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Journal articles on the topic 'Buried soils'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Johnson, William C. "Sequestration in buried soils." Nature Geoscience 7, no. 6 (2014): 398–99. http://dx.doi.org/10.1038/ngeo2172.

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2

Johnson, D. L. "Paleosols are buried soils." Quaternary International 51-52 (January 1998): 7. http://dx.doi.org/10.1016/s1040-6182(98)90185-9.

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3

White, E. M. "Eolian Sediments and Buried Soils." Soil Horizons 42, no. 3 (2001): 93. http://dx.doi.org/10.2136/sh2001.3.0093.

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4

M.P., Babaev, and Feyziyev F.M. "Buried Meadow Gray - Soils Of The Mughan Plain." Journal of Life Sciences and Biomedicine 68, no. 3 (2013): 199–203. https://doi.org/10.5281/zenodo.7443621.

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Morphogenetic diagnostics, physical and chemical characteristics of the buried soils of the Mughan plain as a result of the historical process have been presented in the review article. According to surveys of these two cuts it can be concluded that the reason for the formation of buried soils is the intensive floods and agroirrigation on the surface of the soil. Therefore it is considered necessary to conduct a paleo-soil investigation of these soils. In general, the layer of the soil, which is considered buried, shows the properties of the layer of gray - meadow soils. Despite the fact that

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5

Jiang, Yingying, Zhongxiu Sun, Yubo Zheng, Hongling Wang, and Jiaqing Wang. "Establishing a Soil Health Assessment System for Quaternary Red Soils (Luvisols) under Different Land Use Patterns." Agronomy 13, no. 8 (2023): 2026. http://dx.doi.org/10.3390/agronomy13082026.

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The health status of Quaternary red soil is a comprehensive reflection of the production and ecological service functions, which directly affects agricultural productivity and ecosystem sustainability. Based on the Cornell Soil Health Assessment (CASH) system frame, a health evaluation system for Quaternary red soils was established including the soil’s physical, chemical, and biological indicators. The soil’s health status under different land use patterns (the buried Quaternary red soil, sparse forest and grassland, grassland, woodland, and arable land) was systematically diagnosed in the lo

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6

Keeley, Helen C. M. "Report on the buried soil." Proceedings of the Prehistoric Society 53, S2 (1987): 32. http://dx.doi.org/10.1017/s0079497x00078713.

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Present-day soils in the Borwick area form the Carnforth Association, i.e. freely drained gravelly brown earths, some calcareous brown earths and peaty gleys and peaty soils in hollows. pH is normally 6 to 7, with some soil pH higher than 7.The buried soil beneath the cairn was a truncated stagnopodzol with a pH of 7.35. The Eag, Bf and Bs horizons were present but the lack of a topsoil and relatively high pH suggested that pollen analysis of the soil would be unproductive. Similarly, detailed soil analysis was unlikely to add to the interpretation of the site and was therefore not pursued. Th

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7

Orlova, L. A., and V. A. Panychev. "The Reliability of Radiocarbon Dating Buried Soils." Radiocarbon 35, no. 3 (1993): 369–77. http://dx.doi.org/10.1017/s0033822200060379.

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Variable 14C ages of paleosol organic matter (OM) cause difficulties in interpreting 14C data. We attempt to determine the reliability of OM 14C dates by examining different carbon-containing materials from soil horizons and paleosol fractions.

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8

Boutros, Youssef Zaki, Hassan Mansour El-Saadany, and Ibrahim Abd-El-Hai El-Awadi. "Infiltration from buried pipes in unsaturated soils." Computer Methods in Applied Mechanics and Engineering 81, no. 2 (1990): 173–82. http://dx.doi.org/10.1016/0045-7825(90)90108-x.

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9

Green, F. J., and K. Lockyear. "Plant remains from buried soils, Romsey, Hampshire." Review of Palaeobotany and Palynology 73, no. 1-4 (1992): 57–70. http://dx.doi.org/10.1016/0034-6667(92)90045-i.

