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CHEMICAL ENGINEERING (185 journals)                  1 2     

AATCC Journal of Research     Full-text available via subscription   (Followers: 3)
Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials     Hybrid Journal   (Followers: 4)
Acta Polymerica     Hybrid Journal   (Followers: 6)
Additives for Polymers     Full-text available via subscription   (Followers: 20)
Adhesion Adhesives & Sealants     Hybrid Journal   (Followers: 5)
Advanced Chemical Engineering Research     Open Access   (Followers: 9)
Advanced Powder Technology     Hybrid Journal   (Followers: 16)
Advances in Applied Ceramics     Partially Free   (Followers: 3)
Advances in Chemical Engineering     Full-text available via subscription   (Followers: 17)
Advances in Chemical Engineering and Science     Open Access   (Followers: 24)
Advances in Polymer Technology     Hybrid Journal   (Followers: 11)
African Journal of Pure and Applied Chemistry     Open Access   (Followers: 5)
Annual Review of Analytical Chemistry     Full-text available via subscription   (Followers: 9)
Annual Review of Chemical and Biomolecular Engineering     Full-text available via subscription   (Followers: 10)
Anti-Corrosion Methods and Materials     Hybrid Journal   (Followers: 5)
Applied Petrochemical Research     Open Access   (Followers: 3)
Asia-Pacific Journal of Chemical Engineering     Hybrid Journal   (Followers: 6)
Biochemical Engineering Journal     Hybrid Journal   (Followers: 9)
Biofuel Research Journal     Open Access   (Followers: 1)
Biomass Conversion and Biorefinery     Partially Free   (Followers: 6)
BMC Chemical Biology     Open Access   (Followers: 4)
Brazilian Journal of Chemical Engineering     Open Access   (Followers: 3)
Bulletin of the Chemical Society of Ethiopia     Open Access   (Followers: 2)
Carbohydrate Polymers     Hybrid Journal   (Followers: 9)
Catalysts     Open Access   (Followers: 8)
Chemical and Engineering News     Free   (Followers: 6)
Chemical and Materials Engineering     Open Access   (Followers: 1)
Chemical and Petroleum Engineering     Hybrid Journal   (Followers: 9)
Chemical and Process Engineering     Open Access   (Followers: 3)
Chemical and Process Engineering Research     Open Access   (Followers: 5)
Chemical Communications     Full-text available via subscription   (Followers: 31)
Chemical Engineering & Technology     Hybrid Journal   (Followers: 25)
Chemical Engineering and Processing: Process Intensification     Hybrid Journal   (Followers: 10)
Chemical Engineering and Science     Open Access   (Followers: 3)
Chemical Engineering Communications     Hybrid Journal   (Followers: 10)
Chemical Engineering Journal     Hybrid Journal   (Followers: 22)
Chemical Engineering Research and Design     Hybrid Journal   (Followers: 18)
Chemical Engineering Research Bulletin     Open Access   (Followers: 1)
Chemical Engineering Science     Hybrid Journal   (Followers: 16)
Chemical Geology     Hybrid Journal   (Followers: 10)
Chemical Papers     Hybrid Journal   (Followers: 3)
Chemical Product and Process Modeling     Hybrid Journal   (Followers: 3)
Chemical Reviews     Full-text available via subscription   (Followers: 161)
Chemical Society Reviews     Full-text available via subscription   (Followers: 33)
Chemical Technology     Open Access   (Followers: 5)
ChemInform     Hybrid Journal   (Followers: 3)
Chemistry & Industry     Hybrid Journal   (Followers: 2)
Chemistry Central Journal     Open Access   (Followers: 5)
Chemistry of Materials     Full-text available via subscription   (Followers: 144)
Chemometrics and Intelligent Laboratory Systems     Hybrid Journal   (Followers: 6)
ChemSusChem     Hybrid Journal   (Followers: 8)
Chinese Chemical Letters     Full-text available via subscription   (Followers: 2)
Chinese Journal of Chemical Engineering     Full-text available via subscription   (Followers: 3)
Chinese Journal of Chemical Physics     Hybrid Journal   (Followers: 1)
Coke and Chemistry     Hybrid Journal  
Coloration Technology     Hybrid Journal   (Followers: 1)
Computational Biology and Chemistry     Hybrid Journal   (Followers: 8)
Computer Aided Chemical Engineering     Full-text available via subscription   (Followers: 2)
Computers & Chemical Engineering     Hybrid Journal   (Followers: 8)
CORROSION     Full-text available via subscription   (Followers: 3)
