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Journal articles on the topic 'Gleyic Podzols'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Jonczak, Jerzy. "Vertical distribution of Cu, Ni and Zn in Brunic Arenosols and Gleyic Podzols of the supra-flood terrace of the Słupia River as affected by litho-pedogenic factors." Forest Research Papers 75, no. 4 (2015): 333–41. http://dx.doi.org/10.2478/frp-2014-0030.

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Abstract The aim of the study was to assess the influence of lithological and pedogenic factors in the shaping of Cu, Ni and Zn distribution patterns in the profiles of Brunic Arenosols and Gleyic Podzols of the lower supra-flood terrace of the Słupia River, which is located outside the range of significant anthropogenic sources of pollution with these metals. The contents of the investigated metals were analysed in aqua regia extracts of samples collected from three profiles of Brunic Arenosols, formed from river sands, and three profiles of Gleyic Podzols, formed from river sands transformed

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2

Jonczak, Jerzy. "Vertical distribution of Cu, Ni and Zn in Brunic Arenosols and Gleyic Podzols of the supra-flood terrace of the Słupia River as affected by litho-pedogenic factors." Forest Research Papers 75 (4) (December 1, 2015): 333–41. https://doi.org/10.2478/frp-2014-0030.

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The aim of the study was to assess the influence of lithological and pedogenic factors in the shaping of Cu, Ni and Zn distribution patterns in the profiles of Brunic Arenosols and Gleyic Podzols of the lower supra-flood terrace of the Słupia River, which is located outside the range of significant anthropogenic sources of pollution with these metals. The contents of the investigated metals were analysed in aqua regia extracts of samples collected from three profiles of Brunic Arenosols, formed from river sands, and three profiles of Gleyic Podzols, formed from river sands transformed by eolia

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3

Vasil'chuk, Yurij Kirillovich, Jessica Yur'evna Vasil'chuk, and Alexander Pavlovich Ginzburg. "Cryogenic soils in the area of Batagaika crater in Northern Yakutia." Арктика и Антарктика, no. 3 (March 2020): 52–99. http://dx.doi.org/10.7256/2453-8922.2020.3.33599.

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The subject of this research is the soil and catena soils in the area of Batagaika crater located in Verkhoyansk District of Northern Yakutia. Soils are usually represented by Cryosols Gleyic and Podzols Entic, which are formed on eluvial and eluvial-deluvial deposits under larch forests. Exploration of soils was carried out in 2017, 2018 and 2019. On the slope to the Batagaika crater is the soil-geochemical catena, which included the ridge-top surface of the slope of Kirgilyah Mountain, the middle part of the slope, as well as levelled surfaces of Batagaika crater. Soil types are described in

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4

Jonczak, Jerzy, Marek Degórski, and Bogusława Kruczkowska. "Comparing quartz silt surface microstructures in two sandy soils in young-glacial landscape of northern Poland." Soil Science Annual 67, no. 3 (2016): 131–39. http://dx.doi.org/10.1515/ssa-2016-0016.

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AbstractThe studies on quartz silt surface microstructures using scanning electron microscopy (SEM) were performed in Brunic Arenosol and Gleyic Ortsteinic Podzol, as major components of soil cover of the lower supra-flood terrace of the Słupia River, N Poland. Brunic Arenosols have developed from coarse- and medium-grained fluvioglacial sands, whereas Podzols from aeolian sands of mid-Holocene age, which in some places were covered with younger aeolian deposits. A group of at least 100 randomly selected grains from each soil horizon have been analyzed. The grains were classified into one of t

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Khitrov, N. B. "Representativeness of mixed samples for evaluation of organic carbon in soil." Dokuchaev Soil Bulletin, no. 122 (March 26, 2025): 5–20. https://doi.org/10.19047/0136-1694-2025-122-5-20.

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The aim to solve the methodological problem of assessing variability of soil organic carbon content (Corg) in layer 0–20 cm based on 10-fold independent mixed sampling from the same field during one day. The soil sampling was carried out on 4 fields ranging from 6 to 16 hectares (Tver region). The soil cover pattern is represented by patches of agrosod-podzolic gleyic sandy loam and loam soils (Albic Retisols (Aric, Loamic)) developed from binary deposits and agrosod-podzols (Albic Podzols (Aric, Arenic)) developed from sands underlying loamy moraine from the depth 80–150 cm. It has been estab

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6

Daugaviete, Mudrite, Andis Lazdins, Dagnija Lazdina, Kristaps Makovskis, and Uldis Daugavietis. "Growth and Yield of 15-Year Plantations of Pine, Spruce and Birch in Agricultural Land." Rural Sustainability Research 37, no. 332 (2017): 38–50. http://dx.doi.org/10.1515/plua-2017-0005.

