Search results for "Thermal"

showing 10 items of 3576 documents

Shelter and remotely sensed night temperatures in orange groves

1991

In previous papers we have used a linear regression approach for determining nocturnal air temperature in orange groves from satellite thermal data. However, this procedure has a poor precision (≈ 2 °C) for applications such as frost forecasting. For this reason a theoretical method has been proposed, which is based on the following assumptions: (1) the air temperature (Ta) is the result of the convective heat exchange between ground and air, and between air and orange trees, and (2) the remotely-sensed temperature (T) can be expressed as a function of ground (Tg) and orange tree (Ts) temperatures. So the relationshipT = Ta + (ag − α) (Tg − Ts) has been derived, wherea = (1 +h2πR/h1L)−1 and…

HydrologyAtmospheric ScienceMaterials scienceConvective heat transferThermalEmissivityAnalytical chemistryHeat transfer coefficientOrange (colour)Temperature measurementFruit treeCitrus × sinensisTheoretical and Applied Climatology
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Critical analysis of empirical ground heat flux equations on a cereal field using micrometeorological data

2009

The rate at which the net radiation is transferred to the soil as ground heat flux varies with surface characteristics. Surface energy balance algorithms use empirical relationships taking into account the effects of the canopy cover to insulate the soil through vegetation indexes, the soil capacity to absorb incoming net radiation via the albedo, and the surface temperature promoting the energy transfer. However empirical relationships are often dependent on local conditions, such as the soil humidity and vegetation type. Ground heat flux assumes a minimum value in case of full canopy cover and a maximum value for dry bare soil. Aim of the present research is the critical analysis of some …

HydrologyEnergy balanceHumidityVegetationAlbedoAtmospheric sciencesSurface energy balanceSoil thermal propertiesGeographyHeat fluxSoil heat fluxMicrometeorological measurementsEvapotranspirationVegetation typesoil heat flux surface energy balance micrometeorological measurements.SPIE Proceedings
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Methodological approach for evaluating the geo-exchange potential: VIGOR Project

2012

In the framework of VIGOR Project, a national project coordinated by the Institute of Geosciences and Earth Resources (CNR-IGG) and sponsored by the Ministry of Economic Development (MiSE), dedicated to the evaluation of geothermal potential in the regions of the Convergence Objective in Italy (Puglia, Calabria, Campania and Sicily), is expected to evaluate the ability of the territory to heat exchange with the ground for air conditioning of buildings. To identify the conditions for the development of low enthalpy geothermal systems collected and organized on a regional scale geological and stratigraphic data useful for the preparation of a specific thematic mapping, able to represent in a …

HydrologyEnvironmental EngineeringHydrogeologybusiness.industrymedia_common.quotation_subjectlcsh:QE1-996.5Geotechnical Engineering and Engineering GeologyCivil engineeringlcsh:GeologyGeophysicsThematic mapgeo-exchange thermophysical properties conceptual model Southern ItalyAir conditioningGeothermal heat pumpConceptual modelEnvironmental ChemistryScale (map)businessZoningGeothermal gradientGeologyWater Science and Technologymedia_commonAcque Sotterranee
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Mapping burns and natural reforestation using thematic Mapper data

1991

Abstract Remote sensing techniques are specially suitable to detect and to map areas affected by forest fires. In this work, Landsat 5 Thematic Mapper (TM) data has been used to study a number of forest fires that occurred in the province of Valencia (Spain) and to monitor the vegetation regeneration over burnt areas. A reference area (non‐burnt forest) was established to assess the change produced by fire. The radiance in the thermal band (10.4–12.5 μm) and the normalized difference in reflectance between near 1R (0.76–0.90 μm) and middle IR (2.08–2.35 μm) were the most suitable parameters to map burnt areas. This index can also be used for monitoring vegetation regeneration in burnt areas…

HydrologyGeographyThematic MapperThermal bandGeography Planning and DevelopmentRadianceReforestationForestryEnhanced vegetation indexVegetationVegetation IndexReflectivityWater Science and TechnologyGeocarto International
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Estimating Maize (Zea mays) cvapotranspiration from NOAA-AVHRR thermal data in the Albacete area, Spain

1994

Abstract We have estimated evapotranspiration from maize (Zca mays) using NOAA thermal images infrared and meteorological data, by means of the relation where Ed is the daily evapotranspiration, is the daily net radiation expressed in mm of water per day, (Ta−Ts)i is the temperature difference between air and corn surface obtained near midday, and Bi is a semi-empirical constant which has been calculated as 0·53±0·10mm day−1K−1. We have tested the method obtaining actual daily evapotranspiration of maize with an acceptable precision (±0·9 mm day−1 taken Penman's method as the standard). Finally, a practical example is included, in which the different steps followed for applying the develope…

HydrologyIrrigationRadiometerEvapotranspirationNet radiationThermalGeneral Earth and Planetary SciencesEnvironmental scienceTemperature differenceZea maysMeteorological satelliteInternational Journal of Remote Sensing
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Quantification of deep CO2 fluxes from Central Italy. Examples of carbon balance for regional aquifers and of soil diffuse degassing.

