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Добірка наукової літератури з теми "Soils, Salts in"

Автор: Grafiati

Опубліковано: 4 червня 2021

Оновлено: 28 лютого 2023

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Статті в журналах з теми "Soils, Salts in"

Ngoc, Binh Vu. "Characteristics of Clay Soft Soil in the Mekong Delta of Vietnam and Improvement Result with Cement." Iraqi Geological Journal 55, no. 1A (January 31, 2022): 64–73. http://dx.doi.org/10.46717/igj.55.1a.5ms-2022-01-24.

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The results of research on the characteristics of soft clay soils distributed in some provinces of the Mekong Delta show that most of the soils are contaminated with easily soluble salts, containing organic matter, pH < 7. Sandy clay, clay in An Giang, and clay mud in Tien Giang are less acidic, not salty, and contamination of salts in the form of sulfate- chloride. Clay mud in Hau Giang is less acidic, less salt, and contamination of salts in the form of chloride-sulfate. Clay mud in Bac Lieu and Ca Mau are lots of salty soil, contaminated with chloride of salts. Peat soil in Kien Giang is

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Z.R., Gurbanova, and Ibragimov S.K. "The reclamation of included in the crop rotation of solonetz soils by sulfuric acid situated waste in the Caspian lowland." Ekologiya i stroitelstvo 4 (2018): 25–33. http://dx.doi.org/10.35688/2413-8452-2018-04-004.

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The paper concerns the problems of making healthy salinized soils of pre-Caspian lowland in Azerbaijan Republic by chemical melioration. As a result of carried out experiments it has been determined that washing soils by water results in gyps leaching in the soils and formation alkaline salts. It leads to soda formation, salinization of soils and alkalıne formation. Though washing by drywall does not result in new formation of precipitated gyps, its application as meliorant presents formation of alkaline salts and salinization of solis. Gypsing of soils significantly optimizes leaching of salt

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Opanasenko, N. Ye, A. P. Yevtushenko, and A. P. Grishina. "Magnesian alkalinity of trenching soils of Prichernomorskaya lowland." Fundamental and Applied Soil Science 15, no. 1-2 (March 18, 2014): 33–41. http://dx.doi.org/10.15421/041403.

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The data of scientists about spreading, genesis, composition and properties of low natrium soils with high content of magnesium in soil sorption complex, and its influence on plants have been considered. The aim was to determine the absorbed ability of soils and the level of saturation by bases; to determine the dependence of density of foundation, quantity of silt from the content of absorbed magnesium from magnesium water soluble salts in them; to determine kation-anion and salt composition of irrigation waters. The trenching low natrium remaining alkolinic south black soils, dark-chestnut,

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Manimel Wadu, Mihiri C. W., Tee Boon Goh, and Olalekan O. Akinremi. "Response of Manitoba soils to banding phosphorus with sulfate or carbonate salts." Canadian Journal of Soil Science 96, no. 4 (December 1, 2016): 447–60. http://dx.doi.org/10.1139/cjss-2015-0083.

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Applications of sulfate and carbonate salts have been shown to improve the solubility of phosphorus (P) in model calcareous soils. It is unclear how these treatments will influence P solubility in real soils. The objective of this study was to determine the effect of sulfate or carbonate salts on P solubility in selected Manitoba soils. We hypothesized that the application of carbonate or sulfate salts in a fertilizer band could enhance the solubility of P in Manitoba soils. Different salt mixtures were prepared by mixing either monopotassium phosphate (MPP) or monoammonium phosphate (MAP) wit

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Pessoa, Luiz Guilherme Medeiros, Maria Betânia Galvão dos Santos Freire, José Coelho de Araújo Filho, Patrícia Ribeiros dos Santos, Márcio Fléquisson Alves Miranda, and Fernando José Freire. "Characterization and Classification of Halomorphic Soils in the Semiarid Region of Northeastern Brazil." Journal of Agricultural Science 11, no. 4 (March 15, 2019): 405. http://dx.doi.org/10.5539/jas.v11n4p405.