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10

Bockheim, James G. "Soil preservation and ventifact recycling from dry-based glaciers in Antarctica." Antarctic Science 22, no. 4 (2010): 409–17. http://dx.doi.org/10.1017/s0954102010000167.

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AbstractSoil preservation from three glacial thermal regimes was examined in the Transantarctic Mountains (TAM) using the University of Wisconsin Antarctic Soils Database (http://nsidc.org/data/ggd221). Glacial thermal regimes included temperate (wet-based) glaciers from overriding of the TAM prior to c. 15Ma bp and subsequent polar (dry-based) glaciers. The glacial thermal regimes were distinguished from landform, sediment and erosional features. Buried soils were most common from deposition by dry-based glaciers (44 of 51 pedons). Several of these buried soils had a desert pavement intact wi

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11

Matsibora, O. "THE COMPARATIVE ANALYSIS OF BURIED AND ZONAL SOILS AS A METHOD OF RECONSTRUCTION OF PALEOGEOGRAPHICAL CONDITIONS IN HOLOCENE." Ukrainian Geographical Journal 2011, no. 4 (2011): 28–33. https://doi.org/10.5281/zenodo.1226844.

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The comparative analysis of the buried and zonal Holocene soils in the steppe zone of Ukraine has been carried out. The genesis of the soils, their carbonate and humus profiles have been investigated. The trends of soils evolution on the territory during last 3500 years have been determined. The palaeogeographical reconstructions of the natural conditions during the second half of subboreal period of Holocene have been created on the basis of the made soil investigations.

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12

Nelson, Alan R. "Discordant 14C Ages from Buried Tidal-Marsh Soils in the Cascadia Subduction Zone, Southern Oregon Coast." Quaternary Research 38, no. 1 (1992): 74–90. http://dx.doi.org/10.1016/0033-5894(92)90031-d.

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AbstractPeaty, tidal-marsh soils interbedded with estuarine mud in late Holocene stratigraphic sequences near Coos Bay, Oregon, may have been submerged and buried during great (M > 8) subduction earthquakes, smaller localized earthquakes, or by nontectonic processes. Radiocarbon dating might help distinguish among these alternatives by showing that soils at different sites were submerged at different times along this part of the Cascadia subduction zone. But comparison of conventional 14C ages for different materials from the same buried soils shows that they contain materials that differ i

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13

Basher, L. R. "Is pedology dead and buried?" Soil Research 35, no. 5 (1997): 979. http://dx.doi.org/10.1071/s96110.

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Pedology, the field study of soils as natural landscape bodies, has suffered serious cutbacks in stang and funding in many developed countries. Soil survey, a strong focus for pedology, has been most affected by this recession. The cutbacks to pedology reflect the reduction in funding for general purpose soil resource inventories and a decline in central government planning and land development, as well as changing needs for soil information and perceived failure of soil survey to respond by delivering relevant, timely information at affordable cost. A refocusing of research effort in pedology

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14

Conley, Travis, Stance Hurst, and Eileen Johnson. "Topographic Thresholds and Soil Preservation along the Southern High Plains Eastern Escarpment, Northwest Texas, USA." Geosciences 10, no. 12 (2020): 476. http://dx.doi.org/10.3390/geosciences10120476.

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The eastern escarpment of the Southern High Plains (USA) is today a semi-arid erosional landscape delineated by canyon breaks and topographic relief. A series of buried soils were identified, described, and sampled at 19 soil profile localities exposed along terraces of the South Fork of the Double Mountain Fork of the Brazos River (South Fork) and two associated tributaries (Spring Creek and Macy 285 drainage). Radiocarbon dating revealed late-Pleistocene to early Holocene (~12,580–9100 14C B.P.), middle-Holocene (~6025–4600 14C B.P.), and late-Holocene (~2000–800 14C B.P.) buried soils. The

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15

Hall, Robert D. "A COMPARISON OF SURFACE SOILS AND BURIED SOILS: FACTORS OF SOIL DEVELOPMENT." Soil Science 164, no. 4 (1999): 264–87. http://dx.doi.org/10.1097/00010694-199904000-00006.

