# how to convert gravimetric soil water content to volumetric soil water content

The amount of water or moisture in soil can be measured as either gravimetric soil water content (GWC) or volumetric soil water content (VWC).

But what is GWC and VWC? And how do you convert GWC to/from VWC?

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The easiest way to think of GWC and VWC is that GWC is related to the *mass* of water and soil, whereas VWC is related to the *volume* of water and soil.

GWC is the *mass* of water per *mass* of dry soil in a given sample. To determine GWC, collect soil sample from the field, weigh that soil then dry it in the oven at 105°C for at least 3 days (or, more precisely, weigh the soil periodically until there is no more loss in weight which indicates that all of the water has been dried from the sample). The equation for GWC (*θ*g) is:

*θ*g = (*Wet* - *Dry*) / *Dry* (Equation 1)

where *Wet* is the weight of the soil sample from the field and *Dry* is the weight of the dry soil sample.

VWC is the *volume* of water per *volume* of soil. To determine VWC, you will need to measure *Wet* and *Dry* as described above for GWC. You will also need to know the bulk density of the soil sample (*BD*).

In this case, it is not enough just to collect a handful of soil sample from the field. It is better practice to collect a sample of soil in a known volume, such as a metal cylinder. The *BD *is the ratio of *Dry* to the volume of your sampler. (A You Tube video at the bottom of this article outlines how to collect soil samples to measure soil bulk density.) The equation for VWC (*θ*v) is then given by:

*θ*v = *θ*g * *BD* (Equation 2)

Soil scientists also incorporate the density of water (*WD*) into *θ*v as:

*θ*v = *θ*g * (*BD* / *WD*) (Equation 3)

However, the value of *WD* is close to 1 and is typically ignored when calculating *θ*v.

In summary, Equation 1 is used to calculate gravimetric soil water content and Equation 2 is used to calculate volumetric soil water content.

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