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Journal articles on the topic 'Dark-humus gley soils'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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1

Purtova, Lyudmila N. "INDICATORS OF CHEMODESTRUCTIVE FRACTIONATION OF ORGANIC MATTER SOILS OF NATURAL AND ANTHROPOGENIC-TRANSFORMED LANDSCAPES OF THE SOUTH OF PRIMORYE." UNIVERSITY NEWS. NORTH-CAUCASIAN REGION. NATURAL SCIENCES SERIES, no. 3 (211) (September 30, 2021): 111–16. http://dx.doi.org/10.18522/1026-2237-2021-3-111-116.

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The differences in the qualitative composition of organic matter in the soils of natural and anthropogenically transformed landscapes in the south of Primorye were established by the method of chemodestructive fractionation (CDF). The lowest indices of the easily oxidizable part (EOP) in the organic matter are typical for soils of technogenic landscapes (embryozems) with very low humus content due to low reserves of aboveground phytomass and the supply of fresh organic matter of plant origin. Embryozems are characterized by a low supply of humus with nitrogen. Higher EOP values are characteris

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2

Rusakov, A.V., A.A. Nikonov, L.A. Savelieva, and D.V. Pinakhina. "Buried Late Holocene Paleosols of the Nienshants Cultural–Historical Monument in St. Petersburg." Eurasian Soil Science 46, no. 1 (2013): 15–27. https://doi.org/10.1134/S1064229313010079.

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Buried Late Holocene paleosols of the Nienshants historical monument at the junction of the Neva and Okhta rivers (St. Petersburg) have been studied. These soils developed from estuary deposits of the Littorina basin with abundant artifacts of the Neolithic and Early Iron ages (7–2 ka BP). The soil cover of the area consists of the mature dark-humus profile-gleyed soils on elevated elements of the mesotopography (3.0–3.5 a.s.l.) and dark-humus gley soils in the local depressions (2.0–2.6 m a.s.l.). The soils are characterized by the low to moderate content of humus of the ful

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3

Ananko, T. V., and M. I. Gerasimova. "Dark-humus soils on the updated soil map of Russian Federation scale 1 : 2.5 M." Dokuchaev Soil Bulletin, no. 108 (October 19, 2021): 31–54. http://dx.doi.org/10.19047/0136-1694-2021-108-31-54.

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The dark-humus soil type was included in the updated legend of the Soil Map of the Russian Federation at scale 1 : 2.5 M, converted to the system of Soil Classification of Russia. The soil profile starts with the dark-humus horizon gradually merging to the parent rock; any mid-profile diagnostic horizons are absent. Large areas of dark-humus soils are found in the forest-steppe, steppe and taiga zones of the European Russia, Western and Central Siberia, in the Trans-Baikal region, the Altai-Sayany Mountains, and the Caucasus. The type of dark-humus soils comprises both mesomorphic soils (of no

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4

Ubugunov, V. L., L. L. Ubugunov, and V. I. Ubugunova. "Soils of mountain floodplains in the zone of tectonic joints of Mongol-Okhotsk Orogenic Belt (Mongolia)." IOP Conference Series: Earth and Environmental Science 908, no. 1 (2021): 012035. http://dx.doi.org/10.1088/1755-1315/908/1/012035.

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Abstract New data on the soils of mountain floodplains in the tectonic joints zone of the Mongol-Okhotsk Orogenic Belt on the example of the Upper Kerulen Basin are presented. Soil diversity is mostly determined by sedimentation conditions and drainage of the parent rocks. There are alluvial–humus (Fluvisol (Humic)), mucky–humus (Folic Fluvisol), dark–humus (Fluvisol (Mollic)), dark–humus gley (Gleyic Fluvisol) and dark–humus saline soils (Sodic Gleyic Fluvisol (Mollic)) were diagnosed. Tectonic movements of the earth’s crust lead to the appearance of shaftlike linear dams, blocking river flow

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5

Zamotaev, I. V., R. G. Gracheva, Yu V. Konoplianikova, et al. "Soil Formation on Sugar Industry Waste in the Central Chernozemic Zone." Eurasian Soil Science 56, no. 11 (2023): 1784–802. http://dx.doi.org/10.1134/s1064229323601890.

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Abstract Soils formed in treatment facilities of sugar beet factories in the forest-steppe zone of Kursk oblast were studied. Technogenic factors of soil formation associated with the industrial sugar beet activity and post-technogenic processes during the abandonment of treatment facilities are considered. The alternation of settling ponds and the earth walls separating them are the main factors determining “cellular” pattern of the soil cover. The mode of inflow and discharge and the composition of wastewater, as well as the duration of the abandonment of settling ponds determine the specifi

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6

Gyninova, A. B., M. I. Gerasimova, and M. P. Lebedeva. "Micromorphological Cryogenic Features in Meadow Podbels of Middle-Amur Lowland." Počvovedenie, no. 5 (November 20, 2024): 655–64. http://dx.doi.org/10.31857/s0032180x24050016.

