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Artículos de revistas sobre el tema "Soil taxonomy"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 26 de julio de 2025

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1

Witty, John E., and Richard W. Arnold. "Soil Taxonomy: An Overview." Outlook on Agriculture 16, no. 1 (1987): 8–13. http://dx.doi.org/10.1177/003072708701600102.

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The growth of crops depends on many factors, not least the nature of the soil. It is, therefore, important to be able to describe soils in unequivocal terms, much as living organisms are precisely defined according to the binomial taxonomic system originated by Linnaeus. The very complex and varied nature of soils makes this a difficult problem but since the 1950s it has been vigorously tackled by the US Soil Taxonomy programme. The hierarchical system developed is reviewed here.

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2

Urka, Martin C. "Soil Taxonomy—Soil Trivia." Soil Horizons 33, no. 4 (1992): 108. http://dx.doi.org/10.2136/sh1992.4.0108.

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3

Fenton, Thomas E. "The impact of erosion on the classification of Mollisols in Iowa." Canadian Journal of Soil Science 92, no. 3 (2012): 413–18. http://dx.doi.org/10.4141/cjss2010-042.

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Fenton, T. E. 2012. The impact of erosion on the classification of Mollisols in Iowa. Can. J. Soil Sci. 92: 413–418. The fertile black soils in the Great Plains and Western States of the United States are dark brown Chernozems in the Canadian system of soil taxonomy and Mollisols, when a mollic epipedon is present, according to the United States soil taxonomy. Other primary criteria are organic carbon content, color, structure, and thickness of the mollic epipedon. Accelerated erosion can affect all of these properties and is especially critical for soils that have slope gradients of more than

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4

Finstad, Kari, Marco Pfeiffer, and Ronald Amundson. "Hyperarid Soils and the Soil Taxonomy." Soil Science Society of America Journal 78, no. 6 (2014): 1845–51. http://dx.doi.org/10.2136/sssaj2014.06.0247.

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5

Urka, Martin C. "Soil Trivia and Soil Taxonomy." Soil Horizons 32, no. 1 (1991): 28. http://dx.doi.org/10.2136/sh1991.1.0028.

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6

Urka, Martin C. "Soil Trivia and Soil Taxonomy." Soil Horizons 32, no. 1 (1991): 29. http://dx.doi.org/10.2136/sh1991.1.0029.

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7

Urka, Martin C. "Soil Trivia and Soil Taxonomy." Soil Horizons 32, no. 4 (1991): 122. http://dx.doi.org/10.2136/sh1991.4.0122.

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8

Urka, Martin C. "Soil Trivia and Soil Taxonomy." Soil Horizons 33, no. 1 (1992): 16. http://dx.doi.org/10.2136/sh1992.1.0016.

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9

Buol, S. W., John Witty, Bob Ahrens, and Bob Engel. "Soil Taxonomy Trivia." Soil Horizons 34, no. 1 (1993): 35. http://dx.doi.org/10.2136/sh1993.1.0035.

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10

Waymouth, Vicky, Rebecca E. Miller, Sabine Kasel, Fiona Ede, Andrew Bissett, and Cristina Aponte. "Soil Bacterial Community Responds to Land-Use Change in Riparian Ecosystems." Forests 12, no. 2 (2021): 157. http://dx.doi.org/10.3390/f12020157.

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Riparian forests were frequently cleared and converted to agricultural pastures, but in recent times these pastures are often revegetated in an effort to return riparian forest structure and function. We tested if there is a change in the soil bacterial taxonomy and function in areas of riparian forest cleared for agricultural pasture then revegetated, and if soil bacterial taxonomy and function is related to vegetation and soil physicochemical properties. The study was conducted in six riparian areas in south-eastern Australia, each comprising of three land-use types: remnant riparian forest,

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11

Veenstra, Jessica J., and C. Lee Burras. "Effects of agriculture on the classification of Black soils in the Midwestern United States." Canadian Journal of Soil Science 92, no. 3 (2012): 403–11. http://dx.doi.org/10.4141/cjss2010-018.

