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Thematische Bibliographien / Soils, Salts in / Zeitschriftenartikel

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Zeitschriftenartikel zum Thema „Soils, Salts in“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 28. Februar 2023

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1

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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LI, XIAOYU, CHUNSHENG MU, JIXIANG LIN, YING WANG, and XIUJUN LI. "EFFECT OF ALKALINE POTASSIUM AND SODIUM SALTS ON GROWTH, PHOTOSYNTHESIS, IONS ABSORPTION AND SOLUTES SYNTHESIS OF WHEAT SEEDLINGS." Experimental Agriculture 50, no. 1 (September 9, 2013): 144–57. http://dx.doi.org/10.1017/s0014479713000458.

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SUMMARYPotassium (K) is an essential nutrient and abundant cation in plant cells. The application of K+ could alleviate abiotic stress. However, it was reported that the alleviation of K+ on salt-stressed plants only happened when K+ concentration was low. Most studies were focused on effects of sodium salts on plants in salty soils, and little information was reported about potassium salts, especially a higher level of potassium in alkaline salts. To explore the effects of K+ in alkaline salts on plant growth, and whether it had a same destructive impact as Na+, we mixed two alkaline sodium s

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Płatkowski, Maciej, and Arkadiusz Telesiński. "Effect of different glyphosate salts on phosphodiesterase and phosphotriesterase activities in soil with reference to ecological importance of soil pollution. A laboratory experiment." Ochrona Srodowiska i Zasobów Naturalnych 26, no. 2 (June 1, 2015): 9–14. http://dx.doi.org/10.1515/oszn-2015-0006.

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AbstractThe aim of this study is to determine the effect of the two glyphosate salts: isopropylamine and potassium (contained in preparations Roundup) on the activity of phosphodiesterase and phosphotriesterase in the soil. The experiment was carried out in the laboratory conditions on two soil types: loamy sand (Corg 8.70 g·kg−1, pHKCl 6.39) and sandy loam (Corg 10.90 g·kg−1, pHKCl 6.81). Two glyphosate salts (isopropylamine and potassium) in dosage of 0, 1 and 100 mg·kg−1 were applicate into soils. Phosphodiesterase and phospotriesterase activities in soils were determined spectrophotometric

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Al-Obaidi, Ahmed A. H., and Ibtihal H. S. Al-Mafragei. "Settlement and Collapse of Gypseous Soils." Tikrit Journal of Engineering Sciences 23, no. 1 (February 28, 2016): 20–31. http://dx.doi.org/10.25130/tjes.23.1.03.

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The work in this research presents an experimental, theoretical and field study in order to investigate the settlement of Gypseous soils and the effect of water percolation on collapsibility of this soil. In this research, more than five sites where chosen to extract the gypseous soil samples with different gypsum content; the sites located in different regions in Salah Aldeen Governorate. In order to estimate the settlement and collapse of gypseous soils, field tests consist of standard penetration test for depths (1m to 5m) for each site and plate load test were conducted in dry and soaked c

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King, G. M., and S. Schnell. "Effects of Ammonium and Non-Ammonium Salt Additions on Methane Oxidation by Methylosinus trichosporium OB3b and Maine Forest Soils." Applied and Environmental Microbiology 64, no. 1 (January 1, 1998): 253–57. http://dx.doi.org/10.1128/aem.64.1.253-257.1998.

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ABSTRACT Additions of ammonium and non-ammonium salts inhibit atmospheric methane consumption by soil at salt concentrations that do not significantly affect the soil water potential. The response of soils to non-ammonium salts has previously raised questions about the mechanism of ammonium inhibition. Results presented here show that inhibition of methane consumption by non-ammonium salts can be explained in part by ion-exchange reactions: cations desorb ammonium, with the level of desorption varying as a function of both the cation and anion added; differential desorption results in differen

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Kravchenko, E. I., N. B. Khitrov, and I. N. Gorokhova. "TWO-DIMENSIONAL DISTRIBUTION OF SALINITY IN IRRIGATED SOILS NEAR THE IRRIGATION CHANNEL AT THE PLOT "CHERVLENOE" OF THE SVETLOYAR IRRIGATION SYSTEM." Dokuchaev Soil Bulletin, no. 94 (September 1, 2018): 19–37. http://dx.doi.org/10.19047/0136-1694-2018-94-19-37.

