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The verification of the concept “Facing the critical value challenge” has been performed on 9 arable fields of an agricultural farm (52 ha) located in the village Kujawki (Golancz District, Wielkopolska Region, Poland). In total, 99 soil samples were collected at the depth 0-20 cm from 9 fields. Basic properties were determined, i.e., soil particle distribution, organic carbon, pH (in 0.01 moles CaCl2 dm–3), cation exchange capacity (CEC). Moreover, Cu, Zn, Fe and Mn were extracted by 6 moles HCl dm–3 (pseudo total forms) and 0.005 moles DTPA, pH 7.3 (active and potentially mobile forms). Plant material (99 samples) was collected from winter triticale, winter wheat, winter barley, grass mixtures, winter oilseed rape and sugar beet at respective growth stages, dried, ground and analysed for Zn. The elaboration of soil (Zn-DTPA) and plant (Zn-Plant) critical values proceeded in two steps, i) tabular interpretation of data through adjustment to critical values in literature, ii) graphical readaptation of the C-Shaped, i.e. Piper-Steenbjerg curve. The results revealed that the amounts of Zn-DTPA varied in a wide range, from 0.80 to 4.30 mg kg–1, but its overall share in total Zn fluctuated from 2.0 to 7.9%. This implies that the geoavailability of zinc compounds seems to be relatively high. The relationship established for the pairs Zn-Total versus Zn-DTPA (YZn-DTPA = 0.092Zn-Total – 2.00; R2 = 0.63) yielded a significantly high coefficient of determination as a proof of the importance of Zn-Total in controlling the Zn-DTPA pool. The critical Zn-DTPA range varied from 0.80 to 1.43 mg kg–1 with a mean value of ca 1.08 mg kg–1, reflecting 67% of all investigated sites. The readapted C-Shaped, i.e. Piper-Steenbjerg curve (Zn-Plant versus Zn-DTPA) allowed establishing a critical Zn-Plant content at 15.3-39.7 mg kg–1 for the investigated crop plants. The mean critical value reached 33.3 mg kg–1 and divided plants into two groups, i) experiencing deficiency: winter wheat, winter oilseed rape, sugar beet and grass mixtures and ii) not experiencing deficiency: winter triticale, winter barley and winter wheat. These findings give a new insight into the urgent need for elaborating critical values for a wide range of crop plants in use in Poland.
Eight soils were studied for adsorption reactions of zinc and evaluated for their quantity, intensity and supply parameters for zinc. With the addition of increasing amounts of zinc there was a simultaneous increase in the equilibrium concentration, adsorption, percent saturation of adsorption capacity and supply parameter of zinc. Multiple regression analysis revealed that in all soils quantity, intensity and equilibrium concentration were the main parameters accounting for the supply of zinc. Sandy loam, loamy and loamy sand soils having comparatively higher values for the adsorption maxima, bonding energy constant and differential buffering capacity of the soils will require higher rates of zinc to change in the solution concentration.
The paper outlines a concept related to selecting a site for experimental purposes. Selection of an experimental plot most frequently relies on performing visual evaluation of a given site, followed by the establishment of a field trial. In general, the question of geochemical variability is ‘intentionally’ postponed! Verification of this approach has been undertaken, testing such parameters as soil pH and exchangeable aluminum (Alex) versus spatial (investigated area, 12 672 m2) and downward (sampling depths, i.e., 0-20, 20-40 and 40-60 cm) distribution. Winter wheat biomass at tillering (BBCH29) and grain yield at harvest (BBCH99) were additionally considered. The results have revealed that pH values fluctuated between 3.6 and 4.4 with respective coefficients of variation (CV) ranging from 3.10 to 5.92%. The concentrations of Alex ranged from 38.0 to 144.9 mg kg–1, corresponding to CV within 28.34 and 44.03%. The variograms and geostatistical maps have demonstrated the spatial as well as downward variability of these parameters. The spatial distribution of plant biomass followed quite closely the exchangeable aluminum (Alex) levels, which implies that natural soil parameters such as Alex are not easily compensated for by agricultural practices, for instance nitrogen application. The spatial grain yield – Alex dependence which emerged at harvest confirmed the variability observed at tillering (BBCH29). Thus, the spatial variability of pH, Alex and wheat biomass as well as grain yields (BBCH99) verified the approach to selecting an experimental site. It was demonstrated that selection of a research site on the basis of its appearance and shape alone may lead to misinterpretation of experimental results.
The aim of our study was to evaluate the mobility of Zn in soils subjected to the activity of a zinc smelter and to assess the contamination of 1- and 2-year-old needles of Scots pine species sensitive to and tolerant of heavy metal contamination, particularly zinc. The trees were selected on the basis of their morphology, i.e., tolerant ones exhibited quite normal growth shape, but sensitive ones were more or less dwarves. Mineralogical composition revealed the prevalence of kaolinite in all soils except for two samples, where smectite dominated. Zinc contamination exceeded 30 times the geochemical background, and the reactive Zn forms represented 34.6% of total Zn content (ZnTotal). Proton generation capacity (α) indices calculated for the bioavailable Zn fraction (ZnBio) were 59% higher compared to the reactive Zn pool (ZnReac). Two-year-old tolerant (T) pine needles accumulated 21.9, 38.2, and 13.6% more Zn, Fe, and Mg, respectively, as compared to 1-year-old ones. For sensitive (S) needles, the range followed: 12.4, 48.8, and 7.3%, respectively. Iron was considered a “strategic survival element” for both pines growing under high zinc pollution. The transfer of Zn ions from the soil environment to plants still remains the basic source of maintaining its high concentrations in the needles, since air emissions ceased in 1996. The amounts of Zn accumulated by Scots pine at crucial years of metallurgical emissions may be considered as an additional time-constant source due to the evergreen vegetative lifecycle.
Nowadays, the main objectives of plant crop growers aim at two targets (i) increasing food production and (ii) simultaneously, reducing the environmental impact of increasing fertilizer nitrogen consumption. On a global scale, fertilizer nitrogen recovery ranges from 33 to 50%. The required efforts stimulating production but protecting the environment focus on increasing unit productivity of fertilizer N. Magnesium, owing to its biological functions in plants, should play a much more important role In modern agriculture controlling N economy of crop plants and, consequently, nitrogen dispersion in the environment. In Poland, arable soils are generally poor in total and available magnesium. This state can be considered as indicating the necessity of applying magnesium and then maintaining a wellfeed plant nutritional status of growing crops. Crops well supplied with magnesium since the beginning of their growth, as seen from studies on the response of sugar beets and maize, are in a position to increase nitrogen unit productivity. Cereals respond to Mg supply when a dressing treatment takes place just before the onset of flowering. Another factor significantly affecting fertilizer nitrogen recovery in Poland is soil pH. Acid soils fertilized with Mg contain increased soil exchangeable Mg levels, which in turn depress the pressure of toxic aluminum on growing crops. Improvement of the plant Mg nutritional status enables plants to incorporate some of potentially residual N into biomass, increasing biomass yield. It can therefore be concluded that magnesium, owing to its ameliorating function in arable soils, meets the main requirement of sustainable nitrogen management, both in agriculture and in the environment.
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