Solids Handling · Study · FE Chemical · FE → PE Prep
Solids Handling
3% of exam
Particle properties and size distributions, surface and bulk forces, solids processing (crushing, grinding, and crystallization), and transportation and storage (belt and pneumatic conveying, slurries, tanks, and hoppers).
2 concepts
A. Particle properties
Particle Size, Distributions and Comminution
How to describe a particle-size distribution, compute the right mean diameter, relate surface area to size, and apply the Rittinger/Kick/Bond grinding-energy laws and crystallization basics.
A powder is never one size — it is a ·distribution· of sizes, and almost every property you care about (how fast it dissolves, how it settles, how much it costs to grind, how a catalyst performs) depends on which feature of that distribution you weight by. The single most common FE error in solids work is quoting an arithmetic average diameter when the physics demands a surface- or volume-weighted mean, and they can differ by tens of percent. This concept builds the vocabulary the exam expects: density functions fN,fV
and cumulative functions
FN,FV
, the family of mean diameters, the inverse-size scaling of surface area, and the energy it costs to make small particles out of big ones. The handbook gives the distribution and mean-diameter machinery in the ·Chemical Engineering — Solids Processing· section (particle-size distributions), and it does print a crushing/grinding equipment-selection table and a hydrate-formation phase diagram for crystallization. What it does ·not· tabulate are the specific comminution energy-law equations (Rittinger/Kick/Bond and the work index) and the crystallization supersaturation/yield relations, so memorize those from references such as Perry's or McCabe.
Density and cumulative distribution functions
Two equivalent pictures describe a PSD. The **density function** f tells you the fraction of the sample falling in a narrow band of size around x; the **cumulative function** F tells you the fraction smaller than x, so F rises monotonically from 0 to 1 and f=dF/dx. Crucially, the answer depends on the ·basis·: a number basis (fN,FN, counting particles) and a volume or mass basis (fV,FV, weighting by particle volume) give very different curves, because one large particle carries the mass of thousands of fines. In discrete form the size range is split into m sub-ranges, each with a mean size xi and a fraction ΔFNi (number) or ΔFVi (volume); every sum of fractions is 1. The descriptors d10,d50,d60 — the sizes at which 10%, 50%, 60% of the sample is smaller — come straight off the cumulative curve, and d60/d10 is the uniformity coefficient.
f=dxdF,F(x)=∫0xfdx,i=1∑mΔFi=1
Mean diameters depend on what you weight by
There is no single 'average' particle size — there is a family of means, each correct for a different purpose. The **number-length (mean-length) diameter** XML=∑xiΔFNi is the plain number average. The **Sauter (surface-mean) diameter** XSM is the diameter of a sphere with the same surface-area-to-volume ratio as the whole sample; it is the right size for any rate process governed by surface — dissolution, drying, catalysis, two-film mass transfer — and it is the one examiners most often want. The **volume (mass-mean) diameter** XMV weights toward the coarse end and governs how mass is distributed. Because XSM and XMV over-weight large particles relative to XML — and the Sauter mean leans on the coarse tail most heavily of all — you will always find XML≤XMV≤XSM for the same powder (a power-mean/moment-ratio result, with equality only for a perfectly monodisperse powder); quoting the wrong one is a classic trap.
For a sphere of diameter d, surface area is πd2 and volume is πd3/6, so the surface area per unit volume of solid is av=6/d and per unit mass am=6/(ρpd). The key qualitative fact for the exam: **halve the diameter and you double the specific surface area**. Real particles are not spheres, so we fold in the **sphericity** Φs — the ratio of the surface area of the equal-volume sphere to the actual particle surface area (Φs=1 for a sphere, ≈0.6–0.8 for crushed solids). The surface area per volume becomes av=6/(Φsd), which is exactly the Φs that appears in the Ergun packed-bed equation. This 1/d scaling is why grinding to a finer product is so valuable for reaction and dissolution rates — and so expensive in energy, as the next section shows.
av=Φsd6,am=Φsρpd6,Φs=actual particle surface areasurface area of equal-volume sphere
Comminution and the energy laws
Size reduction (crushing, grinding, milling) is notoriously inefficient — a few percent of the input energy actually creates new surface. The three classical laws all come from the same differential statement that the energy to make a small reduction dx scales as a power of size, dE/dx=−Cx−n, integrated between feed and product sizes. **Rittinger's law** (n=2) says energy is proportional to the ·new surface created· and works best for fine grinding. **Kick's law** (n=1) says energy depends only on the size ·ratio· and suits coarse crushing of large pieces. **Bond's law** (n=1.5) sits between them and, with its empirical work index, is the workhorse for the rod- and ball-mill range that dominates industrial practice. Notice all three predict that pushing to ever-finer products costs disproportionately more energy.
