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The mean values at the age of 28 days are obtained as 7.5 MPa and 13 MPa respectively.
Figure 2(b) shows the plots of D, H and Z for monthly mean values at Alibag for all days.
The treatment mean values at same time point were compared by post hoc least significant difference (LSD) test.
b Same as a but using SD-WACCM simulations and are zonal mean values at 45 km.
The zonal winds in the stratosphere (blue line) were zonal mean values at 10 hPa from ECMWF database.
All assays were repeated at least three times and the results obtained are the mean values at each concentration.
The phytoplankton biomass shows the highest mean values at a duration of integration of 1 month a−1 and decrease with increasing connectivity.
Upon flexion, both medial and lateral loads decrease with mean values at 90° flexion of 30 N (22 N) and 6 N (5 N) respectively.
These results illustrate that a causal relationship between erosion and saprolite production can lead to asynchronous evolutions of their mean values at the mountain range scale.
A previous study has shown good reproducibility of MSPA group mean values at test and retest after 2 weeks in 10 healthy volunteers [12].
The statistically significant differences among mean values at the level of significance (P < 0.05) were evaluated with the paired t test in SPSS (version 19.0).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com