Product Quick Navigation
Get a Quote

Heavy rain can turn a steady treatment shift into a scramble: raw water darkens, floc changes, and filters need washing sooner than expected. If you are asking, “Why is my water treatment coagulant dosage increasing?” the answer usually starts upstream. Stormwater carries suspended particles and natural organic matter into the intake, while changes in alkalinity, pH, temperature, and flow can make the existing treatment settings less effective.
But higher turbidity does not automatically justify a higher dose. Sometimes the plant needs more coagulant; sometimes it needs a different coagulation pH, better mixing, or a dosing-system correction. Distinguishing those situations is what keeps a rainfall event from becoming an expensive cycle of chemical increases and declining performance.
A storm does more than add water to a river or reservoir. It connects the intake to soil, roadside drainage, agricultural land, vegetation, and disturbed sediments across the catchment. The resulting changes may arrive together—or in separate waves.
Runoff often raises raw water turbidity by carrying clay, silt, and other suspended material. Many fine particles remain dispersed because their surface charge prevents them from readily sticking together. Coagulation destabilizes these particles, allowing flocculation and separation to follow.
However, turbidity is an optical measurement, not a direct measure of chemical demand. Coarse mineral particles may settle relatively easily, while a less dramatic increase in fine colloids can create a difficult treatment challenge. Particle size, surface chemistry, and the coagulation mechanism all influence the dose required.
There is no reliable universal conversion from raw water NTU to coagulant mg/L. A relationship developed from plant records can support decisions, but it needs checking when storm conditions change the character of the water.
Rain washes decomposing vegetation, humic substances, and other organic material into source water. This natural organic matter can consume coagulant and change the conditions needed for effective removal. Operators may notice stronger color, rising dissolved organic carbon, or increased UV absorbance where those measurements are available.
This explains a frustrating situation: the river looks clearer after the storm peak, yet returning to the normal dose produces poor results. Suspended solids may have declined while dissolved organic matter remains elevated. In drinking water treatment, controlling those organics can also matter for downstream disinfection by-product formation.
Aluminum- and iron-based coagulants react with water and generally consume alkalinity. If rainfall dilutes a low-alkalinity source, a previously successful dose may depress coagulation pH more than expected. Adding still more coagulant can then worsen the conditions needed for floc formation.
Rain does not always lower alkalinity or pH; the response depends on the catchment and source-water chemistry. Measure both rather than assuming a direction. The important value is not only intake pH, but also the pH after coagulant addition under representative mixing conditions.
Before diagnosing a chemistry problem, separate dose from consumption. Dose is typically expressed in mg/L. Consumption is the amount used over time, such as kg/day. A plant treating more water after rainfall can use more chemical without any change in dose.
On a consistent mass basis:
Chemical consumption (kg/day) = dose (mg/L) × flow (m3/day) ÷ 1,000.
For example, 20 mg/L at 10,000 m3/day equals 200 kg/day on the stated dose basis. If flow rises to 15,000 m3/day, consumption becomes 300 kg/day at the same dose. A 50% increase in daily usage does not, by itself, demonstrate increased coagulant demand.
Keep commercial-product dose, active-content dose, and metal-based dose clearly distinguished. When converting liquid feed volume into mass, use the applicable product density and concentration. Comparing pump percentages or liters per hour across different deliveries can otherwise create a misleading picture.
The most useful first response is a short, coordinated check of source water, chemical delivery, and treatment performance. Avoid changing several variables at once unless immediate operating requirements demand it.
Sample timing matters. Intake water collected now may not reach the clarifier or filters until later. Match raw water measurements, chemical adjustments, and downstream results using the plant’s approximate travel times. Otherwise, a reasonable adjustment may look unsuccessful simply because the corresponding water has not reached the monitoring point.
Check actual pump delivery using the plant’s approved calibration procedure. Inspect for air binding, blocked suction strainers, leaking valves, restricted injection quills, or changes in backpressure. Confirm the flow signal used for flow-paced dosing is credible.
Also review recent deliveries and dilution practices. A different concentration, incorrect make-up ratio, or undocumented product change can mean the same pump setting delivers a different effective dose. These checks are particularly important when a storm coincides with a tank changeover.
A useful storm-event jar test should represent the water currently challenging the plant. Collect fresh raw water and reproduce plant conditions as closely as practical, including chemical addition sequence, rapid mixing, flocculation, temperature, and settling time.
The largest floc is not necessarily the best result. A visually impressive floc may be fragile or carry over under actual hydraulic conditions. Conversely, a dose that gives acceptable settled turbidity may not adequately address organic matter or downstream filtration requirements.
There is no single optimum pH or storm dose for every coagulant. Alum, ferric salts, and prehydrolyzed aluminum products behave differently, and commercial grades can differ in concentration and basicity. Product guidance is a starting point; site-specific testing determines whether a change is suitable.
Heavy rain can push physical treatment units beyond their comfortable operating range. Higher flow reduces available contact time and can increase clarifier loading. Colder runoff may slow floc development, while heavier solids loads increase the burden on sludge removal.
If jar tests produce good water but the plant does not, investigate the process before escalating the dose again:
Extra coagulant also creates additional chemical sludge. Beyond the effective operating range, it may increase solids-handling costs, depress pH, or contribute to residual-metal and filtration problems. Judge performance against established operating limits and applicable water-quality requirements—not raw water appearance alone.
Rainfall can also introduce microbial contamination and other catchment-specific hazards. Coagulant optimization supports treatment, but it does not replace disinfection control or the plant’s broader incident-response procedures.
A prolonged rainfall event can raise daily consumption while transport disruptions make replenishment less predictable. Review stock against a realistic storm-use scenario, available storage, delivery lead time, and the time needed to approve an alternative product. An untested substitution during unstable conditions creates another variable for operators to manage.
For imported chemicals, request the relevant specification, batch certificate of analysis, safety data sheet, and documentation required for the destination and intended application. Drinking-water use may require specific approvals; a general industrial grade is not automatically suitable.
Clear product identification matters when working with broad-portfolio suppliers such as Shandong Huafeng Chemical Co., Ltd. For example, Triethylene glycol CAS#112-27-6 is a hygroscopic liquid used in applications such as natural gas dehydration and certain industrial dehumidification systems. It is not a water treatment coagulant or a substitute for one. Procurement requests should identify the required treatment chemistry and grade explicitly, rather than relying on a general chemical category.
The treatment challenge can outlast the weather. Runoff may arrive after a delay, reservoir layers can respond differently, and organic matter may remain elevated after the turbidity peak has passed. Continue event-based monitoring until the source and treatment response have stabilized.
Reduce dosage through verified adjustments rather than immediately restoring the pre-storm setting. Record rainfall timing, raw water quality, dose basis, coagulation pH, flow, settled-water performance, filter behavior, and sludge conditions. Over successive events, those records can reveal which measurements provide the earliest useful warning.
The practical answer to rising post-rainfall demand is therefore not “add more until the water clears.” It is to identify what changed, confirm what the feed system actually delivers, test the relevant treatment conditions, and follow the result through the plant. That approach gives operators a defensible dose—and a better chance of maintaining stable treatment without unnecessary chemical use.
Send Us Your Inquiry Today