Bond cast his law in a form built around a measurable material property, the **work index** Wi — defined as the energy (in kWh per short ton) needed to reduce a very large feed to a product that is 80% finer than 100 micrometers. With the feed and product characterized by their 80%-passing sizes F80 and P80 in micrometers, the specific grinding energy follows the equation below; multiplying by the mass throughput gives the required mill power. Typical work indices run from about 6–7 kWh/short ton for genuinely soft materials like gypsum or clay, ~11.6–12.7 for limestone, to 15+ for hard rocks like granite or trap rock. Watch the units — Bond's classic constants assume micrometers and short tons (2000 lb), so an SI throughput in t/h must be converted, or the result will be off by the ton-conversion factor.
Crystallization: supersaturation, nucleation, growth, and yield
Crystallization makes particles instead of breaking them, and its driving force is **supersaturation** — a solution holding more solute than its equilibrium solubility C∗. The supersaturation ratio S=C/C∗ (or the difference ΔC=C−C∗) drives two competing rate processes: **nucleation** (birth of new crystals, very steep in S) and **growth** (enlargement of existing crystals). Operating inside the ·metastable zone· — modest supersaturation, reached by cooling or evaporation — favors growth over nucleation and yields large, pure, easily filtered crystals; blow past it and you get a shower of fines. The recoverable **yield** comes from a mass balance: solute in feed minus solute left dissolved at the final solubility equals solute crystallized, and if the solid is a hydrate you must charge the crystal phase with its water of crystallization (the hydrate-to-anhydrous molar-mass ratio) and credit any evaporated solvent. That mass balance, not a memorized formula, is what the exam tests.
S=C∗C,ΔC=C−C∗,mcrystal=anhydrous mass fraction of crystal(solute fed)−(solute in mother liquor)
Exam strategy
First decide the **basis** the question wants: number, surface, or volume/mass. If the process is rate- or surface-limited, reach for the Sauter mean XSM; if it is about mass holdup, use XMV. Build a small table of xi,ΔFNi,xi2ΔFNi,xi3ΔFNi and the means fall out of column sums — do not average the diameters directly. For specific surface area, remember the lone fact a=6/(Φsd) and that it scales as 1/d. For comminution, identify the regime (fine → Rittinger, coarse → Kick, mid-range/work-index data → Bond) and keep Bond's micrometre-and-short-ton units straight. For crystallization, draw the box, label solute and water on every stream, and don't forget the water of crystallization. Scope note: this concept is filed under ·A. Particle properties·, but its comminution (crushing/grinding) and crystallization halves belong to the NCEES Solids spec sub-area ·B. Processing· — treat this single entry as spanning both A and B so the B-area outline is not left uncovered.
Problem. A powder is split into four number sub-ranges with mean sizes and number fractions: xi=50,100,150,200μm and ΔFNi=0.40,0.30,0.20,0.10. Find the number-length, Sauter, and mean-volume diameters.
Solution. Build the column sums.
∑xiΔFNi=50(0.40)+100(0.30)+150(0.20)+200(0.10)=20+30+30+20=100
XSM=∑xi2ΔFNi∑xi3ΔFNi=12,5001,825,000=146μm
Specific surface area of a ground quartz
Problem. Quartz (ρp=2650kg/m3) is ground to a Sauter mean diameter of 50μm. Estimate the specific surface area per unit mass treating particles (a) as spheres and (b) with sphericity Φs=0.80
Grinding power from Bond's work index
Problem. Limestone with a Bond work index Wi=11.6kWh/short ton is reduced from a feed F80=6500μm
Yield from cooling crystallization of a hydrate
Problem. 1000kg of solution containing 30wt% Na2CO3
Common pitfalls
•Averaging diameters directly. The Sauter and mean-volume diameters are ratios of higher moments (∑x3/∑x2, etc.) — never just ∑xiΔFi. Build moment columns and divide.
•Confusing number and volume/mass basis. fN,FN count particles; fV,FV
•Using the wrong mean for the physics. Surface-rate processes (dissolution, catalysis, two-film mass transfer) need the surface (Sauter) mean; mass holdup needs the volume mean. The exam picks the diameter on purpose.
•Forgetting sphericity. Real crushed solids have Φs<1, so the specific surface area is 6/(Φsd), larger than the equal-volume sphere — dividing by Φs
•Mixing Bond units. The classic Bond equation uses micrometres for F80,P80 and kWh per short ton; an SI metric-tonne throughput must be converted, or the power is wrong by the ton factor (1 short ton = 0.907 t).
•Picking the wrong comminution law. Rittinger is for fine grinding (new-surface energy), Kick for coarse crushing (size-ratio energy), Bond for the mid/work-index range — using one regime's law in another's regime gives a misleading energy.
•Crystallization mass balance ignoring water of crystallization or evaporation. A hydrate locks up solvent in the crystal, and any evaporated water leaves the mother liquor — both shift the yield substantially if omitted.