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Abstract The growth data and the potential returns from 15-year-old plantations of pine Pinus sylvestris L. (6 trial sites), spruce Picea abies Karst L. (9 trial sites) and silver birch Betula pendula Roth (13 trial sites), established in abandoned agricultural lands in a variety of soil types (sod calcareous, anthrosols, podzolic, podzols, gley, podzolic gley, alluvial), using the planting density 2,500 and 3,300 and also 5,000 trees/ha are analysed. For tree plantations in agricultural soils (alluvial sod-gley, gley-sod podzolic, sod-podzolic gley, typic podzol) at the survival of 80-98% the

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7

Mandre, Malle, Mari Tilk, and Priit Kõresaar. "Chemical characteristics of soils in Scots pine forests of Cladina and Vaccinium vitis-idaea site types on coastal dunes of Baltic Sea." Forestry Studies / Metsanduslikud Uurimused 49, no. 1 (2008): 5–12. http://dx.doi.org/10.2478/v10132-011-0058-x.

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Chemical characteristics of soils in Scots pine forests of Cladina and Vaccinium vitis-idaea site types on coastal dunes of Baltic Sea The coastal dunes of Southwest Estonia have been undergoing a process of stabilisation and are today covered predominantly with Scots pine forests. For the investigation of soils on dunes sampling sites were selected according to topographical positions and forest site types: two sites in Cladina and two sites in Vaccinium vitis-idaea site types on dunes of different heights. The prevailing soils on dunes are Gleyic Podzols, which are generally poor in humus, w

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8

Ganbat, Byambaa, and Bolormaa Tseden-Ish. "Characteristics and properties of soil reaction (pH) of Mongolian forest." Mongolian Journal of Geography and Geoecology 61, no. 45 (2024): 208–17. https://doi.org/10.5564/mjgg.v61i45.3397.

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This study aimed to identify the soil pH of forests distributed across Mongolia and determine the types of forest soil and their corresponding reaction environments at different depths. The study was based on 1558 samples collected from 301 profiles of forest soil, in which data were collected in Mongolia before 2024. The primary forest soil types found in Mongolia included Umbrisols (Gelic), Leptic umbrisols, Podzols, Mollic Umbrisols, Gleyic Umbrisols, Podzols (Arenic), and fluvisols. The Tukey test was employed to analyze differences in forest soil pH between soil types. Also, the study was

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9

Lasota, Jarosław, Małgorzata Wiecheć, Ewa Błońska, and Stanisław Brożek. "Biodiversity indexes in relation to soil properties in upland fir forests (Abietetum albae)." Forest Research Papers 78, no. 2 (2017): 120–28. http://dx.doi.org/10.1515/frp-2017-0013.

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Abstract The aim of this study was to present the relationship between soil properties and biodiversity indexes in upland fir (Abies alba) forest associations (Abietetum albae). Our study was conducted in six areas representing the growth conditions of upland fir forests and the research plots were located in the Roztoczański and Świętokrzyski National Parks as well as Przedbórz, Radomsko, Piotrków and Janów lubelski Forest District. on every plot, the topography was described, soil cores were examined and samples for laboratory analysis were taken. the following characteristics were determine

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10

Walker, Tony R. "Properties of selected soils from the sub−arctic region of Labrador, Canada." Polish Polar Research 33, no. 3 (2012): 207–24. http://dx.doi.org/10.2478/v10183-012-0013-4.

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Abstract Atotal of 212 soil profiles were described and assessed for physical and chemical properties during July 2006 as part of an Ecological Land Classification study along the Churchill River in central Labrador. Two major soil types were found in the study area along the Churchill River: Podzols and Organic soils. Podzolic soils covered approximately 60% and Organic soils occurred in 24% of the study area. Approximately 15% of the study area was classified as rock and other unconsolidated material. Summary results and a sub−set of the following soil units (from 10 soil profiles) are prese

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Jarosław, Lasota, Wiecheć Małgorzata, Błońska Ewa, and Brożek Stanisław. "Biodiversity indexes in relation to soil properties in upland fir forests (Abietetum albae)." Lesne Prace Badawcze / Forest Research Papers 78, no. 2 (2017): 120–28. https://doi.org/10.1515/frp-2017-0013.

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The aim of this study was to present the relationship between soil properties and biodiversity indexes in upland fir (<em>Abies alba</em>) forest associations (<em>Abietetum albae</em>). Our study was conducted in six areas representing the growth conditions of upland fir forests and the research plots were located in the Roztoczański and Świętokrzyski National Parks as well as Przedbórz, Radomsko, Piotrków and Janów lubelski Forest District. on every plot, the topography was described, soil cores were examined and samples for laboratory analysis were taken. the following

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12

Chodorowski, Jacek, Piotr Bartmiński, Andrzej Plak, and Ryszard Dębicki. "Soil Cover of the City of Lublin (Eastern Poland)." Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 79 (October 4, 2024): 69–85. http://dx.doi.org/10.17951/b.2024.79.0.69-85.

