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Soil Chemical (soil + chemical)

Distribution by Scientific Domains
Earth and Environmental Science100%

Terms modified by Soil Chemical

  • soil chemical property
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    Selected Abstracts

    Decalcification of soils subject to periodic waterlogging

    EUROPEAN JOURNAL OF SOIL SCIENCE, Issue 1 2000
    G. A. Van Den Berg
    Summary Intense decalcification of fine-grained organic-rich soils subject to periodic oxidation and reduction takes place in the Biesbosch, a freshwater, tidally influenced wetland area in the Rhine,Meuse delta in The Netherlands. Soil chemical (sulphide concentration and pore-water characteristics) and hydrological variables (drainage) were measured in three representative Fluvisols differing in hydrology to identify processes inducing calcium carbonate dissolution. Both oxidation of previously formed iron sulphides during periods of low ground water and infrequent inundation, and increased carbon dioxide pressure in the soil during periods of waterlogging combined with drainage of pore-water solutes, contribute significantly to decalcification of the hydric soils. The effects of these individual processes on decalcification are in the same order of magnitude in the studied soils. Depending on site-specific hydrological conditions, approximately 0.1,0.3% calcium carbonate may be dissolved per year by a combination of these two processes, which is comparable to actual decalcification rates at these sites. Estimates of long-term decalcification rates, based on knowledge of the hydrogeochemistry, may be used to assess the risks accompanying the conversion of agricultural soils into wetlands. [source]

    Soil chemical surveying: A path to a deeper understanding of prehistoric sites and societies in Sweden

    GEOARCHAEOLOGY: AN INTERNATIONAL JOURNAL, Issue 4 2007
    Johan Linderholm
    A large number of contract archaeological investigations have been conducted in Sweden over the last 10,15 years. In this article, the applicability of soil chemical surveying in connection with contract archaeology is discussed, focusing on soil sampling, soil magnetic susceptibility, and phosphate analysis. Results from case studies from an area of the west coast of southern Sweden are presented. The investigated sites cover periods ranging from the Bronze Age to the Late Iron Age/Medieval time (3500,1000 B.P.). Results show that the chemical loading of prehistoric settlements varies considerably both quantitatively and spatially depending on different socioeconomic strategies and behavior. © 2007 Wiley Periodicals, Inc. [source]

    Vertical distribution of soil properties under short-rotation forestry in Northern Germany

    JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 5 2010
    Petra Kahle
    Abstract Short-rotation forestry (SRF) on arable soils has high potentials for biomass production and leads to long-term no-tillage management. In the present study, the vertical distributions of soil chemical and microbial properties after 15 y of SRF with willows and poplar (Salix and Populus spp.) in 3- and 6-year rotations on an arable soil were measured and compared to a pertinent tilled arable site. Two transects at different positions in the relief (upper and lower slope; transect 1 and 2) were investigated. Short-rotation forestry caused significant changes in the vertical distribution of all investigated soil properties (organic and microbial C, total and microbial N, soil enzyme activities), however, the dimension and location (horizons) of significant effects varied. The rotation periods affected the vertical distribution of the soil properties within the SRF significantly. In transect 1, SRF had higher organic-C concentrations in the subsoil (Bv horizon), whereas in transect 2, the organic-C concentrations were increased predominantly in the topsoil (Ah horizon). Sufficient plant supply of P and K in combination with decreased concentrations of these elements in the subsoil under SRF pointed to an effective nutrient mobilization and transfer from the deeper soil horizons even in the long term. In transect 1, the microbial-C concentrations were higher in the B and C horizons and in transect 2 in the A horizons under SRF than under arable use. The activities of ,-glucosidases and acid phosphatases in the soil were predominantly lower under SRF than under arable use in the topsoil and subsoil. We conclude, that long-term SRF on arable sites can contribute to increased C sequestration and changes in the vertical distribution of soil microbial biomass and soil enzyme activities in the topsoil and also in the subsoil. [source]

    Impact of organic manures with and without mineral fertilizers on soil chemical and biological properties under tropical conditions

    JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 1 2005
    Kulvinder Kaur
    Abstract Soils receiving organic manures with and without chemical fertilizers for the last 7 yr with pearlmillet,wheat cropping sequence were compared for soil chemical and biological properties. The application of farmyard manure, poultry manure, and sugarcane filter cake alone or in combination with chemical fertilizers improved the soil organic C, total N, P, and K status. The increase in soil microbial-biomass C and N was observed in soils receiving organic manures only or with the combined application of organic manures and chemical fertilizers compared to soils receiving chemical fertilizers only. Basal and glucose-induced respiration, potentially mineralizable N, and arginine ammonification were higher in soils amended with organic manures with or without chemical fertilizers, indicating that more active microflora is associated with organic and integrated system using organic manures and chemical fertilizers together which is important for nutrient cycling. [source]

    Establishment of Retama sphaerocarpa L. seedlings on a degraded semiarid soil as influenced by mycorrhizal inoculation and sewage-sludge amendment

    JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 5 2004
    María del Mar Alguacil
    Abstract A field experiment was carried out to evaluate the effectiveness of mycorrhizal inoculation with three arbuscular mycorrhizal (AM) fungi (Glomus intraradices Schenck & Smith, Glomus deserticola (Trappe, Bloss. & Menge), and Glomus mosseae (Nicol & Gerd.) Gerd. & Trappe) and the addition of composted sewage sludge (SS) with respect to the establishment of Retama sphaerocarpa L. seedlings, in a semiarid Mediterranean area. Associated changes in soil chemical (nutrient content and labile carbon fractions), biochemical (enzyme activities), and physical (aggregate stability) parameters were observed. Six months after planting, both the addition of composted SS and the mycorrhizal-inoculation treatments had increased total N content, available-P content, and aggregate stability of the soil. Values of water-soluble C and water-soluble carbohydrates were increased only in the mycorrhizal-inoculation treatments. Rhizosphere soil from the mycorrhizal-inoculation treatments had significantly higher enzyme activities (dehydrogenase, protease-BAA, acid phosphatase, and ,-glucosidase) than the control soil. In the short-term, mycorrhizal inoculation with AM fungi was the most effective treatment for enhancement of shoot biomass, particularly with G. mosseae (about 146% higher with respect to control plants). The addition of the composted SS alone was sufficient to restore soil structural stability but was not effective with respect to improving the performance of R. sphaerocarpa plants. Besiedlung eines degradierten semiariden Bodens mit Retama sphaerocarpa L.-Setzlingen, beeinflusst durch Mykorrhiza-Inokulation und Klärschlammzugabe Ein Feldversuch wurde durchgeführt, um den Effekt einer Inokulation mit drei arbuskulären Mykorrhizapilzen (AM) (Glomus intraradices Schenck & Smith, Glomus deserticola (Trappe, Bloss. & Menge) und Glomus mosseae (Nicol & Gerd.) Gerd. & Trappe) einerseits und der Zugabe von kompostiertem Klärschlamm (SS) andererseits auf die Besiedlung von Retama sphaerocarpa L.-Setzlingen in einem mediterranen semiariden Gebiet zu untersuchen. Es wurden chemischer Nährstoffgehalt, labile C-Fraktion, biochemische Enzymaktivitäten und physikalische Bodenparameter (Aggregatstabilität) untersucht. Sechs Monate nach der Pflanzung erbrachten beide Behandlungen , die Zugabe von kompostiertem Klärschlamm und die Mykorrhiza-Inokulation , Steigerungen des Gesamtstickstoff-Gehaltes, des verfügbaren Phosphor-Gehaltes sowie der Aggregatstabilität des Bodens. Wasserlöslicher Kohlenstoff und wasserlösliche Kohlenhydrate waren nur nach Mykorrhiza-Inokulation erhöht. Boden aus der Rhizosphäre, der mit Mykorrhizapilzen inokuliert wurde, zeigte signifikant höhere Enzymaktivitäten (Dehydrogenase, Protease-BAA, saure Phosphatase und ,-Glucosidase) als der Kontrollboden. In der kurzen Periode war die Inokulation mit AM-Pilzen die effektivste Behandlung bei der Bildung von Sprossbiomasse, speziell bei G. mosseae (eine um über 146,% höhere Biomasse im Vergleich zu den Kontrollpflanzen). Die Zugabe von kompostiertem Klärschlamm allein war ausreichend, die Stabilität der Bodenstruktur wiederherzustellen, aber sie war nicht effektiv hinsichtlich der Entwicklung der R. sphaerocarpa -Pflanzen. [source]

    Broad-scale vegetation-environment relationships in Eurasian high-latitude areas

    JOURNAL OF VEGETATION SCIENCE, Issue 4 2006
    Risto Virtanen
    Hultén & Fries (1986); Ignatov & Afonina (1992); Konstantinova et al. (1992); Vitikainen et al. (1997) Abstract Question: How is tundra vegetation related to climatic, soil chemical, geological variables and grazing across a very large section of the Eurasian arctic area? We were particularly interested in broad-scale vegetation-environment relationships and how well do the patterns conform to climate-vegetation schemes. Material and Methods: We sampled vegetation in 1132 plots from 16 sites from different parts of the Eurasian tundra. Clustering and ordination techniques were used for analysing compositional patterns. Vegetation-environment relationships were analysed by fitting of environmental vectors and smooth surfaces onto non-metric multidimensional scaling scattergrams. Results: Dominant vegetation differentiation was associated with a complex set of environmental variables. A general trend differentiated cold and continental areas from relatively warm and weakly continental areas, and several soil chemical and physical variables were associated with this broad-scaled differentiation. Especially soil chemical variables related to soil acidity (pH, Ca) showed linear relationships with the dominant vegetation gradient. This was closely related to increasing cryoperturbation, decreasing precipitation and cooler conditions. Remarkable differences among relatively adjacent sites suggest that local factors such as geological properties and lemming grazing may strongly drive vegetation differentiation. Conclusions: Vegetation differentiation in tundra areas conforms to a major ecocline underlain by a complex set of environmental gradients, where precipitation, thermal conditions and soil chemical and physical processes are coupled. However, local factors such as bedrock conditions and lemming grazing may cause marked deviations from the general climate-vegetation models. Overall, soil chemical factors (pH, Ca) turned out to have linear relationship with the broad-scale differentiation of arctic vegetation. [source]