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The results indicate that the optimum number of passes to achieve maximum density is four passes.
At salinities less than 24.7 psu the density maximum is reached before the ice point, while at the higher salinities more typical of the open oceans the maximum density is never achieved naturally.
The diurnal maximum density is found in the local noon or in the afternoon hours and the minimum occurs in the pre sunrise hours.
The outer region of maximum density is centred at an altitude of about 15,000 to 20,000 km (9,300 to 12,400 miles), though some estimates place it as far above the surface as six Earth radii (about 38,000 km [23,700 miles]).
At small size ratio, the maximum packing density can be achieved by different atomic size distributions, whereas for medium size ratios the maximum density is always correlated to a concave size distribution.
As discussed in Ref. [13], the maximum density is however achieved taking (2).
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Data from the strands with a 0.68 theoretical maximum density are compared to available literature.
The addition of ground limestone advantageously increased the moisture content at which maximum density was achieved by about 2%.
The inner edge of the torus was located at (r_{mathrm{in}} = 6.0) and the maximum density was located at (r_{max} = 12.0).
The densification data of BLTM ceramics sintered at various temperatures between 1,000 to 1,150°C (not shown here) indicated that the optimum sintering condition for achieving maximum density was 1,100°C and 4 h dwell time.
They concluded that one cubic decimetre of water at its maximum density was equal to 99.92072% of the mass of the provisional kilogram made earlier that year.
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