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Lublin is a voivodeship city located in the Lublin Upland (Eastern Poland). The study aimed to present the spatial differentiation of soils of the city of Lublin and some of their properties. The knowledge of soil cover is very important for spatial planning and for protection and proper use of soil resources of each city. The environmental-genetic map of Lublin’s soils included in this work was made on the basis of soil-agricultural map in the scale 1:25 000 of Lublin and the soil-habitat map of the Świdnik Forest District. The soil units distinguished on the map were classified according to

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13

PANKIV, Zenoviy, Olena KALYNYCH, Taras YAMELYNETS, and Oksana BONISHKO. "FORMS OF FERRUM IN PROFILE-DIFFERENTIATED SOILS OF PRECARPATHIAN UKRAINE AND THEIR ROLE IN DIAGNOSTICS OF SOIL-FORMING PROCESSES." AgroLife Scientific Journal 12, no. 2 (2023): 140–47. http://dx.doi.org/10.17930/agl2023219.

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The profiles of sod-podzolic surface-gleyed soils (Stagnic Retisols) and brown podzolic soil profile (Neocambic Gleyic Retisols) are characterized by differentiation of gross Ferrum content and moderately low degree of Ferrum content. The composition of gross Ferrum is dominated by Fes, the maximum share of which is characteristic of A2B g horizon. The minimum content of Fes belongs to A1A2 g, which indicates the processes of destruction of primary and secondary minerals in the upper part of the profile. The accumulation of Ferrum oxides was diagnosed in the ortstein and nodules of the studied

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14

Nykytiuk, Y., and O. Kravchenko. "Landscape and soil cover diversity in Polissia and Forest-Steppe of Ukraine." Agrology 7, no. 3 (2024): 95–106. http://dx.doi.org/10.32819/202413.

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Recent research has revealed the patterns of spatial and temporal variability of crop yields for the Polissia and the Forest-Steppe regions of Ukraine. In addition, the approaches to differentiating agroeconomic and agroecological components in the variability of the productive potential of the territories were developed. Approaches have been developed to quantify the spatial and temporal variability of soil erosion for individual areas of the region. The issue of assessing the impact of erosion processes on crop yields at the regional level remains unresolved. The diversity of landscapes and

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15

Akhmetova, G. V. "Geochemical features of soils in an undulating glaciolacustrine sandy plain in the middle taiga subzone of Karelia." Dokuchaev Soil Bulletin, no. 100 (January 3, 2020): 53–82. http://dx.doi.org/10.19047/0136-1694-2019-100-53-82.

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The geochemically conjugate series of soils (Albic Podzol – Albic Podzol Gleyc – Hystosol) formed on an undulating glaciolacustrine plain in the middle taiga of Karelia was investigated. Surveys for redox conditions showed them to vary from oxidizing in automorphic soils to reducing in soils occupying accumulation-favoring locations. The geochemical coefficients descriptive of the features of accumulation and directions of migration in the studied soils were calculated and analyzed. The distribution of silicic acid and a majority of sesquioxides inside the profile of the studied soils is typic

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16

Tatiana, V. Raudina, I. Istigechev Georgyi, and V. Loiko Sergey. "Soil-ecological conditions of the north taiga flat-mound bog, Western Siberia." Acta Biologica Sibirica 9 (April 24, 2023): 195–208. https://doi.org/10.5281/zenodo.7854816.

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Of particular interest in the north of Western Siberia are frozen flat-mound bogs. Being formed in a transitional climatic zone, on the southern front of the permafrost zone, these frozen peatlands may turn out to be highly reactive upon thawing and deliver high amounts of solutes to the hydrological network. A detailed study of a flat-mound bog was carried out in a key area of about 3 hectares (Purovsky district, Yamalo-Nenets Autonomous Okrug). The soil-ecological conditions of the site are described, as well as the effect of spatial heterogeneity on the composition and properties of soils.

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17

Gabov, D. N., V. A. Beznosikov, and B. M. Kondratenok. "Polycyclic aromatic hydrocarbons in background podzolic and gleyic peat-podzolic soils." Eurasian Soil Science 40, no. 3 (2007): 256–64. http://dx.doi.org/10.1134/s1064229307030039.

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18

Ananko, T. V., M. I. Gerasimova, and N. V. Savitskaya. "Podzolic-brown soils of the Far East on the Soil map of Russian Federation, scale 1 : 2.5 M, and their correlation with soils in the Russian soil classification." Dokuchaev Soil Bulletin, no. 118 (March 25, 2024): 48–78. http://dx.doi.org/10.19047/0136-1694-2024-118-48-78.

