YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.
ORP is determined by measuring the potential of a chemically-inert (platinum) electrode which is immersed in the solution. The sensing electrode potential is read relative to the reference electrode of the pH probe and the value is presented in millivolts.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.
ORP is determined by measuring the potential of a chemically-inert (platinum) electrode which is immersed in the solution. The sensing electrode potential is read relative to the reference electrode of the pH probe and the value is presented in millivolts.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.
ORP is determined by measuring the potential of a chemically-inert (platinum) electrode which is immersed in the solution. The sensing electrode potential is read relative to the reference electrode of the pH probe and the value is presented in millivolts.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.
ORP is determined by measuring the potential of a chemically-inert (platinum) electrode which is immersed in the solution. The sensing electrode potential is read relative to the reference electrode of the pH probe and the value is presented in millivolts.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.
ORP is determined by measuring the potential of a chemically-inert (platinum) electrode which is immersed in the solution. The sensing electrode potential is read relative to the reference electrode of the pH probe and the value is presented in millivolts.

YSI pH and pH/ORP sensors have been carefully designed to perform under all ionic strength conditions, from seawater with a conductivity of 53,000 ?S/cm, to "average" freshwater lakes and rivers with conductivities of 200 to 1500 ?S/cm, to pure mountain streams with conductivities as low as 15 ?S/cm, which has historically been the most difficult medium with respect to accuracy, quick response to pH changes, and minimal flow dependence.