ETUDE COMPARATIVE DE SOLS DES LAURENTIDES, QUEBEC

1975 ◽  
Vol 55 (3) ◽  
pp. 363-379 ◽  
Author(s):  
B. MUTWEWINGABO ◽  
C. R. DE KIMPE ◽  
G. A. BOURBEAU ◽  
R. W. BARIL ◽  
P. LAJOIE
Keyword(s):  
Particle Size ◽  
Clay Fraction ◽  
Parent Material ◽  
The Other ◽  
Quebec City ◽  
X Ray Diffraction ◽  
X Ray ◽  
High Bulk Density ◽  
Diffraction Patterns ◽  
High Bulk

Five profiles were sampled in the till deposits of the Laurentides Hills. Two were obtained at Duchesnay, near Quebec City and three north of Montreal, including two profiles of the Gatineau and one of the Sainte-Agathe series of soils. Results of the particle-size distribution, morphological and mineralogical analyses suggested that the parent material was similar in all profiles. A high bulk density, about 2.00 g/cm3, was observed in the fragic horizon. Maximum weathering was found in the A horizons resulting in the formation of montmorillonite and kaolinite. The X-ray diffraction patterns obtained for the samples from Duchesnay were better defined than those obtained from the other profiles. In addition to illite, chlorite and vermiculite, two types of interstratified minerals were observed: illite–montmorillonite in the Podzolic-B and illite–vermiculite in the fragic horizons. High values, up to about 700 meq/100 g were obtained for the Al interlayers in the clay fraction. These profiles were classified as fragic ferro-humic Podzols (Sainte-Agathe and the profiles from Duchesnay) and fragic humo-ferric Podzols (Gatineau). The concept of fragic horizon in the soils from the Laurentides is discussed.

Semiquantitative Analysis by X-Ray Powder Diffraction (SQXRD) of the < 2 mm to 0.002 mm and < 0.002 mm Fractions of Soil

1988 ◽  
Vol 3 (3) ◽  
pp. 144-152 ◽  
Author(s):  
G. A. Raab
Keyword(s):  
Particle Size ◽  
Clay Fraction ◽  
Internal Standard ◽  
Xrd Analysis ◽  
X Ray Diffraction ◽  
X Ray ◽  
Heat Treated ◽  
Freeze Dried ◽  
Strict Protocol ◽  
Attention To Detail

AbstractThe method described in this paper is a strict protocol for X-ray diffraction (XRD) analysis of mineral phases found in soils. Its application is not restricted to soils and is an attempt to standardize XRD sample preparation and analysis. The protocol requires the particle size of the < 2 mm - 0.002 mm fraction be reduced to 0.002 mm before analysis. In die qualitative section, the clay fraction ( < 0.002 mm particle size) is prepared as oriented slides. The suspended clay fraction is saturated with ethylene glycol, K +, and Mg+2; pipeted; air-dried; heat-treated at 110°C, 350°C, and 550°C; and X-rayed at each step in order to properly identify the clay minerals. In the quantitative section, the method employs a matrix-flushing agent, corundum (Al2O3). The corundum acts also as an internal standard, a calibration standard, and a reference standard. The suspended clay fraction is freeze-dried and corundum is added to each sample. Randomly oriented powder mounts are prepared from the < 2 mm - 0.002 mm fraction, and the < 0.002 mm fraction, and X-rayed. A series of reference standards are prepared based on the existing mineralogy, corundum is added, and each mixture is X-rayed. The software integrates the area under specific peaks (chosen for intensity and no overlap) in each sample, calculates the reference intensity ratios (RIRs) and calculates the percentage of each mineral based on the equation of Chung (1974). The attention to detail allows documentation and verification of the results yielding data of known quality.

