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Wyszukujesz frazę "ionic ratios" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Effect of Guano Fertilisation on Yield and Some Quality Traits of Perennial Ryegrass Biomass
Autorzy:
Możdżer, Ewa
Tematy:
guano
lolium perenne
yield
contenet macroelement
ionic ratios
correlation
Pokaż więcej
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Powiązania:
https://bibliotekanauki.pl/articles/59114316.pdf  Link otwiera się w nowym oknie
Opis:
Due to the lack of conclusive articles on the effect of guano, which is classified as a natural fertiliser, an experiment was conducted to evaluate its effect on the yield and quality of perennial ryegrass of the Rela variety. The guano used in the experiment contained significant concentrations in g·kg-1 DM of nitrogen (23.1), phosphorus (9.52) and magnesium (2.90). The concentration of heavy metals did not exceed the applicable standards in organic fertilisers. The total content of N and P in guano was higher relative to K, and Mg and Ca were similar. The concentration of N and Mg in guano is comparable to the content of these elements in poultry manure. The guano reaction was slightly acidic (5.86). The fertiliser value of guano was assessed in a vegetation-weed two-factor experiment. The test scheme included control, guano and guano with ammonium nitrate applied at three doses. The dry biomass yield of perennial ryegrass from individual cuts varied considerably. The objects with applied guano and guano with ammonium nitrate increased the average yield of perennial ryegrass from cut 1 by 102.9% compared to the control object. Applied guano fertilisation significantly increased the sum of perennial ryegrass yield from three cuts. As a result of the applied fertilisation, there was an increase in N, P and Ca content in perennial ryegrass, while K and Mg content increased to a negligible extent and thus contributed to optimal ionic ratios of Ca:P and K:(Ca+Mg). In contrast, the ionic ratio K:Mg deviated significantly from the optimal values for plants. The application of guano and guano with ammonium nitrate influenced the positive correlation between N and Ca content and the obtained yield of perennial ryegrass.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrogeological settings and origin of groundwater composition in the southern part of the Gorce Mts, Kowaniec Mały catchment
Autorzy:
Żaczek, J.
Porowski, A.
Tematy:
groundwater chemical composition
groundwater origin
ionic ratios
water-rock interaction
recognition of source rocks
Pokaż więcej
Wydawca:
Polskie Towarzystwo Geologiczne
Powiązania:
https://bibliotekanauki.pl/articles/191405.pdf  Link otwiera się w nowym oknie
Opis:
The Gorce Mts of southern Poland occur in a natural upland area that is viewed as valuable and is protected. It has an inadequate and irregular network of long-term monitoring points at the national level with regard to groundwater quality and vulnerability to contamination. The paper discusses the results of an investigation of groundwater in the Kowaniec Mały drainage basin, in the southern part of the Gorce Massif. It provides new hydrogeochemical data that shed light on the origin and evolution of groundwater chemistry in this region. On the basis of a hydrogeological survey of 33 natural springs, trends in the spatial and temporal variation of the physicochemical properties of the groundwater are presented. Three hydrochemical types of water were distinguished, namely HCO3-Ca, HCO3-Ca-Mg and HCO3-SO4-Ca. The detailed analysis of ionic ratios shows that the dissolution of carbonates (mainly calcite) and aluminosilicates (mainly albite) played a fundamental role in the formation of the chemical composition of the groundwater in the study area. These processes are responsible for the presence of the dominant ions, such as HCO3- and Ca2+, as well as SiO2 and in part Na+ and K+. Chloride–sodium mineralization is connected first of all with recharge by rain water and the direct dissolution of halite, contained in the aquifer rocks or formed during the evaporation of the water. The most probable sources of dissolved SO42- are the atmospheric sulphates contained in recharge meteoric waters in the case of springs located at higher altitudes and the reduced inorganic sulphur compounds dispersed in fine-grained sedimentary rocks, mostly as pyrite, which undergoes oxidation during rock weathering. Ion exchange processes involving clay minerals also were present and affected mainly the concentrations of Na+ + K+ and Ca2+.
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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