Published December 1999
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Contribution of isotope techniques to evaluate water resources in the Peruvian Altiplano
- 1. AMATOSA Ingenieria, Madrid (Spain)
- 2. Instituto Peruano de Energia Nuclear, Lima (Peru)
- 3. Proyecto Especial Tacna, Tacna (Peru)
- 4. Proyecto Especial Pasto Grande, Moquegua (Peru)
- 5. Charles University, Prague (Czech Republic)
Description
Environmental isotopes H, 18O, 13C, 3H, and 14C were regularly measured in precipitation, surface, and ground water to investigate a series of problems linked with the management of water resources in the Peruvian Altiplano, a plateau located in Southern Peru
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Additional details
Publishing Information
- Imprint Title
- Isotope techniques in water resources development and management. Proceedings
- Imprint Pagination
- [CD-ROM]
- Journal Issue
- no. 2/C
- Series
- C and S papers series
- Journal Page Range
- [2 p.]
- ISSN
- 1562-4153
Conference
- Title
- International symposium on isotope techniques in water resources development and management
- Dates
- 10-14 May 1999
- Place
- Vienna (Austria)
INIS
- Country of Publication
- International Atomic Energy Agency (IAEA)
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 31009522
- Subject category
- S58: GEOSCIENCES;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- ATMOSPHERIC PRECIPITATIONS; CARBON 13; CARBON 14; DEUTERIUM; GROUND WATER; ISOTOPE RATIO; OXYGEN 18; PERU; SURFACE WATERS; TRITIUM; WATER INFLUX; WATER RESOURCES
- Descriptors DEC
- BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; CARBON ISOTOPES; DEVELOPING COUNTRIES; EVEN-EVEN NUCLEI; EVEN-ODD NUCLEI; HYDROGEN COMPOUNDS; HYDROGEN ISOTOPES; ISOTOPES; LATIN AMERICA; LIGHT NUCLEI; NUCLEI; ODD-EVEN NUCLEI; ODD-ODD NUCLEI; OXYGEN COMPOUNDS; OXYGEN ISOTOPES; RADIOISOTOPES; RESOURCES; SOUTH AMERICA; STABLE ISOTOPES; WATER; YEARS LIVING RADIOISOTOPES
Optional Information
- Notes
- Data in PDF format; Acrobat Reader for Windows 3.x, 95, 98, NT and Macintosh included
- Secondary number(s)
- IAEA-CSP--2/C; IAEA-SM--361