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W. Majewski and D. C. Miller, eds.. Predicting Effects of Power Plant Once-Through Cooling on Aquatic Systems, Technical Papers in Hydrology 20, United Nations Educational, Scientific and Cultural Organization (Unesco), Paris, 1979. [Pg.480]

Copyright Taws and Treaties of the World, Unesco, Paris, and Bureau of National Affairs, Washington, D.C., 1990. The complete text of every country s copyright statute. [Pg.267]

E Parent, P Hubert, B Bobee, I Miquel, eds. Statistical and Bayesian Methods in Hydrological Sciences. Pans UNESCO Press, 1998. [Pg.345]

Milos Hudlicky, a native of Czechoslovakia, obtained his Ph D from the Technical University in Prague, Czechoslovakia. After spending 1948 at the Ohio State University as a UNESCO postdoctoral fellow, he taught as an assistant professor and later as an associate professor at the Technical University in Prague until 1958. He then worked as a research associate at the Research Institute of Pharmacy and Biochemistry in Prague. After the Russian occupation of Czechoslovakia in 1968, he moved to the United States, where he was offered a professorship at Virginia Polytechnic Institute and State University He has been Professor Emeritus since 1989. He received the Votocek Medal in Prague in 1992 for his work in chemistry. [Pg.1299]

Sing, M. (1998). The Timeless Energy of the Sun. New York Sierra Club Books/UNESCO. [Pg.895]

Bequette, F. (1998). Harnessing Ocean Energy. UNESCO Courier 51 (7/8) 33-35. [Pg.895]

Global freshwater reserves (discounting pollution) are a small percentage of global water, accounting for only 35 x 10 km of the total 1.386 X 10 km global water supply (UNESCO,... [Pg.115]

Falkenmark, M. and Chapman, T. (1989). "Comparative Hydrology An Ecological Approach to Land and Water Resources." UNESCO, Paris. [Pg.130]

UNESCO (1978). "World Water Balance and Water Resources of the Earth." UNESCO Press, Paris. (Translation of 1974 USSR publication.)... [Pg.131]

FAO (1971-1981). "The FAO-UNESCO Soil Map of the World." Legend and 9 volumes. UNESCO, Paris. [Pg.191]

UNESCO (1981). Background papers and supporting data on the Practical Salinity Scale 1978. UNESCO Technical Papers in Marine Science No. 37. UNESCO. [Pg.278]

Zrinyi, M., New generation of smart elastomers, demonstrated on the website http / academic.sun.ac. za/unesco/Conferences/Conference2002/Zrinyi%20(3).pdf... [Pg.296]

UNESCO (United Nations Educational, Scientific and Cultural Organisation) (2002) Teaching and Learning for a Sustainable Euture. [Pg.158]

Jeffrey, S.W., Structural relationships between algal chlorophylls, in Phytoplankton Pigments in Oceanography Guidelines to Modem Methods, Jeffrey, S.W., Mantoura, R.F.C. and Wright, S.W., Eds., UNESCO, Paris, 1997, 566. [Pg.45]

Martin JM, Nijampurkar V, Salvation F (1978b) Uranium anti Thorium isotope behavior in estuarine systems. In Biogeochemistry of estuarine sediments. UNESCO, p 111-127 Mathieu D, Bemat M, Nahon D (1995) Short-lived U and Th isotope distribution in a tropical laterite derived from Granite (Pitinga river basin, Amazoitia, Brazil) application to assessment of weathering rate. Earth Planet Sci Lett 136 703-714... [Pg.573]

Martin J-M, Nijampurkar V, Salvadori F (1978b) Uranium and thorium isotope behavior in estuarine systems. In Biogeochemistiy of Estuarine Sediments. Goldberg ED (ed) UNESCO, Paris p 111-127 McKee BA, Todd JF (1993) Uranium behavior in a permanently anoxic Qord microbial control Limnol Oceanogr 38 408-414... [Pg.603]

Pages 10/11 BASF AG UNESCO Photodisc, Philips AG Getty Images... [Pg.114]

A more useful approach relies on knowledge of the empirical relationship between measured PET and certain variables, allowing PET calculation from just mean monthly temperature data and the average number of daylight hours by month. This method, established by C.W. Thomthwaite in 1948, has a practicality relevant to the scale of this study and to the drylands where environmental data are scarce, and was used by P. Meigs for his 1953 UNESCO map of world aridity. Though a more sophisticated related method that calculates evapotranspiration rates for... [Pg.7]

Meigs P. Review of Research on Arid Zone Hydrology. Paris UNESCO, 1953. [Pg.345]

Verheye W. Soils of arid and semi-arid areas. In UNESCO Encyclopedia of Life Support Systems. 2006. Submitted for publication. [Pg.353]

The area is 7,808 hectares and the altitude ranges from 250 to 762 m. The soil is categorized as an Orthic Acrisol according to the FAO/UNESCO scheme (FAO/UNESCO 1979). The vegetation includes dry evergreen forest (DEF), dry deciduous forest (DDF) and plantation plots as the major vegetative types (Fig. 1). The climate is classified as Aw (Koppen 1931). The annual precipitation is 1,260 mm and the average temperature is 26°C. [Pg.319]

FAO/UNESCO (1979) Soil map of the world. IX, Southeast Asia, UNESCO, Paris, France... [Pg.340]

Jeffrey SW, Mantoura RFC, Wright SW (1997) Phytoplankton Pigments in Oceanography. UNESCO Publishing, Paris, France... [Pg.99]

IOC (1975) Report of the ICG for GIPME Task Team for the Evaluation of Recommendation No. IV of the Joint IOC/WMO Task Team II on the Marine Pollution Monitoring Project UNESCO Paris... [Pg.441]

Isotope Hydrology Section, International Atomic Energy Agency, Nuclear techniques in ground-water hydrology, In Ground-water studies, UNESCO, Paris, Sections 10.1-10.4, 38 p., 1973. [Pg.220]

Martin, J. M., Nijampurkar, V. N., Salvador , F., Uranium and Thorium isotopes behaviour in estuarine systems, In Bio-geochemistry of Estuarine Sediments, Proceedings of Workshop held in Melreux, Belgium, Unesco Pub., 111-127... [Pg.384]

The receptors of interest are soils of agricultural (arable lands, grasslands) and non-agricultural (forests, steppes, heath lands, savanna, etc.) ecosystems. In non-agricultural ecosystems, the atmospheric deposition is the only input of heavy metals. Regarding the Forest ecosystems, a distinction should at least be made between Coniferous and Deciduous Forest ecosystems. When detailed information on the areal distribution of various tree species (e.g., pine, fir, spruce, oak, beech and birch) is available, this should be used since tree species influence the deposition and uptake of heavy metals and the precipitation excess. On a world scale, soil types can be best distinguished on the basis of the FAO-UNESCO Soil Map of the World, climate and ecosystem data from NASA database (1989). [Pg.74]

Remittance enclosed (Please make cheques payable to Rapra Technology Ltd. in Sterling drawn on a UK bank or in USS / Euros - Unesco coupons are also accepted.)... [Pg.126]

UNESCO satellite centre for trace element research... [Pg.97]

UNESCO, The Race Concept Results of an Inquiry (Paris UNESCO, 1952), pp. 11-15. [Pg.323]


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Responsibility UNESCO

UNESCO (United Nations

UNESCO (United Nations Education

UNESCO (United Nations Education Scientific and Cultural Organization

UNESCO (United Nations Educational, Scientific and

UNESCO (United Nations Scientific

United Nations Scientific Education UNESCO)

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