and a busy railway (an industrial zone in the central part of the city). In the natural reserve, the average dust deposition rate was 0.82 um yr1 (0.082 mm/100 yr) due to stardust, atmospheric aerosols and biogenic processes of pedogenesis. The mineral part of soils, which had formed on the solid bitumen in 45 years in the city’s industrial zone, differs from the soil developed in 320-350 years without the involvement of the parent rock in the protected area by higher content of V (9 times) and Cr (2 times), as well as CaO, SiO2 and Pb. In the industrial zone of the city, emission dust mostly contributes to the accumulation of V, Cr and Cu in comparison with the pedogenesis conditions in the ecologically clean area, where the rate of solid-phase soil matter accumulation is twice lower due to background aerosols and biogenic factors.

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16

., E. U. Onweremadu. "Pedogenesis of Soils of a Colliery". Research Journal of Environmental Toxicology 1, n.º 4 (1 de abril de 2007): 184–90. http://dx.doi.org/10.3923/rjet.2007.184.190.

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17

Bonifacio, Eleonora y Elisabetta Barberis. "PHOSPHORUS DYNAMICS DURING PEDOGENESIS ON SERPENTINITE". Soil Science 164, n.º 12 (diciembre de 1999): 960–68. http://dx.doi.org/10.1097/00010694-199912000-00009.

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18

Pozdnyakov, A. I. "Electrical parameters of soils and pedogenesis". Eurasian Soil Science 41, n.º 10 (octubre de 2008): 1050–58. http://dx.doi.org/10.1134/s1064229308100062.

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19

Laliberté, Etienne, James B. Grace, Michael A. Huston, Hans Lambers, François P. Teste, Benjamin L. Turner y David A. Wardle. "How does pedogenesis drive plant diversity?" Trends in Ecology & Evolution 28, n.º 6 (junio de 2013): 331–40. http://dx.doi.org/10.1016/j.tree.2013.02.008.

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20

Turner, Benjamin L., Leo M. Condron, Sarah J. Richardson, Duane A. Peltzer y Victoria J. Allison. "Soil Organic Phosphorus Transformations During Pedogenesis". Ecosystems 10, n.º 7 (2 de octubre de 2007): 1166–81. http://dx.doi.org/10.1007/s10021-007-9086-z.

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21

Kleber, Markus, Christian Mikutta y Reinhold Jahn. "Andosols in Germany—pedogenesis and properties". CATENA 56, n.º 1-3 (abril de 2004): 67–83. http://dx.doi.org/10.1016/j.catena.2003.10.015.

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22

Minasny, Budiman, Alex B. McBratney y Sébastien Salvador-Blanes. "Quantitative models for pedogenesis — A review". Geoderma 144, n.º 1-2 (marzo de 2008): 140–57. http://dx.doi.org/10.1016/j.geoderma.2007.12.013.

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23

RUTHERFORD, G. K. y D. J. THACKER. "CHARACTERISTICS OF TWO MAFIC SAPROLITES AND THEIR ASSOCIATED SOIL PROFILES IN CANADA". Canadian Journal of Soil Science 68, n.º 2 (1 de mayo de 1988): 223–31. http://dx.doi.org/10.4141/cjss88-022.

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Two soil profiles developed from mafic saprolites were examined at Economy Mountain, Nova Scotia and Kamloops, British Colombia. The underlying rocks, a tholeiitic basalt in Nova Scotia and a basic greenstone schist at Kamloops, were apparently transformed to predominantly smectitic saprolites in pre-Holocene times. During the Wisconsinan glacial stage the sola and a significant portion of the saprolites were removed. Holocene pedogenesis has produced new sola on the saprolites. In Nova Scotia, the solum may have some locally derived till or colluvium component. Key words: Mafic pedogenesis, Paleosols, soil mineralogy

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24

Zerboni, Andrea, Guido S. Mariani, Lanfredo Castelletti, Elena S. Ferrari, Marco Tremari, Franz Livio y Rivka Amit. "Was the Little Ice Age the coolest Holocene climatic period in the Italian central Alps?" Progress in Physical Geography: Earth and Environment 44, n.º 4 (7 de noviembre de 2019): 495–513. http://dx.doi.org/10.1177/0309133319881105.

