Bibliografías temáticas / Soils Soils Soils Soils Serpentine Serpentine

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Literatura académica sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 16 de febrero de 2022

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Artículos de revistas sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

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Gladish, Sandra, Jonathan Frank, and Darlene Southworth. "The serpentine syndrome below ground: ectomycorrhizas and hypogeous fungi associated with conifers." Canadian Journal of Forest Research 40, no. 8 (2010): 1671–79. http://dx.doi.org/10.1139/x10-092.

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Serpentine soils select for unique plant communities, often with sparse vegetation. Mycorrhizal fungi mediate the interaction between plants and soils, yet little is known about the mycorrhizal fungi of serpentine-tolerant plants. Ectomycorrhizas and hypogeous fungal sporocarps were sampled on paired serpentine and nonserpentine soils in southwestern Oregon. We hypothesized that conifers on serpentine soils would have fewer species of mycorrhizal fungi, a distinct assemblage of ectomycorrhizal fungi, and fewer hypogeous sporocarps with less species richness. Sporocarps were sampled and soil co
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Baugé, S. M. Y., L. M. Lavkulich, and H. E. Schreier. "Serpentine affected soils and the formation of magnesium phosphates (struvite)." Canadian Journal of Soil Science 93, no. 2 (2013): 161–72. http://dx.doi.org/10.4141/cjss2012-117.

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Baugé, S. M. Y., Lavkulich, L. M. and Schreier, H. E. 2013. Serpentine affected soils and the formation of magnesium phosphates (struvite). Can. J. Soil Sci. 93: 161–172. The Sumas River watershed, located in the intensive agricultural region of the Lower Fraser Valley of British Columbia (Canada), contains serpentine asbestos from a natural landslide. Serpentinic soils have a high Mg to Ca ratio that can affect soil fertility, including soil-solution P relations. The objectives of the study were: (i) to evaluate some common methods of estimating plant available phosphorus in the surface horiz
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Mróz, Lucyna. "Between-population variation in plant performance traits and elemental composition of Colchicum autumnale L. and its relation to edaphic environments." Acta Societatis Botanicorum Poloniae 77, no. 3 (2011): 229–39. http://dx.doi.org/10.5586/asbp.2008.029.

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Variation in vegetative and reproductive performance and leaf mineral composition among 25 populations of <em>Colchicum autumnale</em> (meadow saffron) from soils derived from six parent materials (limestone, marl, sandstone, greenstone, melaphyre and serpentine) in southwestern Poland has been investigated. The plant size (PS), total le-af area (TLA), leaf shape (LS), number of fruits per plant (NFP), number of seeds per plant (NFP), total weight seed per plant (TWSP) were estimated, and concentrations of seventeen elements (N, P, K, Ca, Mg, Na, S, Fe, Mn, Cu, Zn, Pb, Cd, Ni, Co,
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McAlister, Rachel L., Duane A. Kolterman, and A. Joseph Pollard. "Nickel hyperaccumulation in populations of Psychotria grandis (Rubiaceae) from serpentine and non-serpentine soils of Puerto Rico." Australian Journal of Botany 63, no. 2 (2015): 85. http://dx.doi.org/10.1071/bt14337.

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Metal hyperaccumulators are plants that store heavy metals or metalloids in their leaves, often to concentrations much higher than in the soil. Though most occur exclusively on metalliferous soils, some species are facultative, occurring on both metalliferous and nonmetalliferous soils. Psychotria grandis Sw.(Rubiaceae) occurs from Central America through the Caribbean on many soil types, and hyperaccumulates nickel (Ni) on serpentine soils in several localities. In this study, four Puerto Rican populations of P. grandis – two from serpentine soil and two from non-serpentine soil – were examin
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Sánchez-Marañón, M., E. Gámiz, G. Delgado, and R. Delgado. "Mafic-ultramafic soils affected by silicic colluvium in the Sierra Nevada Mountains (southern Spain)." Canadian Journal of Soil Science 79, no. 3 (1999): 431–42. http://dx.doi.org/10.4141/s98-063.

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Soil properties, mineral composition, available microelements for plant uptake and ultramicromorphological gravel characteristics in skeletal soils from amphibolite and serpentinite rocks with additions of silicon-rich colluvial materials were studied in the Mediterranean region (Sierra Nevada, southern Spain). The soils (Entic Cryumbrept, Typic Xerochrept, Pachic Cryoboroll and Typic Cryorthent) showed mineralogical discontinuities, exchangeable Ca:Mg ratios greater than 1 and a pH and base saturation profile that decreases in the central and lower parts of the solum. The different soil parti
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Bulmer, C. E., and L. M. Lavkulich. "Pedogenic and geochemical processes of ultramafic soils along a climatic gradient in southwestern British Columbia." Canadian Journal of Soil Science 74, no. 2 (1994): 165–77. http://dx.doi.org/10.4141/cjss94-024.

