Italian Spring Accelerometer (ISA)
- ISA is a high-sensitivity, three-axis mass-spring accelerometer designed to detect minute non-gravitational perturbations and perform the first in-situ measurement of a planetary gravity gradient.
- It integrates advanced mechanical, electrical, and thermal systems, achieving noise levels of ~1×10⁻⁹ m/s²/√Hz and a resolution of ~10⁻¹¹ m/s² within a ±5×10⁻⁴ m/s² dynamic range.
- ISA plays a pivotal role in precise orbit determination by enabling real-time data fusion with Ka-band radio tracking, effectively isolating external forces during critical mission phases.
The Italian Spring Accelerometer (ISA) is a high‐sensitivity, three‐axis mass‐spring accelerometer deployed on the Mercury Planetary Orbiter (MPO) of the ESA–JAXA BepiColombo mission. Designed to detect minute non‐gravitational perturbations and gravity gradients, ISA plays a crucial role in the BepiColombo Radio Science Experiment (BC-RSE), notably achieving the first direct in‐situ measurement of an extraterrestrial body's gravity gradient during the second Venus swing-by. ISA’s technical sophistication in mechanical, electrical, and thermal domains, along with advanced data fusion with Ka-band radio tracking, yields unprecedented measurement and orbit determination accuracy.
1. Mechanical and Electrical Architecture
ISA comprises three nominally identical one-dimensional sensing elements (SE0, SE1, SE2), each consisting of a trapezoidal proof-mass suspended from a rigid frame via a thin flexure (“blade”) spring. The proof-mass is equipped with capacitive pick-up electrodes on two opposing faces for displacement read-out, and four electrostatic actuation electrodes for centering and internal calibration. The overall mechanical system constitutes a simple harmonic oscillator with mass (nominally kg) and spring constant chosen such that the natural frequency %%%%3%%%% Hz.
The electrical design segregates the system into:
- ISA Detector Assembly (IDA): houses the sensing elements and front-end electronics (FEE), nested within thermal/shielding structures, with temperature controlled at C C.
- ISA Control Electronics (ICE): incorporates digital electronics, power converters, and data-handling interfaces. Digital feedback loop centers the proof-mass via controlled actuation voltages on electrodes.
Pick-up electrodes interface with low-noise capacitive-bridge electronics in the FEE. ICE communicates with the MPO on-board computer via SpaceWire and operates on a regulated 28 V supply.
2. Calibration, Reference Frames, and Reduction Procedures
ISA’s three sensing axes are not perfectly orthogonal. On-ground calibration produces an orthogonal “Instrument Line-of-Sight” frame (ISA_ILS) with origin at the center of mass of the Y-axis element. In-flight, raw acceleration signals from each element SE undergo “vertex reduction” to yield a single acceleration vector at the ISA_ILS origin. This transformation accounts for the spatial offsets from MPO center of mass to each sensing element, as well as common-mode rotational and gravity-gradient corrections.
Key calibration metrics:
- Measurement band: Hz to Hz
- Noise-equivalent acceleration floor: m/s/√Hz (at 10 mHz)
- Calibration capability: m/s range, ppm-level accuracy
- Dynamic range: m/s per axis
- Resolution: m/s (band-limited)
3. Integration on BepiColombo and Role in BC-RSE
The Detector Assembly is rigidly mounted on the MPO payload panel in a thermally optimized location, shielded by multilayer insulation, dedicated heaters, and sensors. ICE resides in the MPO avionics rack. ISA operates in conjunction with the Ka-band Transponder (KaT), enabling the BC-RSE (also referred to as MORE) to combine high-precision Doppler/range data with real-time vector accelerometry from ISA.
BC-RSE’s dynamic filter subtracts the non-gravitational perturbation force from spacecraft equations of motion, isolating pure gravitational dynamics, including relativistic effects. This methodology enables orbit determination accuracy better than 5 cm in range and in post-Newtonian measurements.
4. Gravity-Gradient and Non-Gravitational Perturbation Measurements at Venus Swing-By
During the second Venus swing-by (VSB2), BepiColombo’s trajectory passed Venus at 550 km altitude (planetary radius 6051 km). The expected gravity gradient across the 1 m separation between MPO CoM and ISA elements, modeled as:
with km/s, gave a peak m/s, substantially above the ISA noise threshold. ISA data aligns with SPICE-predicted gravity-gradient acceleration to within m/s over a 1-hour window, validating the first direct in-situ gravity gradient measurement due to a planetary body.
At closest approach (CA), a spurious acceleration spike was observed, lasting approximately 7 minutes (CA to CA), peaking at m/s predominantly along the Y-axis. The magnitude and profile could not be attributed to any modeled non-gravitational disturbance (solar pressure, albedo, IR emission, thermal recoil).
5. Attribution and Localization of the Non-Gravitational Event
Discrimination between instrument artifact and true external force leveraged contemporaneous Attitude and Orbit Control System (AOCS) reaction wheel torque telemetry. A clear deviation in commanded torques coincided with the acceleration spike, indicating compensation for a disturbance along consistent with the recorded ISA acceleration.
Disturbance torque satisfies:
where kg and locates the point of force application relative to MPO CoM. The misalignment angle is defined:
during the spike interval confirms alignment of RW torque and ISA acceleration as responding to the same physical disturbance. Fitting by non-linear least squares in the interval yields:
in the MPO body-fixed reference, localized near the Y radiator panel. Formal uncertainties are 5 cm in X and Z, 20 cm in Y.
Net impulsive velocity increment:
aligns with ESOC’s independently estimated m/s, both along .
6. Scientific and Methodological Implications
ISA’s measurement at VSB2 constitutes the undisputed first direct in-situ detection of a planet’s tidal gravity gradient by a spacecraft accelerometer at the m/s scale. The contemporaneously observed non-gravitational acceleration event—a transient m/s spike—is localized to the vicinity of the MPO radiator. A companion paper (De Filippis et al.) attributes the event to short-lived outgassing.
Combined ISA and AOCS analysis demonstrates the capacity of high-sensitivity accelerometry to isolate and quantify external forces producing mm/s, which would otherwise confound precision orbit determination.
A plausible implication is that future missions demanding micrometer-per-second-level velocity accuracy should embed accelerometers of at least ISA-class sensitivity ( m/s/√Hz). Instrument mounting, thermal management, and shielding require stringent engineering to mitigate micro-thrusts and thermally driven outgassing effects.
ISA’s validation of the pseudo-drag-free BC-RSE strategy underscores the feasibility of achieving sub-ppm gravity-field and relativistic parameter sensitivity without recourse to complex drag-free platforms.
Table: Key Instrument Parameters
| Parameter | Value | Description |
|---|---|---|
| Measurement band | Hz – Hz | Frequency range for acceleration detection |
| Acceleration floor | m/s/√Hz (10 mHz) | Minimum resolvable signal |
| Resolution (band-limited) | m/s | Smallest resolved change |
| Range (per axis) | m/s | Dynamic detection range |
| Proof-mass | kg | Movable mass for each axis |
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