Search results for "Soil Science"

showing 10 items of 1336 documents

Effective Removal and Mineralization of 8-Hydroxyquinoline-5-sulfonic Acid through a Pressurized Electro-Fenton-like Process with Ni−Cu−Al Layered Do…

2020

Ni−Cu−Al layered double hydroxide (Ni−Cu−Al LDH) was proposed as an electro‐Fenton‐like catalyst for 8‐hydroxyquinoline‐5‐sulfonic acid (8‐HQS) removal in water. The properties of the prepared catalysts were characterized by using X‐ray, SEM and EDAX analyses. The effect of numerous operative parameters on the removal of 8‐HQS and total organic carbon (TOC) was studied. Very high level removal of both 8‐HQS and TOC (87 and 79 %, respectively) were obtained by using a pressurized electro‐Fenton‐like process (PrEFL‐LDH) at P=10 bars, using a Ti/IrO2‐Ta2O5 anode for 6 h. The process presented good performances in a large range of pH (3–10) and gave better removals of 8‐HQS and TOC with respect…

chemistry.chemical_classificationchemistry.chemical_compoundChemistry8-hydroxyquinoline-5-sulfonic acid heterogeneous catalysis Ni−Cu−Al layered double hydroxide nitrogen heterocycles pressurized-electro-FentonElectrochemistryHydroxide8-HydroxyquinolineMineralization (soil science)Sulfonic acidSettore ING-IND/27 - Chimica Industriale E TecnologicaHeterogeneous catalysisCatalysisNuclear chemistry
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Formation and Changes of Humic Acid Properties during Peat Humification Process within Ombrotrophic Bogs

2012

Studies of the living organic matter humification process are essential for understanding the carbon biogeochemical cycle. The aim of this study is to analyze relations between the properties of peat, peat humic acids and peat humification degree. The analysis has been done on samples of humic substances extracted from peat profiles in two ombrotrophic bogs and relations between peat age, decomposition and humification degree, botanical composition and properties of peat humic acids (elemental, functional composition) were studied. The found variability of peat properties is less significant than differences in the properties of peat-forming living matter, thus revealing the dominant impact…

chemistry.chemical_classificationgeographyBiogeochemical cyclegeography.geographical_feature_categoryPeatChemistryOmbrotrophicSoil scienceDecompositionHumusEnvironmental chemistryHumic acidOrganic matterBogOpen Journal of Soil Science
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Genesis of Peat Humic Acid Structure and Properties Within Bog Profiles

2012

Studies of living organic matter humification process are essential for understanding of carbon biogeochemical cycle, and considering this, the aim of this study is to analyse relations between properties of the peat, peat humic acids (HAs) and humification degree on example of analysis of two bog profiles in ombrotrophic bogs to identify the links between peat age, decomposition and humification degree, botanical composition and properties of peat humic acids (elemental, functional composition). The found variability of peat properties is much less than the significant differences in properties of peat-forming living matter, thus stressing the dominant impact of humification process on pea…

chemistry.chemical_classificationgeographyBiogeochemical cyclegeography.geographical_feature_categoryPeatOmbrotrophicSoil scienceDecompositionHumuschemistryEnvironmental chemistryHumic acidOrganic matterBogGeology
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Characterization of Humic Acids from Raised Bog Peat

2014

Abstract Humic substances form most of the organic component of soil, peat and natural waters, but their structure and properties are very much dependent on the source. The aim of this study was to characterize humic acids from raised bog peat to evaluate the homogeneity of humic acids isolated from the bog bodies and to study peat humification impact on the properties of humic acids. Peat humic acids (HA) have an intermediate position between the living organic matter and coal organic matter, with their structure formed in a process where the relatively labile moieties (carbohydrates, amino acids, etc.) are destroyed, and thermodynamically more stable aromatic and polycyclic structures eme…

chemistry.chemical_classificationgeographygeography.geographical_feature_categoryPeatbusiness.industryNatural waterSoil sciencecomplex mixturesHumusHumic substances; composition; soil; peat; LatviachemistryEnvironmental chemistryEnvironmental scienceOrganic matterCoalOrganic componentbusinessBogRaised bogMaterial Science and Applied Chemistry
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Organic matter dynamics and aggregation in soils under rain forest and pastures of increasing age in the eastern Amazon Basin

1997

Abstract In the eastern Amazon basin, four neighbouring clayey Oxisols with similar particle-size distributions were selected, one under rain forest and three under pasture for 7, 12 and 17 years, respectively. These soils were sampled at depth intervals of 0.1 m down to 1 m. Although no clear effect of pasture establishment on aggregate stability was assessed, significant negative effects of cattle trampling on porosity and water retention and of vegetation change on clay water-dispersion were observed in the organic-rich horizons (0–0.40 m layers). Indirect evidence of a great change of the nature of organic materials was also suggested, particularly with (i) an increase in both negative …

chemistry.chemical_classificationgeographygeography.geographical_feature_categorySoil organic matterSoil ScienceSoil scienceVegetationDispersion (geology)PasturechemistryOxisolSoil waterEnvironmental scienceOrganic matterTramplingGeoderma
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Influence of operational variables on the photodegradation kinetics of Monuron in aqueous titanium dioxide dispersions

