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Anonymous, 1972: Calculation of basic hydrological data as reflected in the WMO programme in operational hydrology. Congress on Irrigation and Drainage 8th Varna 1972transactions: 29
Wilkins, H.F., 1986: The influence of 32 degrees , 21 degrees , 4 degrees or 27 degrees , 18 degrees , 10 degrees or 21 degrees , 17 degrees , 13 degrees C light/dark temperature combinations during the various growth phases of the Easter lily (Lilium longiflorum Thunb.). In 3-year studies, Nellie White plants were grown in natural days or in a 12/12 h light/dark photoperiod at a wide range of temperature combinations. Regardless of the developmental stage the range of acceptable forcing temperatures was very narro...
Hohlin, D., 1986: Can basic numbers be solved by new calculation methods? Use of basic numbers in the calculation of personnel needs oriented to care categories. Krankenpflege 40(3): 102-104
Arnorsson Stefan; Sigurdsson Sven; Svavarsson Hoerdur, 1982: The chemistry of geothermal waters in Iceland; I, Calculation of aqueous speciation from 0 degrees to 370 degrees C. Geochimica et Cosmochimica Acta: , Pages 1513-1532. 1982.
Garcia B.J.; Lopezd. J., 1970: Formula for the calculation of potential evapotranspiration adapted to the tropics (15 degrees N.-15 degrees S.). The formula proposed was found to give consistently more accurate results than other methods when compared with measured evapotranspiration at 6 locations in Venezuela.
Stefansson Andri, 2001: Dissolution of primary minerals of basalt in natural waters; I, Calculation of mineral solubilities from 0 degrees C to 350 degrees C. The solubilities of forsterite, fayalite, enstatite, ferrosilite, hedenbergite, diopside, anorthite, high-albite, magnetite, hematite, ulvospinel, ilmenite, F-apatite and OH-apatite and olivine, plagioclase, orthopyroxene, clinopyroxene and Fe-Ti...
Hovey, J.K.; Hepler, L.G., 1990: Thermodynamics of sulphuric acid: apparent and partial molar heat capacities and volumes of aqueous HSO4- from 10-55 degrees C and calculation of the second dissociation constant to 350 degrees C. Apparent molar heat capacities and volumes of aqueous solutions containing H2SO4 have been determined from 10 to 55 degrees C. These results are complicated by the presence of bisulphate and sulphate ions as well as effects due to chemical relaxat...
Hald N., 1978: Field investigations of Tertiary basic igneous rocks between 72 degrees and 73 degrees 30'N, northern East Greenland. Rapport - Groenlands Geologiske Undersoegelse = Report - Geological Survey of Greenland 90): 109-113
Scarfe C.M., 1973: Experimental determination of water solubilities in basic melts at 1150 degrees C and 1350 degrees C at 1 and 2 kilobars pressure. Basaltic melts dissolve similar amounts of water to granitic melts at same P-T conditions, picrite and olivine melanephelinite melts have lower solubilities than basaltic melts.
Nicastro, C., 1978: Basic contradictions in the concept of day-degrees. Study of day-degrees in relation to plants of wheat, maize and groundnut grown in different environments. In an attempt to see if there was any relationship between day-degrees and yield, data on the accumulation of day-degrees during the growth of wheat cv. Pitic 62 grown in 13 countries between long. 4 deg -40 deg N, maize cv. Dekalb 361 XL in Pisa...