Search results for " SOIL"

showing 10 items of 774 documents

Comment on “Effects of different tillage practices on the hydraulic resistance of concentrated flow on the loess plateau in China” by J. Sun et al

2020

Abstract For concentrated flows, which are characterized by small water depth and steep sloping beds, hydraulic conditions different from those typical of streams and rivers occur. In this study a new theoretically deduced flow resistance equation was tested using the experimental data by Sun et al. for three different tilled surfaces (Manual Dibbling, MD, Manual Hoeing, MH, and Contour Drilling, CD). At first, the profile parameter-relationship, which is the relationship between the velocity profile parameter Γ, the channel slope and the flow Froude number, was calibrated using rill flow data by Di Stefano et al. Then, the applicability of this relationship was tested by the measurements o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFlow (psychology)Soil science04 agricultural and veterinary sciencesSurface finish01 natural sciencesTillageRillsymbols.namesakeFlow velocity040103 agronomy & agricultureFroude numbersymbolsCalibrationSurface roughness0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDimensional analysis Flow resistance Self-similarity Soil erosion Velocity profileGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Uso del método mejorado del uso del injerto (Isum) como herramienta para determinar el valor de factores topográficos alternativos en la estimación d…

2020

Made available in DSpace on 2020-12-12T02:01:35Z (GMT). No. of bitstreams: 0 Previous issue date: 2020-03-15 The Improved Stock Unearthing Method (ISUM) was initially designed to assess soil mobilisation rates in vineyards; however, other grafted crops such as citrus orchards could also be successfully used. The results obtained from ISUM have been used for several goals, but have not yet been applied for computing the LS factor (length and slope) as a part of the Universal Soil Loss Equation (USLE), which could give useful information to improve soil management system plans. This investigation was conducted in an 8-year old clementine field located in Canals (Valencia, Spain) and values of…

geographygeography.geographical_feature_categoryClementine cropErosive processSoil ScienceSoil scienceEnvironmental modelling04 agricultural and veterinary sciences010501 environmental sciences01 natural sciencesBulk densityRillSoil managementTillageAgricultural managementUniversal Soil Loss Equation040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSurface runoffTransectStock (geology)LS factor0105 earth and related environmental sciencesSpanish Journal of Soil Science
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A New Web-Based Catalog of Earth Degassing Sites in Italy

2008

Italy is a region characterized by intense and widespread processes of Earth degassing. High-temperature gases are released by crater plumes and fumaroles in volcanic environments throughout Italy. Also prevalent are numerous low-temperature gas emissions rich in carbon dioxide (CO2). These low-temperature emissions are located in a large area, mainly in the western sector of central and southern Italy (Figure 1).

geographygeography.geographical_feature_categoryEarth scienceGas emissionsSoil degassing - gas hazard - catalog soil manifestationsFumaroleSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundchemistryVolcanoImpact craterCarbon dioxidegas emissions in ItalyGeneral Earth and Planetary Sciencescatalogue of gas emissionsCO2 degassing; catalogue of gas emissions; gas emissions in ItalyCO2 degassingGeologyEarth (classical element)Eos, Transactions American Geophysical Union
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Fluorine speciation in topsoils of three active volcanoes of Sicily (Italy)

2008

Fluorine is one of the many environmental harmful elements released by volcanic activity. The content of total oxalate-extractable and water-extractable fluorine was determined in 96 topsoils of three active volcanic systems of southern Italy (Mt Etna, Stromboli and Vulcano). Total fluorine (F) content (F TOT) ranges from 112 to 7,430 mg kg−1, F extracted with oxalate (F OX) ranges from 16 to 2,320 mg kg−1 (2–93% of F TOT) and F extracted with distilled water ( $$ F_{{{\text{H}}_{{\text{2}}} {\text{O}}}} $$ ) ranges from 1.7 to 159 mg kg−1 (0.2–40 % of F TOT). Fluorine in the sampled topsoils derives both from the weathering of volcanic rocks and ashes and from the enhanced deposition due t…

geographygeography.geographical_feature_categoryGeneral EngineeringMineralogychemistry.chemical_elementWeatheringOxalateVolcanic rockchemistry.chemical_compoundchemistryVolcanoEnvironmental chemistrySoil waterContent (measure theory)Earth and Planetary Sciences (miscellaneous)FluorineGeneral Earth and Planetary SciencesEnvironmental ChemistryDeposition (chemistry)topo soilsGeologyGeneral Environmental ScienceWater Science and TechnologyEnvironmental Geology
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Impact of climate, soil properties and grassland cover on soil water repellency

2021

Abstract Numerous soil water repellency (SWR) studies have investigated the possible causes of this temporal phenomenon, yet there remains a lack of knowledge on the order of importance of the main driving forces of SWR in the context of changing environmental conditions under grassland ecosystems. To study the separate and combined effects of soil texture, climate, and grassland cover type on inducing or altering SWR, four sites from different climatic and soil regions were selected: Ciavolo (CI, IT), Csolyospalos (CSP, HU), Pwllpeiran (PW, UK), Sekule (SE, SK). The investigated parameters were the extent (determined by repellency indices RI, RIc and RIm) and persistence (determined by wat…

geographygeography.geographical_feature_categoryHydrophobic soilSoil textureSorptivitySoil ScienceSoil properties Soil water repellency Grass Length of dry periods Climate factors04 agricultural and veterinary sciences010501 environmental sciences01 natural sciencesSink (geography)GrasslandAgronomyHydraulic conductivitySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil fertility0105 earth and related environmental sciences
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Repercussion of anthropogenic landscape changes on pedodiversity and preservation of the pedological heritage

