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Artykuły w czasopismach na temat „Soil stratigraphy”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 19 lutego 2022

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1

Walker, PH. "Contributions to the understanding of soil and landscape relationships." Soil Research 27, no. 4 (1989): 589. http://dx.doi.org/10.1071/sr9890589.

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A new approach to pedology was developed in Australia in the 1950's. It was based on geomorphic and stratigraphic principles and recognized the cyclic or episodic nature of soil and landscape development. The research reviewed here represents a contribution to that approach and further developments of it in fluvial erosional and depositional landscapes of south-eastern Australia and in glaciated landscapes of midwestern U.S.A. This research features detailed studies of hillslope layers and their relationship to alluvial valley fills; soil chronosequences on flights of alluvial terraces; the st

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2

Paepe, R., I. Mariolakos, E. Van Overloop, S. Nassopoulou, J. Hus, M. Hatziotou, T. Markopoulos, E. Manutsoglu, G. Livaditis, and V. Sabot. "QUATERNARY SOIL-GEOLOGICAL STRATIGRAPHY IN GREECE." Bulletin of the Geological Society of Greece 36, no. 2 (July 23, 2018): 856. http://dx.doi.org/10.12681/bgsg.16833.

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Peloponnesus and Crete are probably offering the best possible standard sections for Eastern Mediterranean Pleistocene Series. Complete Pleistocene Standard Lithostratigraphic Sections from Sparta (Peloponnesus) and Kandanos (Crete) reveal continuous Pleistocene Land Sequences composed of cyclic palaeosol levels interfering with clastic fluvial, eolian (loess) and gravel deposits comparable with analogues found elswhere over the earth. Most suitable for correlation are: a) the standard Idfess area of Northern Europe, Russia and China, and b) the subtropical and tropical regions of Africa and A

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3

Wang, Jun Peng, Ye Du, and Dong Tian. "Identifying Soil Stratigraphy in Shanghai from Piezocone Soundings." Applied Mechanics and Materials 170-173 (May 2012): 857–62. http://dx.doi.org/10.4028/www.scientific.net/amm.170-173.857.

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This article presents a case history of piezocone penetration test (CPTU) of soft deposit in Shanghai. In Shanghai, stratigraphy for soft deposit is mainly obtained by the laboratory test with borehole samples. The stratigraphy identified by CPTU was developed and improved in recent decades. The analysis is carried out with the field data at test site of Yan’an Road Tunnel in Shanghai. The stratigraphy chart proposed by Robertson (1990) is employed to identify soil layer. The results show that the Robertson charts (1990) is suitable to identify the stratigraphy of the soft deposit in Shanghai.

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4

Cao, Zi-Jun, Shuo Zheng, Dian-Qing Li, and Kok-Kwang Phoon. "Bayesian identification of soil stratigraphy based on soil behaviour type index." Canadian Geotechnical Journal 56, no. 4 (April 2019): 570–86. http://dx.doi.org/10.1139/cgj-2017-0714.

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The cone penetration test (CPT) has been widely used to determine the soil stratigraphy (including the number N and thicknesses HN of soil layers) during geotechnical site investigation because it is rapid, repeatable, and economical. For this purpose, several deterministic and probabilistic approaches have been developed in the literature, but these approaches generally only give the “best” estimates (e.g., the most probable values) of N and HN based on CPT data according to prescribed soil stratification criteria, providing no information on the identification uncertainty (degrees-of-belief)

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5

Wang, Jun Peng, Yong Nan Wu, and Yao Liu. "Comparison and Analysis of Identification of Soil Stratigraphy in Shanghai between CPTU Test and Laboratory Test." Applied Mechanics and Materials 204-208 (October 2012): 732–37. http://dx.doi.org/10.4028/www.scientific.net/amm.204-208.732.

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This article presents a comparison and analysis between piezocone penetration test (CPTU) and laboratory test in identifying soil stratigraphy of Shanghai. In China, stratigraphy for soft deposit is mainly obtained from plasticity index and grain size distribution of borehole samples in the laboratory (refer to code method). Identification of soil stratigraphy with CPTU was developed and improved in recent decades. The analysis is carried out with the field data at test site of Yan’an Road Tunnel in Shanghai. The stratigraphy charts proposed by Robertson in 1990 (refer to Robertson charts (199

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6

Engstrom, D. R., and B. C. S. Hansen. "Postglacial vegetational change and soil development in southeastern Labrador as inferred from pollen and chemical stratigraphy." Canadian Journal of Botany 63, no. 3 (March 1, 1985): 543–61. http://dx.doi.org/10.1139/b85-070.

