temperature, time, solids, and heat-up candidates generated in Docker
Docker-Generated Kinetic Calibration
Kinetics Lab
A 3D kinetic calibration workspace for sewage-sludge HTL oil formation, aqueous products, char, gas, ash dissolution, nitrogen transfer, overcracking, and continuous-flow validation.
kinetic calibration runs selected
top modeled fit condition, still requiring measured mass and elemental closure
best modeled oil yield across the screening surface
350 C, 40 min, 10 wt% solids, 8 C/min heat-up
Oil formation window condition with 14.52% aqueous products, 22.73% char,5.44% gas, 51.4% ash dissolution, and 100% modeled mass closure.
- Oil N
- 4.78%
- Oil O
- 9.35%
- HHV
- 31.35 MJ/kg
- Energy recovery
- 78%
The CEJ kinetics source calibrated at 300 C and 350 C and validated at 370 C. This screen preserves that logic by forcing calibration anchors and a high-severity validation stress run.
The Docker selector picked 6 runs from 216 modeled candidates. Portfolio average oil yield is 40.73%, mass closure is 100%, and average overcrack index is 17.3. Pyomo-formulated six-run kinetic calibration package with 300 C, 350 C, 370 C, overcracking, ash-dissolution, and fast-continuous proxy gates; selected by deterministic category enumeration.
The top modeled condition is 320 C, 60 min, 20 wt% solids, 8 C/min heat-up. It is a kinetic fit target, not an operating recipe, until measured elemental balances and continuous-flow residence-time data match the same pathway.
RDKit marker molecules connect the kinetic lumps to lipid, protein, carbohydrate, oil-nitrogen, oxygenate, fuel-proxy, gas, and sulfur chemistry.
Ash dissolution and aqueous COD are modeled alongside oil yield because process water and dissolved minerals can become scale-up limits even when the oil-yield curve looks attractive.
Current kinetics decision
Fit kinetics before calling any HTL condition optimized
The new literature makes the next step clear: oil yield is not enough. The bench campaign needs time-resolved oil, aqueous, gas, char, ash, carbon, nitrogen, sulfur, and oxygen balances at 300 C, 350 C, and 370 C, then a fast heat-up continuous proxy. This page shows which runs should calibrate the lumped kinetic model before scale-up claims are promoted.
Four-lump sewage-sludge HTL kinetics with first-order ash dissolution and CHNSO balances at 8 C/min heat-up.
Reported modeled versus experimental pilot biocrude yield, showing why predictive models still need measured validation.
Continuous-reactor simulation yield anchor for tying reaction kinetics to residence time, geometry, heat transfer, and stress analysis.
Selected kinetic calibration package
Six runs to fit oil formation, overcracking, ash dissolution, and continuous behavior
300 C, 20 min, 20 wt% solids, 8 C/min heat-up
Oil 25.22%, aqueous 7.01%, char 25.61%, gas 1.92%, ash dissolution 15.5%, overcrack index 0.
350 C, 40 min, 10 wt% solids, 8 C/min heat-up
Oil 45.08%, aqueous 14.52%, char 22.73%, gas 5.44%, ash dissolution 51.4%, overcrack index 0.
370 C, 20 min, 20 wt% solids, 8 C/min heat-up
Oil 44.45%, aqueous 12.97%, char 24.95%, gas 5.07%, ash dissolution 37.7%, overcrack index 29.4.
370 C, 40 min, 10 wt% solids, 8 C/min heat-up
Oil 42.31%, aqueous 16.23%, char 22.02%, gas 7.67%, ash dissolution 61.2%, overcrack index 45.
320 C, 90 min, 15 wt% solids, 8 C/min heat-up
Oil 47.04%, aqueous 15.5%, char 19.88%, gas 4.9%, ash dissolution 64.9%, overcrack index 29.4.
350 C, 20 min, 20 wt% solids, 60 C/min heat-up
Oil 40.27%, aqueous 11.72%, char 25.44%, gas 3.78%, ash dissolution 30.3%, overcrack index 0.