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The current state of irrigated soils’ salinity at the key plot located along the buried irrigation channel within the irrigated plot Chervlenoye of the Svetloyar Irrigation System (Volgograd Region) was studied. In the 1990-s a strong sec-ondary soil salinization was detected during the aerial survey. Its boundaries were clearly observed on the image. After the irrigation had been ceased, a par-tial soluble salts leaching from the soil took place at the key plot as a result of precipitation and decrease of the groundwater table. Basing on the field data obtained in 2017 a model of two-dimensio

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McBride, Murray B., and Meifang Cai. "Copper and zinc aging in soils for a decade: changes in metal extractability and phytotoxicity." Environmental Chemistry 13, no. 1 (2016): 160. http://dx.doi.org/10.1071/en15057.

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Environmental contextTrace metal toxicities to soils and plants depend on residence time in soils, a poorly understood phenomenon termed ‘aging’. Our research aimed to better understand long-term aging by measuring the solubility and toxicity of copper and zinc over a 10-year period after their addition to soils as soluble salts. We determined that, while metal solubility and toxicity did decrease in a decade, the highest levels of added metals (200 and 400mgkg–1) still had toxic effects on soybeans. AbstractTo assess long-term effects of field aging on Cu and Zn availability and phytotoxicity

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Khadeeva, E. R., O. G. Lopatovskaya, L. I. Saraeva, and T. E. Tkachuk. "Diversity of Soils of Southern Transbaikalia (on the Example of the Daursky Reserve)." Bulletin of Irkutsk State University. Series Biology. Ecology 36 (2021): 79–86. http://dx.doi.org/10.26516/2073-3372.2021.36.79.

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The paper presents the study of soil cover of the steppe areas on the territory of the Daursky State Nature Biosphere Reserve in Transbaikalia (East Siberia). We determined the types of soils in the area surrounding the currently dry Barun-Torey lake according to the modern classification: Chestnut typical and saline, Saline gleyed typical and sulfide (sor) typical. Typical chestnut soils are formed on the tops of lake terraces and form complexes with saline soils. Salted chestnut soils occupy transit landforms. Saline soils are confined to low relief forms of the shoreline and the bottom of t

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Zhang, Ying, Fa Yun Li, Ting Ting Sun, and Jin Long Wang. "Effect of Deicing Salts on Urban Soils and the Health of Roadside Pines (Pinus tabulaeformis) in Northeast China." Applied Mechanics and Materials 178-181 (May 2012): 353–56. http://dx.doi.org/10.4028/www.scientific.net/amm.178-181.353.

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Accumulation of high concentrations of Na and Cl ions in soils is one factor that hampers plant establishment along roadsides in regions where deicing salts are used to improve winter driving conditions. However, there is little information on the accumulation of deicing salts in roadside soil as well as on the phytotoxic impact of deicing salts on pines in Northeast China. The accumulation of salt in soil and injuries on pine needles (Pinus tabulaeformis) were investigated in the urban areas of Shenyang city in 2011. The results showed that the use of deicing salts on roads leads to the high

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Hootman, R. G., P. D. Kelsey, R. Reid, and K. von der Heide-Spravka. "Factors Affecting Accumulation of Deicing Salts in Soils Around Trees." Arboriculture & Urban Forestry 20, no. 3 (May 1, 1994): 196–201. http://dx.doi.org/10.48044/jauf.1994.035.

