Search results for "SOIL ORGANIC"

showing 10 items of 214 documents

Effect of Organic Amendments on the Evolution of Soil Organic Matter in Soils Stressed by Intensive Agricultural Practices

2013

Losses of soil organic carbon often occur because of intensive agricultural practices that lead to removal of organic carbon following harvest production and to insufficient inputs. Organic amendments can be a very appropriate matrix for enhancing organic carbon content in very stressed agricultural soils. In general, they, enhancing soil organic matter, play an important role in environmental matrices due, for example, to their capacity in retaining water, in interacting with organic and inorganic pollutants, and in enhancing nutrient availability to plants. For this reason, the understanding of the mechanisms with which organic amendments interact with other chemicals in the environment i…

AgroforestryChemistrybusiness.industrySoil organic matterSettore AGR/13 - Chimica AgrariaOrganic ChemistryAmendements FFC-NMR relaxometry FT-IR Humic acids NMR soil orgaqnic matterhumic acidNMRFT-IRAgronomyFFC-NMR relaxometryAgriculturesoil organic matterSoil waterAmendmentbusiness
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Soil structural stability and erosion rates influenced by agricultural management practices in a semi-arid Mediterranean agro-ecosystem

2012

Unsuitable agricultural practices can cause loss in soil quality and erodibility to thus increase or trigger desertification under Mediterranean conditions. A field experiment was performed at the El Teularet-Sierra de Enguera Experimental Station (eastern Spain) to assess the influence during a 5-yr period of different agricultural practices on physical and chemical indicators of soil quality (total and water-soluble carbohydrates, glomalin-related soil proteins (GRSP), total organic carbon, aggregate stability (AS), vegetation cover and soil erosion). The management practices included residual herbicide use, ploughing, ploughing + oats, addition of oat straw mulch and a control (land aban…

AgroforestrySoil biodiversitySoil organic matterfood and beveragesSoil SciencePollutionSoil qualitySoil managementNo-till farmingAgronomyAgricultural soil scienceSoil retrogression and degradationEnvironmental scienceSoil fertilityAgronomy and Crop ScienceSoil Use and Management
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Soil organic carbon stocks under recommended management practices in different soils of semiarid vineyards

2019

The Intergovernmental Panel on Climate Change (IPCC) approach is widely used to estimate the C account through the use of standardized coefficients that are not site specific. For these reasons, the aim of the work was to define specific IPCC coefficient taking into account differences in pedological characteristics that affect soil C steady state. In a vineyard area of Sicily, the effectiveness of 5 years of recommended management practice (RMP) adoption on soil organic carbon (SOC) stock increases was evaluated by considering 100 paired sites distributed over four functional soil groups. Each site consisted of two neighbouring plots. The soil of one plot was managed with cover crops accor…

Agroforestryvineyard soil management2Mediterranean environmentSoil ScienceDevelopmentSettore AGR/02 - Agronomia E Coltivazioni ErbaceeCOmitigationSoil watercarbon steady stateSoil organic carbon stocksEnvironmental ChemistryEnvironmental scienceCover cropcover croppingManagement practicesGeneral Environmental ScienceLand Degradation & Development
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Litter contribution to soil organic carbon in the agriculture abandons processes

2015

Abstract. Mechanisms of litter decomposition, translocation and stabilization into soil layers are fundamental processes in ecosystem functioning as it regulates the cycle of soil organic matter (SOM), CO2 emission into the atmosphere, carbon sequestration into the soil. In this study, it was investigated the contribution of litters of different stages of Mediterranean secondary succession on Carbon sequestration, analyzing the role of earthworms on translocation of SOM into soil profile. For this purpose δ13C difference between meadow C4-Csoil and C3-Clitter were used in a field experiment. Four undisturbed litters of different stages of succession were collected (45, 70, 100 and 120 since…

AgronomyAgriculturebusiness.industrySoil organic matterLitterEnvironmental scienceSoil carbonbusiness
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Aspects of soil phenolic matter (SPM): An explorative investigation in agricultural, agroforestry, and wood ecosystems

2014

Abstract This paper assesses the distribution of soil phenolic matter (SPM) in soil environments from a pedological perspective, with particular emphasis on soil horizonation and its involvement in pedogenic processes. The study was conducted on 15 soil profiles (Andosols, Calcisols, Cambisols, Lixisols, Phaeozems, Podzols, Umbrisols) covering five distinct ecosystems. Although the ecosystems were virtually homogeneous in and of themselves, they represented strongly contrasting climates, geolithology and morphology, land use and vegetation cover (intensive agriculture, chestnut grove, alpine pasture, woody reforestations, and natural woods). Three main SPM fractions were categorised: (i) “t…

Anthropised ecosystemCambisolIntensive farmingSoil organic matterSoil SciencePedogenesiSoil scienceWeatheringPodzolPedogenesisSettore AGR/14 - PedologiaNatural ecosystemEnvironmental chemistryLeaching (pedology)Environmental scienceEcosystemSoil phenolic matter Natural ecosystems Anthropised ecosystems Horizonation PedogenesisHorizonationSoil phenolic matterGeoderma
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Changes in soil chemical properties as affected by pyrogenic organic matter amendment with different intensity and frequency

2017

Pyrogenic organic matter (PyOM) has long been used as a soil amendment to improve soil physicochemical properties. However, few studies simultaneously investigated both intensities and frequencies of PyOM addition on soil chemical properties of soil base cations, soil pH buffering capacity (pHBC), and plant available micronutrients. In the main food production area of lower Liaohe River Plain in Northeast China, a field manipulation of PyOM addition was initiated in 2013 to examine how the intensities (0, 1%, 3%, and 5% of 0–20 cm soil mass) and frequencies (3% of soil mass applied once versus yearly for 3 years) of PyOM amendment affected soil chemical properties. Higher intensity of PyOM …

