Auswahl der wissenschaftlichen Literatur zum Thema „Sols carbonatés“
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Zeitschriftenartikel zum Thema "Sols carbonatés"
Timbal, J., und J. Gelpe. „Croissance juvénile du chêne rouge sur des sols carbonatés à des profondeurs variables“. Annales des Sciences Forestières 46, Supplement (1989): 694s—696s. http://dx.doi.org/10.1051/forest:198905art0153.
Der volle Inhalt der QuelleDupla, Jean-Claude, Elisabeth Palix, Guillaume Damblans, Alain Puech, Mathieu Blanc, Christophe Dano, Hussein Mroueh et al. „Le projet ANR SOLCYP+ pour améliorer le dimensionnement des monopieux utilisés comme fondations d’éoliennes marines“. Revue Française de Géotechnique, Nr. 158 (2019): 4. http://dx.doi.org/10.1051/geotech/2019010.
Der volle Inhalt der QuelleEl Howayek, Alain, Antonio Bobet und Marika Santagata. „Microstructure and cementation of two carbonatic fine-grained soils“. Canadian Geotechnical Journal 56, Nr. 3 (März 2019): 320–34. http://dx.doi.org/10.1139/cgj-2018-0059.
Der volle Inhalt der QuelleWang, Dunling, und Darwin W. Anderson. „Pedogenic carbonate in Chernozemic soils and landscapes of southeastern Saskatchewan“. Canadian Journal of Soil Science 80, Nr. 2 (01.05.2000): 251–61. http://dx.doi.org/10.4141/s99-063.
Der volle Inhalt der QuelleMILLER, J. J., D. F. ACTON und R. J. ST. ARNAUD. „THE EFFECT OF GROUNDWATER ON SOIL FORMATION IN A MORAINAL LANDSCAPE IN SASKATCHEWAN“. Canadian Journal of Soil Science 65, Nr. 2 (01.05.1985): 293–307. http://dx.doi.org/10.4141/cjss85-033.
Der volle Inhalt der QuelleKassim, Jabbar K. „Method for Estimation of Calcium Carbonate in Soils from Iraq“. International Journal of Environment 1, Nr. 1 (30.08.2013): 9–19. http://dx.doi.org/10.3126/ije.v1i1.8524.
Der volle Inhalt der QuelleSouza, Renato Ferreira de, Valdemar Faquin, Ruy Carvalho, Paulo Rogério Ferreira Torres und Adélia Aziz Alexandre Pozza. „Atributos químicos de solos influenciados pela substituição do carbonato por silicato de cálcio“. Revista Brasileira de Ciência do Solo 32, Nr. 4 (August 2008): 1563–72. http://dx.doi.org/10.1590/s0100-06832008000400020.
Der volle Inhalt der QuelleJarnuszewski, Grzegorz. „Some physical properties of mursh developed on limnic limestones in NW Poland“. Soil Science Annual 68, Nr. 3 (01.09.2017): 132–39. http://dx.doi.org/10.1515/ssa-2017-0016.
Der volle Inhalt der QuelleGarcía-Montero, L. G., I. Valverde-Asenjo, P. Díaz und C. Pascual. „Statistical patterns of carbonates and total organic carbon on soils of Tuber rufum and T. melanosporum (black truffle) brûlés“. Soil Research 47, Nr. 2 (2009): 206. http://dx.doi.org/10.1071/sr08084.
Der volle Inhalt der QuelleGordienko, O. A., und E. A. Ivantsova. „Morphological features of the soil cover of slope lands in the south of the Volga uplands within the urban landscapes of Volgograd“. Dokuchaev Soil Bulletin, Nr. 106 (27.03.2021): 77–104. http://dx.doi.org/10.19047/0136-1694-2021-106-77-104.
Der volle Inhalt der QuelleDissertationen zum Thema "Sols carbonatés"
Metzger, Laure. „Comportement du rimsulfuron dans deux sols carbonatés“. Nancy 1, 1997. http://www.theses.fr/1997NAN10302.
