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Journal articles on the topic 'Pedogenesis'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Medeiros, Edgardo Ramos, Fabrício De Araújo Pedron, and Anderson Augusto Volpato Sccoti. "EVIDÊNCIAS DE PEDOGÊNESE ALÓCTONE SOBRE ARENITOS BOTUCATU NO SUDOESTE GAÚCHO." Ciência e Natura 35, no. 1 (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

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2

UGOLINI, F. C., M. G. STONER, and D. J. MARRETT. "ARCTIC PEDOGENESIS." Soil Science 144, no. 2 (1987): 90–100. http://dx.doi.org/10.1097/00010694-198708000-00002.

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3

STONER, M. G., and F. C. UGOLINI. "ARCTIC PEDOGENESIS." Soil Science 145, no. 1 (1988): 46–51. http://dx.doi.org/10.1097/00010694-198801000-00006.

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4

Ryzhov, Yu V., V. A. Golubtsov, and M. V. Smirnov. "LATE GLACIAL AND HOLOCENE EROSIONAL DISSECTION AND FILL IN THE TEMPORAL (EPHEMERAL) STREAM VALLEY ON THE RIGHT BANK OF THE SELENGA RIVER." Geodynamics & Tectonophysics 15, no. 6 (2024): 0801. https://doi.org/10.5800/gt-2024-15-6-0801.

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The structure, composition and cut and fill sequence of the Late Glacial and Holocene erosional landforms in the Kuitunka River basin on the right bank of the Selenga River were studied based on a detailed analysis and radiocarbon dating of the soil-sedimentary sequence in the Studenyi Klyuch 2 and Kovalev Pad’ sections. A correlation was carried out between seven sections in the intermittent stream valleys in the Kuitunka River basin. There are three episodes of the Late Glacial and Holocene cutting dated back to ~18–17, ~14.7–14.3, and 0.25–0 cal. kyr BP (ka BP). There are distinguished the

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5

Rodriguez, Victoria, Lisa-Marie Moskwa, Rómulo Oses, et al. "Impact of Climate and Slope Aspects on the Composition of Soil Bacterial Communities Involved in Pedogenetic Processes along the Chilean Coastal Cordillera." Microorganisms 10, no. 5 (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 Planc

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6

Cunha, Luis, George G. Brown, David W. G. Stanton, et al. "Soil Animals and Pedogenesis." Soil Science 181, no. 3/4 (2016): 110–25. http://dx.doi.org/10.1097/ss.0000000000000144.

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7

Phillips, Jonathan D. "Soil Complexity and Pedogenesis." Soil Science 182, no. 4 (2017): 117–27. http://dx.doi.org/10.1097/ss.0000000000000204.

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8

JOHNSON, D. L., and D. WATSON-STEGNER. "EVOLUTION MODEL OF PEDOGENESIS." Soil Science 143, no. 5 (1987): 349–66. http://dx.doi.org/10.1097/00010694-198705000-00005.

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9

Chesworth, Ward. "Pedogenesis and soil taxonomy." Geochimica et Cosmochimica Acta 49, no. 1 (1985): 309. http://dx.doi.org/10.1016/0016-7037(85)90214-5.

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10

Leguédois, Sophie, Geoffroy Séré, Apolline Auclerc, et al. "Modelling pedogenesis of Technosols." Geoderma 262 (January 2016): 199–212. http://dx.doi.org/10.1016/j.geoderma.2015.08.008.

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11

Jigău, Gheorghe, Liviu Apostol, Ana Barsan, and Elena Tofan. "Elements of Climate Evolution in yhe Area Between Prut and Dniester Rivers. Landscape and Pedogenetic Implications." Present Environment and Sustainable Development 9, no. 1 (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 th

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12

Brevik, Eric C., and Andreas G. Lazari. "Rates of Pedogenesis in Reclaimed Lands as Compared to Rates of Natural Pedogenesis." Soil Horizons 55, no. 1 (2014): 0. http://dx.doi.org/10.2136/sh13-06-0017.

