Search results for "erosion"

showing 10 items of 637 documents

Nestriktās matemātikas morfoloģijas operatori: teorijas pamati un operatoru realizācija konkrētiem konjuktoru-implikatoru pāriem

2021

Maģistra darbā apskatīti matemātiskās morfoloģijas pamatoperatoru - dilācija, erozija, atvēršana, slēgšana - paplašinājumi nestriktās kopās. Vispārīga nestrikta morfoloģijas operatora definīcija realizēta konkrētiem konjunktoru-implikātoru pāriem. Operatoru realizācijā par konjunktoriem izvēlētas minimuma, reizinājuma un Lukasieviča t-normas un par implikatoriem - tām atbilstošie rezidiji un Klīnī-Dinesa implikācija. Konkrētie konjunktoru-implikatoru pāriem iegūtie operatori ilustrēti ar vizuāliem piemēriem, to realizācijai izstrādāta arī lietojumprogramma. Veikta iegūto rezultātu analīze.

fuzzy setMatemātikaopeningdilationerosionfuzzy mathematical morphology
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Assessing dye-tracer technique for rill flow velocity measurements

2018

Abstract Rill erosion is considered one of the most important processes affecting soil because of the large amount of soil loss. The rill network acts as sediment source and is able to transport both rill flow-detached particles and those delivered from the interrill areas. Small flow depth in a rill and steep slope values of its bed affect significantly flow hydraulics. When rill flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measured surface velocity of the leading edge of the tracer plume by a correction factor. The main uncertainty of the dye-tracing technique stands in the relationship between mean and surface flow velocity. In …

geographyLeading edgegeography.geographical_feature_categoryCorrection factorDye methodHydraulics0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyDarcy–Weisbach equation020801 environmental engineeringPlumelaw.inventionRillFlow velocityFlow resistanceFlow velocitylawTRACERRill flowSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeologyEarth-Surface Processes
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Modelling of piping collapses and gully headcut landforms: Evaluating topographic variables from different types of DEM

2021

Abstract The geomorphic studies are extremely dependent on the quality and spatial resolution of digital elevation model (DEM) data. The unique terrain characteristics of a particular landscape are derived from DEM, which are responsible for initiation and development of ephemeral gullies. As the topographic features of an area significantly influences on the erosive power of the water flow, it is an important task the extraction of terrain features from DEM to properly research gully erosion. Alongside, topography is highly correlated with other geo-environmental factors i.e. geology, climate, soil types, vegetation density and floristic composition, runoff generation, which ultimately inf…

geographyQE1-996.5geography.geographical_feature_category010504 meteorology & atmospheric sciencesAdvanced land observation satellite (ALOS)Water flowLandformCforestGully erosion susceptibility (GES)ElevationElastic netTerrainCubistGeologyVegetation010502 geochemistry & geophysics01 natural sciencesAdvanced Spaceborne Thermal Emission and Reflection RadiometerGeneral Earth and Planetary SciencesSurface runoffDigital elevation modelGeomorphologyDigital elevation model (DEM)Geology0105 earth and related environmental sciencesGeoscience Frontiers
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Badlands in the Tabernas Basin, Betic Chain

2014

The complex badland landscape at Tabernas results from a combination of relief amplitude generated by tectonic uplift since the Pliocene and reactivated several times during the Pleistocene, the properties of the Tortonian sedimentary rocks and a predominantly arid climate. The landscape is dominated by deep incision of the main river systems, which continues in part of the headwater tributaries, and characterized by contrasting slope morphologies and a variety of microecosystems. The Tabernas badlands exhibit a diversity of landforms resulting from the combination of multi-age soil surface components that allow a variety of processes to operate at different rates. These are dominated by ri…

geographyTectonic upliftgeography.geographical_feature_categoryPleistoceneLandformTributaryErosionSedimentary rockStructural basinSurface runoffGeomorphologyGeology
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Improved discrimination of subglacial and periglacial erosion using10Be concentration measurements in subglacial and supraglacial sediment load of th…