Der volle Inhalt der QuelleThe fate of rimsulfuron, a sulfonylurea herbicide, was studied in a rendzina and an alluvial soil, through (i) laboratory soil incubations and (fi) batch experiments to de termine the capacity and the dynamics of rimsulfuron adsorption. The application of rimsulfuron, at 4-5 times the recommended field doses, did not modify the soil microbial activity, measured by the soil respiration. The mineralization of rimsulfuron occured only in the presence of an active microflora and was very low: 2 and 0. 75 % of the applied radioactivity for the alluvial soil and the rendzina soil, respectively. The lower rimsulfuron mineralization observed in the rendzina could be explained by high amounts of organic matter that (i) constituted an alternative source of organic carbon for the microflora, and (ii) might increase the adsorption of rimsulfuron residues, thus reducing their availability for mineralization processes. Lndeed, adsorption studies showed not only that the specific surface area influenced the rimsulfuron adsorption, but also that higher clay contents seemed to enhance the adsorption dynamics and that organic matter seemed to increase the adsorption capacity. Besides, non extractable residues (NER) of rimsulfuron were more concentrated in the grain-size fractions having the higher organic matter contents and a non negligible proportion of these NER has been co-extracted with alcalino-soluble organic compounds. However, 65 to 80 % of rimsulfuron residues were still extractable, even after 3 to 7 months. This potential mobility of rimsulfuron residues was confirmed by the Kd values obtained from the adsorption experiments, ranging from 0. 12 to 1. 7. Thus rimsulfuron residues can accumulate in soil and be available for migration or for absorption by plants. The processes influencing the behavior of rimsulfuron in soil are similar to those affecting the evolution of natural organic matter but the relative importance of these processes and their kinetics are different
Achour, Yosra. „Etude de la mobilité des métaux (Pb, Zn, Cd) et des métalloïdes (As, Sb) dans les sols carbonatés contaminés par les rejets miniers“. Electronic Thesis or Diss., Orléans, 2022. https://theses.univ-orleans.fr/prive/accesESR/2022ORLE1041_va.pdf.
Der volle Inhalt der QuelleThis thesis provides answers on the ecodynamics and phytoavailability of potentially toxic elements (PTE) in agricultural soils heavily contaminated by mining waste developed on a carbonated bedrock of northern Tunisia (Jebel Ressas (JRS), Jebel Hallouf (JH1) and Sidi Bouaoune (SB) in a semi-arid climate.The main contaminants in question are Zn, Pb, Cd, As and Sb which can respectively reach 185037 mg.kg-1 at JRS, 28,000 mg.kg-1 at (JH1), 1021 mg.kg-1 at JRS, 1,355 mg.kg-1 and 338 mg.kg-1 at (JH1).These soils are essentially made up of clays (kaolinite, illite, and montmorillonite), carbonates (calcite, dolomite, and hydrozincite), silicates (quartz and hemimorphite), and sulfates (barite and anglesite).The rhizospheric effect on the mobility of PTE has been investigated using kinetic test with a mixture of low molecular weight organic acids. The results showed an increase in the pH of the solution (initial pH 2.8) up to near neutrality, leading to the dissolution of carbonates. Our results suggest that the most extractable elements are Cd and Zn and to a lesser extent Pb. an extraction percentage not exceeding 1% for Sb and 0.1% for As, respectively, was observed. for metalloids (As and Sb) their extractibility was relatively low with the exception of the soils of Jebel Hallouf and Sidi Bouaouane, with an extraction percentage not exceeding 1% for Sb and 0.1% for As, respectively.For the determination of the forms of the PTE in soils, two methods of sequential extractions were applied (BCR and Maiz). Jointly, the total dissolved concentration in pore waters, the labile fraction (DGT probes) and the absorption by plants (barley and peas) were measured in order to study the speciation, mobility and phytoavailability of two sites post-mining (Jebel Hallouf - Sidi Bouaouane and Jebel Ressas).Our résultats showed that the PTE in the mobile and mobilisable fraction(Maiz scheme) of the soils are low compared to their total concentrations. The BCR scheme revealed that most of the PTE are bound to the residual fraction with the exception of Zn at JRS which is much more concentrated in the exchangeable fraction. An exception was also observed for Pb in JH(1) and JH(2) soils where it was distributed evenly in the exchangeable, oxidizable and residual fractions, the percentage of which varies between 23 % and 32 %.The response of plants to these contaminants shows that peas and barley have accumulated TPE levels exceeding the levels absorbed by plants in control soils.Total dissolved concentrations soil power water as well as concentrations measured by DGT are not correlated with primary plant leaf content. This result is explained by the fact that the concentrations of PTE accumulated in the plants are higher than those available in the power waters and that the replenishment of the solid phase is practically negligible.The risk of transfer of PTE to water was studied by percolation in saturated conditions in soil columns reproducing the surface profile. A progressive decrease in the redox potential related to the concentration of organic carbon in the soil induced an increase in the mobility of arsenic probably related to the microbial reduction of iron oxides
Santerre, Yannick. „Influence de la diagenèse précoce et de la dynamique sédimentaire sur la distribution des propriétés pétrophysiques dans les réservoirs carbonatés“. Aix-Marseille 1, 2010. http://www.theses.fr/2010AIX11042.