Kinetic parameter ledger
Every rate constant is a hypothesis until measured against sludge-specific data
Solid organics to biocrude
- Ea
- 58 kJ/mol
- k350
- 0.055
- 370/300
- 3.8x
- Must fit
- oil-yield rise at 300 C and 350 C before validating at 370 C
Solid organics to aqueous organics
- Ea
- 52 kJ/mol
- k350
- 0.015
- 370/300
- 3.3x
- Must fit
- COD and nitrogen in process water as residence time increases
Solid organics to hydrochar
- Ea
- 64 kJ/mol
- k350
- 0.006
- 370/300
- 4.3x
- Must fit
- solid residue decline, fixed carbon, ash concentration, and char HHV
Solid organics to gas
- Ea
- 78 kJ/mol
- k350
- 0.003
- 370/300
- 5.9x
- Must fit
- CO2, methane, and light gas increase at high severity
Biocrude secondary cracking
- Ea
- 105 kJ/mol
- k350
- 0.003
- 370/300
- 11x
- Must fit
- loss of oil yield and rise of gas/aqueous products under long high-temperature holds
First-order ash dissolution
- Ea
- 45 kJ/mol
- k350
- 0.018
- 370/300
- 2.8x
- Must fit
- ash movement from solid residue to process water and equipment-fouling risk
Biocrude hydrotreating denitrogenation
- Ea
- 84 kJ/mol
- k350
- 0.02
- 370/300
- 6.8x
- Must fit
- stabilization, oxygen/sulfur/chlorine removal, and nitrogen-family disappearance during staged hydrotreating before fuel-quality claims
Kinetic surface averages
Temperature and time shift oil yield, oil carbon, gas, and overcracking together
- Oil
- 4.85%
- Water
- 1.47%
- Gas
- 1.16%
- Overcrack
- 0
- Oil
- 9.24%
- Water
- 2.8%
- Gas
- 1.3%
- Overcrack
- 0
- Oil
- 16.78%
- Water
- 5.1%
- Gas
- 1.55%
- Overcrack
- 0
- Oil
- 27.95%
- Water
- 8.56%
- Gas
- 1.96%
- Overcrack
- 0
- Oil
- 35.35%
- Water
- 10.91%
- Gas
- 2.28%
- Overcrack
- 0
- Oil
- 41.97%
- Water
- 13.15%
- Gas
- 2.64%
- Overcrack
- 15.8
- Oil
- 7.34%
- Water
- 2.12%
- Gas
- 1.28%
- Overcrack
- 0
- Oil
- 13.61%
- Water
- 3.95%
- Gas
- 1.52%
- Overcrack
- 0
- Oil
- 23.52%
- Water
- 6.88%
- Gas
- 1.93%
- Overcrack
- 0
- Oil
- 35.91%
- Water
- 10.7%
- Gas
- 2.55%
- Overcrack
- 0
- Oil
- 42.32%
- Water
- 12.87%
- Gas
- 2.99%
- Overcrack
- 0
- Oil
- 46.34%
- Water
- 14.62%
- Gas
- 3.53%
- Overcrack
- 21.2
- Oil
- 10.66%
- Water
- 2.97%
- Gas
- 1.47%
- Overcrack
- 0
- Oil
- 19.03%
- Water
- 5.34%
- Gas
- 1.87%
- Overcrack
- 0
- Oil
- 30.76%
- Water
- 8.78%
- Gas
- 2.5%
- Overcrack
- 0
- Oil
- 42.15%
- Water
- 12.53%
- Gas
- 3.38%
- Overcrack
- 0
- Oil
- 45.89%
- Water
- 14.32%
- Gas
- 4.04%
- Overcrack
- 0
- Oil
- 46.42%
- Water
- 15.74%
- Gas
- 4.92%
- Overcrack
- 29.5
- Oil
- 14.84%
- Water
- 4%
- Gas
- 1.76%
- Overcrack
- 0
- Oil
- 25.2%
- Water
- 6.91%
- Gas
- 2.38%
- Overcrack
- 0
- Oil
- 37.34%
- Water
- 10.61%
- Gas
- 3.29%
- Overcrack
- 0
- Oil
- 45.13%
- Water
- 14.01%
- Gas
- 4.59%
- Overcrack
- 0
- Oil
- 45.38%
- Water
- 15.61%
- Gas
- 5.64%
- Overcrack
- 6.9
- Oil
- 42.61%
- Water
- 17.28%
- Gas
- 7.15%
- Overcrack
- 42.9
- Oil
- 17.23%
- Water
- 4.59%
- Gas
- 1.96%
- Overcrack
- 0
- Oil
- 28.37%
- Water
- 7.73%
- Gas
- 2.71%
- Overcrack
- 0
- Oil
- 39.96%
- Water
- 11.47%
- Gas
- 3.81%
- Overcrack
- 0
- Oil
- 45.15%
- Water
- 14.72%
- Gas
- 5.39%
- Overcrack
- 0
- Oil
- 43.65%
- Water
- 16.41%
- Gas
- 6.75%
- Overcrack
- 13.5
- Oil
- 39.37%
- Water
- 18.44%
- Gas
- 8.71%
- Overcrack
- 52.3
- Oil
- 22.46%
- Water
- 5.88%
- Gas
- 2.48%
- Overcrack
- 13.9
- Oil
- 34.31%
- Water
- 9.41%
- Gas
- 3.57%