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Veenstra, J. J. and Burras, C. L. 2012. Effects of agriculture on the classification of Black soils in the Midwestern United States. Can. J. Soil Sci. 92: 403–411. Soil surveys are generally treated as static documents. Many soil survey users assume that pedon data generated 30 to 50 yr ago still represents today's soil, as short-term changes in soil properties are perceived to be limited to the soil surface and thus pedologically insignificant. In this study, we re-sampled and re-analyzed 82 pedons with historical descriptions and laboratory data in Iowa, United States, to evaluate changes in

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12

Baillie, I. C. "Soil Survey Staff 1999, Soil Taxonomy." Soil Use and Management 17, no. 1 (2006): 57–60. http://dx.doi.org/10.1111/j.1475-2743.2001.tb00008.x.

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13

Bockheim, J. G., A. N. Gennadiyev, A. E. Hartemink, and E. C. Brevik. "Soil-forming factors and Soil Taxonomy." Geoderma 226-227 (August 2014): 231–37. http://dx.doi.org/10.1016/j.geoderma.2014.02.016.

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14

Ivanyuk, Halyna. "Analysis of “Systematics of Polish Soils”." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 122–32. http://dx.doi.org/10.30970/vgg.2013.44.1210.

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The “Systematics of Polish Soils” (SgP, 2011) is very close to WRB and “Soil Taxonomy”. The morphological characteristics of the soils, investigated in the field, rather than soil genesis are diagnostic criteria. The main provisions of the new “Systematics”, properties of soils of higher taxonomic levels have been reviewed. Some diagnostic horizons, which were not borrowed from other classifications, have been described. We tried to find equivalents in the Ukrainian classification for some soils names. The correlation of Poland soils and WRB has been analyzed. Key words: Systematics of Polish

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15

Grossman, Bob. "Change in Soil Taxonomy." Soil Horizons 49, no. 1 (2008): 28. http://dx.doi.org/10.2136/sh2008.1.0028.

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16

Florea, Nicolae. "Soil Taxonomy in Romania." Soil Horizons 53, no. 3 (2012): 24. http://dx.doi.org/10.2136/sh12-01-0006.

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17

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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18

Rougerie, Rodolphe, Thibaud Decaëns, Louis Deharveng, et al. "DNA barcodes for soil animal taxonomy." Pesquisa Agropecuária Brasileira 44, no. 8 (2009): 789–802. http://dx.doi.org/10.1590/s0100-204x2009000800002.

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The biodiversity of soil communities remains very poorly known and understood. Soil biological sciences are strongly affected by the taxonomic crisis, and most groups of animals in that biota suffer from a strong taxonomic impediment. The objective of this work was to investigate how DNA barcoding - a novel method using a microgenomic tag for species identification and discrimination - permits better evaluation of the taxonomy of soil biota. A total of 1,152 barcode sequences were analyzed for two major groups of animals, collembolans and earthworms, which presented broad taxonomic and geograp

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19

Mckenzie, NJ, and MP Austin. "Utility of the factual key and soil taxonomy in the Lower Macquarie Valley, NSW." Soil Research 27, no. 2 (1989): 289. http://dx.doi.org/10.1071/sr9890289.

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The utility of the Factual Key and Soil Taxonomy was tested by using comprehensive soil survey data from the lower Macquarie Valley, N.S.W. The aim was to assess whether the two classification schemes partitioned soil variation efficiently and to establish their usefulness for predicting variables not used during profile allocation. A numerical taxonomic method was used to generate a local classification which served as a benchmark to assess the two national systems. The effectiveness of the three classifications was determined by comparing the proportion of variation accounted for in a range

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20

Pettry, D. E. "Pedogenesis and Soil Taxonomy, II. The Soil Orders." Geoderma 35, no. 4 (1985): 356. http://dx.doi.org/10.1016/0016-7061(85)90019-9.

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21

Stolt, Mark H., and Brian A. Needelman. "Fundamental Changes in Soil Taxonomy." Soil Science Society of America Journal 79, no. 4 (2015): 1001–7. http://dx.doi.org/10.2136/sssaj2015.02.0088.

