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There are other minor numerical differences in the tables (Table 2, Johnson et al. 2003, and Tables 1 and 3, Dawson et al. 1993), not remarked upon by Hardin et al., which derive from the more extensive statistical analysis in the later paper.
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The differences in these tables and figures indicate that Buckley Leverett linear displacement is not appropriate for peripheral waterflood reservoirs.
In part because the analysis data set contained more than 400,000 observations, all of the differences shown in the tables are statistically significant at the p <.05 level.
There are two key differences in the life tables.
Unlike the raw group differences in the descriptive tables, these coefficients are estimated controlling for initial (preexposure) status and for period of exposure.
The differences in the affinities (Table 2) reflect the variability in hydrogen concentrations, but the magnitude of these differences is quite small, because the intensive term (ΔrG°) in the Gibbs energy calculation is very large for both reactions.
There were no differences in the subgroups (Table 4).
The southern-northern splits received strong statistical support in the combined analyses, and were further supported by statistically significant differences in the AMOVA (Table 1).
A complete list of naming differences appears in the Table S9.
Because the purpose of a data warehouse differs from that of an operational system, there are differences in the types of tables that make up the design.
Furthermore, the maximum difference percentage in the table is under 1.5%.
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