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13

Delgado-Baquerizo, Manuel, Richard D. Bardgett, Peter M. Vitousek, et al. "Changes in belowground biodiversity during ecosystem development." Proceedings of the National Academy of Sciences 116, no. 14 (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 stoi

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14

Phillips, Jonathan D. "Progressive and Regressive Pedogenesis and Complex Soil Evolution." Quaternary Research 40, no. 2 (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 Carol

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15

PROTZ, R., M. J. SHIPITALO, G. J. ROSS, and J. TERASMAE. "PODZOLIC SOIL DEVELOPMENT IN THE SOUTHERN JAMES BAY LOWLANDS, ONTARIO." Canadian Journal of Soil Science 68, no. 2 (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 p

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16

Devnita, Rina. "Mineralogical Characteristics and The Pedogenetic Processes of Soils on Coral Reefs in Ambon." Indonesian Journal on Geoscience 4, no. 1 (2009): 19–29. http://dx.doi.org/10.17014/ijog.4.1.19-29.

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http://dx.doi.org/10.17014/ijog.vol4no1.20093The mineralogical characteristics of soils developed on coral reef parent materials in Hitu and Wailiha, Ambon, were investigated regarding to the relationship to pedogenesis. The analyses concerned with the characteristics of soil chemical, physical, and mineralogy of the rock fragment and sand, silt and clay fractions are to investigate the pedogenesis processes. Both soil profiles indicate the clayey texture, slightly neutral reaction, high cation exchange capacity, base saturation, and iron oxide. The mineralogical analyses of rock fragments and

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17

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, no. 1 (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. W

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18

RUTHERFORD, G. K., and D. J. THACKER. "CHARACTERISTICS OF TWO MAFIC SAPROLITES AND THEIR ASSOCIATED SOIL PROFILES IN CANADA." Canadian Journal of Soil Science 68, no. 2 (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, P

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19

Aji, Krishna, Lely Adriani Nasution, Rohana Sufia, Sarif Robo, and Tri Mulya Hartati. "Karakteristik Geomorfologi Tanah pada Formasi Geologi Kuarter Gunung Api Holocen di Wilayah Kepulauan Maluku Utara." Jurnal Ecosolum 13, no. 2 (2024): 130–43. https://doi.org/10.20956/ecosolum.v13i2.39868.

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Variability of soil types in the Quaternary geological formations on the islands presents different soil morphological characteristics. The process of geomorphogenesis and geology determines the characteristics of soil morphology. This study aims to determine the characteristics of soil morphology, pedogenesis process, soil development based on landforms in Quaternary geological formations in North Maluku Islands region. Six soil profiles were observed, which were determined based on geographical location. Descriptive research methods based on USDA standards were used as the basis for determin

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20

., E. U. Onweremadu. "Pedogenesis of Soils of a Colliery." Research Journal of Environmental Toxicology 1, no. 4 (2007): 184–90. http://dx.doi.org/10.3923/rjet.2007.184.190.

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21

Bonifacio, Eleonora, and Elisabetta Barberis. "PHOSPHORUS DYNAMICS DURING PEDOGENESIS ON SERPENTINITE." Soil Science 164, no. 12 (1999): 960–68. http://dx.doi.org/10.1097/00010694-199912000-00009.

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22

Pozdnyakov, A. I. "Electrical parameters of soils and pedogenesis." Eurasian Soil Science 41, no. 10 (2008): 1050–58. http://dx.doi.org/10.1134/s1064229308100062.

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23

Laliberté, Etienne, James B. Grace, Michael A. Huston, et al. "How does pedogenesis drive plant diversity?" Trends in Ecology & Evolution 28, no. 6 (2013): 331–40. http://dx.doi.org/10.1016/j.tree.2013.02.008.

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24

Turner, Benjamin L., Leo M. Condron, Sarah J. Richardson, Duane A. Peltzer, and Victoria J. Allison. "Soil Organic Phosphorus Transformations During Pedogenesis." Ecosystems 10, no. 7 (2007): 1166–81. http://dx.doi.org/10.1007/s10021-007-9086-z.

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25

Kleber, Markus, Christian Mikutta, and Reinhold Jahn. "Andosols in Germany—pedogenesis and properties." CATENA 56, no. 1-3 (2004): 67–83. http://dx.doi.org/10.1016/j.catena.2003.10.015.