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Podzolic-brown forest soils on the Soil Map of Russian Federation, scale 1 : 2.5 M, are widespread on the plains and plateaus of the Far East, referred to the Eastern brown-forest-soil area in the scheme of soil-geographical zoning. There, in Primorye and Priamurye regions, they are confined to various parent rocks and to different climatic and biota conditions. In the Classification of Soils of Russia (2004, 2008), there are no direct analogues of podzolic-brown soils in the map legend. To name these soils in the Russian classification system, regional publications (N.A. Kreida, G.I. Ivanov,

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19

Kuznetsov, N. B., S. A. Alekseeva, G. V. Shashkova, T. Ya Dronova, and T. A. Sokolova. "Buffer capacities of podzolic and peat gleyic podzolic soils to sulfuric and nitric acids." Eurasian Soil Science 40, no. 4 (2007): 353–66. http://dx.doi.org/10.1134/s1064229307040011.

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20

Litvinovich, A. V., and O. Yu Pavlova. "Changes in the humus status of a layland sandy gleyic soddy-podzolic soil." Eurasian Soil Science 40, no. 11 (2007): 1181–86. http://dx.doi.org/10.1134/s1064229307110051.

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21

Smaga, I. S. "Diagnostic problems of elementary soil processes and profile-differentiated soils of the Precarpathian region." Fundamental and Applied Soil Science 17, no. 1-2 (2016): 40–48. http://dx.doi.org/10.15421/041604.

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Present condition, scientific concepts and ways of further development of diagnosis problem of elementary soil processes and genetic nature profiled-differentiated gleyed soils of the Pre-Carpathian region, known as brownish-podzolic, brownsoil-podzolic and sod-podzolic, based on stable indicators of soil properties are studied. Eluvial-illuvial differentiation nature of the soil profile of the studied soils is founded. The aim of research was to develop criteria for the diagnosis of elementary soil processes and genetic nature profiled-differentiated soil deposits of Ciscarpathia and discover

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22

Zamotaev, I. V., and V. P. Belobrov. "Position of soils and soil-like formations of football grounds in the soil classification system." Dokuchaev Soil Bulletin, no. 79 (July 1, 2015): 91–110. http://dx.doi.org/10.19047/0136-1694-2015-79-91-110.

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Under consideration is the classification of soils and soil-like formations in special landscapes and the football ground in particular. The latter is usually represented by soils subjected to human impacts of varying intensity: from weakly transformed by technogenic processes to artificial soils or technogenic superficial formations. The objects of research are more than 40 football grounds in Russia and the Republic of Byelarus. They differ in the age (exploitation time), regular and intensive technogenic loads, natural conditions and soil properties. The football grounds under study were di

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23

Haskevych, Volodymyr. "Change of granulometric composition of drained soils of Male Polissia in the context of development of degradation processes." Visnyk of the Lviv University. Series Geography, no. 52 (June 27, 2018): 42–52. http://dx.doi.org/10.30970/vgg.2018.52.10167.

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Sod-podzolic (Albenuvisoils Gleyic), meadow (Gleyic Chernic Phaeozems) and sod (Arenosols) soils are typical for Male Polissia. In the natural state, these soils are waterlogged, characterized by unsatisfactory physical properties, unsuitable for agricultural use. After the drainage reclamation, the soils are intensively used as arable land, pastures, and hayfields. The drainage has led to a significant decrease in groundwater levels, increased the washing water regime, intensified the processes of lessivage, which affected the physical properties of soils, in particular, granulometric composi

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24

Kovaleva, Ekaterina Ig, Sergey Ya Trofimov, and Sergey A. Shoba. "The functioning of petroleum hydrocarbon contaminatied soils in the taiga zone of Western Siberia." Lomonosov Soil Science Journal 79, no. 4, 2024 (2024): 214–27. https://doi.org/10.55959/msu0137-0944-17-2024-79-4-214-227.

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The soils of two pairs of catena were studied under conditions of petroleum hydrocarbon (PH) contamination and lack of exposure within the Middle Taiga subzone (Tyumen region). 1st pair of catena: Gleyic Albic Podzol, Dystric Gleyic Histic Fluvisols, Dystric Gleyic Fluvisols; 2nd pair of catena:Albic Gleyic Retisols, Albic Gleyic Histic Retisols, Dystric Histic Gleysols . The effects of PH contamination on the biological characteristics of soils (respiration and catalase activity) and the possibility of their use for rationing the content of PH in soils were evaluated. The lateral migration of

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25

Kammer, Frank v. d., and Ulrich Förstner. "Natural colloid characterization using flow-field-flow-fractionation followed by multi-detector analysis." Water Science and Technology 37, no. 6-7 (1998): 173–80. http://dx.doi.org/10.2166/wst.1998.0750.

