Search results for "ORGANIC MATTER"

showing 10 items of 577 documents

Pedogenesis and Variability in Soil Properties in a Floodplain of a Semiarid Environment in Southwestern Sicily (Italy).

2010

We performed a pedological study of the variability in soils in a floodplain area of a semiarid region in southwestern Sicily. The objectives of our research were to (i) investigate the role of parent material, erosion, and distribution processes on soil pedogenesis and horizon differentiation; (ii) evaluate the statistical distribution of soil properties; and (iii) interpret these distributions in terms of pedogenic and other processes. Our results showed that not all soil properties examined followed a normal distribution and that even when logtransformed, the degree of normality of the soil salinity data did not improve. Furthermore, principal component analysis was performed to investig…

HydrologyTopsoilgeographygeography.geographical_feature_categorySoil salinityFloodplainSoil SciencePedogenesis semiarid environments Sicily organic matter hydromorphic conditions.PedogenesisSettore AGR/14 - PedologiaSoil waterErosionAlluviumPedologyGeology
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Estimating the USLE soil erodibility factor in Sicily, South Italy

2012

The Universal Soil Loss Equation (USLE) is used by professionals and technicians to predict soil loss by water erosion and to establish soil conservation measures. One of the key elements of the USLE is the K factor, which is a measure of the soil erodibility. Given the difficulty in collecting sufficient data to adequately measure K, early in the USLE's history the soil erodibility nomograph method was developed to allow estimation of K based on standard soil properties. Since the nomograph approach was developed based on a small number of soils in the United States, it is necessary for other contexts to check the nomograph's ability to predict the soil's true erodibility. Considering that…

HydrologyWater erosionerodibilitàSoil organic matterGeneral EngineeringSoil scienceK factorUniversal Soil Loss EquationSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSoil propertiesSoil conservationClay soil
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Nutrient dynamics in water and sediment of Mediterranean ponds across a wide hydroperiod gradient

2012

Abstract In Mediterranean ponds, summer drought enhances seasonality whose intensity varies along topographic and climatic gradients. The alternation of wet and dry periods in rain dependent ponds affects their biogeochemistry and differentiates them from ponds fed by more stable water sources, such as groundwater springs. Superimposed onto this, land use is also a very strong factor of variability. In this study we compared nutrients and organic matter concentrations, in water and in sediment, among different types of Mediterranean ponds based on the source of water, hydroperiod and land use. Forty-three ponds were sampled in Eastern Spain corresponding to five pond types: (1) permanent sp…

Hydrologychemistry.chemical_classificationBiogeochemical cyclechemistryAquatic ecosystemDenitrification pathwayEnvironmental scienceSedimentBiogeochemistryOrganic matterWater qualityAquatic SciencePlanktonLimnologica
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Impacts of Climate on the Flux of Dissolved Organic Carbon from Catchments

2010

Recent increases in dissolved organic carbon (DOC) concentrations in surface waters across both Europe and North America have focused attention on the factors controlling the export of DOC compounds from catchments. Waters containing high concentrations of DOC generally have a characteristic brown colour and are associated with the presence of highly organic soils. Catchments dominated by these soils typically export between 10 and 300 kg DOC ha−1 year−1 (Billett et al., 2004; Laudon et al., 2004; Jonsson et al., 2006). A portion of this DOC is mineralised in streams and lakes to CO2, while the remainder is transported to the sea (Jonsson et al., 2006). Organic matter accumulates in soils w…

Hydrologychemistry.chemical_classificationBrown colourFlux (metallurgy)chemistryScienceSoil waterDissolved organic carbonEnvironmental scienceOrganic matterSTREAMSDecomposition
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D/H ratios of methoxyl groups of the sedimentary organic matter of Lake Holzmaar (Eifel, Germany): A potential palaeoclimate/-hydrology proxy

2014

Stable hydrogen isotope ratios (dD values) of methoxyl groups in lignin and pectin from a variety of plant types from different locations have been shown to mirror dD values of precipitation, with a mean uniform isotopic fractionation. Since dD in precipitation is mainly influenced by climatic conditions, including temperature, evaporation and precipitation amount, methoxyl groups of organic matter have been proposed as a potential palaeoclimate proxy. Here, we measured the dD values of the methoxyl groups of sedimentary organic matter derived from sediment core segments of Lake Holzmaar (Eifel, Germany). The sediment core covers the entire Holocene and part of the Late Glacial (until 13,65…

Hydrologychemistry.chemical_classificationIce corechemistryGeochemistry and PetrologySedimentary organic matterOrganic matterFractionationGlacial periodYounger DryasGeologyHoloceneProxy (climate)Geochimica et Cosmochimica Acta
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Impact of catchment properties on aquatic chemistry in the rivers of Latvia