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Parkways, street tree planter boxes, and highway medians and roadsides are locations where soil accumulation of deicing salts is highest. Sodium chloride is the most common deicer applied in the United States. Sodium chloride and other salts accumulating in the root zone may instigate and exacerbate street tree decline. Salts affect soil aggregate stability, porosity, and water and nutrient uptake in trees. Data collected in Chicago, Illinois show much higher soil sodium (1,272 jxg/g) and chloride (348 |ig/g) in the center of newly installed, narrow, raised medians along Lake Shore Drive after

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Kumar, Ashok. "Use of Leptochloa fusca for the Improvement of Salt-Affected Soils." Experimental Agriculture 32, no. 2 (April 1996): 143–49. http://dx.doi.org/10.1017/s0014479700026053.

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SUMMARYThe grass Leptocloa fusca is very useful on salt-affected soils as it can tolerate extremely saline and alkaline conditions, Since its growth is not affected by gypsum application, planting with Leptochloa is a good biological method for the reclamation of alkaline soils. It is also well adapted to the waterlogging encountered on saline and alkaline soils, and improves the soil's physical, chemical and biological properties so that within two or three years many commercial and forage crops can be grown. Leptochloa excretes salts through specialized glands and is therefore reasonably pal

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Rocha, Vanessa. "Comparative study on Biochar salt absorption capacity in different saline concentrated solutions." Bionatura 6, no. 4 (November 15, 2021): 2150–55. http://dx.doi.org/10.21931/rb/2021.06.04.3.

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Salt-affected soils are caused by excess accumulation of salts. As soil salinity increases, salt effects can result in the degradation of soils. Previous studies have determined that biochar has the potential to reduce salt stress in soils. In this study, the electroconductive properties of biochar to adsorb salts were investigated in different saline-concentrated solutions. Pelletized, fragmented and powdered biochar were placed in solutions with concentrations of 0, 50, 500, 1000, and 2000 parts per million sodium chloride, respectively. Control treatments consisted of deionized water mixed

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Takhirova, N. B., F. I. Khudoyberdiyev, S. Bauatdinov, T. S. Bauatdinov, and M. N. Muratova. "Research of Reclamation Properties of Agricultural Glaukonite Ores on Salted Soils." Alinteri Journal of Agriculture Sciences 36, no. 1 (June 22, 2021): 598–601. http://dx.doi.org/10.47059/alinteri/v36i1/ajas21084.

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The article presents the results of studies of the agro-ore of glauconite of Karakalpakstan, its reclamation properties when used on saline soils of the Aral Sea region. The results of the studies showed that the annual application of enriched glauconite leads to a decrease in chloride and sulfate salts in the soil, and the content of harmless salts increases.

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Agyekum, Kofi, Joshua Ayarkwa, and Christian Koranteng. "Holistic Diagnosis of Rising Damp and Salt Attack in Two Residential Buildings in Kumasi, Ghana." Journal of Construction Engineering 2014 (July 24, 2014): 1–13. http://dx.doi.org/10.1155/2014/398627.

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Rising damp is one of the most severe phenomena that leads to decay and deterioration of both old and modern types of buildings. This study employed a holistic approach to dampness investigation and sought to examine the problem of rising damp in the walls of two residential apartments in Kumasi, Ghana. The study sought to determine the types of soluble salts and their concentrations in the soils and accumulated percentages in the walls over time and whether there exists any linkage between the salts in the walls and those in the ground. Results from the geotechnical survey of the building sit

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Biggs, A. J. W., K. Bryant, and K. M. Watling. "Soil chemistry and morphology transects to assist wetland delineation in four semi-arid saline lakes, south-western Queensland." Soil Research 48, no. 3 (2010): 208. http://dx.doi.org/10.1071/sr09127.

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Soils at 4 saline lakes (Wyara, Numalla, Wombah and Bindegolly) in semi-arid south-western Queensland were described and sampled to determine soil attributes that assist in the delineation of wetlands. Up to 4 sites were described in transects perpendicular to the lake edge. Samples from fixed depths were analysed for limited ionic chemistry and, in some cases, selected acid sulfate soil parameters. Lakebed soils were alkaline Hypersalic Hydrosols, changing to a variety of soils, including alkaline Rudosols and Podosols on adjacent lunettes and beach ridges. Gley colours and mottling were indi

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Rutherford, P. M., S. J. Dickinson, and J. M. Arocena. "Emergence, survival and growth of selected plant species in petroleum-impacted flare pit soils." Canadian Journal of Soil Science 85, no. 1 (February 1, 2005): 139–48. http://dx.doi.org/10.4141/s03-088.

