Autor: Polláková, N. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: The content and profile distribution of carbon and nitrogen fractions susceptible to acid hydrolysis in Haplic Chernozems and Mollic Fluvisols of western Slovakia
Autorzy:: Jonczak, J.
Šimanský, V.
Polláková, N.
Powiązania:: https://bibliotekanauki.pl/articles/962617.pdf
Data publikacji:: 2017
Wydawca:: Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Opis:: The studies on the content and profile distribution of carbon and nitrogen fractions of varied susceptibility to acid hydrolysis were performed in arable Haplic Chernozems and Mollic Fluvisols at four locations near Krakovany, Slovakia. The soils were sampled every 10 cm and analyzed, including the content of total organic carbon (TOC) and nitrogen (TN) and fractions of these elements after sequential extraction in 0.25 mol dm-3 KCl, 0.25 mol dm-3 H2SO4 and 2.5 mol dm-3 H 2SO4. Based on extractions, the content of easy hydrolyzable (EHC), hardly hydrolyzable (HHC) and nonhydrolyzable carbon (NHC) and the content of ammonium nitrogen (NH4-N), nitrate nitrogen (NO3-N), dissolved organic nitrogen (DON), easy hydrolyzable nitrogen (EHN), hardly hydrolyzable nitrogen (HHN) and nonhydrolyzable nitrogen (NHN) was calculated. Mollic Fluvisols were more abundant in TOC and TN as compared to Haplic Chernozems. The content of carbon and nitrogen fractions varied among the soils, showing correlations with the total content of these elements. A low contribution of EHC and HHC in TOC and NO3-N, EHN, HHN in TN and a large share of nonhydrolyzable fractions of these elements were characteristic features of the studied soils. In general, trends in HHC (as % of TOC) and NO3-N, NH4-N, EHN (as % of TN), increasing with depth with a simultaneous decrease of NHN were observed. A-horizons of Haplic Chernozems were characterized by a higher contribution of EHN, NH4-N and NO3-N in TN, but a lower share of NHN as compared to Mollic Fluvisols.
Źródło:: Journal of Elementology; 2017, 22, 4
1644-2296
Pojawia się w:: Journal of Elementology
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Zawartość i profilowe rozmieszczenie frakcji fosforu w uprawnych i leśnych czarnoziemach z poziomem cambic
Content and profile distribution of phosphorus fractions in arable and forest Cambic Chernozems
Autorzy:: Jonczak, J.
Simansky, V.
Pollakova, N.
Powiązania:: https://bibliotekanauki.pl/articles/989926.pdf
Data publikacji:: 2015
Wydawca:: Polskie Towarzystwo Leśne
Tematy:: gleboznawstwo
gleby uprawne
gleby lesne
czarnoziemy
fosfor
zawartosc fosforu
frakcje fosforu
specjacja chemiczna
rozmieszczenie profilowe
chernozems
arable soils
forest soils
phosphorus speciation
Opis:: Comparative studies on the content and profile distribution patterns of phosphorus fractions in arable and forest Cambic Chernozems were conducted near the village Báb (western Slovakia). Soil samples were collected from every 10 cm and analyzed using standard procedures in soil science. Long term differences in the type of the studied soils usage were reflected in their physical and chemical properties (bulk density, porosity, acidity, the total content of organic carbon and nitrogen), as well as in the content and profile distribution patterns of phosphorus fractions. Total phosphorus content ranged from 498.8 to 754.7 mg/kg in arable soil and from 480.4 to 835.9 mg/kg in forest soil. Residual fraction, which constituted 54.9−77.8% of total phosphorus in arable soil and 57.3−79.2% in forest soil, was a predominant fraction. Such large contribution of this fraction is typical for young soils, with weakly weathered mineral substrates. Exchangeable phosphorus in arable soil constituted 0.6−6.1%, while 0.5−3.0% in forest soil, showing decreasing trends with depth in both soils. Free iron oxides and carbonates were important factors influencing profile distribution of phosphorus in the investigated soils. Iron oxides bound the element mainly in acidified horizons, whereas carbonates in alakaline (Bw and C) horizons. Organic fraction significantly differed in the investigated soils. A much larger content and contribution of this fraction in total phosphorus was noticed in forest soil. The content of organic phosphorus was positively related to the content of organic carbon. Stable fraction of organic phosphorus predominated over labile one in both soils.
Źródło:: Sylwan; 2015, 159, 11; 931-939
0039-7660
Pojawia się w:: Sylwan
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Effects of conventional and reduced tillage technologies on basic soil chemical properties
Autorzy:: Pollakova, N.
Simansky, V.
Jonczak, J.
Parzych, A.
