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  Subjects -> ENGINEERING (Total: 1957 journals)
    - CHEMICAL ENGINEERING (150 journals)
    - CIVIL ENGINEERING (146 journals)
    - ELECTRICAL ENGINEERING (84 journals)
    - ENGINEERING (1124 journals)
    - ENGINEERING MECHANICS AND MATERIALS (284 journals)
    - HYDRAULIC ENGINEERING (43 journals)
    - INDUSTRIAL ENGINEERING (53 journals)
    - MECHANICAL ENGINEERING (73 journals)

CHEMICAL ENGINEERING (150 journals)                  1 2     

ACS Combinatorial Science     Full-text available via subscription   (7 followers)
Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials     Hybrid Journal   (3 followers)
Acta Polymerica     Hybrid Journal   (4 followers)
Additives for Polymers     Full-text available via subscription   (17 followers)
Adhesion Adhesives & Sealants     Hybrid Journal   (3 followers)
Advanced Chemical Engineering Research     Open Access   (7 followers)
Advances in Applied Ceramics     Partially Free   (2 followers)
Advances in Chemical Engineering     Full-text available via subscription   (14 followers)
Advances in Chemical Engineering and Science     Open Access   (19 followers)
Advances in Polymer Technology     Hybrid Journal   (9 followers)
African Journal of Pure and Applied Chemistry     Open Access  
Annual Review of Analytical Chemistry     Full-text available via subscription   (8 followers)
Annual Review of Chemical and Biomolecular Engineering     Full-text available via subscription   (8 followers)
Anti-Corrosion Methods and Materials     Hybrid Journal   (3 followers)
Applied Petrochemical Research     Open Access   (3 followers)
Asia-Pacific Journal of Chemical Engineering     Hybrid Journal   (6 followers)
Biochemical Engineering Journal     Hybrid Journal   (8 followers)
Biomass Conversion and Biorefinery     Partially Free   (5 followers)
BMC Chemical Biology     Open Access   (4 followers)
Brazilian Journal of Chemical Engineering     Open Access   (2 followers)
Bulletin of the Chemical Society of Ethiopia     Open Access   (1 follower)
Carbohydrate Polymers     Hybrid Journal   (8 followers)
Catalysts     Open Access   (5 followers)
Chemical and Petroleum Engineering     Hybrid Journal   (7 followers)
Chemical and Process Engineering     Open Access   (3 followers)
Chemical and Process Engineering Research     Open Access   (5 followers)
Chemical Communications     Full-text available via subscription   (28 followers)
Chemical Engineering & Technology     Hybrid Journal   (24 followers)
Chemical Engineering and Processing: Process Intensification     Hybrid Journal   (9 followers)
Chemical Engineering and Science     Open Access   (2 followers)
Chemical Engineering Communications     Hybrid Journal   (10 followers)
Chemical Engineering Journal     Hybrid Journal   (16 followers)
Chemical Engineering Research and Design     Hybrid Journal   (15 followers)
Chemical Engineering Science     Hybrid Journal   (9 followers)
Chemical Geology     Hybrid Journal   (9 followers)
Chemical Papers     Hybrid Journal   (3 followers)
Chemical Product and Process Modeling     Full-text available via subscription   (3 followers)
Chemical Reviews     Full-text available via subscription   (184 followers)
Chemical Society Reviews     Full-text available via subscription   (26 followers)
Chemical Technology     Open Access   (4 followers)
ChemInform     Hybrid Journal   (3 followers)
Chemistry & Industry     Hybrid Journal   (2 followers)
Chemistry Central Journal     Open Access   (5 followers)
Chemistry of Materials     Full-text available via subscription   (134 followers)
Chemometrics and Intelligent Laboratory Systems     Hybrid Journal   (6 followers)
ChemSusChem     Hybrid Journal   (6 followers)
Chinese Chemical Letters     Full-text available via subscription   (1 follower)
Chinese Journal of Chemical Engineering     Full-text available via subscription   (3 followers)