1994

The degradation of Monuron [N′—(4-chlorophenyl)—N, N dimethyl urea] in aqueous TiO 2 dispersions irradiated in the near-UV region has been investigated using a Pyrex batch photoreactor. The influence on the degradation kinetics of pH, initial Monuron concentration and catalyst concentration has been studied. The mineralization of the pollutant was also investigated. Measurements of photon absorbed flows allowed to determine the quantum yield values; they were found to increase by increasing the initial pH of the dispersion.

chemistry.chemical_compoundAqueous solutionChemistryInorganic chemistryKineticsTitanium dioxideQuantum yieldMineralization (soil science)PhotodegradationDispersion (chemistry)Catalysis
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Linking food webs to ecosystem processes: Piecewise linear models of soil microcosms

2008

Abstract A piecewise linear approach to link decomposer biomass and soil nitrogen dynamics is proposed. Dynamics of a detritus–fungus–nematode food chain were studied in a microcosm experiment and modelled to evaluate the role of fungal-feeding nematodes in N mineralization. The nematode dynamics switched from exponential growth to a resource-limited phase. At the same time the amount of ammonium nitrogen in soil started to increase, following an initial immobilization phase. Both nematode and ammonium dynamics could be described by two-phase linear equations. Two nitrogen models were compared. A model in which the nematode accounted for all mineralization could be fitted to the ammonium da…

chemistry.chemical_compoundFood chainAgronomychemistryEcological ModelingSoil waterEcosystemAmmoniumMineralization (soil science)BiologyMicrocosmNitrogen cycleDecomposerEcological Modelling
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Soil‐plant relationships, micronutrient contents, and cardenolide production in natural populations of Digitalis obscura

2004

The production of secondary metabolites by plants growing in natural populations is conditioned by environmental factors. In the present study, we have investigated the relationships among soil properties, micronutrients in soils and plants, and cardenolide production from wild Digitalis obscura (Scrophulariaceae) populations. Young and mature leaves and soil samples were collected in ten different populations, corresponding to three Mediterranean bioclimatic belts (Thermo-, Meso-, and Supramediterranean belts). Soil (total and EDTA-extractable) and leaf micronutrients (Fe, Mn, Zn, and Cu), and leaf cardenolide accumulation have been determined. Significant negative correlations were observ…

chemistry.chemical_compoundbiologyChemistryBotanyDigitalis obscuraCardenolideSoil SciencePlant Sciencebiology.organism_classificationMicronutrientJournal of Plant Nutrition and Soil Science
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Evaluation of the factors affecting direct polarization solid state (31)P-NMR spectroscopy of bulk soils

2008

Summary 31 P-NMR spectroscopy on bulk soils is a powerful tool for the identification of the different phosphorus forms in soils and for the evaluation of the dynamics of soil P. Up to now the majority of the papers dealt with liquid state 31 P-NMR spectroscopy on soluble soil organic substances. Only few papers were addressed to the study of the different phosphorus forms directly in bulk soils. In the present paper, some organic and inorganic phosphates of known structures, which are likely to be present in soil systems, were studied by direct polarization (DP) magic angle spinning (MAS) 31 P-NMR spectroscopy in order to understand the electronic factors responsible for chemical shifts of…

chemistry.chemical_compoundchemistryCovalent bondChemical shiftSoil waterAnalytical chemistryMagic angle spinningSoil ScienceMoleculeOrganic chemistrySpectroscopyPhosphateElectronic density
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CLAYS IN COSMETICS AND PERSONAL-CARE PRODUCTS

2021

Clays are used in various cosmetic formulations, such as sunscreens, toothpastes, deodorants, creams, hair cosmetics, makeups, nail polish, facial masks, and shampoos, among others, to improve the organoleptic and physicochemical characteristics, to increase the stability, or to facilitate elaboration. Together with their technological functionalities, clays are cosmetologically active ingredients with cleaning, anti-aging, anti-wrinkling, and sun-care functionalities. Talc, kaolinite, mica, and some smectites are the clay minerals used most frequently in cosmetic products, but several other phyllosilicates as well as modified and synthetic clays are also used. Sometimes, clays are useful i…

clay mineralsGeochemistry and PetrologyTrade namesEarth and Planetary Sciences (miscellaneous)Clays and clay mineralsSoil ScienceClaysCosmeticsSettore CHIM/06 - Chimica OrganicaPhyllosilicatesWater Science and TechnologyCosmetological functionsINCI names
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