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Palynological and geochemical analyses of Holocene lake sediments are used to evaluate long-term interactions between vegetation and soils from four sites in southeastern Labrador, Canada. Changes in soil composition are inferred from the stratigraphy of humic materials and the elemental composition of authigenic and allogenic fractions of the sediment. Early Holocene lake muds deposited under tundra vegetation are predominantly inorganic and contain high concentrations of allogenic elastics derived from the erosion of barren soils. Concentrations of humic materials and redox–pH-sensitive elem

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7

Hryciw, Roman D., and Scott A. Raschke. "Development of Computer Vision Technique for in Situ Soil Characterization." Transportation Research Record: Journal of the Transportation Research Board 1526, no. 1 (January 1996): 86–97. http://dx.doi.org/10.1177/0361198196152600111.

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Construction and rehabilitation of highways, tunnels, and bridges require detailed information about subsurface stratigraphy. This study presents development of a new method for characterizing subsurface soil in situ using computer vision. Hardware and software systems are integrated to obtain the grain-size distribution (GSD) of subsurface soils continuously with depth and to identify small-scale subsurface anomalies. Research is being conducted in three phases. The first phase consists of measuring the GSD of detached cohesionless soil specimens in the laboratory from digital images obtained

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8

VALENTINE, K. W. G., C. TARNOCAI, C. R. DE KIMPE, R. H. KING, J. F. DORMAAR, W. J. VREEKEN, and S. A. HARRIS. "SOME ASPECTS OF QUATERNARY SOILS IN CANADA." Canadian Journal of Soil Science 67, no. 2 (May 1, 1987): 221–47. http://dx.doi.org/10.4141/cjss87-021.

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This review describes some aspects of Canadian soils that are relevant to the Quaternary. It includes a description of the Quaternary Period in Canada, including a chronology of the major events that influenced soil formation, and the implication of the Quaternary to Canadian soils. The contribution of relict and buried paleosols to Quaternary stratigraphy and the reconstruction of paleoenvironments is then discussed, including some of the inherent problems. Pedologic evidence of environmental change in the southern Rocky Mountains, including tephrostratigraphy, is followed by a description, w

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9

Karlstrom, Eric T. "Stratigraphy and genesis of five superposed paleosols in pre-Wisconsinan drift on Mokowan Butte, southwestern Alberta." Canadian Journal of Earth Sciences 24, no. 11 (November 1, 1987): 2235–53. http://dx.doi.org/10.1139/e87-211.

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Five paleosols in five superposed diamicts (probably tills) on Mokowan Butte permit subdivision of pre-Wisconsinan drift and a description of Quaternary and probably late Tertiary soil-forming environments. The surface soil and upper two buried paleosols (soils 5, 4, and 3, respectively) have strongly developed, 1–5 m thick, leached, reddish, clay-rich (20–48% clay), argillic horizons overlying indurated petrocalcic, calcic, or leached B horizons. The lower two buried paleosols (soils 2 and 1) are strongly developed and have 40–150 cm thick, clay-rich (18–49% clay) argillic horizons over calci

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10

Han, Wei-Chung, Yi-Wei Lu, and Sheng-Chung Lo. "Seismic prediction of soil distribution for the Chang-Bin offshore wind farm in the Taiwan Strait." Interpretation 8, no. 4 (August 31, 2020): T727—T737. http://dx.doi.org/10.1190/int-2020-0020.1.

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Direct soil measurements are limited to borehole locations and are therefore sparse in the oceans. To effectively characterize the soil distributions for the Chang-Bin offshore wind farm, which is an area with the greatest wind energy potential in the Taiwan Strait, we have developed a workflow to predict the soil distribution in the subsurface based on integrated analysis of seismic data and borehole data. First, we characterize the key seismic units and their seismic response in order to understand the regional stratigraphy. Then, we correlate the soil types to each stratigraphic unit as the

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11

Atkinson, G. "A multivariate analysis of alluvial terrace soils of the clarendon and cranebrook formations, Nepean River, NSW." Soil Research 26, no. 2 (1988): 243. http://dx.doi.org/10.1071/sr9880243.

