Katsuko Saruhashi (猿橋 勝子, Saruhashi Katsuko; March 22, 1920 – September 29, 2007) was a Japanese geochemist who created tools that let her take some of the first measurements of carbon dioxide (CO2) levels in seawater. She later showed evidence of the dangers of radioactive fallout and how far it can travel. Along with this focus on safety, she also researched peaceful uses of nuclear power. Her other major area of significance involved raising the number and status of women scientists, especially in Japan. She established both the Society of Japanese Women Scientists and the Saruhashi Prize, which is awarded annually to a female scientist who serves as a role model for younger women scientists. Among her other honors, she was the first woman elected to the Science Council of Japan, to earn a doctorate in chemistry from the prestigious University of Tokyo, and to win the Miyake Prize for Geochemistry.
Education Saruhashi was born in Tokyo in 1920. At a very young age, Saruhashi wanted to know what made it rain. This fascination was derived from watching raindrops slide down windows one day during primary school. Kuniharu and Kuno Saruhashi both saw the importance of education and supported their daughter after their shared experience during World War 2, where many women struggled to support themselves without husbands or fathers. Saruhashi and her mother understood that there was a lack of women with technical knowledge and figured that it could be useful to gain financial independence. At the age of 21, Saruhsashi quit her secure job at an insurance firm to attend the Imperial Women's College of Science, now known as Toho University, where she earned a degree in chemistry. After graduating in 1943 with an undergraduate degree in chemistry, Saruhashi took a position at the Meteorological Research Institute where she worked with her mentor Miyake Yasuo, and her scientific career took off. Saruhashi went back to school to get her PhD in chemistry at the University of Tokyo in 1957, where she was the first woman to graduate with a PhD in science. Her dissertation was on "The Behavior of Carbonic Matter in Natural Water".
Career Saruhashi conducted research with Teruko Kanzawa from 1973 to 1978. They began their research by measuring the pH of every rainfall event over the five-year period at the Meteorological Research Institute in Tokyo. On average, they found the pH to be around 4.52 which was an increase from 4.1 in the previous years of research done by Miyake in 1939. According to Miyake, the pH varied during different seasons (summer and winter); however, Saruhashi noted no variation between seasons in their findings, showing how conditions changed during the 1970s.
Nuclear tests Katsuko Saruhashi made several discoveries in both geochemistry and, most notably, oceanography. The most salient of these are: Saruhashi's Table; her novel method for measuring the amounts of caesium-137 and strontium-90 in seawater, and her research concerning the environmental impact of the US bomb test site, Bikini Atoll, which ultimately provided justification for the prohibition of above-ground nuclear testing. She also made important contributions to the study of the carbon dioxide system in the oceans, finding that the Pacific Ocean emits more CO2 than it absorbs.
Saruhashi's table Presented in her 1955 paper ‘On the Equilibrium Concentration Ratio of Carbonic Acid Substances Dissolved in Natural Waters: A study on the Metabolism in Natural Waterways’, Saruhashi's table provided oceanographers with a method for determining the composition of three carbonic acid substances based on water temperature, pH, and salinity.
Artificial radioisotopes in seawater In response to the influx of nuclear testing occurring in the Pacific, the Japanese Government requested that Saruhashi – along with Yasuo Miyake - lead a research project into the long-term and global effects of such activities. To do so, Saruhashi worked at the Central Meteorological Observatory in Tokyo to find a new method for measuring radioactive fallout. The findings of Saruhashi and Miyake investigation were explicated in their paper 'Cesium 137 and Strontium 90 in Sea Water'. Their studies concluded that in the Western North Pacific, there were substantially higher amounts of 137Cs and 90Sr than were found in samples obtained from the Atlantic and Northeast Pacific. Given these results, Saruhashi and Miyake concluded that the differing quantities of artificial radioisotopes found in the Pacific was a direct consequence of the nuclear testing occurring in the Pacific Tropics. Despite the corroborating evidence in favor of Saruhashi's claim concerning the discrepancy in the quantity of 137Cs and 90Sr present in different regions of the Atlantic and North Pacific, conclusion was challenged by {American scientists}, who called into doubt the methodology and technique applied by Saruhashi's team; contending that their novel investigatory method was fallible and erroneous.
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