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651.
652.
Siegmund Probst 《Planta》1927,4(5):651-709
Ohne ZusammenfassungMit 4 Textabbildungen. 相似文献
653.
Diphtheria toxin catalyzes the ADP-ribosylation of elongation factor 2 (EF-2) in eukaryotes and archaebacteria. As the reaction is strictly EF-2 specific and introduces two negative charges into the molecule, the resulting shift in the isoelectric point (pI) by 0.2 pH units was used to establish a new purification method for EF-2 from Sulfolobus acidocaldarius. The cells were lysed with dithiothreitol at pH 9 and EF-2 was purified by ammonium sulfate precipitation, gel filtration on Sephadex G-200, and three isoelectric focusing steps. The EF-2-containing fractions from the first isoelectric focusing step at pH 4-9 were refocused in a more narrow pH-gradient (pH 5-7). The EF-2 peak from the second step was eluted, collecting only the fractions above the pH region where ADP-ribosylated EF-2 would focus. The EF-2 was then ADP-ribosylated with diphtheria toxin and NAD and subjected to further isoelectric focusing (pH 5-7). The EF-2 was almost homogeneous since ADP-ribosylation had shifted it into a region of the pH gradient free of contaminating proteins. Diphtheria toxin was immobilized on CNBr-activated Sepharose to prevent a possible contamination by proteins from the diphtheria toxin preparation which might have the same pI as ADP-ribosylated EF-2. Finally, the ADP-ribosyl group was removed by equilibrium dialysis using diphtheria toxin and nicotinamide at pH 6.3. The obtained EF-2 was active in protein synthesis. 相似文献
654.
Is the sequential in situ incubation of undisturbed soil cores, developed for forest stands applicable to arable soils? The incubation of covered and uncovered soil cores allows the estimation of net nitrogen mineralization (NNM), plant nitrogen uptake (Nuptake) and potential leaching losses (Ntrans). The amounts and temporal dynamics of these N fluxes were determined at four arable soils in a two-year study. Results suggest that: (i) the method can not be recommended for the estimation of N uptake and leaching losses, but (ii) it is suitable for the estimation of NNM; (iii) incubations should preferably be started when soil is moist; (iv) the length of incubation periods should be reduced (<4 weeks); (v) dynamics of NNM is mainly determined by temperature and moisture conditions if there is no interference by agricultural management. Inputs of straw, manure, slurry or green manure strongly influence the amount and the dynamics of NNM. 相似文献