2010

The relationships between land use characteristics and aquatic chemistry (nutrient concentrations, major inorganic ions and indicators of organic matter concentrations) were analyzed to determine factors controlling the runoff of dissolved substances, spatial variability of water chemical composition and possible impacts of pollution sources in Latvia. Groups of factors were found to determine the variability of nutrient, organic matter and major inorganic ions concentrations. Bedrock geology and weathering of soil minerals affect the concentrations of inorganic ions, but the nature of the relationships between nutrient concentrations and those of land use are good indicators of human impac…

Hydrologychemistry.chemical_classificationPollutionmedia_common.quotation_subjectInorganic ionsNutrientchemistrySoil waterSpatial variabilityOrganic matterWater qualitySurface runoffWater Science and Technologymedia_commonHydrology Research
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Organic lacustrine sediment varves as indicators of past precipitation changes: a 3,000-year climate record from Central Finland

2015

Annually laminated (varved) sediments from Lake Kallio-Kourujärvi, Central Finland, provide high-resolution sedimentological data for the last three millennia. These varves consist of two laminae that represent (1) deposition during the spring-to-autumn growing season, composed of degraded organic matter and a variety of microfossils, and (2) deposition during winter, composed of fine-grained homogenous organic matter. Because of the absence of a clastic lamina, these varves differ from the typical, well-described, clastic-organic varve sequences in Fennoscandian lakes. Such organic varves in Finnish lakes have not been studied in detail before. Three thousand varves were counted and their …

Hydrologychemistry.chemical_classificationVarvePaleoclimateLacustrine varvesNorthern EuropeSedimentOrganic sedimentsPrecipitation reconstructionAquatic ScienceDeposition (geology)Late HoloceneWater columnchemistryClastic rockPaleoclimatologyOrganic matterPhysical geographySedimentologyGeologyEarth-Surface ProcessesJournal of Paleolimnology
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Vulnerability of Mediterranean ecosystems to Climatic Change, study of soil degradation under different climatological conditions in an altitudinal t…

1995

Abstract To investigate the potential response of soils to climatic change, measurements of soil physical and chemical properties were carried out during a year in a mountain zone in Alicante (Spain), along an altitudinal and climatological gradient. Hydrological properties (infiltration runoff and sediment concentration) were measured under winter and summer conditions. Chemical and physical soil properties were analyzed for reference soil profiles along the transect. The erosional response of the soils as well as soil properties like organic matter and CEC are found to be under the direct influence of the climate, and as a result they have to be considered as important factors in the dese…

Hydrologychemistry.chemical_classificationmedia_common.quotation_subjectClimate changeInfiltration (hydrology)DesertificationchemistrySoil retrogression and degradationSoil waterEnvironmental scienceOrganic matterTransectSurface runoffmedia_common
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Distribution of soil organic carbon in Wadi Al-Thulaima, Saudi Arabia: A hyper-arid habitat altered by wastewater reuse

2018

The carbon cycle is being altered as a result of human-induced changes in the Earth's system. Therefore, ecosystems such as wetlands, authentic CO2 sinks, are becoming especially important. Little information exits on the soil organic carbon (SOC) stock for the middle east-countries man-made wetlands making wadis permanent with the outflow of wastewater treatment plants. This paper presents the vertical distribution of SOC content, soil bulk density (SBD) and SOC density in soil of vegetated and bare sites in Wadi Al-Thulaima, one of the artificial wetlands in central Saudi Arabia. The mean distribution of SBD in the vegetated and bare sites increased significantly with depth. Inversely, th…

Hydrologygeographygeography.geographical_feature_categoryCarbon depth distributionGlobal warmingSoil organic matterSaudi ArabiaCarbon sinkKyoto ProtocolWetland04 agricultural and veterinary sciencesSoil carbon010501 environmental sciencesCarbon sequestration01 natural sciencesSoil qualityCarbon cycleCarbon pool040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSoil fertility0105 earth and related environmental sciencesEarth-Surface ProcessesCATENA
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δ pattern of dissolved inorganic carbon in a small granitic catchment: the Strengbach case study (Vosges mountains, France)

1999

Abstract The transfers and origins of dissolved inorganic carbon (DIC) were studied for a year in a soil–spring–stream system in the Strengbach catchment, Vosges mountains, France. This 80 ha experimental research basin is located on the eastern side of the mountains, at an altitude ranging from 883 to 1146 m.a.s.l. and is mainly covered by spruce (80%). Brown acid and podzolic soils developed on a granitic basement, and, as a result, the DIC originates solely from CO2 generated by oxidation of soil organic matter. The ( δ 13 C DIC ) in catchment waters is highly variable, from about −22‰ in the springs and piezometers to about −12‰ in the stream at the outlet of the catchment. In the sprin…

Hydrologygeographygeography.geographical_feature_categoryδ13CSoil organic matterGeochemistryDrainage basinGeologyStructural basinBasementAltitudeGeochemistry and PetrologyDissolved organic carbonSoil waterGeologyChemical Geology
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