Distinguish useful conduction, leakage and a changed response law
A synthetic heater maintains a hot body while a cold calorimeter and ambient stay at 300 K. The first hot temperature is 400 K. In a linear model the useful path has conductance K and the leak has L, both in W/K. Heater power is 100(K+L); independent cold-side calorimetry reads 100K. The two measurements must have genuinely independent calibration premises.
Learning outcome: Fit useful and leak conductances with explicitly distinct records. Freeze both changed-temperature predictions, inspect the unused record, and propagate the direct prediction bound without double counting shared errors.
Starting recap
Review logarithmic integrals, equilibrium states, absolute temperature and the first-law work convention. State the domain and distinguish calibration data from unused validation.
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Try
For K=2, L=1, first heater/cold records are 300/200 W. The linear fresh prediction is 600 W, while the fitted quadratic leak predicts 800 W. The supplied generator yields 600 W, supporting the linear family for this test but not independently proving calibration or real-device behavior.
Open the experimentPredict
Which extra record separates K from L after one heater power reading?
Experiment
Fit useful and leak conductances with explicitly distinct records. Freeze both changed-temperature predictions, inspect the unused record, and propagate the direct prediction bound without double counting shared errors.
Separate a heat leak from useful conduction
Worked teaching model · synthetic values · Cold body and ambient both fixed300 K. Synthetic first records at hot400 K: heater power100(K+L), cold calorimeter100K. These independently calibrated readings identify K and L in the linear-leak model. A fresh hot500 K record tests it against a quadratic leak fitted at400 K. Controls reveal generators, not independent calibration evidence.
Reset keeps your prediction, captures and practice history.
Equal calibration record does not ensure equal extrapolation
Graph axes rescale independently; read units and values, not screen angles. 1: linear leak fitted at 400 K (solid).2: quadratic leak fitted at 400 K (dashed).3: unused 500 K heater record (open-circle marked location). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Equal calibration record does not ensure equal extrapolation
linear leak fitted at 400 K
| hot temperature (K) | heater power (W) |
|---|---|
| 300 | 0 |
| 302.5 | 7.5 |
| 305 | 15 |
| 307.5 | 22.5 |
| 310 | 30 |
| 312.5 | 37.5 |
| 315 | 45 |
| 317.5 | 52.5 |
| 320 | 60 |
| 322.5 | 67.5 |
| 325 | 75 |
| 327.5 | 82.5 |
| 330 | 90 |
| 332.5 | 97.5 |
| 335 | 105 |
| 337.5 | 112.5 |
| 340 | 120 |
| 342.5 | 127.5 |
| 345 | 135 |
| 347.5 | 142.5 |
| 350 | 150 |
| 352.5 | 157.5 |
| 355 | 165 |
| 357.5 | 172.5 |
| 360 | 180 |
| 362.5 | 187.5 |
| 365 | 195 |
| 367.5 | 202.5 |
| 370 | 210 |
| 372.5 | 217.5 |
| 375 | 225 |
| 377.5 | 232.5 |
| 380 | 240 |
| 382.5 | 247.5 |
| 385 | 255 |
| 387.5 | 262.5 |
| 390 | 270 |
| 392.5 | 277.5 |
| 395 | 285 |
| 397.5 | 292.5 |
| 400 | 300 |
| 402.5 | 307.5 |
| 405 | 315 |
| 407.5 | 322.5 |
| 410 | 330 |
| 412.5 | 337.5 |
| 415 | 345 |
| 417.5 | 352.5 |
| 420 | 360 |
| 422.5 | 367.5 |
| 425 | 375 |
| 427.5 | 382.5 |
| 430 | 390 |
| 432.5 | 397.5 |
| 435 | 405 |
| 437.5 | 412.5 |
| 440 | 420 |
| 442.5 | 427.5 |
| 445 | 435 |
| 447.5 | 442.5 |
| 450 | 450 |
| 452.5 | 457.5 |
| 455 | 465 |
| 457.5 | 472.5 |
| 460 | 480 |
| 462.5 | 487.5 |
| 465 | 495 |
| 467.5 | 502.5 |
| 470 | 510 |
| 472.5 | 517.5 |
| 475 | 525 |
| 477.5 | 532.5 |
| 480 | 540 |
| 482.5 | 547.5 |
| 485 | 555 |
| 487.5 | 562.5 |
| 490 | 570 |
| 492.5 | 577.5 |
| 495 | 585 |
| 497.5 | 592.5 |
| 500 | 600 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
quadratic leak fitted at 400 K
| hot temperature (K) | heater power (W) |
|---|---|