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16

Trader, Patrick D. "A Hidden Landscape: Interpreting Buried Archaeological Site Potential in the White River Valley, Indiana." Midcontinental Journal of Archaeology 48, no. 3 (2023): 203–26. http://dx.doi.org/10.5406/23274271.48.3.02.

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Abstract A model for buried site potential has been developed and presented here following extensive geoarchaeological investigations conducted along the White River valley in Indiana. Backhoe-trenching efforts identified 35 buried archaeological sites dating from the Late Archaic through postcontact periods. Buried archaeological sites were found primarily in soils classified as inceptisols, with fewer found in soils classified as mollisols and entisols. Geochronological dating and artifact analysis suggest that after 3000 BP the White River valley transitioned from lateral to vertical accret

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17

Orlova, Lyubov A., and Valentina S. Zykina. "Radiocarbon Dating of Buried Holocene Soils in Siberia." Radiocarbon 44, no. 1 (2002): 113–22. http://dx.doi.org/10.1017/s0033822200064717.

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We have constructed a detailed chronological description of soil formation and its environments with data obtained on radiocarbon ages, palynology, and pedology of the Holocene buried soils in the forest steppe of western and central Siberia. We studied a number of Holocene sections, which were located in different geomorphic situations. Radiocarbon dating of materials from several soil horizons, including soil organic matter (SOM), wood, peat, charcoal, and carbonates, revealed three climatic periods and five stages of soil formation in the second part of the Holocene. 14C ages of approximate

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18

Seastedt, T. R., W. J. Parton, and D. S. Ojima. "Mass loss and nitrogen dynamics of decaying litter of grasslands: the apparent low nitrogen immobilization potential of root detritus." Canadian Journal of Botany 70, no. 2 (1992): 384–91. http://dx.doi.org/10.1139/b92-052.

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Litter-bag studies and simulation modeling were used to examine the relationship between mass loss and nitrogen content of decaying prairie foliage and root litter. In contrast with forest studies, grassland roots were low in lignin and nitrogen, decayed more rapidly than foliage, and demonstrated very low nitrogen immobilization potentials. Our findings agree with reports indicating that buried substrates with high C:N ratios do not immobilize substantial amounts of nitrogen and that nitrogen-limited environments induce steeper slopes in the mass loss – nitrogen concentration relationship. Ho

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19

Fei-hong, Gu. "Evaluation of Soil Liquefaction in Harbor District in Tianjin City." Open Civil Engineering Journal 10, no. 1 (2016): 293–300. http://dx.doi.org/10.2174/1874149501610010293.

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The liquefaction of soils in the harbor district in Tianjin City near Tangshan, where a great earthquake occurred is a very important issue related to the soil’s compaction, grain composition and content of clay particle. This problem has not been fully considered due to the complexity and uncertainty of the soil properties data, since none of the previous investigations has been concerned about the liquefaction characteristics of this new harbor district. The evaluation of soil liquefaction has been made based on related data of the standard penetration test (SPT) from 26 investigation bore h

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20

Höfle, Claudia, Mary E. Edwards, David M. Hopkins, Daniel H. Mann, and Chien-Lu Ping. "The Full-Glacial Environment of the Northern Seward Peninsula, Alaska, Reconstructed from the 21,500-Year-Old Kitluk Paleosol." Quaternary Research 53, no. 2 (2000): 143–53. http://dx.doi.org/10.1006/qres.1999.2097.

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AbstractPaleoenvironmental conditions are reconstructed from soils buried under volcanic ash ca. 21,500 years ago on the Seward Peninsula. Soil development was minimal, reflecting the continuous regional deposition of loess, which originated from river floodplains and the exposed Chukchi shelf. Cryoturbated soil horizons, ice wedges, and ice-lens formation indicate a permafrost environment and mean annual temperatures below −6° to −8°C. Shallow active layers (average 45 cm), minimal evidence for chemical leaching of soils, and the presence of earthen hummocks indicate a cold and seasonally dry

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21

Miller, T. W., J. M. H. Hendrickx, and B. Borchers. "Radar Detection of Buried Landmines in Field Soils." Vadose Zone Journal 3, no. 4 (2004): 1116–27. http://dx.doi.org/10.2113/3.4.1116.

