Search results for "forest"

showing 10 items of 3780 documents

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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Response of wood-inhabiting fungal community to fragmentation in a beech forest landscape

2014

Fragmentation of natural habitats has become one of the main causes of the loss of biodiversity. To assess the effects of forest fragmentation on wood-inhabiting fungal community in a beech-dominated landscape, 15 differently shaped beech forest fragments were examined in northern Spain. This work covers all the wood-inhabiting macromycetes, including Basidiomycota and Ascomycota. A modelling approach was used to examine the predictability of the fungal community in a fragmented beech forest landscape. In the beech forest patches, a large proportion of edge, low tree densities and low levels of variety of woody debris caused a decrease of wood-inhabiting fungal richness. The fungal communit…

geographygeography.geographical_feature_categoryEcologybiologyCommunityEcologyAgroforestryEcological ModelingfungiForest managementBiodiversityFragmentation (computing)Plant Sciencebiology.organism_classificationOld-growth forestHabitatta1181Species richnessBeechEcology Evolution Behavior and SystematicsFungal Ecology
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Grasslands and Shrublands of Kazakhstan and Middle Asia

2020

Abstract Kazakhstan and Middle Asia comprise 4 million km2 of plains, uplands and tall mountain ranges in the core of the Eurasian continent. The region's semi-arid climate, grazing pressure by wild and domestic ungulates, and long pastoral tradition, have given rise to a variety of open habitat types and a distinct flora and fauna. Grasslands and shrublands are a natural and dominant vegetation type in the forest-steppe and steppe zone of northern and central Kazakhstan, as part of the Eurasian grassland biome. In Middle Asia, grasslands and shrublands are widespread habitat types in the Tian Shan, Pamir-Alai and Pamir—mountain systems that have been recently acknowledged as a global biodi…

geographygeography.geographical_feature_categoryHabitat destructionSteppeAgroforestryVegetation typeBiodiversityOvergrazingGrasslandGlobal biodiversityShrubland
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Are wide but selectively logged buffer strips better than narrow ones?

2020

The microclimate of streamside habitats are protected from the effects of logging with buffer strips of retained trees. However, these buffer strips are often narrow due to their financial loss. Wi...

geographygeography.geographical_feature_categoryHabitatTaigaForest managementLoggingMicroclimateEnvironmental scienceForestryBuffer stripBryophyteForestryRiparian zoneScandinavian Journal of Forest Research
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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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Discussion on 'Estimating depth-averaged velocities in rough channels'

2002

In this short communication the four estimate criteria of the depth-averaged local velocity proposed by Byrd et al. (Earth Surface Processes and Landforms, 2000, Vol. 25, pp. 167-173) are compared both with the three-point method of Bathurst and with the average velocity obtained by integrating the velocity profile (FPa2) suggested by Ferro and Pecoraro (Water Resources Research, 2000, vol. 36, pp. 2761-2770). The comparison was carried out using 84 velocity profiles measured by an acoustic Doppler velocimeter in a rectangular flume with a gravel bed. Copyright © 2002 John Wiley and Sons, Ltd.

geographygeography.geographical_feature_categoryLandformDepth averagedGeography Planning and DevelopmentEarth surfaceFlumeGravel bedRiemann averageVelocity profileEarth and Planetary Sciences (miscellaneous)Large-scale roughneSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineeringAcoustic Doppler velocimetryGeomorphologyGeologyEarth-Surface ProcessesEarth Surface Processes and Landforms
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Testing GIS-morphometric analysis of some Sicilian badlands

2014

Abstract Calanchi badlands are erosion landforms characterized by areas with scarce or absent vegetation, steep slopes, knife-edge divides and high erosion rates. They are originated by a combination of morphogenetic processes, partly similar to those shaping bigger fluvial landforms, and therefore can be considered as field “laboratories.” This paper presents the results of an investigation carried out in two badland sites located in Sicily, where the geometry of 25 calanchi has been characterized using Digital Elevation Models having a mesh size equal to 2 m. For each landform, a power length–volume relationship is established. This relationship demonstrates that length of calanchi channe…

geographygeography.geographical_feature_categoryLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaEphemeral keyDrainage basinFluvialVegetationCatchment hydrologySoil erosion Calanchi DEM GIS Hack's lawErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDigital elevation modelGeomorphologyGeologyEarth-Surface ProcessesCATENA
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A new empirical model for estimating calanchi Erosion in Sicily, Italy

2015

Abstract Calanchi (plural of calanco) are typical badland landforms of the Italian landscape. They consist of dense networks of V-shaped valleys, with a sparse or absent vegetation cover, which frequently develop on unconsolidated or poorly consolidated clayey deposits. In this paper, the dimensional analysis and the incomplete self-similarity theory were used to deduce a model relating the volume of sediments eroded from the calanchi area to a set of geometric attributes of their tributary areas. The morphometric characteristics of 209 calanchi basins were used to calibrate and validate the model. The predictive skill of the model was assessed by calculating the mean square error and the N…

geographygeography.geographical_feature_categoryLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaSoil erosion Badlands Calanchi Dimensional analysis Self-similarity theory SicilyTributaryErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeomorphologyGeologyEarth-Surface ProcessesVegetation coverGeomorphology
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Drained organic soils under agriculture — The more degraded the soil the higher the specific basal respiration

2019

Abstract Drained peatlands are hotspots of carbon dioxide (CO2) emissions from agricultural soils. As a consequence of both drainage-induced mineralisation and anthropogenic mixing with mineral soils, large areas of former peatlands under agricultural use underwent a secondary transformation of the peat (e.g. formation of aggregates). These soils show contents of soil organic carbon (SOC) at the boundary between mineral and organic soils. However, the carbon (C) dynamics of such soils have rarely been studied so far. The aim of the present study was to evaluate the vulnerability of soil organic matter (SOM) to decomposition over the whole range of peat-derived soils under agriculture includ…

geographygeography.geographical_feature_categoryPeatSoil testPhosphorusSoil organic matterSoil Sciencechemistry.chemical_element04 agricultural and veterinary sciencesSoil carbon010501 environmental sciences01 natural scienceschemistry.chemical_compoundchemistryEnvironmental chemistrySoil waterCarbon dioxide040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceBog0105 earth and related environmental sciences
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Characterization and modeling of water movement and salts transfer in a semi-arid region of Tunisia (Bou Hajla, Kairouan) – Salinization risk of soil…

2012

Abstract The semi-arid region of Bou Hajla (Kairouan – Central Tunisia) is exposed to the risk of soils and aquifers salinization. A characterization of water movement through the use of TDR probes installed at up to 4 m in depth, and of salts transfer by soil sampling was conducted to highlight this risk. At the same time, climatic parameters were monitored. The results were gathered over the period of approximately 1 year (June 12, 2006 to May 08, 2007). Water infiltration and evaporation, occurred at within distinct materials: two zero flux planes at 1 and 3 m, and a clay-silt layer at 2 m where the soil water content and electrical conductivity is highly varied. Saline profiles show sal…

geographygeography.geographical_feature_categorySoil salinityEvaporationEnvironmental engineeringHumidityForestrySoil scienceAquiferHorticultureAridComputer Science ApplicationsFlux (metallurgy)Vadose zoneSoil waterEnvironmental scienceAgronomy and Crop ScienceComputers and Electronics in Agriculture
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