2022
DOI: 10.3390/agriculture12040488
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Changes in Organic Carbon in Mineral Topsoil of a Formerly Cultivated Arenosol under Different Land Uses in Lithuania

Abstract: This study aims to determine the differences in the organic carbon, humic acid (HA), and fulvic acid (FA) concentrations in the A and AB horizons, depending on land use, in order to determine the influence of the land use on the soil organic carbon (SOC) sequestration rate in the A horizon, and to assess the impact of the land use on the quality of the humic substances (HS) (the humification rate (HR) and the HA/FA ratio). On the basis of the data of 1995–2018, it would be expedient to convert cropland (CL) ar… Show more

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Cited by 9 publications
(4 citation statements)
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“…The carbon-to-nitrogen ratio (C/N) in 1995 ranged from 12.5 to 13.6, and this was favourable for the transformation of the organic matter in the soil. For the long-term experiment, the experimental land use changes and experimental design are described in more detail in [31].…”
Section: Study Object and Experimental Sitementioning
confidence: 99%
“…The carbon-to-nitrogen ratio (C/N) in 1995 ranged from 12.5 to 13.6, and this was favourable for the transformation of the organic matter in the soil. For the long-term experiment, the experimental land use changes and experimental design are described in more detail in [31].…”
Section: Study Object and Experimental Sitementioning
confidence: 99%
“…In the previous studies regarding the occurrence of humic acids in the environment, the environmentally relevant concentration ranged from ∼0.1 to 1970 mg L −1 . [54][55][56] Therefore, 100 mg L −1 of humic acids is still environmentally relevant concentration and it may act as an inhibition factor of SGaptasensor applications to environmental samples.…”
Section: Environmental Inhibitorsmentioning
confidence: 99%
“…During the long-term experiment, various biological and agroecological properties were analysed separately [27]. At the beginning of the experiment, the pHKCl of the humus layer ranged from 6.0 to 6.8, SOC was between 9.5 and 9.9 g kg −1 , and there was 157-188 mg P2O5 kg −1 and 170-194 mg K2O kg −1 .…”
Section: Study Area and Soil Samplingmentioning
confidence: 99%