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22

Arnold, P. W. "Soil taxonomy, achievements and challenges." Geoderma 37, no. 3 (1986): 255. http://dx.doi.org/10.1016/0016-7061(86)90052-2.

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23

YLI-HALLA, M., and D. MOKMA. "Soil temperature regimes in Finland." Agricultural and Food Science 7, no. 4 (1998): 507–12. http://dx.doi.org/10.23986/afsci.5606.

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Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly in temperate areas. To facilitate correct classification of soils of Finland, the temperature regimes in soils of the country were determined. The mean annual soil temperature, measured at 50 cm below soil surface, ranged from 6.4°C at the warmest site (Anjala) to 1.9°C at the coldest one (Utsjoki, Kevo), and the mean summer soil temperature from 13.7°C to 6.2°C at the same stations, all being in the range of the cryic temperature regime. The mean annual soil temperature was 2 to 5°C higher than

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24

Yli-Halla, Markku, and Delbert L. Mokma. "Classification of Soils of Finland According to Soil Taxonomy." Soil Horizons 40, no. 2 (1999): 59. http://dx.doi.org/10.2136/sh1999.2.0059.

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25

Song, Kwan-Cheol, Byung-Keun Hyun, and Ho-Jun Kang. "Reclassification of Korean Soils According to Revised Soil Taxonomy." Korean Journal of Soil Science and Fertilizer 52, no. 2 (2019): 93–104. http://dx.doi.org/10.7745/kjssf.2019.52.2.093.

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26

Abakumov, Evgeny, Aleksei Zverev, Evgeny Andronov, and Timur Nizamutdinov. "Microbial Composition of Natural, Agricultural, and Technogenic Soils of Both Forest and Forest-Tundra of the Russian North." Applied Sciences 13, no. 15 (2023): 8981. http://dx.doi.org/10.3390/app13158981.

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Technogenic processes and agrodevelopment of the soil cover lead to significant transformations of soil chemical and biological properties. New methods of soil microbiology, including next-generation sequencing, allows us to investigate soil microbial composition in detail, including the taxonomy and ecological functions of soil bacteria. This study presents data on the taxonomic diversity of mature and anthropogenically disturbed soils in various ecosystems of Russia. Natural soils in the southern taiga (Leningrad region and Novgorod region), northern taiga (Komi republic), forest-tundra, and

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27

Sun, Wanlong, Zhouyuan Li, Jiesi Lei, and Xuehua Liu. "Bacterial Communities of Forest Soils along Different Elevations: Diversity, Structure, and Functional Composition with Potential Impacts on CO2 Emission." Microorganisms 10, no. 4 (2022): 766. http://dx.doi.org/10.3390/microorganisms10040766.

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Soil bacteria are important components of forest ecosystems, there compostion structure and functions are sensitive to environmental conditions along elevation gradients. Using 16S rRNA gene amplicon sequencing followed by FAPROTAX function prediction, we examined the diversity, composition, and functional potentials of soil bacterial communities at three sites at elevations of 1400 m, 1600 m, and 2200 m in a temperate forest. We showed that microbial taxonomic composition did not change with elevation (p = 0.311), though soil bacterial α-diversities did. Proteobacteria, Acidobacteria, Actinob

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28

Aisyah, Veti Nur, Mohammad Nurcholis, and Djoko Mulyanto. "MORFOLOGI DAN KLASIFIKASI TANAH PADA FORMASI PENIRON BAHAN INDUK ANDESIT PIROKSEN DI DESA PAGEDONGAN, BANJARNEGARA." Jurnal Tanah dan Sumberdaya Lahan 10, no. 1 (2023): 125–33. http://dx.doi.org/10.21776/ub.jtsl.2023.010.1.14.