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The techniques of cluster analysis and principal component analysis (PCA) were applied to soils data from two Pleistocene alluvial terraces on the Nepean River, N.S.W., the Clarendon and Cranebrook Formations, to address issues raised in the literature regarding their stratigraphic relationships. A total of 160 profiles were sampled at four fixed depths to 1 8 m. Profiles were located in four 1000 by 400 m sample areas, two on each terrace. Soil samples were analysed for colour, pH, and 2.8 M HCl extractable Fe2+, Mn2+, Na2+, K+, Ca2+ and Mg2+. Data were analysed by using whole profiles as the

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12

Sastrawan, Febrian Dedi, Meidi Arisalwadi, and Rahmania. "Analyzing of 1D Resistivity Data to Determine Subsurface Condition on the Development Area of Institut Teknologi Kalimantan (ITK) Balikpapan." Advances in Science and Technology 104 (February 2021): 41–45. http://dx.doi.org/10.4028/www.scientific.net/ast.104.41.

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Information of subsurface stratigraphy is needed during the process of preparing multi-story buildings to avoid problems in determining the level of multi-story building piles. This research was conducted using the geoelectric method to study the subsurface stratigraphic conditions in the area. Based on the measurement results, we find an overview of the subsurface stratigraphic conditions consisting of soil in the first layer with resistivity values ranging from 305 to 570 Ωm, the soil in the study area is red-yellow, namely podsolic soil mixed with sand and gravel. The second layer is clay

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13

Francis, Ronen, Mark N. Wuddivira, Junior Darsan, and Matthew Wilson. "Soil slaking sensitivity as influenced by soil properties in alluvial and residual humid tropical soils." Journal of Soils and Sediments 19, no. 4 (November 13, 2018): 1937–47. http://dx.doi.org/10.1007/s11368-018-2189-7.

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14

Abujabhah, Ibrahim S., Richard Doyle, Sally A. Bound, and John P. Bowman. "The effect of biochar loading rates on soil fertility, soil biomass, potential nitrification, and soil community metabolic profiles in three different soils." Journal of Soils and Sediments 16, no. 9 (April 1, 2016): 2211–22. http://dx.doi.org/10.1007/s11368-016-1411-8.

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15

Simonson, Roy W. "Lithology and Stratigraphy of Loess and Paleosols." Geoderma 39, no. 2 (December 1986): 163–64. http://dx.doi.org/10.1016/0016-7061(86)90078-9.

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16

Chichagova, O. A., and A. E. Cherkinsky. "Problems in Radiocarbon Dating of Soils." Radiocarbon 35, no. 3 (1993): 351–62. http://dx.doi.org/10.1017/s0033822200060355.

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We discuss our progress in three principal applications of 14C dating of recent and fossil soils: 1) new methods; 2) problems of interpreting 14C soil data (e.g.,14C age of soils, age of soils, duration of humus formation, rate of carbon cycling); and 3) 14C analysis of soil organic matter (OM) in pedology and paleogeography (e.g., soil genesis and evolution, humus formation and OM metamorphosis, geochronology and stratigraphy of Late Pleistocene and Holocene sediments). We suggest exploring the above issues in the analysis of each 14C profile in conjunction with paleogeographical data, and by

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17

Kulakovska, L. V., N. P. Gerassimenko, V. I. Usik, and O. L. Votiakova. "MIDDLE PALEOLITHIC SITE RUBAN’ IN TRANSCARPATHIA: STRATIGRAPHY, CHRONOLOGY, INDUSTRY." Archaeology and Early History of Ukraine 26, no. 1 (March 22, 2018): 7–19. http://dx.doi.org/10.37445/adiu.2018.01.01.

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The Ruban’ Paleolithic site was discovered in 2005 by the Transcarpathian Paleolithic expedition of the Archaeological Museum of the IA NASU. The site is located on the territory of the former Zatysnansky chemical plant (Fig. 1b) at a distance of 800 m north of the eastern outskirts of the village of Gorbky, Vynohradiv district, in the Transcarpathian region, in the Ruban’ tract, and about 2 km to the southeast of the Korolevo site. At the time when the site Ruban’ was discovered, the upper part the quarry wall where the site is located, has been ruined by the quarrying that made it impo

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18

Zhukov, O., and K. Maslikova. "The dependence of the technosols models functional properties from the primary stratigraphy designs." Journal of Geology, Geography and Geoecology 27, no. 2 (November 2, 2018): 399–407. http://dx.doi.org/10.15421/111864.