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The Estimation of the relative intensity of different cold periods occurring during the Late Quaternary is a difficult task, particularly in non-glaciated mountain landscapes and where high- to medium-resolution archives for proxy data are lacking. In this paper, we study a Holocene polycyclic soil sequence in the central Alps (Val Cavargna, Northern Italy) to estimate climatic parameters (specifically Temperature) changes in non-glaciated, high altitude environments. We investigate this key site through palaeopedological and micromorphological analyses in order to understand phases of soil development and detect hidden evidence of cold conditions during its formation. Three phases of pedogenesis can be recognized and attributed in time to different periods during the Holocene. Pedogenetic phases were separated by two truncation and deposition episodes related to the reactivation of slope processes under cold conditions at the onset of the Neoglacial and the Iron Age Cold Epoch, respectively. Micromorphological evidence of frost action in the soil can instead relate to pedogenetic processes acting in the Little Ice Age. The different expression of these three cold periods corresponds to changes in climatic conditions, pointing to the Little Ice Age as a cooler/drier period in comparison to the preceding ones.

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25

Prietzel, Jörg, Jaane Krüger, Klaus Kaiser, Wulf Amelung, Sara L. Bauke, Michaela A. Dippold, Ellen Kandeler et al. "Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material". Biogeochemistry 158, n.º 1 (febrero de 2022): 39–72. http://dx.doi.org/10.1007/s10533-021-00884-7.

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AbstractSustainable forest management requires understanding of ecosystem phosphorus (P) cycling. Lang et al. (2017) [Biogeochemistry,https://doi.org/10.1007/s10533-017-0375-0] introduced the concept of P-acquiring vs. P-recycling nutrition strategies for European beech (Fagus sylvatica L.) forests on silicate parent material, and demonstrated a change from P-acquiring to P-recycling nutrition from P-rich to P-poor sites. The present study extends this silicate rock-based assessment to forest sites with soils formed from carbonate bedrock. For all sites, it presents a large set of general soil and bedrock chemistry data. It thoroughly describes the soil P status and generates a comprehensive concept on forest ecosystem P nutrition covering the majority of Central European forest soils. For this purpose, an Ecosystem P Nutrition Index (ENIP) was developed, which enabled the comparison of forest P nutrition strategies at the carbonate sites in our study among each other and also with those of the silicate sites investigated by Lang et al. (2017). The P status of forest soils on carbonate substrates was characterized by low soil P stocks and a large fraction of organic Ca-bound P (probably largely Ca phytate) during early stages of pedogenesis. Soil P stocks, particularly those in the mineral soil and of inorganic P forms, including Al- and Fe-bound P, became more abundant with progressing pedogenesis and accumulation of carbonate rock dissolution residue. Phosphorus-rich impure, silicate-enriched carbonate bedrock promoted the accumulation of dissolution residue and supported larger soil P stocks, mainly bound to Fe and Al minerals. In carbonate-derived soils, only low P amounts were bioavailable during early stages of pedogenesis, and, similar to P-poor silicate sites, P nutrition of beech forests depended on tight (re)cycling of P bound in forest floor soil organic matter (SOM). In contrast to P-poor silicate sites, where the ecosystem P nutrition strategy is direct biotic recycling of SOM-bound organic P, recycling during early stages of pedogenesis on carbonate substrates also involves the dissolution of stable Ca-Porg precipitates formed from phosphate released during SOM decomposition. In contrast to silicate sites, progressing pedogenesis and accumulation of P-enriched carbonate bedrock dissolution residue at the carbonate sites promote again P-acquiring mechanisms for ecosystem P nutrition.

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26

Demas, George P. y Martin C. Rabenhorst. "Subaqueous Soils Pedogenesis in a Submersed Environment". Soil Science Society of America Journal 63, n.º 5 (septiembre de 1999): 1250–57. http://dx.doi.org/10.2136/sssaj1999.6351250x.

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27

Scalenghe, Riccardo, Eleonora Bonifacio, Luisella Celi, Fiorenzo C. Ugolini y Ermanno Zanini. "Pedogenesis in disturbed alpine soils (NW Italy)". Geoderma 109, n.º 3-4 (octubre de 2002): 207–24. http://dx.doi.org/10.1016/s0016-7061(02)00176-3.