- Overcrack
- 20.4
- Oil
- 43.02%
- Water
- 13.11%
- Gas
- 5.15%
- Overcrack
- 29.9
- Oil
- 42.25%
- Water
- 16.42%
- Gas
- 7.61%
- Overcrack
- 44.6
- Oil
- 37.54%
- Water
- 18.69%
- Gas
- 9.79%
- Overcrack
- 75.7
- Oil
- 30.46%
- Water
- 21.69%
- Gas
- 12.78%
- Overcrack
- 100
Molecular anchors
Representative chemistry behind the kinetic lumps
Glucose C6H12O6
- Weight
- 73.8
- MW
- 180.156
- N atoms
- 0
- Hetero
- 6
Oleic acid C18H34O2
- Weight
- 60.5
- MW
- 282.468
- N atoms
- 0
- Hetero
- 2
Glycine C2H5NO2
- Weight
- 50.5
- MW
- 75.067
- N atoms
- 1
- Hetero
- 3
Indole C8H7N
- Weight
- 42.8
- MW
- 117.151
- N atoms
- 1
- Hetero
- 1
Pyridine C5H5N
- Weight
- 38.7
- MW
- 79.102
- N atoms
- 1
- Hetero
- 1
Acetic acid C2H4O2
- Weight
- 35.8
- MW
- 60.052
- N atoms
- 0
- Hetero
- 2
Hydrogen sulfide H2S
- Weight
- 34.7
- MW
- 34.083
- N atoms
- 0
- Hetero
- 1
Carbon dioxide CO2
- Weight
- 34.6
- MW
- 44.009
- N atoms
- 0
- Hetero
- 2
Dodecane C12H26
- Weight
- 34.5
- MW
- 170.34
- N atoms
- 0
- Hetero
- 0
Phenol C6H6O
- Weight
- 32.9
- MW
- 94.113
- N atoms
- 0
- Hetero
- 1
Ammonia H3N
- Weight
- 32.7
- MW
- 17.031
- N atoms
- 1
- Hetero
- 1
Methane CH4
- Weight
- 19.2
- MW
- 16.043
- N atoms
- 0
- Hetero
- 0
Kinetic modelling and elemental balances applied to sewage-sludge HTL
Open-access CEJ source for four-lump HTL kinetics, first-order ash dissolution, CHNSO balances, 300/350 C calibration, and 370 C validation.
Open sourceReaction mechanism and kinetics of hydrothermal liquefaction
2025 review supporting mechanism/kinetics framing and the need to understand product-distribution pathways.
Open sourceContinuous multiphase plug-flow reactor optimization for sewage-sludge HTL
Continuous PFR source tying kinetic modeling to mass, energy, momentum, and scale-up behavior.
Open sourceKinetic process model for sewage-sludge HTL in Aspen Plus
Pilot-validated process-model source reporting 31.4 wt% modeled biocrude versus 29 wt% pilot yield under varying residence times and temperatures.
Open sourceHydrotreatment kinetic model for sewage-sludge HTL biocrude
Energy & Fuels source for downstream kinetic modeling with distributed lumps and first-order reactions for sewage-sludge biocrude hydrotreatment.
Open sourceMild hydrotreatment as a stabilization step for nitrogen-rich sewage-sludge biocrude
Open-access pilot trickle-bed source showing useful stabilization boundaries near 240 C, strong chlorine/sulfur/oxygen relief, and persistent nitrogen conversion limits.
Open sourceContinuous slurry hydrotreating of sewage-sludge HTL biocrude
Pilot-scale upgrading source showing continuous slurry operation can remove sulfur/oxygen and much nitrogen, while long-run operability remains a gate.
Open sourceContinuous-reactor sludge HTL simulation with kinetics, CFD, and stress analysis
Continuous-reactor simulation source for coupling kinetic conversion with reactor geometry, flow, heat transfer, and mechanical stress.
Open sourcePilot-scale sewage-sludge HTL energy and micropollutant fate
Pilot-scale source showing why process-water matrices and contaminant fate need measured validation alongside kinetic product yields.
Open sourcekinetic outputs are calibration priorities, not commercial operating conditions, until oil, aqueous, gas, char, ash, nitrogen, and continuous-flow data close the same mass and elemental balances