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One of the prerequisites to phytoremediation of hydrocarbon-contaminated soils is that plants be able to germinate and become established in the presence of contaminants. This 5-wk growth chamber study examined the tolerance of five grasses and one legume to petroleum hydrocarbons (PHCs) and associated salts in three weathered, fine-textured, flare pit soils obtained from NE British Columbia. Plant tolerance to these soils was measured by percent seedling emergence (PSE), percent seedling survival (PSS) and 5-wk dry shoot biomass; a non-contaminated control soil was included in the study. The

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Zinchenko, E. V., I. N. Gorokhova, N. G. Kruglyakova, and N. B. Khitrov. "Modern state of irrigated soils at the south of the Volga upland." Dokuchaev Soil Bulletin, no. 104 (December 3, 2020): 68–109. http://dx.doi.org/10.19047/0136-1694-2020-104-68-109.

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The goal is to assess the impact of 50-year irrigation by sprinkling on soil processes occurring in the light-chestnut soils (Luvic Kastanozem (Loamic, Aric, Protosodic, Bathysalic)) of the southern slopes of the Volga upland at the Volga-Don interfluve (FSUE “Oroshaemoe”, the Volgograd region) with deep ground water. Water for irrigation is supplied from the Varvarovsky reservoir of the Volga-Don Canal system. It is characterized by a total dissolved salts of about 1 g/l, a bicarbonate-chloride-sulfate compositionwith an increased sodium content. Detailed morphological description of soil pro

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Ahmed, M., S. A. AI-Rawahy, M. S. AI-Kalbani, and J. K. AI-Handaly. "Leaching Potential of Some Omani Soils: Soil Column and Drip Irrigation Studies." Journal of Agricultural and Marine Sciences [JAMS] 4, no. 2 (June 1, 1999): 65. http://dx.doi.org/10.24200/jams.vol4iss2pp65-70.

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This paper reports the findings from leaching experiments conducted on some Omani soils. Seven samples from two locations in the Batinah coastal area of Oman were analyzed. Repacked soil columns of up to 30 cm in length were used in laboratory experiments to estimate the amount of water required for adequate leaching of salts from the soil profile. Two methods of leaching: continuous ponding and intermittent ponding were investigated. Results show that most of the salt (50-90%) is removed from the soil profile by the application of water equal in amount to the depth of soil to be leached. The

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Savenko, A. V., and V. S. Savenko. "About salt fractionation in the process of terrigenous aerosol generation." Геохимия 64, no. 1 (January 15, 2019): 96–100. http://dx.doi.org/10.31857/s0016-752564196-100.

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The content of water-soluble salts in samples of surface soils from arid regions and separated from them fraction <0.1 mm was analyzed. Existence of salt fractionation in the aleurite was shown. The fractionation coefficients, defined as the ratio of ions concentrations in the water extracts from fraction <0.1 mm and soil as a whole, are arranged in the successions: Na > K > Mg > Ca and SO4 > HCO3 > Cl. It was found that the fractionation of salts depends on their solubility: than solubility below, that enrichment of soils fine fraction is more.

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Л.Д., Гасымов. "Defination of the optimum dimensions in agroecosystems productivity under Lankaran Lowland condition in Azerbaijan." Ekologiya i stroitelstvo 2 (2019): 35–42. http://dx.doi.org/10.35688/2413-8452-2019-02-005.