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28

Autin, W. J., A. Aslan, E. A. Bettis y P. M. Walthall. "Report from working group on alluvial pedogenesis". Quaternary International 51-52 (enero de 1998): 85–86. http://dx.doi.org/10.1016/s1040-6182(98)90233-6.

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29

Bouzouidja, Ryad, Gustave Rousseau, Violaine Galzin, Rémy Claverie, David Lacroix y Geoffroy Séré. "Green roof ageing or Isolatic Technosol’s pedogenesis?" Journal of Soils and Sediments 18, n.º 2 (22 de julio de 2016): 418–25. http://dx.doi.org/10.1007/s11368-016-1513-3.

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30

Haslinger, E., F. Ottner y U. S. Lundström. "Pedogenesis in the Alnö carbonatite complex, Sweden". Geoderma 142, n.º 1-2 (noviembre de 2007): 127–35. http://dx.doi.org/10.1016/j.geoderma.2007.08.014.

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31

Meulemans, Germain. "Urban Pedogeneses". Environmental Humanities 12, n.º 1 (1 de mayo de 2020): 250–66. http://dx.doi.org/10.1215/22011919-8142330.

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Abstract This article examines the rise of urban soils as a topic of scientific inquiry and ecological engineering in France, and questions how new framings of soil as a material that can be designed reconfigure relationships between urban life and soils in a context of fast-growing cities. As a counterpoint to the current situation, the article first examines how the hard-surfacing of Paris, in the nineteenth century, sought to background the vital qualities of soils in urban areas, making their absence seem perfectly stable and natural. It then shows how the new urban soil science moved away from classical descriptive approaches to soils, and set out to fabricate soils as a research experiment on anthropo-pedogenesis. In the French context, urban soil scientists soon formed new bonds with the worlds of urbanism, administration, and waste management, reframing their approach as a technical response to issues brought by sprawling cities, backgrounding soils again under a trope centered on the management of soil services. These stories allow to critically inhabit soil scientists’ claim that humans participate in pedogenesis by examining the specific conditions in which modern modes of being in the world and urban soils become entangled or disentangled in modern metropolis.

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32

Haynes, C. Vance. "Bagnold's Barchan: A 57-Yr Record of Dune Movement in the Eastern Sahara and Implications for Dune Origin and Paleoclimate Since Neolithic Times". Quaternary Research 32, n.º 2 (septiembre de 1989): 153–67. http://dx.doi.org/10.1016/0033-5894(89)90072-0.

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AbstractDiscovery in 1980 of Camp 18 of the 1930 Bagnold expedition in northwestern Sudan has resulted in an exceptionally long record of barchan movement from which an average rate of 7.5 m/yr has been calculated. Measurements of the rate of dune advance since 1980 have not varied significantly, indicating a state of quasiequilibrium exists. The dune field is moving over an undulating sand sheet exhibiting various stages of Holocene pedogenesis and containing Neolithic sites. The sand sheet overlies Pleistocene alluvium with stronger stages of pedogenesis. All of these deposits may be a significant source of dune sand. Wind-blown grass fragments trapped by advancing slipfaces mark former slipface positions and indicate late Holocene rainfall events, which can be radiocarbon dated. Parabolic forms (revealed by SPOT images) at the windward ends of the dune fields are transitional to barchans, suggesting sand accumulation in vegetation germinated during a Holocene wet period. In addition, sand streaks from sand-sheet undulations suggest that active eolian erosion of sand sheets contributes to the sand supply of dune fields. Pedogenesis during pluvial periods contributes to silt and clay fractions of bimodal sand sheet sediments. From wind streaks on LANDSAT images and an estimated average rate of dune advance, positions of dune fields during past hyperarid periods can be estimated.

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33

Jigau, Gheorghe, Leșanu Mihai, Bîrsan Ana, Blidari Anton, Borș Natalia, Plăcintă Nina y Cernolev Elena. "Trends of the Typogenetic Processes in the Carpato-Danubiano-Pontic Space. Results in Agriculture in Northeastern Area Climate Conditions". Present Environment and Sustainable Development 12, n.º 1 (1 de junio de 2018): 249–62. http://dx.doi.org/10.2478/pesd-2018-0020.