Chinese Journal of Chemical Physics     Hybrid Journal   (1 follower)
Coke and Chemistry     Hybrid Journal  
Coloration Technology     Hybrid Journal   (1 follower)
Computational Biology and Chemistry     Hybrid Journal   (8 followers)
Computer Aided Chemical Engineering     Full-text available via subscription   (2 followers)
Computers & Chemical Engineering     Hybrid Journal   (6 followers)
Corrosion Engineering, Science and Technology     Hybrid Journal   (18 followers)
Corrosion Reviews     Full-text available via subscription   (4 followers)
Crystal Research and Technology     Hybrid Journal   (2 followers)
Current Opinion in Chemical Engineering     Open Access   (2 followers)
Education for Chemical Engineers     Hybrid Journal   (3 followers)
European Polymer Journal     Hybrid Journal   (41 followers)
Fibers and Polymers     Full-text available via subscription   (3 followers)
Focusing on Modern Food Industry     Open Access   (3 followers)
Frontiers of Chemical Science and Engineering     Hybrid Journal   (1 follower)
Geochemistry International     Hybrid Journal  
High Performance Polymers     Hybrid Journal  
Indian Chemical Engineer     Hybrid Journal   (3 followers)
Indian Journal of Chemical Technology (IJCT)     Open Access   (12 followers)
Industrial & Engineering Chemistry     Full-text available via subscription   (9 followers)
Industrial & Engineering Chemistry Research     Full-text available via subscription   (16 followers)
Industrial Chemistry Library     Full-text available via subscription   (4 followers)
International Journal of Chemical and Petroleum Sciences     Open Access   (1 follower)
International Journal of Chemical Engineering     Open Access   (6 followers)
International Journal of Chemical Reactor Engineering     Full-text available via subscription   (3 followers)
International Journal of Chemical Technology     Open Access   (3 followers)
International Journal of Chemoinformatics and Chemical Engineering     Full-text available via subscription   (2 followers)
International Journal of Food Science     Open Access   (2 followers)
International Journal of Industrial Chemistry     Open Access  
International Journal of Polymeric Materials     Hybrid Journal   (3 followers)
International Journal of Science and Engineering     Open Access   (7 followers)
International Journal of Waste Resources     Open Access   (3 followers)
ISRN Chemical Engineering     Open Access   (3 followers)
ISRN Polymer Science     Open Access   (10 followers)
Journal of Applied Crystallography     Hybrid Journal   (4 followers)
Journal of Applied Electrochemistry     Hybrid Journal   (6 followers)
Journal of Applied Polymer Science     Hybrid Journal   (120 followers)
Journal of Biomaterials Science, Polymer Edition     Hybrid Journal   (7 followers)
Journal of Chemical & Engineering Data     Full-text available via subscription   (6 followers)
Journal of Chemical Ecology     Hybrid Journal   (1 follower)
Journal of Chemical Engineering     Open Access   (3 followers)
Journal of Chemical Engineering and Materials Science     Open Access  
Journal of Chemical Science and Technology     Open Access   (1 follower)
Journal of Chemical Sciences     Partially Free   (13 followers)
Journal of Chemical Technology & Biotechnology     Hybrid Journal   (2 followers)
Journal of Chemical Theory and Computation     Full-text available via subscription   (8 followers)
Journal of Coatings     Open Access   (2 followers)
Journal of Crystallization Process and Technology     Open Access   (4 followers)
Journal of Food Measurement and Characterization     Hybrid Journal  
Journal of Fuel Chemistry and Technology     Full-text available via subscription   (5 followers)
Journal of Geochemical Exploration     Hybrid Journal  
Journal of Industrial and Engineering Chemistry     Hybrid Journal   (1 follower)

