Search results for " eros."

showing 10 items of 418 documents

A coupled eco-hydro-geomorphic investigation of basin response to climate change: Examining the role of climate on internal basin dynamics

2009

Much attention has been devoted to assessing the relationship between changes in climate and landscape evolution. Given the complexity of dependence of geomorphic processes on hydrological and vegetation properties of the system, it is not surprising that different studies of fluvial response to climate change often appear contradictory, making difficult to generalize about how any given drainage basin will respond to changes in climate and/or land use. In this study, an integrated geomorphic component of the physically-based, spatially distributed hydrological model, tRIBS, the TIN-based Real-time Integrated Basin Simulator, is used to analyze the sensitivity of landscapes to climate chang…

Hydrology Climate impacts Erosion GeomorphologySettore ICAR/02 - Costruzioni Idrauliche E Marittime E Idrologia
researchProduct

Using a physically-based model, tRIBS-Erosion, for investigating the effects of climate change in semi-arid headwater basins.

2013

Soil erosion due to rainfall detachment and flow entrainment of soil particles is a physical process responsible for a continuous evolution of landscapes. The rate and spatial distribution of this phenomenon depend on several factors such as climate, hydrologic regime, geomorphic characteristics, and vegetation of a basin. Many studies have demonstrated that climate-erosion linkage in particular influences basin sediment yield and landscape morphology. Although soil erosion rates are expected to change in response to climate, these changes can be highly non-linear and thus require mechanistic understanding of underlying causes. In this study, an integrated geomorphic component of the physic…

Hydrology Soil erosion Climate change
researchProduct

Effects of climate, land cover and topography on soil erosion risk in a semiarid basin of the Andes

2016

Understanding soil erosion processes in the Ecuadorian Andes with a tropical wet-dry climate and a variable topography, is fundamental for research on agriculture sustainable, environmental management, as well as for a stable water supply for the local populations. This work proposes method to estimate soil erosion risk in the semiarid Catamayo basin with limited data. The results show that the rainfall distribution and the erosivity along with the rugged topography, followed by the land cover (C-factor), are the most important factors to estimate soil erosion risk. The soil erodibility is the most important factor in the dry season for agricultural areas and where the ground cover is spars…

Hydrology010504 meteorology & atmospheric sciencesAgroforestrySoil biodiversityClimatedrylandlandform04 agricultural and veterinary sciencesVegetationLand cover01 natural sciencesC-factorSoil retrogression and degradation040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceDryland salinityWEPPSurface runoffSoil conservationsoil erosion riskEcuadorian Andes0105 earth and related environmental sciencesEarth-Surface ProcessesCATENA
researchProduct

Soil erosion susceptibility assessment and validation using a geostatistical multivariate approach: a test in southern Sicily

2008

A certain number of studies have been carried out in recent years that aim at developing and applying a model capable of assessing water erosion of soil. Some of these have tried to quantitatively evaluate the volumes of soil loss, while others have focused their efforts on the recognition of the areas most prone to water erosion processes. This article presents the results of a research whose objective was that of evaluating water erosion susceptibility in a Sicilian watershed: the Naro river basin. A geomorphological study was carried out to recognize the water erosion landforms and define a set of parameters expressing both the intensity of hydraulic forces and the resistance of rocks/so…

HydrologyAtmospheric SciencegeographyHydrogeologygeography.geographical_feature_categorySoil textureLandformBedrockWater erosion GIS Multivariate statistical analysis Validation Naro river basin Southern Italy SicilySoil waterEarth and Planetary Sciences (miscellaneous)ErosionSurface runoffStream powerGeologyWater Science and Technology
researchProduct

MANUAL SAMPLING AND TANK SIZE EFFECTS ON THE CALIBRATION CURVE OF PLOT SEDIMENT STORAGE TANKS

2004

In many experimental soil erosion plots, runoff is collected and carried by a conveyance system to a sequence of storage tanks. If the soil loss is measured by collecting, after mixing, samples of the stored suspension, then a calibration curve between the actual mean concentration (C) and the measured concentration (Cm) in the storage tank occurs. The aim of this article was to evaluate experimentally the factors affecting the relationship between C and Cm. For a sandy loam soil, the replicated measurements of Cm (20 samples) for two values of the actual concentration (C = 5 and 25 g/L) showed that the variability of the measurements of Cm is low and confirmed the reliability of a calibrat…

HydrologyCalibration curveLoamStorage tankCalibrationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSampling (statistics)SedimentSurface runoffAgricultural and Biological Sciences (miscellaneous)Calibration Sediment concentration Soil erosion measurement Soil erosion plotWater levelTransactions of the ASAE
researchProduct

