Search results for "Soil Science"

showing 10 items of 1336 documents

Reversing agriculture from intensive to sustainable improves soil quality in a semiarid South Italian soil

2010

Intensive agriculture (IA) is widespread in South Italy, although it requires frequent tillage, large amounts of fertilizers and irrigation water. We have assessed the efficacy of reversing IA to sustainable agriculture (SA) in recovering quality of a typical South Italy soil (Lithic Haploxeralf). This reversion, lasting from 2000 to 2007, replaced 75% of nutrients formerly supplied inorganically by farmyard manuring and reduced the tillage frequency. Several chemical and biochemical properties, functionally related to C and N mineralisation–immobilisation processes and to P and S nutrient cycles, were monitored annually from 2005 to 2007 in the spring. Reversing IA to SA decreased soil bul…

chemistry.chemical_classificationSoil salinitySoil microbial biomaIntensive farmingSoil organic matterSettore AGR/13 - Chimica AgrariaSustainable agricultureSoil ScienceSoil quality ; Sustainable agriculture .; Soil chemstryMicrobiologySoil qualitySoil qualitySoil chemstryTillageMicrobial activityAgronomychemistrySemiarid Mediterranean environmentSoil waterOrganic matterSoil fertilityAgronomy and Crop Science
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Humic substances along the profile of two Typic Haploxerert

2002

Abstract In Vertisols, organic matter contributes to soil colour by formation of organo-mineral complexes and affects morphological, physico-chemical, biological and biochemical properties. Turbation may affect the chemical and structural composition of the most stabilised fractions of soil organic matter (SOM), i.e., humic substances (HS). The objectives of this study were to: (1) characterise SOM in two Vertisols (V1 and V2) developed under Mediterranean climate in Italy, using some HS characteristics as indicators of SOM turnover in Vertisols, and (2) explore possible differences related to the pedomorphologic conditions of the area under which two soils have formed. SOM evolution along …

chemistry.chemical_classificationSoil structurePedogenesischemistryEnvironmental chemistrySoil organic matterSoil waterSoil ScienceSoil horizonMineralogyOrganic matterVertisolHumusGeoderma
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Changes in soil microbial activity and physicochemical properties in agricultural soils in Eastern Spain

2015

Agricultural land management greatly affects soil properties. Microbial soil communities are the most sensitive and rapid indicators of perturbations in land use and soil enzyme activities are sensitive biological indicators of the effects of soil management practices. Citrus orchards frequently have degraded soils and this paper evaluates how land management in citrus orchards can improve soil quality. A field experiment was performed in an orchard of orange trees (<em>Citrus Sinensis</em>) in the Alcoleja Experimental Station (Eastern Spain) with clay-loam agricultural soils to assess the long-term effects of herbicides with inorganic fertilizers (H), intensive ploughing and i…

chemistry.chemical_classificationSoil testAgroforestrySoil organic matterSoil biologySoil Sciencecomplex mixturesSoil qualitySoil managementSoil respirationchemistryAgronomySoil waterEnvironmental scienceOrganic matterSpanish Journal of Soil Science
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Responses of soil carbon and nitrogen transformations to stump removal

2012

We studied in central Finland whether stump harvesting after clear felling of coniferous forest poses further short-term changes in soil carbon and nitrogen dynamics when compared to the traditional site preparation method, mounding. Exposed mineral soil patches in Norway spruce (Picea abies) dominated clear-cut stands were sampled 1–5 years after the treatments. The extent of the exposed mineral soil surface was significantly larger at the stump removal sites when compared to the mounding sites. No differences were found in soil pH, organic matter content or total concentration of soil C between the treatments or treatment years. Total concentration of soil N was consistently higher and …

chemistry.chemical_classificationSoil testEcological ModelingSoil organic matterfungiForestrySoil classificationSoil scienceSoil carbondigestive systemcomplex mixturesSoil qualitybody regionssurgical procedures operativeAgronomychemistrySoil pHStump harvestinglcsh:SD1-669.5Environmental scienceOrganic matterlcsh:ForestrySilva Fennica
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Reduction of the frequency of herbaceous roots as an effect of soil compaction induced by heavy grazing in rangelands of SW Spain

2017

Rangelands in SW Spain constitute the most extensive ranching system on the Iberian Peninsula. During the last few decades, a significant increase in livestock numbers, along with a progressive substitution of cattle for sheep, have led to land degradation processes such as the reduction of grass cover and increased soil compaction in heavily grazed areas. Nevertheless, a better understanding of how soil compaction affects grass production is still needed. In this study, some of the effects of soil compaction due to heavy grazing are analysed, mainly the reduction of the frequency of herbaceous roots and its relationships with bulk density and soil penetration resistance. The study was carr…

chemistry.chemical_classificationSòls ErosióSoil organic matterSoil science04 agricultural and veterinary sciences010501 environmental sciencesHerbaceous plant01 natural sciencesBulk densitychemistryAgronomyGrazing040103 agronomy & agriculture0401 agriculture forestry and fisheriesSoil horizonEnvironmental scienceOrganic matterRangelandWater content0105 earth and related environmental sciencesEarth-Surface ProcessesCATENA
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Influence of inheritance and pedogenesis on heavy metal distribution in soils of Sicily, Italy