        1 2     

Geochemistry International    Follow    
  Hybrid Journal Hybrid journal (It can contain Open Access articles)
     ISSN (Print) 1556-1968 - ISSN (Online) 0016-7029
     Published by Springer-Verlag Homepage  [2187 journals]   [SJR: 0.401]   [H-I: 13]
  • Geochemistry, age, and petrogenesis of rocks from the Garevka metamorphic
           complex, Yenisey Ridge
    • Abstract: Abstract The mineralogical, petrological, geochemical and geochronological data on the Garevka metamorphic complex (GMC) of the Yenisey Ridge were used to evaluate the age, nature, and provenance of their protoliths. The evolution of the GMC occurred in two stages with different ages, thermodynamic regimes, and metamorphic field gradients. The final emplacement of granitoids was marked by high-pressure (HP) amphibolite facies regional metamorphism (970 Ma). At the second stage, these rocks experienced Late Riphean (900–870 Ma) retrograde epidote-amphibolite facies metamorphism accompanied by the formation of blastomylonitic complexes within narrow zones of brittle-ductile deformation. The metamorphism of migmatites (850 Ma) is coeval with the collisional medium-pressure metamorphism of the kyanite-sillimanite type. The GMC is different from the other rock complexes of the Yenisey Ridge in the presence of rapakivi-type granites. The geochemistry of these rocks, which is characterized by stronger enrichment in K2O, FeO, Y, Th, U, Zr, Hf, Nb, Ta, and REE relative to the other mineral assemblages of the GMC, is typical of anorogenic (A-type) within-plate granites. Among other distinctive features of these rocks are the strong iron enrichment of the melanocratic minerals, the presence of ilmenite as the sole Fe-Ti oxide, and crystallization from higher temperature (T = 825°C vs. T = 750°C) water-poor magmas under reducing conditions below the FMQ buffer. Significant variations in the geochemical and petrological characteristics of the GMC rocks suggest that they could not be derived from a single source. The main volume of the high-K rocks varying in composition from A-type to S-type granites was generated by melting of mixed mantlecrustal sources. The products of melting of the Late Archean-Early Proterozoic infracrustal gneisses of the Siberian Craton could be a possible source for the least oxidized rocks.
      PubDate: 2014-01-01
       
  • Experimental study of ZrO       class="a-plus-plus">2(c) solubility in water and
           aqueous perchloric acid solutions at 150 and 250°C
    • PubDate: 2014-01-01
       
  • Supergene transformed naphthides: Peculiarities of trace-element
           composition
    • Abstract: Abstract Available data on the transformation of naphthides (oils and bitumens) in various petroleum basins (PB) during supergene processes were generalized to reveal their characteristic features for more accurate prediction of pool preservation and commercial quality of oils as hydrocarbon raw material enriched in economically significant toxic metals. Using petroleum basins of the United States, Canada, Brazil, Venezuela, Nigeria, Russia, Kazakhstan, and Turkmenia as examples, itwas demonstrated that trace-element concentrations and ratios as well as metalloporphyrin complexes (MPC), including vanadium (Vp) and nickel (Nip) ones, which are associated with heavy resinous-asphaltene components of oils, serve as geochemical criteria of supergene transformed fluids. During supergenesis, oils show differential enrichment in metals. Considerable enrichment in V, Ni, Co, Mo, Cr, and other trace elements as well as MPC were found in oils generated by sapropel organic matter (OM) and initially enriched in metals (deposits of the South Tatar arch of the Volga-Urals, Buzachi arch, Afghan-Tajik Basin, and Marakaibo petroleum province of Venezuela). Oils initially depleted in trace elements and usually generated by humic OM also show increase in trace elements, but their concentrations are 1–3 orders of magnitude lower than those in enriched oils (oil fields in the coastal basins of Nigeria and Brazil). It was shown that supergene transformed fluids are well deciphered on the basis of a complex use of hydrocarbon and trace element criteria.
      PubDate: 2014-01-01
       
  • Duration of the formation and sources of the granitoids of the
           Litsk-Araguba Complex, Kola Peninsula
    • Abstract: Abstract Postorogenic granitoids of the Litsk-Araguba Complex compose a chain of intrusive bodies around 850 km2 in area, which are confined to the NE-trending deep-seated fault zone. Results of U-Pb zircon dating indicate that the formation of granitoids of the Litsk-Araguba Complex lasted 28 ± 9 Ma. Note that the rocks of the first-fourth phases have similar age within (1774–1762 Ma), while quartz syenites of the fifth phase were formed much later (1746 ± 8 Ma). The study of Sm-Nd isotopic system revealed that the quartz syenites plot in the field of the Nd isotopic evolution of the lower crust represented mainly by the Paleoproterozoic garnet granulites with model ages TNd(DM) = 2.4–2.7 Ga and ɛNd(T) from −5.6 to −6.3. It was found that the near-contact syenites of the Litsk Massif contain composite zircons with an age of 1758 ± 9Ma. They differ from zircons in coeval porphyraceous granites in lowered U and Th concentrations, which are close to those in zircons from the lower crustal garnet granulites of this region. These data in combination with internal structure of the crystals determine xenogenic lower-crustal origin of zircons from syenites and confirm geochemical data on the lower crustal input in the formation of granitoid melts.
      PubDate: 2014-01-01
       