Der volle Inhalt der QuelleDeville, de Periere Matthieu. „Origine sédimento-diagénétique de réservoirs carbonatés microporeux : exemple de la formation Mishrif (Cénomanien) du Moyen-Orient“. Thesis, Dijon, 2011. http://www.theses.fr/2011DIJOS107/document.
Der volle Inhalt der QuelleMicroporosity may account for as much as 95% of the total porosity of hydrocarbon and water reservoirs in Cretaceous limestones of the Arabian Gulf. In these microporous facies porosity is moderate to excellent (up to 35%) while permeability is poor to moderate (up to 190mD). Conversely, microporous facies may form dense inter-reservoir or cap rock layers with very low porosity and permeability values (2–8% and 0.01–2mD, respectively). For this study, samples were mainly collected from the Cenomanian Mishrif Formation, but also from the Berriasian-Valanginian Habshan Formation, so as to examine the wide vertical and lateral discrepancies in their petrophysical parameters. Scanning Electron Microscopy was used to investigate two potential controls of reservoir properties: (1) micrite particle morphology (shape and inter-crystal contacts); and (2) micrite crystallometry, defined as the median size of micrite particles measured on SEM photomicrographs. The morphometric data are compared with three petrophysical parameters (porosity, permeability and pore threshold radius distribution). Results reveal that micrite matrixes can be subdivided into three petrophysical classes each with its own distinctive crystallometry, morphology and reservoir properties. Class C (strictly microporous limestones with coarse punctic-to-partially coalescent micrites) is made up of coarse (>2µm) polyhedral to rounded micritic crystals, it has good to excellent porosity (8–28%), poor to moderate permeability (0.2–190mD) and a mean pore threshold radius of more than 0.5µm. The class C is usually observed in rudist-rich bioclastic shoal facies where several sedimentary factors (hydrodynamism, bioproduction …) would disfavour deposition of the finer micritic crystals. Diagenetic study shows that the development of coarse micrites (Class C) must also be explained by the early dissolution of fine aragonite and high magnesium calcite particles in oxygenated meteoric fluids leading to a simultaneous in-situ overgrowth on LMC particles at the top of the meteoric phreatic lens. These processes induce an increase of the crystallometry of micritic particles, an early lithification of the carbonate mud, and so the mineralogical stabilization of coarse Class C micrites. Class F (strictly microporous limestones with fine punctic-to-partially coalescent micrites) is composed of fine (<2µm) polyhedral to rounded micrites with poor to excellent porosity (3–35%), but permeability values of less than 10mD and a mean pore threshold radius of less than 0.5µm. It is mostly observed in sediments deposited in a low energy muddy inner platform setting. The formation of fine micrites (Class F) is also explained by an early mineralogical stabilization of micritic particles in confined meteoric waters, favoring neomorphism processes, which may proceeds during burial. Later, during burial, reservoir properties of classes C and D strictly microporous samples where locally enhanced by mesogenetic dissolution (probably due to organic acids) affecting the microporous matrix during the oil emplacement. Class D (strictly microporous mud-dominated facies with compact anhedral to fused dense micrites) comprises subhedral to anhedral crystals with sutured to fused contacts forming a dense matrix. It has very low porosity and permeability. Class D is only found in low energy muddy inner platform facies and forms inter-reservoir or caps rock layers usually in association with stylolites and clay contents that exceed 10%. Regardless of how they formed, though, the three classes can be usefully incorporated into future rock-typing of the microporous carbonate reservoirs of the Middle East
Hanich, Lahoucine. „Les traçages d'essai en aquifère hétérogène : méthodes, intérêt et limites : application au milieu alluvionnaire languedocien et comparaison avec les milieux carbonatés et fissurés du nord de la france“. Lille 1, 1991. http://www.theses.fr/1991LIL10157.
