12 research outputs found

    Plant Nutrients

    No full text

    Oilseed rape (Brassica napus L.) genotypic variation in response to boron deficiency

    No full text
    Boron efficiency of 16 oilseed rape genotypes was tested using both hydroponic and pot-soil growing techniques. From the nutrient solution experiment (0.1 and 10 mu M B), 4 representative contrasting genotypes were selected based on relative root and shoot growth. These were then grown in pots with low-B soil (0.25 mg kg(-1)). From the nutrient solution experiment, 2 genotypes selected as B-inefficient did not show any growth disorders, and the concentration of B in the shoots was above critical. Furthermore, 4 contrasting genotypes were subjected to the stable B-11 isotope-enriched uptake solution for 6 h to verify possible low B-induced active uptake by roots and xylem loading of B. The concentration of B-11 in either root cell sap or xylem exudate was higher than in the external nutrient solution, which indicated the presence of low B-induced active uptake for all tested genotypes, and, to some extent, their efficiency with low B. In conclusion, a combination of different growing techniques under controlled environmental conditions together with different parameters including relative root and shoot weight, shoot B concentration, and B uptake provided reliable B efficiency results in oilseed rape genotypes

    Silicon ameliorates manganese toxicity in cucumber by decreasing hydroxyl radical accumulation in the leaf apoplast

    No full text
    This work was focused on the role of silicon (Si) in amelioration of manganese (Mn) toxicity caused by elevated production of hydroxyl radicals (center dot OH) in the leaf apoplast of cucumber (Cucumis sativus L.). The plants were grown in nutrient solutions with adequate (0.5 mu M) or excessive (100 mu M) Mn concentrations with or without Si being supplied. The symptoms of Mn toxicity were absent in the leaves of Si-treated plants subjected to excess Mn, although the leaf Mn concentration remained extremely high. The apoplastic concentration of free Mn2+ and H2O2 of high Mn-treated plants was significantly decreased by Si treatment. Si supply suppressed the Mn-induced increased abundance of peroxidase (POD) isoforms in the leaf apoplastic fluid, and led to a rapid suppression of guaiacol-POD activity under excess Mn. The spin-trapping reagent 5-(diethoxyphosphoryl)-5-methyl-1-pyrroline-N-oxide was used to detect center dot OH by electron paramagnetic resonance spectroscopy. Although supplying Si markedly decreased the accumulation of center dot OH in the leaf apoplast with excess Mn, adding monosilicic acid to the Mn2+/H2O2 reaction mixture did not directly affect the Fenton reaction in vitro. The results indicate that Si contributes indirectly to a decrease in center dot OH in the leaf apoplast by decreasing the free apoplastic Mn2+, thus regulating the Fenton reaction. A direct inhibitory effect of Si on guaiacol-POD activity (demonstrated in vitro) may also contribute to decreasing the POD-mediated generation of center dot OH

    Isotopologue ratios of N2O emitted from microcosms with NH4+ fertilized arable soils under conditions favoring nitrification

    No full text
    Soils represent the major source of the atmospheric greenhouse gas nitrous oxide (N2O) and there is a need to better constrain the total global flux and the relative contribution of the microbial source processes. The aim of our study was to determine variability and control of the isotopic fingerprint of N2O fluxes following NH4+-fertilization and dominated by nitrification. We conducted a microcosm study with three arable soils fertilized with 0-140 mg NH4+-N kg(-1). Fractions of N2O derived from nitrification and denitrification were determined in parallel experiments using the N-15 tracer and acetylene inhibition techniques or by comparison with unfertilized treatments. Soils were incubated for 3-10 days at low moisture (30-55% water-filled pore space) in order to establish conditions favoring nitrification. Dual isotope and isotopomer ratios of emitted N2O were determined by mass spectrometric analysis of 6180, average delta N-15 (delta N-15 bulk) and N-15 site preference (SP = difference in delta N-15 between the central and peripheral N positions of the asymmetric N2O molecule). N2O originated mainly from nitrification (> 80%) in all treatments and the proportion of NH4+ nitrified that was lost as N2O ranged between 0.07 and 0.45%. delta O-18 and SP of N2O fluxes ranged from 15 to 28.4 parts per thousand and from 13.9 to 29.8 parts per thousand, respectively. These ranges overlapped with isotopic signatures of N2O from denitrification reported previously. There was a negative correlation between SP and delta O-18 which is opposite to reported trends in N2O from denitrification. Variation of average N-15 signatures of N2O (delta N-15(bulk)) did not supply process information, apparently because a strong shift in precursor signatures masked process-specific effects on delta N-15(bulk). Maximum SP of total N2O fluxes and of nitrification fluxes was close to reported SP of N2O from NH4+ or NH2OH conversion by autotrophic nitrifiers, suggesting that SP close to 30 parts per thousand is typical for autotrophic nitrification in soils following NH4+-fertilization. The results suggest that the delta O-18/SP fingerprint of N2O might be used as a new indicator of the dominant source process of N2O fluxes in soils. (C) 2008 Elsevier Ltd. All rights reserved.Deutsche Forschungsgemeinschaft (DFG
    corecore