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2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures

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Chem. Listy, 102, s265–s1311 (2008) Environmental Chemistry & Technology<br />

nutrient transport assessment from soils to surface<br />

water was studied through transport of dissolved and adsorbed<br />

forms of n and P.<br />

Table II<br />

Concentration of n and P in SWB sediments<br />

Sample n tot [%] P tot [%]<br />

S1 0.26 0.112<br />

S1’ (100 %) 0.26 0.112<br />

S2 0.24 0.113<br />

S2’ (97.65 %) 0.24 0.110<br />

S3 0.22 0.066<br />

S4 0.23 0.066<br />

S5 0.24 0.112<br />

S5’ (89.24 %) 0.25 0.115<br />

S6 0.20 0.090<br />

S7 0.17 0.049<br />

S8 0.14 0.070<br />

Fig. <strong>2.</strong> Influence of sampling distance from the dyke on the N<br />

and P sediment concentration<br />

For determining nutrient concentrations in dissolved<br />

phase several leaching experiments were realized. Expe-<br />

s398<br />

riment results have shown that portion of dissolved phase<br />

represented 0.46–0.65 % of total P and 0.37–0.46 % of total n<br />

in the soil sample. According these findings, dissolved phase<br />

weren’t considered.<br />

As follows from Table I, nitrogen concentrations in<br />

adsorbed phase of soils varied from 0.08 % to 0.23 % and<br />

phosphorus concentrations were in range 0.054 % to 0.082 %.<br />

It depends on rates and date of fertilizer application and also<br />

on type of grown crop and its uptake rates (samples P1–P4<br />

before and P5–P8 after nitrogenous fertilizer application).<br />

Conclusions<br />

The concentration of nutrients in studied soil samples<br />

wasn’t influenced by their granularity and depends on the<br />

applicable fertilizer rates and grown plant uptake.<br />

The results from chemical analyses confirmed the literary<br />

information that the concentrations of P, n in chosen<br />

sediment samples are diverse due to irregular sediment deposition<br />

in the reservoir and increase with proportion of the<br />

finest particle fraction.Concentrations of P, n in sediments<br />

correspond to their concentrations in soils what is in accord<br />

with our results about their maximal portion in adsorbed<br />

phase.<br />

This work has been supported by the Slovak Grant<br />

Agency for Science (Grant No. 1/0613/08).<br />

REFEREnCES<br />

1. Bálintová M., Kovaliková n.: Sel. Sci. Pap. 1, 189<br />

(2005).<br />

<strong>2.</strong> Mahler R. L., Tindall T. A.: Coop. Ext. Bull.1997, 704<br />

3. Methodological instruction of Ministry of environment<br />

SR no. 549/98-2<br />

4. Kovaliková n., Bálintová M.: Acta Facultatis Ecologiae<br />

16, 129 (2007).

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