  • Thermodynamic properties of Pd chloride complexes and the Pd       class="a-plus-plus">2+(aq) ion in aqueous
           solutions
    • Abstract: Abstract Based on the expert review of literature data on the thermodynamic properties of species in the Cl-Pd system, stepwise and overall stability constants are recommended for species of the composition [PdCl n ]2 − n , and the standard electrode potential of the half-cell PdCl 4 2− /Pd(c) is evaluated at E 298,15° = 0.646 ± 0.007 V, which corresponds to Δ f G 298.15° = −400.4 ± 1.4 kJ/mol for the ion PdCl 4 2− (aq). Derived from calorimetric data, Δ f H 298.15° PdCl 4 2− (aq) = −524.6 ± 1.6 kJ/mol and Δ f H 298.15° Pd2+(aq) = 189.7 ± 2.6 kJ/mol. The assumed values of the overall stability constant of the PdCl 4 2− ion and the standard electrode potential of the PdCl 4 2− /Pd(c) half-cell correspond to Δ f G 298.15° = 190.1 ± 1.4 kJ/mol and S 298.15° = −94.2 ± 10 J/(mol K) for the Pd2+(aq) ion.
      PubDate: 2014-01-01
       
  • Mechanism of density inversion formation in partially molten rocks
    • Abstract: Abstract This paper addresses the problem of the interpretation of geochemical laboratory experiments aimed at investigating partially molten rocks. The material of the terrestrial planets is differentiated at a certain stage of their evolution. In a gravity field, heavy and light particles move in a melt in different directions. This results in the formation of layers with different chemical and petrographic compositions in laboratory experiments and in planetary interiors. A density inversion appears in these layers under certain conditions. The dynamics of partially molten rocks was investigated using two analytical models. One of them is a problem of two bodies in a liquid governed by hydrodynamic Stokes equations. The second model describes the relative motion of solid particles in different directions in a viscous porous layer.
      PubDate: 2014-01-01
       
  • Rb-Sr dating of gold-sulfide mineralization in the Shaukhokh orefield,
           north Ossetia, Russia
    • PubDate: 2014-01-01
       
  • Geochemical characterization of adsorbed light gaseous alkanes in near
           surface soils of the eastern Ganga basin for hydrocarbon prospecting
    • Abstract: Abstract This study aims to assess the hydrocarbon potential of Ganga basin utilizing the near surface geochemical prospecting techniques. It is based on the concept that the light gaseous hydrocarbons from the oil and gas reservoirs reach the surface through micro seepage, gets adsorbed to soil matrix and leave their signatures in soils and sediments, which can be quantified. The study showed an increased occurrence of methane (C1), ethane (C2) and propane (C3) in the soil samples. The concentrations of light gaseous hydrocarbons determined by Gas Chromatograph ranged (in ppb) as follows, C1: 0–519, C2: 0–7 and C3: 0–2. The carbon isotopic (VPDB) values of methane varied between −52.2 to −27.1‰, indicating thermogenic origin of the desorbed hydrocarbons. High concentrations of hydrocarbon were found to be characteristic of the Muzaffarpur region and the Gandak depression in the basin, signifying the migration of light hydrocarbon gases from subsurface to the surface and the area’s potential for hydrocarbon resources.
      PubDate: 2014-01-01
       