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The properties of halomorphic soils are controlled by the presence of either soluble salts, exchangeable sodium or both, and it is important to know and understand these properties in order to reforest and/or recover the soils. The objective of this study was to characterize and classify halomorphic soils from the semiarid region of Northeast Brazil. Four profiles of halomorphic soils were studied, which were described morphologically and the samples were collected from all soil horizons. Physical and chemical analyzes of the soils were carried out for classification purposes, as well as geoch

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Pochernyaeva, E. P., V. O. Okata, O. V. Kotovych, and V. M. Yakovenko. "Influence of irrigated mineralized waters on properties of ordinary chernozem in the conditions of Prysamaria Dniprovske." Ecology and Noospherology 31, no. 2 (October 25, 2020): 93–98. http://dx.doi.org/10.15421/032015.

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Irrigation of lands in arid climates helps to solve the problem of water deficit of soils in order to increase their fertility. However, under the influence of mineralized waters used for irrigation, there is a degradation of chemical, physico-chemical, water-physical and physical properties of soils. Soil monitoring is one of the effective mechanisms that allowsassessing the current state of soils and predicting the negative consequences of economic activity in the future. The area where the research was conducted is in the zone of insufficient moisture where there is an annual deficit of wat

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Černohlávková, J., J. Hofman, T. Bartoš, M. Sáňka, and P. Anděl. "Effects of road deicing salts on soil microorganisms." Plant, Soil and Environment 54, No. 11 (December 2, 2008): 479–85. http://dx.doi.org/10.17221/431-pse.

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In this study, the effects of road salting on the quality of forest soils near the road were monitored in the Krkonoše Mountains (Czech Republic). Physical, chemical properties and microbial parameters of soils were determined and the toxic potentials of soil water extracts were evaluated using the bacterial tests (Microtox and <I>Pseudomonas putida</I> growth inhibition test). Increased concentrations of Na<sup>+</sup> ions (up to 100 mg/kg) and pH values up to 8 were found closer to the road. Microbial biomass and respiration activity were significantly reduced at the

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Gulledge, Jay, and Joshua P. Schimel. "Low-Concentration Kinetics of Atmospheric CH4 Oxidation in Soil and Mechanism of NH4+ Inhibition." Applied and Environmental Microbiology 64, no. 11 (November 1, 1998): 4291–98. http://dx.doi.org/10.1128/aem.64.11.4291-4298.1998.

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ABSTRACT NH4 + inhibition kinetics for CH4 oxidation were examined at near-atmospheric CH4 concentrations in three upland forest soils. Whether NH4 +-independent salt effects could be neutralized by adding nonammoniacal salts to control samples in lieu of deionized water was also investigated. Because the levels of exchangeable endogenous NH4 + were very low in the three soils, desorption of endogenous NH4 +was not a significant factor in this study. TheKm(app) values for water-treated controls were 9.8, 22, and 57 nM for temperate pine, temperate hardwood, and birch taiga soils, respectively.

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Pukish, Arsen. "STUDY OF THE RESTORATION FEATURES OF SOILS THAT WERE INFLUENCED BY FORMATION WATERS." Scientific Bulletin Series D : Mining, Mineral Processing, Non-Ferrous Metallurgy, Geology and Environmental Engineering 31, no. 2 (2017): 71–76. http://dx.doi.org/10.37193/sbsd.2017.2.10.

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The article presents the studies results on the restoration of saline soils affected by formation waters. Soil restoration was carried out using solutions of various water-soluble salts. The author determined that treatment of saline soils with a solution of magnesium sulfate at a concentration of 0,3 mol/dm3 helps to decrease the content of chlorides, sodium, calcium, while the content of magnesium and sulfates increases, but the total content of toxic salts in the soil decreases by 60,9%.

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Chartres, CJ. "Sodic soils - an introduction to their formation and distribution in Australia." Soil Research 31, no. 6 (1993): 751. http://dx.doi.org/10.1071/sr9930751.

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This paper briefly summarizes existing Australian data about causes of sodicity and the distribution of sodic soils in Australia. Sources of salts and sodium include atmospheric accession, salts released by weathering processes and saline groundwaters. A traditional model of sodic soil pedogenesis is contrasted with more recent data demonstrating the role of several factors including mineralogy, EC/ESP relationships and exchangeable magnesium percentage on development and behaviour of sodic soils. Limited data about the national distribution of sodic soils are presented. There has been very li

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Дисертації з теми "Soils, Salts in"

Barzegar, Abdolrahman. "Structural stability and mechanical strength of salt-affected soils." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09PH/09phb296.pdf.

