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ENGINEERING Hydraulics class, taught straight. Pump curves, head loss, sinkhole cascades. The Heart Lab’s mechanical cross-lab — this is the room where you don’t need cardiology to run a lift station.
LESTER’S LAB
ELUSK · OPA Building 10 · College X
HYDR 301 · Section 4.10.1
OPA 4.10.1 · College X · ELUSK · Hydraulics & Drainage

Pumps, Head, & the Clarksville Cascade

A pump has a curve. A pipe has a system. They meet at one point — that’s the operating point. Move the pipe, the point moves. Choke the line, the pump fights harder for less. Stack three sinkholes in series with check valves between them and you have stormwater engineering in dirt and concrete instead of muscle and blood. The Heart Lab’s cross-lab. Same physics, two doors, only one direction.

3
Sinkholes
1
Operating Point
Check Valves
1
PRV (it has one)
Tab I · The Foundational Concept (think water tower)

Head & Head Loss

First — What is “Head”? (think water tower)

You’ve seen a water tower — the tall standpipe with a tank on top sitting at the edge of town. The HEIGHT of the water surface in that tank is the head that pressurizes every faucet in town. A hundred-foot-tall water tower delivers about 43 psi at ground level. The pressure at the bottom comes from one thing: how tall the column of water above it is. That’s head.

In hydraulics, every pressure can be re-expressed as “how tall a water tower would give me that pressure?” 20 feet of head ≈ 8.7 psi. 100 feet of head ≈ 43.3 psi. Engineers use feet of water column because it’s the most intuitive for pumps and pipes — you’re always thinking about lifting water to a height.

When you see shutoff head (the tallest water tower this pump can match), static lift (the actual height the water has to climb), or head loss (the height that friction eats away from the system), the unit is always feet of water column. A pump is an artificial water tower — it gives you the equivalent of N feet of elevation without anyone having to build the tower. Everything else in this lab is reading that one idea in different lights.

HEAD (height) 100 ft WATER water surface 43 psi 100 ft of water column — 43 psi at the base head is the height of water above the point you tap into

Once you can picture head as “how tall a water tower would give me this pressure,” the next idea drops into place: friction in the pipe steals head as the water moves. A hundred-foot tower delivers 43 psi at ground level — until you make the water flow through a thousand feet of pipe to get to the house, and friction eats some of that 43 psi along the way. That eaten part is called head loss (hf), and the equation that governs it is one of the most-used in civil engineering. Same unit (feet of water column). Same intuition.

100 ft WATER 43 psi house 35 psi 1,000 ft h_f = 8.4 ft friction tax across the pipe (feet of water column)
Tower Height (H)100 ft
The tank's water surface above ground. Head IS this height. 100 ft ≈ 43 psi of static pressure at the base. Raise it and the gauge climbs.
Distance to House (L)1,000 ft
Longer pipe = more wall to drag against. Watch the house pressure drop as you slide it further away. Loss is linear with length.
Pipe Diameter (D)8 in
Bigger pipe = lower velocity at the same flow = much less loss. Head loss scales as 1/D⁵. Doubling diameter cuts loss by 32×.
Flow Rate (Q)400 gpm
No flow, no friction. Double the flow through the same pipe and the friction loss quadruples — velocity is squared in the equation.
Friction Factor (f, Moody)0.020
Pipe roughness. Smooth new PVC ~0.014, average steel ~0.020, old cast iron ~0.030, rough concrete ~0.040. Watch the pipe color rust over as you crank it up.
House Service Pressure

The Equation, Plain

hf  =  f · (L ÷ D) · (v² ÷ 2g)

Read it left to right: friction factor (how rough the pipe is) times length over diameter (the shape of the pipe) times velocity squared over twice gravity (the kinetic energy you’re pushing per pound of water). The product is feet of head — the height of water column your pump has to provide just to push the flow through. No flow, no friction. Faster flow, way more friction. Bigger pipe, dramatically less friction.