Der volle Inhalt der QuelleBruna, Pierre-olivier. „Evolution des propriétés réservoir des carbonates peu poreux : exemple des calcaires du Crétacé Inférieur de la Moyenne Durance“. Thesis, Aix-Marseille, 2013. http://www.theses.fr/2013AIXM4745.
Der volle Inhalt der QuelleHemipelagic limestones from the South-East of France are characterized by low values of porosity and permeability that allow considering these rocks as potential analogs to unconventional oil and gas reservoirs or fissured aquifers. These reservoirs are of primary importance in today’s economical context where the energy and the water’s demands grow with the increase in the world population. Nevertheless, the industrial exploitation of such reservoirs faces series of environmental risks and technical challenges that require to be managed in order to reduce their footprint on the environment.This work brought a significant amount of new data on unconventional carbonate reservoirs. It highlights how important compaction features (stylolites, microstylolites, solution seams) may be to fluids storage in such reservoirs. It shows that the diagenetic evolution of hemipelagic carbonate sediments depends on both early processes (sorting, early cementation, differential compaction) and eventual late reactivations (under tectonic stress inversion for example). Coupling three-dimensional modeling with geostatistics appear as an accurate and fast protocol to identify key elements (facies, fractures and stylolite) that play a role in the petrophysical heterogeneity of such unconventional reservoirs. This method also allows identifying equiprobable models of fractures geobodies and investigating the distribution of flow preferential pathways
El, Mansour Nadia. „Caractérisation physico-chimique de la carbonatation minérale des résidus miniers ultramafiques de la région de Thetford Mines, Québec“. Master's thesis, Université Laval, 2019. http://hdl.handle.net/20.500.11794/33851.
Der volle Inhalt der QuelleNourtier-Mazauric, Elise. „Modélisation géochimique et numérique des interactions entre des solutions solides et une solution aqueuse. Extension du logiciel de réaction-transport Archimède et application à la diagénèse minérale des réservoirs“. Phd thesis, Ecole Nationale Supérieure des Mines de Saint-Etienne, 2003. http://tel.archives-ouvertes.fr/tel-00088991.
Der volle Inhalt der QuelleCe modèle a été intégré au logiciel de transport réactif en milieu poreux ARCHIMEDE, puis appliqué à divers exemples. Dans le cas de solutions solides binaires, une méthode graphique a permis de déterminer les compositions des solutions solides qui précipitent, à l'aide des potentiels chimiques des pôles.
Le logiciel ainsi obtenu pourrait être utilisé pour modéliser notamment la diagenèse des réservoirs pétroliers argileux ou carbonatés, ou la dispersion de polluants dans le sol.
Junior, Jairo Calderari de Oliveira. „Processos pedogenéticos atuais e pretéritos em solos alcalino-sódicos do Pantanal Norte“. Universidade de São Paulo, 2014. http://www.teses.usp.br/teses/disponiveis/11/11140/tde-15042015-153823/.