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22

James, T. K., and A. Rahman. "Longevity of buried ragwort seed in four soils." New Zealand Plant Protection 53 (August 1, 2000): 253–57. http://dx.doi.org/10.30843/nzpp.2000.53.3703.

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The viability of ragwort (Senecio jacobaea L) seed buried for several years at 0 2 4 6 and 19 21 cm depths was evaluated in four different soil types Seed samples in nylon mesh bags were removed after 1 2 3 5 11 and 16 years burial and their viability determined by germination After 16 years no viable seed was found in the clay soil In the silt loam and peat soils 1 3 viable seed remained while in the sandy soil up to 13 remained viable In the surface 0 2 cm layer of soil it took from 109 to 146 years for the percentage of viable seed to fall to 1 of the original viable seed depending on soil

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23

Boutros, Y., H. Mansour, and I. El-Awadi. "Infiltration from Buried Pipes in Unsaturated Soils.(Dept.M)." MEJ. Mansoura Engineering Journal 13, no. 2 (2021): 44–55. http://dx.doi.org/10.21608/bfemu.2021.173227.

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24

Córdoba, V. C., M. A. Mejía, F. Echeverría, M. Morales, and J. A. Calderón. "Corrosion mitigation of buried structures by soils modification." Ingeniare. Revista chilena de ingeniería 19, no. 3 (2011): 486–97. http://dx.doi.org/10.4067/s0718-33052011000300016.

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25

Miller, T. W., J. M. H. Hendrickx, and B. Borchers. "Radar Detection of Buried Landmines in Field Soils." Vadose Zone Journal 3, no. 4 (2004): 1116–27. http://dx.doi.org/10.2136/vzj2004.1116.

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26

Dahms, Dennis E. "Mid-Holocene Erosion of Soil Catenas on Moraines near the Type Pinedale Till, Wind River Range, Wyoming." Quaternary Research 42, no. 1 (1994): 41–48. http://dx.doi.org/10.1006/qres.1994.1052.

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AbstractBuried soils are described from the floors of four kettles on Pinedale piedmont moraines of the southwestern Wind River Range, Wyoming, near the type locality of the Pinedale Till. The buried soils indicate that a previously unreported episode of slope erosion has occurred along adjacent catenas on some of the moraines in this region. Radiocarbon ages of the buried soils indicate that slope erosion occurred during the middle Holocene from 8540 ± 190 to 4800 ± 60 14C yr B.P. The presence of buried soils in moraine kettles indicates that profiles on the crests and backslopes of some of t

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27

Wang, Z., K. Van Oost, A. Lang, W. Clymans, and G. Govers. "Long-term dynamics of buried organic carbon in colluvial soils." Biogeosciences Discussions 10, no. 8 (2013): 13719–51. http://dx.doi.org/10.5194/bgd-10-13719-2013.

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Abstract. Colluvial soils are enriched in soil organic carbon (SOC) in comparison to the soils of upslope areas due to the deposition and subsurface burial of SOC. It has been suggested that the burial of SOC has important implications for the global carbon cycle, but the long-term dynamics of buried SOC remains poorly constrained. We address this issue by determining the SOC burial efficiency (i.e., the fraction of originally deposited SOC that is preserved in colluvial deposits) of buried SOC as well as the SOC stability in colluvial soils. We quantify the turnover rate of deposited SOC by e

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28

de Jong, E., R. J. Heck, and E. V. Ponomarenko. "Magnetic susceptibility of soil separates of Gleysolic and Chernozemic soils." Canadian Journal of Soil Science 85, no. 2 (2005): 233–44. http://dx.doi.org/10.4141/s04-034.