Identification of Different Crystalline Forms of Diatrizoic Acid

1978 ◽  
Vol 61 (1) ◽  
pp. 72-75
Author(s):  
Victor A Folen ◽  
George Schwartzman ◽  
Millard Maienthal ◽  
Wilson L Brannon
Keyword(s):  
Weight Loss ◽  
The Other ◽  
Reference Standard ◽  
Thermal Gravimetric ◽  
X Ray Diffraction ◽  
X Ray ◽  
No Weight Loss ◽  
Diffraction Patterns ◽  
Crystalline Forms ◽  
Reference Samples

Abstract Standard reference samples of diatrizoic acid gave 2 different infrared (IR) spectra, x-ray diffraction patterns, and differential thermal and thermal gravimetric curves. One form, the anhydrous acid, shows no weight loss when heated to 170°C. The other form, the dihydrate, loses 5.36% of its weight when heated from 86 to 144°C. The anhydrous diatrizoic acid is the preferred reference standard, because it has an IR spectrum and x-ray diffraction pattern suitable for identification purposes.

Possible effects of land use on the clay mineralogy of a brown forest soil

Clay Minerals ◽  
2002 ◽  
Vol 37 (4) ◽  
pp. 663-670 ◽  
Author(s):  
D. C. Bain ◽  
D. T. Griffen
Keyword(s):  
Land Use ◽  
Clay Mineralogy ◽  
Parent Material ◽  
X Ray Diffraction ◽  
Brown Forest Soil ◽  
X Ray ◽  
Close Proximity ◽  
Diffraction Patterns ◽  
Effects Of Land Use ◽  
Brown Forest Soils

AbstractThree soil profiles classed as brown forest soils on schistose parent material, in close proximity but under different land uses, have been studied. The profile under 50 year-old Sitka spruce trees is the most acidic, the second profile under rough grassland is less acidic, and the third profile in an arable field which has been fertilized is the least acidic. The clay fractions (ς μm) of all three profiles are very similar. However, computer simulations of the X-ray diffraction patterns of clay phases using a modified version of NEWMOD revealed two possible weathering trends: (1) an increasing proportion of vermiculite in interstratified mica-vermiculite in the upper horizons of the arable and forested soils; (2) formation of high-charge corrensite by weathering of chlorite in all three profiles but least pronounced in the arable soil. The differences in clay mineralogy amongst the profiles are minor, but these two different weathering trends may be due to the effects of different land use.

Powder X-Ray Data for Synthetic Anhydrous Sodium Zirconium Silicates

1987 ◽  
Vol 2 (3) ◽  
pp. 176-179 ◽  
Author(s):  
G. Wilson ◽  
F. P. Glasser
Keyword(s):  
Solid State ◽  
Diffraction Pattern ◽  
Powder Diffraction ◽  
Solid State Reaction ◽  
The Other ◽  
X Ray Diffraction ◽  
Powder Diffraction File ◽  
X Ray ◽  
Sodium Zirconium ◽  
Diffraction Patterns

AbstractA systematic survey of phase formation in the Na2O-ZrO2-SiO2 system has revealed inconsistencies in the number and identity of ternary phases, and of their X-ray powder data. The phases Na2ZrSiO5, Na4Zr2Si3O12, Na2ZrSi2O7 and Na2ZrSi4O11 were prepared by solid-state reaction and their experimental X-ray diffraction patterns measured. Calculated X-ray diffraction patterns were generated by computer, using published crystallographic data, and critically compared with the experimentally observed values. The unit-cell constants were redefined to a greater accuracy than the presently accepted values published in the Powder Diffraction File. Only Na4Zr2Si3O12 produced an X-ray diffraction pattern which agreed with that previously published; those from the other phases were significantly different in both the intensities and positions of the reflections. Data for synthetic Na2ZrSi4O11 identical to the mineral vlasovite are reported.