| 300 | 0 |
| 302.5 | 5.0625 |
| 305 | 10.25 |
| 307.5 | 15.5625 |
| 310 | 21 |
| 312.5 | 26.5625 |
| 315 | 32.25 |
| 317.5 | 38.0625 |
| 320 | 44 |
| 322.5 | 50.0625 |
| 325 | 56.25 |
| 327.5 | 62.5625 |
| 330 | 69 |
| 332.5 | 75.5625 |
| 335 | 82.25 |
| 337.5 | 89.0625 |
| 340 | 96 |
| 342.5 | 103.0625 |
| 345 | 110.25 |
| 347.5 | 117.5625 |
| 350 | 125 |
| 352.5 | 132.5625 |
| 355 | 140.25 |
| 357.5 | 148.0625 |
| 360 | 156 |
| 362.5 | 164.0625 |
| 365 | 172.25 |
| 367.5 | 180.5625 |
| 370 | 189 |
| 372.5 | 197.5625 |
| 375 | 206.25 |
| 377.5 | 215.0625 |
| 380 | 224 |
| 382.5 | 233.0625 |
| 385 | 242.25 |
| 387.5 | 251.5625 |
| 390 | 261 |
| 392.5 | 270.5625 |
| 395 | 280.25 |
| 397.5 | 290.0625 |
| 400 | 300 |
| 402.5 | 310.0625 |
| 405 | 320.25 |
| 407.5 | 330.5625 |
| 410 | 341 |
| 412.5 | 351.5625 |
| 415 | 362.25 |
| 417.5 | 373.0625 |
| 420 | 384 |
| 422.5 | 395.0625 |
| 425 | 406.25 |
| 427.5 | 417.5625 |
| 430 | 429 |
| 432.5 | 440.5625 |
| 435 | 452.25 |
| 437.5 | 464.0625 |
| 440 | 476 |
| 442.5 | 488.0625 |
| 445 | 500.25 |
| 447.5 | 512.5625 |
| 450 | 525 |
| 452.5 | 537.5625 |
| 455 | 550.25 |
| 457.5 | 563.0625 |
| 460 | 576 |
| 462.5 | 589.0625 |
| 465 | 602.25 |
| 467.5 | 615.5625 |
| 470 | 629 |
| 472.5 | 642.5625 |
| 475 | 656.25 |
| 477.5 | 670.0625 |
| 480 | 684 |
| 482.5 | 698.0625 |
| 485 | 712.25 |
| 487.5 | 726.5625 |
| 490 | 741 |
| 492.5 | 755.5625 |
| 495 | 770.25 |
| 497.5 | 785.0625 |
| 500 | 800 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
unused 500 K heater record
| hot temperature (K) | heater power (W) |
|---|---|
| 500 | 600 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
| Quantity | Value | Unit |
|---|---|---|
| Calibration heater power at 400 K | 300 | W |
| Independent cold calorimeter at 400 K | 200 | W |
| Inferred useful conductance | 2 | W/K |
| Inferred linear leak conductance | 1 | W/K |
| Frozen linear prediction at 500 K | 600 | W |
| Quadratic-leak alternative prediction at 500 K | 800 | W |
| Fresh generated heater power | 600 | W |
| Useful-conductance error bound for ±2 W calorimetry | 0.02 | W/K |
| Leak-conductance error bound for each reading ±2 W | 0.04 | W/K |
| Direct heater prediction bound from ±2 W first heater record | 4 | W |
An independent cold-side record separates useful conduction from leak, and a new temperature tests the leak law.
A single heater record constrains K+L only. Independent cold-side calorimetry gives K; subtraction yields L. The quadratic alternative L deltaT²/(100 K) shares the first calibration but differs at the fresh temperature. For independent absolute errors ε in each first record, K error≤ε/100 and L error≤2ε/100; the direct total heater prediction is twice the first heater record, so its bound is 2ε, not a sum treating fitted K and L errors as independent. Add fresh-record error when judging residuals. Shared calibration gain remains unidentifiable without independent calibration.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
An independent cold-side record separates useful conduction from leak, and a new temperature tests the leak law.
A single heater record constrains K+L only. Independent cold-side calorimetry gives K; subtraction yields L. The quadratic alternative L deltaT²/(100 K) shares the first calibration but differs at the fresh temperature. For independent absolute errors ε in each first record, K error≤ε/100 and L error≤2ε/100; the direct total heater prediction is twice the first heater record, so its bound is 2ε, not a sum treating fitted K and L errors as independent. Add fresh-record error when judging residuals. Shared calibration gain remains unidentifiable without independent calibration.
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Which system boundary, reference path, constitutive law or independently calibrated record supports this entropy inference?
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