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The cracks in the clay samples are probably formed due to weaker network at elevated temperatures due to weaker bridging interaction between clay platelets as compared to stronger network resulting from dense entanglement and bridging of carbon nanotubes.
Other elevated element concentrations, especially those in B-depth samples, are probably natural with high As, Bi, Sb and W reflecting proximity to Au mineralisation, Pt and Re near PGE mineralisation, and accumulation of heavy mineral-associated elements such as Cr in alluvium-derived soils related to the effects of both source material and hydraulic effects on flood plains.
The relative levels of these amino acids in different CCA samples are probably responsible for the differences in the sulfur volatiles.
The slightly higher ID/IG ratios in C-face samples are probably due to the presence of the boundary-like folds.
The slightly increasing trends of Fe and Mn in few samples are probably due to chemical weathering dissolution and the process of ferromagnetism.
The trace element concentration indicates that the slightly increasing trends of Fe and Mn in few samples are probably due to chemical weathering dissolution and the process of ferromagnetism.
Similar(44)
This reduced level of ribosome synthesis in the flight samples is probably the result of an accelerated cell cycle.
Ni Al mixed phases, observed on the E-Cat samples, were probably formed during ageing and are expected to be inactive.
This high reducibility of cobalt species in the bimetallic samples is probably due to the formation of Co3O4 domains at the gold CoO interface perimeter, which are absent in the gold free cobalt containing UVM-7 catalysts.
Some of the samples were probably deposited at this time as a result of filling the gap that was created.
The chromite in our samples was probably exposed to oxidised fluids containing micro- or nanosized colloidal Mn(IV -oxides that was IV -oxides inthathe system.
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CEO of Professional Science Editing for Scientists @ prosciediting.com