Der volle Inhalt der QuelleSodic soils are commonly associated to semi-arid climates, closed drainage systems (endorheic) and evaporative environments. In Brazilian Pantanal, knowns as the largest continental flooded area in the earth, sodic soils have significant expression in terms of area and environmental functionality, the specificity on plants development and soil intentional consumption (geophagy) by several animals, also playing as a refuge along the flooding events. These soils are located in the higher ground of the landscape (paleodiques), different from common situation. Pedogenic processes on north Pantanal sodic soils were studied in the Private Natural Heritage Reserve (PRNP) SESC Pantanal, in Barão do Melgaço-MT, performed on \"paleodiques\" from five sectors at different dissection stages. Pedogenic process was studied by means of morphologic descriptions was done in various scales, 14C dating on carbonate precipitates and optically stimulated luminescence (OSL) in sediments, geochemical and mineralogical modeling, spatial analysis of chemical and physical properties of the soil, apparent soil electrical conductivity performed by sensor electromagnetic (EM-38) and multivariate statistics. Soil profile from more conserved sectors shows typical features of lentic sedimentation environment, calcium carbonate layer and diatoms occurrence, suggesting that the formation of these features occurred by water concentration. Current condition is the opposite from earlier, wherein the flood plains remained isolated, with limited lateral and vertical drainage promoting water loss by evaporation and therefore concentrating the ions in solution. Simulation of the evaporation of water from São Lourenço and Cuiabá rivers points out similar results, suggesting that water evaporation from both could result in calcite precipitation and Na+ saturation in exchange complex. However, the features observed in both, field morphology and thin sections suggested that sodic soils are currently in degradation. The argilluviation is very intense and stands out as the main transformation process of these soils, occurring from the most preserved even in the most advanced dissection stage of. The ferrolysis is evident in the most advanced stage processing at E and Bt transition, where it establishes a cavity porosity depletion by both mechanical and chemical. Carbonates associated with channels, old pores and channels, without a cortex, suggests the current conditions do not favor sodic soil formation. Mineralogical analyzes indicates smectite presence in the paleodique of the most preserved sector, while present conditions promotes a smectite-kaolinite interestratification. Current hydrology promotes the gradual erosion of paleodiques that previously isolated the lakes from each other, becoming a slight open drainage system. The principal component analysis (PCA) identified the redox process as major process in the study area and, along the flood events, are primarily responsible for soil transformations. Pathway of sodic soil transformation in the RPPN SESC Pantanal paleodiques was Typic Natrudalf-Glossic Natraqualf. The latter are very susceptible to erosion process, promoted by flooding and tend to disappear, narrowing the paleodique progressively. Erosion process results in smalls and circulars elevations, named mounds, with high levels of Na+.
Al, Qabany Ahmed Abdul Aziz. „Microbial carbonate precipitation in soils“. Thesis, University of Cambridge, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.609845.
Der volle Inhalt der QuelleBücher zum Thema "Sols carbonatés"
P, Le Tirant, und Nauroy Jean-François, Hrsg. Foundations in carbonate soils. Paris: Editions Technip, 1994.
Den vollen Inhalt der Quelle findenR, Lal, Hrsg. Global climate change and pedogenic carbonates. Boca Raton, Fla: Lewis, 2000.
Den vollen Inhalt der Quelle findenGeological Survey (U.S.), Hrsg. The distribution of calcium carbonate in soils: A computer simulation using program CALSOIL. [Denver, Colo.]: U.S. Dept. of the Interior, Geological Survey, 1986.
Den vollen Inhalt der Quelle findenGeological Survey (U.S.), Hrsg. The distribution of calcium carbonate in soils: A computer simulation using program CALSOIL. [Denver, Colo.]: U.S. Dept. of the Interior, Geological Survey, 1986.
Den vollen Inhalt der Quelle findenKamilov, O. K. Genezis i svoĭstva okarbonachenno-zagipsovannykh pochv T͡S︡entralʹnoĭ Fergany. Tashkent: Izd-vo "Fan" Akademii nauk Respubliki Uzbekistan, 1992.
Den vollen Inhalt der Quelle findenNettleton, W. D., Hrsg. Occurrence, Characteristics, and Genesis of Carbonate, Gypsum, and Silica Accumulations in Soils. Madison, WI, USA: Soil Science Society of America, 1991. http://dx.doi.org/10.2136/sssaspecpub26.