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Copies of author's previously published articles in pocket inside back cover. Bibliography: leaves 147-160. This thesis outlines the factors affecting soil strength and structural stability and their interrelationship in salt-affected soils. The objectives of this study are to investigate the influence of clay particles on soil densification and mellowing, the mellowing of compacted soils and soil aggregates as influenced by solution composition, the disaggregation of soils subjected to different sodicities and salinities and its relationship to soil strength and dispersible clay and the effec

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Chang, Jingwei, and 常经纬. "Effect of pore water salt content on the coefficient of earth pressure at rest of fine-grained soils." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hdl.handle.net/10722/202253.

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Wong, Vanessa Ngar Lai. "The effects of salinity and sodicity on soil organic carbon stocks and fluxes /." View thesis entry in Australian Digital Theses Program, 2007. http://thesis.anu.edu.au/public/adt-ANU20080428.223144/index.html.

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Nathan, Muhammad. "Clay movement in a saline-sodic soil toposequence." Title page, contents and summary only, 2001. http://web4.library.adelaide.edu.au/theses/09A/09an274.pdf.

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Includes bibliographical references (leaves 78-86) In the Herrmanns sub-catchment in the Mt. Lofty Ranges (near Mt. Torrens) soil sodicity was the dominant factor in causing clay to disperse in the eroded area along the foot slopes, wheras in non-eroded areas of the mid-slopes and on the stream banks, the dispersive power of sodicity was attenuated by the flocculative power of other soil properties.

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Wearing, Cameron. "Sodicity and soil microstructure /." [St. Lucia, Qld.], 2005. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18523.pdf.

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McCarthy, Alan John. "Landcare : a means of sustaining viticulture in the Barossa Valley /." Title page, table of contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09ENV/09envm1228.pdf.

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Marwan, M. M. "Changes in physical and chemical properties of saline-sodic soils during removal of salts by leaching with water." Thesis, University of Reading, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.234663.

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Vernon, Daniel Marc. "Molecular biology of salt tolerance in the facultative halophyte Mesembryanthemum crystallinum: Identification and regulation of stress-responsive mRNAs." Diss., The University of Arizona, 1992. http://hdl.handle.net/10150/185921.

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As sessile organisms, plants are subject to numerous environmental insults. Of these, salinity is one of the most widespread and important in terms of limiting plant distribution and productivity. Molecular studies have established that plants challenged by high salinity respond by increasing expression of specific genes. A functional role for the products of such genes in stress tolerance has not been established, however, and little is known about the biochemical mechanisms that allow plants to tolerate osmotic stress. Mesembryanthemum crystallinum is a facultative halophyte capable of adjus

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Gao, Yuan. "Changes of tomato fruit composition in response to salinity /." Title page, contents and summary only, 1991. http://web4.library.adelaide.edu.au/theses/09A/09ag211.pdf.

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Sessoms, Holly Nicol. "Water use potential and salt tolerance of riparian species in saline-sodic environments." Thesis, Montana State University, 2004. http://etd.lib.montana.edu/etd/2004/sessoms/SessomsH0805.pdf.

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Книги з теми "Soils, Salts in"

Peinemann, Norman. Procesos de salinización en el partido de Guaminí. [Bahía Blanca, Argentina]: Departamento de Agronomía, Universidad Nacional del Sur, 1997.

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K, Gupta S. Crop production in waterlogged saline soils. Jodhpur: Scientific Publishers, 1997.

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Hazelden, J. Saline soils in North Kent. Harpenden: Soil Survey of England and Wales, 1986.

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Finlayson, Nancy M. Salt movement in disturbed soils. Edmonton, Alta: Alberta Land Conservation and Reclamation Council, Reclamation Research Technical Advisory Committee, 1993.

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Burvill, G. H. The soils of the Salmon Gums district - Western Australia. Perth: Western Australia Department of Agriculture, 1988.

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Abrol, I. P. Salt-affected soils and their management. Rome: Food and Agriculture Organization of the United Nations, 1988.

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College, Manitoba Agricultural, ed. Suggestions on the treatment of alkali soils. [Winnipeg: s.n.], 1997.

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Salt-affected soils. Boca Raton, Fla: CRC Press, 1989.

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K, Saxena R., Indian Council of Agricultural Research. National Bureau of Soil Survey and Land Use Planning., and Central Soil Salinity Research Institute (Karnāl, India), eds. Salt affected soils, Etah District, Uttar Pradesh. Nagpur: National Bureau of Soil Survey & Land Use Planning, 2004.

