Measuring the invisible: how scientists quantify the water hidden within solids
In short: Whether it is the moisture in a piece of timber or the hydration of agricultural soil, water content is more than just a simple number. It is a complex ratio that can be measured by weight, volume, or even from the far reaches of space using microwave radiation.
Water content, or moisture content, describes the quantity of water held within materials like soil, wood, or crops. Because materials like coal or soil can change in volume or mass as they dry, scientists use different mathematical frameworks to express this value. One approach is gravimetric water content, which is expressed by mass. Depending on the field, this can be calculated on a 'wet basis'—the mass of water relative to the total moist specimen—or a 'dry basis,' which compares the water mass to the weight of the dry material itself. In disciplines such as woodworking, geotechnics, and soil science, the dry basis is the standard convention.
Another method is volumetric water content, which focuses on the ratio of the volume of water to the total volume of the dry material. This is particularly useful in soil science. In related engineering fields, researchers also look at the degree of saturation, which measures how much of the material's pore space is filled with water. While engineers often use idealizations where saturation reaches 1 (completely full) or 0 (completely dry), in physical reality, these extremes are rarely reached.
Determining these values requires diverse techniques. In a laboratory, the oven-dry method is a primary standard: a sample is heated in a kiln—often at 105 degrees Celsius for 24 hours in the case of wood—and the weight loss is measured. Other chemical methods include Karl Fischer titration or the Dean-Stark method used in food science. On a much larger scale, satellite remote sensing uses microwave radiation to estimate surface soil moisture. Because microwave signals can penetrate clouds and vegetation canopies, satellites like SMAP and RADARSAT can monitor the hydration of the Earth's surface from orbit.
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