Thermal and Structural Characterization of Nanocomposite Iron Nitride - Alumina and Iron Nitride - Silica Particles

2001 ◽  
Vol 703 ◽  
Author(s):  
Ann M. Viano ◽  
Sanjay R. Mishra
Keyword(s):  
Particle Size ◽  
Milling Time ◽  
Iron Nitride ◽  
X Ray Diffraction ◽  
X Ray ◽  
Thermal Peak ◽  
Transmission Electron ◽  
Diffraction Patterns ◽  
The One

ABSTRACTNanocomposite iron nitride based powders are known to have enhanced magnetic and other physical properties. To further explore their potential for application in various fields, we have performed a systematic study of the iron nitride - alumina and iron nitride - silica systems. Iron nitride powder of composition FexN (2 < x < 4), containing both Fe3N and Fe4N phases, was mechanically milled with Al2O3 or SiO2 powder for 4, 8, 16, 32, and 64 hours at the following compositions; (FexN)0.2(Al2O3)0.8, (FexN)0.6(Al2O3)0.4, (FexN)0.2(SiO2)0.8, and (FexN)0.6(SiO2)0.4. Differential thermal analysis and X-ray diffraction were performed to investigate thermal and structural transitions as a function of milling time. As the milling time is increased, the thermal peak corresponding to Fe4N is diminished, while the one corresponding to Fe3N is enhanced. These transitions are correlated with X-ray diffraction patterns. All XRD peaks broaden as a function of milling time, corresponding to smaller particle size. Transmission electron microscopy also reveals a decrease in particle size as the milling time in increased.

Characterization of Clay from Vale do Mulembá - ES

2008 ◽  
Vol 591-593 ◽  
pp. 487-492 ◽  
Author(s):  
Monica Castoldi Borlini Gadioli ◽  
J.C.G. Correia ◽  
A. Caranassios
Keyword(s):  
Particle Size ◽  
Chemical Analysis ◽  
Thermal Analyses ◽  
The Other ◽  
High Plasticity ◽  
X Ray Diffraction ◽  
X Ray ◽  
Characterization Studies ◽  
And Behavior

This work has for objective to characterize the clay from Vale do Mulembá-ES. The Vale do Mulembá is located in Joana D´Arc, Vitória in Espírito Santo State, Brazil. That clay is used in the production of the traditional clay pans of the State, what contributes to the economy of the area. The clay from Vale do Mulembá presents characteristics and behavior different from the other clays used for the production of clay pans. The characterization studies were carried out through chemical analysis, X-ray diffraction, particle size distribution, plasticity and thermal analyses (DTA, TGA). The results showed that the clay is typical kaolinitic, present relatively to the amount high of Al2O3 and high plasticity.

scholarly journals Reciprocal Powered Time model for Release Kinetic Analysis of Ibuprofen Solid Dispersions in Oleaster Powder, Microcrystalline Cellulose and Crospovidone

2010 ◽  
Vol 13 (2) ◽  
pp. 152 ◽  
Author(s):  
Ghobad Mohammadi ◽  
Mohammad Barzegar-Jalali ◽  
Hadi Valizadeh ◽  
Hossein Nazemiyeh ◽  
Azim Barzegar-Jalali ◽  
...  
Keyword(s):  
Particle Size ◽  
Drug Release ◽  
Solid Dispersions ◽  
Release Kinetic ◽  
X Ray Diffraction ◽  
X Ray ◽  
Ft Ir ◽  
Diffraction Patterns ◽  
Release Data ◽  
Dsc Thermograms

ABSTRACT- Purpose. A physically sound derivation for reciprocal power time (RPT) model for kinetic of drug release is given. In order to enhance ibuprofen dissolution, its solid dispersions (SDs) prepared by cogrinding technique using crospovidone (CP), microcrystalline cellulose (MC) and oleaster powder (OP) as a novel carrier and the model applied to the drug release data. Methods. The drug cogrounds with the carriers were prepared and subjected to the dissolution studies. For elucidation of observed in vitro differences, FT-IR spectroscopy, X-ray diffraction patterns, DSC thermograms and laser particle size measurement were conducted. Results. All drug release data fitted very well to newly derived RPT model. The efficiency of the carriers for dissolution enhancement was in the order of: CP>OP>MC. The corresponding release kinetic parameter derived from the model, t50% (time required for 50% dissolution) for the carrier to drug ratio 2:1 were 2.7, 10.2 and 12.6 min, respectively. The efficiency of novel carrier, OP, was between CP and MC. FT-IR showed no interaction between the carriers and drug. The DSC thermograms and X-ray diffraction patterns revealed a slight reduced crystallinty in the SDs. Also grinding reduced mean particle size of drug from 150.7 to 44.4 µm. Conclusion. An improved derivation for RPT model was provided which the parameter of the model, t50%, unlike to previous derivations was related to the most important property of the drug i.e. its solubility. The model described very well drug release kinetics from the solid dispersions. Cogrinding was an effective technique in enhancing dissolution rate of ibuprofen. Elaeagnus angostifolia fruit powder was suggested as a novel potential hydrophilic carrier in preparing solid dispersion of ibuprofen.

