Literatura académica sobre el tema "Soil"

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Artículos de revistas sobre el tema "Soil"

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Hamad, Asal Mahmud, and Mahmood Gazey Jassam. "A Comparative Study for the Effect of Some Petroleum Products on the Engineering Properties of Gypseous Soils." Tikrit Journal of Engineering Sciences 29, no. 3 (2022): 69. http://dx.doi.org/10.25130/tjes.29.3.7.

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Gypseous soils are considered problematic soils because the soil cavities happen during receiving the water or this type of soil and solving gypsum materials and contract in a soil volume. In this study, three types of gypseous soils are used; soil1, soil2, and soil3 with gypsum content (28.71%, 43.6%, and 54.88%) respectively, petroleum products (engine oil, fuel oil, and kerosene) are added to the soils with percentages (3%, 6%, 9%, and 12%) for each product. The result showed that specific gravity, liquid limit, optimum moisture content (O.M.C), and maximum dry density decreased with an inc
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Brodský, L., A. Klement, V. Penížek, R. Kodešová, and L. Borůvka. "Building soil spectral library of the Czech soils for quantitative digital soil mapping." Soil and Water Research 6, No. 4 (2011): 165–72. http://dx.doi.org/10.17221/24/2011-swr.

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  Spectral libraries are the data archives of spectral signatures measured on natural and/or man-made materials. Here, the objective is to build a soil spectral library of the Czech soils (SSL-CZ). Further on, the overall aim is to apply diffuse reflectance spectroscopy as a tool for digital soil mapping. An inevitable part of the library is a metadata database that stores the corresponding auxiliary information on the soils: type of material (soil, parent material), sample preparation, location of the sample with geographic coordinates, soil classification, morphological features, so
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Aitken, RL, and PW Moody. "Interrelations between soil pH measurements in various electrolytes and soil solution pH in acidic soils." Soil Research 29, no. 4 (1991): 483. http://dx.doi.org/10.1071/sr9910483.

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Ninety soil samples (81 surface, 9 subsurface) were collected from eastern Queensland and soil pH (1:5 soi1:solution) was measured in each of deionized water (pH,), 0.01 M CaCl2, 0-002 M CaCl2 and 1 M KCl. Soil solution was extracted from each soil after incubation for 4 days at the 10 kPa matric suction moisture content, and pH (pHss) and electrical conductivity were measured. The objectives of this work were to investigate interrelationships between soil pH measurements in various electrolytes and soil solution pH in a suite of predominantly acidic soils. Although the relationships between p
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Poyon Kizi, Khayitova Sanobar. "SOIL SCIENCE AND SOIL TERMINOLOGY." European International Journal of Multidisciplinary Research and Management Studies 02, no. 11 (2022): 42–44. http://dx.doi.org/10.55640/eijmrms-02-11-12.

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Soil science involves the study of the formation and distribution of soil, the biological, chemical and physical properties and processes of soil and how these processes interact with wider systems to help inform environmental management, industry and sustainable development.
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Najafi-Ghiri, M., and A. Abtahi. "Potassium fixation in soil size fractions of arid soils." Soil and Water Research 8, No. 2 (2013): 49–55. http://dx.doi.org/10.17221/52/2012-swr.

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Amounts of potassium (K) fixed in soil fractions of 10 calcareous soils of southern Iran were measured to evaluate the contributions of different soil size fractions to K fixation. Soil particles were fractionated after dispersion of the soils with an ultrasonic probe. Potassium fixation analysis was done by addition of 1000 mg K/kg samples. Mineralogy of the size fractions was determined by X-ray diffraction. The clay fractions were dominated by smectite, chlorite, mica, and palygorskite. Potassium fixation capacities ranged from 104 to 148 mg/kg for clay, from 102 to 155 mg/kg for s
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Vopravil, J., M. Janeček, and M. Tippl. "Revised soil erodibility K-factor for soils in the Czech Republic." Soil and Water Research 2, No. 1 (2008): 1–9. http://dx.doi.org/10.17221/2100-swr.

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In the territory of the Czech Republic there are more than 50% of agricultural soils exposed to water erosion; it is a very urgent problem both at present and for the future. It must be solved now when there is still something to be protected. It is rather complicated to describe the soil properties in terms of soil susceptibility to water erosion because it is a complex relation in which many factors participate. For the complex evaluation of all main factors participating in erosion origination it is possible to apply the Universal Soil Loss Equation (USLE). It consists of six factors intera
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Behrens, T., K. Gregor, and W. Diepenbrock. "Separation of soil and canopy reflectance signatures of Mid German agricultural soils." Plant, Soil and Environment 51, No, 7 (2011): 296–303. http://dx.doi.org/10.17221/3589-pse.

