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FRC V.V. Dokuchaev Soil Science Institu... Publications | LitMetric

7 results match your criteria: "FRC V.V. Dokuchaev Soil Science Institute[Affiliation]"

The Waelz Slag from Electric Arc Furnace Dust Processing: Characterization and Magnetic Separation Studies.

Materials (Basel)

May 2024

I.P. Bardin Laboratory of Issues of Complex Ore Metallurgy, A.A. Baikov Institute of Metallurgy and Materials Science, Russian Academy of Science, 49 Leninsky Prosp, 119334 Moscow, Russia.

The Waelz slag generated during electric arc furnace dust processing is an iron-rich product with significant amounts of iron, zinc and copper. About 600-800 kg of the Waelz slag is generated per ton of the dust processed. The Waelz slag samples from two different plants were thoroughly characterized using inductively coupled plasma optical emission spectroscopy (ICP-AES), X-ray diffraction analysis (XRD), chemical phase analysis, Mössbauer spectroscopy and other supporting methods.

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Long-term application of organic and mineral fertilizers can lead to changes in the elemental composition of agroecosystem components. Both the levels of nutrients and potentially toxic elements can change, as can the potential for these elements to be available to plants through changes in soil properties. Soil and plant samples of two species (pea L.

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Paleosols are frequently used to recreate past climates. In the forest-steppe zone of the Russian Plain (Lipetsk region, Russia), Early Iron and Middle Ages defensive ramparts' buried soils were discovered. The parent material and similar topographic situations served as the foundation for the comparison of buried and surface soils.

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The fact of global climate change is generally recognized by the world scientific community. However, the spatial distribution of climatic parameters is very heterogeneous. In this regard, studies of the local response of individual territories to global climate change are of particular importance.

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The soils of arid regions are sensitive to short-term climate changes, which are most quickly manifested in the saline state of alkaline and saline soils. Long-term climate changes are reflected in more stable soil characteristics, such as grain size distribution and microstructure. These properties can be used as indicators to assess the direction and degree of soil transformation under the influence of climate change in the longer term.

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The implementation of the sustainable management of the interaction between agriculture and the environment requires an increasingly deep understanding and numerical description of the soil genesis and properties of soils. One of the areas of application of relevant knowledge is digital irrigated agriculture. During the development of such technologies, the traditional methods of soil research can be quite expensive and time consuming.

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The soil cover of semi-desert territories is sensitive to modern climatic changes, responding to a change in the composition of soil complexes. Soil microstructure features reflect minor changes in microrelief or fluctuations in the level of groundwater. This property of soil microstructure to memorize soil formation conditions is used for subsequent characterization of changes in long-term climatic trends.

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