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Rock formation as parent material in Pagedongan Village, Banjarnegara influences the properties of the soil formed. The purpose of this research was to identify the morphology and soil classification according to USDA Taxonomy, National Soil Classifications, and World Reference Base for Soils. This study uses a survey method by determining observation points based on a rock formation, namely Peniron Formation, with pyroxene andesite as parent material for observing soil morphology, physical and chemical of soil in the field, then laboratory analysis included soil texture, bulk density, organic

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29

Hao, Shiheng, Kening Wu, Ling Li, et al. "Revised Proposed Classifications for Typical Anthropogenic Soils in China." Land 12, no. 11 (2023): 1974. http://dx.doi.org/10.3390/land12111974.

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As global industrialization and its associated anthropogenic activities rapidly increase, so too does the areal extent of human-altered soils. The soil classification framework must incorporate the classification schemes of these disturbed soils in order to remediate land. Soil Taxonomy (ST) and the World Reference Base for Soil Resources (WRB) are the most widely used soil classification systems in the world. In this study, 15 typical anthropogenic soil profiles with engineering and technical characteristics from China were selected for a classification study. The aim of this study was to cla

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30

Phillips, Jonathan D., and Daniel A. Marion. "Soil geomorphic classification, soil taxonomy, and effects on soil richness assessments." Geoderma 141, no. 1-2 (2007): 89–97. http://dx.doi.org/10.1016/j.geoderma.2007.05.011.

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31

Hewitt, AE. "Soil classification in New Zealand - Legacy and lessons." Soil Research 30, no. 6 (1992): 843. http://dx.doi.org/10.1071/sr9920843.

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A brief review of the history of soil classification in New Zealand is made in order to place the most recent work in its historical context. The first comprehensive system was inspired by the Russian concepts of zonality, and was published as the New Zealand Genetic Soil Classification by Taylor in 1948. It may be regarded as a grand soil-landscape model that related soil classes to environmental factors. Although successful in stimulating the reconnaissance survey of New Zealand soils, it failed to support the requirements of more intensive land use. Soil Taxonomy was tested as an alternativ

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32

Mokma, D. L., and M. Yli-Halla. "Keys to Soil Taxonomy for Finland." Soil Horizons 44, no. 3 (2003): 101. http://dx.doi.org/10.2136/sh2003.3.0101.

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33

Galbraith, John M., Ray B. Bryant, and Robert J. Ahrens. "AN EXPERT SYSTEM FOR SOIL TAXONOMY." Soil Science 163, no. 9 (1998): 748–58. http://dx.doi.org/10.1097/00010694-199809000-00008.

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34

Huang, J., M. C. Ebach, and J. Triantafilis. "Cladistic analysis of Chinese Soil Taxonomy." Geoderma Regional 10 (September 2017): 11–20. http://dx.doi.org/10.1016/j.geodrs.2017.03.001.

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35

Chen, Huaihai, Kayan Ma, Yu Huang, et al. "Lower functional redundancy in “narrow” than “broad” functions in global soil metagenomics." SOIL 8, no. 1 (2022): 297–308. http://dx.doi.org/10.5194/soil-8-297-2022.

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Abstract. Understanding the relationship between soil microbial taxonomic compositions and functional profiles is essential for predicting ecosystem functions under various environmental disturbances. However, even though microbial communities are sensitive to disturbance, ecosystem functions remain relatively stable, as soil microbes are likely to be functionally redundant. Microbial functional redundancy may be more associated with “broad” functions carried out by a wide range of microbes than with “narrow” functions in which specific microorganisms specialize. Thus, a comprehensive study to

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36

Embrechts, Jef, and René Tavernier. "Soil temperature regimes in Cameroon as defined in soil taxonomy." Geoderma 37, no. 2 (1986): 149–55. http://dx.doi.org/10.1016/0016-7061(86)90027-3.

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37

Duniway, Michael C., Mark E. Miller, Joel Brown, and Gordon Toevs. "An alternative to soil taxonomy for describing key soil characteristics." Frontiers in Ecology and the Environment 11, no. 10 (2013): 527–28. http://dx.doi.org/10.1890/13.wb.020.

