Optimization and robustness of cost-efficient seismic arrays for Newtonian noise cancellation at the Einstein Telescope
Pith reviewed 2026-06-26 13:38 UTC · model grok-4.3
The pith
Arrays using multiple seismometers per borehole plus tunnel sensors achieve stable Newtonian noise mitigation above 3-4 Hz for the Einstein Telescope.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
Arrays with multiple seismometers per borehole combined with additional seismometers in the interferometer tunnels provide promising broadband mitigation above 3 to 4 Hz; such arrays remain particularly stable against variations in seismometer positions, delivering mitigation factors greater than 6 for an array of 20 boreholes with 3 sensors each and greater than 15 for a large array of 50 boreholes with 10 sensors each.
What carries the argument
Position optimization of borehole and tunnel seismometers to cancel Newtonian noise via measurements of the seismic wave field.
Load-bearing premise
The seismic wave field model used for optimization accurately represents real conditions at the site so that computed mitigation factors translate to actual performance.
What would settle it
A side-by-side comparison of measured Newtonian noise reduction at the Einstein Telescope site against the model's predicted mitigation factors for the same array layout.
Figures
read the original abstract
Newtonian noise is expected to be the dominating noise source for low frequencies at the Einstein Telescope. It originates from seismic waves that cause density fluctuations in the rock around the interferometer. The mitigation strategy for Newtonian noise relies on an array of seismometers, placed at depth in boreholes, which provides measurements of the seismic wave field. We optimize the positions of the individual seismometers for the mitigation capabilities of the array for a full corner of the Einstein Telescope. We find that the mitigation capabilities of arrays with multiple seismometers in each borehole match the capabilities of only somewhat smaller arrays but with only one seismometer per borehole. Mitigation is further improved by extending the array with seismometers in the interferometer tunnels. Such configurations may hence provide a cost-effective way towards realizing an efficient seismic array. In each case, we quantify the broadband mitigation performance in the range from 1 to 10 Hz for arrays that are optimized for a frequency of 10 Hz, as well as the robustness of the arrays with respect to variations from their optimized positions. We find that larger arrays with several seismometers per borehole and additional seismometers in the tunnels provide promising broadband performance above 3 to 4 Hz and that such arrays are particularly stable against variations in the seismometer positions with mitigation factors $>6$ for an array of 20 boreholes with 3 seismometers each and $>15$ for a large array of 50 boreholes with 10 seismometers.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper optimizes the geometry of seismic arrays (boreholes with multiple seismometers plus tunnel sensors) to cancel Newtonian noise at a corner of the Einstein Telescope. Using forward modeling of the seismic wave field, it reports that arrays optimized at 10 Hz achieve broadband mitigation factors >6 (20 boreholes, 3 sensors each) and >15 (50 boreholes, 10 sensors each) above 3–4 Hz, with good robustness to position perturbations; multi-sensor boreholes are claimed to be nearly as effective as larger single-sensor arrays.
Significance. If the underlying seismic model is faithful to site conditions, the results identify cost-effective array designs that could substantially reduce a dominant low-frequency noise source for ET, directly supporting interferometer sensitivity goals.
major comments (1)
- [Seismic model and optimization procedure (methods/results sections)] The mitigation factors and robustness claims rest entirely on the fidelity of the forward seismic wave-field model (spatial correlations, dispersion, density fluctuations between 1–10 Hz). No validation against site-specific data, no error propagation, and no sensitivity analysis to model assumptions (isotropy, layering, scattering) are described; without these the quoted factors >6 and >15 cannot be shown to translate to on-site performance.
minor comments (2)
- [Results on broadband performance] Clarify whether the broadband factors are computed from the same optimization run or require separate frequency-dependent optimizations.
- [Discussion of array configurations] Specify the exact cost metric used when claiming multi-sensor boreholes are 'cost-efficient' relative to single-sensor arrays of comparable performance.
Simulated Author's Rebuttal
We thank the referee for their detailed review and constructive comments on our manuscript. We address the major comment regarding the seismic model below.
read point-by-point responses
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Referee: [Seismic model and optimization procedure (methods/results sections)] The mitigation factors and robustness claims rest entirely on the fidelity of the forward seismic wave-field model (spatial correlations, dispersion, density fluctuations between 1–10 Hz). No validation against site-specific data, no error propagation, and no sensitivity analysis to model assumptions (isotropy, layering, scattering) are described; without these the quoted factors >6 and >15 cannot be shown to translate to on-site performance.
Authors: We agree that the reported mitigation factors are dependent on the assumptions of the forward seismic model used. The manuscript presents an optimization procedure and results for a generic model of the seismic wave field at the ET site, without site-specific validation or sensitivity analysis to model parameters such as isotropy or scattering. This is a limitation of the current work, as detailed site data for the 1-10 Hz range may not be fully available or the study focused on the array optimization methodology itself. We have revised the manuscript to include a new subsection in the discussion explicitly stating the model assumptions and noting that the quantitative mitigation factors (>6 and >15) should be interpreted as indicative for the assumed model, with on-site performance requiring calibration using local seismic measurements. No error propagation was included, which we acknowledge as a point for future work. The robustness analysis to position variations is performed within the model framework. revision: partial
Circularity Check
No circularity: mitigation factors obtained via forward modeling of array response
full rationale
The derivation consists of optimizing seismometer positions inside an explicit forward model of the seismic wave field, then computing mitigation factors as the resulting cancellation performance of those optimized arrays. These steps are independent computations; the quoted broadband factors (>6, >15) and robustness metrics are outputs of the optimization, not parameters fitted to the target quantities or renamed inputs. No self-citations, uniqueness theorems, or ansatzes are invoked in a load-bearing way. The chain is self-contained against external benchmarks and does not reduce by construction.
Axiom & Free-Parameter Ledger
axioms (1)
- domain assumption A sufficiently accurate model of the seismic wave field exists that permits reliable prediction of Newtonian noise mitigation from array geometry.
Reference graph
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