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A design for a flow-field-flow-fractionation with UV/VIS-, fluorescence- and laser-light-scattering-detectors is presented and tested with extracts from a humus rich horizon of a gleyic podzol. It is tested to show how the system can retrieve relevant information about changes in the constitution of the colloid samples. The main objective is the investigation of colloid alteration during processes provoked by main geochemical driving forces (e.g. pH or ionic strength), in this case changes of redox potential. Therefore fluorescence- and UV/VIS-fractograms are taken at different wavelengths and

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26

Golodnaya, Olga M., and Elena A. Zharikova. "Particle-Size Distribution in Soils of the Khankaiskiy Nature Reserve (Primorye Territory)." UNIVERSITY NEWS. NORTH-CAUCASIAN REGION. NATURAL SCIENCES SERIES, no. 2 (210) (June 28, 2021): 99–105. http://dx.doi.org/10.18522/1026-2237-2021-2-99-105.

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Soil texture is determined and the features of particle-size vertical distribution in soils of different landscapes of the Khankaiskiy Nature Reserve are considered. Three variants of the distribution of clay (&lt;0.001 mm) and physical clay (&lt;0.01 mm) fractions along the vertical profiles soils are identified: accumulative, regressive, with a maximum in the middle-profile horizon and with their approximately equal contents in the upper and the lower horizons. A regressive variant is revealed in burozems gleyic, podzoliс-brownzems, dark-humus gley and alluvial meadow gley soils. The

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27

Sokolova, T. A., I. I. Tolpeshta, and I. V. Topunova. "Biotite weathering in peaty-podzolic gleyic soil under conditions of a model field experiment." Moscow University Soil Science Bulletin 65, no. 2 (2010): 61–68. http://dx.doi.org/10.3103/s0147687410020031.

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28

Litvinovich, A. V., O. Yu Pavolva, A. I. Maslova, and D. V. Chernov. "The potassium status of sandy gleyic soddy-podzolic soils under forest, cropland, and fallow." Eurasian Soil Science 39, no. 7 (2006): 785–91. http://dx.doi.org/10.1134/s1064229306070131.

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29

Ivanyuk, Halyna. "Grey forest soils in the different classification systems." Visnyk of the Lviv University. Series Geography, no. 51 (December 27, 2017): 120–34. http://dx.doi.org/10.30970/vgg.2017.51.8851.

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According to various data, the area of grey forest soils in the world is 94–120.2 million ha, in Ukraine – 4.7–5.5 million ha (about 9 % of the country’s territory). The diversity of conditions for the formation of these soils, discussions about their genesis are the causes of different approaches to the classification of grey forest soils. The history of the classification of grey forest soils is analysed; the most common variants of their classification in Ukraine are presented. Seeking to find approximate equivalents, an attempt to find grey forest soils in the classification systems of dif

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Litvinovich, Andrey, Anton Lavrishchev, Vladimir Bure, Tara Grujić, and Elmira Saljnikov. "Agrogenic evolution of soddy-podzolic soil: Feasibility of repeated re-involvement in cultivation of the fallow lands formed on band clays." Zemljiste i biljka 71, no. 2 (2022): 11–26. http://dx.doi.org/10.5937/zembilj2202086l.

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Transformations of the soddy-podzolic gleyic clay soil in a long-term agricultural use (> 200 years) was studied in Leningrad region, northwest Russia. This feasibility study investigated the possibility of re-cultivation of these soils after long term fallowing. Morphological structure, particle size distribution, content and ratio of ferrous and oxide forms of iron in the profile of virgin (indigenous forest) and arable drained soil were analysed. In addition, changes in the organogenic-profile were traced in the course of long-term agrogenesis (> 200 years). In virgin forest soil, dur

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31

Beznosikov, V. A., and E. D. Lodygin. "Characteristics of the structure of humic substances of podzolic and peaty podzolic gleyey soils." Russian Agricultural Sciences 35, no. 2 (2009): 103–5. http://dx.doi.org/10.3103/s1068367409020116.

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32

Karavanova, E. I., and M. S. Malinina. "Spatial and temporal variation in the elemental composition of soil solution from gleyic peaty-podzolic soils." Eurasian Soil Science 40, no. 8 (2007): 830–38. http://dx.doi.org/10.1134/s1064229307080042.

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33

Чебыкина, Е. В., Т. В. Таран, П. А. Котяк, and М. А. Казнина. "AGROCHEMICAL ASSESSMENT OF LONG-TERM USE OF STRAW AND MINERAL FERTILIZERS ON SODDY PODZOLIC GLEYIC SOIL." Vestnik APK Verhnevolzh`ia, no. 4(64) (December 26, 2023): 5–13. http://dx.doi.org/10.35694/yarcx.2023.64.4.001.