1999

Abstract In Central Italy non-volcanic CO 2 is discharged by focused degassing (strong diffuse emission and vents) and by high-CO 2 groundwater. 3 He / 4 He data and the carbon isotopic composition of CO 2 are compatible with derivation from mantle degassing and/or metamorphic decarbonation. The gases produced at depth accumulate in permeable reservoirs composed of Mesozoic carbonates. When total pressure (roughly corresponding to p CO 2 ) of the reservoir fluid exceeds hydrostatic pressure, a free gas phase forms gas reservoirs within the permeable host rocks from which gases may escape toward the surface. This process generates both the focused vents and the CO 2 -rich springs which chara…

HydrologygeographyHydrogeologygeography.geographical_feature_categoryHydrostatic pressureGeochemistryGeologyAquiferMantle (geology)Hydrothermal circulationchemistry.chemical_compoundchemistryGeochemistry and PetrologyCarbon dioxideCarbonateGroundwaterGeology
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The role of the aquifer in soil CO2 degassing in volcanic peripheral areas: A case study of Stromboli Island (Italy)

2017

Abstract The peripheral area of Stromboli Island, Italy, named “Scari”, was continuously studied between January 2009 and December 2010. Data on soil CO 2 flux and the partial pressure of CO 2 (pCO 2 ) in equilibrium with the thermal aquifer linked to the magmatic system are presented. Soil CO 2 fluxes range from 20 to 370 g m − 2  d − 1 and have been strongly affected by soil temperature variations. Soil CO 2 flux data were filtered with respect to the soil temperature and the calculated values, called “residuals”, were considered to detect changes induced by the magmatic system. The pCO 2 values change in a wide range from 0.03 to 0.6 (atm), showing rapid variations. The results of this s…

Hydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences2GeologySoil scienceAquiferin waterPartial pressure010502 geochemistry & geophysics01 natural sciencesfluxVolcano-hydrothermal systemSoil temperatureFlux (metallurgy)VolcanoGeochemistry and PetrologypCOMagmaSoil COGeologyGas-water interaction0105 earth and related environmental sciencesChemical Geology
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Total (fumarolic + diffuse soil) CO2 output from Furnas volcano

2015

Furnas volcano, in São Miguel island (Azores), being the surface expression of rising hydrothermal steam, is the site of intense carbon dioxide (CO2) release by diffuse degassing and fumaroles. While the diffusive CO2 output has long (since the early 1990s) been characterized by soil CO2 surveys, no information is presently available on the fumarolic CO2 output. Here, we performed (in August 2014) a study in which soil CO2 degassing survey was combined for the first time with the measurement of the fumarolic CO2 flux. The results were achieved by using a GasFinder 2.0 tunable diode laser. Our measurements were performed in two degassing sites at Furnas volcano (Furnas Lake and Furnas Villag…

Hydrologygeographygeography.geographical_feature_categoryFurnas volcanoFull PaperSoil diffuse degassingCo2 fluxMineralogyCarbon dioxide fluxGeologyFumarolesFumaroleFumaroleHydrothermal circulationSettore GEO/08 - Geochimica E VulcanologiaSoil co2 fluxchemistry.chemical_compoundchemistryVolcano13. Climate actionSpace and Planetary ScienceSoil waterCarbon dioxideSurface expressionGeologyEarth, Planets, and Space
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Volcanic steam output directly measured in fumaroles: the observed variations at Vulcano Island, Italy, between 1983 and 1987

1992

The mass of steam emitted by the fumaroles of the crater of Vulcano (Aeolian Islands, Italy) was evaluated by using a direct measuring method. Measurements were effected with this method between 1983 and 1987 in nine field campaigns, the results of which are given in this paper. The steam flux measurements were performed by an instrument expressly designed for steam condensation. The estimates of the thermal energy transported daily by the steam gave values of up to 10E12 J. The sharp variations in the total mass outputs recorded in 1984 and 1985 are here interpreted as being a consequence of the probable accumulation of fluid pressure at depth, during the evolution of volcanic activity. Th…

Hydrologygeographygeography.geographical_feature_categorybusiness.industryGeothermal energyMineralogyFluxFumaroleGeothermal explorationVolcanoImpact craterGeochemistry and PetrologyMagmabusinessGeologyThermal energyBulletin of Volcanology
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Fumarolic alteration products at Sousaki (Greece) : occurrence and environmental impact

2009

Fumarolic alteration crusts and efflorescences have been sampled at the Sousaki solfataric field. Samples have been analysed for mineralogical (XRD) and chemical composition (HNO3 digestion and leaching with distilled water). Results show that mineralogical and chemical compositions (major, minor and trace metals) are controlled by microenvironmental conditions. The sample collected in the anoxic part of a cave is composed almost exclusively by native sulfur. The samples collected in the oxidizing part of the cave and outside in relatively sheltered position are mainly composed by very soluble sulfates. Chemical composition evidence strong enrichments in Al, Ca, Cr, Fe, Mg and Ni which are …

Hydrothermal alteration productelementstoxic metalsulfateSettore GEO/08 - Geochimica E Vulcanologia
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