2013

Over a period of time people have lived in and with their surrounding landscapes and for several thousand years transformed the soilscapes and the vegetation into cultural landscape types important for their economy and to meet their needs (Richter 2007, Ellis 2011, Hjelle 2012). The sustainable provision of goods and services depends critically on managing soils without damaging the natural soilscapes and the related natural resources. To support the transition towards sustainable development, science needs to understand how land-use change affects the environment and how this, in turn, feeds back into human livelihood strategies or infl uences the vulnerability of the environment (Rounsev…

geographygeography.geographical_feature_categoryLandformSettore AGR/14 - PedologiaPhysical geographyland-use change pedotecniques antrhopogenic soils pedodiversityPedodiversity
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Early warning thresholds for partially saturated slopes in volcanic ashes

2013

Rainfall-induced landslides in steep soil slopes of volcanic origin are a major threat to human lives and infrastructure. In the context of constructing early warning systems in regions where extensive data on landslide occurrences and associated rainfall are inexistent, physically-based tools offer the possibility to establish thresholds for measurable field quantities. In this paper, a combined finite element infinite slope model is presented to study the transient hydraulic response of volcanic ash slopes to a series of rainfall events and to estimate seasonal safety factors. Furthermore, analytical considerations of partially saturated infinite slopes are made to define capillary stress…

geographygeography.geographical_feature_categorySeepage analysiWarning systemComputer Science Applications1707 Computer Vision and Pattern RecognitionContext (language use)Partially saturatedLandslideGeotechnical Engineering and Engineering GeologyComputer Science Applicationsearly warning thresholdseepage analysisPartially saturated soilslope stabilityVolcanorain infiltrationSlope stabilityvolcanic ashEarly warning systemGeomorphologyGeologyVolcanic ash
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A pedotransfer function for estimating the soil erodibility factor in Sicily

2009

The soil erodibility factor, K, of the Universal Soil Loss Equation (USLE) is a simple descriptor of the soil susceptibility to rill and interrill erosion. The original procedure for determining K needs a knowledge of soil particle size distribution (PSD), soil organic matter, OM, content, and soil structure and permeability characteristics. However, OM data are often missing and soil structure and permeability are not easily evaluated in regional analyses. The objective of this investigation was to develop a pedotransfer function (PTF) for estimating the K factor of the USLE in Sicily (south Italy) using only soil textural data. The nomograph soil erodibility factor and its associated firs…

geographygeography.geographical_feature_categorySoil textureMechanical EngineeringSoil organic matterlcsh:SBioengineeringSoil sciencelcsh:S1-972Industrial and Manufacturing EngineeringSoil gradationRilllcsh:AgricultureSoil erosion Soil erodibility Pedotransfer functionsUniversal Soil Loss EquationSoil structurePedotransfer functionErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalilcsh:Agriculture (General)Mathematics
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Soil geography and diversity of the European biogeographical regions

2013

For decades, soil geography has beenmainly a qualitative and descriptive discipline. There are nowtechnologies and mathematical tools available that allow formalizing soil geography in more quantitative terms. In this paper, the distribution and diversity of the soils of Europe are analyzed using GIS tools and pedodiversity algorithms. Soil data were taken from the European Soil Database (V2.0) and computed within the spatial framework of the Biogeographical Regions of Europe (BGRE) as defined by the European Environmental Agency (EEA) on the basis of climate and vegetation. The results obtained show the soil assemblages, including dominant soils and endemic and non-endemic soil minorities,…

geographygeography.geographical_feature_categorySteppeEcologyBiomeBiogeographical regionsSoil ScienceContext (language use)VegetationSoil typeBiodiversity hotspotEuropeSoil endemismsPedodiversityEuropean Soil DatabaseEurope Soil geography Pedodiversity Biogeographical regions Soil minorities Soil endemismsSettore AGR/14 - PedologiaSoil minoritiesPedodiversitySoil geography
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Greenhouse gas as a nutrient: methanotrophic activity in soils of hydrothermal systems

2012

Methane is the most abundant hydrocarbon in the atmosphere and a significant contributor to the radiative forcing with a global warming potential about 21 times that of CO2. Methane is released to the atmosphere by a wide number of sources, both natural and anthropogenic, with the latter being twice as large as the former. Significant amounts of geological methane, produced within the Earth’s crust (e.g. volcanic/geothermal areas), are currently released into the atmosphere (48 Tg CH4/y). Microbial oxidation in soils by methanotrophic bacteria contributes to the removal of CH4 from the atmosphere for about 3-9%. Methanotrophs belong to the Gamma- and Alpha-proteobacteria and to the recently…

geothermal soilMethanotrophySettore BIO/19 - Microbiologia GeneraleMethaneSettore GEO/08 - Geochimica E Vulcanologia
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