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This paper presents information on pedogenic processes, weathering status and geochemical evolution of ultramafic soils at three areas in southwestern British Columbia characterized by climatic conditions ranging from relatively wet–cool to relatively dry–cool. The soils of the Coquihalla serpentine belt have Podzolic profiles that resulted from intense weathering in a moist environment. The Tulameen area has a moderately dry climate, and Brunisolic soils have developed in serpentinized peridotite and dunite. Brunisolic soils with composite profiles of tephra overlying serpenite developed in a
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Alexander, E. B. "Serpentine Soils of Northern Alaska." Soil Horizons 45, no. 4 (2004): 120. http://dx.doi.org/10.2136/sh2004.4.0120.

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Oze, Christopher, Scott Fendorf, Dennis K. Bird, and Robert G. Coleman. "Chromium Geochemistry of Serpentine Soils." International Geology Review 46, no. 2 (2004): 97–126. http://dx.doi.org/10.2747/0020-6814.46.2.97.

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SUDARMONO, SUDARMONO. "Endemic plants of serpentine soils." Biodiversitas, Journal of Biological Diversity 8, no. 4 (2007): 330–35. http://dx.doi.org/10.13057/biodiv/d080417.

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Southworth, Darlene, Linda E. Tackaberry, and Hugues B. Massicotte. "Mycorrhizal ecology on serpentine soils." Plant Ecology & Diversity 7, no. 3 (2013): 445–55. http://dx.doi.org/10.1080/17550874.2013.848950.

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Tesis sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

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McIntyre, Todd Ian. "Analysis of selected ions in Allium cratericola growing on serpentine and non-serpentine soil." Scholarly Commons, 1991. https://scholarlycommons.pacific.edu/uop_etds/2212.

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The primary problems which plants growing on serpentine soil must overcome are high magnesium concentrations and calcium deficiency. The ability of Allium cratericola to successfully exploit both serpentine and non-serpentine habitats may be due to physiological adaptations which compensate for unusual mineral composition of the soil. Although the Table Mountain soil is described as non serpentine, it bears ionic similarities to the three serpentine soils studied in this investigation. With the advent of modern biochemical techniques in plant physiology, there are ample opportunities to expand
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Boulet, Frederic. "Mycorrhizal symbiosis as a strategy for survival in ultramafic soils." University of Western Australia. Soil Science and Plant Nutrition Discipline Group, 2003. http://theses.library.uwa.edu.au/adt-WU2004.0051.

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Ultramafic soils enriched in nickel, such as found in Australia and New Caledonia, are associated with unique, diverse and poorly known vegetation communities. Re-establishment of these highly specific ecosystems is still a challenge for Ni mining companies. Ultramafic vegetation communities are the outcome of a long evolution process resulting in their adaptation to the extreme soil conditions found on ultramafic outcrops. Mycorrhizal fungi, a very common plant symbiont, are generally thought to be beneficial to plants in other ecosystems, providing plants with phosphorus and even promoting m
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Cooke, Sarah Spear. "The edaphic ecology of two western North American composite species /." Thesis, Connect to this title online; UW restricted, 1994. http://hdl.handle.net/1773/5569.

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Nyberg, Berglund Anna-Britt. "Postglacial colonization and parallel evolution of metal tolerance in the polyploid Cerastium alpinum /." Uppsala : Dept. of Plant Biology and Forest Genetics, Swedish University of Agricultural Sciences, 2005. http://epsilon.slu.se/200565.pdf.

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Jansen, Nora Catharine Mary. "Vegetation ecology of Rawhide Hill, Toulumne County, California." Scholarly Commons, 1991. https://scholarlycommons.pacific.edu/uop_etds/2208.

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Hollstein, R. W. M. "The dependence of mycorrhrizae in Sitka spruce roots, on the availability of phosphorus in serpentine and basaltic soils." Thesis, University of Aberdeen, 1986. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU006854.