  • Aquatic geochemistry of small lakes: Effects of environment changes
    • Abstract: Abstract This paper reports the results of an extensive investigation of water chemistry in the small lakes of European Russia and Western Siberia along a climatic gradient. It was demonstrated that small lakes unaffected by any direct contamination can be used as indicators of natural geochemical conditions of water formation, as well as global and regional fluxes of airborne pollution and climate warming. A novel concept was developed for within- and between-zone variability in water chemistry over vast areas of tundra, taiga, forest, and steppe, and contributions of natural and anthropogenic factors to its formation under present-day conditions were estimated. A proposed predictive scenario showed that climate warming will result in an increase in water salinity in southern regions and ubiquitous phosphorus enrichment in terrestrial waters; the hydrologic and geochemical conditions of water formation in northern Siberia will change significantly in response to permafrost thawing. Zonal features in the development of anthropogenically-induced processes in terrestrial surface waters (acidification, eutrophication, and metal enrichment) were determined. It was demonstrated that, in addition to naturally acidified lakes with high contents of humic acids, acid lakes of anthropogenic origin occur over the whole humid region discussed here, and acidification processes were characterized for each subregion. The trophic status of lakes and limitation of their bioproductivity with respect to nutrients were estimated. The concentrations and distribution of trace elements were analyzed in terrestrial waters from various climatic zones of European Russia and Western Siberia, and the first estimates were obtained for the mean concentrations and coefficients of migration of a wide range of elements in terrestrial freshwaters. We distinguished a group of metal (Mo, As, U, Bi, Sb, Cd, Ag, Se, Re, Pb, Cd, W, etc.) the enrichment of which in natural waters results from their global dispersion in the environment. Experimental results and natural observations are presented on the processes of metal ion complexation with humus substances, and sequences of their increasing activity in competing for organic ligands were derived. Data are presented on the speciation of metals depending on natural water chemistry in the tundra, taiga, and steppe zones. The pioneering investigations on the geochemistry of natural waters allowed us to substantiate new regional norms for water quality.
      PubDate: 2013-12-01
       
  • Geochemical signature of bottom sediments in the mixing zones of Ob and
           Yenisei waters with Kara Sea water
    • Abstract: Abstract This paper reports the results of a study of the geochemistry of bottom sediments from the zones of mixing between the freshwater of the Ob and Yenisei rivers and the saline water of the Kara Sea by means of neutron activation analysis. Using separate datasets for the sediments of the Ob and Yenisei estuaries accumulated under identical facies conditions, some characteristic features of the distribution of a number of chemical elements (mostly lithophile group elements) were established. The differences between them were attributed to distinctive regional geological and geochemical features of the catchments of the Ob and Yenisei, which are inherited by the geochemical characteristics of terrigenous material transported to the sea. The choice of the most informative indicator elements and their grouping on the basis of the character of behavior demonstrated that bottom sediments of the Ob or Yenisei origin can be identified in the marine region studied using the geochemical characteristics of a small group of samples.
      PubDate: 2013-12-01
       
  • FeO activity and oxygen potential in magnesian magmas
    • Abstract: Abstract An equation for the excess free energy of melts containing all major components is derived from published experimental data on equilibria between silicate liquids with either metallic iron or spinel at controlled oxygen partial pressure. The FeO activities in mafic and ultramafic magmas calculated with this equation were used to develop an oxygen barometer (geoxometer) for the association spinel + melt. Data derived with the application of the geoxometer confirm that meymechite magmas in the Siberian trap province had oxygen fugacities higher than in other magmatic systems. The origin of lower lithospheric domains with elevated redox potential can be explained by the intense diffusion of hydrogen from zones in which water-rich near-solidus melts from asthenospheric sources were emplaced into harzburgites, which had lost water and other incompatible elements in the course of earlier large-scale melting.
      PubDate: 2013-12-01
       
  • First data on noble metal minerals in the metamafic rocks of the Ilikan
           lithotectonic zone, southeastern framing of the North-Asian craton
    • PubDate: 2013-12-01
       
  • Use of platinum capsules in the study of the carbon and hydrogen
           solubility in silicate melts in equilibrium with liquid iron alloys at
           high pressures and temperatures
    • PubDate: 2013-12-01
       
  • Hydrogeochemistry and geothermometry of the Jowshan thermal springs,
           Central Iran
    • Abstract: Abstract Jowshan geothermal system comprises 6 thermal springs with outlet temperatures ranging from 39.3 to 46.6°C. The thermal water of these springs is presently used for swimming and as a treatment for rheumatism, sinusitis and skin diseases. The pH value of these springs is slightly acidic to neutral and the electrical conductivities about 1500 μS/Cm. The presence of many faults in the area, the alignment of all springs along the Sirch Fault and the similar chemical and isotopic composition of all springs in combination with the hydrogeological setting and geochemistry of water samples indicate that these springs are associated with deep circulation of meteoric water. According to this heating mechanism, meteoric waters infiltrate through fault openings to depth and after heating by geothermal gradient rise to the ground surface due to the hydraulic and buoyancy forces, a mechanism which is common in the southern parts of Iran. The use of various chemical geothermometers and mineral equilibrium states suggests a range of temperature about 50–90°C for the reservoir of Jowshan geothermal system.
      PubDate: 2013-12-01
       
