Search results for "Water table"

showing 10 items of 27 documents

Global Groundwater-Vegetation Relations

2017

Groundwater is an integral component of the water cycle, and it also influences the carbon cycle by supplying moisture to ecosystems. However, the extent and determinants of groundwater-vegetation interactions are poorly understood at the global scale. Using several high-resolution data products, we show that the spatial patterns of ecosystem gross primary productivity and groundwater table depth are correlated during at least one season in more than two-thirds of the global vegetated area. Positive relationships, i.e., larger productivity under shallower groundwater table, predominate in moisture-limited dry to mesic conditions with herbaceous and shrub vegetation. Negative relationships, …

010504 meteorology & atmospheric sciencesWater table0208 environmental biotechnology02 engineering and technologyecohydrological patterns01 natural sciencesgroundwaterEcosystemWater cycleplant productivity0105 earth and related environmental sciencesHydrologyecosystemVegetation15. Life on land6. Clean water020801 environmental engineeringGeophysicsProductivity (ecology)13. Climate actionSpatial ecologyGeneral Earth and Planetary SciencesEnvironmental scienceGroundwaterWater usespatial covariation
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Methane production and oxidation potentials in relation to water table fluctuations in two boreal mires

1999

We studied the response of methane production and oxidation potentials in a minerotrophic and an ombrotrophic mire to water table fluctuations. In profiles where water table had not varied, the water-saturated layers showed significant potentials while the unsaturated layers did not. The production potentials in the saturated layers below water level ranged from 0.1 to 2.4 m gC H4 h ˇ1 (g d.w.) ˇ 1 and oxidation potentials (first order reaction rate constants) betweenˇ0.010 andˇ0.120 h ˇ1 (g d.w.) ˇ 1 . In profiles with constant water level, the maximal production potential occurred 20 cm and maximal oxidation potential 10 cm below water level. When water table varied only a little, product…

010504 meteorology & atmospheric sciencesbiologyWater tableMinerotrophicMethanogenesisEcologySoil ScienceOmbrotrophic04 agricultural and veterinary sciences15. Life on landbiology.organism_classification01 natural sciencesMicrobiologySphagnumMethaneCarbon cycleWater levelchemistry.chemical_compoundchemistryEnvironmental chemistry040103 agronomy & agriculture0401 agriculture forestry and fisheries0105 earth and related environmental sciencesSoil Biology and Biochemistry
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Roman Rhine settlement dynamics evidenced by coin distribution in a fluvial environment (Oedenburg, Upper Rhine, France).

2008

International audience; On the basis of archaeological and alluvial records, this paper presents the first spatial analysis of artefacts in relation to the evolution of the Rhine River, at the Gallo-Roman site of Oedenburg, during the first four centuries AD. The dataset consisted of several thousand Roman artefacts found by pedestrian prospecting over the last twenty years, over half of which were coins. This dataset was used together with high-resolution topography and geomagnetic mapping, to reconstruct settlement evolution, both on the terrace and in the floodplain. A comprehensive monetary chart has been compiled for the Oedenburg site, which highlights four major phases of settlement.…

010506 paleontologyArcheologyFloodplain[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryTerrace (agriculture)Water tableFluvialContext (language use)01 natural sciences[SHS]Humanities and Social Sciences[ SHS ] Humanities and Social SciencesClimate change0601 history and archaeologyGeoarchaeology0105 earth and related environmental sciencesPalynologygeographygeography.geographical_feature_category060102 archaeologyRhine River06 humanities and the artsRoman Period15. Life on landArchaeologyFluvial impact[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryPeriod (geology)AlluviumCoin distribution
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How warm? How wet? Hydroclimate reconstruction of the past 7500 years in northern Carpathians, Romania

2017

Abstract As natural and anthropogenic ecosystems are dependent on the local water availability, understanding past changes in hydroclimate represents a priority in research concerning past climate variability. Here, we used testate amoebae (TA) and chironomid analysis on a radiocarbon dated complex of small pond and peat bog sediment profiles from an ombrotrophic bog (Taul Muced, northern Carpathians, Romania) to quantitatively determine major hydrological changes and July air temperature over the last 7500 years. Wet mire surface conditions with a pH between 2.3 and 4.5 were inferred for the periods 4500–2700 and 1300–400 cal yr BP by the occurrence of Archerella flavum , Amphitrema wright…

010506 paleontologygeographyPeatgeography.geographical_feature_category010504 meteorology & atmospheric sciencesWater tablePaleontologyOmbrotrophic580 Plants (Botany)Oceanography01 natural sciencesMireClimatologyDominance (ecology)Physical geographyTestate amoebaeBogEcology Evolution Behavior and SystematicsHoloceneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Magma Degassing at Piton de la Fournaise Volcano

2015

Since about 1860 AD, magmatic gas release at Piton de la Fournaise volcano is very weak during intra-eruptive phases and essentially occurs during the relatively short-lived eruptions. Recent gas measurements performed during an eruption in October 2010, combined with detailed review of melt and fluid inclusion composition in magmas erupted over the past 50 kyrs, indicate that most PdF eruptions extrude magmas having variably degassed at shallow depth (P 1 kbar) and the shallow magmas, whose fluids are efficiently scrubbed by the hydrothermal system and the water table. Quantification of SO2 fluxes permits to track syn-eruptive magma ascent at shallow level (above sea level). Deeper exsolut…

