The development and validation of a profiling glider deep ISFET-based pH sensor for high resolution observations of coastal and ocean acidification

Grace Saba1, Elizabeth Wright-Fairbanks1, Baoshan Chen2, Wei-Jun Cai2, Andrew Barnard3, Clayton P Jones4, Charles William Branham5, Kui Wang2 and Travis N Miles6, (1)Rutgers University, Department of Marine and Coastal Sciences, New Brunswick, NJ, United States, (2)University of Delaware, School of Marine Science and Policy, Newark, DE, United States, (3)Sea-Bird Scientific, Bellevue, WA, United States, (4)Teledyne Webb Research, North Falmouth, MA, United States, (5)Sea-Bird Scientific, R&D, Bellevue, WA, United States, (6)Rutgers University, Marine and Coastal Sciences, New Brunswick, NJ, United States
Abstract:
Coastal and ocean acidification can alter ocean biogeochemistry, with ecological consequences that may result in economic and cultural losses. Yet few time series and high resolution spatial and temporal measurements exist to track the existence and movement of water low in pH and/or aragonite saturation state (ΩArag). Past acidification monitoring efforts have either low spatial resolution or high cost and low temporal resolution. We developed the first integrated glider platform sensor system for sampling pH throughout the water column of the coastal ocean. A deep ISFET (Ion Sensitive Field Effect Transistor)-based pH sensor system was modified and integrated into a Slocum glider, tank tested in natural seawater to determine sensor conditioning time under different scenarios, and validated in situ during deployments in the U.S. Northeast Shelf. Comparative results between glider pH and pH measured spectrophotometrically from discrete seawater samples indicate that the glider pH sensor is capable of accuracy of 0.011 pH units or better for several weeks throughout the water column in the coastal ocean, with a precision of 0.005 pH units or better. Furthermore, simultaneous measurements from multiple sensors on the same glider enabled salinity-based estimates of total alkalinity (AT) and ΩArag. During a Spring 2018 Mid-Atlantic deployment, glider pH and derived ATArag data along the cross-shelf transect revealed higher pH and ΩArag associated with the depth of chlorophyll and oxygen maxima and a warmer, saltier water mass and lower pH and ΩArag in bottom waters of the middle shelf and slope and nearshore following a precipitation event. Biofouling was revealed to be the primary limitation of this sensor, whereby offsets in pH and AT increased dramatically during a summer deployment. These data presented here demonstrate the ability for gliders to routinely provide high resolution water column data on regional scales that can be applied to acidification monitoring efforts in other ocean regions.