Temat: Odra - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: System for flood protection in Odra River basin - its efficiency during the flood of 1997
Autorzy:: Radczuk, L.
Dubicki, A.
Olearczyk, D.
Powiązania:: https://bibliotekanauki.pl/articles/25214.pdf
Data publikacji:: 1998
Wydawca:: Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:: topographical condition
Polska
flood protection
geological condition
hydrographic condition
Odra River
Źródło:: International Agrophysics; 1998, 12, 4
0236-8722
Pojawia się w:: International Agrophysics
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Odra 1997 flood effects on soil properties of cultivated areas in Germany
Autorzy:: Eulenstein, F.
Muller, L.
Helming, K.
Powiązania:: https://bibliotekanauki.pl/articles/26179.pdf
Data publikacji:: 1998
Wydawca:: Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:: flood effect
denitrification
soil fertility
concentration
Germany
cultivated area
soil property
Odra River
heavy metal
Źródło:: International Agrophysics; 1998, 12, 4
0236-8722
Pojawia się w:: International Agrophysics
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Effect of soil inundation on its properties in the Region of Swiecko during summer flooding
Autorzy:: Drzymala, S
Spychalski, W.
Rybczynski, P.
Powiązania:: https://bibliotekanauki.pl/articles/1401878.pdf
Data publikacji:: 2000
Wydawca:: Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:: flood
agricultural land
Fluvisol
Polska
Swiecko Region
disaster flood
summer flood
soil property
soil inundation
Odra River
heavy metal
Opis:: The present experiments were earned out pn the soilrf of the Rybocice polder near Swiecko, which was purposefully flooded with waters of the Odra river during the summer flood of' 1977 that causet complete destruction of crops and meadow sward. The flooded areas remained under water for more than 30 days. The dominant soils found in this area are river alluvial soils (Fluvi- sols) of varying texture. Rceause of their location and poorly operating drainage system, the discussed soils are periodically too wet by nature or water-logged. In the spring (March/April) of 1998 the ground water table occurred at the depth of 30 cm on damaged grasslands and at 90 cm on some arable Holds. The content of organic carbon ranged from 0.7 to 3.2% in horizon A with depth of approximately 30 cm. Soil reaction was found to vary considerably - from pH (KCI) 4.2 to pH 7.6. Long purposeful inundation with flood waters was not found to have caused significant negative effects on chemical properties of the examined soils. No noticeable contamination with heavy metals (Pb„ Cu, Zn, Cd, Cr and Mn) or polieyclic aromatic hydrocarbons (PAH) was observed. Bulk density in this region, without any treatment from the period of flooding to the spring of 1998 was approximately 1.60 Mg/m3 as compared with 1.40 Mg/m3 on the field cultivated (ploughed) in spring and sown with spring cereal. The mean crop yield in 1998, when appropriate agro-techniques were applied, did not vary significantly from the long-term averages.
Źródło:: Acta Agrophysica; 2000, 35; 61-67
1234-4125
Pojawia się w:: Acta Agrophysica
Dostawca treści:: Biblioteka Nauki

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