2000

Abstract The recognition of the potential health hazards associated with heavy metals has focused attention on the levels and behaviours of these elements both in natural and contaminated environments. Various soil types developed from different parent materials in Sicily, Italy, have been analysed in order to compare heavy metal distribution under different geopedological conditions. Total metal concentrations, metal partitioning and distribution profiles are discussed in relation to the inheritance factor and pedogenic processes. Parent material composition largely influences the contents of heavy metals in most of the analysed soils, mainly differentiating pedons for their metal concentr…

chemistry.chemical_classificationTopsoilInceptisolSoil ScienceSoil scienceVertisolPedogenesischemistryEnvironmental chemistryCation-exchange capacitySoil horizonOrganic matterEntisolGeologyGeoderma
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Selenium Partitioning and Stable Isotope Ratios in Urban Topsoils

2011

oxides. Th e δ82/76 Se values of total Se in the topsoils were close to the bulk Earth composition with an average δ82/76 Se value of −0.03 ± SD 0.38‰ suggesting that there was no or little Se isotope fractionation in soil. We attribute the small isotope fractionation to the low bioavailability of Se as a consequence of the presence of Fe oxides (adsorbing the dominating Se(IV) forms strongly), organic matter, and SO 4 2− (prevents biouptake of the Se(IV) forms) in the study soils. Small Se isotope fractionations of −0.59 to −0.35‰ in mainly forest soils and of 0.26 to 0.45‰ in mainly alluvial soils were presumably caused by soil/plant-recycling and Se contamination by river water, respecti…

chemistry.chemical_classificationTopsoilIsotopeStable isotope ratioSoil Sciencechemistry.chemical_elementSoil scienceFractionationIsotope fractionationchemistryEnvironmental chemistrySoil waterOrganic matterSeleniumSoil Science Society of America Journal
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Pedogenesis in disturbed alpine soils (NW Italy)

2002

In alpine environments, natural or man-induced disturbances are fairly common and acknowledged as determining factors in pedogenesis and soil distribution. We have selected a representative alpine valley in the Italian Northwestern Alps to evaluate the effects of perturbations of different intensity and frequency on soil development and weathering during the last few centuries. In order of decreasing disturbances, we selected: (i) an active avalanche shoot; (ii) a man-built terrace; (iii) a park-like forest; and (iv) a coniferous forest. In the two most disturbed sites, independently of the intensity and frequency of the disturbances, the active pedogenic processes are restricted to the top…

chemistry.chemical_classificationTopsoilSoil ScienceSoil scienceWeatheringVegetationengineering.materialPodzolPedogenesischemistryIlliteengineeringSoil horizonOrganic matterGeologyGeoderma
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Effect of climate and vegetation on soil organic carbon, humus fractions, allophanes, imogolite, kaolinite, and oxyhydroxides in volcanic soils of Et…

2007

A soil sequence along an elevational gradient ranging from subtropical to subalpine climate zones in the Etna region (Sicily, southern Italy) was investigated with respect to organic C, kaolinite, and crystalline to noncrystalline Al and Fe phases. Special emphasis was given to the stabilization of soil organic carbon (SOC) and its interaction with the inorganic phases. The soils were variations of Vitric Andosols that developed on a trachy-basaltic lava flow with an age of 15,000 years. Two main vegetation systems dominated the sites: at the lower sites, it was mainly maquis vegetation and, at the higher elevated sites, predominantly coniferous forest. The concentration of SOC in the topso…

chemistry.chemical_classificationTopsoilSoil organic matterSoil ScienceSoil scienceSoil carbonHumusAndosolSoil organic matter kaolinite fulvic and humid acidschemistrySoil waterVegetation typeOrganic matterGeology
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Factors influencing carbon decomposition of topsoils from the Brazilian Amazon Basin

1999

The influence of texture and local climate, especially precipitation, on C decomposition was evaluated in topsoils under forest and pastures at different sites located in the western, central, and eastern Brazilian Amazon Basin. Independent of the geographical location and vegetation cover, C decomposition was lower in topsoils of fine texture with a sand/clay ratio of less than 1, compared to topsoils of coarse a texture with a sand/clay ratio ranging from 2 to 8. In the former, the low sand/clay ratio appears to reduce C decomposition. In the latter, besides the effect of the high sand/clay ratio, the local climate, especially the annual precipitation, seems to play an important role in c…

chemistry.chemical_classificationTopsoil[SDV]Life Sciences [q-bio]Soil biologySoil ScienceSoil scienceRainforestMicrobiologyTexture (geology)Soil qualityCarbon cyclechemistry[SDE]Environmental SciencesEnvironmental scienceOrganic matterPrecipitationAgronomy and Crop ScienceBiology and Fertility of Soils
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