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In the present article the assumption that the design of the soil-like artificial body in zero-moment of existence determines the dynamics and trajectory of soilforming process was tasted. It was shown that an important aspect of the experiment is the search criteria that you can perform evaluation of the functional properties of the generated structures depending on their organization. The study of the water infiltration dynamics from the soil surface is highlyinformative non-destructive testing for evaluating the properties of the soil body. Studies showed that technosols as artificial creat

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19

Davis, Anthony M. "IDENTIFYING SOIL UNITS IN ARCHAEOLOGICAL SITES WITH COMPLEX STRATIGRAPHY." Canadian Geographer/Le Géographe canadien 30, no. 1 (March 1986): 85–87. http://dx.doi.org/10.1111/j.1541-0064.1986.tb01032.x.

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20

Bloomberg, D., S. B. Upchurch, M. L. Hayden, and R. C. Williams. "Cone-penetrometer exploration of Sinkholes: Stratigraphy and soil properties." Environmental Geology and Water Sciences 12, no. 2 (October 1988): 99–105. http://dx.doi.org/10.1007/bf02574794.

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21

Miglioranza, Karina S. B., Julia E. Aizpún de Moreno, and Víctor J. Moreno. "Trends in soil science: organochlorine pesticides in argentinean soils." Journal of Soils and Sediments 3, no. 4 (December 2003): 264–65. http://dx.doi.org/10.1007/bf02988686.

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22

HENRY, J. L., P. R. BULLOCK, T. J. HOGG, and L. D. LUBA. "GROUNDWATER DISCHARGE FROM GLACIAL AND BEDROCK AQUIFERS AS A SOIL SALINIZATION FACTOR IN SASKATCHEWAN." Canadian Journal of Soil Science 65, no. 4 (November 1, 1985): 749–68. http://dx.doi.org/10.4141/cjss85-080.

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The stratigraphy and hydrology of saline soils were investigated at 15 sites in Saskatchewan, Canada. At five sites (Series A) nests of piezometers were installed and at 10 sites (Series B) a single piezometer was installed in or near an aquifer. Piezometric surface data from the nests showed the potential for upward movement in all Series A sites. The electrical conductivity (EC) of water from Series A piezometers increased from the deepest to shallowest and there was a general increase in soil EC towards the soil surface. Hydraulic conductivity of strata was measured at three sites and varie

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23

Mohamad, Habib M., B. Kasbi, M. Baba, Z. Adnan, S. Hardianshah, and S. Ismail. "Investigating Peat Soil Stratigraphy and Marine Clay Formation Using the Geophysical Method in Padas Valley, Northern Borneo." Applied and Environmental Soil Science 2021 (May 18, 2021): 1–12. http://dx.doi.org/10.1155/2021/6681704.

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A geophysical survey including electrical resistivity tomography (ERT), induced polarization (IP), and seismic refraction (SR) was carried out to estimate peatland thickness in Beaufort District, Eastern Malaysia. Peatlands are important natural carbon storage and play a key role in the global carbon cycle. The ERT and IP studies were performed along three profiles over different peat thicknesses using Schlumberger configuration. The SR survey was carried out using vertical geophones along the same profiles. The peat soil material was characterized by low seismic velocity and high resistivity.

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Din, Moeen-ul, Jamal Ali, Abdul Qudoos Khan, and Farjad Sami. "Geotechnical Characteristics of Subsoil for Different Sectors of Islamabad." NUST Journal of Engineering Sciences 11, no. 1 (March 10, 2019): 33–40. http://dx.doi.org/10.24949/njes.v11i1.179.

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Geotechnical site investigations are essential in determining subsoil stratigraphy and soil strength and is considered mandatory for design of foundations. This study presents the generalized profiles for subsurface stratigraphy and insitu soil strength (average SPT N values) for different sectors of Islamabad on the basis of wide-ranging experimental work carried out by several agencies in fieldand laboratory testing carried out at the number of locations in the study area. Data from 208 geotechnical site investigations of Islamabad have been collected and subsurface profiling for those secto

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25

Wang, Qiang, Bingfang Wu, Alfred Stein, Liang Zhu, and Yuan Zeng. "Soil depth spatial prediction by fuzzy soil-landscape model." Journal of Soils and Sediments 18, no. 3 (August 19, 2017): 1041–51. http://dx.doi.org/10.1007/s11368-017-1779-0.