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Remote sensing can provide visual indications of crop growth during production season. In past, spectral optical estimations were well performed in the ability to be correlated with crop and soil properties but were not consistent within the whole production season. To better quantify vegetation properties gathered via remote sensing, models of soil reflectance under changing moisture conditions are needed. Signatures of reflected radiation were acquired for several Mid German agricultural soils in laboratory and field experiments. Results were evaluated at near-infrared spectral region at the
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Romanova, Tatyana, Aliaksandr Chervan, and Nadezhda Ivakhnenko. "The essence of soil and soil formation in accordance with soil water regime." Journal of Geography and Cartography 7, no. 2 (2024): 6271. http://dx.doi.org/10.24294/jgc.v7i2.6271.

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The obtaining of new data on the transformation of parent materials into soil and on soil as a set of essential properties is provided on the basis of previously conducted fundamental studies of soils formed on loess-like loams in Belarus (15,000 numerical indicators). The study objects are autochthonous soils of uniform granulometric texture. The basic properties without which soils cannot exist are comprehensively considered. Interpolation of factual materials is given, highlighting the essential properties of soils. Soil formation is analyzed as a natural phenomenon depending on the life ac
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Kodešová, R. "Miroslav Kutílek – Professor of soil science, soil physics and soil hydrology." Soil and Water Research 3, Special Issue No. 1 (2008): S5—S6. http://dx.doi.org/10.17221/1412-swr.

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Beylich, Anneke, Hans-Rudolf Oberholzer, Stefan Schrader, Heinrich Höper, and Berndt-Michael Wilke. "Evaluation of soil compaction effects on soil biota and soil biological processes in soils." Soil and Tillage Research 109, no. 2 (2010): 133–43. http://dx.doi.org/10.1016/j.still.2010.05.010.

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Tesis sobre el tema "Soil"

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Alvenäs, Gunnel. "Evaporation, soil moisture and soil temperature of bare and cropped soils /." Uppsala : Swedish Univ. of Agricultural Sciences (Sveriges lantbruksuniv.), 1999. http://epsilon.slu.se/avh/1999/91-576-5714-9.pdf.

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Robert, Dilan Jeyachandran. "Soil-pipeline interaction in unsaturated soils." Thesis, University of Cambridge, 2010. https://www.repository.cam.ac.uk/handle/1810/265508.

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Pipelines that are used for the transport of energy and services are very important lifelines to modem society. Though pipelines are generally buried in unsaturated soils, the design guidelines are based on the assumption that the soil is either dry or fully saturated. For certain geotechnical problems, this assumption may not be acceptable because the water meniscus formed between soil particles creates an additional normal force between them by suction, which in turn forms temporary bonds. A recent series of large-scale physical model experiments at the Pipeline Engineering Research Laborato
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Ekanayake, Jagath C. "Soil water movement through swelling soils." Lincoln University, 1990. http://hdl.handle.net/10182/1761.

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The present work is a contribution to description and understanding of the distribution and movement of water in swelling soils. In order to investigate the moisture distribution in swelling soils a detailed knowledge of volume change properties, flow characteristics and total potential of water in the soil is essential. Therefore, a possible volume change mechanism is first described by dividing the swelling soils into four categories and volume change of a swelling soil is measured under different overburden pressures. The measured and calculated (from volume change data) overburden potentia
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Zhang, Guanghui, and 張廣輝. "Soil-water characteristics of sandy soil and soil cement with and without vegetation." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/208025.

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The use of soil cement as a growth medium was examined in this study. During the monitoring, green soil cement revealed diverse ecological values. The survival rates of plants in each soil conditions were higher than 80%,which was very promising. Furthermore, the survival rates dropped when the soil density reached95%, which means soil density might influence the survival rate of plant. Plant growth rates in sandy soil were higher than that in soil cement. In particular, low soil density facilitated plant growth in sandy soil, whereas density effect was not clear to plant growth performance in
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Corneo, Paola Elisa. "Understanding soil microbial community dynamics in vineyard soils: soil structure, climate and plant effects." Doctoral thesis, country:CH, 2013. http://hdl.handle.net/10449/23970.