Why D⁵ Matters More Than You Expect

Velocity v = Q/A = 4Q/(πD²). Plug that into Darcy-Weisbach and v² becomes 16Q²/(π²D⁴). The (L/D) factor adds another 1/D. Total: head loss scales as L·Q²/D⁵. Bumping diameter from 6″ to 8″ isn’t a 33% improvement — it’s a (8/6)⁵ = 4.2× reduction in head loss. This is why upsizing a stuck system is often cheaper than upsizing the pump.

Tab 1 of 4Head & Head Loss
Tab II · The Operating Point Is Where Two Curves Meet

The Pump Curve

A pump doesn’t deliver one flow at one pressure. It delivers a curve — high flow at low head, low flow at high head, and a whole family of operating possibilities in between. The piping system you bolt onto the pump has its own curve — mostly static lift plus friction loss that grows with the square of velocity (you just learned that in Tab I). Where the two curves cross is the operating point. Move either curve and the operating point moves with it. That’s the whole shape of the conversation.

Lester
Director · College X ELUSK Hydraulics · 20+ years TDOT
The OPA canon’s pencil-and-yellow-pad engineer — Lester’s Legal-Sized Yellow Note Pad is the namesake of half the tool folders in the universe. Twenty-plus years of TDOT structures-and-hydraulics, the lab’s second-floor classroom where pump curves and head loss are just pump curves and head loss, no metaphor. Cardiology students cross the quad to take Lester’s class — the engineering students don’t cross back. Same physics, two doors, one direction.
“If you can sketch a pump curve and a system curve and find where they cross, you can have a real conversation about flow. If you can’t, you’re guessing at the pump catalog.”
 
FLOW Q (gpm) HEAD H (ft) PUMP SYSTEM OP 0 500 1000 0 50 100 SYSTEM LAYOUT 20 ft
Pump Shutoff Head100 ft
The head the pump produces at zero flow (closed valve, “deadhead”). Sets the height of the pump curve. Catalog spec.
Pump Max Flow900 gpm
The flow at zero head (free discharge). Sets the right edge of the pump curve. Larger pump = curve extends further right.
Static Lift20 ft
Vertical lift from suction water surface to discharge. Doesn’t change with flow — just sets where the system curve starts on the Y axis.
Friction Coefficient (K)0.00008
Friction losses grow with Q² (this is the same Darcy-Weisbach behavior from Tab I, rolled up into a single K coefficient for the whole system). Higher K = steeper system curve = pump fights harder for less flow.
Operating Point

What the Curves Tell You

Pump curve is the pump’s catalog promise: at flow Q, I’ll give you head H, as long as you keep me in this band. Falls from shutoff head (Q=0) to free discharge (H=0).
System curve is what the piping demands: to move flow Q through this layout, you’ll need head H. Starts at the static lift (the height you have to overcome regardless of flow) and climbs with Q².
Operating point is where the two cross — the one flow + head combination at which the pump’s supply equals the system’s demand. Below the OP the pump is under-pumping; above it the system can’t accept what the pump wants to give.
Move the pump (different size, different impeller) → pump curve shifts → OP moves. Change the piping (bigger diameter, less restriction) → system curve flattens → OP moves right (more flow, less head).

The Frank-Starling Echo (from the Heart Lab side)

In College VII, the Frank-Starling curve relates ventricular preload (filling) to stroke volume (output). Same shape as a pump curve. The body’s system curve is total peripheral resistance + arterial elasticity. The heart’s operating point is called “cardiac output” and lives in L/min instead of gpm. We don’t need to know that to run a lift station. They need to know this to understand a heart.