Corrosion Engineering, Science and Technology     Hybrid Journal   (Followers: 22)
Corrosion Reviews     Hybrid Journal   (Followers: 4)
Crystal Research and Technology     Hybrid Journal   (Followers: 2)
Current Opinion in Chemical Engineering     Open Access   (Followers: 3)
Education for Chemical Engineers     Hybrid Journal   (Followers: 4)
Ekologia : The Journal of Institute of Landscape Ecology of Slovak Academy of Sciences     Open Access  
Eksergi     Open Access  
Emerging Trends in Chemical Engineering     Full-text available via subscription  
European Polymer Journal     Hybrid Journal   (Followers: 43)
Fibers and Polymers     Full-text available via subscription   (Followers: 3)
Fluorescent Materials     Open Access  
Focusing on Modern Food Industry     Open Access   (Followers: 3)
Frontiers of Chemical Science and Engineering     Hybrid Journal   (Followers: 1)
Gels     Open Access  
Geochemistry International     Hybrid Journal  
Handbook of Powder Technology     Full-text available via subscription   (Followers: 3)
Heat Exchangers     Open Access   (Followers: 1)
High Performance Polymers     Hybrid Journal  
Indian Chemical Engineer     Hybrid Journal   (Followers: 3)
Indian Journal of Chemical Technology (IJCT)     Open Access   (Followers: 11)
Industrial & Engineering Chemistry     Full-text available via subscription   (Followers: 9)
Industrial & Engineering Chemistry Research     Full-text available via subscription   (Followers: 20)
Industrial Chemistry Library     Full-text available via subscription   (Followers: 4)
Info Chimie Magazine     Full-text available via subscription   (Followers: 2)
International Journal of Chemical and Petroleum Sciences     Open Access   (Followers: 1)
International Journal of Chemical Engineering     Open Access   (Followers: 7)
International Journal of Chemical Reactor Engineering     Hybrid Journal   (Followers: 3)
International Journal of Chemical Technology     Open Access   (Followers: 4)
International Journal of Chemoinformatics and Chemical Engineering     Full-text available via subscription   (Followers: 2)
International Journal of Food Science     Open Access   (Followers: 3)
International Journal of Industrial Chemistry     Open Access  
International Journal of Polymeric Materials     Hybrid Journal   (Followers: 3)
International Journal of Science and Engineering     Open Access   (Followers: 7)
International Journal of Waste Resources     Open Access   (Followers: 5)
Journal of Chemical Engineering & Process Technology     Open Access   (Followers: 3)
Journal of Applied Crystallography     Hybrid Journal   (Followers: 4)
Journal of Applied Electrochemistry     Hybrid Journal   (Followers: 12)
Journal of Applied Polymer Science     Hybrid Journal   (Followers: 128)
Journal of Biomaterials Science, Polymer Edition     Hybrid Journal   (Followers: 8)
Journal of Bioprocess Engineering and Biorefinery     Full-text available via subscription  

        1 2     

Journal Cover   Geochemistry International
  [SJR: 0.491]   [H-I: 14]   Follow
   Hybrid Journal Hybrid journal (It can contain Open Access articles)
   ISSN (Print) 1556-1968 - ISSN (Online) 0016-7029
   Published by Springer-Verlag Homepage  [2291 journals]
  • Brines in the western part of the Tunguska artesian basin
    • Abstract: Abstract Geochemistry of brines in the Tunguska artesian basin indicates that these brines were in equilibrium with carbonate, sulfate, and secondary aluminosilicate minerals but not with primary aluminosilicates. Salinity of brines saturated with halite is greater than 360 g/dm{sn3}. Analysis of the Ca/Cl, Sr/Cl, and Br/Cl ratios of the brines testifies that an increase in the salinity of the brines and variations in their composition result from metamorphism in the water–rock system. The principal Ca and Sr sources of the brines are sulfates (anhydrite, gypsum, and celestine), which are dissolved because of reduction of the sulfate ion and its removal from the system: CaSO4 + 2Corg + MgCl2 + 2H2O = MgCa(CO3)2 + H2S + 2HCl. Another process forming the chemical composition of the brines is interaction with primary (Ca, Mg) aluminosilicates according to the reaction: CaAl2Si2O8 + 3H2O + 2CO2 = Al2Si2O5(OH)4 + Ca{sn2+} + 2HCO − 3 .The principal source of Br for the brines is seawater.
