Paper

{
  "raw_xml": "<entry>\n    <id>http://arxiv.org/abs/2603.15157v1</id>\n    <title>ANNA: a toolbox for Newtonian Noise Analysis</title>\n    <updated>2026-03-16T11:52:01Z</updated>\n    <link href='https://arxiv.org/abs/2603.15157v1' rel='alternate' type='text/html'/>\n    <link href='https://arxiv.org/pdf/2603.15157v1' rel='related' title='pdf' type='application/pdf'/>\n    <summary>The Einstein Telescope (ET) is a third-generation underground gravitational wave observatory designed to achieve an unprecedented sensitivity down to 3 Hz. Waves propagating in the soil due to anthropogenic or natural vibration sources generate density fluctuations which cause gravitational attraction, resulting in motion of the mirrors of the laser interferometer known as Newtonian noise. The latter is computed by integrating density fluctuations due to seismic wave fields over the soil domain surrounding the test mass.\n  ANNA Newtonian Noise Analysis is a toolbox that computes Newtonian Noise from a seismic wave field defined on a finite element mesh, using Gaussian quadrature. 3D finite element meshes composed of linear and quadratic tetrahedral (4-node and 10-node) and brick (8-node and 20-node) elements are supported. The user computes (or interpolates) a seismic wave field on a finite element mesh and the toolbox computes the total Newtonian noise, as well as the bulk and surface contributions. ANNA runs in the MATLAB programming and numeric computing platform and is compatible with the open-source GNU Octave Scientific Programming Language; a Python version is also available.\n  The toolbox is verified for plane P- and S-waves propagating in an elastic homogeneous full space with a mirror suspended in a spherical cavity, assuming that the wavelength is much larger than the radius of the cavity, so that wave scattering can be ignored. Excellent agreement with analytical solutions is obtained. Similar good agreement is reported for the Newtonian noise on a test mass suspended at a finite distance above the free surface of a homogeneous elastic halfspace in which a Rayleigh wave propagates.\n  The proposed finite element framework provides a physically consistent and computationally efficient approach for computing gravitational-seismic coupling in heterogeneous media.</summary>\n    <category scheme='http://arxiv.org/schemas/atom' term='physics.app-ph'/>\n    <category scheme='http://arxiv.org/schemas/atom' term='astro-ph.IM'/>\n    <category scheme='http://arxiv.org/schemas/atom' term='physics.comp-ph'/>\n    <published>2026-03-16T11:52:01Z</published>\n    <arxiv:comment>Preprint submitted to the Journal of Computational Physics</arxiv:comment>\n    <arxiv:primary_category term='physics.app-ph'/>\n    <author>\n      <name>Pieter Reumers</name>\n    </author>\n    <author>\n      <name>Xhorxha Kucia</name>\n    </author>\n    <author>\n      <name>Stijn François</name>\n    </author>\n    <author>\n      <name>Geert Degrande</name>\n    </author>\n  </entry>"
}