  • Formation of nitrogen-rich hot springs: Modeling physicochemical
           interactions in a water-granite system
    • Abstract: Abstract The chemical evolution of solutions and secondary minerals was studied in the systems water-granite without volatiles and granite with average concentrations of volatiles under constant thermodynamic conditions corresponding to those observed in natural nitrogen-rich hot springs and at variable (rock/water) ratio. The results show that, at average concentrations of volatiles, the concentrations of anions in solution can approach those observed in natural nitrogen-rich thermal waters, although the TDS (total dissolved solids) is higher than that of natural analogues. Natural nitrogen-rich thermal waters are formed in rocks with volatile abundances higher than the average values.
      PubDate: 2013-12-01
       
  • Geochemistry and metamorphic parameters of rocks in the Batomga
           granite-greenstone terrane, Aldan Shield
    • Abstract: Abstract The protoliths of the Early Proterozoic metamorphic complex in the Batomga granite-greenstone terrane are proved to comprise two petrochemical series of volcanic rocks: calc-alkaline and komatiite-tholeiite. The metavolcanic rocks of the calc-alkaline series are metamorphosed basalts, andesites, dacites, and rhyolites. The topology of the trace-element patterns of the acid volcanics is similar to that of Archean gray gneisses in platform basements, and this suggests that the petrologic mechanisms that produced the protoliths could be similar. The metavolcanics of the komatiite-tholeiite series are determined to include komatiite and tholeiite basalts. Their chemical composition is consistent with the fractionation model of high-Mg basalts in intermediate chambers under low pressures. The Nb, Y, and Zr concentrations of the metatholeiites testify that their parental melts were derived from a plume source. The metamorphic culmination parameters of the rocks corresponded to the boundary between the amphibolite and granulite facies of elevated pressure.
      PubDate: 2013-12-01
       
  • He implantation and concentrations in minerals and lunar regolith
           particles
    • Abstract: Abstract Solar-wind erosion of rocks on the lunar surface and the implanting of solar-wind particles in minerals of lunar regolith are principally important processes of space weathering. The latter process leads to the accumulation of inert gases in mineral particles of lunar regolith. Literature data indicate that, depending on the composition and structure of the particles, the concentrations of implanted He in various minerals range within roughly three to four orders of magnitude. The lowest He implantation coefficient was determined in amorphous particles (glass), and very low implantation coefficients were also obtained in experiments on He implantation in glass (obsidian).
      PubDate: 2013-12-01
       
  • Thirteenth international conference on physicochemical and petrophysical
           studies in Earth Sciences
    • PubDate: 2013-11-01
       
  • Phase equilibria in the system lamprophyllite-nepheline
    • Abstract: Abstract Experimental studies of the melting diagram for the lamprophyllite-nepheline system and data on the phases crystallizing in this system indicate that lamprophyllite incongruently melts with the origin of melt and titanium oxide. The maximum temperature at which nepheline and lamprophyllite can occur in equilibrium is estimated at 833 ± 6°C. Our pioneering data on lamprophyllite crystallization from melt prove that this mineral can be of magmatic genesis. The distribution coefficients between lamprophyllite and melt are evaluated for K (0.1–0.25), Mn (0.82–1.06), Fe (0.13–0.40), and Mg (0.82–1.5); and the Sr/Ba lamprophyllite/melt exchange coefficient is estimated at 1.8–3.7.
      PubDate: 2013-11-01
       
  • Thermodynamic properties of compounds in the PdO-H       class="a-plus-plus">2O system at 25°C
    • Abstract: Abstract Literature thermodynamic data on species and particles existing in the heterogeneous PdO-H2O system were checked for consistency, and the equilibrium constants for dissolution of palladium oxide and hydroxide in water and for Pd2+ (aq) hydrolysis were recommended. Δ f G 298.15 ° obtained in this work for Pd2+(aq) sharply differs (no less than by 6 kJ/mol) from values that are reported in fundamental thermodynamic reference books and based on experimentally measured palladium electrode potential at 25°C. Detailed examination of literature data on the thermodynamic properties of compounds in the Cl-Pd(aq) system is required to account for revealed inconsistency.
      PubDate: 2013-11-01
       
 
 
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