Measurement of
Moisture Content
Specific Gravity
Humidity
Measurement of Moisture
Direct methods measure moisture content without an intermediate variable, including measuring the moisture content by weighing or titration before and after drying
Indirect measurement methods determine the moisture content by measuring the variation of a physical property (e.g., temperature, refractive index, pressure) relative to a baseline or over time. This property, transformed into a signal (e.g., wavelength shift, electric current), is then correlated to moisture content
Gravimetric method
Karl Fischer titration method
Colorimetric titration method
Indirect methods
Indirect methods include optical, dielectric, nuclear, and hygrometric approaches, which are considered to be quantitative methods.
Most indirect methods, with the exception of hygrometric methods,
use electromagnetic radiation to determine moisture content by exploiting the strong influence of water in a material on the electromagnetic field
If a known electromagnetic field is applied to a sample before and after drying, the moisture content can be
determined by comparing the changes in physical properties, such as refractive index (e.g., optical methods), caused by the alternating electromagnetic field in the presence of water
The manner in which the waves propagate and interact with an applied electromagnetic field is influenced by the electrical, magnetic, physicochemical (e.g., homogeneity, texture, size, shape) properties of a material, and the distance at which the sensor is placed
Material characteristic calibration curves are needed to convert the radiation signal into moisture content.
The choice of spectrum range depends on the absorption, reflectance, and transmittance of the targeted material, the expected moisture content in the sample, the type of water bonds, and on the contrast in optical properties between the targeted material and water
Optical methods
Infrared spectroscopy
Infrared (IR) thermography
Hyperspectral imaging (HSI).
Dielectric methods
Electrical conductivity
Microwave method.
Radio frequency (RF) method
Hygrometric methods
Hygrometric methods are based on equilibrium relative humidity
(ERH) instead of moisture content.
ERH is numerically equal to water activity but expressed as a percentage of the actual amount of water in the air versus the amount of water the air could hold at saturation
RH or water activity sensors are relatively easy to use in the context
of foods. The measurement approach is relatively simple but regular
calibration using desiccant salts (e.g., sulphuric acid, NaCl) is required
Sensors based on capacitance and resistivity may be used, but their measurement may be affected by high temperatures and humidity.
Advantages
Specific Gravity Determination
Specific gravity is the ratio of the density of a substance to the density of a reference substance;
The reference substance is nearly always water at its densest (4°C) for liquids; for gases it is air at room temperature (21°C)
Specific gravity is commonly used in industry as a simple means of obtaining information about the concentration of solutions of various materials, or of quality control: to evaluate physical changes, or determine the degree of uniformity between samples or lots.
A hydrometer is an instrument used for measuring the relative density of liquids based on the concept of buoyancy. They are typically calibrated and graduated with one or more scales such as specific gravity.
Specialized hydrometers
Alcoholometer
Lactometer
Saccharometer
Salinometer
Acidometer
Digital density meters (Typical ASTM Test method D4052)
Vibrating Element Transducers:
Digital density meters based on the oscillating U-tube technique: The sample to be measured is filled into a U-shaped tube which is induced to vibrate. The eigen frequency of the oscillation of the U-tube is influenced by the mass and therefore by the density of the sample.
https://www.gpsil.co.uk/our-products/density-meters/measuring-principle/