      PubDate: 2015-08-01
  • Geochemical evidence of an oceanic provenance of cherts in accretionary
           complexes in the Sikhote Alin
    • Abstract: Abstract The paper reports pioneering data on the distribution of REE in cherts in the Taukha terrane of the Late Jurassic–Early Cretaceous accretionary prism in the Sikhote Alin and a calculated value of the Ce anomaly. The values of the Ce anomaly, the ratios of certain major components, and the ratios of these components and REE are used to estimate the facies environments in which the cherty material was accumulated. This material is proved to have started accumulating within a zone adjacent to the spreading ridge and continued on the abyssal plane. The uppermost portion of the vertical section, which is made up of siliceous mudstone, was deposited in the marginal part of the paleoocean adjacent to the continental marginal sedimentation region. The sedimentation environments systematically alternating in a single geologic section suggest that the part of the seafloor on which the cherty sediments were accumulated moved from the spreading cen-ter to the margin of the paleocontinent, and this caused the drift of the stratigraphic section across various oceanic facies zones.
      PubDate: 2015-08-01
  • Equilibrium of nitrogen-rich spring waters of the Baikal Rift Zone with
           host rock minerals as a basis for determining mechanisms of their
    • Abstract: Abstract This paper presents calculations of equilibria between nitrogenrich hot springs of the Baikal Rift Zone (BRZ) and a secondary mineral assemblage (carbonate, fluoride, clay, zeolite, and other minerals). The results confirm the equilibrium–nonequilibrium character of the nitrogen spring water–rock system. Unlike other water types, the system evolves under conditions of continuous incorporation of chemical elements released from the host minerals into the newly formed secondary minerals. This allows the system to remain dynamically stable with no increase in salinity, despite continued water–rock interaction. The main factor responsible for this state of the system is a deficiency of acids, i.e., high pH. As a result, the disturbance of relationships between concentrations of aqueous species compared to the starting composition of dissolved solids produces a deficiency of some elements (Ca, Mg, Fe, Al, etc.) and an excess of other elements (Na, Si, F, etc.).
      PubDate: 2015-08-01
  • Distribution of 137 Cs, 90 Sr, and plutonium isotopes in grounds at the
           peaceful nuclear explosion site
    • PubDate: 2015-08-01
  • Evidence of Middle Neoproterozoic extensional tectonic settings along the
           western margin of the Siberian craton: Implications for the breakup of
    • Abstract: Abstract The new results of U–Pb and 40Ar/39Ar dating and petrological and geochemical studies of rocks from the Yenisey regional shear zone (YRSZ) in the Transangarian part of the Yenisey Ridge were used to identify a dike belt at the western margin of the Siberian craton and constrain the timing of formation of rift-related structures accompanied by within-plate magmatism. The magmatism of this epoch produced felsic and mafic intrusive rocks. The extension processes are recorded by the 797–787 Ma dike swarms. The rift origin of the rocks studied here is confirmed by their occurrence as dikes and sills confined to the YRSZ, bimodal composition of magmatic rock associations, and petrochemical characteristics of rocks typical of within-plate settings. The formation of the 800 Ma dike belt within the study area could be associated with the Neoproterozoic extensional tectonic events along the western margin of the Siberian craton which coincided with the onset of the breakup of the Rodinia supercontinent. These events provide the upper age limit for the collisional metamorphism that took place at the final stage of orogeny. The evolutionary phases identified in the region agree well with the sequence and style of tectonothermal events within the Valhalla Orogen at the Arctic margin of Rodinia and provide further support for the spatial proximity between Siberia and North Atlantic cratons during this epoch, as indicated by recent paleomagnetic data.
