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The results indicated net mineralization during the vermicomposting of salvinia weed.
Sole application of manure resulted in positive priming effect of 91 and 124% at the 13 and 26 tons ha−1 application rates, respectively; equivalent to additional 272 and 369 mg SOC g−1 soil mineralization during the 56 days incubation (Fig. 2).
The total concentrations of nutrients (Na, K, Ca and Mg) and heavy metals (Zn, Cu, Mn, Fe, Ni, Pb, Cd and Cr) increased due to weight loss of the dry matter from the decomposition of the organic matter resulting in release of CO2 and the subsequent mineralization during the composting process (Singh and Kalamdhad 2013a).
However, simple subtraction of initial differences between pairs from final differences to isolate the treatment effect neglect the fact that the soil with the higher initial SOC content will lose proportionally more C through mineralization during the experimental period higher SOC content caused higher SOC mineralisation during the experimental period.
We found that viscosin stimulated n-hexadecane mineralization during the initial 48 h of the experiment.
To elucidate the interactions of MEPE in the growth plate, this study was undertaken to examine the presence and function of MEPE and its ASARM peptide in growth plate matrix mineralization during the endochondral ossification process.
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On interaction of these pesticides with AgNPs, pesticide undergoes mineralization during which the metal changes into metal salt [23].
These results were corroborated by Von Kossa test results, which showed strong formation of mineralization nodules during the same time period.
It was found that N-deethylation, destruction of chromophores, opening-ring and mineralization occurred during the confined ferrous Fenton rhodamine B oxidation process.
According to the micro-CT analysis mineralization on silk fibroin scaffolds with pores of 112 224 μm diameter was most efficient with an initial cell pre-culture period of 9 days, showing 6.87 ± 0.81× higher mineralization values during the whole cultivation period than without an initial cell pre-culture period.
Thus, the conductors C1a and C1b were formed in the Cambay rift due to the emplacement of fluids, and the conductors C3 and C4 in Aravalli Delhi formations were formed due to sulfide mineralization during various metamorphic phases and the presence of fluids within the fault and shear zones.
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