Abstract
A non-glass type of in-situ pH sensor which uses an ion-sensitive field-effect transistor (ISFET) as the pH electrode and a chloride ion selective electrode (Cl-ISE) as the reference electrode was reported in 1998. An in-situ pCO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> sensor that the pH sensor was sealed with a gas permeable membrane filled with the inner solution was also informed in 2002. In the field tests, the in-situ response time of the devised pH sensor was as quick as 1 second or less, and the estimated measurement accuracy was ±0.005 pH units and a depth rating of 6000 m. The in-situ (3000 m depth, 1.8°C) response time of the pCO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> sensor was less than 60 seconds. In order to adapt the in-situ pH-pCO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> sensor to wide area mapping and/or long term monitoring of pH and pCO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> in the ocean, next generation of electro-circuit of the sensor and ISFET-pH electrode were newly developed. Several mapping observations of pH and pCO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> were performed using ROV or AUV, and the sensor detected distributions of low pH and high CO <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sub> seawater which were derived from hydrothermal vent. The long term monitoring by the sensor for one month showed daily variation of pH.
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