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This thesis aimed at characterising the structure of the bacterial and fungal community living in vineyard soils, identifying and describing the parameters that explain the distribution of the microbial communities in this environment. Vineyards represent an economical relevant agro-ecosystem, where vines, long-lived woody-perennial plants, are normally cultivated at different altitudes. The maintenance of the soil quality is at the base of a productive agriculture and thus the investigation of its biological component, its structure and all the processes that take place into the soil a
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Njie, Momodou. "Modelling soil moisture dynamics in vegetated soils." Thesis, Imperial College London, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.406159.

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Dash, Suresh R. "Lateral pile soil interaction in liquefiable soils." Thesis, University of Oxford, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.543468.

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Gebhardt, Martha Mary. "Soil Amendment Effects on Degraded Soils and Consequences for Plant Growth and Soil Microbial Communities." Thesis, The University of Arizona, 2015. http://hdl.handle.net/10150/556614.

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Human activities that disrupt soil properties are fundamentally changing ecosystems. Soil degradation decreases microbial abundance and activity, leading to changes in nutrient availability, soil organic matter, and plant growth and establishment. Land use and land cover change are widespread and increasing in semiarid regions of the southwestern US, which results in reductions of native plant and microbial abundance and community diversity. Here we studied the effects of soil degradation and amendments (biochar and woodchips) on microbial activity, soil carbon and nitrogen availability, and p
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Wagai, Rota. "Climatic and Lithogenic Controls on Soil Organic Matter-Mineral Associations." Fogler Library, University of Maine, 2005. http://www.library.umaine.edu/theses/pdf/WagaiR2005.pdf.

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Keller, Thomas. "Soil compaction and soil tillage - studies in agricultural soil mechanics /." Uppsala : Dept. of Soil Sciences, Swedish Univ. of Agricultural Sciences, 2004. http://epsilon.slu.se/a489.pdf.

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Libros sobre el tema "Soil"

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Fanning, Delvin Seymour. Soil. Wiley, 1989.

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Troeh, Frederick R. Soils and soil fertility. 5th ed. Oxford University Press, 1993.

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M, Thompson Louis, ed. Soils and soil fertility. 6th ed. Blackwell Pub., 2005.

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Remmelzwaal, A. Botswana soil database: Guidelines for soil profile description. Food and Agriculture Organization of the United Nations, 1988.

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K, Davis B. N., ed. The Soil. HarperCollins, 1991.

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Bowman, Chris. Soil. Bellwether Media, 2014.

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Cunningham, Kevin. Soil. Morgan Reynolds Pub., 2009.

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Walker, Kate. Soil. Marshall Cavendish Benchmark, 2012.

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Gershuny, Grace. The soul of soil: A guide to ecological soil management. 3rd ed. agAccess, 1995.

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W, Buol S., and Buol S. W, eds. Soil genesis and classification. 4th ed. Iowa State University Press, 1997.

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Capítulos de libros sobre el tema "Soil"

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Waddington, Donald V. "Soils, Soil Mixtures, and Soil Amendments." In Turfgrass. American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, 2015. http://dx.doi.org/10.2134/agronmonogr32.c10.

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Shah, Atul K. "Soil and Soul." In Organic Finance. Routledge, 2025. https://doi.org/10.4324/9781003534532-2.

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Castilho, Pierre del, and Rainer Breder. "Soils and Soil Solutions." In Sampling and Sample Preparation. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60632-8_5.

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McGrath, Timothy J. "Soils and soil models." In Analysis and Design of Gravity Flow Conduits and Buried Bridges. CRC Press, 2024. https://doi.org/10.1201/9780429162619-4.

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Huntley, Brian John. "Soil, Water and Nutrients." In Ecology of Angola. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-18923-4_6.

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AbstractThis Chapter provides an introduction to basic elements of soil science, from an understanding of the soil profile, its develop and its importance to plant growth. The processes of weathering and the development of laterites, calcretes, salinised and other major soil types and their distribution in Angola are described. Soil water relations and soil chemistry and thus the availability of water and nutrients are fundamental determinants of plant growth, species composition and productivity. The differences between dystrophic (low base status) and eutrophic (high base status) soils and t
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Hågvar, Sigmund. "Soil Biology: Soil Animals and Soil Acidity." In Ecological Studies. Springer New York, 1994. http://dx.doi.org/10.1007/978-1-4612-2604-8_5.

