True soil moisture = a + b ✕ soil moisture meter reading
Here, a and b are so-called coefficients that convert the readings from your soil moisture meter (a number between 1 and 10) to true soil moisture (a number between 0 and 1, often less than 0.5). Our lab has collected soil moisture readings using both a low-cost off-the-shelf soil moisture meter (the one with a 7-inch rod) and a research-grade soil moisture meter (HydroGO Portable Soil Sensor System, Stevens Water Monitoring Systems, Portland, OR) to obtain coefficients a and b.
Examples of relationships between low-cost soil moisture readings and true soil moisture measurements for different soil texture types.
Soil Texture Triangle from the US Department of Agriculture
The coefficients a and b are not the same for different soils and depend on a soil property named "soil texture". In the US, people classify soils into 12 soil texture classes (see figure above) and each class has a different ability to hold water (and nutrients) and a unique set of coefficients a and b. Some people even believe that soil texture controls the quality of the wine, along with climate, exposure to sunlight, and grape varieties.
Soil texture can be measured using a quick "dirty" ribbon test or estimated using a web-based App (Web Soil Survey, watch Video 2 to learn how to use it). You can select either method or compare if both methods give you the same soil texture class for your measurement site.