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The major horizons of Gleysolic and Chernozemic soils and the underlying deep till of five cores were separated into sand-, silt- and clay-sized fractions. Pedogenesis increased the ranges of magnetic susceptibility (χ) and oxalate (Feo) and dithionite-citrate extractable (Fed) iron in bulk samples and size separates of the A, B and IC horizons compared to the deep till. In the A, B and IC horizons the relationships between χ of the bulk (< 2 mm diameter) soil and χ of the sand and silt fractions was much stronger than in the deep till. Generally, χ of the clay was much lower than that of t

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Manucharova, Natalia A., Timur D. Karimov, Maria M. Pevzner, et al. "The Prokaryotic Complex of Modern and Buried Soils on the Kamchatka Peninsula." Forests 13, no. 7 (2022): 1066. http://dx.doi.org/10.3390/f13071066.

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A prokaryotic heterotrophic mesophilic community was studied in volcanic soil samples from Kamchatka. A phylogenetic and physiological characterization of the prokaryotic complex of modern and buried soils of the Kamchatka Peninsula is given. Volcanic Paleolithic soils (2500 and 11,300 years old) and their modern equivalents were investigated. It was found that the biomass of metabolically active prokaryotes in modern volcanic and Paleolithic soils reached 50 and 40 µg/g, respectively. The proportion of archaea in the metabolically active prokaryotic complex varied from 20% to 30% and increase

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30

Sverchkova, A. E., O. S. Khokhlova, A. O. Makeev, et al. "Geoarchaeological Analysis of Soils and Structures of the Kurgan Shumny, Krasnodar Region." Почвоведение, no. 11 (November 1, 2023): 1303–26. http://dx.doi.org/10.31857/s0032180x23600129.

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The chronosequence of soils buried under constructions of different ages at the large (h – 3.5 m, d – 74 m) kurgan Shumny in the Krasnodar Region has been studied. The kurgan was built sequentially by the people of Catacomb (XXVIII–XXII centuries BC) and Srubnaya (XV–X centuries BC) cultures, and includes five constructions, that built from the material of local soils and anthropogenic material. Each of the subsequent construction overlapped the previous one and went beyond it, covering some an additional space which allow studying a consecutive series of buried under the constructions soils.

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31

KEMP, R. A. "The cause of redness in some buried and non-buried soils in eastern England." Journal of Soil Science 36, no. 3 (1985): 329–34. http://dx.doi.org/10.1111/j.1365-2389.1985.tb00339.x.

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32

Malyk, Roman, Andriy Kyrylchuk, Zinovy Pankiv, and Ihor Kasiyanyk. "Ecological and Geographical Features of Ontogenesis of Holocene Soils of Kamianets-Podilskyi Fortress." SHS Web of Conferences 100 (2021): 05006. http://dx.doi.org/10.1051/shsconf/202110005006.

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The article analyzes the degree of study of the genetic features of Holocene soils of beligerative complexes. A detailed description of natural and anthropogenic conditions and factors determining the geography, genesis and ecological condition of modern and buried soils of beligerative structures of Kamianets-Podilskyi Fortress is given. Considerable attention is paid to the problem of ontogenesis of the dominant natural and anthropogenic soils within the study area, represented by urborendzins and constructional soils. The morphogenetic features of these soils have been studied. The soils of

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33

Vladova, Alla Yu. "Remote Geotechnical Monitoring of a Buried Oil Pipeline." Mathematics 10, no. 11 (2022): 1813. http://dx.doi.org/10.3390/math10111813.

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Extensive but remote oil and gas fields in Canada and Russia require extremely long pipelines. Global warming and local anthropogenic effects drive the deepening of seasonal thawing of cryolithozone soils and enhance pathological processes such as frost heave, thermokarst, and thermal erosion. These processes lead to a reduction in the subgrade capacity of the soils, causing changes in the spatial position of the pipelines, consequently increasing the number of accidents. Oil operators are compelled to monitor the daily temperatures of unevenly heated soils along pipeline routes. However, they

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34

Al-Darraji, M. M., and V. S. Tshovrebov. "Morphological characteristics, humus and nutrient content of recent and buried soils of the Inozemtsevo mound." E3S Web of Conferences 420 (2023): 03016. http://dx.doi.org/10.1051/e3sconf/202342003016.

