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Nine 0.8-m diameter experimental VF units (depth 0.6 m) were used: three units were planted with Typha angustifolia L., another three units were planted with Cyperus involucratus Rottb and three units were unplanted.
Particle size, specific gravity, number of units, depth, manning coefficient, volume of grit, detention time and air supply per unit length of tank in grit removal are 0.02 cm, 2.65, 2, 1.2 m, 0.035, 3 × 10−5 m3 grit/m3, 2.5 min and 0.28 N m3/min/m, respectively.
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In other words, the LLL algorithm is of insertion with a unit depth.
For example, a sandstone from the Karlstal unit (depth = 1083 m) was about two orders of magnitude more permeable when measured parallel to bedding (Griffiths et al. 2016).
A unit hydrograph (Sherman 1932) is defined as the hydrograph of direct runoff resulting from a unit depth of effective rainfall (ER) occurring uniformly over the basin and at a uniform rate for a specified duration.
Momentums and energy per unit depth have also been computed which are of important parameters in the design concept of either the target or the projectile (hollow charge) itself.
Nitrate storage per unit depth in the vadose zone is highest under PO (1703 kg/ha), followed by VE (970 kg/ha), WM (736 kg/ha) and CO (727 kg/ha).
The resistance per unit depth increased exponentially with solids content, so much so that there is an optimal solids content in relation to the rate of production of dried material.
Lower sub-unit (depth 80 70 cm): Starts by reverse graded basal brownish sands (see formation on Fig. 5), containing an accumulation (20 to 30 cm in thickness) of carbonate concretions and rip-up clasts of the underlying dark grey silt and dark brown organic matter (OM).
Although solutions involving feedback of the measured bulk density into a time-budgeting algorithm are conceivable, a simple approach where equal time is spent per unit depth may be best, providing an accuracy in bulk density of around 5 20%, for 25 mm slices and the expected range of parameters.
The attractive part, a well of approximately unit depth whose steepness near r = σ + w is set by the length scale αatt, vanishes continuously at r = σ + 2 w.
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