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pH is an important and commonly measured parameter of precipitation and other natural waters. The various sources of errors in pH measurement were analyzed and procedures for improving the accuracy and precision of pH measurements in natural waters with conductivities of < 100 uS/cm at 25 C are suggested. Detailed procedures are given for the preparation of dilute sulfuric acid standards to evaluate the performance of pH electrodes in low conductivity waters. A daily check of the pH of dilute sulfuric acid standards and deionized water saturated with a gas mixture of low carbon dioxide at partial pressure (air) prior to the measurement of the pH of low conductivity waters is suggested. (Author 's abstract)
Suggested Citation
Busenberg, E., Plummer, N., 1987, pH measurement of low-conductivity waters: U.S. Geological Survey Water-Resources Investigations Report 87-4060, iv, 22 p. :ill. ;28 cm., https://doi.org/10.3133/wri874060.
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
pH measurement of low-conductivity waters
Series title
Water-Resources Investigations Report
Series number
87-4060
DOI
10.3133/wri874060
Year Published
1987
Language
ENGLISH
Publisher
U.S. Geological Survey ;
Books and Open-File Reports [distributor],