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The main objective of the work was to identify the evolutionary changes in the profile of recent and buried soil in the Holocene, the content of humus and the composition of mobile forms of nutrients in the solonetzol- silted black soil in the insufficiently wetted zone of Stavropol Krai. The research was carried out near the village of Inozemtsevo, Stavropol Krai. The soils of the study area are formed on marine sediments. A 1.5-metre-high grave was erected more than 5,000 years ago. At a distance of 150 metres, an incision was made on recent virgin soils. According to morphological character

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35

Gavrilov, D. A., and M/ K. Khabdulina. "Ancient Irrigated Soils of the Bozok Archaeological District, Northern Kazakhstan (11th to 12th Centuries)." Archaeology, Ethnology & Anthropology of Eurasia 46, no. 4 (2018): 83–93. http://dx.doi.org/10.17746/1563-0102.2018.46.4.083-093.

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Results of an interdisciplinary (archaeological and pedological) study of the ancient soils in the Bozok district (8th to 15th centuries) are presented. Part of the district is a complex irrigation system dating to the 11th to 12th centuries. To detect the traces of ancient irrigation, surface and buried soils were studied. Results of the morphogenetic analysis, as well as the assessment of physical and chemical properties of soils and their microbiomorph composition, suggest that soils relating to various functional parts of the irrigation system within the same catena indicate agricultural u

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36

Bockheim, J. G. "Paleosols in the transantarctic mountains: indicators of environmental change." Solid Earth Discussions 5, no. 2 (2013): 1007–29. http://dx.doi.org/10.5194/sed-5-1007-2013.

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Abstract. The Transantarctic Mountains (TAMs), a 3500 km long chain that subdivides East Antarctica from West Antarctica, are important for reconstructing the tectonic, glacial, and climatic history of Antarctica. With an ice-free area of 24 200 km2 (50% of the total in Antarctica), the TAMs contain an unusually high proportion of paleosols, including relict and buried soils. The unconsolidated paleosols range from late Quaternary to Miocene in age, the semi-consolidated paleosols are of early Miocene to Oligocene age, and the consolidated paleosols are of Paleozoic age. Paleosols on unconsoli

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37

Bockheim, J. G. "Paleosols in the Transantarctic Mountains: indicators of environmental change." Solid Earth 4, no. 2 (2013): 451–59. http://dx.doi.org/10.5194/se-4-451-2013.

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Abstract. The Transantarctic Mountains (TAMs), a 3500 km long chain that subdivides East Antarctica from West Antarctica, are important for reconstructing the tectonic, glacial, and climatic history of Antarctica. With an ice-free area of 24 200 km2 (50% of the total in Antarctica), the TAMs contain an unusually high proportion of paleosols, including relict and buried soils. The unconsolidated paleosols range from late Quaternary to Miocene in age, the semi-consolidated paleosols are of early Miocene to Oligocene age, and the consolidated paleosols are of Paleozoic age. Paleosols on unconsoli

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38

Trepanier, Kaitlyn E., Laura Manchola-Rojas, and Bradley D. Pinno. "Effects of Buried Wood on the Development of Populus tremuloides on Various Oil Sands Reclamation Soils." Forests 13, no. 1 (2022): 42. http://dx.doi.org/10.3390/f13010042.

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Buried wood is an important but understudied component of reclamation soils. We examined the impacts of buried wood amounts and species on the growth of the common reclamation tree species trembling aspen (Populus tremuloides). In a greenhouse study, aspen seedlings were planted into four soil types, upland derived fine forest floor-mineral mix (fFFMM), coarse forest floor-mineral mix (cFFMM), and lowland derived peat and peat-mineral mix (PMM), that were mixed with either aspen or pine wood shavings at four concentrations (0%, 10%, 20% and 50% of total volume). Height and diameter growth, chl

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39

Matviyishyna, Zhanna, Sergiy Doroshkevich, and Anatoliy Kushnir. "Reconstruction of trypilliantime landscapes using paleopedological studies." Visnyk of the Lviv University. Series Geography, no. 48 (December 23, 2014): 107–16. http://dx.doi.org/10.30970/vgg.2014.48.1298.

