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Finally, the most variable component in energy expenditure is physical activity, which includes exercise and other voluntary activities as well as involuntary activities such as fidgeting, shivering, and maintaining posture.
However, the most variable component of the holoenzyme is the regulatory subunit, which can belong to one of four different families termed B (or PR55), B' (or B56 or PR61), B″ (or PR72) and B"' (or PR93/PR110).
Body fat mass is the most variable component of the human body.
EAA is the most variable component as it can account from 10%to20%0% of total energy expenditure (in bedridden subjects) to 60%to80%0% in athletes.
The energy cost of physical activity, as determined by body movement, is the most variable component of daily energy expenditure (Starling 2002).
Physical activity energy expenditure (PAEE) is the most variable component of total energy expenditure (1), and both PAEE and body movement are important determinants of cardiometabolic health in adults (2– 4) and children (5, 6).
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These findings, coupled with blast results (Table 1), suggest that these VirB6 genes are the most variable components of the Rickettsia vir system, particularly when the regions flanking the VirB6/TrbL domains are considered.
Consequently Seg-2 and 6 vary in a manner that correlates with both the geographic origins (topotype) of the virus strain and virus serotype (particularly Seg-2), making them the most variable components of the BTV genome [35].
Comparisons of the full genome of the northern European strain of BTV-8 to other European isolates, have confirmed Seg-2 and -6 as the most variable components of the BTV genome [13], showing variations that correlate with both virus serotype and the geographic origins (topotype) of the virus isolate.
Comparison of cell wall-anchored proteins among streptococcal species shows that they are one of the most variable components of the genome; 13 out of the 29 proteins in P1/7 were unique to S. suis (Table S2), the rest being intermittently distributed.
The groundwater recharging river was the most variable recharge component, and ranged from 1% of the total runoff at the beginning of the melting season to even 27% at the end of summer.
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