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To know the direction of exchange during the path of groundwater through the aquifer, Schoeller (1967, 1977) suggested two chloro-alkaline indices CaI1 and CaI2 to indicate the exchange of ions between groundwater and its host environment.
They indicate the exchange of Na and K from the water with Mg and Ca of the rocks which are mainly of granitic origin (Nagaraju et al. 2015).
Together, these results indicate the exchange of genetic material between phylogenetically distinct Clostridia found within the intestine of the marine iguana that are potentially involved in agar degradation and are the subject of ongoing research.
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Chloro-alkaline indices reveal that the majority of samples show negative values in all the litho units indicating the exchange of Na and K in groundwater with Mg or Ca in rock.
We also observed such evidence in P. spp. Phylogenetic structure of MAT-locus and other regions with noncanonical topology indicates the exchange of this genome fragments between P. spp. lineages.
They indicate that the exchange of Mg2+ and Ca2+ of the water with Na and K in its host environment is prevalent in the studied area.
The results indicate that the exchange of the counter-ion Cl− of PTHT by a linear long chain with RSO−3 group is a general procedure to obtain PPV polymer at lower conversion temperature (ca. 110 °C) with significant increase in the emission efficiency, regardless of the chemical position and the number of sulfonate groups.
Results from the above analyses indicate that the exchange of the C-terminal domain in SSB significantly changed the ssDNA-binding ability and the DNA-binding behavior (complex number).
This indicates that the exchange of dfr-genes between E. coli and K. pneumoniae may be an uncommon event in man.
Nevertheless, it is somewhat remarkable that the introduction of regions with a significant number of different residues did not affect the catalytic events, indicating that the exchange of regions with different amino acid composition is well tolerated.
This finding indicates that the exchange of DNA occurred mainly between exons 2 and 3/4.
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