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Based on studies of buried soils at two archaeological sites Holocene (Likarove, Myropill) territory Podolski–at-Dnieper forest-steppe zone of Ukraine reconstructed landscapes time of life Trypilska cultural community (6 000-4 000 B.P). The research results are based on data from a comprehensive study of active paleopedolohichnoho using micromorphological analysis of ancient and modern soils. These data illustrate partially offset boundaries of modern landscape areas to the north compared to the corresponding stage of the long-standing nature. Key words: landscape, buried soil, Holocene, paleo

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40

Sabatier, James, Ning Xiang, and Ron Craig. "High‐resolution velocity images of targets buried in soils." Journal of the Acoustical Society of America 104, no. 3 (1998): 1783. http://dx.doi.org/10.1121/1.424149.

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41

Dahal, Kumar P., Dinesh KC, and Jagadeesh Bhattarai. "Study on the soil corrosivity towards the buried water supply pipelines in Madhyapur Thimi municipality, Bhaktapur." BIBECHANA 11 (May 10, 2014): 94–102. http://dx.doi.org/10.3126/bibechana.v11i0.10387.

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This research work is carried out to identify the corrosive nature of soils towards the buried-galvanized steel and cast iron pipelines buried in Sanothimi areas of Madhyapur Thimi municipality, Bhaktapur based on different soil parameters such as organic content, moisture content, pH, resistivity, oxidation-reduction potential, chloride and sulfate ions. The soil parameters of the collected soil samples from the study areas were analyzed using standard ASTM methods. Concentrations of these soil parameters measured in this study were found as: organic content (0.9- 7.9%), moisture content (8.0

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42

James, T. K., and A. Rahman. "Survival of giant buttercup seeds buried at different depths in four soils." Proceedings of the New Zealand Plant Protection Conference 52 (August 1, 1999): 234–39. http://dx.doi.org/10.30843/nzpp.1999.52.11577.

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The viability of giant buttercup (Ranunculus acris) seed buried at three depths in four different soils in the Waikato region was evaluated over a 16 year period. Most seed buried in the top 2 cm soil layer disappeared within the first year. When buried at 4 ? 6 cm, numbers declined rapidly over the first two years and were no longer found at three of the four sites within 16 years. At the end of the study, up to 22% of the seed was still viable at the 19 - 21 cm depth. If left undisturbed and assuming exponential decay, it could take up to 51 years for deeply buried viable seed numbers to be

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Artikov, H., M. Kočárek, A. Fraňková, T. Abdrakhmanov, L. Borůvka, and U. Sharipov. "Residues of organochlorine pesticides in irrigated sierozem-meadow soils around buried chemicals stock." Soil and Water Research 13, No. 2 (2018): 108–14. http://dx.doi.org/10.17221/131/2017-swr.

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The concentration and distribution of organochlorine pesticides (OCPs) were studied in sierozem-meadow soils around a buried obsolete chemicals stock in Mirzaabad district of Syrdarya region of Uzbekistan. 23 soil samples were collected from the topsoil (0–30 cm of soil depth) and 15 samples were collected from three soil profiles (down to 125 cm of soil depth) located in nearby vicinity of the stock. They were extracted using an automated Soxhlet extractor and analyses were done by gas chromatography-mass spectrometry. The detected OCPs were DDTs, HCHs, aldrin, dieldrin, endrin, chlorpyrifos,

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Tkachev, V. V. "The Ishkinino Bronze Age Mining Complex in the Southern Urals: Radiocarbon Dating." Archaeology, Ethnology & Anthropology of Eurasia 47, no. 3 (2019): 38–47. http://dx.doi.org/10.17746/1563-0110.2019.47.3.038-047.

