Long Term Study of Sedimentation and Biofouling at Cascadia Basin, the Site of the Pacific Ocean Neutrino Experiment

Abstract: We present a study of the effects of biofouling and sedimentation on pathfinder instrumentation for the Pacific Ocean Neutrino Experiment (P-ONE), which will be located in the Cascadia Basin region of the North Pacific Ocean. P-ONE will look for high-energy neutrinos by observing the light produced when these neutrinos interact in the water, detecting and digitizing single photon signals in the ultraviolet-visible range. We measure that biofouling and sedimentation caused a decrease in the transparency of upward-facing optical surfaces over 5 years of operations. A majority of downward-facing optical surfaces, which will dominate P-ONE's sensitivity to astrophysical sources, showed no visible biofouling. Extrapolations motivated by biological growth models estimated that these losses started around 2.5 years after deployment, and suggest a final equilibrium transparency ranging between 0$\%$ and 35$\%$ of the original for the upward-facing modules.