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The real and prognosticated dimensions of the farming lands productivity under natural agroecosystems in the Lankaran lowland condition have been defined. It was determined that the soil, climate, subsoil level and other factors of the landscape influence on the farming land productivity under the Lankaran Lowland condition. The productivity of cereals on these soils is 45.2 centner/ha, vegetables 318.2 centners per hectare, tea 81.2 centners per hectare, fruit 62.1 centner/ha. With the implementation of agroecological measures to increase the fertility of yellow–meadow soils, it is optimal to

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Montes de Oca, Paulina, Rafael Mata, and Marco A. Chaves. "Estudios de salinidad en la provincia de Guanacaste (Costa Rica) y caracterización de algunos suelos con influencia salina." Agronomía Mesoamericana 7, no. 2 (June 2, 2016): 77. http://dx.doi.org/10.15517/am.v7i2.24766.

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The soils wich are affected by salts are developing preferently in regions where the precipitation is limited, the temperature is high and the conditions of drainage are restricted like in some soils of Guanacaste's area. A bibliography review about some soils with high salts contents was made in Ing. Taboga, Guanacaste's area. Two soils samples was taking classified in Typic hapluster and Fluventic ustropept. There are analized with methods that caracterize the salinity of soils jour with the technics of rutinary analysis.

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Kakuturu, Sai, and Shirley E. Clark. "Deicing Salts' Effects on Engineered Bioretention Soils." Proceedings of the Water Environment Federation 2012, no. 5 (January 1, 2012): 568–76. http://dx.doi.org/10.2175/193864712811699294.

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Smettan, U., and H. P. Blume. "Salts in sandy desert soils, southwestern Egypt." CATENA 14, no. 4 (August 1987): 333–43. http://dx.doi.org/10.1016/0341-8162(87)90025-7.

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Hoshan, Muhsen N. "Review of Reclamation of salinity affected soils by leaching and their effect on soil properties and plant growth." Tikrit journal for agricultural sciences 22, no. 1 (March 31, 2022): 149–68. http://dx.doi.org/10.25130/tjas.22.1.14.

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The irrigated soils in dry and semi-arid areas suffer from the problem of salt accumulation because of not using sufficient leaching water to remove the salts added with the irrigation water. Soil salinity contributes to a decrease in the growth and productivity of plants grown in those conditions, as well as affecting the physical, chemical and hydraulic properties of the soil. The reclamation process is a radical solution to the problem of salinization, and one of the most important basic ingredients for the success of the process of reclamation of saline soils is to determine the optimal am

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Elizarov, N. V., T. G. Lomova, M. T. Ustinov, and V. V. Popov. "EFFECT OF AGROBIOLOGICAL MELIORATION ON THE SALT PROFILE OF ALKALI SOIL IN EASTERN BARABA DISTRICT." Bulletin of NSAU (Novosibirsk State Agrarian University), no. 1 (March 27, 2019): 18–25. http://dx.doi.org/10.31677/2072-6724-2019-50-1-18-25.

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The solonetz soil cover 21.7 % of Novosibirsk Region, or 3 686.2 thousand hectares. In the Barabinsk lowland and northern Kulunda, solonetz soil is seen as agricultural land, as it doesn’t make solid massifs, but occur as small spots among zonal soils (black soils, meadow-black soils and black earth-meadow soils). Regardless the vast area, solonetz soils fulfil 20 - 25 % only of the needs of the livestock industry, which is caused by low productivity in the natural state (1.0 - 3.0 c/ha of dry matter in the steppe and 3.0 - 5.0 c/ha in the forest steppe). The authors outline the necessity to i

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Endo, Tsuneyoshi, Sadahiro Yamamoto, Juan A. Larrinaga, Hideyasu Fujiyama, and Toshimasa Honna. "Status and Causes of Soil Salinization of Irrigated Agricultural Lands in Southern Baja California, Mexico." Applied and Environmental Soil Science 2011 (2011): 1–12. http://dx.doi.org/10.1155/2011/873625.

