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Very low hydraulic conductivities of four selected samples were measured, ranging from 1.46 × 10−11 m/s to 2.94 × 10−11 m/s.
On nine occasions, runoff was measured (ranging from 1 to 59% of rainfall) when the soil surface was dry and rainfall was intense (greater than 0.1 mm/min).
Continuous variations in the anomaly were measured ranging from 0 W m− 2 up to a maximum heat flux of at least 94 W m− 2 (at the 28.5 m pixel scale).
We use the Varshni empirical formula to fit the temperature dependence: E ( T ) = E 0 − α T 2 T + β, (6) Figure 4 Real part of Δ r/r of samples A and B measured ranging from 80 to 300 K. Figure 5 Measured CP energies of samples A and B as function of temperature and RD instensity of CP1.
BDE-47 was the largest contributor to the ΣpentaBDE concentration measured, ranging from 18% to 72% of the total in individual samples, and averaging 52% overall.
For each condition, ankle joint was measured ranging from dorsiflexion 15° to plantar flexion 45° with increments of 15° using the hand-held dynamometer and, for each position, three trails of muscle contractions were tested.
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was obtained whereas the bias measured ranged from 10to18%8%.
The sum of all components measured ranged from 91.3% to 93%.
The amount of pleural effusion measured ranged from 10 to 1,600 mL.
The time from onset of dengue illness to CRP measured ranged from 1 to 5 days (median, 3 days).
Other parameters measured ranged from changes in the immune response to changes in retention rates of bacteria in lungs.
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