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This article presents the results of radiocarbon dating of buried soils beneath the dumps of ancient mines in the Ishkinino cobalt and copper pyrite deposit area, in the Southern Urals. The conserved upper horizons of stratigraphic sequences underlying the dumps of four mines were subjected to radiocarbon analysis. For comparison, samples from Bronze Age sites in the same area were used. Chronological ranges of the Yamnaya, Sintashta, and Kozhumberdy cultures were evaluated. Calibrated intervals of the buried soils from the Ishkinino mines show a good agreement with respective intervals relati

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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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Bronnikova, Maria A., Yuliya V. Konoplianikova, Anna R. Agatova, Roman K. Nepop, and Marina P. Lebedeva. "HOLOCENE ENVIRONMENTAL CHANGE IN SOUTH-EAST ALTAI EVIDENCED BY SOIL RECORD." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 11, no. 4 (2019): 100–111. http://dx.doi.org/10.24057/2071-9388-2018-11-4-100-111.

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The soils of Russian Altai highlands were used as a paleoenvironmental archive, as a source of dating material, and as a chronostratigraphic marker to describe Holocene environmental change in the studied area. Based on calibration intervals of 14C dates obtained for buried humus horizons (11 buried soils in 6 studied soil-sedimentary sequences) and some dates from pendants of contemporary soils, following stages of pedogenesis were recorded in studied soil-sedimentary systems and surface soils: 6.4 – 11.5 ky cal BP; about 4.9-5.3 cal BP; 2.5-3.8 cal BP; 0.6 – 1.2 cal BP. All studied surface s

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Su, Hong, Shuofu Mi, Xiaowei Peng, and Yejun Han. "The mutual influence between corrosion and the surrounding soil microbial communities of buried petroleum pipelines." RSC Advances 9, no. 33 (2019): 18930–40. http://dx.doi.org/10.1039/c9ra03386f.

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Martin, Charles W., and William C. Johnson. "Variation in Radiocarbon Ages of Soil Organic Matter Fractions from Late Quaternary Buried Soils." Quaternary Research 43, no. 2 (1995): 232–37. http://dx.doi.org/10.1006/qres.1995.1023.

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AbstractRadiocarbon dating of three organic matter fractions (total, humic acid, and residue) isolated from late Quaternary buried soils of the central Great Plains reveals that there often are considerable differences among, but no consistent order to, the ages of fractions. For late Holocene soils, the residue fraction or the total fraction generally produces the oldest age; for late Pleistocene soils, however, no fraction was consistently the oldest. The absence of a consistent sequence of fraction ages is attributed to postburial contamination of soils. When bulk samples from the same soil

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Kaiser, K., A. Barthelmes, S. Czakó Pap, et al. "A Lateglacial palaeosol cover in the Altdarss area, southern Baltic Sea coast (northeast Germany): investigations on pedology, geochronology and botany." Netherlands Journal of Geosciences - Geologie en Mijnbouw 85, no. 3 (2006): 197–220. http://dx.doi.org/10.1017/s0016774600021478.

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AbstractA new site with Lateglacial palaeosols covered by 0.8 - 2.4 m thick aeolian sands is presented. The buried soils were subjected to multidisciplinary analyses (pedology, micromorphology, geochronology, dendrology, palynology, macrofossils). The buried soil cover comprises a catena from relatively dry (’Nano’-Podzol, Arenosol) via moist (Histic Gleysol, Gleysol) to wet conditions (Histosol). Dry soils are similar to the so-called Usselo soil, as described from sites in NW Europe and central Poland. The buried soil surface covers ca. 3.4 km2. Pollen analyses date this surface into the lat

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Chykailo, Yuliia, and Ivan Voloshyn. "Deflation's soil and technogenic pollutants of the near-highway zones of road Lviv–Krakovets." Visnyk of the Lviv University. Series Geography, no. 51 (December 27, 2017): 370–81. http://dx.doi.org/10.30970/vgg.2017.51.8903.

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In the article is analyzed the soils’ properties in near-highway road strips of M-10 Lviv- Krakovets with width up to 150 m. Within the near-road strips of the highway, have been established 12 experimental polygons under forest, meadow vegetation and agricultural lands. On each polygons from soils profile samples are selected the most common soils: sod-podzolic, formed on fl uvio-glacial and gray-forest soils formed onloess loam. Completed description of soil profiles to depth of 0-100 cm. Part of experimental soils are formed under hornbeam-beech forests (11, 12 polygons) and oak-hornbeam-pi

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