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Fernando, Chanduvi, Lesch S. M, and Food and Agriculture Organization of the United Nations., eds. Soil salinity assessment: Methods and interpretation of electrical conductivity measurements. Rome: Food and Agriculture Organization of the United Nations, 1999.

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Частини книг з теми "Soils, Salts in"

Akramkhanov, Akmal, Ramazan Kuziev, Rolf Sommer, Christopher Martius, Oksana Forkutsa, and Luiz Massucati. "Soils and Soil Ecology in Khorezm." In Cotton, Water, Salts and Soums, 37–58. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1963-7_3.

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Howari, Fares M., Philip C. Goodell, and Seiichi Miyamoto. "Spectroscopy of Salts Common in Saline Soils." In From Laboratory Spectroscopy to Remotely Sensed Spectra of Terrestrial Ecosystems, 1–20. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-017-1620-8_1.

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Chhabra, Ranbir. "Nature and Origin of Salts, Classification, Area and Distribution of Salt-affected Soils." In Salt-affected Soils and Marginal Waters, 1–47. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-78435-5_1.

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Pulatov, Alim, Oybek Egamberdiev, Abdullah Karimov, Mehriddin Tursunov, Sarah Kienzler, Ken Sayre, Latif Tursunov, John P. A. Lamers, and Christopher Martius. "Introducing Conservation Agriculture on Irrigated Meadow Alluvial Soils (Arenosols) in Khorezm, Uzbekistan." In Cotton, Water, Salts and Soums, 195–217. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1963-7_13.

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Al-Ani, A. F. "The Influence of Salts on Physical Properties of Soils." In Hydraulic Design in Water Resources Engineering: Land Drainage, 365–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-662-22014-6_34.

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Shahid, Shabbir A., Mahmoud A. Abdelfattah, and Henda Mahmoudi. "Innovations in Soil Chemical Analyses: New ECs and Total Salts Relationship for Abu Dhabi Emirate Soils." In Developments in Soil Classification, Land Use Planning and Policy Implications, 799–812. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5332-7_46.

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Montoroi, Jean-Pierre. "Soil Salinization and Management of Salty Soils." In Soils as a Key Component of the Critical Zone 5, 97–126. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2018. http://dx.doi.org/10.1002/9781119438298.ch5.

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Choudhary, Madhu, Priyanka Chandra, and Sanjay Arora. "Soil-Plant-Microbe Interactions in Salt-affected Soils." In Research Developments in Saline Agriculture, 203–35. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-5832-6_6.

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Felix-Henningsen, P., B. Rummel, and H. P. Blume. "Soil Processes and Salt Dynamics in Dune Soils." In Ecological Studies, 225–38. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-75498-5_16.

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Chhabra, Ranbir. "Alkali Soils." In Salt-affected Soils and Marginal Waters, 209–54. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-78435-5_5.

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Тези доповідей конференцій з теми "Soils, Salts in"

Nosova, M. V., and V. P. Seredina. "COMPARATIVE CHARACTERISTICS OF THE ECOLOGICAL STATE OF SOILS CONTAMINATED WITH MINERALIZED LIQUIDS AND OIL (WESTERN SIBERIA)." In SAKHAROV READINGS 2022: ENVIRONMENTAL PROBLEMS OF THE XXI CENTURY. International Sakharov Environmental Institute of Belarusian State University, 2022. http://dx.doi.org/10.46646/sakh-2022-2-275-278.

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The features of the distribution of technogenic halogenesis processes on the soil of various cascade-geochemical positions of the landscape are determined. It was revealed that technogenic salinization is the most detrimental for floodplain soils, since these soils are a kind of main “collection point” for all pollutants. The features and chemistry of technogenic halogenesis processes (content, qualitative composition, patterns of migration and distribution of easily soluble salts, including those toxic to plants) in soils of various pollution zones - the epicenter, the impact zone, the bounda

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Gray, D. H. "Movement of Moisture and Dissolved Salts from Soils into Concrete Foundations." In Geo-Denver 2000. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40510(287)36.

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Abbeche, K., O. Bahloul, T. Ayadat, and A. Bahloul. "Treatment of Collapsible Soils by Salts Using the Double Consolidation Method." In GeoShanghai International Conference 2010. Reston, VA: American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41103(376)10.