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В работе представлена агрохимическая оценка дерново-подзолистой глееватой почвы в агроландшафтах Ярославской области при многократном использовании соломы и минеральных удобрений как при раздельном, так и совместном их внесении. Экспериментальная работа проводилась в многолетнем трёхфакторном стационарном полевом опыте. Представлен анализ полученных на 28-й год после распашки многолетней залежи и закладки опыта экспериментальных данных по вариантам применения различных систем удобрения при отвальной системе обработки почвы и интегрированной системе защиты растений от сорняков. За 28-летний пер

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34

Balsanova, L. D. "Ecological Sustainability of Soils of Recreational Zones of the Eastern Shore of Lake Baikal." Bulletin of Irkutsk State University. Series Biology. Ecology 49 (2024): 52–66. https://doi.org/10.26516/2073-3372.2024.49.52.

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Tourist activities on the eastern coast of Lake Baikal have a significant impact on soils. The main load falls on its coastal territory, which is characterized by the greatest vulnerability. There is also the problem of assessing the resistance of soils to anthropogenic impacts, taking into account the natural and climatic characteristics of the territory. Soil studies were carried out within the middle part of the eastern coast of Lake Baikal from the Barguzinsky Bay to the Ust-Selenginsky depression. In soil samples, the pH was determined by a potentiometric method; exchangeable cations - co

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35

Mitrofanov, Yu I., M. V. Gulyaev, and N. K. Pervushina. "Influence of agromelioration and drainage methods on the field crops productivity." Вестник российской сельскохозяйственной науки, no. 3 (December 15, 2023): 63–69. http://dx.doi.org/10.31857/2500-2082/2023/3/63-69.

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The effectiveness of ameliorative strip loosening to a depth of 50-60 cm and volumetric soil slotting to 45-50 cm, their influence on the productivity of field crops and agrophysical properties of drained soils with different ameliorative systems (interdrainage distance of 18 and 28 m) was studied. The experiment was carried out in the period 2015-2021. at the Gubino agricultural polygon of the All-Russian Research Institute of Reclaimed Lands (Tver Region). The soil is soddy-podzolic cultivated light loamy gleyic, drained by closed pottery drainage, formed on a moraine. Volumetric slotting wa

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Wang, C., G. R. Brewster, and K. T. Webb. "Micromorphological evidence of pedogenetic pathway of a Podzolic Gray Luvisol (Falmouth series) in Nova Scotia." Canadian Journal of Soil Science 75, no. 4 (1995): 491–96. http://dx.doi.org/10.4141/cjss95-070.

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A catena of Podzolic Gray Luvisols (Falmouth series) – Gleyed Gray Luvisols (Queens series) – Orthic Gleysols (Kingsville series) is commonly found on fine loamy, weakly calcareous parent materials in Nova Scotia, with Podzolic Gray Luvisols occupying the best drained landscape positions. The hypothesis that podzolic B horizons of Podzolic Gray Luvisols were developed on degraded Bt horizons was investigated by micromorphological characterization of one Podzolic Gray Luvisol pedon. Although not visible in field examinations, argillans were common in thin sections of the Bf and Bm horizons. The

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Nikorych, V. A., and I. V. Chervonogrodska. "Colouristic criteria of S-matrix of the precarpathians brownish-podzolic gleyed soils." Fundamental and Applied Soil Science 17, no. 1-2 (2016): 49–64. http://dx.doi.org/10.15421/041605.

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The scientific literature dedicated to the analysis of peculiarities of the soils colouring and interconnection the genetic horizons colour as well as separate morphological elements with their properties have been analyzed. The identification of colour of genetic horizons in 20 profiles of brownish-podzolic gleyed soils of Ukrainian and Polish Precarpathians has been conducted. The colour of investigated genetic horizons and separate morphological elements was determined according to both national and international systems. The analysis of the appropriateness of national approaches rejecting

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Bouda, S., and K. P. Isaac. "Influence of soil redox conditions on oxidation of biotite." Clay Minerals 21, no. 2 (1986): 149–57. http://dx.doi.org/10.1180/claymin.1986.021.2.04.

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AbstractBiotites from three peaty gleyed podzol soil profiles on ranite bedrock were examined to investigate the oxidation of the octahedral Fe during weathering. Oxidation of these biotites as determined by Mössbauer spectroscopy shows a good correlation with the in situ measured soil Eh values of the sampled horizons. In every soil profile the highest Eh measured is in the A horizon and the lowest in the C horizon. Similarly, biotites from the A horizons are the most oxidized compared with those from the lower horizons. In most of the samples the oxidation is accompanied by loss of K+ from t

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Matinian, Natalia N., Anastasia L. Gusareva, Kseniia A. Bakhmatova, and Anastasia A. Sheshukova. "Microbiological indicators and heavy metal concentration in ecological assessment of urban soils of Saint Petersburg, Russia." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 13, no. 1 (2020): 214–23. http://dx.doi.org/10.24057/2071-9388-2019-63.

