Science & Tech

Pierre Perrault

French hydrologist
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

Print
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

Born:
1611?, Paris, Fr.
Died:
1680, Paris
Subjects Of Study:
spring
water cycle

Pierre Perrault (born 1611?, Paris, Fr.—died 1680, Paris) was a French hydrologist whose investigation of the origin of springs was instrumental in establishing the science of hydrology on a quantitative basis. He showed conclusively that precipitation was more than adequate to sustain the flow of rivers; thus he refuted theories traceable as far back as the writings of Plato and Aristotle that invoked some variety of subterranean condensation or return flow of seawater to account for the discharge of water in springs and rivers.

Perrault was not a scientist by profession but had been, in succession, a lawyer, a government administrator, and a writer. In his most significant scientific work, De l’origine des fontaines (1674; On the Origin of Springs), he presented a study of a substantial section of the Seine River, beginning at its source, northwest of the city of Dijon. His numerical estimates demonstrated that the annual river runoff was only one-sixth of the amount of water falling as rain or snow over the drainage basin in a year.

This article was most recently revised and updated by Encyclopaedia Britannica.