Water quality assessment relies on a suite of chemical parameters, among which organic indicators are pivotal for evaluating pollution from natural and anthropogenic sources. Unlike simple inorganic ions, organic matter in water is enormously diverse—ranging from humic substances to synthetic pesticides—so testing focuses on aggregate proxies rather than individual compounds.
The two most universal organic indicators are Chemical Oxygen Demand (COD) and Biochemical Oxygen Demand (BOD). COD measures the oxygen equivalent of all oxidizable organic material, using a strong chemical oxidant under acidic conditions. It captures nearly everything, including recalcitrant compounds that resist biological breakdown. BOD, in contrast, mimics natural aerobic degradation: it quantifies the dissolved oxygen consumed by microorganisms over a fixed incubation period (typically 5 days, BOD₅). The ratio of BOD to COD reveals biodegradability—a high BOD/COD ratio suggests wastewater amenable to biological treatment, while a low ratio indicates persistent or toxic organics.
Another critical indicator is Total Organic Carbon (TOC). Instead of inferring organic load from oxygen demand, TOC directly measures the carbon content of organic molecules after inorganic carbon is removed. It is more precise and faster than BOD or COD, and increasingly used in real-time process control. However, TOC does not distinguish between harmless natural organics and hazardous synthetic ones, so it is often paired with specific target analyses.
For drinking water and environmental monitoring, Dissolved Organic Carbon (DOC) is frequently measured after filtration (0.45 µm) to focus on the truly soluble fraction, which is more reactive in disinfection by‑product formation. Speaking of which, a distinct category of organic indicators concerns specific trace contaminants—volatile organic compounds (VOCs), polycyclic aromatic hydrocarbons (PAHs), pesticides, and pharmaceuticals. These are not captured by bulk parameters but are regulated separately due to their toxicity, even at microgram-per-liter levels. Their detection requires advanced chromatography and mass spectrometry.
Lastly, absorbance and fluorescence at certain ultraviolet wavelengths (e.g., UV₂₅₄) serve as rapid surrogate indicators for aromatic organic structures, especially humic substances. While not a direct concentration measurement, UV absorbance correlates well with TOC and trihalomethane formation potential in many source waters.