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This paper aimed to characterize urbostratozems (Urbic Technosol, WRB) of Saint Petersburg located in industrial (“Electrodepo” railway station) and residential (region Polish Garden) zones. These soils were also compared with background (natural) soddy podzol soil (Umbric Albic Gleic Podzol, WRB) sampled in recreational zone (suburban park “Oranienbaum”). Soil samples were collected from soil horizons for chemical analysis and from top of soils for microbialogical analysis in June of 2012. Chemical properties (pH, total organic carbon, mobile forms of K and P) and content of heavy metals (Pb,

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Muromtsev, N. A., and K. B. Anisimov. "THE PECULIAR FORMATION OF THE WATER REGIME IN SODDY-PODZOLIC SOIL IN DIFFERENT POSITIONS OF SOIL CATENA." Dokuchaev Soil Bulletin, no. 77 (March 1, 2015): 78–93. http://dx.doi.org/10.19047/0136-1694-2015-77-78-93.

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Under consideration is the dynamics of moisture reserves and soil water potential in different parts of the catena represented by soddy-podzolic slightly gleyed soil. Peculiar features in the development of moisture reserves have been identified in different elevated positions of this catena and their transformation in time depending on the weather conditions. It is shown that the dynamics of soil water potential in dependence on the depth of the soil profile and time well agrees with the peculiar changes in moisture reserves.

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Troyan, Tatiana. "Efficient control of the productivity of agrophytocenosis of soybean (Glicyne max (L.) Merill)." BIO Web of Conferences 64 (2023): 02002. http://dx.doi.org/10.1051/bioconf/20236402002.

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Around the world, there is a surging demand for soy, the ‘king of beans’. Soy is a globally traded foodstuff produced in both temperate and tropical regions and is a major source of protein and vegetable oils. In the conditions of the Kaliningrad region, the duration of soybean vegetation in soddy-weakly podzolic gleyic light loamy soil, with the medium reaction close to neutral, high and very high content of mobile phosphorus, and exchangeable potassium attains 144 days. The agrophytocenosis productivity is controlled through application of different mineral and bacterial fertilizers. Analysi

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Voronin, A. N., A. M. Trufanov, P. A. Kotyak, and S. V. Shchukin. "Influence of tillage and fertilizers on the fauna of sodpodzolic gleyic soil and the yield of field crops." Siberian Herald of Agricultural Science 53, no. 3 (2023): 5–14. http://dx.doi.org/10.26898/0370-8799-2023-3-1.

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The results of the study of the mouldboard, surface-mouldboard and surface soil treatment systems, as well as straw-based fertilizer systems used both separately and in combination with full mineral fertilizer are presented. Data for 2019-2021 on soil fauna, yield of perennial grasses of the 1st and 2nd years of use and spring wheat are given. The studies were conducted on sod-podzolic gleyic middle-loamy soils (experimental field of the Yaroslavl State Agricultural Academy). During the period under study, the highest abundance of beneficial soil fauna (earthworms (Lumbricina), ladybugs (Cocci

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Kudin, Maxim V., Evgeniy B. Evseev, Dmitry K. Garbaruk, Alesya N. Voronetskaya, and Alexander V. Dragun. "Parameters of the transition of radionuclides into the biomass of miscanthus gigantus on the lands of the exclusion zone of the Polesie State Radiation-Ecological Reserve." Journal of the Belarusian State University. Ecology., no. 4 (December 27, 2024): 44–54. https://doi.org/10.46646/2521-683x/2024-4-44-54.

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The article describes a new culture for Belarus, Miscanthus gigantus, introduced in the conditions of Belarusian Polesie, and also describes its biological and environmental features. It is proposed to use the studied crop for energy purposes. It is assumed that growing plants for energy purposes in Belarus is most promising in the natural and climatic conditions of the Gomel region. The cultivation of miscanthus contributes to solving a number of significant environmental issues. First of all, it ensures obtaining a sustainable harvest of high-quality crop products, which increases the effici

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Karbivska, U. M., A. O. Butenko, V. I. Onichko, et al. "Effect of the cultivation of legumes on the dynamics of sod-podzolic soil fertility rate." Ukrainian Journal of Ecology 9, no. 3 (2019): 8–12. http://dx.doi.org/10.15421/2019_702.