scholarly journals THERMAL BEHAVIOR OF PARACETAMOL AND TABLETS OF REFERENCE, GENÉRIC AND SIMILAR

2012 ◽  
Vol 09 (17) ◽  
pp. 28-37
Author(s):  
Francisca Edivânia MORAIS ◽  
Sheila Pricila Marques CABRAL ◽  
Eliane Gonçalves ARAUJO ◽  
Carlos Alberto MARTINEZ-HUITLE ◽  
Nedja Suely FERNANDES
Keyword(s):  
Particle Size ◽  
Thermal Behavior ◽  
Pharmaceutical Formulations ◽  
Endothermic Peak ◽  
X Ray Diffraction ◽  
X Ray ◽  
Thermoanalytical Techniques ◽  
Diffraction Patterns ◽  
Dsc Curves

The present study utilized the thermoanalytical techniques (TG, DTG, DTA and DSC) to evaluate the thermal behavior of tablets containing paracetamol and marketed as reference, generic and similar. The samples were also characterized by IR, X-ray diffraction and SEM. The TG/DTG curves presented similar behaviour indicanting a low influence of the excipients present in pharmaceutical formulations. The DTA and DSC curves showed an endothermic peak between about 165.0 and 195.0 oC characteristic of melting of paracetamol in all samples. The X-ray diffraction patterns showed similarities and characterized the compounds as crystallines. The micrographs indicated heterogeneity in particle size.

Untersuchungen zum Kristallisationsprozeß in Selenpreßkörpern

1972 ◽  
Vol 27 (7) ◽  
pp. 1124-1126
Author(s):  
J Kispéter ◽  
L Gombay ◽  
J Lang
Keyword(s):  
Particle Size ◽  
Spectral Dependence ◽  
Crystallization Rate ◽  
Trap Depth ◽  
X Ray Diffraction ◽  
Thermally Stimulated Current ◽  
X Ray ◽  
Diffraction Patterns

Abstract The crystallization of compressed selenium was investigated by measurements of the spectral dependence of the photocurrent and of the thermally stimulated current (TSC). A comparison of these results with X-ray diffraction patterns indicates that the maxima of the photocurrent and trap depth calculated from TSC measurements depend on changes in crystallization rate and in-crease in particle size

A method to eliminate the background in X-ray diffraction patterns of oriented clay mineral samples

Clay Minerals ◽  
1981 ◽  
Vol 16 (4) ◽  
pp. 383-393 ◽  
Author(s):  
S. J. Van Der Gaast ◽  
A. J. Vaars
Keyword(s):  
Clay Mineral ◽  
Quantitative Estimate ◽  
Considerable Increase ◽  
The Other ◽  
X Ray Diffraction ◽  
X Ray ◽  
Two Samples ◽  
Diffraction Patterns ◽  
Mineral Mixtures

AbstractA method is described for calculating, and then subtracting, the background from X-ray diffraction patterns of oriented clay mineral samples. Ti-Kα radiation is used and, to minimize the absorption of this radiation by air, a vacuum and helium-flushed device has been developed. This device can be used with other X-ray sources, offering a considerable increase of intensity—e.g. Co-Kα radiation is increased by 125%. With the background-eliminated patterns a better semi-quantitative estimate of the composition of clay mineral mixtures is possible. Small differences in composition of two samples can be identified by subtracting one of the background-eliminated patterns from the other. Using this method, peak maxima of smectite-group minerals can also be accurately determined.

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