docs(appendix-e): offset fault is geophone-side — operator swap test + MicL evidence
Operator report: attaching a different geophone to an affected unit makes the offset go away. That rules out the unit's analog front-end and any stored per-channel zero constant (a constant lives in the unit and would survive a sensor swap). The stored data agrees — MicL, a separate transducer on its own cable, shows no offset during either episode (|mean|/peak 0.17 and 0.02) while the geo channels on the same unit at the same moment are pinned. Two distinct sensor-side patterns recorded: BE18438 Vert 0.97, Tran 0.16, Long 0.18 -> one conductor pair BE9558 Long 0.99, Tran 0.90, Vert 0.81 -> shared return / ground Candidate mechanisms narrowed to three, since a geophone coil is passive and cannot generate sustained DC: galvanic corrosion at a connector or splice (matches the ~46 mV referred to the ADC input), a leakage path to shield, or changed coil DC resistance interacting with the amplifier's input bias current. Also records the confound: swapping a sensor requires a monitoring restart, and these units run Sensor Check "Before monitoring", so the restart re-zeros too. The swap does not cleanly separate "new sensor" from "the restart re-zeroed it". Controls and the single best measurement (open-circuit DC across the suspect connector) documented. Co-Authored-By: Claude Opus 5 (1M context) <noreply@anthropic.com> Claude-Session: https://claude.ai/code/session_01HgTe8CamXAHcAmaQ6QNcog
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@@ -3536,26 +3536,65 @@ steps. A small common-mode diurnal wobble rides on top of it, but that
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wobble is present on the healthy channels too (it is the unit's normal
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thermal breathing) and is not the fault.
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**Open: two candidate mechanisms.**
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**The fault is on the geophone side.** Operator report (2026-08-25):
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*attaching a different geophone to an affected unit makes the offset go
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away.* That is the channel-swap test, already run in the field many
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times, and it rules out the unit's analog front-end and any stored
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per-channel zero constant — a constant lives in the unit and would
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survive a sensor swap.
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1. *A latched bad zero.* These units run Sensor Check "Before
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monitoring", so a baseline is captured at session start. Disturb the
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geophone at that instant and the unit bakes a non-zero reading in as
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"zero". Fits the discrete steps, the rock-steadiness between them,
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surviving power cycles, the sensor check still passing, and clearing
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on a clean re-zero. Also explains why it is episodic rather than
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constant — it needs a disturbance at the moment of zeroing.
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2. *A degrading analog front-end.* Fits BE9558 better: it was clean for
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nine months, then escalated 3 → 1 → 1 → 193 events over five weeks
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**and moved from Tran to Long**, which a single bad channel would
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not do.
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The stored data agrees. MicL — a separate transducer on its own cable —
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shows no offset during either episode (`|mean|/peak` = 0.17 and 0.02),
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while the geo channels on the same unit at the same moment are pinned.
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BE18438 (same channel twice, months apart) looks like (1); BE9558
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(escalating, channel-migrating) looks like (2). The decisive test is to
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force a clean re-zero on a faulted unit: if the offset clears and stays
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clear it is (1) and fixable in the field — potentially over the wire,
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since we already speak SUB `0x0E` (channel sensor data) and `0x98`
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(trigger test), see §7.10.
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**Two distinct failure patterns**, both geophone-side:
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| unit | Tran | Vert | Long | MicL | reading |
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|---|---|---|---|---|---|
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| BE18438 | 0.16 | **0.97** | 0.18 | 0.02 | one element only |
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| BE9558 | 0.90 | 0.81 | **0.99** | 0.17 | all three, Long dominant |
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(values are `\|mean\|/peak` on the dominant axis)
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BE18438 has a single faulted conductor pair with the other two clean.
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BE9558 has all three geo channels offset by different amounts
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(Long +0.340, Tran +0.037, Vert −0.020) — that points at a shared return
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or ground path in the housing rather than one element.
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**Candidate mechanisms.** A geophone coil is passive and cannot
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generate sustained DC on its own, so an offset originating on the sensor
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side has to come from one of:
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1. *Galvanic corrosion at a connector or splice* — dissimilar metals
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plus moisture form a literal cell. This generates DC directly, in
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the tens-of-millivolts range that matches the measured offset
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(0.29 in/s ÷ 6.206053 in/s per volt ≈ 46 mV referred to the ADC
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input). Fits the discrete steps, surviving power cycles, and being
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cured by swapping the sensor.
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2. *A leakage path to shield or another conductor*, letting the unit's
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own bias/reference divide into the signal pair. Best fit for the
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BE9558 all-three-channels pattern.
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3. *Changed coil DC resistance* (partial short or degraded winding)
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interacting with the amplifier's input bias current —
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`V_offset = I_bias × R_source`. Best fit for the BE18438
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single-element pattern. Note the on-device sensor check would not
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catch this: it measures ring-down frequency and damping, not DC.
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**Caveat on the swap test.** Swapping a geophone requires stopping and
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restarting monitoring, and these units run Sensor Check "Before
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monitoring" — so the restart also re-zeros the channels. The swap
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therefore does not cleanly separate *"new sensor"* from *"the restart
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re-zeroed it"*. Two cheap controls settle it: restart monitoring
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**without** swapping (if the offset clears, it was the re-zero), or swap
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the **original** sensor back (if the offset returns, it is the sensor).
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The operator's remedy being a swap rather than a restart is weak
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evidence for the sensor, since a restart is the easier thing to try
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first.
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**Best single measurement when it recurs:** DC voltage across the
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suspect geophone's connector pins with the sensor **disconnected from
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the unit**. A galvanic cell (mechanism 1) shows an open-circuit
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voltage; mechanisms 2 and 3 do not.
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**Note:** the surveyed population is subject to survivorship bias —
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flooded events were routinely deleted before this snapshot, so units
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