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38

YLI-HALLA, M., and D. L. MOKMA. "Soils in an agricultural landscape of Jokioinen, south-western Finland." Agricultural and Food Science 10, no. 1 (2001): 33–43. http://dx.doi.org/10.23986/afsci.5677.

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Eleven pedons in an agricultural landscape at elevations 80-130 m above sea level in Jokioinen, south-western Finland were investigated and classified according to Soil Taxonomy, the FAO-Unesco system (FAO), and the World Reference Base for Soil Resources system (WRB). The soils were related to geomorphology of the landscape which is characterized by clayey fields and forested bedrock high areas covered with glacial till. A Spodosol/Podzol was found in a coarse-sandy soil in an esker while the sandy loam in a bedrock high area soils did not have an E horizon. A man-made mollic epipedon was fou

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39

Salehi, Mohammad Hassan. "Challenges of Soil Taxonomy and WRB in classifying soils: some examples from Iranian soils." Bulletin of Geography. Physical Geography Series 14, no. 1 (2018): 63–70. http://dx.doi.org/10.2478/bgeo-2018-0005.

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AbstractThe two most widely used soil classifications are the Soil Taxonomy (ST) and the World Reference Base for Soil Resources (WRB). The purpose of this paper is to clarify the differences and the similarities between ST and WRB in their current state, with some examples for representative soils in arid and semi-arid regions of Iran. Four representative pedons were classified and soil units from WRB were compared to those obtained by using ST at the family level. WRB could show the status of soils polluted by heavy metals through the Toxic qualifier and its subqualifiers. On the other hand,

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40

Wang, Xin Jing, Zhen Qi Hu, Yan Ling Zhao, Yu Ming Guo, and Pei Jun Wang. "Analysis and Mechanism of Impact of GPR Detection Effect Result from Soil Water Content." Applied Mechanics and Materials 226-228 (November 2012): 2098–102. http://dx.doi.org/10.4028/www.scientific.net/amm.226-228.2098.

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Using the ground-penetrating radar (GPR) system with the different frequencies and neutron probe, combing with radar image interpretation and the amplitude spectrum, the impact of GPR detection effects on the soil taxonomy and underground pipe were analyzed. The results indicate that when the soil content is 17.02%, the effect on soil taxonomy of 750MHZ antenna is better than 400MHZ, but the effect on underground pipe is same. As soil water content increases to 25.333%, the soil taxonomy of two antennas’ detection tends to same, and “fake stratifications” existed. The soil water content accele

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41

Zhan, Yang. "Research on Retrieval System for Soil Taxonomy." Applied Mechanics and Materials 519-520 (February 2014): 1525–28. http://dx.doi.org/10.4028/www.scientific.net/amm.519-520.1525.

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Automatic classification retrieval for soil types has become a hot spot in the study of soil science and related fields in recent years. But almost all the studies ignored that the retrieval rules need to made revision continuously. When the retrieval rules have changed, we had to rewrite the reasoning code. It hinders the popularization and application of automatic soil classification retrieval system. This paper attempts to utilize the rule engine technique to solve the problem mentioned above. According to "Keys to Chinese Soil Taxonomy", the rule based on the form of RuleML was established

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42

Collins, J. F., and T. Reeves. "Soil-geological and Soil-geomorphological relationships in Avondale Forest Park, Co. Wicklow." Irish Geography 13, no. 1 (2016): 54–64. http://dx.doi.org/10.55650/igj.1980.794.

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The relationships between parent materials, geomorphic features and soil types in Avondale Forest Park are reported and discussed. The occurrence of contrasting rocks (acid tuffs, diorite, dolerite and shales) and a variety of glacial and fluvial materials are largely responsible for the heterogeneity of the soils. Soil Orders/Great Groups include Podzols, Brown Podzolics, Brown Earths, Gleys, Lithosols, Regosols and Rankers. The soils are also placed in the Subgroups of the new U.S. Soil Taxonomy. The influence of glacial, periglacial and post-glacial conditions on the soil distribution patte

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43

MOKMA, D. L., M. YLI-HALLA, and H. HARTIKAINEN. "Soils in a young landscape on the coast of southern Finland." Agricultural and Food Science 9, no. 4 (2000): 291–302. http://dx.doi.org/10.23986/afsci.5670.