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The nature and occurrence of mycorrhizal associations, with particular reference to the anatomy, carbohydrate physiology, plant mineral nutrition and occurrence of ectomycorrhizae (ECM), is discussed. The ecology and forest relations of <i>Picea sitchensis</i> - the Sitka spruce concludes the literature review. Identification of areas of good and poor Sitka growth on related soils and the quantification of their ECM status, investigation of the effect of phosphate addition to Sitka seedlings in pots, subsequent and changes to their ECM status, and the effects of soluble aluminium on phosphate
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Bani, Aïda. "Phytoextraction du Ni dans les sols ultramafiques d'Albanie." Thesis, Vandoeuvre-les-Nancy, INPL, 2009. http://www.theses.fr/2009INPL042N/document.

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Phytoextraction du nickel dans les sols ultramafiques d’Albanie La phytoextraction minière est un procédé de récupération des métaux des sols minéralisés naturels ou pollués à l’aide de plantes hyperaccumulatrices. Elle est une alternative à l’agriculture vivrière des zones ultramafiques. L’objectif de la thèse est le développement d’une technologie de phytoextraction extensive du Ni avec Alyssum murale sur les Vertisols ultramafiques. Pour cela, il s’agissait : i) d’identifier les plantes hyperaccumulatrices les plus efficaces dans le prélèvement du Ni et comprendre les relations entre le pré
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Chardot, Vanessa. "Réponse de Brassicacées hyperaccumulatrices à la disponibilité du nickel des sols ultramafiques." Thesis, Vandoeuvre-les-Nancy, INPL, 2007. http://www.theses.fr/2007INPL045N/document.

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Les plantes hyperaccumulatrices de métaux ont développé des mécanismes spécifiques de prélèvement de la fraction disponible des métaux du sol, conduisant à leur accumulation dans les parties aériennes. L’utilisation agronomique de ces plantes pourrait être une voie de dépollution des sols contaminés en métaux. Ce travail a pour objectif de contribuer à la compréhension des mécanismes chimiques et biologiques qui conditionnent l’accumulation du Ni par les plantes hyperaccumulatrices, en réponse à la disponibilité du métal dans le sol. Après observation du fonctionnement naturel du système sol u
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Springer, Yuri P. "Epidemiology, resistance structure, and the effects of soil calcium on a serpentine plant-pathogen interaction /." Diss., Digital Dissertations Database. Restricted to UC campuses, 2006. http://uclibs.org/PID/11984.

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Rossington, Natalie L. "How are rare species maintained?: Reproductive barriers between Layia jonesii, a rare serpentine endemic, and L. platyglossa." DigitalCommons@CalPoly, 2015. https://digitalcommons.calpoly.edu/theses/1494.

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Reproductive barriers are vital to generating new species as well as maintaining distinct species. Investigating reproductive barriers between closely related plant taxa helps us to understand how these barriers are maintained, particularly between rare and widespread relatives. Layia jonesii, a rare San Luis Obispo County serpentine endemic, and L. platyglossa, a common coastal species, co-occur on serpentine derived hillsides and are interfertile. At these locations, L. jonesii is isolated to dry soils near serpentine rock outcrops and L. platyglossa is located on slightly deeper grassland s
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Libros sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

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Kruckeberg, Arthur R. Introduction to California soils and plants: Serpentine, vernal pools, and other geobotanical wonders. University of California Press, 2006.

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Introduction to California soils and plants: Serpentine, vernal pools, and other geobotanical wonders. University of California Press, 2005.

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Serpentine: The evolution and ecology of a model system. University of California Press, 2010.

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International Conference on Serpentine Ecology (1st 1991 University of California, Davis). The vegetation of ultramafic (serpentine) soils: Procedings of the first International Conference on Serpentine Ecology ... 1991. Intercept, 1992.

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International Conference on Serpentine Ecology (1st 1991 University of California, Davis). The vegetation of ultramafic (serpentine) soils: Proceedings of the First International Conference on Serpentine Ecology, University of California, Davis, 19-22 June 1991. Intercept, 1992.

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Brooks, R. R. Serpentine and its vegetation: A multidisciplinary approach. Croom Helm, 1987.

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Brooks, R. R. Serpentine and its vegetation: A multidisciplinary approach. Dioscorides Press, 1987.

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International Conference on Serpentine Ecology (2nd 1995 Nouméa, New Caledonia). Ecologie des milieux sur roches ultramafiques et sur sols métallifères: Actes de la Deuxième Conférence internationale sur l'écologie des milieux serpentiniques, Nouméa, 31 juillet-5 août 1995. Edited by Jaffré Tanguy, Reeves R. D. 1940-, Becquer T, and O.R.S.T.O.M. (Agency : France). Centre de Nouméa. Centre ORSTOM de Nouméa, 1995.

