Cobalt(II) cation extraction from solutions containing ethylenediaminetetraacetate and oxalate ions

Atomic Energy ◽  
2011 ◽  
Vol 110 (5) ◽  
pp. 347-351 ◽  
Author(s):  
E. P. Lokshin ◽  
V. I. Ivanenko ◽  
R. I. Korneikov
Author(s):  
Elena Yusenko ◽  
Evgeniya Polyntseva ◽  
Anna Lyzhova ◽  
Olga Kalyakina

Abstract Oxalate concentration differs in various daily consumed food products. The role of oxalic acid in the human body is very significant, as its compounds are responsible for the stability of biological membranes. However, insoluble calcium and magnesium oxalates can be accumulated in the body in the form of kidney stones. Oxalate concentration has been measured by high performance liquid, gas after derivatization and ion chromatography (IC). The most effective method for the simultaneous determination of oxalate and inorganic anions is ion chromatography with conductometric detection. Here, we report the results of the measurement of oxalic acid in bleak and green tea samples. Separation was performed by IC on an anion-exchange column Shodex IC SI-90 with surface-layer sorbent and conductimetric detection. The main analytical features of the method were: limit of detection of oxalic acid 0.03 mg/l, linear range 0.1-20 mg/l, correlation 0.9998, relative standard deviation 1%. The method did not need specific sample treatment and was successfully applied to the analysis of black and green tea samples. Oxalic acid was determined in the ranges 16.7-84 mg/l for green tea and 63-116 mg/l for black tea. Green tea contained lower oxalate ions concentration than black tea. The IC method has a lower detection limit for oxalate ions than HPLS and GC, ten and two times less, respectively


2016 ◽  
Vol 5 (2) ◽  
pp. 144
Author(s):  
Doungmo Giscard ◽  
Théophile Kamgaing ◽  
Ranil Clément Tonleu Temgoua ◽  
Ervice Ymele ◽  
Francis Merlin Melataguia Tchieno ◽  
...  

In this study, sorption properties of a synthesized anionic clay were enhanced by the intercalation of oxalate ions in its interlayer space. The pristine and modified clay materials were characterized by X-ray diffraction, Fourier transform infrared spectroscopy and thermal analysis. These techniques confirmed the presence of oxalate ions in the interlayer space of the clay. The intercalated clay was then used as a matrix for the sorption in batch mode of nickel ions in aqueous solution. The influence of a number of parameters such as contact time, pH, initial concentration of the analyte and adsorbent dosage were studied. The maximum adsorption of nickel was obtained at pH 6, that is, about 90% Ni2+ removal. The adsorbent/adsorbate equilibrium follows a pseudo-second order kinetics and best matches the Langmuir model. The modified clay was shown to be efficient matrix for the sorption of nickel ions.


1956 ◽  
Vol 34 (2) ◽  
pp. 170-178 ◽  
Author(s):  
K. Ito ◽  
H. J. Bernstein

The infrared spectra of the formate, acetate, and oxalate ions have been obtained for both the solid and aqueous solution. The Raman spectra of these ions with depolarization ratios have been obtained in aqueous solution. Vibrational assignments have been made which differ slightly for the acetate ion and more markedly for the oxalate ion from earlier work. The depolarization ratios confirm Fonteyne’s assignment for the formate ion.


1968 ◽  
Vol 33 (5) ◽  
pp. 493-498 ◽  
Author(s):  
ALI A. MOHAMMADZADEH-KHAYAT ◽  
B. S. LUH
Keyword(s):  

2014 ◽  
Vol 70 (8) ◽  
pp. o852-o852 ◽  
Author(s):  
Błażej Dziuk ◽  
Bartosz Zarychta ◽  
Krzysztof Ejsmont

In the title hydrated molecular salt, C3H8N+·C2HO4−·0.5H2O, the water O atom lies on a crystallographic twofold axis. The C=C—C—N torsion angle in the cation is 2.8 (3)° and the dihedral angle between the CO2and CO2H planes in the anion is 1.0 (4)°. In the crystal, the hydrogen oxalate ions are linked by O—H...O hydrogen bonds, generating [010] chains. The allylammonium cations bond to the chains through N—H...O and N—H...(O,O) hydrogen bonds. The water molecule accepts two N—H...O hydrogen bonds and makes two O—H...O hydrogen bonds. Together, the hydrogen bonds generate (100) sheets.


2011 ◽  
Vol 50 (12R) ◽  
pp. 125802
Author(s):  
Ayako Omura ◽  
Yutaro Kurihara ◽  
Tomoyuki Matsuda ◽  
Hajime Tanida ◽  
Tomoya Uruga ◽  
...  

2002 ◽  
Vol 43 (42) ◽  
pp. 7627-7629 ◽  
Author(s):  
Viktor Csokai ◽  
Alajos Grün ◽  
Gyula Parlagh ◽  
István Bitter

2006 ◽  
Vol 62 (4) ◽  
pp. o1524-o1525 ◽  
Author(s):  
Mustafa Odabaşoğlu ◽  
Orhan Büyükgüngör

The title compound, C6H18N2O2 2+·C2O4 2−, crystallizes with one half-cation and one half-anion in the asymmetric unit. It contains cyclic N—H...O hydrogen-bonded rings involving 3,6-dioxaoctane-1,8-diammonium and oxalate ions, forming a three-dimensional network.


1995 ◽  
Vol 73 (S1) ◽  
pp. 1384-1390 ◽  
Author(s):  
P. Hirsch ◽  
F. E. W. Eckhardt ◽  
R. J. Palmer Jr.

Fungal colonization of sandstone and granite from Antarctica was studied. Granite from a church, sandstones from a monument and a courthouse in Germany, glazed bricks from a German cathedral, and some other stone types were also examined. All samples contained fungi and heterotrophic bacteria, often also cyanobacteria or algae. For cell counting and enrichment of microorganisms the samples were crushed aseptically, suspended in NaCl–Tween-80, plated on oligotrophic media, and incubated at 16–25 °C dark or in dim light. Total biomass was determined as phospholipid-bound phosphate (PLP). Rock samples were also viewed by electron microscopy. Typical viable fungal cell numbers (CFU∙g−1 dry weight) were the following: sandstone 1.6 × 104, granite 6.2 × 105, and glazed bricks 1.2 × 105. Total biomass ranged from 41 (sandstone) to 137 (glaze) nmol PLP∙g−1 dry weight; antarctic sandstone had 88 nmol PLP∙g−1. Fungal genera identified were the following: Alternaria, Aspergillus, Aureobasidium, Candida, Cladosporium, Paecilomyces, Phoma, Penicillium, and Sporobolomyces. Scanning electron microscopy revealed fungal bridging of open spaces with their hyphae or close contact between fungal hyphae and coccal cells believed to be algae. In some cases fungi were found to produce secondary minerals or their hyphae were covered with partially etched mineral layers. Exopolymer formation was common among the endolithic microorganisms. Mites were found to feed on epiliths. In pure culture, fungi from sandstone produced in 24 h cultures organic acids (citrate, glutamate, pyruvate, malate, succinate, lactate, formate, fumarate, and oxalate). Many of these acids could also be extracted from rock samples. Fungal growth on glucose and mineral powder resulted in up to 60% cation extraction from the mineral. Some fungi were antibiotically active against bacteria or yeasts but also stimulated other bacterial isolates. In summary, epi- and endo-lithic communities contained fungi that probably contribute substantially to the deterioration of many stones and monuments. Key words: rock weathering, biomass, acid excretion, cation extraction.


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