 Shared-offset cancellation in a baseline-corrected pulse integral

Shared-offset cancellation in a baseline-corrected pulse integral occurs when the raw integral and its background estimate assign exactly the same coefficient to a common additive error. For sampled readings $\mathbf{x}$, let the corrected energy be $\hat{U}={\mathbf{a}}^T\mathbf{x}$, with weights expressed in the required time and calibration units. Adding an unknown common power offset $c$ givesThus exact cancellation requires ${\mathbf{a}}^{T}1=0$. It is a property of the measurement weights, not an assumption that the offset is negligible. The parent covariance between a raw pulse integral and its baseline correction gives the corresponding variance identity.

An original mismatch example integrates the raw trace over $T=8.0\mu \mathrm{s}$ but mistakenly scales the baseline with $\hat{T}=7.8\mu \mathrm{s}$. With identical calibration, the residual offset is $(T-\hat{T})c$. If $c$ has standard uncertainty $0.30\mathrm{mW}$, its contribution is $0.060\mathrm{nJ}$. It would have vanished for matched durations. A calibration mismatch between raw and blank paths similarly changes their effective coefficients even when their nominal durations agree.

The same linear-algebra test extends to a shared linear drift. If each sample at time $t_i$ gains an error $c_0+c_1{t}_i$, both components cancel whenThese moment conditions for baseline-drift cancellation require the actual sample times and weights. Removing a constant offset does not automatically remove drift, and timing uncertainty can spoil the second condition.

NIST's thermocouple pulse-energy apparatus used before/after baseline averages to compensate background and thermal drift.^[ref] The weight test above is an original general formulation. For uncertain residual errors, propagate the complete joint covariance rather than treating repeated appearances of the same offset as independent.^[ref]