Tab 2 of 4The Pump Curve
Tab III · Real Tennessee Flood Practice

The Clarksville Sinkhole Cascade

Karst geology under Clarksville. A pump basin in the floodplain receiving runoff from a sinking stream upstream. The basin’s discharge point isn’t a river — it’s a sinkhole, and the geology can only swallow so much at a time. When sinkhole #1 caps out, the system has to pump overflow to sinkhole #2. When #2 caps, on to #3. Series pumps against head, storage-and-transfer, check valves at every stage so a backed-up sinkhole doesn’t reverse flow into the previous one. The reason it’s a cascade and not a single sinkhole + a river discharge: the Red River was rising during the design storm. The engineering had to absorb the load through bedrock infiltration rather than make the Red River’s flood worse. An engineer’s answer to the right-heart-lung-left-heart series-pump problem, written in dirt and concrete instead of muscle.

Map & Site Reference

The actual three-sinkhole site in Clarksville, Tennessee — Pleasant View / Sango area, about 9 km east of downtown. Site identified 2026-05-31 by walking the candidate cluster through Underground Pulse v0.1’s NED depression overlay against memory of the presenter’s slides. Engineering rationale: the Red River was rising during the event; rather than dump basin overflow into the river, the operator used the three-stage karst cascade to absorb the load through bedrock infiltration. Travis is still reaching out to the presenter for the slides and full attribution; the geometry below is from memory of his presentation cross-referenced to the published USGS data.

Latitude: 36.5426° N
Longitude: 87.2521° W
Confirmed 2026-05-31 by Travis via Underground Pulse v0.1 NED karst overlay — site is in the Pleasant View / Sango area of Clarksville, approximately 9 km east of city center.
Open in Google Maps →

Site coordinates confirmed. When the presenter’s slides arrive, the lab will add: full attribution by name, the surveyed per-sinkhole coords (currently the location pin is centered on the cluster), and the actual storm-event date and stage hydrograph. The cascade mechanism (three karst stages, Red River avoidance) is the canon teaching point and is locked.

PUMP BASIN floodplain storage P1 CV SINKHOLE #1 accepting P2 CV SINKHOLE #2 standby P3 CV SINKHOLE #3 standby CV = check valve (one-way) P = stage pump water level rises as upstream SH caps
StageStatePumpCV
SH-1AcceptingP1 → SH-1at outflow
SH-2StandbyP2 (engages when SH-1 saturated)between SH-1 & SH-2
SH-3StandbyP3 (engages when SH-2 saturated)between SH-2 & SH-3
Storm Intensity2-year event
Drag to escalate. 2-yr / 10-yr / 25-yr / 100-yr / 500-yr design storms. As intensity climbs, the basin fills faster than SH-1 can swallow, P2 kicks in, then P3.
SH-1 Karst Capacity8 cfs
How fast the geology can swallow. Karst features vary — flow rate observed during pump test, not designed.
SH-2 Karst Capacity10 cfs
Second sinkhole, typically higher capacity than the first because it’s sized to handle the overflow plus a margin.
SH-3 Karst Capacity12 cfs
Third sinkhole, the final outlet. Sized for the design event with a check valve protecting against any backflow during the recession limb.
Cascade Status

What This Is Really Solving For

Karst geology won’t give you a reliable single discharge point. The sinkhole you measured during dry weather might cap out in a 10-year storm. A single-point system has a single-point failure mode. The cascade is redundancy as engineering, not as luxury. SH-2 isn’t a backup — it’s the design’s acknowledgment that geology is variable. Check valves between stages mean a backed-up SH-2 doesn’t reverse-flood the basin. Pumps engage in sequence, not in parallel, because head climbs as you transfer to higher-elevation outlets.

The Heart Lab’s Series-Pump Twin

Right ventricle pumps to the lungs at low pressure (pulmonary circuit). Left ventricle pumps to the body at high pressure (systemic circuit). Same closed loop, sharing the same volume, two pumps in series. If the right falls behind, blood backs up into the venous system (peripheral edema). If the left falls behind, blood backs up into the pulmonary veins (pulmonary edema). The Clarksville cascade is a closed loop too, sized so that SH-3 can’t back up into SH-2 because of the CV between them. The body has no CV between right heart and lungs. That’s why heart failure floods the lungs while sinkhole cascade failure just spills basin water back to the floodplain.

