1,721,017 research outputs found

    Silicio, Alluminio, Ferro, e Manganese. Contenuto Totale e Frazionamento Chimico.

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    Sono riportati i metodi di laboratorio per la determinazione del contenuto totale e di varie forme chimiche (estraibili con ditionito-citrato-bicarbonato, ammonio ossalato acido, sodio pirofosfato, rame cloruro, sodio tetraborato) di quattro importanti elementi per la scienza del suolo: silicio, alluminio, ferro e manganese

    Soil genesis and evolution on calanchi (badland-like landform) of central Italy

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    Calanchi are badland-like erosional landforms, common in the Mediterranean region, which form from accelerated erosion processes. The calanchi slopes, naked or differently vegetated, can be considered as formed by different ecological tesserae originated by the mutual interaction of several factors such as erosion, geomorphology, microclimatic conditions, vegetation, ground cover, and pedogenesis. However, information about pedogenesis is rather scarce mainly because the soils developing on calanchi slopes are incessantly disturbed by erosion processes. To understand the role of soil evolution on landslide erosion,we considered three land facets each one made up of four tesserae (T1 to T4), which represented the different steps of soil and vegetal evolution of calanchi. The soil of each tesserawas described, sampled by genetic horizons, and the samples were characterized for their physical, mineralogical and chemical properties. Field observations and laboratory data suggest that pedogenesis in the calanchi badlands may progress until a critical threshold. Indeed, advanced plant colonization and solumdevelopment improve soil structure, increase soil organic matter, and favor redistribution of nutrients along the profile. The improvement of structure at depth fosters water storage and clay dispersion through soil leaching and reduction of ionic strength of the soil solution, making soil less stable. Depending on the slope gradient, the soil weight acquired during rainfall events may trigger landsliding, mudflows, or collapses that rejuvenate the surface

    Adaptive Strategy of Three Typical Plant Species Over Majella Massif (central Italy): Differences in Microbial Community and Nutrient Uptake

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    The rhizosphere represents a highly dynamic and complex interface for chemical, physical and biological interactions between plant and soil (Berg and Smalla, 2008). We report the adaptive strategy induced by the rhizosphere of three plants colonizing the high-elevated base-rich soils of Majella Massif (central Italy): Silene acaulis (L.), Dryas octopetala (L.), Helianthemum nummularium (L.) Mill. subsp. grandiflorum (Scop.). The aims of the research were to investigate the effects of these species, distinguishing between rhizospheric and bulk soil, on: (i) the main chemical characteristics (ii) the microbial community structure, abundance and activity, and (iii) the nutrient absorption strategy

    Properties, best management practices and conservation of terraced soils in Southern Europe (from Mediterranean areas to the Alps): a review.

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    Terrace soils are distinctive features of the agricultural landscape in Europe. Due to their historical and aesthetic significance, they are a resource for agriculture and tourism: however they are also a challenge for land conservation and management. Nevertheless, the fundamental role of terrace soils for agricultural quality and natural hazard prevention has not been fully investigated. In the past, terraced slopes became ideal sites for human settlement and agricultural activities. At present, they are often used for high quality crops that grow on soils with specific chemical and physical properties. The filling material used for building terraces is a human-reworked substrate, where pedogenesis occurs under a strong human influence. This leads to soils with a generally limited pedogenic development and coarse texture, although, often, with good productivity. When abandoned, terraces are subjected to progressive decay due to erosion processes and slope failures. This review focuses on terrace soil properties, conservation and management in Southern Europe. In particular, it reports some examples from the northwestern Italian Alps, where terraced slopes are characterised by ancient origin and, presently, are subjected to specific practices for their preservation. The different effects of land degradation at hill slope scale may be mitigated through appropriate management practices favoring the terrace walls maintenance, drainage optimization, and the presence of a spontaneous vegetation cover. These subjects require careful planning and conservation measures that could be collected in “best practices” guidelines for farmers, landowners and decision-makers
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