Forty-one millisiemens per centimetre on the handheld, chloride at 14,000 milligrams per litre, and a gel that would not firm up past a thick soup no matter what the crew did. The site was 900 metres from the shoreline, the liner was intact, and the salt was coming in with the refuse and the groundwater. It had been creeping up for three years and nobody had looked at the conductivity trend until the batches started failing.
Seawater intrusion is the obvious cause at a coastal site and it is not the only one. Salt-laden refuse, brackish cover material, and saline groundwater under a damaged toe drain all produce the same signature. What they have in common is a dissolved load high enough to defeat a polymer that works perfectly well twenty kilometres inland.
A polyacrylate gel swells because the fixed charges on the polymer chain repel each other and draw water in to dilute the counter-ions trapped inside the network. That mechanism depends on the ion concentration outside the gel being lower than inside. Raise the outside concentration and the driving force falls, roughly in proportion to the ionic strength.
Sea salt is a particularly efficient way to do this because sodium is small, mobile and abundant, and it floods the network with counter-ions. At 15 mS/cm a typical grade might hold 20 to 25 grams of water per gram of polymer. At 40 mS/cm the same grade holds 9 to 12. You have not halved the dose you need; you have halved what each kilogram will do, so the dose roughly doubles.
There is a second effect that costs more. Divalent ions — calcium and magnesium, both present in seawater at several hundred milligrams per litre — cross-link the polymer at the surface and form a hard, less permeable skin. The granule stops swelling while the core is still dry. In a beaker you see particles that stay the same size for ten minutes and then never grow.
| Conductivity | Expected absorption | Dose guide | Comment |
|---|---|---|---|
| Under 15 mS/cm | 20-25 g/g | 20-25 kg/m³ | Normal inland liquor |
| 15-25 mS/cm | 15-19 g/g | 25-30 kg/m³ | Brackish influence |
| 25-35 mS/cm | 11-15 g/g | 30-38 kg/m³ | Coastal, tidal groundwater |
| Above 35 mS/cm | 8-11 g/g | 38-50 kg/m³ | Consider dilution or a different route |
Those bands assume a standard grade. A grade with a higher degree of neutralisation tolerates divalent ions better, and a coarser particle size wets through more slowly but forms a less brittle skin, which matters at the top of this table.
At 40 mS/cm the cheapest answer is often to add water. Diluting the leachate 1:1 with treated effluent or with low-conductivity site water halves the ionic strength, roughly restores absorption to 18 grams per gram, and cuts the polymer dose back to around 27 kilograms per cubic metre on the blended volume.
Run the arithmetic before rejecting it as madness. One cubic metre of leachate at 46 kilograms per cubic metre costs 101 dollars in polymer. Two cubic metres of blend at 27 kilograms costs 119 dollars in polymer and gives you two cubic metres of gel to haul instead of one. On a short haul with a low gate rate, blending is worse. On a long haul where the polymer is the dominant cost, it can be better. There is no universal answer, and anyone who gives you one without asking about your haul distance has not done the sum.
Do not keep raising the dose past the point where the batch stops improving. At a coastal site that went to 55 kilograms per cubic metre, the gel came out as a rubbery mass with visible dry powder inside, the mixer stalled twice, and three tankers were rejected for free liquid. The extra polymer had gone into unhydrated lumps, not into the water.
Do not use fresh water to wash the mixing tank and then dump the washings into the next batch without accounting for the dilution. It is the same arithmetic as deliberate blending, just unmeasured.
Do not assume the number is stable. Tidal groundwater moves. A spring tide with a high water table can push conductivity up 8 to 12 mS/cm in a week, and a dry spell can pull it back. A weekly reading logged against the tide table is not excessive at a site this close to the water.
If the salt is structural — seawater in the groundwater, not a temporary intrusion — then plan for it rather than fighting it batch by batch. That means a dose table with four bands, a mixer sized for a thicker batch, and a budget line that assumes 35 kilograms per cubic metre rather than 22. It also means checking the trailer loading: salt-laden gel is denser, at 1.3 tonnes per cubic metre and above, which eats into your axle allowance faster than the volume suggests.
The high-tolerance polymer grades are worth a bench trial at these conductivities, because the difference between a standard and a salt-tolerant grade at 40 mS/cm can be 30 percent of the dose — which at 12,000 cubic metres a year is not a rounding error.
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