Base cationSoil acidificationAmendmentSoil ScienceBiomass010501 environmental sciencesSoil fertilitycomplex mixtures01 natural sciencesSoil pHBiocharOrganic matterSoil acidification0105 earth and related environmental scienceschemistry.chemical_classificationSoil organic matterfood and beverages04 agricultural and veterinary sciencesBodemfysica en LandbeheerSoil Physics and Land ManagementBiocharAgronomychemistryEnvironmental chemistryTrace element040103 agronomy & agriculture0401 agriculture forestry and fisheriesSoil fertilityEcologia dels sòlsGeoderma
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Influence of parent material and soil use on arsenic forms in soils A case study in the Amblés Valley (Castilla-León, Spain)

2014

Abstract The total, water soluble and extractable concentrations with EDTA of As from topsoils from the Ambles Valley (Avila, Spain) were determined. The geochemical baseline concentrations of total As were established, and the relationships between the concentration of the different As forms and soil properties were investigated. Total As content in soils was related with parent material, whereas anthropogenic activities affected its mobility. Iron, aluminium, clay content, soil organic matter and soil pH were the main controlling factors for As soil concentrations. The geochemical baseline concentrations obtained (mg kg − 1 ) were 7.3–35 in soils on granite parent material and 2.2–6.8 in …

Baseline concentrationsSoil organic matterchemistry.chemical_elementcomplex mixturesWater solubleParent materialchemistryGeochemistry and PetrologySoil pHEnvironmental chemistrySoil waterAnthropogenic activitiesEconomic GeologySoil propertiesBaseline concentrationGeologyArsenic
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Impact of hydrologically driven hillslope erosion and landslide occurrence on soil organic carbon dynamics in tropical watersheds

2016

The dynamics of soil organic carbon (SOC) in tropical forests play an important role in the global carbon (C) cycle. Past attempts to quantify the net C exchange with the atmosphere in regional and global budgets do not systematically account for dynamic feedbacks among linked hydrological, geomorphological, and biogeochemical processes, which control the fate of SOC. Here we quantify effects of geomorphic perturbations on SOC oxidation and accumulation in two adjacent wet tropical forest watersheds underlain by contrasting lithology (volcaniclastic rock and quartz diorite) in the Luquillo Critical Zone Observatory. This study uses the spatially-explicit and physically-based model of SOC dy…

Biogeochemical cycleEnvironmental Engineering010504 meteorology & atmospheric sciencesTropical forestsLithologyLife on Land0208 environmental biotechnologyTRIBS02 engineering and technologyCoupled processesStructural basin01 natural sciencesCivil EngineeringPhysical Geography and Environmental GeoscienceTropical forestLandscape0105 earth and related environmental sciencesWater Science and TechnologyHydrologySoil organic carbonSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaLandslideSoil carbonCoupled processe020801 environmental engineeringDioriteDenudationErosionApplied EconomicsErosionCoupled processes; Erosion; Landscape; Soil organic carbon; TRIBS; Tropical forests; Water Science and TechnologyGeology
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The Relations between the Sulphur Forms and the Organic and Mineral Components in Soils Developed under Spruce Forests in the Mont Lozere (France)

1992

Mean interannual (1981–1985) hydrochemical input-output budgets indicate net gains of sulphur in forested and unforested watersheds (1150–1450m deviation range) of Mont Lozere (2). The values of the sulphur gains, ranging from 5 to 10 kg/ha/yr. according to the watersheds are underestimated, since dry deposition is not considered in the budgets (1). It is now well known (3,4) that sulphur accumulation in forest catchments is mediated physically by sulphate adsorption on mineral amorphous surfaces and microbially by incorporation of sulphur into soil organic matter. To get a better assessment of these processes, in order to foresee their long term effects upon the proton-budgets and biogeoch…

Biogeochemical cycleMineralchemistrySoil organic matterEnvironmental chemistrySoil waterSoil horizonchemistry.chemical_elementInorganic sulphateSoil scienceEcosystemSulfurGeology
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Relationships between soil water repellency and microbial community composition under different plant species in a Mediterranean semiarid forest

2014

Abstract Soil water repellency (SWR) can influence many hydrological soil properties, including water infiltration, uneven moisture distribution or water retention. In the current study we investigated how variable SWR persistence in the field is related to the soil microbial community under different plant species (P. halepensis, Q. rotundifolia, C. albidus and R. officinalis) in a Mediterranean forest. The soil microbial community was determined through phospholipid fatty acids (PLFA). The relationships between microbiological community structure and the soil properties pH, Glomalin Related Soil Protein (GRSP) and soil organic matter (SOM) content were also studied. Different statistical …

BiohydrologyMediterranean climatesoil hydrophobicityTA Engineering (General). Civil engineering (General)Phospholipids fatty acidsActinobacteriaBotanymedicinebiohydrologyGlomalin Related Soil ProteinWater Science and TechnologyFluid Flow and Transfer Processesglomalin related soil proteinbiologyphospholipids fatty acidsMechanical EngineeringSoil organic matterCommunity structureactinobacteriaMicrobial community structureHydraulic engineeringbiology.organism_classificationWater retentionActinobacteriaGlomalinMicrobial population biologyAgronomymicrobial community structureSoil waterbiology.proteinEnvironmental sciencemedicine.symptomTC1-978Soil hydrophobicity
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