Tab 3 of 4The Clarksville Cascade
Tab IV · The X → VII Seam, From the Engineer’s Side

Cross-Lab to the Heart

The Heart Lab’s asymmetry rule says: medical students visit engineering, engineers never visit the hospital. From the engineering side, that means this lab teaches the physics straight, and the cardiology students who walk in get the lesson without metaphor. Wing Ming had to learn light before he could fix an eye; a flood-pump operator doesn’t need cardiology to run a lift station. You’re already in the room they’re trying to find.

The Mapping Table (Engineer’s View)

Pump curveFrank-Starling curve. Both describe how a pump’s output responds to its input state.
System curveTotal peripheral resistance + arterial elasticity. Both are the load the pump fights.
Operating pointCardiac output. The one steady-state intersection in units of L/min instead of gpm.
Head loss in narrowed pipePressure rise from arterial stenosis. Same v² physics, biological pipe.
Check valveMitral, tricuspid, aortic, pulmonary valves. Same failure mode (doesn’t seat → backflow).
Series pumps with CVRight heart + lungs + left heart. Closed loop. The biology lacks the CV between right pump and lung circuit, which is why pulmonary edema is possible. The cascade has CVs at every stage, which is why basin overflow stays basin overflow.
Pressure relief valve (PRV)… does not exist on the biological side. This is the load-bearing absence the Heart Lab teaches.

What You Won’t Find Across the Quad

The Heart Lab is honest about what the analogy doesn’t cover: the heart is a biological pump, not a perfect mechanical one. It tires, it remodels under sustained load (hypertrophy), and its “pump curve” is responsive to nervous and hormonal control in ways a centrifugal pump isn’t. The math rhymes; the medicine doesn’t reduce to math. If you’re an engineer reading this, you’re looking at a teaching analogy — powerful where it lands, dishonest if pushed past where the math actually agrees.

About This Lab

Lester’s Lab is the first lab in College X / ELUSK. The faculty canonical: Elegant · Lucky · Ungovernable · Skilled · Khaos — ELON MUSK compressed (he took Twitter to X; we took ELON MUSK to ELUSK). The student backronym: Engineering · Land Use · Stormwater · & Karst — coined by a group of seniors building Underground Pulse as their senior project; they took the building name and back-fitted words that fit their domain. Same building, two readings, both real. The OPA tradition of close-words-that-mean-something-else — the kind that produced KELPT (Kept Showing U :P), DOSA (Denial of Service Attack / Delivery of Security Always), and DCV (Don't Crash Vehicles / Doctorate in Civic Voice).. Director: Lester — the canonical pencil-and-yellow-pad engineer whose namesake folders hold half the tools in the universe. The lab teaches hydraulics straight: pump curves, system curves, Darcy-Weisbach head loss, and the Clarksville sinkhole cascade as the worked example of series pumping against karst geology.

Cross-listed to The Heart Lab (4.7.1, College VII), one direction only. Cardiology students learn hydraulics here; engineering students don’t take cardiology there. The Heart Lab’s honored anchor Dr. Michael De Blakely (the roller-pump pioneer) is the historical bridge between the two rooms.

Cross-suite note — Pulse tools vs OPA labs: Streambed Pulse and Stream Environment Pulse are sister tools in development, not OPA labs — the Pulse Suite is the civic-tier websites (SnapBasin, Watershed Pulse, Quake Sim, Space Pulse, Quantum Pulse, and others), while OPA labs are the university courses. Same engineering pedigree underneath, different distribution channel. The Pulse tools are at hydraulictoybox.com and elsewhere; this lab is at opathorlokanuniversity.net.

Tab 4 of 4Cross-Lab to the Heart