      PubDate: 2015-08-01
  • Enthalpy of formation of palladium bismuthides PdBi and PdBi 2 from
    • PubDate: 2015-08-01
  • Study of complex molecular species in the gas phase over the
           CaO–MgO–Al 2 O 3 –TiO 2 –SiO 2 system
    • Abstract: Abstract Experimental mass spectrometric data obtained by the Knudsen effusion mass spectrometry are used to analyze principal tendencies in the formation of complex oxides contained in the gas phase over compounds and melts in the CaO–MgO–Al2O3–TiO2–SiO2 system. Dependences are derived for concentrations of the complex molecular species in the gas phase at the vaporization of mullite Al6Si2O13, wollastonite CaSiO3, spinel MgAl2O4, perovskite CaTiO3, and the Al2O3–SiO2 and CaO–SiO2 binary boundary systems on temperature, melt composition, and oxygen partial pressure.
      PubDate: 2015-08-01
  • Organic carbon in the Razdol’naya River Estuary (Amur Bay, Sea of
           Japan) during the period of ice cover
    • Abstract: Abstract The paper presents data on organic carbon concentrations in riverine suspended matter and surficial bottom sediments measured in the estuary of the Razdol’naya River during the period of ice cover (February 2010). In the suspended matter, humic substances and phytoplankton accounted for 30% and 14% of total organic carbon, respectively. The concentration of humic substances in riverine suspended matter was determined for the first time by spectrophotometry. The concentration of phytoplankton carbon was calculated from the chlorophyll-a content. Concentrations of organic carbon, humic substances, and chlorophyll-a were measured in the surface sediment layer. The proportions of these three components show no marked variability with an increase in salinity to 23‰. The degree of humification in bottom sediments was about 52%. Organic carbon concentrations were almost an order of magnitude lower and the proportion of bioavailable (nonhumified) carbon was two times lower in the bottom sediments than in the riverine suspended matter.
      PubDate: 2015-08-01
  • Possibility of estimating acid-base properties of minerals and rocks by
           means of physicochemical simulations (with the Selector-C program package)
    • Abstract: Abstract The basicity-acidity of minerals and rocks is estimated by the Gibbs free energy minimization technique with the use of modern thermodynamic data (Selector-C program package). A provisional scale of acid-base properties of minerals and rocks is constructed based on the properties of pure water in equilibrium with them. The composition of solution under standard conditions and base-acid parameters (pH25) are calculated for reactions of pure water with various rock-forming minerals that dissolve congruently or incongruently. A method is suggested for evaluating the base-acid parameters of rocks on the basis of solving the inverse problems of convex programming of the composition and properties of solution (supercritical fluid) in equilibrium with a real mineral association.