Der volle Inhalt der QuelleD, Nettleton W., und Soil Science Society of America. Division S-5., Hrsg. Occurrence, characteristics, and genesis of carbonate, gypsum, and silica accumulations in soils. Madison, Wis., USA: Soil Science Society of America, 1991.
Den vollen Inhalt der Quelle findenG, Tindle A., und Webb P. C, Hrsg. Geochemical reference material compositions: Rocks, minerals, sediments, soils, carbonates, refractories & ores used in research & industry. Latheronwheel, Caithness, U.K: Whittles Pub., 1992.
Den vollen Inhalt der Quelle findenEl-Gobbi, Mahgub Omar. The effect of organic matter in corporation on the behaviour of calcareous growing media. Dublin: University College Dublin, 1997.
Den vollen Inhalt der Quelle findenCanada, Geological Association of, Canadian Geological Foundation, Devon Energy Corporation, University of Saskatchewan und Geological Association of Canada. Meeting, Hrsg. Dynamics of epeiric seas. [St. John's, Nfld.]: Geological Association of Canada, 2008.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Sols carbonatés"
Lutenegger, Alan J. „Carbonate Content“. In Laboratory Manual for Geotechnical Characterization of Fine-Grained Soils, 71–84. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9781003263289-7.
Der volle Inhalt der QuelleCoop, M. R., und J. D. McAuley. „Shaft Friction of Piles in Carbonate Soils“. In Advances in Underwater Technology, Ocean Science and Offshore Engineering, 645–59. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-017-2473-9_30.
Der volle Inhalt der QuelleHallmark, C. T. „Family Mineralogy of Soils with Free Carbonates and Gypsum“. In SSSA Special Publications, 53–60. Madison, WI, USA: Soil Science Society of America and American Society of Agronomy, 2015. http://dx.doi.org/10.2136/sssaspecpub16.c4.
Der volle Inhalt der QuelleWhittig, L. D., und P. Janitzky. „Mechanisms of Formation of Sodium Carbonate in Soils“. In Selected Papers in Soil Formation and Classification, 367–78. Madison, Wisconsin, USA: Soil Science Society of America, Inc., 2015. http://dx.doi.org/10.2136/sssaspecpub1.c30.
Der volle Inhalt der QuelleVirto, Iñigo, Isabel de Soto, Rodrigo Antón und Rosa M. Poch. „Management of carbonate-rich soils and trade-offs with soil inorganic carbon cycling“. In Understanding and fostering soil carbon sequestration, 707–36. Burleigh Dodds Science Publishing, 2022. http://dx.doi.org/10.19103/as.2022.0106.22.
Der volle Inhalt der QuelleSposito, Garrison. „Soil Salinity“. In The Chemistry of Soils. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780190630881.003.0016.
Der volle Inhalt der QuelleAitken, R. A., und K. M. Aitken. „With Carbonates“. In Nitro, Nitroso, Azo, Azoxy, and Diazonium Compounds, Azides, Triazenes, and Tetrazenes, 1. Georg Thieme Verlag KG, 2010. http://dx.doi.org/10.1055/sos-sd-041-00233.
Der volle Inhalt der QuelleBeignet, J. „Using Carbonates“. In Three Carbon-Heteroatom Bonds: Acid Halides; Carboxylic Acids and Acid Salts, 1. Georg Thieme Verlag KG, 2007. http://dx.doi.org/10.1055/sos-sd-020-01269.
Der volle Inhalt der QuelleStien, D. „From Carbonates“. In Three Carbon-Heteroatom Bonds: Esters and Lactones; Peroxy Acids and R(CO)OX Compounds; R(CO)X, X=S, Se, Te, 1. Georg Thieme Verlag KG, 2005. http://dx.doi.org/10.1055/sos-sd-021-00008.
