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Italian Spring Accelerometer (ISA)

Updated 17 November 2025
  • 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 mm (nominally 0.02\approx 0.02 kg) and spring constant kk 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 2020^\circC ±0.1\pm 0.1^\circC.
  • 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 aja_j from each element SEj_j undergo “vertex reduction” to yield a single acceleration vector aISAa_{ISA} at the ISA_ILS origin. This transformation accounts for the spatial offsets rjr_j from MPO center of mass to each sensing element, as well as common-mode rotational and gravity-gradient corrections.

Key calibration metrics:

  • Measurement band: 3×1053 \times 10^{-5} Hz to 1×1011 \times 10^{-1} Hz
  • Noise-equivalent acceleration floor: 1×109\sim 1 \times 10^{-9} m/s2^2/√Hz (at 10 mHz)
  • Calibration capability: 10610^{-6} m/s2^2 range, ppm-level accuracy
  • Dynamic range: ±5×104\pm 5 \times 10^{-4} m/s2^2 per axis
  • Resolution: 1011\sim 10^{-11} m/s2^2 (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 FNGP=mscaISAF_{NGP} = m_{sc} \cdot a_{ISA} 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 3×1053 \times 10^{-5} in post-Newtonian γ\gamma 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 \sim1 m separation between MPO CoM and ISA elements, modeled as:

aGGj=(μVenR3)[3(R^R^)I3]rja_{GG}^j = \left(\frac{\mu_{Ven}}{R^3}\right) [3 (\hat{R} \otimes \hat{R}) - I_3] r_j

with μVen=3.2486×105\mu_{Ven} = 3.2486 \times 10^5 km3^3/s2^2, gave a peak aGG1.1×106|a_{GG}| \approx 1.1 \times 10^{-6} m/s2^2, substantially above the ISA noise threshold. ISA data aligns with SPICE-predicted gravity-gradient acceleration to within 108\sim 10^{-8} m/s2^2 over a ±\pm1-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 (CA4-4' to CA+3+3'), peaking at 3.5×1063.5 \times 10^{-6} m/s2^2 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 +Ybody+Y_{body} consistent with the recorded ISA acceleration.

Disturbance torque satisfies:

Tdis=msc(rA×aISA)T_{dis} = m_{sc} (r_A \times a_{ISA})

where msc=3991m_{sc} = 3991 kg and rAr_A locates the point of force application relative to MPO CoM. The misalignment angle is defined:

β=arcsin(TdisaISATdisaISA)\beta = \arcsin \left( \frac{T_{dis} \cdot a_{ISA}}{|T_{dis}| |a_{ISA}|} \right)

β0\beta \approx 0^\circ during the spike interval confirms alignment of RW torque and ISA acceleration as responding to the same physical disturbance. Fitting rAr_A by non-linear least squares in the β<10\beta < 10^\circ interval yields:

rA[+0.0235,2.1841,1.7233]mr_A \approx [ +0.0235, -2.1841, -1.7233 ]\, \mathrm{m}

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:

ΔVISA=aISAdt(5.8±0.4)×104m/s\Delta V_{ISA} = \int a_{ISA}\, dt \approx (5.8 \pm 0.4) \times 10^{-4}\,\mathrm{m/s}

aligns with ESOC’s independently estimated ΔVradio=(5.95±2.71)×104\Delta V_{radio} = (5.95 \pm 2.71) \times 10^{-4} m/s, both along +Ybody+Y_{body}.

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 10610^{-6} m/s2^2 scale. The contemporaneously observed non-gravitational acceleration event—a transient 3.5×106\sim 3.5 \times 10^{-6} m/s2^2 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 ΔV0.6\Delta V \sim 0.6 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 (10910^{-9} m/s2^2/√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 3×1053 \times 10^{-5} Hz – 1×1011 \times 10^{-1} Hz Frequency range for acceleration detection
Acceleration floor 1×109\sim 1 \times 10^{-9} m/s2^2/√Hz (10 mHz) Minimum resolvable signal
Resolution (band-limited) 1011\sim 10^{-11} m/s2^2 Smallest resolved change
Range (per axis) ±5×104\pm 5 \times 10^{-4} m/s2^2 Dynamic detection range
Proof-mass 0.02\sim 0.02 kg Movable mass for each axis
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