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Baraza Piazuelo, Teresa, and Elizabeth A. Hasenmueller. "DO SOILS SLOW THE TRANSPORT OF WINTER DEICING SALTS TO SHALLOW GROUNDWATER?" In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321022.

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Drovovozova, T. I., S. A. Marias, E. S. Kulakova, and N. N. Panenko. "GEOECOLOGICAL CYCLES OF SALT-FORMING IONS IN AGRICULTURAL LANDSCAPES." In STATE AND DEVELOPMENT PROSPECTS OF AGRIBUSINESS. DSTU-PRINT, 2020. http://dx.doi.org/10.23947/interagro.2020.1.509-513.

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The analysis of the chemical composition of natural water bodies-receivers of drainage and discharge waters. It is shown that the background concentrations of salt-forming ions in water bodies exceed the Mpcrx, which indicates the dominant influence of surface runoff from the entire catchment area and underground feeding by mineralized sulphate groundwater on the formation of the quality of the water environment. The chemical composition of water extract from the soil from irrigated areas adjacent to reservoirs was studied on the example of semikarakorsky district of the Rostov region. The cla

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Diaz, Melisa A., Byron J. Adams, Ian Hogg, Noah Fierer, Diana H. Wall, Christopher B. Gardner, Marcella Shaver-Adams, and W. Berry Lyons. "DISTRIBUTION OF WATER-SOLUBLE SALTS IN SOILS OF THE SHACKLETON GLACIER REGION, ANTARCTICA AND IMPLICATIONS FOR SOIL HABITABILITY." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319464.

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Ribeiro, A., C. Vilarinho, J. Araújo, and J. Carvalho. "Electrokinetic Remediation of Contaminated Soils With Chromium." In ASME 2018 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/imece2018-87552.

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Soil is a vital natural resource that regulates our environment sustainability and provide essential resources to humans and nature. Nowadays, with an increasingly populated and urbanized world, pollution is widely recognized as a significant challenge to soil and groundwater resources management. The most common chemicals found in soils and water plumb in a dissolved state and considered as potential pollutants are heavy metals, dyes, phenols, detergents, pesticides, polychlorinated biphenyls (PCBs), and others organic substances, such as organic matter. Unlike organic contaminants, heavy met

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Pristipa, K. V., T. A. Kukulyanskaya, and E. A. Khramtsova. "The content of low molecular weight antioxidants in transgenic plants Nicotiana tabacum under heavy metal salts conditions." In 2nd International Scientific Conference "Plants and Microbes: the Future of Biotechnology". PLAMIC2020 Organizing committee, 2020. http://dx.doi.org/10.28983/plamic2020.199.

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We were studied several of antioxidants in transgenic Nicotiana tabacum, plants cultivated in heavy metal polluted soils. The content of phenolic compounds, vitamins C and E in plants increased under these conditions.

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Vlasyuk, Anatoliy, Tetiana Tsvetkova, Pawel Falat, Aleksandra Klos-Witkowska, and Kornel Warwas. "Mathematical modelling of infiltration effect on process of salts transfer in layered saturated-non-saturated soils." In 2017 9th IEEE International Conference on Intelligent Data Acquisition and Advanced Computing Systems: Technology and Applications (IDAACS). IEEE, 2017. http://dx.doi.org/10.1109/idaacs.2017.8095100.

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Larson, Steven, John Ballard, Christopher Griggs, J. Kent Newman, and Catherine Nestler. "An Innovative Non-Petroleum Rhizobium Tropici Biopolymer Salt for Soil Stabilization." In ASME 2010 International Mechanical Engineering Congress and Exposition. ASMEDC, 2010. http://dx.doi.org/10.1115/imece2010-38933.

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Construction site soils are a significant source of sediment, and pollutants carried by sediment, to surface water runoff. Currently, silt fences/barriers, petroleum-derived polymers, and re-vegetation are the primary tools to prevent sediment loss from construction areas. Even with these methods in place, the U. S. Environmental Protection Agency estimates that 20 to 150 tons of soil per acre is lost to storm water runoff from construction sites each year. A low-cost, environmentally friendly soil amendment that reduces erosion from construction sites would improve surface water quality. An e

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Shaw, P., B. Anderson, and D. Davis. Laboratory scale vitrification of low-level radioactive nitrate salts and soils from the Idaho National Engineering Laboratory. Office of Scientific and Technical Information (OSTI), July 1993. http://dx.doi.org/10.2172/10192334.