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Olsen, Rolf Arnt. "Soil Biology: Soil Microflora and Soil Acidity." In Ecological Studies. Springer New York, 1994. http://dx.doi.org/10.1007/978-1-4612-2604-8_6.

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Adewara, O. A., T. C. Adebayo-Olajide, J. S. Ayedun, et al. "Soil Formation, Soil Health and Soil Biodiversity." In Earth and Environmental Sciences Library. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-53270-2_5.

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Saha, Madhumita. "Poor Soil, Rich Soil." In The Making of Modern Agriculture in Independent India. Routledge India, 2025. https://doi.org/10.4324/9781003500285-2.

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Wallander, Håkan. "Our Indispensable Soil." In Soil. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-08458-9_1.

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Actas de conferencias sobre el tema "Soil"

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Shishkov, Toma, Emil Dimitrov, and Ekaterina Filchev. "FOREST SOILS FROM SREDNA GORA MOUNTAIN IN BULGARIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s13.29.

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The soils from the central part of Sredna Gora Mountain in Bulgaria were studied aiming to establish the occurrence of contemporal soil forming processes occured in the forest ecosystem. Soils were analyzed to determine the carbon content, the soil organic matter composition and the total soil acidity. The precise soil classification based on the detail morphological diagnostic was carried out. The ecological conditions in forest ecosystem determine the mode of humic substances in the studies soils. Soils are characterized with low degree of humification and considerable amount of organic matt
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Haseeb, Muhammad, Anas Ayub, and Aimen Nawaz. "Impact of Climate Change on Organic soil: A Comprehensive Literature Review." In 14th International Civil Engineering Conference. Trans Tech Publications Ltd, 2025. https://doi.org/10.4028/p-fw5pfm.

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This paper focuses on the effects of climate change on soil systems which is an important research topic due to importance of soil in offering support to plants, controlling water, and supporting ecosystems. The intention was to review how increasing worldwide temperatures and changes in precipitation impact the properties that define the soil such as organic matter turnover, nutrient dynamics, and soil structure. The findings suggest that the rates of decomposition of soil organic matter increases with rising temperatures; therefore, rising temperatures would bring about drastic shifts in the
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Ponomaryov, Andrey B. "REINFORCEMENT OF SOIL FOUNDATIONS." In VIII Петрухинские чтения. АО «НИЦ «Строительство», 2024. http://dx.doi.org/10.37538/2713-1149-2024-104-123.

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This article gives the basic terms and definitions of geosynthetic materials currently used in construction. The main functions and types of geosynthetics are shown. Most of the article is devoted to the results obtained by various researchers of the Perm Scientific School. The results of reinforcing sandy and clayey soils with geosynthetic materials, reinforcing soil pads, using fiber soil, reinforcing karst soils, and using geosynthetics in seasonally freezing soils are shown.
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Singh, Shikha, Sindhu Jagadamma, Junyi Liang, Gangsheng Wang, and Melanie Mayes. "SENSITIVITY OF MICROBIAL PROCESSING OF SOIL CARBON TO SOIL MOISTURE IN DIFFERENTLY-TEXTURED SOILS." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312541.

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Baumgartl, Thomas, J. Chan, F. Bucka, and E. Pihlap. "Soil organic carbon in rehabilitated coal mine soils as an indicator for soil health." In 14th International Conference on Mine Closure. QMC Group, Ulaanbaatar, 2021. http://dx.doi.org/10.36487/acg_repo/2152_121.

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Pospisilova, Lubica. "APPLICATION OF SOIL CONDITIONERS IN SANDY SOILS." In 15th International Multidisciplinary Scientific GeoConference SGEM2015. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2015/b32/s13.005.

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Andromalos, Kenneth B., Yasser A. Hegazy, and Brian H. Jasperse. "Stabilization of Soft Soils by Soil Mixing." In Soft Ground Technology Conference. American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40552(301)16.

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Zou, L., and E. C. Leong. "Soils with Bimodal Soil-Water Characteristic Curve." In Second Pan-American Conference on Unsaturated Soils. American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481684.006.

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Bean, E. Z., and M. D. Dukes. "Soil Amendments for Mitigation of Compacted Soils." In Low Impact Development International Conference (LID) 2010. American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41099(367)66.