      PubDate: 2015-07-01
  • Pt behavior in the Pt-C-S ± Fe-H 2 O system at 200–400°C
           and P tot = 1 kbar: Experimental results
    • Abstract: Abstract The effect of sulfur on platinum adsorption on carbonaceous matter (CM) was experimentally studied at 200–400°C and P tot = 1 kbar. The IR spectra of the experimental products indicate that sulfur accelerates HC condensation and aromatization, but the effect of sulfur on platinum concentrations in the organic fractions is within the analytical uncertainties. SEM images show the development of a multilayer porous carbonaceous film on the walls of the ampoules and platinum in physical contact with carbonaceous matter. The composition of the film varies, depending on its thickness (3–25 μm), within the following limits: 61.06–100 wt % C, 0–33.7 wt % Pt, 0–5.17 wt % O, and 0–0.74 wt % S. The film contains tiny Pt crystals, whose morphology varies with increasing duration of the experiments from nanometer- and micrometer-sized spheroids to subequant, tabular, and wire-like. Depending on their size, the composition of the crystals varies as follows: 23.30–52.45 wt % Pt, 49.57–73.52 wt % C, and 0–4.20 wt % O. According to our SEM data, the kerogen also contains tiny crystalline segregations of carbon aceous platinum whose morphology and composition are analogous to those on the film. The presence of carbon in the tiny platinum crystals deposited from solution can be explained by the background effect of the kerogen of the film and/or by their crystallization from organo-platinum complexes. In our kinetic experiments, local electrochemical reactions produced aggregates of nanometer-sized (60–250 nm) spheroids around larger micrometer-sized (up to 10 μm) spheroids, whose aggregation resulted in larger crystals and their further transformation. The polymorphism, hierarchical aggregation, and compositional variability of the platinum segregations are likely typical of car- bon-bearing systems because of their crystallization from metastable organo-platinum complexes.
      PubDate: 2015-07-01
  • Natural 226 Ra and 232 Th radionuclides in xenophyophores of the Pacific
    • PubDate: 2015-07-01
  • Heat capacity and thermodynamic functions of SmPO 4 at 10–1600 K
    • Abstract: Abstract The heat capacity of SmPO4 was measured by adiabatic calorimetry at 10–346 K. Thermodynamic functions of Sm orthophosphate at 10–1600 K were calculated based on our experimental and available literature data. The Gibbs energy of Sm orthophosphate formation is Δ f G 0(298.15 K) − Δ f G 0(10 K) = −1844.7 ± 2.4 kJ mol−1.
      PubDate: 2015-07-01
  • Results of experimental determination of the intrinsic oxygen fugacity of
           Ru-Os-Ir alloys from the Verkh-Neivinsky Dunite-Harzburgite Massif, Middle
           Urals, Russia
    • PubDate: 2015-07-01
  • Calorimetric determination of the enthalpy of formation of natural
    • Abstract: Abstract The enthalpies of formation of natural trioctahedral smectite from elements were determined for the first time by high-temperature melt solution calorimetry using Tian-Calvet microcalorimeter: Δ f H 0(298.15 K): −5799.1 ± 5.1 kJ/mol for saponite Ca0.1Na0.1K0.1(Mg2.6Fe 0.1 2+ Fe 0.2 3+ )[Si3.6Al0.4O10](OH)2 (Arkhangelsk diamond province) and −5937.3 ± 6.0 kJ/mol for saponite Ca0.4(Mg2.6Al0.2)[Si3.4Al0.6O10](OH)2 (Mt. Kukisvumchorr, Khibiny). The enthalpies of formation of magnesian and magnesium-iron saponites of theoretical composition were estimated.
      PubDate: 2015-07-01
  • Sources of high-pressure fluids involved in the formation of hydrothermal
    • Abstract: Abstract Available fluid inclusion data on hydrothermal deposits, deep-seated xenoliths, magmatic and metamorphic rocks were used to generalize the determinations of physicochemical parameters (temperature, pressure, and compositions) of natural fluids. It was established that fluid pressures during formation of hydrothermal deposits often exceeded lithostatic loading (250–270 bar/km) of the overlying rocks. Fluids from deep-seated xenoliths, magmatic and metamorphic objects are considered as the possible sources of high-pressure fluids. Data on temperatures, pressures, and fluid composition are generalized for each object.