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26

Antarissubhi, Lawalenna Samang, Tri Harianto, and Indrabayu. "Study of Soil Layer Stratigraphy Based on Georesistivity and Geological Techniques." Materials Science Forum 998 (June 2020): 335–40. http://dx.doi.org/10.4028/www.scientific.net/msf.998.335.

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The purpose of study was to determine the structure of the studied soil layer based on measurement of geo-resistivity with the Wenner configuration and geotechnical drilling method. Geotechnical drilling was one way of soil/rock investigations to determine the parameters soil layers. Based on the objective, field tests and laboratory tests were carried out to support scientific investigations. The results of measurements in the field using geo-resistivity were performed to a depth of 23 meters, resulted in 2 types of soil sediment layers namely clay and sand. At a depth of approx. 8 meters, th

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27

Johnson, William C., Karen L. Willey, Joseph A. Mason, and David W. May. "Stratigraphy and environmental reconstruction at the middle Wisconsinan Gilman Canyon formation type locality, Buzzard's Roost, southwestern Nebraska, USA." Quaternary Research 67, no. 3 (May 2007): 474–86. http://dx.doi.org/10.1016/j.yqres.2007.01.011.

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AbstractThe middle Wisconsinan Gilman Canyon Formation at the Buzzard's Roost type locality in southwestern Nebraska was investigated to document the stratigraphy and to reconstruct the environmental and climate record. The Gilman Canyon Formation was subdivided into three loess units and three soils, with radiocarbon ages constraining it between about 40 ka and 25 ka. Stable carbon isotope ratios, magnetic susceptibility, and carbon content were used to define and characterize soils within both the Gilman Canyon Formation and underlying Illinoian Loveland Loess. At the height of soil developm

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28

Liang, Xiaomin, Qin Chen, Muhammad Shoaib Rana, Zhihao Dong, XiaoDong Liu, Chengxiao Hu, Qiling Tan, Xiaohu Zhao, Xuecheng Sun, and Songwei Wu. "Effects of soil amendments on soil fertility and fruit yield through alterations in soil carbon fractions." Journal of Soils and Sediments 21, no. 7 (May 3, 2021): 2628–38. http://dx.doi.org/10.1007/s11368-021-02932-z.

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Szilágyi, Gábor, Pál Sümegi, Sándor Gulyás, and Dávid Molnár. "Revision of the Age of Construction Phases of a Mound Dated to the Late Copper–Early Bronze Age in Eastern Hungary Relying on14C-Based Chronologies." Radiocarbon 60, no. 5 (October 2018): 1403–12. http://dx.doi.org/10.1017/rdc.2018.107.

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ABSTRACTEcse Mound is a burial mound in the Hortobágy region of eastern Hungary. Built by prehistoric nomadic peoples from the east, it now stands on the border between two modern settlements. The construction of the mound was assumed to be related to representatives of the Pit Grave Culture populating the area between the Late Copper and Bronze Ages. This theory considered similarities in shape, orientation, and stratigraphy of this mound with other absolute-dated ones in the Hortobágy region alone. The mound comprises two construction layers as indicated by magnetic susceptibility and on-sit

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Pereira, Marlon Correa, Roisin O’Riordan, and Carly Stevens. "Urban soil microbial community and microbial-related carbon storage are severely limited by sealing." Journal of Soils and Sediments 21, no. 3 (January 29, 2021): 1455–65. http://dx.doi.org/10.1007/s11368-021-02881-7.

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Abstract Purpose Urbanisation causes changes in land use, from natural or rural to urban, leading to the sealing of soil and the replacement of vegetation by buildings, roads and pavements. The sealing process impacts soil properties and services and can lead to negative consequences for microbial attributes and processes in soil. At present, information about the microbial community following soil sealing is limited. As such, we investigated how changes in soil physical and chemical properties caused by sealing affect the soil microbial community and soil ecosystem services. Material and meth

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31

ZAADY, ELI, and ZVI Y. OFFER. "Biogenic soil crusts and soil depth: a long-term case study from the Central Negev desert highland." Sedimentology 57, no. 2 (February 2010): 351–58. http://dx.doi.org/10.1111/j.1365-3091.2009.01081.x.

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D'Amore, David V., Scott R. Stewart, J. Herbert Huddleston, and J. Reed Glasmann. "Stratigraphy and Hydrology of the Jackson-Frazier Wetland, Oregon." Soil Science Society of America Journal 64, no. 4 (July 2000): 1535–43. http://dx.doi.org/10.2136/sssaj2000.6441535x.

