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Soilless Media
Because soilless media tend to be hydrophobic and have a
tendency to shrink dramatically when very dry, wetting
the material and allowing it to dry over time is not the
ideal method for collecting data for a media-specific cali-
bration. The recommended procedure is to establish dif-
ferent moisture contents by adding water to a known
quantity of material and shaking or tumbling it into the
soilless media. This is best done on a mass wetness (MW)
basis where mass wetness is defined as:
2)
Where:
MW = target mass wetness (expressed as percent)
M
water
= mass of water needed
M
material
= total air-dry mass of sample
We have found that, for sphagnum peat moss, the relation-
ship between volumetric water content (VWC) and MW is
on the order of:
This can be used as a benchmark to determine your target
MW values. If later you discover you’ve selected too nar-
row a range, this experiment can be repeated.
material
water
M
M
MW
*
2
*
100
=
VWC = 0.243*MW + 0.5008
Содержание WaterScout SMEC 300
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