Slurry concentration converter
Density, mass concentration and volume concentration — give any one and the other two follow. For mineral slurries, tailings, FGD liquor, dredged spoil, cement grout and other settling two-phase systems.
1. Material
2. Known quantity (pick one)
3. Result
4. Pipeline throughput
5. Deposition velocity
VD = FL·√( 2·g·D·(ρs/ρl − 1) ), with FL bilinearly interpolated off the Durand chart from d50 and Cv.
Durand only covers settling slurries. It was fitted to sand, gravel and coarse tailings in water, so it applies to heterogeneous (settling) systems, roughly d50 0.05–5 mm and Cv up to 20–25 %. Fine tailings, paste backfill and red mud are homogeneous or non-Newtonian — a “deposition velocity” does not exist for them, and a number from this formula would be meaningless.
The result is a floor, not a design value. VD is the point at which a bed just stops forming; practice keeps 10–30 % above it. Going much higher does not help either — wear and power climb faster than throughput.
Pressure drop is deliberately not calculated here. Durand’s hydraulic-gradient correlation can be tens of percent off on a real line, and a concrete number would mislead pump selection. Use the manufacturer’s curves or dedicated software.
6. Error amplification
Sensitivity dCw/dρ = ρs·ρl / (ρ²·(ρs − ρl)). The smaller the solids-to-liquid density gap and the thinner the slurry, the more a given density error is amplified — an intrinsic limit of inferring solids content from density, independent of which density meter you use.
7. Three things to confirm before you trust these numbers
① The solids density must be known and stable. Inferring solids content from density rests entirely on that one constant. Change the mineral, the blend ratio or the concentrate grade and ρs changes with it — Cw then drifts systematically while the density reading itself looks perfectly normal. Weight it by the actual blend for mixed feeds, or sample and measure periodically.
② Entrained air pulls every result low. Bubbles are a third phase (ρ≈0.0012) in what the maths treats as two; measured density comes out low and so do Cv and Cw. Aeration basins, pump suction under vacuum and runs after a free fall are the usual offenders. There is no computational fix — only tapping-point placement and pipework design.
③ Everything here is a cross-section average. Solids are not evenly distributed: coarse particles run along the invert and the section carries a concentration gradient. Where the meter sits and which side the sampling port opens can shift the reading noticeably. Horizontal runs are the worst; vertical runs are much better.
8. Formulas
9. Reference solids densities
| Material | ρs (g/cm³) | Material | ρs (g/cm³) |
|---|---|---|---|
| Quartz / silica sand | 2.65 | River / dredged sand | 2.65 |
| Tailings (silicate) | 2.65~2.75 | Limestone (calcite) | 2.71 |
| Dolomite | 2.85 | Feldspar | 2.56 |
| Kaolin | 2.60 | Gypsum (dihydrate) | 2.32 |
| Phosphate rock | 2.8~3.2 | Bauxite | 2.4~2.8 |
| Raw coal | 1.30~1.50 | Dense-medium magnetite | 4.9~5.2 |
| Magnetite | 5.17 | Hematite | 5.26 |
| Pyrite | 5.01 | Iron concentrate | 4.6~5.0 |
| Copper concentrate | varies with grade | Potassium chloride KCl | 1.99 |
| Sodium chloride NaCl | 2.16 | Portland cement | 3.15 |
| Fly ash | 2.1~2.4 |
Common literature values. Real materials vary with source, grade and impurities — measure when it matters.