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Meadow podbels (dark-humus gleyic and gleypodbels in the Classification of soils of Russia) are subject to deep and prolonged freezing in the western part of their area. It is manifested in cryogenic deformations of genetic horizons as well as in thin sections. Micromorphological features of soils on permafrost are well known. and the purpose of this research was to reveal them in three profiles of meadow podbels as related to soil cryological and hydrological regimes. Unlike northern cryogenic soils. the meadow podbels have dark-humus horizons with weak cryogenic manifestations; in eluvial ho

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7

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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8

Gordienko, O. A., N. V. Onistratenko, and D. A. Andreeva. "Features of soils of the natural park “Scherbakovsky” Volgograd region." Dokuchaev Soil Bulletin, no. 115 (August 4, 2023): 32–53. http://dx.doi.org/10.19047/0136-1694-2023-115-32-53.

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The paper presents the results of a study of the soil cover of the Shcherbakovsky Nature Park in the Kamyshinsky district of the Volgograd region. To achieve the results 12 soil sections were laid along the studied soil catena (1.5 km), so that morphological and chemical features of the soils of the study area were investigated. Variety and diversity are due to vertical zonality and geological and hydrological peculiarities. So, in the gullies and in massive forest plantations various dark humus and gley soils have become widespread. On steppe, slope and watershed areas lithosolic light humus

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9

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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10

Tolstokoneva, E. N., and E. A. Zharikova. "Base-buffering properties of native and agrogenically transformed dark-humus gley soils of the Primor’e region." Eurasian Soil Science 42, no. 9 (2009): 989–95. http://dx.doi.org/10.1134/s1064229309090051.

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11

Sosorova, S. B., M. G. Merkusheva, L. N. Boloneva, and I. N. Lavrentieva. "Phosphorus Sorption by Saline Soils of Western Transbaikalia." Почвоведение, no. 10 (October 1, 2023): 1230–43. http://dx.doi.org/10.31857/s0032180x22601414.

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The sorption of phosphorus by salt marshes of the dry-steppe zone of the Republic of Buryatia from an aqueous solution of KN2PO4 in the concentration range from 0.25 to 5.0 mM/L (mmol/L) was studied under static conditions. The interaction time is 24 hours with a soil: solution ratio of 1 : 10. The amount of sorbed phosphorus was calculated from the difference in its content in the initial solutions and in the filtrates of soil suspensions. Based on experimental data, phosphorus adsorption isotherms were constructed by soil and sorption parameters were calculated using the Langmuir and Freundl

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12

Martynova, Natalia A., and Victoria Yu Vlasova. "Properties and genesis of soils in the Balagansk forest-steppe of Central Siberia and their ecological and resource potential." Почвы и окружающая среда 2, no. 4 (2020). http://dx.doi.org/10.31251/pos.v2i4.33.

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The aim of the study. To study the properties and genesis of natural soils of forest-steppe areas of Balagansk steppe. Location and time. The environs of Balagansk settlement in the Balagansky district of Irkutsk region, 2013-2018. Methodology. Combined field and laboratory studies of soil cover and soil properties using soil-morphological, pedo-lithological, climatostratigraphic, botanical, geological-geomorphological and comparative geographical methods, as well as various physical and chemical analyses. Main results. The study of soil properties of the Balagansk’ forest-steppe and assessmen

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13

Klimova, Nina V., Natalia A. Chernova, Art’em N. Nikiforov, and Anatoliy G. Dyukarev. "The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain." Journal of Siberian Federal University. Biology, March 2020, 25–43. http://dx.doi.org/10.17516/1997-1389-0314.

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The present study addresses the floristic composition and ecological and community structure of paludified birch forests (peat depth reaching 30 cm) in the southern taiga. The growing conditions were evaluated based on the indicator values of plants and soil chemical properties. The study plots were located on transects directed from upland forests through peripheral wetland forests to bogs, which are situated in topographic lows, at the North-East edge of the Great Vasyugan mire. The sites of the forest-to-bog ecotone that are transformed to various degrees by the bog water regime are conside

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14

"Evaluation of pedotransfer functions to predict saturated hydraulic conductivity of Ukrainian soils." Visnyk of V.N. Karazin Kharkiv National University, series Geology. Geography. Ecology, no. 52 (2020). http://dx.doi.org/10.26565/2410-7360-2020-52-05.

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Literature overview. The parameterization of hydrological models requires knowledge of the soil filtration properties. Generally, soil profiles are characterized by properties such as sand, silt and clay content, bulk density, organic carbon fraction or humus content, and no data on filtration properties are available. Ukrainian soil database, created in Geoecophysics of soil laboratory of National Scientific Center “Institute for Soil Science and Agrochemistry Researched named after O.N. Sokolovsky” (Laktionova et al., 2012), among other properties has extensive data on texture and bulk densi

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15

Sorokina, O. A., and A. N. Danilov. "Soil fertility transformation of abandoned soils along a catena in the Krasnoyarsk forest-steppe." Почвы и окружающая среда 7, no. 3 (2024). http://dx.doi.org/10.31251/pos.v7i3.267.

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The aim of the study was to assess the transformation of some abiotic factors and soil fertility indicators, as well as erosion progress in the post-agrogenic dark-gray glei soil, undergoing spontaneous revegetation after abandonement, and after it was once again putt into agricultural use (ploughed)on a catena in the Krasnoyarsk forest-steppe. Location and time of the study. The study was conducted in the Krasnoyarsk forest-steppe in 2017-2019 using 1) abandoned dark-gray glei soil and 2) the same abandoned soil after it was again put into agricultural use and tilled. The studied land, abando

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