Chloride Conservative Mass Balance Checker

Audit conservative dissolved chloride inventory with trapezoidal sampled mass-flux integration and independent final inventory; this tracer is not chlorine disinfectant, and groundwater/deposition inputs must be included externally.

Description

Dissolved chloride can act as a conservative tracer in a lake water budget.

Dissolved chloride can act as a conservative tracer in a lake water budget. Integrating sampled flow-concentration products predicts the inventory change for comparison with an independently observed final inventory.1

The tool returns integratedImportedChlorideKg, integratedExportedChlorideKg, predictedFinalChlorideInventoryKg, observedMinusPredictedResidualKg, withinClosureTolerance. The computation uses supplied observations and parameters rather than acquiring measurements.

When to use Chloride Conservative Mass Balance Checker

Use this for the following task: Audit conservative dissolved chloride inventory with trapezoidal sampled mass-flux integration and independent final inventory; this tracer is not chlorine disinfectant, and groundwater/deposition inputs must be included externally. Prepare observations and calibration parameters on the same unit and reporting basis.

How to use Chloride Conservative Mass Balance Checker and understand its results

  1. Prepare the measured quantities and supplied model parameters. Match the units and align paired lists before calculating.
  2. Enter timesDays, inflowM3PerDay, inflowChlorideMgPerLiter, outflowM3PerDay, outflowChlorideMgPerLiter, initialChlorideInventoryKg, observedFinalChlorideInventoryKg, closureToleranceKg according to the field table, then run the tool.
  3. Read integratedImportedChlorideKg, integratedExportedChlorideKg, predictedFinalChlorideInventoryKg, observedMinusPredictedResidualKg, withinClosureTolerance. Use the calculation below to interpret the selected mean or the model’s signs, units and comparison flags.
  4. Review the supplied assumptions and calibration before comparing or reporting the result.
Input fieldMeaningValue type and boundsRequirement
timesDaysTimes dayslist of numberRequired
inflowM3PerDayInflow m3 per daylist of numberRequired
inflowChlorideMgPerLiterInflow chloride mg per literlist of numberRequired
outflowM3PerDayOutflow m3 per daylist of numberRequired
outflowChlorideMgPerLiterOutflow chloride mg per literlist of numberRequired
initialChlorideInventoryKgInitial chloride inventory kgnumberRequired
observedFinalChlorideInventoryKgObserved final chloride inventory kgnumberRequired
closureToleranceKgClosure tolerance kgnumberRequired

Supply increasing times, aligned nonnegative flow/concentration records, nonnegative inventory measurements and closure tolerance. Reject a negative predicted final inventory and compare the absolute observed-minus-predicted residual with an inclusive tolerance.

massFlux kg/day=flow m³/day×chloride mg/L/1000; predictedFinal=initial+trapezoidIntegral(import)−trapezoidIntegral(export)

The symbols and boundary conditions refer to the supplied fields and the implementation described above.

Output fieldMeaningValue type
integratedImportedChlorideKgIntegrated imported chloride kgnumber
integratedExportedChlorideKgIntegrated exported chloride kgnumber
predictedFinalChlorideInventoryKgPredicted final chloride inventory kgnumber
observedMinusPredictedResidualKgObserved minus predicted residual kgnumber
withinClosureToleranceWithin closure toleranceboolean
json
{
  "input": {
    "timesDays": [
      0,
      1,
      2
    ],
    "inflowM3PerDay": [
      10,
      10,
      10
    ],
    "inflowChlorideMgPerLiter": [
      100,
      100,
      100
    ],
    "outflowM3PerDay": [
      5,
      5,
      5
    ],
    "outflowChlorideMgPerLiter": [
      200,
      200,
      200
    ],
    "initialChlorideInventoryKg": 10,
    "observedFinalChlorideInventoryKg": 11,
    "closureToleranceKg": 0.1
  },
  "output": {
    "integratedImportedChlorideKg": 2,
    "integratedExportedChlorideKg": 2,
    "predictedFinalChlorideInventoryKg": 10,
    "observedMinusPredictedResidualKg": 1,
    "withinClosureTolerance": false
  }
}

Limitations and assumptions

Chloride is distinct from chlorine disinfectant. Groundwater, deposition and other exchanges must be accounted for externally; closure alone does not establish measurement accuracy.

Numerical inputs must be finite. Input-shape and calculation checks do not establish measurement quality or the validity of a supplied calibration.

Alternative or Complementary methods

Choose Phosphorus Retention Coefficient when you need its operation: Close matched phosphorus inflow/outflow/storage budget to apparent retention; negative retention or ratios above one expose unmodeled exchange and are not clamped. Choose Dilution Capacity Low Flow for the complementary operation: Invert ideal complete mixing for an effluent flow capacity when receiving concentration < target < effluent; not a legal discharge allowance, mixing-zone model or ecological guarantee.

Background reference: Chloride Mass Balance in Streams to Estimate Recharge.

References

  1. Chloride Mass Balance in Streams to Estimate Recharge — U.S. Geological Survey

Similar or alternative tools

  • Phosphorus Retention Coefficient

    Close matched phosphorus inflow/outflow/storage budget to apparent retention; negative retention or ratios above one expose unmodeled exchange and are not clamped.

  • Dilution Capacity Low Flow

    Invert ideal complete mixing for an effluent flow capacity when receiving concentration < target < effluent; not a legal discharge allowance, mixing-zone model or ecological guarantee.

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