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  • Arid land ; Brown soils ; European part of USSR ; Irrigation ; Kalmykia ; Pedogenesis ; Saline soil ; Solonets soil
  • Haloxylon aphyllum is productive and perspective cultures on typical brown slight solonets soils, its desease and insect control should be carried out. H. aphyllum can be used pasture forest stands of semideserts of the RSFSR south-east. (Ed.).
  • Introduction: soil horizons
  • Soil horizons
  • Congress ; Soil ; Soil classification ; Soil properties ; Soil science ; Taxonomy
  • The A. presents the meeting and its objective: to discuss the various concepts of soil horizons and the role that soil horizons play in soil characterization, classification and mapping. This number of Catena contains selected papers of this meeting.
  • Defining kinds of soil horizon
  • Soil horizons
  • Concept ; Soil ; Soil classification ; Soil properties
  • Some remarks on soil horizon classes
  • Soil horizons
  • Soil ; Soil classification ; Soil properties ; Soil science ; Taxonomy
  • Soil horizons are the results of pedological processes and classes of soil horizon descriptions are seen as fundamental to soil classification. A fuzzy-sets approach to horizon classes is suggested to deal with the intergrading and multivariate
  • nature of soil horizons.
  • Pedological regional variations in well-drained soils, Denmark
  • Denmark ; Pedogenesis ; Soil ; Soil classification;Classification of soils ; Soil properties ; Spatial variation ; Statistics
  • Soil profile investigations were carried out within a national 7 km grid. The profiles were classified according to the 1974 FAO-Unesco Soil Classification System. This paper describes the regional variations in soil profile development
  • and the related dominant soil formation processes.
  • Soil materials, a layer based approach to soil description and classification
  • Soil horizons
  • Australia ; Cartography ; Concept ; Land use ; New South Wales ; Soil ; Soil classification ; Soil properties
  • The Soil Conservation Service of New South Wales (Australia) is mapping soil landscapes at a scale of 1:100,000 and is using a soil layer based entity, termed soil materials, as the basic entity for soil description and classification. This paper
  • Seasonal dynamics of soil-water pressure in a cracking clay soil
  • Clay ; England ; Model ; Oxfordshire ; Precipitation ; Seasonal variation ; Soil ; Soil properties ; Soil water ; United Kingdom
  • This paper describes the results of an investigation of changes in soil water pressure head and its relationship to the macropore network in a cracking clay soil at Brimstone Farm, Oxfordshire, UK.
  • Struktura pudniho fondu v CSR. (Structure of soil fund in the Czech Socialist Republic)
  • A survey of soil fund structure in the CSR for the height soil zones of hydromorphic soils, chernozems, brown soils, illimeric podzol soils, brown forest soils and mountain podzol soils. (MS).
  • A Tolnai-dombsag genetikai talajtipusai és talajlepusztulasa. (Genetic soil types and soil erosion in the Tolna Hills)
  • The loess covered and minutely dissected hilly region of high relief is described by various soil types (brown forest soils, chernozem brown soils, chernozems, earthy barren grounds, hydromorphous soils). Surfaces are classified according
  • to the extent of soil loss.
  • Degradation of soil structure by welding. A micromorphological study
  • Agricultural practice ; Agropedology ; Limburg ; Loess ; Micromorphology ; Netherlands (The) ; Soil ; Soil erosion ; Soil properties ; Splash
  • In 1985 a plot study was started on sloping cultivated loess soils in South-Limbourg (The Netherlands) to evaluate the effects of various cropping systems of fodder maize on runoff, soil loss and crop yield under natural rainfall. In 1988
  • , in addition a soil micromorphological investigation was undertaken of the soil layer at and immediately below the soil surface on the experimental plots. In this paper the results of the micromorphological analysis of the processes of soil structure
  • degradation and crust formation are presented including the applicability of the McIntyre model of soil crust formation.
  • Soil science reference books
  • Bibliography ; Soil ; Soil classification ; Soil properties ; Soil science ; Textbook
  • This paper focuses on the 7 major soil reference books that were published between 2000 and 2012 : Handbook of Soil Science (2000 and 2012), Encyclopedia of Soil Science (2002 and 2006), Encyclopedia of Soils in the Environment (2005), Encyclopedia
  • of Soil Science (2008), and Soil Science — Reference collection (2009). These soils science reference books contain 1920 articles authored by some 2000 authors. The Handbook of Soil Science covers the basic subdisciplines (physics, chemistry, biology
  • , pedology) most extensively whereas the encyclopedia have more applied entries/articles. Overall, these intradisciplinary reference works show that the soil science discipline is vibrant and has a rapidly expanding knowledge base.
  • [b1] Univ. of Wisconsin, Dep. of Soil Science, Madison, Etats-Unis
  • Jordklassificering Danmark. Basisdatakort = Soil classification of Denmark. Soil maps.
  • Relation of weathering and soil formation in the mountain soils of Western Georgia
  • Soil formation and soils of the Mediterranean coastal belt of Libya
  • Fire impacts on soil nutrients and soil erosion in a Mediterranean pine forest plantation
  • Ecosystem ; Fire ; Forest ; Israel ; Rill wash;Runoff ; Soil ; Soil erosion ; Soil properties ; Soil science
  • Detailed measurements of soil nutrients, runoff and sediment discharge were made in two plots about 200 m2 each in a plantation of Aleppo and Brutia Pine in the Mediterranean climatic region of Israel. One of the plots was affected by a moderate
  • wildfire at the end of summer 1988. The results suggest that light and moderate forest fires may increase soil fertility without cousing a marked difference in soil runoff and erosion.
  • Soil horizon use by the U.S. soil survey
  • Soil horizons
  • Concept ; Soil ; Soil classification ; Soil properties ; Soil science ; Taxonomy ; United States
  • There are many more possibilities for designating horizons and layers in field descriptions than there are when applying the defined diagnostic horizons that are used in Soil Taxonomy. The first set are based on qualitative judgements, the latter
  • are based on quantitative measurements. The Soil Survey in the United States has found it useful to keep the two kinds of horizon designations separate.
  • Detachment of soil particles by shallow flow : sampling methodology and observations
  • Erodibility ; Grain size distribution ; Methodology ; Precipitation ; Rill wash ; Sampling ; Sediment budget ; Soil ; Soil erosion ; Soil properties ; Splash
  • This study compares several methodologies for conducting flow detachment tests. Particularly, differences in initial soil moisture conditions and soil surface characteristics due to the combined effects of various types of crops and applied raindrop
  • kinetic energy caused differences in soil detachability by overland flow. Furthermore, soil sampling in different periods of the year resulted in variations in soil detachment indicating a seasonal trend in soil detachability.
  • Farmer perception of soils in the mountains of the Dominican Republic
  • Dominican Republic ; Environmental perception ; Perception ; Rural geography ; Soil ; Soil conservation ; Soil erosion
  • In Las Cuevas north of Azua 80 farmers were interviewed about their soils : 48% of them were aware of soil erosion, but had little interest in soil conservation. None of the farmers named more than six kinds of soil. Stoniness or soil depth were
  • not considered by them to be important in defining soil quality. - (DWG)
  • Soil erosion and soil structure in Impact of water and external forces on soil structure. Selected papers of the 1st Workshop on soilphysics and soilmechanics, Hannover 1986.
  • Recent studies show that measured soil losses due to water erosion differ significantly from estimated values using nomographs derived from loess soils. Under identical environmental conditions these deviations seem to be caused by the parent
  • material affecting soil structure. The final questions show that research on the interaction between soil loss and soil structure needs to be forced.