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Abstract The chernozems evolution of the Carpatho-Danubian-Pontic space clearly shows two consecutive phases: climatogenic and anthropo-climatogenic. The latter is characterized by increasing agrogenic impact on soil climate. The soil cover of Carpathian-Danubian-Pontic space is the hierarchical functional system long-time product. Pedogenetic factors → pedogenetic regimes → pedogenetic processes → soil (soil cover). During Pleistocene, the chernozem pathogenesis in the region resumed 13 times, each time starting from the carbonic chernozem phase. Zonal climatic cyclicality has led to the differentiation of chernozem subtypes, determined by the zonal differentiation of pedogenic regimes and typogenetic elemental processes. The current stage of chernozem cleavage in the region began 10-12 thousand years ago. The evolution of soils in the soil was determined by the climate cyclicality and the increase of anthropogenic imputations and involves the succession over time of several phases: - Cryogenic with poorly developed soil by A (AO) - C Order; - Early dynamic halocene with developed zonal soil formation; - Late halocene with climatic evolution of the profile; - Natural-anthropogenic. During the last one, four eras were accelerated: natural-anthropo-turbian, naturalanthropic modification, natural-anthropic restructuring and natural-anthropic stagnation. Increasing the anthropogenic impulses led to the modification of the climatic → soil relations in the sense of increasing the degree of continentalisation of the soil climate materialized in the aridization of the soil cover, the change of the sense and intensity of the typogenic processes and the induction of some nontypical elementary processes of the chernozemic pedogenesis.

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34

Lisetskii, Fedor. "Estimates of Soil Renewal Rates: Applications for Anti-Erosion Arrangement of the Agricultural Landscape". Geosciences 9, n.º 6 (20 de junio de 2019): 266. http://dx.doi.org/10.3390/geosciences9060266.

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Engineering and geographic substantiation of the anti-erosion organization of agricultural landscapes requires not only differentiated estimations of erosion losses, but also commensurate (in terms of space–time scales) estimations of the soil loss tolerance. The main approaches for determining the participation of estimations of soil formation in the substantiation of erosion tolerance have been defined. This study is aimed at justifying the methods of incorporating the results of pedogenesis modeling into computational methods for organizing agricultural landscapes. This paper presents the results of a study of the process of formation of the humus horizon and the accumulation of organic carbon in soils, based on soils from archaeological sites in the Crimean Peninsula over a period from 25 to 2000 years ago, with differences in climate and parent rock, in a region with a thousand-year history of human activity. The patterns of variation in the thickness of the humus horizons over time and the accumulation of carbon were determined, and estimates for the rate of the pedogenesis were obtained. In connection with the slowing of the rate of pedogenesis over time, the chronofunction of the change in the thickness of soils (of both exponential and logistic types) may be applied and, on this basis, it is possible to calculate the rates of the formation of the humus horizon depending on the morphological status of the soils. During re-naturation of highly degraded soils, maximum renewal rates may take place only with a very high input of organic matter, which is crucial to take into account in the development and implementation of programs for the rehabilitation of degraded lands. Under the conditions of slope agriculture, the rationale for T-values should be linked to many factors of the input and consumption of organic carbon, which provides a logical mathematical model of the formation of soil quality. For soil quality management on agricultural lands, a formula for calculating T-values, using an equation where the rate of pedogenesis is associated with a variety of changes in soil organic carbon, is proposed in this article.

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35

Xiong, Wu, Manuel Delgado-Baquerizo, Qirong Shen y Stefan Geisen. "Pedogenesis shapes predator-prey relationships within soil microbiomes". Science of The Total Environment 828 (julio de 2022): 154405. http://dx.doi.org/10.1016/j.scitotenv.2022.154405.

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36

McBurnett, S. L. y D. P. Franzmeier. "Pedogenesis and Cementation in Calcareous Till in Indiana". Soil Science Society of America Journal 61, n.º 4 (julio de 1997): 1098–104. http://dx.doi.org/10.2136/sssaj1997.03615995006100040016x.