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26

Minasny, Budiman, Alex B. McBratney, and Sébastien Salvador-Blanes. "Quantitative models for pedogenesis — A review." Geoderma 144, no. 1-2 (2008): 140–57. http://dx.doi.org/10.1016/j.geoderma.2007.12.013.

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27

Prietzel, Jörg, Jaane Krüger, Klaus Kaiser, et al. "Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material." Biogeochemistry 158, no. 1 (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

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28

Zerboni, Andrea, Guido S. Mariani, Lanfredo Castelletti, et al. "Was the Little Ice Age the coolest Holocene climatic period in the Italian central Alps?" Progress in Physical Geography: Earth and Environment 44, no. 4 (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 de

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29

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, no. 2 (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 signi

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30

Jigau, Gheorghe, Boris Turchin, Sergiu Dobrojan, et al. "Agrogenesis: manifestations in the physical state of the arable chernozems in the area between Prut and Dniester." Studia Universitatis Moldaviae. Seria Științe ale Naturii, no. 6(166) (April 2024): 70–77. http://dx.doi.org/10.59295/sum6(166)2023_9.

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Increasing the pressure of techno-anthropogenic factors on arable chernozems, in conditions of intensification of the degree of continentality of the soil climate induced by climate change, against the background of unidirectional reduction of the role of the biological factor in the anthropo-natural chernozem pedogenesis, involved a newphase in its evolution in which the decisive role belongs to physical degradation. It is distinguished by significant changes in typogenetic chernozeomic processes: a) formation and accumulation of humus; b) aggregation-structuring of the soil mass. Within the

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31

Meulemans, Germain. "Urban Pedogeneses." Environmental Humanities 12, no. 1 (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

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32

Demas, George P., and Martin C. Rabenhorst. "Subaqueous Soils Pedogenesis in a Submersed Environment." Soil Science Society of America Journal 63, no. 5 (1999): 1250–57. http://dx.doi.org/10.2136/sssaj1999.6351250x.

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33

Scalenghe, Riccardo, Eleonora Bonifacio, Luisella Celi, Fiorenzo C. Ugolini, and Ermanno Zanini. "Pedogenesis in disturbed alpine soils (NW Italy)." Geoderma 109, no. 3-4 (2002): 207–24. http://dx.doi.org/10.1016/s0016-7061(02)00176-3.

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34

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

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35

Bouzouidja, Ryad, Gustave Rousseau, Violaine Galzin, Rémy Claverie, David Lacroix, and Geoffroy Séré. "Green roof ageing or Isolatic Technosol’s pedogenesis?" Journal of Soils and Sediments 18, no. 2 (2016): 418–25. http://dx.doi.org/10.1007/s11368-016-1513-3.

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36

Haslinger, E., F. Ottner, and U. S. Lundström. "Pedogenesis in the Alnö carbonatite complex, Sweden." Geoderma 142, no. 1-2 (2007): 127–35. http://dx.doi.org/10.1016/j.geoderma.2007.08.014.

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37

Jigau, Gheorghe, Leșanu Mihai, Bîrsan Ana, et al. "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, no. 1 (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 diff

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38

Lisetskii, Fedor. "Estimates of Soil Renewal Rates: Applications for Anti-Erosion Arrangement of the Agricultural Landscape." Geosciences 9, no. 6 (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 r

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39

Nepop, R. K., A. R. Agatova, M. A. Bronnikova, E. P. Zazovskaya, I. YU Ovchinnikov, and P. Moska. "Radiocarbon dating of organic-rich deposits: Difficulties of paleogeographical interpretations in highlands of Russian Altai." Geochronometria 47, no. 1 (2020): 138–53. http://dx.doi.org/10.2478/geochr-2020-0018.