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Ukalska-Jaruga, Aleksandra, Guillaume Debaene, and Bożena Smreczak. "Dissipation and sorption processes of polycyclic aromatic hydrocarbons (PAHs) to organic matter in soils amended by exogenous rich-carbon material." Journal of Soils and Sediments 20, no. 2 (September 16, 2019): 836–49. http://dx.doi.org/10.1007/s11368-019-02455-8.

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Abstract Purpose The aim of the research was to assess the effect of biochar addition on aging, degradation, and sorption processes of polycyclic aromatic hydrocarbons (PAHs) to soil organic matter. The study was carried out as a sorption experiment in strictly controlled water and air conditions, which allowed for the accurate observation and prediction of PAH behavior in soils. Materials and methods Four soils were fortified with a PAH mixture (Fluorene-Flu, Anthracene-Ant, Phenanthrene-Phe, Pyrene-Pyr, Chrysene-Chry) at 20 mg kg−1 of single-compound concentration level. The experiment was c

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Philippot, Laurent, Cristina Abbate, Antonio Bispo, Thierry Chesnot, Sara Hallin, Philippe Lemanceau, Kristina Lindström, et al. "Soil microbial diversity: an ISO standard for soil DNA extraction." Journal of Soils and Sediments 10, no. 7 (July 6, 2010): 1344–45. http://dx.doi.org/10.1007/s11368-010-0265-8.

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Kruczkowska, Bogusława, Jerzy Jonczak, Sandra Słowińska, Arkadiusz Bartczak, Mateusz Kramkowski, Łukasz Uzarowicz, Sebastian Tyszkowski, and Michał Słowiński. "Stages of soil development in the coastal zone of a disappearing lake—a case study from central Poland." Journal of Soils and Sediments 21, no. 3 (January 29, 2021): 1420–36. http://dx.doi.org/10.1007/s11368-021-02880-8.

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Abstract Purpose The aim of this study was to estimate the impact of lake disappearance, groundwater table fluctuations, and some aspects of human pressure on stages of soil cover development in the catchment of Lake Rakutowskie. Materials and methods Research was conducted in soil chronosequence composed of eight soil profiles located in 785-m-long transect. Soils were sampled every 10 cm. Physical and chemical properties were determined with the use of disturbed and undisturbed samples. Radiocarbon dates were obtained for the bottom part of peat in each soil profile. The mineral composition

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Kulatilake, Pinnaduwah H. S. W. "Modelling of cyclical stratigraphy using Markov chains." International Journal of Mining and Geological Engineering 5, no. 2 (July 1987): 121–30. http://dx.doi.org/10.1007/bf01560870.

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Römbke, Jörg. "Workshop on Research Projects on Soil Biology, Soil Ecotoxicity and Precautionary Soil Protection (Bonn, 22nd—23rd October 2001)." Journal of Soils and Sediments 2, no. 3 (September 2002): 159. http://dx.doi.org/10.1007/bf02988473.

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Wang, Ke, Xiaoyuan Zhang, Cengceng Sun, Kaiqi Yang, Jiyong Zheng, and Jihai Zhou. "Biochar application alters soil structure but not soil hydraulic conductivity of an expansive clayey soil under field conditions." Journal of Soils and Sediments 21, no. 1 (September 30, 2020): 73–82. http://dx.doi.org/10.1007/s11368-020-02786-x.

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Gunarathne, Viraj, Nishanta Rajakaruna, Udaya Gunarathne, Jayanta Kumar Biswas, Zach A. Raposo, and Meththika Vithanage. "Influence of soil water content and soil amendments on trace metal release and seedling growth in serpentine soil." Journal of Soils and Sediments 19, no. 12 (June 4, 2019): 3908–21. http://dx.doi.org/10.1007/s11368-019-02349-9.

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Kwiatkowska-Malina, Jolanta. "Qualitative and quantitative soil organic matter estimation for sustainable soil management." Journal of Soils and Sediments 18, no. 8 (December 28, 2017): 2801–12. http://dx.doi.org/10.1007/s11368-017-1891-1.

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Urbańska, Magdalena, and Przemysław Charzyński. "SUITMAs as an archive of the human past: educational implications." Journal of Soils and Sediments 21, no. 5 (February 18, 2021): 1928–37. http://dx.doi.org/10.1007/s11368-021-02886-2.