Carbon input threshold for soil carbon budget optimization in eroding vineyards

2016

Abstract Previous studies have documented that, relative to conventional tillage (CT), alternative soil management (reduced tillage, mulching, or cover crops) decreases soil erosion and increases soil organic matter (SOM) in vineyards. These previous studies, however, failed to consider the loss of soil organic carbon (SOC) with erosion that could occur with the adoption of agro-environmental measures (AEM) in a semiarid environment. Accordingly, the aims of this study were to determine whether changes in SOC content under AEM management are always positive and to develop a conceptual model for estimating the “SOC threshold”. The SOC threshold was defined as that level of SOC in an AEM-mana…

HydrologyConventional tillageSoil organic matterAgro-environmental measureSoil ScienceSoil science04 agricultural and veterinary sciencesSoil carbon010501 environmental sciencesAgro-environmental measure; Degradation; Organic carbon; Soil erosion; Soil Science01 natural sciencesSettore AGR/02 - Agronomia E Coltivazioni ErbaceeMinimum tillageSoil managementTillageDegradation040103 agronomy & agricultureErosionSoil erosion0401 agriculture forestry and fisheriesEnvironmental scienceCover cropOrganic carbon0105 earth and related environmental sciences
researchProduct

European small portable rainfall simulators: A comparison of rainfall characteristics

2013

28 páginas, 6 figuras, 2 tablas.- The definitive version is available on: http://www.sciencedirect.com/science/article/pii/S0341816213001252

HydrologyDrop sizeDrop (liquid)Rainfall simulator comparisonSpatial rainfall distributionBodemfysica en LandbeheerSpatial distributionRainfall simulationSoil Physics and Land ManagementDrop velocityProcess dynamicsErosionEnvironmental scienceResearch questionsPrecipitationDrop sizeWater erosionKinetic energyEarth-Surface ProcessesCATENA
researchProduct

Predicting event soil loss from bare plots at two Italian sites

2013

Abstract Including runoff in USLE-type empirical models is expected to improve plot soil loss prediction at the event temporal scale and literature yields encouraging signs of the possibility to simply estimate runoff at these spatial and temporal scales. The objective of this paper was to develop an estimating procedure of event soil loss from bare plots (length = 11–44 m, slope steepness = 14.9–16.0%) at two Italian sites, i.e. Masse, in Umbria, and Sparacia, in Sicily, having a similar sand content (5–7%) but different silt (33% at Sparacia, 59% at Masse) and clay (62% and 34%, respectively) contents. A test of alternative erosivity indices for the Masse station showed that the best perf…

HydrologyEmpirical modellingSoil scienceSiltSoil water erosion Soil loss prediction Empirical models USLE-MUSLE-MMSoil lossEmpirical modelSoil loss predictionEmpirical modelsErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliUSLE-MUSLE-MMEnvironmental scienceSoil water erosionTemporal scalesSurface runoffScale (map)Earth-Surface ProcessesEvent (probability theory)CATENA
researchProduct

Data Mining Technique (Maximum Entropy Model) for Mapping Gully Erosion Susceptibility in the Gorganrood Watershed, Iran

2019

Soil erosion is a serious problem affecting most of the countries. This study was carried out in Gorganrood Watershed (Iran), which extends for 10,197 km2 and is severely affected by gully erosion. A gully headcut inven- tory map consisting of 307 gully headcut points was provided by Google Earth images, field surveys, and national reports. Gully conditioning factors including sig- nificant geo-environmental and morphometric variables were selected as predictors. Maximum entropy (ME) model was exploited to model gully susceptibility, whereas the area under the ROC curve (AUC) and draw- ing receiver operating characteristic (ROC) curves were employed to evaluate the performance of the model.…

HydrologyGully erosion Susceptibility Geographic information systems (GIS) Maximum entropy (ME) model Area under the ROC curve (AUC)WatershedReceiver operating characteristicPrinciple of maximum entropySettore GEO/04 - Geografia Fisica E GeomorfologiaGully erosionArea under the roc curveSettore GEO/05 - Geologia ApplicataGeology
researchProduct

Comparing theoretically supported rainfall-runoff erosivity factors at the Sparacia (South Italy) experimental site

2018

Interpreting rainfall‐runoff erosivity by a process‐oriented scheme allows to conjugate the physical approach to soil loss estimate with the empirical one. Including the effect of runoff in the model permits to distinguish between detachment and transport in the soil erosion process. In this paper, at first, a general definition of the rainfall‐runoff erosivity factor REFe including the power of both event runoff coefficient QR and event rainfall erosivity index EI30 of the Universal Soil Loss Equation (USLE) is proposed. The REFe factor is applicable to all USLE‐based models (USLE, Modified USLE [USLE‐M] and Modified USLE‐M [USLE‐MM]) and it allows to distinguish between purely empirical m…

HydrologyRainfall runoffplot measurements rainfall‐runoff erosivity soil erosion USLE‐M0208 environmental biotechnology040103 agronomy & agricultureSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0401 agriculture forestry and fisheriesEnvironmental science04 agricultural and veterinary sciences02 engineering and technology020801 environmental engineeringWater Science and TechnologyHydrological Processes
researchProduct