
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/">
  <dc:source>Agriculture 108(2)</dc:source>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:format>application/pdf</dc:format>
  <dc:format>698293 bytes</dc:format>
  <dc:language>eng</dc:language>
  <dc:description xml:lang="eng">Abstract: The results of 8-variable column experiment on a strongly acidic sod-podzolic sandy loam reclaimed by the finely  ground dolomite in a wide dose range are presented. The aim of the research was to measure and estimate leaching  of magnesium (Mg) and its migration pattern. The dolomite powder at the different doses calculated by hydrolytic  acidity (Hy) was applied at 225, 337.5, 450, 675, 900, 1350 and 1800 mg, that corresponded to 0.5, 0.75, 1.0, 1.5,  2.0, 3.0 and 4.0 Hy, respectively. The migratory ability of Mg was studied in 12-times washing column experiment.  Each washing was carried out by 400 ml distilled water, simulating the volume of annual precipitation percolating  through the soil stratum yearly. The increase in the amount of leaked moisture contributed to the enhancement of  the eluvial losses of Mg. The maximum loss of Mg due to migration was established in the filtrates of the first  washing. As the dose of dolomite increased, the amount of the soil Mg migrating with the total amount of Mg  decreased from 27% to 7.5%. Complete removal of water-soluble Mg from the soil was not achieved in any of the  studied treatments. Applied empirical estimations correctly described the process of leaching of Mg during repeated  washing of the soil. Based on the data on the amount of leached Mg from soil reclaimed by a wide range of dolomite  doses, a clustering of the empirical equations was performed. It was shown that in the 1st stage of the experiment  (from 1 to 4 washings) the rate of Mg leaching increased significantly with an increase in the dose of the dolomite.  In the 2nd stage (4 to 12 washings) such a pattern was not established. Depending on the dolomite dose applied, the  losses of Mg increased from 14.05 to 50.6 mg compared to 3.8 mg in the non limed (control) treatment.  The main finding is that finely ground dolomite in an amount exceeding a full dose calculated by 1 Hy applied to  sod-podzolic forest soil resulted in unproductive losses of Mg, i.e., with increasing dolomite dose, the losses of  Mg increased.</dc:description>
  <dc:date>2021</dc:date>
  <dc:subject xml:lang="eng">clustering, empirical estimations, leaching rate, magnesium, migration.</dc:subject>
  <dc:title xml:lang="eng">Magnesium leaching processes from sod-podzolic sandy loam  reclaimed by increasing doses of finely ground dolomite</dc:title>
  <dc:identifier>https://unilib.phaidrabg.rs/o:717</dc:identifier>
  <dc:identifier>doi:10.13080/z-a.2021.108.014</dc:identifier>
  <dc:rights>All rights reserved</dc:rights>
  <dc:creator>Litvinovich, Andrey</dc:creator>
  <dc:creator>Pavlova, Olga</dc:creator>
  <dc:creator>Lavrishchev, Anton</dc:creator>
  <dc:creator>Bure, Vladimir</dc:creator>
  <dc:creator id="https://orcid.org/0000-0002-6497-2066">Saljnikov, Elmira</dc:creator>
</oai_dc:dc>
