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We considered that the moisture value differentiations depend on species, season, nutritional regime, size, spawning season, sex, and catching area.
Drought intensity is defined as the number of negative standard deviations between the observed soil moisture value and the respective normal climatological conditions.
The absolute moisture value is 0.40 ∼ 0.55, and is consistent with the value found by a soil test (Grossman and Reinsch, 2002) of 0.51±0.04 on 8 November, 2008.
Furthermore, when Ds is changed from 1.0 × 10−6 down to 3.0 × 10−7 and up to 3.0 × 10−6 [m2/s], the moisture value falls by about 0.08 and rises by about 0.07, respectively (Fig. 12(b)).
The lower soil moisture limit of 7% corresponds to the minimum value above wilting point, while the soil moisture value of 20% matched the hydrostatic state of the lysimeter (Table 1).
The steady-state soil moisture value at ground surface level during the two years, 0.5 ≤ Z ≤ 3 [m] (Fig. 3(d)), is 0.41 ∼ 0.50 and coincides with the observed moisture at Mizusawa (Fig. 3(c)).
Similar(49)
In addition the range in calculated soil moisture values was reduced compared to observed soil moisture.
The study concluded that the krigged values were consistent and true representative of soil moisture values.
However, assimilation of streamflow observations systematically increased the simulated soil moisture values.
Calorific values are not correspondent to that of fuel for combustion whereas, moisture values are very high.
The moisture values obtained for eucalyptus were higher than those for citrus honey samples independent of the analysis method used.
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