2018
DOI: 10.7251/afts.2018.1018.063r
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Humic Acids Optical Properties of Rendzina Soils in Diverse Environmental Conditions of Serbia

Abstract: This study examined the impact of climate, altitude and landforms on humic acids (HA) opticalproperties (E4/E6, ΔlogK, RF indexes) in Serbian Rendzina soils. HA humification degree of calcareousand decarbonated Rendzinas under natural vegetation (forest and grassland, separately) decreased withaltitude increasing. This particular rule was not manifested in arable Rendzinas. HA humificationdegree in Rendzinas on flat positions (hilltop and footslope) is significantly higher than in Rendzinas onslope sides. Humi… Show more

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Cited by 4 publications
(3 citation statements)
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“…Susmel's formulas were constructed on the basis of measurements in Italian relict nuclei and primary (virgin) forests in Croatia [94,[128][129][130][131]. In the spirit of Susmel they should serve as a potential ecological model for Italian alpine forests.…”
Section: Examples In Alpine Environmentmentioning
confidence: 99%
“…Susmel's formulas were constructed on the basis of measurements in Italian relict nuclei and primary (virgin) forests in Croatia [94,[128][129][130][131]. In the spirit of Susmel they should serve as a potential ecological model for Italian alpine forests.…”
Section: Examples In Alpine Environmentmentioning
confidence: 99%
“…The UV-Vis spectroscopy method makes it possible to conduct qualitative assessment of HA humification degree with estimated coefficients ∆logK and E 4 /E 6 [16,40]. Maxima of absorption of key aromatic structures in HA (lignin, phenol fragments, aromatic amino acids) were observed in the wavelength range of 260-280 nm, while in the 400-465 nm region a change in the HA absorption curve was obvious [41,42]. E 270 , E 465 coefficients indicated a gradual increase in molecular complexity of HAs from permafrost layers as compared to HAs of STL of the peatlands under study.…”
Section: Elemental Composition and Optical Properties Of Hasmentioning
confidence: 99%
“…Lighter fractions possibly may have been recently It is important to note that from the depth of 100 cm (Plots 1-1 and 1-2) a gradual increase in the ash content of soil samples was observed, from 40 to 90% in the lower part of the profile. According to the data [42], ash elements can lead to neutralization and weak polymerization of HA molecules. The increase in number-average HA molecular weight in the permafrost was likely to be caused by coagulation of HAs on the mineral matrix of peat deposits with the formation of high molecular weight HAs.…”
Section: Molecular Weight Distribution Of Hasmentioning
confidence: 99%