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instrument mechanism / verified-clean
Rational Method Peak Runoff Calculator mechanism
The inspectable method record for Rational Method Peak Runoff Calculator, kept separate from implementation and qualification.
Model scope
The arithmetic and core Rational Method are valid under the stated unit assumptions. Verdict is NEEDS_REVIEW because the specification does not identify the local IDF source, return period, duration/time-of-concentration linkage, runoff-coefficient convention, interpolation policy, or jurisdiction-specific area limit. The honest label should say 'simplified Rational Method estimate for small, relatively homogeneous catchments' rather than treating 200 acres as a universal boundary.
- Q=CiA is the standard Rational Method relationship, but the specification omits the unit-conversion constant. In SI units, Q(m^3/s)=C·i(mm/h)·A(ha)/360; in US customary units, Q(ft^3/s)=1.008333333·C·i(in/h)·A(acres).
- Rainfall intensity i must correspond to the catchment time of concentration and the selected return period; accepting arbitrary IDF intensity without those constraints can produce an invalid peak-flow estimate.
- C must be a dimensionless, bounded runoff coefficient, normally 0<=C<=1, selected for the actual surface, soil, slope, and antecedent conditions. The specification does not define how mixed surfaces are area-weighted.
- The stated '<200 acre' applicability limit is not universal. Rational Method limits vary by jurisdiction and project standard; some standards use much smaller limits or permit larger areas only with additional checks.
- The specification calls for runoff-coefficient and local-IDF tables but does not identify their editions, geographic applicability, return period, duration, or interpolation rules.
Units and conventions
- Each vector explicitly states the intensity, area, and flow units; the production instrument must require an unambiguous unit system.
- C is dimensionless.
- For SI calculations, i is in mm/h, A is in hectares, and Q is in m^3/s, using the exact dimensional factor 1/360.
- For US customary calculations, i is in inches per hour, A is in acres, and Q is in ft^3/s, using 1 acre-inch per hour = 1.008333333 ft^3/s.
- IDF intensity values are assumed uniform over the catchment and applicable to a duration equal to the time of concentration.
Inspectable vector
One of 4 source-bound review vectors:
{
"inputs": {
"C": 0.9,
"surface_type": "impervious roof",
"i": 100,
"i_units": "mm/h",
"A": 2,
"A_units": "ha",
"output_units": "m^3/s"
},
"expected_outputs": {
"Q": 0.5,
"Q_units": "m^3/s"
},
"reference_data": {
"runoff_coefficient": {
"surface_type": "impervious roof",
"C": 0.9,
"source_convention": "widely tabulated standard value (ASCE/municipal Rational Method tables)"
},
"rainfall_intensity": {
"duration": "local IDF duration equal to time of concentration",
"i_mm_per_h": 100,
"source_convention": "user-supplied local IDF data; geographic source and return period must be specified"
},
"si_conversion_factor": {
"value": 360,
"meaning": "Q(m^3/s)=C*i(mm/h)*A(ha)/360",
"source_convention": "SI dimensional conversion from hectare and millimetre per hour"
}
},
"working": "Q = C*i*A/360 = 0.90*100*2/360 = 180/360 = 0.500 m^3/s. The C=0.90 value is used exactly as the tabulated impervious-roof entry."
}Failure boundary
BREAK_CLAIMED · SELF_FLAGGED
The specification has no unit-conversion or sign-convention definition, does not explicitly enforce the strict less-than-200-acre scope boundary, and permits extreme inputs that overflow ordinary arithmetic. It also has no true mathematical formula branch; only an applicability switch can be tested.
Other records
Sources and evidence
These pointers bind the page to evidence. They do not grant authority or collapse verification into deployment.
VERIFIED_LEDGER.jsonevidence-tranche7/tranche7-results.jsonBOUNDARY_HAZARD_CATALOG.json