RESEARCH FOR
RESEARCH FOR
RESEARCH FOR
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Andrius Litvinaitis,<br />
Lina Bagdžiūnaitė-Litvinaitienė<br />
period of time due to denitrification (Denver et al.,<br />
2009).<br />
While migrating, nitrogen compounds can pollute<br />
larger water bodies (Bagdžiūnaitė-Litvinaitienė, 2005;<br />
Lebedynets et al., 2005), thus explicit regulation on<br />
use and storage of nitrogen is defined in the areas of<br />
agriculture and environmental protection.<br />
This research aims to ascertain consistent patterns<br />
in migration of biogenic substances within the aeration<br />
zone of sand sediments in banks of Lithuanian rivers.<br />
materials and methods<br />
Two sandy river banks of basins with typical<br />
sand lithology structure were chosen for the research<br />
(Fig. 1). These two basins were chosen subsequently<br />
for analysis of lithology structures of 17 basins<br />
of Lithuanian rivers (Litvinaitis, 2010; 2011a).<br />
The lithologic factor of basins was estimated and<br />
ReseaRch foR RuRal Development 2012<br />
<strong>RESEARCH</strong> OF NUTRIENTS MIGRATION OF SANDY<br />
SEDIMENT AERATION ZONE OF THE RIVER BANK BUFFER AREA<br />
Figure 1. Basins of studied rivers.<br />
research sites were chosen with the help of maps of<br />
Lithuanian Quaternary and rivers (M1:50000) and<br />
ArcGis software. Later, research sites were specified<br />
according to data of core samples taken from river<br />
banks.<br />
The authors state that the main migration of<br />
nitrogen and phosphorus occurs by water, which<br />
filters through sediments; meanwhile transformations<br />
depend on the amount of oxygen and acidity within<br />
the environment. All these parameters can be assessed<br />
in a borehole. The lysimetric type of a borehole was<br />
chosen for the empiric groundwater level and quality<br />
analyses. This choice was influenced by the following<br />
reasons:<br />
1) during the installation process, the deformation<br />
of the natural status of sediments and<br />
underground water is minimal;<br />
Figure 2. Situation of lysimetric boreholes on the bank of the river.<br />
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