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Abstract The high mountainous southeastern part of Russian Altai is characterized by complicated sedimentation history. As a result of tectonic movements, Paleogene, Neogene, and even more old Carboniferous and Jurassic organicrich deposits had been partly uplifted and exhumed on the ridge’s slopes, where during the Pleistocene, they were affected by various exogenous processes including glaciation, glacio-fluvial erosion, winnowing activity of ice-dammed lakes, sliding during lake-draining events, followed by further intensive Holocene erosion, pedogenesis, and permafrost formation/degradatio

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40

Golubtsov, V. A., A. A. Cherkashina, and V. A. Snytko. "First data on the age and formation conditions of secondary carbonate accumulations in upper pleistocene and holocene soils of Upper Angara region." Доклады Академии наук 486, no. 6 (2019): 727–32. http://dx.doi.org/10.31857/s0869-56524866727-732.

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The first data on the age of secondary carbonate pendants in the soils of the Upper Angara region are given. Based on the study of the conditions of occurrence, morphology, material and isotopic composition, three groups of carbonate kutans were identified. The direct 14C AMS dating of the coating’s microlayers allowed to determineintervals of their formation. Pendants of the first group were formed in the middle Holocene (3.6-3.3 kyr BP). The formation of coatings of the second and third groups took place in the second half of MIS-3 (24.1-23.3 and ~34-35 kyr BP, respectively). The paleoecolog

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41

Grison, Hana, Eduard Petrovsky, Ales Kapicka, and Hana Hanzlikova. "Detection of the pedogenic magnetic fraction in volcanic soils developed on basalts using frequency-dependent magnetic susceptibility: comparison of two instruments." Geophysical Journal International 209, no. 2 (2017): 654–60. http://dx.doi.org/10.1093/gji/ggx037.

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Abstract In studies of the magnetic properties of soils, the frequency-dependent magnetic susceptibility percentage (χFD%) is often used for the identification of ultrafine magnetically superparamagnetic/stable single-domain (SP/SSD) particles. This parameter is commonly used as an indicator for increased pedogenesis. In strongly magnetic soils, the SP/SSD magnetic signal (mostly bio-pedogenic) may be masked by lithological signals; making pedogenesis hard to detect. In this study, we compare results for the detection of ultrafine SP/SSD magnetic particles in andic soils using two instruments:

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42

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

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43

McBurnett, S. L., and D. P. Franzmeier. "Pedogenesis and Cementation in Calcareous Till in Indiana." Soil Science Society of America Journal 61, no. 4 (1997): 1098–104. http://dx.doi.org/10.2136/sssaj1997.03615995006100040016x.

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44

Artieda, O., and J. Herrero. "Pedogenesis in Lutitic Cr Horizons of Gypsiferous Soils." Soil Science Society of America Journal 67, no. 5 (2003): 1496–506. http://dx.doi.org/10.2136/sssaj2003.1496.

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45

Zehetner, F., W. P. Miller, and L. T. West. "Pedogenesis of Volcanic Ash Soils in Andean Ecuador." Soil Science Society of America Journal 67, no. 6 (2003): 1797–809. http://dx.doi.org/10.2136/sssaj2003.1797.

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46

Wiederhold, Jan G., Nadya Teutsch, Stephan M. Kraemer, Alex N. Halliday, and Ruben Kretzschmar. "Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils." Soil Science Society of America Journal 71, no. 6 (2007): 1840–50. http://dx.doi.org/10.2136/sssaj2006.0379.

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47

Zubillaga, Marta S., and Lidia Giuffré de López Camelo. "Phosphorus fractions in argentine soils of different pedogenesis." Communications in Soil Science and Plant Analysis 27, no. 9-10 (1996): 2137–45. http://dx.doi.org/10.1080/00103629609369693.

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48

Stockmann, U., B. Minasny, T. J. Pietsch, and A. B. McBratney. "Quantifying processes of pedogenesis using optically stimulated luminescence." European Journal of Soil Science 64, no. 1 (2013): 145–60. http://dx.doi.org/10.1111/ejss.12012.

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49

TOMAR, K. P. "Chemistry of pedogenesis in Indo-Gangetic alluvial plains." Journal of Soil Science 38, no. 3 (1987): 405–14. http://dx.doi.org/10.1111/j.1365-2389.1987.tb02275.x.

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50

Daniels, J. Michael. "Floodplain aggradation and pedogenesis in a semiarid environment." Geomorphology 56, no. 3-4 (2003): 225–42. http://dx.doi.org/10.1016/s0169-555x(03)00153-3.

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