Powiązania:: https://bibliotekanauki.pl/articles/1192039.pdf
Data publikacji:: 2020
Wydawca:: Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Tematy:: base saturation
hydrolytic acidity
pH
soil organic matter
tillage systems
Opis:: Since tillage technologies considerably influence soil properties and have a major impact on soil sustainability, the objective of this study was to evaluate the effects of conventional (CT) and reduced (RT) tillage on basic soil chemical properties at selected Slovak agricultural farms. Subsequently, the relationships between the chemical properties and soil organic matter (SOM) in both tillage technologies were ascertained. Differences in soil properties between long-term RT and CT were investigated at the adjacent plots on thirteen sites, where six soil pits were excavated on each RT and CT plots. Soil samples were collected from all pits, for each 0.1 m layers from the depth of 0.0-0.4 m. The results revealed that the regular overturn of topsoil, and thus the transfer of leached base cations to the surface layer, as well as deeper incorporation of crop residues and fertilizers in the soil cultivated conventionally has been manifested by higher values of pH, lower hydrolytic acidity (H) and the almost uniform content of base cations (mainly in the layer 0.0-0.3 m) compared to the soil cultivated by RT. Apart from H,, none of the examined sorption properties and pH differed significantly between the compared tillage technologies. Therefore, H can be considered as an important indicator of the change of basic chemical soil characteristics. While in RT, there was a significant correlation only between labile SOM fractions and basic soil chemical properties, in CT the sorption parameters and pH were influenced by labile and also stable SOM.
Źródło:: Journal of Elementology; 2020, 25, 3; 1101-1114
1644-2296
Pojawia się w:: Journal of Elementology
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Will the nutrient content in biochar be reflected by their higher content of corn organs?
Autorzy:: Simansky, V.
Horak, J.
Pollakova, N.
Juriga, M.
Jonczak, J.
Powiązania:: https://bibliotekanauki.pl/articles/14999.pdf
Data publikacji:: 2019
Wydawca:: Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Źródło:: Journal of Elementology; 2019, 24, 2
1644-2296
Pojawia się w:: Journal of Elementology
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:: Accumulation of heavy metals in needles and bark of Pinus species
Autorzy:: Parzych, A.
Mochnacky, S.
Sobisz, Z.
Kurhaluk, N.
Pollakova, N.
Powiązania:: https://bibliotekanauki.pl/articles/38440.pdf
Data publikacji:: 2017
Wydawca:: Instytut Badawczy Leśnictwa
Źródło:: Folia Forestalia Polonica. Series A . Forestry; 2017, 59, 1
0071-6677
Pojawia się w:: Folia Forestalia Polonica. Series A . Forestry
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: The Effect of Different Rates of Biochar and Biochar in Combination with N Fertilizer on the Parameters of Soil Organic Matter and Soil Structure
Autorzy:: Juriga, M.
Šimanský, V.
Horák, J.
Kondrlová, E.
Igaz, D.
Polláková, N.
Buchkina, N.
Balashov, E.
Powiązania:: https://bibliotekanauki.pl/articles/125202.pdf
Data publikacji:: 2018
Wydawca:: Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:: biochar
soil organic matter
soil structure
nitrogen fertilizer
Opis:: Since biochar is considered to be a significant source of carbon, in this work we have evaluated the changes in soil organic matter (SOM) and soil structure due to application of biochar and biochar with N fertilization, and have considered the interrelationships between the SOM parameters and the soil structure. The soil samples were collected from Haplic Luvisol at the locality of Dolná Malanta (Slovakia) during 2017. The field experiment included three rates of biochar application (B0 – no biochar, B10 – biochar at the rate of 10 t ha^-1, B20 – biochar at the rate of 20 t ha^-1) and three levels of N fertilization (N0 – no nitrogen, N160 – nitrogen at the rate of 160 kg ha^-1, N240 – nitrogen at the rate of 240 kg ha^-1). The rate of biochar at 20 t ha^-1 caused an increase in the organic carbon (C_org) content. The combination of both rates of biochar with 160 and 240 kg N ha^-1 also caused an increase in C_org. In the case of B20 the extractability of humic substances carbon (C_HS) was 17.79% lower than at B0. A significant drop was also observed in the values of the extraction of humic acids carbon (C_HA) and fulvic acids carbon (C_FA) after the addition of biochar at a dose of 20 t ha^-1 with 160 kg N ha^-1. However, both rates of biochar had a significant effect at 240 kg N ha^-1. After application of 20 t ha^-1 of biochar the content of water-stable macro-aggregates (WSA_ma) significantly increased compared to control. This rate of biochar also increased the mean weight diameter (MWD_W) and the index of water-stable aggregates (Sw) and decreased the coefficient of vulnerability (Kv). The biochar at a rate of 20 t ha^-1 with 240 kg N ha^-1 the value of MWD_W increased and value of Kv decreased significantly. The contents of C_org and C_L correlated positively with WSA_ma, MWD_W and Sw and negatively with WSA_mi and Kv. The extraction of C_HA and C_FA was in negative relationship with MWD_W. We conclude that the application of biochar and biochar combined with N fertilizer had a positive influence on SOM and soil structure.
Źródło:: Journal of Ecological Engineering; 2018, 19, 6; 153-161
2299-8993
Pojawia się w:: Journal of Ecological Engineering
Dostawca treści:: Biblioteka Nauki

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