      PubDate: 2015-07-01
  • Devonian ore clastic turbidites of the Molodezhnoe massive copper sulfide
           deposit, Southern Urals
    • Abstract: Abstract We present data on the composition of Devonian ore clastic sediments accumulated at the boundaries of the orebodies of the Molodezhnoe massive copper sulfide deposit, Southern Urals. They are interpreted to be accumulated during the synsedimentary and postsedimentary stages. The synsedimentary stage was marked by gravity transport and accumulation of products of the destruction of high-temperature black smoker chimneys. During the postsedimentary stage, the deposits underwent two types of mineralogical and geochemical transformation: (1) infiltration-metasomatic effects of ore-bearing solutions and infiltration effects of seawater causing redistribution of copper and carbonates in the sediments and formation of authigenic minerals (chalcopyrite, siderite, secondary calcite, and apatite and replacement of aluminosilicates by chlorite) and (2) dehydration accompanied by the replacement of iron hydroxides by hematite and amorphous silica by quartz. Temperatures of the postsedimentary alteration were estimated from a fluid inclusion study and thermodynamic computer modeling as 150–250°C and correspond to the metagenesis stage (burial metamorphism). The organic matter composition was characterized by TOC, hydrogen and oxygen indices (HI and OI), and δ13C values.
      PubDate: 2015-07-01
  • Hydrogeochemistry of high fluoride groundwater in hard rock aquifer in a
           part of Dharmapuri district, Tamil Nadu, India
    • Abstract: Abstract Fluoride is one of the important ions that affect the groundwater quality. F− concentration above 1.5 mg/L in drinking water affects teeth and bones of humans. Usually the F− concentration in groundwater is controlled by local geological setting and climatic condition of an area. The present study aims to assess the hydrogeochemistry of groundwater in Vaniyar River basin, Dharmapuri district and to understand the F− abundance in groundwater. Forty four representative groundwater samples were collected for once in two months and analyzed for major cations and anions using ion chromatograph. The general order of the dominance of major cations is Na+ > Ca2+ > Mg2+ > K+ and that of major anions is Cl− > HCO 3 − > SO 4 2− > CO 3 − > F−. Most of the samples are Na-Cl type and few are Ca-Mg-Cl and Ca-Cl types. The F− concentration in groundwater of this region ranges from 0.15 to 6.48 mg/L and many of the residents are affected by dental and skeletal fluorosis. The arid climatic conditions of the region, dominance of gneissic rocks and the low freshwater exchange due to periodical drought conditions endorse the presence of high F− concentration in the groundwater of the area.
      PubDate: 2015-06-01
  • New data on zircon geochemistry and age (U-Pb, SHRIMP II) of the
           Yastrebetskoe Zr-REE-Y deposit, Ukrainian shield
    • PubDate: 2015-06-01
  • Solubility of ZrO 2 , HfO 2 , Ta 2 O 5 , Nb 2 O 5 , and H 2 O + H 2 in
           fluid-saturated haplogranite melt at 100 MPa, 800°C, and variable
           redox conditions
    • PubDate: 2015-06-01
  • Types of OH-bearing point defects in olivine and their transformation
           under changing petrological conditions
    • Abstract: Abstract In this paper, we characterize the most common coupled point defects in the olivine structure of the hydrous olivine {v Me, 2OH−}, humite {v Si, 4OH−}, laihunite {v Me, 2Fe3+}, hydroxyl {v Me, Fe3+, OH−}, and Schottky {v Me, v O} types, where v is a vacancy. Their segregation and evolution under changing physicochemical conditions were considered. During the development of deformation textures, the segregation of {v Me, 2OH−} and {v Si, 4OH−} defects is accompanied by the formation of planar features in olivine consisting of hydrous olivine, n(Mg,Fe)2SiO4 · MgH2SiO4, and humite-like layers, n(Mg,Fe)2SiO4 · Mg(OH)2, respectively. Under the conditions of low-temperature oxidation, the segregation of {v Me, 2Fe3+} defects in anhydrous olivine results in the formation of planar laihunite-type defects. The OH-bearing defects undergo dehydrogenation and oxidation during heating with decompression, which results in the transformation of hydrous olivine-type defects into laihunite-type {vMe, 2Fe3+} or hydroxyl-type {v Me, Fe3+, OH−} defects. The mobility of coupled point defects and their ability to segregate and form new phases in the host olivine, the possibility of releasing a proton with transformation into defects of a different type, and potential role as an oxidizer in dehydrogenation processes are manifested upon changes in physicochemical conditions and can be considered as indicators of geologic processes accompanied by variations in P, fO2, and aH2O.
      PubDate: 2015-06-01
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