2015

Deciphering the complex interplays between climate, uplift and erosion is not straightforward and estimating present-day erosion rates can provide useful insights. Glaciers are thought to be powerful erosional agents, but most published ‘glacial’ erosion rates combine periglacial, subglacial and proglacial erosion processes. Within a glaciated catchment, sediments found in subglacial streams originate either from glacial erosion of substratum or from the rock walls above the glacier that contribute to the supraglacial load. Terrestrial cosmogenic nuclides (TCN) are produced by interactions between cosmic ray particles and element targets at the surface of the Earth, but their concentration …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBedrockGeography Planning and DevelopmentSedimentGlacier15. Life on land010502 geochemistry & geophysics01 natural sciencesSubglacial stream13. Climate actionEarth and Planetary Sciences (miscellaneous)Subglacial eruptionErosionGlacial periodCosmogenic nuclideGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEarth Surface Processes and Landforms
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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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Late Paleozoic Ice Age glaciers shaped East Antarctica landscape

2019

International audience; The erosion history of Antarctica is fundamental to our understanding of interlinks between climate and glacier dynamics. However, because of the vast polar ice sheet covering more than 99% of Antarctica land mass, the continental surface response to glacial erosion remains largely unknown. Over the last decade the subglacial topography of Antarctica has been imaged by airborne radar surveys. These studies revealed high and complex sub-glacial relief in the core of the East Antarctic shield, interpreted as resulting from rifting episodes and low long-term erosion rates, or repeated large-scale glacial retreats and advances. In East Antarctica, thermochronology studie…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesPermianGlacier010502 geochemistry & geophysics01 natural sciencesThermochronologyPaleontologyGeophysicsDenudation13. Climate actionSpace and Planetary ScienceGeochemistry and Petrology[SDU]Sciences of the Universe [physics]Earth and Planetary Sciences (miscellaneous)Ice ageErosionGlacial period[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentCenozoicGeology0105 earth and related environmental sciences
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LA-ICP-MS analyses on coral growth increments reveal heavy winter rain in the Eastern Mediterranean at 9 Ma

2009

Abstract Sediment particles incorporated into coral skeletons reflect variation in composition and amount of suspended material in ambient water during coral growth. They can be used to identify periods of enhanced storm frequency and associated freshwater discharge. Tortonian (Late Miocene) Porites corals from Crete (Aegean Sea, Eastern Mediterranean) show pronounced annual density bands in X-ray photographs. δ18O compositional variability reflects the annual banding equivalent with a ~ 7 °C annual sea surface temperature (SST) cycle over a seven-year period. Fine sediment particles are concentrated in layers with skeletal porosity parallel to growth increments. Variations in the chemical …

geographygeography.geographical_feature_categoryCoralAragoniteTrace elementPaleontologySedimentLate MioceneMineral dustengineering.materialOceanographyOceanographyErosionengineeringReefEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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La reserva de semillas en una cuenca de "badlands" (Petrer, Alicante)

1992

In order to determine the influence of erosion in the absence of vegetation of badlands slopes, the seed content of the regolith and the seed removal by runoff in five storms were analyzed in an experimental catchment at Petrer (Alicante). Both, seed redistribution and seed loss were detected, but these seem to be insufficient to explain the lack of vegetation. It is hypothesized that besides the erosion process, factors such as pedoclimate, and chemical and physical properties of the regolith should be considered.

geographygeography.geographical_feature_categoryEcologySoil seed bankDrainage basinfood and beveragesForestrybadlandsVegetationalicante (spain)erosionRegolithlcsh:QH540-549.5ErosionSoil seed bank; badlands; erosion; Alicante (Spain)Environmental sciencelcsh:Ecologysoil seed bankSurface runoffAlicante (Spain)Ecology Evolution Behavior and SystematicsQH540-549.5
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Erosion and stabilisation sequences in relation to base level changes in the El Cautivo badlands, SE Spain

2008

Abstract The complex multiple-age badlands at El Cautivo are cut in upper Miocene marls of the uplifted and dissected Tabernas Basin, Almeria, in semi-arid SE Spain. Previous work identified six episodes of erosion and subsequent stabilisation, with ages ranging from the late Pleistocene to the present day. This paper uses newly-acquired digital elevation models, orthorectified aerial photographs, and field survey data to illustrate the development sequence of a series of gullies which drain into the Rambla de Tabernas. Changing drainage directions and phases of incision and stabilisation are related to the filling and subsequent dissection of the Tabernas lower lake sediments, differential…

geographygeography.geographical_feature_categoryLandformAggradationBedrockPediment (geology)TributaryErosionDrainage basinRavineGeomorphologyGeologyEarth-Surface ProcessesGeomorphology
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