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The effect of cultivation of legumes on the fertility rate of sod-podzolic surface-gleyed soil has been investigated. Based on the obtained results it has been found that on average, during the years of cultivation, the fertilizer factor with a percentage of 62% turns out to be more influential in terms of yield obtained from 1 ha of dry mass. The highest nutrient content is observed on the alfalfa variant: alkaline hydrolyzed nitrogen-80.4 mg/kg of soil, mobile phosphorus-81.5 mg/kg of soil and exchangeable potassium-77.3 mg/kg of soil.

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Sokolova, T. A., I. I. Tolpeshta, and I. V. Topunova. "Bentonite variations in a peaty-podzolic-gleyish soil under the field model experiment conditions." Moscow University Soil Science Bulletin 68, no. 3 (2013): 104–15. http://dx.doi.org/10.3103/s0147687413030083.

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Tsybulka, Mikalai M., and Yury V. Putyatin. "Biological availability of 137Cs and 90Sr in soddy-podzolic soils in the long period of the accident at the Chernobyl NPP." Journal of the Belarusian State University. Ecology, no. 4 (December 27, 2022): 108–17. http://dx.doi.org/10.46646/2521-683x/2022-4-108-117.

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The content of 137Cs and 90Sr forms in soddy-podzolic automorphic and gleyic soils of different textures (loamy, sandy loamy, sandy) was studied. It has been established that over a long post-accident period, the physical and chemical forms of 137Cs and 90Sr have been transformed in soils, and a dynamic balance has come in their content. 137Cs compounds have undergone non-exchange fixation, and their content in the form available to plants is currently an insignificant fraction -5-15 %. 90Sr compounds, on the contrary, are predominantly in easily accessible forms, which make up from 60 to 75 %

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Mitrofanov, Yu I., L. V. Pugacheva, M. V. Gulyaev, and N. K. Pervushina. "The effect of drainage, fertilizers, and agro-reclamation techniques on spring wheat productivity." Grain Economy of Russia, no. 6 (December 20, 2023): 82–89. http://dx.doi.org/10.31367/2079-8725-2023-89-6-82-89.

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The current study was conducted at the agricultural site ‘Gubino’ of the All-Russian Research Institute of Reclaimed Lands (Tver Region) in 2011–2022. The purpose was to study the efficiency of drainage of waterlogged soils, fertilizers and agro-reclamation techniques when growing spring wheat in the conditions of the North-Western part of the Non-Blackearth region. The soil of the agricultural site was soddy-podzolic, light loamy and gleyic sandy loam, drained by closed drainage. The field trials have established the influence of drainage of gleyic soils, the use of fertilizers, volumetric sl

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Tolpeshta, I. I., and T. A. Sokolova. "The total concentration and fractional composition of the aluminum compounds in soil solutions from peaty-podzolic-gleyic soils developed on binary deposits." Eurasian Soil Science 44, no. 2 (2011): 137–48. http://dx.doi.org/10.1134/s1064229311020062.

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Li, H., L. É. Parent, C. Tremblay, and A. Karam. "Potato response to crop sequence and nitrogen fertilization following sod breakup in a Gleyed Humo-Ferric Podzol." Canadian Journal of Plant Science 79, no. 3 (1999): 439–46. http://dx.doi.org/10.4141/p98-042.

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Meadow soils could supply significant amounts of N for several years and reduce N requirements for the potato (Solanum tuberosum L.). We examined a combination of three crop sequences, three cultivars and six N rates in relation to tuber yield and quality. Superior, Kennebec and Snowden were grown as follows on a Tilly silty loam between 1993 and 1995: (1) 3-yr continuous potato cropping of Superior, (2) 3-yr continuous potato cropping starting with Snowden and followed by 2 yr of Kennebec, and (3) 3-yr sequence of Kennebec, oat (Avena sativa L. 'Marion') and Superior. There were six N treatme

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Kukumägi, Mai, Veiko Uri, and Olevi Kull. "Mullahingamise sesoonne dünaamika kuusikute aegreas / Seasonal dynamics of soil respiration in a chronosequence of the Norway spruce stands." Forestry Studies 54, no. 1 (2011): 5–17. http://dx.doi.org/10.2478/v10132-011-0091-9.

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Abstract. Soil respiration resulting from microbial and root respiration is a major component of the forest carbon cycle. The response of soil respiration to varying environmental factors (soil temperature and soil moisture) was studied in a Norway spruce chronosequence composed of four age classes (4, 27, 36, and 84 year old) on Gleyic Podzol. Soil respiration was measured monthly with closed dynamic chamber system, soil temperature and soil moisture were measured simultaneously. Mean soil respiration rate averaged over three years was 3.3 μmol CO2 m-2s-1, ranging from 0.6 to 5.4 μmol CO2 m-2

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