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Selected farmlands in southern Baja California, Mexico, were surveyed to determine the levels and the causes of salinization/sodication in irrigated agricultural soil. The salt dynamics observed in profiles differed from farm to farm. Low EC and high pH levels were observed in the profiles of sandy fields, because the salt composition of these soils can easily change when salts are leached by irrigation water that contains carbonates of sodium. On the other hand, high levels of salinity and sodicity were observed in the soils of clayey fields. Soil salinization/sodication is complexly interrel

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Schuerger, Andrew C., Rebecca L. Mickol, and Petra Schwendner. "The Hypopiezotolerant Bacterium, Serratia liquefaciens, Failed to Grow in Mars Analog Soils under Simulated Martian Conditions at 7 hPa." Life 10, no. 6 (May 26, 2020): 77. http://dx.doi.org/10.3390/life10060077.

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The search for life on Mars is predicated on the idea that Earth and Mars life (if present) should be both carbon- and water-based with similar forms of evolution. However, the astrobiology community can currently only investigate plausible Martian microbial ecosystems by using Terran life-forms as proxies. In order to examine how life might persist on Mars, we used a hypopiezotolerant bacterium (def., able to grow at 7–10 hPa)—Serratia liquefaciens—in growth assays with four Mars analog soils conducted under a subset of simulated Martian conditions including 7 hPa, 0 °C, and a CO2-enriched an

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MILLER, J. J., D. F. ACTON, and R. J. ST. ARNAUD. "THE EFFECT OF GROUNDWATER ON SOIL FORMATION IN A MORAINAL LANDSCAPE IN SASKATCHEWAN." Canadian Journal of Soil Science 65, no. 2 (May 1, 1985): 293–307. http://dx.doi.org/10.4141/cjss85-033.

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The results of this study indicate the importance of groundwater flow and water table depth on the genesis, characteristics and distribution of soils within a hummocky morainal landscape. Non-saline and non-carbonated soils in upland depressions can be attributed to "depression-focused" recharge by snowmelt and snowmelt runoff in the spring, as evidenced by deep sola and/or eluvial horizons. Non-saline and carbonated soils on lower slopes adjacent to depressions are associated with local discharge and/or lateral flow from the adjacent groundwater mounds under the depressions in spring, as well

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Rakhimgaliyeva, Saule, Sonja Tošić, Frank Eulenstein, Uwe Schindler, and Elmira Saljnikov. "How withdrawing arable land affected the productive capacity of Haplic Kastanozems after 19 years of fallowing in dry steppes of the Ural piedmont." Zemljiste i biljka 70, no. 2 (2021): 10–32. http://dx.doi.org/10.5937/zembilj2102010r.

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The fertile arable lands in the dry steppe zone of the Ural piedmont, which were intensively used for cereal production for 30 years of the last century, have been withdrawn from cultivation and abandoned for the last 20 years. The Republic of Kazakhstan's new strategy to restore the productivity of natural pasture presents a challenge to scientists when it comes to restoring the natural soil properties to the natural pastoral conditions of the dark chestnut soils studied (Haplic Kastanozems). This chapter presents the results of a project devoted to investigating the changes in the soil's phy

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Rengasamy, P., and KA Olsson. "Sodicity and soil structure." Soil Research 29, no. 6 (1991): 935. http://dx.doi.org/10.1071/sr9910935.

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Sodic soils are widespread in Australia reflecting the predominance of sodium chloride in groundwaters and soil solutions. Sodic soils are subject to severe structural degradation and restrict plant performance through poor soil-water and soil-air relations. Sodicity is shown to be a latent problem in saline-sodic soils where deleterious effects are evident only after leaching profiles free of salts. A classification of sodic soils based on sodium adsorption ratio, pH and electrolyte conductivity is outlined. Current understanding of the processes and the component mechanisms of sodic soil beh

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Nanba, K., and Gary M. King. "Response of Atmospheric Methane Consumption by Maine Forest Soils to Exogenous Aluminum Salts." Applied and Environmental Microbiology 66, no. 9 (September 1, 2000): 3674–79. http://dx.doi.org/10.1128/aem.66.9.3674-3679.2000.