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Abstract Purpose The relics of the industry are widely used for educational and touristic purposes. There are many examples of brownfield sites turned into tourist attractions. Interest in post-industrial areas concerns not only an infrastructure and ruins but also the soil cover. Soils in such areas should be also considered as important element of this type of landscape due to the artefacts’ stored. This article aim is to present educational potential of post-industrial soils and artefacts to be found there on the example of the area of “Polchem”. Methods and materials This publication is ba

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Zuo, Feng-Lin, Xiao-Yan Li, Xiao-Fan Yang, Yang Wang, Yu-Jun Ma, Yu-Han Huang, and Chao-Fu Wei. "Soil particle-size distribution and aggregate stability of new reconstructed purple soil affected by soil erosion in overland flow." Journal of Soils and Sediments 20, no. 1 (August 9, 2019): 272–83. http://dx.doi.org/10.1007/s11368-019-02408-1.

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Schneckenburger, Tatjana, and Sören Thiele-Bruhn. "Sorption of PAHs and PAH derivatives in peat soil is affected by prehydration status: the role of SOM and sorbate properties." Journal of Soils and Sediments 20, no. 10 (June 23, 2020): 3644–55. http://dx.doi.org/10.1007/s11368-020-02695-z.

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Abstract Purpose Sorption of organic compounds to soil largely determines their mobility and bioavailability in ecosystems. It is well known that molecular properties of the organic sorbates affect the sorbed amounts and sorption kinetics. But also changes in the hydration status of soils alter the physicochemical and sorptive properties of soil organic matter (SOM), which is the main sorbent for organic compounds in soils. This study elucidates the effects of varying SOM prehydration status on sorption of PAHs and PAH derivatives in peat soil. Materials and methods For sorption experiments, t

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Yu, Kun, Yang Duan, Maosheng Zhang, Ying Dong, Luchen Wang, Ye Wang, Xu Guo, and Fusheng Hu. "Using micro focus industrial computed tomography to characterize the effects of soil type and soil depth on soil pore characteristics, morphology, and soil compression in Xi’an, China." Journal of Soils and Sediments 20, no. 4 (December 19, 2019): 1943–59. http://dx.doi.org/10.1007/s11368-019-02536-8.

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Anker, Yaakov, Eliahu Rosenthal, Haim Shulman, and Akiva Flexer. "Multi-disciplinary modeling, in stratigraphy and groundwater stratigraphy of the Jordan River basin." Environmental Geology 57, no. 2 (May 7, 2008): 275–83. http://dx.doi.org/10.1007/s00254-008-1335-8.

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Sipos, Péter, Viktória Kovács Kis, Réka Balázs, Adrienn Tóth, and Tibor Németh. "Effect of pedogenic iron-oxyhydroxide removal on the metal sorption by soil clay minerals." Journal of Soils and Sediments 21, no. 4 (February 19, 2021): 1785–99. http://dx.doi.org/10.1007/s11368-021-02899-x.

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Abstract Purpose The close association of Fe-oxyhydroxides and clay minerals might influence the sorption properties of these components. We aimed to study the effect of removing the pedogenic Fe-oxyhydroxides on the sorption of Cd, Cu, Pb, and Zn by the clay mineral particles in soils with contrasting pH. Methods Competitive batch sorption experiments before and after Fe-oxyhydroxide extraction in soils were carried out together with the direct analysis of the metal sorption on individual particles of ferrihydrite, smectite, and illite/smectite by TEM. Results Ferrihydrite was a more effectiv

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Matschullat, Jörg. "Fundamentals of Soil Ecology." Journal of Soils and Sediments 5, no. 4 (October 2005): 256. http://dx.doi.org/10.1065/jss2005.11.005.

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Guerin, Turlough F. "Soil and sediments listservers." Journal of Soils and Sediments 1, no. 3 (September 2001): 133–36. http://dx.doi.org/10.1007/bf02986475.

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Blum, Winfried E. H. "European soil protection strategy." Journal of Soils and Sediments 3, no. 4 (December 2003): 242. http://dx.doi.org/10.1007/bf02988670.

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Blum, Winfried E. H., Martin H. Gerzabek, and Sigrid Schwarz. "Soil protection in Austria." Journal of Soils and Sediments 3, no. 4 (December 2003): 245–46. http://dx.doi.org/10.1007/bf02988672.

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