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Miyamoto, Seiichi, and Rami Keren. Improving Efficiency of Reclamation of Sodium-Affected Soils. United States Department of Agriculture, December 2000. http://dx.doi.org/10.32747/2000.7570569.bard.

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Sodium affected soils, along with salt-affected soils, are distributed widely in irrigated areas of the arid and semi-arid region of the world. Some of these soils can and must be reclaimed to meet the increasing demand for food, and existing irrigated lands must be managed to reduce salinization and alkalization associated with deteriorating irrigation water quality. This project was conducted for examining ways to reduce the use of chemical amendments and large quantities of leaching water for reclaiming sodic soils or for preventing soil sodification, We hypothesized that sodicity of calcar

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Steenhuis, Tammo S., Israela Ravina, Jean-Yves Parlange, Rony Wallach, and Larry D. Geohring. Improving Preferential Flow Modules by Experimentation. United States Department of Agriculture, September 1994. http://dx.doi.org/10.32747/1994.7570552.bard.

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Preferential flow is the process whereby water and solutes move by preferred pathways. During preferential flow, local wetting fronts propagate to considerable depths in the soil profile, essentially bypassing the matrix pore space. Under such conditions classical methods, such as the convective-dispersive equation, for quantifying flow of water and solutes in uniform soils are not valid. This project set out to develop methods to predict fast and early breakthrough of solutes. To facilitate understanding of these processes, several field drainage studies were conducted in the United States an

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Bradford, Joe, Itzhak Shainberg, and Lloyd Norton. Effect of Soil Properties and Water Quality on Concentrated Flow Erosion (Rills, Ephermal Gullies and Pipes). United States Department of Agriculture, November 1996. http://dx.doi.org/10.32747/1996.7613040.bard.

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Concentrated flow erosion in rills, pipes, ephermal gullies, and gullies is a major contributor of downstream sedimentation. When rill or gullies form in a landscape, a 3- to 5-fold increase in soil loss commonly occurs. The balance between the erosive power of the flow and the erosion resistance of the bed material determines the rate of concentrated flow erosion. The resistance of the bed material to detachment depends primarily on the magnitude of the interparticle forces or cohesion holding the particles and aggregates together. The effect of soil properties on bed material resistance and

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Huiskes, A. H., and J. Nieuwenhuize. Uptake of Heavy Metals from Contaminated Soils by Salt-Marsh Plants. Fort Belvoir, VA: Defense Technical Information Center, May 1985. http://dx.doi.org/10.21236/ada157174.

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M., Devkota, Gupta R.K., Martius C., Lamers J.P.A., Sayre K.D., and Vlek P.L.G. Soil salinity management on raised beds with different furrow irrigation modes in salt-affected lands. Center for International Forestry Research (CIFOR), 2015. http://dx.doi.org/10.17528/cifor/005519.

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Dermatas, D. Stabilization and reuse of heavy metal contaminated soils by means of quicklime sulfate salt treatment. Final report, September 1992--February 1995. Office of Scientific and Technical Information (OSTI), August 1995. http://dx.doi.org/10.2172/201739.

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Berkowitz, Jacob, Christine VanZomeren, and Nicole Fresard. Rapid formation of iron sulfides alters soil morphology and chemistry following simulated marsh restoration. Engineer Research and Development Center (U.S.), September 2021. http://dx.doi.org/10.21079/11681/42155.

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Many marshes show signs of degradation due to fragmentation, lack of sediment inputs, and erosion which may be exacerbated by sea level rise and increasing storm frequency/intensity. As a result, resource managers seek to restore marshes via introduction of sediment to increase elevation and stabilize the marsh platform. Recent field observations suggest the rapid formation of iron sulfide (FeS) materials following restoration in several marshes. To investigate, a laboratory microcosm study evaluated the formation of FeS following simulated restoration activities under continually inundated, s

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Langton, C. TECHNETIUM OXIDATION IN SLAG-BASED SODIUM SALT WASTE FORMS EXPOSED TO WATER AND MOIST HANFORD SOIL. Office of Scientific and Technical Information (OSTI), August 2014. http://dx.doi.org/10.2172/1165533.

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Langton, C. TC OXIDATION IN SLAG-BASED SODIUM SALT WASTE FORMS EXPOSED TO WATER AND MOIST HANFORD SOIL. Office of Scientific and Technical Information (OSTI), August 2014. http://dx.doi.org/10.2172/1150632.

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