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Elam, Diane R. Draft recovery plan for serpentine soil species of the San Francisco Bay area. U.S. Fish and Wildlife Service, Pacific Region, 1998.

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Bradley, Goettle, Wright David H, and U.S. Fish and Wildlife Service. Region 1., eds. Draft recovery plan for serpentine soil species of the San Francisco Bay area. U.S. Fish and Wildlife Service, Pacific Region, 1998.

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Capítulos de libros sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

1

Jeffrey, David W. "Calcareous and serpentine soils and their vegetation." In Soil~Plant Relationships. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-011-6076-6_19.

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Husna, Faisal Danu Tuheteru, and Asrianti Arif. "Arbuscular Mycorrhizal Fungi and Plant Growth on Serpentine Soils." In Arbuscular Mycorrhizas and Stress Tolerance of Plants. Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-4115-0_12.

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Mengoni, Alessio, Lorenzo Cecchi, and Cristina Gonnelli. "Nickel Hyperaccumulating Plants and Alyssum bertolonii: Model Systems for Studying Biogeochemical Interactions in Serpentine Soils." In Soil Biology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-23327-2_14.

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Effendi, Syarif, Satoru Miura, Nagaharu Tanaka, and Seiichi Ohta. "Serpentine Soils on Catena in the Southern Part of East Kalimantan, Indonesia." In Rainforest Ecosystems of East Kalimantan. Springer Japan, 2000. http://dx.doi.org/10.1007/978-4-431-67911-0_7.

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Harrison, Susan. "Population Persistence and Community Diversity in a Naturally Patchy Landscape: Plants on Serpentine Soils." In The Biology of Biodiversity. Springer Japan, 2000. http://dx.doi.org/10.1007/978-4-431-65930-3_10.

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Hseu, Zeng-Yei, Zueng-Sang Chen, Chen-Chi Tsai, and Shih-Hao Jien. "Portable X-Ray Fluorescence (pXRF) for Determining Cr and Ni Contents of Serpentine Soils in the Field." In Progress in Soil Science. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28295-4_3.

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White, G. Norman, and Joe B. Dixon. "Kaolin-Serpentine Minerals." In Soil Mineralogy with Environmental Applications. Soil Science Society of America, 2018. http://dx.doi.org/10.2136/sssabookser7.c12.

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Nabais, C., H. Freitas, and J. Hagemeyer. "Seasonal variations of amino acids and organic acids in the xylem sap of Quercus ilex L. growing on serpentine and sandy loam soils." In Plant Nutrition for Sustainable Food Production and Environment. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-009-0047-9_121.

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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Serpentine Soil Distributions and Environmental Influences." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0010.

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Serpentine soils occur in all but one of the twelve orders (Alexander 2004b), which is the highest level in Soil Taxonomy (Soil Survey Staff 1999), the primary system of soil classification utilized in this book (appendix C). They occur in practically every environment from cold arctic to hot tropical and from arid to perhumid (always wet). Thus the variety of serpentine soils is very great even though they occupy only a small fraction of the earth. Serpentine soils have been found in all states and provinces that are adjacent to the Pacific Ocean from Baja California to Alaska. They are most concentrated in the California Region, where they have been mapped in 34 counties in California and in 5 counties in southwestern Oregon. Serpentine lateritic (or “nickel laterite”) soils, which have not been mapped separately from other soils, are economically significant in California and southwest Oregon, even though they are not widely distributed in western North America. A representative serpentine soil is shown in figure 6-1. Serpentine soils, or soils in magnesic (serpentine) families, are represented in 11 of the 12 soil orders. Spodosols and Histosols in magnesic families occur only where there is a thin cover of nonserpentine materials over the serpentine materials, and there are no serpentine Andisols. Andisols contain amorphous and poorly ordered aluminum-silicate minerals, which are responsible for andic soil properties of these soils. Serpentine soil parent materials do not contain enough aluminum for the development of andic soil properties that are definitive of Andisols. Alfisols are soils with argillic (or natric) horizons having more than 35% exchangeable bases (Ca2+, Mg2+, Na+, and K+) on the cation exchange complex. Al3+ and H+ are the common nonbasic (acidic) cations on the exchange complex. The Mg2+ that serpentine soil parent materials release upon weathering keeps the basic cation status of soils high, unless they are leached intensively. Some of the soil horizon sequences are A-Bt, A-Btn, and A-Bt-Btk in Alfisols. Soils of Dubakella Series and other moderately deep Mollic Haploxeralfs with a mesic soil temperature regime are the most extensively mapped serpentine Alfisols in California and southwestern Oregon. Figure 6-1 is representative of the Mollic Haploxeralfs.
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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Serpentine Soils as Media for Plant Growth." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0012.

