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Almost all of it was less than 50,000 years old, suggesting that the mineralization process was actually much faster.
A savings of more than 40% of the H2O2 dosage required for the phenol mineralization process was confirmed.
The mineralization process was studied using microbiological (microbial viability), morphological (scanning and transmission electron microscopy), biochemical (GC-MS, Microarray immunoassay and Rock-Eval) and spectroscopic (FTIR and RAMAN spectroscopy) methods.
The overall mineralization process was optimized using a Central-Composite Experimental Design (CCED) with four variables (initial concentrations of H2O2 and Fe(II), amplitude and pulse length).
A biologically inspired mineralization process was first developed to nucleate Mg-doped hydroxyapatite crystals on type I collagen fibers during their self-assembling.
The results showed that CO2 production during the DOC mineralization process was facilitated by Fe(III) reduction at the expense of CH4 production.
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The mineralization process is regulated in a Ca2+ concentration- and minerlization time-dependent way.
This suggests that some steps in the 17β-estradiol mineralization process are occurring in the sorbed phase.
However, the lower mineralization on F-TiO2, which produced more OH, implies that the role of OH in the photocatalytic mineralization process is minor.
Carbon (C) and nitrogen (N) mineralization process is a key indicator of soil quality which regulate nutrient availability and supply to the crops.
The mineralization process is all about chemistry, so we can't use any old rocks – we need only those rich in calcium, magnesium and iron silicate materials.
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CEO of Professional Science Editing for Scientists @ prosciediting.com