References
NCEES FE Reference Handbook — Chemical Engineering (Solids Processing: particle-size distributions and mean diameters)
Perry's Chemical Engineers' Handbook — particle-size statistics, comminution energy laws and work index, crystallization
McCabe, Smith & Harriott, Unit Operations of Chemical Engineering — size reduction and crystallization fundamentals
C. Transportation and storage
Solids Conveying, Slurries and Storage
Belt and pneumatic conveying, slurry critical-deposition velocity, hopper mass- versus funnel-flow, arching and rat-holing, and the angle of repose that ties bulk-solid behavior together.
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= number fraction in that sub-range (dimensionless, summing to 1).
Diameter of a sphere with the same surface-to-volume ratio as the sample; use for surface-rate processes (dissolution, drying, catalysis). ΔFVi = volume/mass fraction in sub-range i.
Volume-weighted mean; governs mass distribution. Always XML≤XMV≤XSM for the same powder.
Surface area per unit volume (av, m2/m3) or per unit mass (am, m2/kg). Scales as 1/d: halving size doubles area. ρp = particle density.
Φs
= sphericity (0–1): area of equal-volume sphere divided by actual surface area; the same
Φs
used in the Ergun equation.
Rittinger,
n=1
Kick,
n=1.5
Bond.
x
= particle size;
C
= material constant.
Energy ∝ new surface created; best for fine grinding. x1 feed, x2 product size; KR Rittinger constant.
Energy depends only on size reduction ratio; best for coarse crushing. KK = Kick constant.
Intermediate law for rod/ball mills. KB = Bond constant tied to the work index.
Specific energy in kWh/short ton; Wi = Bond work index (kWh/short ton), F80,P80 = 80%-passing feed and product sizes in μm. Mill power =W× mass throughput.
Crystallization driving force. C = actual concentration, C∗ = equilibrium solubility at the operating temperature. S>1 required for nucleation and growth.
Laminar (Re≤1) settling/classification of a particle of diameter d; ρp,ρf = particle and fluid density, μ = fluid viscosity. Ties particle size to separation.
here reflects the surface mean over-weighting the coarse tail; all three lie inside the 50–200
μ
m range, as they must.
.
Solution. (a) Sphere: am=ρpd6=2650×50×10−66=0.13256=45.3m2/kg.
(b) With sphericity: am=Φsρpd6=0.8045.3=56.6m2/kg.
Answers: am≈45.3m2/kg (spheres), 56.6m2/kg (Φs=0.80). Sanity check: rough crushed grains expose more surface than the equal-volume sphere, so dividing by Φs<1 correctly raises the area; ∼45 m2/kg (≈0.045 m2/g) is typical for a fine sand.
am=Φsρpd6=0.80(2650)(50×10−6)6=56.6m2/kg
to a product
P80=100μm
at a throughput of
50short ton/h
. Find the specific energy and the mill power.
Solution. Specific energy from Bond:
W=10(11.6)(1001−65001)=116(101−80.61)=116(0.1000−0.01240).
W=116(0.08760)=10.16kWh/short ton.
Power =W×m˙=10.16tonkWh×50hton=508kW.
Answers: W=10.16kWh/short ton (the full-precision value; W rounds to 10.2, but carrying 10.16 is what gives 10.16×50=508 kW), P=508kW. Sanity check: units kWh/ton × ton/h = kW; the feed term contributes little (1/6500 is small), so almost all the energy is spent making the fine product — exactly the inefficiency the energy laws predict.
W=10Wi(P801−F801)=10.16kWh/short ton
is cooled so the salt crystallizes as the decahydrate Na
2
CO
3⋅
10H
2
O. The final solubility is
12.5g
anhydrous Na
2
CO
3
per
100g
water, and
5%
of the original water evaporates. Find the mass of crystals. (Molar masses: anhydrous
=106
, decahydrate
=286g/mol
.)
Solution. Feed: 0.30(1000)=300kg anhydrous Na2CO3 and 700kg water. Water lost to evaporation =0.05(700)=35kg, leaving 665kg water in the system.
Let C = mass of decahydrate crystals. Anhydrous fraction of the crystal =106/286=0.3706; water of crystallization fraction =180/286=0.6294.
Anhydrous left in mother liquor =300−0.3706C; free water in mother liquor =665−0.6294C. The solubility constraint is
665−0.6294C300−0.3706C=10012.5=0.125.
300−0.3706C=0.125(665)−0.125(0.6294)C=83.13−0.07868C.
300−83.13=(0.3706−0.07868)C⇒216.9=0.2919C⇒C=743kg.
Answer: C≈743kg of Na2CO3⋅10H2O. Sanity check: anhydrous in crystals =0.3706(743)=275kg, leaving 25kg in 197kg of mother-liquor water, ratio 0.125 — matches the solubility exactly.
665−0.6294C300−0.3706C=0.125⇒C=743kg
weight by volume. The two cumulative curves and their means differ greatly because one coarse particle equals thousands of fines by mass.