The use of (18)O/(16)O and (2)H/(1)H ratios of water in studying river run-off

Mook, W.J.

The use of (18)O/(16)O and (2)H/(1)H ratios of water in studying river run-off

1989

Mook, W.J.

In nature variations occur in the (18)O/(16)O and (2)H/(1)H (stable oxygen and hydrogen) isotopic ratio of waters of various origins and pathways. Relatively simple models can explain that (18)O/(16)O and (2)H/(1)H differences are observed between different storms, seasons and locations. This project requires regular sampling of small quantities of river water and precipitation. (18)O/(16)O and (2)H/(1)H studies may also serve for hydrography separation, i.e. the reaction rate of surface run-off to rainfall.

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AGROVOC Keywords

cours d'eau cursos de agua eau de ruissellement escorrentia lluvia pluie radioisotopos

Bibliographic information

Publisher

BRB

Other Subjects

Hidrogeno; Oxigeno; Oxygene; Isotope radioactif; Hydrogene

Language

English

Note

Summary only

Type

Conference; Summary

Source

Proceedings of the International Seminar on Bangladesh floods: regional and global environmental perspectives, Bangladesh Research Bureau, Dhaka (Bangladesh). Scientific Committee on Problems of Environment.- Dhaka (Bangladesh): BRB, 1989. p. 30

Conference

International Seminar on Bangladesh Floods: Regional and Global Environmental Perspectives, Dhaka (Bangladesh), 4-6 Mar 1989

In AGRIS since: 1990-08-15

Format: AGRIS AP

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The use of (18)O/(16)O and (2)H/(1)H ratios of water in studying river run-off

1989

AGROVOC Keywords

Bibliographic information