Study of the fragment composition of humic acids of different origin using IR-EXPERT software

2012 ◽  
Vol 68 (1) ◽  
pp. 86-94 ◽  
Author(s):  
V. D. Tikhova ◽  
T. F. Bogdanova ◽  
V. P. Fadeeva ◽  
V. N. Piottukh-Peletsky
Author(s):  
Jānis Šīre ◽  
Māris Kļaviņš

Influence of the humification process on the properties of peat humic acids Comparative and complex characterisation of peat humic acids (HAs) isolated from peat profiles of different origin in Latvia was conducted. Elemental and functional analysis of the isolated HAs was made and their acidity and molecular weight were estimated. Spectral characterisation included UV-Vis, IR, electron spin resonance and fluorescence spectra. Structural characterisation of HAs was by both 1H and13C nuclear magnetic resonance spectra. Properties of HAs isolated from the Latvian peat were compared with HA from other sources (soil, water, coal and synthetic humic substances). Major properties of peat HAs depended on their origin, indicating the importance of humification processes. HAs isolated from peat of more recent origin were more similar to soil Has, while there was a greater degree of humification in part from older sources.


2014 ◽  
Vol 87 (8) ◽  
pp. 1070-1076 ◽  
Author(s):  
E. V. Maltseva ◽  
A. V. Savel’eva ◽  
A. A. Ivanov ◽  
N. V. Yudina ◽  
O. I. Lomovskii

Chemosphere ◽  
1999 ◽  
Vol 39 (2) ◽  
pp. 183-198 ◽  
Author(s):  
V. D'Orazio ◽  
E. Loffredo ◽  
G. Brunetti ◽  
N. Senesi
Keyword(s):  

2009 ◽  
Vol 43 (7) ◽  
pp. 418-421 ◽  
Author(s):  
M. V. Gostishcheva ◽  
M. V. Belousov ◽  
M. S. Yusubov ◽  
R. R. Ismatova ◽  
S. E. Dmitruk

2016 ◽  
Vol 50 (2) ◽  
pp. 133-139
Author(s):  
T. A. Yarkova ◽  
A. M. Gyul’maliev
Keyword(s):  

1991 ◽  
Vol 52-53 (1) ◽  
Author(s):  
J. I. Kim ◽  
D. S. Rhee ◽  
G. Buckau
Keyword(s):  

2020 ◽  
pp. 15-27

In order to study the effect of phosphogypsum and humic acids in the kinetic release of salt from salt-affected soil, a laboratory experiment was conducted in which columns made from solid polyethylene were 60.0 cm high and 7.1 cm in diameter. The columns were filled with soil so that the depth of the soil was 30 cm inside the column, the experiment included two factors, the first factor was phosphogypsum and was added at levels 0, 5, 10 and 15 tons ha-1 and the second-factor humic acids were added at levels 0, 50, 100 and 150 kg ha-1 by mixing them with the first 5 cm of column soil and one repeater per treatment. The continuous leaching method was used by using an electrolytic well water 2.72 dS m-1. Collect the leachate daily and continue the leaching process until the arrival of the electrical conductivity of the filtration of leaching up to 3-5 dS m-1. The electrical conductivity and the concentration of positive dissolved ions (Ca, Mg, Na) were estimated in leachate and the sodium adsorption ratio (SAR) was calculated. The results showed that the best equation for describing release kinetics of the salts and sodium adsorption ratio in soil over time is the diffusion equation. Increasing the level of addition of phosphogypsum and humic acids increased the constant release velocity (K) of salts and the sodium adsorption ratio. The interaction between phosphogypsum and humic acids was also affected by the constant release velocity of salts and the sodium adsorption ratio. The constant release velocity (K) of the salts and the sodium adsorption ratio at any level of addition of phosphogypsum increased with the addition of humic acids. The highest salts release rate was 216.57 in PG3HA3, while the lowest rate was 149.48 in PG0HA0. The highest release rate of sodium adsorption ratio was 206.09 in PG3HA3, while the lowest rate was 117.23 in PG0HA0.


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