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ABSTRACT Atmospheric methane consumption by Maine forest soils was inhibited by additions of environmentally relevant levels of aluminum. Aluminum chloride was more inhibitory than nitrate or sulfate salts, but its effect was comparable to that of a chelated form of aluminum. Inhibition could be explained in part by the lower soil pH values which resulted from aluminum addition. However, significantly greater inhibition by aluminum than by mineral acids at equivalent soil pH values indicated that inhibition also resulted from direct effects of aluminum per se. The extent of inhibition by exoge

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Macdonald, BCT, and MD Melville. "A comparison of the soils from two areas of sorted step chenopod patterned ground, at Fowlers Gap Field Station, Western New South Wales." Rangeland Journal 22, no. 1 (2000): 72. http://dx.doi.org/10.1071/rj0000072.

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Sorted step patterned ground at Fowlers Gap Field Station occurs within a variety of different Landsystem Units. Areas of sorted step patterned ground from Nuntherungie and Gap Hills Landsystems were selected and the soil properties compared. Soils from areas of sorted step patterned ground are composed of bare saline soils which surround the less saline vegetated soils. Despite occurring within different Landsystems, the suite of soil chemical properties (EC, soluble cations, and pH) between the bare and vegetated area within the patterned ground were statistically the same in most cases. Dif

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Pekeč, Saša, Marina Milović, and Velisav Karaklić. "Properties and groundwater level of humogley soil of southern Bačka." Zemljiste i biljka 70, no. 1 (2021): 60–67. http://dx.doi.org/10.5937/zembilj2101060p.

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The paper examines hydromorphic soils from the class of gley soils, soil type humogley. The examined soils are located in the protected part of the inundation of the middle course of the Danube. According to the chemical properties of the examined soils, the pH value ranges from 7,64 to 8,15 on average, and with depth there is an increase in alkalinity. The total salts of the examined soils had increased values in the humus horizon and ranged from 0,06 to 0,09%. The texture classes of the humus horizon of these soils are: clay loam to sandy clay loam, while the lower sub-horizons of the gley a

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Belovolova, Alla, Natal’ya Gromova, Alexander Esaulko, Evgeniy Golosnoy, and Ylia Grechishkina. "Influence of saline soils and mineral fertilizers on the germination and formation of sunflower seeds." E3S Web of Conferences 164 (2020): 06016. http://dx.doi.org/10.1051/e3sconf/202016406016.

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The research was carried out with the aid of vegetation experiments and on saline soils in production crops of the Stavropol territory farms (Andropovsky, Mineralovodsky and Kochubeyevsky districts). The goal of the research was to identify patterns of germination and formation of sunflower seeds, depending on the influence of saline soils and the use of mineral fertilizers. It was found that sunflower seeds germinate at fairly high concentrations of soil salts. In vegetation experiments, where saline soil containing 1.14% and 1.71% of chloride- sulfate salts was used, the number of sprouted s

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Miller, J. J., and J. A. Brierley. "Solonetzic soils of Canada: Genesis, distribution, and classification." Canadian Journal of Soil Science 91, no. 5 (October 2011): 889–902. http://dx.doi.org/10.4141/cjss10040.

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Miller, J. J. and Brierley, J. A. 2011. Solonetzic soils of Canada: Genesis, distribution, and classification. Can. J. Soil Sci. 91: 889–902. Soils of the Solonetzic order are defined as having a Solonetzic B horizon designated as a Bn or Bnt horizon. The Solonetzic Order includes four great groups: Solonetz, Solodized Solonetz, Solod, and Vertic Solonetz. Solonetzic soils are thought to develop via the stepwise pedogenic processes of salinization, solonization (desalinzation and alkalization), and solodization. Soluble salts are brought into the soil pedon of Solonetzic soils by capillary mov

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Naveed, Muhammad, Muhammad Kamran Aslam, Zulfiqar Ahmad, Tasawar Abbas, Asma A. Al-Huqail, Manzer H. Siddiqui, Hayssam M. Ali, Irfan Ashraf, and Adnan Mustafa. "Growth Responses, Physiological Alterations and Alleviation of Salinity Stress in Sunflower (Helianthus annuus L.) Amended with Gypsum and Composted Cow Dung." Sustainability 13, no. 12 (June 16, 2021): 6792. http://dx.doi.org/10.3390/su13126792.