Der volle Inhalt der QuelleMaltman, Alex. „How Minerals Work“. In Vineyards, Rocks, and Soils. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190863289.003.0007.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Sols carbonatés"
Skripnikov, P., und A. Nalivaichenko. „ACCUMULATION OF ORGANIC CARBON UNDER WOODY PLANT COMMUNITIES IN URBAN FORESTS OF ROSTOV-ON-DON“. In Reproduction, monitoring and protection of natural, natural-anthropogenic and anthropogenic landscapes. FSBE Institution of Higher Education Voronezh State University of Forestry and Technologies named after G.F. Morozov, 2022. http://dx.doi.org/10.34220/rmpnnaal2021_97-102.
Der volle Inhalt der QuelleThi, Bang Le, Hoang Quoc Khai, Bui Duc Long und S. Ramesh. „Fabrication of nanoparticle carbonated hydroxyapatite by phase transformation of calcium carbonate prepared by sol-gel hydrothermal method“. In 8TH BRUNEI INTERNATIONAL CONFERENCE ON ENGINEERING AND TECHNOLOGY 2021. AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0113867.
Der volle Inhalt der QuelleYadla, Nanda Kishore, Rama Mohan Gajulapalli, Kandasamy K. K und Faris Kamal. „Optimization of Jacket Structure in Carbonate Soils“. In The 7th World Congress on Civil, Structural, and Environmental Engineering. Avestia Publishing, 2022. http://dx.doi.org/10.11159/icgre22.210.
Der volle Inhalt der QuelleAvakyan, A. A. „ABOUT THE CRYSTALLIZATION OF STIBNITE FROM THE AQUEOUS SOLUTIONS OF HYDROGEN SULPHIDE AND ABOUT THE COMPOSITION OF THESE SOLUTIONS“. In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. ПЕРМСКИЙ ГОСУДАРСТВЕННЫЙ НАЦИОНАЛЬНЫЙ ИССЛЕДОВАТЕЛЬСКИЙ УНИВЕРСИТЕТ, 2022. http://dx.doi.org/10.17072/chirvinsky.2022.3.
Der volle Inhalt der QuelleBrandes, Horst G. „Permeability of Marine Sediments and Tropical Volcanic Soils“. In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-83543.
Der volle Inhalt der QuelleBeavers, J. A., und R. G. Worthingham. „The Influence of Soil Chemistry on SCC of Underground Pipelines“. In 2002 4th International Pipeline Conference. ASMEDC, 2002. http://dx.doi.org/10.1115/ipc2002-27146.
Der volle Inhalt der QuelleStupar, Vladanka, Markola Saulić, Milica Blažić, Zlata Živković, Darko Stojićević, Marko Stokić und Bojan Stević. „STATE OF SOIL FERTILITY IN THE AREA OF THE POŽAREVAC CITY“. In 1st International Symposium on Biotechnology. University of Kragujevac, Faculty of Agronomy, 2023. http://dx.doi.org/10.46793/sbt28.289s.
Der volle Inhalt der QuelleCao, Jianchun, Zhibin Zhong und Ashish Budhiraja. „Numerical Investigation on Suction Pile’s Holding Capacity Installed in Carbonate-Type Soils“. In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-18107.
Der volle Inhalt der QuelleBrunning, Paul, und Baidrul Ishak. „Improved Pile Driving Predictions in Carbonate Soils and Rock“. In Offshore Technology Conference. Offshore Technology Conference, 2012. http://dx.doi.org/10.4043/23232-ms.
Der volle Inhalt der QuelleLehane, Barry M., J. Antonio H. Carraro, Nathalie Boukpeti und Sarah Elkhatib. „Mechanical Response of Two Carbonate Sediments From Australia’s North West Shelf“. In ASME 2014 33rd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/omae2014-23340.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Sols carbonatés"
Francis, C. W., S. Y. Lee, J. H. Wilson, M. E. Timpson und M. P. Elless. The use of carbonate lixiviants to remove uranium from uranium-contaminated soils. Office of Scientific and Technical Information (OSTI), August 1997. http://dx.doi.org/10.2172/510339.
Der volle Inhalt der QuelleReeder, Richard J. Spectroscopic and Microscopic Characterization of Contaminant Uptake and Retention by Carbonates in Soils and Vadose Zone Sediments. Office of Scientific and Technical Information (OSTI), Juni 2001. http://dx.doi.org/10.2172/833624.
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