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Soils in an agricultural landscape on the southern coast of Finland (60° 13'N 25° 02'E) were characterized and classified according to Soil Taxonomy, the FAO-Unesco system (FAO), and the World Reference Base for Soil Resources system (WRB). The impact of human activity (

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44

GUAN, Xin, Qiao-yun LI, and Feng-rong ZHANG. "Comparison of soil genetic classification and soil taxonomy for plain soil in Xinjiang." JOURNAL OF HUNAN AGRICULTURAL UNIVERSITY 37, no. 3 (2011): 312–17. http://dx.doi.org/10.3724/sp.j.1238.2011.00312.

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45

Radmanovic, Svjetlana, Jelena Bogosavljevic, Mladen Dugonjic, and Aleksandar Djordjevic. "Classification of the soils of river island micro-depressions (Great War Island, Serbia)." Journal of Agricultural Sciences, Belgrade 70, no. 1 (2025): 61–75. https://doi.org/10.2298/jas2501061r.

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Great War Island (GWI) is a river island formed at the confluence of the Sava and Danube rivers, heavily exposed to groundwater and flooding and is therefore suitable as a case study for the investigation of hydromorphic soils. The aim of this study was to classify the soils in two different micro-depression on Great War Island according to the local (Skoric 1985) and international (WRB 2022 and USDA Soil Taxonomy 1999) systems, with particular attention to the soil-forming factors that influenced the classification of the soils. The results obtained could help to improve the existing local cl

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46

Kairis, Orestis, Vassiliki Dimitriou, Chrysoula Aratzioglou, et al. "A Comparative Analysis of a Detailed and Semi-Detailed Soil Mapping for Sustainable Land Management Using Conventional and Currently Applied Methodologies in Greece." Land 9, no. 5 (2020): 154. http://dx.doi.org/10.3390/land9050154.

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Two soil mapping methodologies at different scales applied in the same area were compared in order to investigate the potential of their combined use to achieve an integrated and more accurate soil description for sustainable land use management. The two methodologies represent the main types of soil mapping systems used and still applied in soil surveys in Greece. Diomedes Botanical Garden (DBG) (Athens, Greece) was used as a study area because past cartographic data of soil survey were available. The older soil survey data were obtained via the conventional methodology extensively used over

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47

Lee, Dan-Bi, Young-Nam Kim, Yeon-Kyu Sonn, and Kye-Hoon Kim. "Comparison of Soil Taxonomy (2022) and WRB (2022) Systems for Classifying Paddy Soils with Different Drainage Grades in South Korea." Land 12, no. 6 (2023): 1204. http://dx.doi.org/10.3390/land12061204.

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Soil classification is the systematic classification of soils based on distinguishing the characteristics of soil, aiding in understanding the properties of soils through soil survey and establishing appropriate strategies for effective soil utilization and management. Globally, the Soil Taxonomy (ST) and the World Reference Base for soil resources (WRB) are widely used for soil classification. However, the two classification systems have differences in criteria, thus exhibiting difficulties in exchanging classification results. In South Korea, soil classification has been steadily implemented

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48

Mount, Henry R., and Steve R. Base. "A Methodology for Testing Soil Taxonomy Proposals." Soil Horizons 32, no. 1 (1991): 12. http://dx.doi.org/10.2136/sh1991.1.0012.

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49

Nonomura, Hideo. "Isolation, taxonomy and ecology of soil actinomycetes." Actinomycetologica 3, no. 1 (1989): 45–54. http://dx.doi.org/10.3209/saj.3_45.

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50

Galbraith, John M., Mark H. Stolt, Martin C. Rabenhorst, and Michel D. Ransom. "Impacts of fundamental changes to Soil Taxonomy." South African Journal of Plant and Soil 35, no. 4 (2018): 263–67. http://dx.doi.org/10.1080/02571862.2017.1419386.

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