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Plants and animals require water, energy sources, and nutrients to make tissues and perform vital functions. The primary source of energy is the sun. Green plants use solar energy to manufacture organic compounds that are later oxidized to produce energy for both plants and animals. Many microorganisms produce energy by inorganic chemical reactions, but that source of energy is minor compared to the very large amounts of solar energy used by green plants. The major source of water and nutrients (other than CO2) for green plants is soil. Barren rocks, including ultramafic rock outcrop and talus, are colonized by lichens, which are symbiotic alliances of fungi and either cyanobacteria or green algae. These and other small organisms promote weathering and contribute to soil formation. Once soils are deep enough to support vascular plants (plants with roots), plants are the primary users of soils and producers of ecosystem biomass. Vascular plants send roots into soils and exploit both a high soil particle surface area and soil solutions, neither of which are available to lichens growing on rock surfaces. The surface area of particles in a soil 10 cm deep is about a thousand times greater than a planar bedrock surface if the soil is coarse sand, or about a billion times greater if the soil is clayey. With these dramatic increases in surface area accompanying soil formation, and lack of water retained on rock surfaces, it is easy to understand that ecosystem productivity is relatively low on rock surfaces and increases greatly with soil depth in very shallow soils. Annual plants approach maximum productivity in moderately deep soils and trees in deep or very deep soils. Ecosystems with serpentine soils are generally less productive than ecosystems with other kinds of soils, and they have unique plant species distributions. Therefore, serpentine soils attract attention from botanists who are interested in the profound effects that serpentine soils have on plant distributions and growth. These effects include those that affect the supply of water (section 8.1) and those that affect the supply of nutrients (section 8.2) to plants. These in turn affect plant growth and productivity (section 8.3).
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Actas de conferencias sobre el tema "Soils Soils Soils Soils Serpentine Serpentine"

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KARA, Zekeriya. "TOTAL HEAVY METAL CONTENTS IN SERPENTINITE SOILS FROM TURKOGLU-KAHRAMANMARAS/TURKEY." In 18th International Multidisciplinary Scientific GeoConference SGEM2018. Stef92 Technology, 2018. http://dx.doi.org/10.5593/sgem2018/3.2/s13.085.

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Medeiros, Ian Daniel, and Nishanta Rajakaruna. "DOCUMENTING THE ROCKS, SOILS, AND BIOTA OF SERPENTINITE OUTCROPS IN WESTERN MASSACHUSETTS." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272908.

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PEKARSKAS, Juozas, Algirdas GAVENAUSKAS, Anželika DAUTARTĖ, and Aida STIKLIENĖ. "RECYCLING OF MINERAL SERPENTINITE WASTE FROM MINING INDUSTRY AND ITS USE IN AGRICULTURE TO IMPROVE SOIL AGROCHEMICAL PROPERTIES." In RURAL DEVELOPMENT. Aleksandras Stulginskis University, 2018. http://dx.doi.org/10.15544/rd.2017.102.

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The influence of processing the serpentinite quarry from the Caucasian mountains at the foot of the Mount Elbrus crushed waste on soil agrochemical properties, phytotoxicity of spring barley, influence on barley plant biomass and its chemical composition were investigated. Ground and granular serpentinite had a different effect on soil and plants. Application of serpentinite fertilizers significantly increased the content of calcium, iron, 227.95-376.75 and 5.05-9.62 mg kg-1, total and plant-derived magnesium 0.34-0.52 and 1.19-2.16 mg kg-1, lead and nickel, while the amount of copper dropped
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Fullem, Abby, Alain F. Plante, and Donald C. Barber. "AN ANALYSIS OF RESTORATION PRACTICES: A SOIL SURVEY OF THE UNIONVILLE SERPENTINE BARRENS, CHESTER CO., PA." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272905.

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Lorente, S., and A. Bejan. "Flow Architectures for Ground-Coupled Heat Pumps." In ASME 2016 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/imece2016-65410.

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In this paper we report the main advances made by our research group on the heat transfer performance of complex stream architectures embedded in a conducting solid. The immediate application of this review work deals with ground-coupled heat pumps. Various configurations are considered: U-shaped with varying spacing between the parallel portions of the U, serpentines with three elbows, and trees with T- and Y-shaped bifurcations. In each case the volume ratio of fluid to soil is fixed. We determine the critical geometric features that allow the heat transfer density of the stream-solid config
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