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37

Artieda, O. y J. Herrero. "Pedogenesis in Lutitic Cr Horizons of Gypsiferous Soils". Soil Science Society of America Journal 67, n.º 5 (septiembre de 2003): 1496–506. http://dx.doi.org/10.2136/sssaj2003.1496.

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38

Zehetner, F., W. P. Miller y L. T. West. "Pedogenesis of Volcanic Ash Soils in Andean Ecuador". Soil Science Society of America Journal 67, n.º 6 (noviembre de 2003): 1797–809. http://dx.doi.org/10.2136/sssaj2003.1797.

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39

Wiederhold, Jan G., Nadya Teutsch, Stephan M. Kraemer, Alex N. Halliday y Ruben Kretzschmar. "Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils". Soil Science Society of America Journal 71, n.º 6 (noviembre de 2007): 1840–50. http://dx.doi.org/10.2136/sssaj2006.0379.

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40

Zubillaga, Marta S. y Lidia Giuffré de López Camelo. "Phosphorus fractions in argentine soils of different pedogenesis". Communications in Soil Science and Plant Analysis 27, n.º 9-10 (mayo de 1996): 2137–45. http://dx.doi.org/10.1080/00103629609369693.

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41

Stockmann, U., B. Minasny, T. J. Pietsch y A. B. McBratney. "Quantifying processes of pedogenesis using optically stimulated luminescence". European Journal of Soil Science 64, n.º 1 (28 de enero de 2013): 145–60. http://dx.doi.org/10.1111/ejss.12012.

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42

TOMAR, K. P. "Chemistry of pedogenesis in Indo-Gangetic alluvial plains". Journal of Soil Science 38, n.º 3 (septiembre de 1987): 405–14. http://dx.doi.org/10.1111/j.1365-2389.1987.tb02275.x.

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43

Daniels, J. Michael. "Floodplain aggradation and pedogenesis in a semiarid environment". Geomorphology 56, n.º 3-4 (diciembre de 2003): 225–42. http://dx.doi.org/10.1016/s0169-555x(03)00153-3.

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44

Vaniman, David T., Steve J. Chipera y David L. Bish. "Pedogenesis of siliceous calcretes at Yucca Mountain, Nevada". Geoderma 63, n.º 1 (septiembre de 1994): 1–17. http://dx.doi.org/10.1016/0016-7061(94)90106-6.

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45

Harshavardhana, B. G. y R. Shankar. "Topographical influence on pedogenesis – Insights from Rock Magnetism". CATENA 198 (marzo de 2021): 105013. http://dx.doi.org/10.1016/j.catena.2020.105013.

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46

He, Xiubin, Yuhai Bao, Hongwei Nan, Donghong Xiong, Li Wang, Yanfeng Liu y Jingbo Zhao. "Tillage pedogenesis of purple soils in southwestern China". Journal of Mountain Science 6, n.º 2 (10 de mayo de 2009): 205–10. http://dx.doi.org/10.1007/s11629-009-1038-y.

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47

Pettry, D. E. "Pedogenesis and Soil Taxonomy, I. Concepts and Interactions". Geoderma 35, n.º 4 (septiembre de 1985): 355. http://dx.doi.org/10.1016/0016-7061(85)90018-7.

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48

Pettry, D. E. "Pedogenesis and Soil Taxonomy, II. The Soil Orders". Geoderma 35, n.º 4 (septiembre de 1985): 356. http://dx.doi.org/10.1016/0016-7061(85)90019-9.

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49

Hoosbeek, Marcel R. y Ray B. Bryant. "Towards the quantitative modeling of pedogenesis — a review". Geoderma 55, n.º 3-4 (noviembre de 1992): 183–210. http://dx.doi.org/10.1016/0016-7061(92)90083-j.

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50

Chenot, Julie, Renaud Jaunatre, Elise Buisson, Fabrice Bureau y Thierry Dutoit. "Impact of quarry exploitation and disuse on pedogenesis". CATENA 160 (enero de 2018): 354–65. http://dx.doi.org/10.1016/j.catena.2017.09.012.

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