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Drnevich, Vincent P., Carlos E. Zambrano, Sochan Jung, and Julia P. Clarke. "Electrical Conductivity of Soils and Soil Properties." In GeoCongress 2008. American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40972(311)40.

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Informes sobre el tema "Soil"

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Ponder, Felix Jr, and Darrell E. Alley. Soil sampler for rocky soils. U.S. Department of Agriculture, Forest Service, North Central Research Station, 1997. http://dx.doi.org/10.2737/nc-rn-371.

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Wentworth, Jonathan, and Cagla Stevenson. Sustaining the soil microbiome. Parliamentary Office of Science and Technology, 2019. http://dx.doi.org/10.58248/pn601.

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The soil microbiome, communities of microorganisms in soils, underpin natural processes in soil habitats and are affected by environmental and land use change. This POSTnote gives an overview of the benefits provided by the soil microbiome, ways of assessing the soil microbiome, and measures to improve its condition.
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Dehaene, Michiel, Daniel López-García, Jana Fried, et al. SOIL NEXUS: Urban soil care for food production, community greenspace, and environmental resilience. Coventry University, 2024. https://doi.org/10.18552/cawr/2024/0002.

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Global urbanisation is leading to the degradation of living soils, with substantial and direct impacts on climate, biodiversity, food security, and human health. Urban land use policies are beginning to address soil protection. However, they rarely address the depollution and remediation of urban soils and the revitalisation of the agricultural socio-economic fabric, both essential to recover and maintain healthy soils. Instead polluted soils are often managed through further soil sealing (i.e. covering with a plastic ‘geotextile’ layer to isolate it and adding new soil on top). As alternative
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Keller, Adrienne Blair, and Stephen Dwight Handler. Soil organic carbon in temperate managed ecosystems. Northern Forests Climate Hub, 2024. http://dx.doi.org/10.32747/2024.8633528.ch.

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Soils store more carbon than the atmosphere and vegetation combined, an impressive fact that underscores the importance of considering soils when managing for ecosystem carbon. Not only do soils store vast amounts of carbon, but soil carbon also persists in the ecosystem for much longer than other pools of carbon. This primer is an introduction to soil organic carbon storage, sequestration, and cycling in terrestrial managed ecosystems. The effects of site factors, climate change, and management on soil carbon are discussed.--
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Lundström, Christina, Elin Wärm, Margherita Caggiano, and Mayte Gallego. Good examples of soil education for youth to increase soil literacy. Department of Soil and Environment, Swedish University of Agricultural Sciences, 2025. https://doi.org/10.54612/a.2bqc5135bc.

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One of eight aims of the EU Mission Soil, is to increase soil literacy in society. One way to do that would be to reach out to teachers and inspire them to involve soil topics in their teaching. Therefore PREPSOIL Task 6.2 aimed to identify good examples of soil education and learning activities for youth and communicate them with teachers and pedagogic representatives across Europe. During 2023 and 2024 teachers were invited to share their good examples on soil education targeting primary, secondary and vocational training pupils. A committee which consisted of three teachers, one soil scient
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Gombert, D. II. Evaluation of soil washing for radiologically contaminated soils. Office of Scientific and Technical Information (OSTI), 1994. http://dx.doi.org/10.2172/10163686.

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Cunnane, J. C., V. R. Gill, S. Y. Lee, et al. Uranium soils integrated demonstration: Soil characterization project report. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/10180428.

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Busby, Ryan, H. Torbert, and Stephen Prior. Soil and vegetation responses to amendment with pulverized classified paper waste. Engineer Research and Development Center (U.S.), 2022. http://dx.doi.org/10.21079/11681/44202.

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The United States Army produces a significant amount of classified paper waste that is pulverized to a fine consistency unsuitable for recycling. However, cheap, high quality organic materials such as classified paper waste are useful as soil amendments. The objective of this research was to evaluate the utilization of pulverized classified paper waste as a soil amendment to improve soil health and increase establishment of desirable native grasses on degraded Army training lands. Paper was applied at rates of 9 to 72 Mg ha⁻¹ to two soil types at Fort Polk, LA: an alfisol (very fine sandy loam
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Wentworth, Jonathan. Soil as an essential national asset. Parliamentary Office of Science and Technology, 2021. http://dx.doi.org/10.58248/hs22.

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Siegrist, R. L. (Contaminated soil). Office of Scientific and Technical Information (OSTI), 1991. http://dx.doi.org/10.2172/6076299.

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