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Salt accumulation in soils poses severe challenges for crop production in arid and semi-arid regions. Scarcity of rainfall and a high evaporation rate in these regions are considered major reasons for salt accumulation. It drastically reduces the leaching of excessive salts below the root zone of crops. The toxic effects of salts on plants can be greatly reduced with the use of biological and inorganic amendments. The present study was conducted to investigate the positive influence of gypsum (GP), composted cow dung (CCD) and the combined use of gypsum and composted cow dung (GP+CCD) on the g

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KASYANOV, A. E., and ISMAIL KHEBA ISMAIL KHEBA. "INSTALLATION FOR PHYSICAL MODELING OF SALINE SOILS WASHING." Prirodoobustrojstvo, no. 2 (2021): 31–35. http://dx.doi.org/10.26897/1997-6011-2021-2-31-35.

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Gradients of salts concentrations of the soil solution, rinsing water pressures, filtration coefficients determine the flow intensity of the salt solutions in the aeration zone. There are known a lot of software for calculating the motion of salt solutions in the porous medium. To assess the accuracy of calculations of the salts movement in the soil, the data of gradient measurements are used. The implementation of the known methods of physical modeling on the soil monoliths mounted according to Astapov, lysimetric installations, in experimental leaching of saline soils in the field requires s

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Mohiuddin, Muhammad, Muhammad Irshad, Sadaf Sher, Faisal Hayat, Ammar Ashraf, Salman Masood, Sumera Bibi, Jawad Ali, and Muhammad Waseem. "Relationship of Selected Soil Properties with the Micronutrients in Salt-Affected Soils." Land 11, no. 6 (June 4, 2022): 845. http://dx.doi.org/10.3390/land11060845.

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The present study aimed to assess the relationship of soil properties in salt-affected soils. The soil samples were collected from 14 districts of Pakistan. Soil salinity and sodicity are the common features of the arid and semiarid regions. The effects of the salt’s interactions with soil micronutrients have not been well studied. Therefore, saline and non-saline soil samples were collected from different locations. The microelements (Fe, Cu, Mn, and Zn) were fractionated into water-soluble, exchangeable, carbonate, Fe + Mn oxide, organic, and residual fractions. Univariate and multivariate a

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Герасимов, А. О., М. В. Чугунова та Ю. М. Поляк. "СЕЗОННЫЕ ИЗМЕНЕНИЯ СОДЕРЖАНИЯ ПРОТИВОГОЛОЛЕДНЫХ СРЕДСТВ В ДЕРНОВО-ПОДЗОЛИСТОЙ ПОЧВЕ В ЛАБОРАТОРНОМ И ПОЛЕВОМ ЭКСПЕРИМЕНТАХ". Biosfera 11, № 4 (12 лютого 2020): 1. http://dx.doi.org/10.24855/biosfera.v11i4.512.

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De-icing preparations (DIP) used in winter to prevent ice and snow deposits in cities are one of the most harmful anthropogenic factors. Numerous investigations on this topic are dedicated to the environmental impact of technical sodium chloride, whereas less attention is paid to new-generation reagents. The present paper reports the results of laboratory and field studies of nine DIPs used in Saint Petersburg, including chlorides and newer preparations of acetates and formates. The laboratory experiments showed that high doses of chloride reagents can increase salt content in soils to levels

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Tu, S., G. J. Racz, and C. M. Cho. "Extraction of Manganese from Soils with Potassium Salts." Soil Science Society of America Journal 59, no. 5 (September 1995): 1280–88. http://dx.doi.org/10.2136/sssaj1995.03615995005900050011x.

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Nedriga, V. P., and �. A. Dem'yanova. "Construction of dams on soils containing soluble salts." Hydrotechnical Construction 20, no. 2 (February 1986): 116–21. http://dx.doi.org/10.1007/bf01427164.

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