Below sea levelgeographygeography.geographical_feature_categoryVolcanoWater tableEarth scienceMagmaGas releaseInclusion (mineral)PetrologySea levelGeologyHydrothermal circulation
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Geochemical classification of groundwater using multivariate statistical analysis in Latvia

2016

Multivariate statistical methods – principal component analysis (PCA) and hierarchical cluster analysis (HCA) – are applied to identify geochemically distinct groundwater groups in the territory of Latvia. The main processes observed to be responsible for groundwater chemical composition are carbonate and gypsum dissolution, fresh and saltwater mixing and ion exchange. On the basis of major ion concentrations, eight clusters (C1–C8) are identified. C6 is interpreted as recharge water not in equilibrium with most sediment forming minerals. Water table aquifers affected by diffuse agricultural influences are found in C3. Groundwater in C4 reflects brine or seawater admixture and gypsum dissol…

Calcite010506 paleontologygeographygeography.geographical_feature_categoryWater tableDolomiteMineralogyWeatheringAquiferGroundwater recharge010501 environmental sciences01 natural scienceschemistry.chemical_compoundchemistryCarbonateGeologyGroundwater0105 earth and related environmental sciencesWater Science and TechnologyHydrology Research
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Estimation of the water table depth of the Calarasi district Island (Romania) at the Danube River using ASTER/DEM data

2014

The water table is the top level of ground water by definition. Therefore surface water is an exposed part of the water table. Airborne measurements, resistivimeters determinations or perforation analyses can be used to determine the water table depth. These methods require, approximately, taking a sample per hectare, which is a very expensive and time-consuming procedure. However, remote sensing constitutes an ideal alternative to determine water table depth, because unlike the existing methodologies, which are very expensive due to equipment and travel expenses, the proposed methodology is cheap and simple. The ASTER GDEM data is available at no charge to users via electronic download and…

HydrologyAtmospheric Science010504 meteorology & atmospheric sciencesbiologyWater tableApplied MathematicsPerforation (oil well)0211 other engineering and technologies02 engineering and technologybiology.organism_classification01 natural sciencesAltitudeGeographyRemote sensing (archaeology)Computers in Earth SciencesAster (genus)Scale (map)Surface waterGroundwater021101 geological & geomatics engineering0105 earth and related environmental sciencesGeneral Environmental ScienceEuropean Journal of Remote Sensing
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Wheat growth simulation and yield prediction with seasonal forecasts and a numerical model

2007

Abstract Wheat is a major winter crop in northern Italy. Italian agricultural markets and government agencies would undoubtedly benefit from the early availability of wheat yield forecasts at the regional and national scales as useful support in decision making. In this study we tested the skill of seasonal weather forecasts, in combination with observed weather data, as input to a crop model working in water limited conditions. The observations were used to simulate wheat growth from sowing up to 2 months before harvest, while seasonal forecasts were used afterwards to predict final yields. Observations included climatic variables and water table levels from a location in the Po river plai…

HydrologyAtmospheric ScienceGlobal and Planetary ChangeWater tablebusiness.industryWater flowYield (finance)SowingForestrySeasonalitymedicine.diseaseAgricultureClimatologymedicineEnvironmental sciencebusinessScale (map)Agronomy and Crop ScienceDownscalingAgricultural and Forest Meteorology
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Changes in Pore Water Quality After Peatland Restoration: Assessment of a Large-Scale, Replicated Before-After-Control-Impact Study in Finland

2017

Drainage is known to affect peatland natural hydrology and water quality, but peatland restoration is considered to ameliorate peatland degradation. Using a replicated BACIPS (Before-After-Control-Impact Paired Series) design, we investigated 24 peatlands, all drained for forestry and subsequently restored, and 19 pristine control boreal peatlands with high temporal and spatial resolution data on hydroclimate and pore water quality. In drained conditions, total nitrogen (Ntot), total phosphorus (Ptot), and dissolved organic carbon (DOC) in pore water were several-fold higher than observed at pristine control sites, highlighting the impacts of long-term drainage on pore water quality. In gen…

HydrologyPeat010504 meteorology & atmospheric sciencesWater table010501 environmental sciences01 natural sciencesPore water pressureNutrientHydrology (agriculture)Dissolved organic carbonEnvironmental scienceWater qualityDrainage0105 earth and related environmental sciencesWater Science and TechnologyWater Resources Research
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Effects of initialization on response of a fully-distributed hydrologic model

2008

Summary Knowledge of initial conditions is very important to correctly model the basin response at the storm event scale. Of particular interest is the influence of topography and soil type on the principal hydrologic variables and runoff generation mechanisms as a function of antecedent wetness conditions. This study addresses the influence of initial states on the short-term hydrologic response and characterizes the effects of topography and soils on the dissipation of the influence of the initialization conditions. Two case studies are considered: a synthetic two-dimensional planar hillslope with various assumed slope magnitudes and soil types; and a real basin (∼800 km2) with actual lan…

HydrologyWatershedWater tableflood forecastingSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaFlood forecastingInitializationSoil sciencedistributed hydrologic modelinginitial conditionVadose zoneSoil watersurface-subsurface interactionsEnvironmental sciencePrecipitationSurface runoffWater Science and TechnologyJournal of Hydrology
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