Water data

U.S. Geological Survey, Water Resources Data for New York, vol. 1 Eastern New York Excluding Eong Island—WaterYear 1988, E.S. Geological Survey Water Data Report NY 551, Springfield, Va., National Technical Information Service 1989. 

M. W. KeUogg Co., Saline Water Data Conversion Engineering Data Book, 3rd ed.. Office of Saline Water Contract No. 14-30-2639, U.S. Department of the Interior, Washington, D.C., 1975. 

Figure 9-43 represents the water-air and ammonia-water data for Berl saddles by [65, 67] ... 

The effective interfacial area is used in mass transfer studies as an undivided part of individual and overall coefficients when it is difficult to separate and determine the effective area. The work of Shulman et.al.,65 presents a well organized evaluation of other work in addition to their own. One of the difficulties in correlating tower packing performance lies in obtaining the correct values for the effective interfacial areas of the packing on which the actual absorption, desorption, chemical reaction, etc. are completed. Figures 9-47 A, B, C, D, E, F, G present a correlation for Avater flow based on the ammonia-water data of Fellinger [27] and are valid for absorption work. 

Variability of Seawater Vertical sections through seawater showing the distribution of temperature, salinity, and oxygen for the Pacific Ocean and Western Atlantic Ocean are shown in Figures 21.3 and 21.4. The global variability of natural seawater and its effects on corrosion have been reviewed in particular with respect to seasonal variation of temperature, salinity, oxygen and pH in the Pacific surface water. Data is also given on... 

Fig. 9. CD for poly(L-proIine) II helix in water. Data from Carver et al.18)...

VIII. The Correlation of Water Data for Uniformly Heated Channels. 249... 

A less rigorous approach to modeling than the one described above is an empirical procedure whereby water data for a given geometry may be linked with that of another fluid by numerical scaling factors without actually... 

Fig. 6.30 Comparison of correlation predictions with (a) R-134a (Lee and Mu-dawar (2005a)) and (b) water Qu and Mudawar s (2003a) micro-channel water data. Reprinted from Lee and Mu-dawar (2005a) with permission...

Figure 6.3. 5 "0 in surface water (data from Gat 1980) compared with that in biogenic phosphates of various mammals from many world regions (data shown in squares are from conventional phosphate analyses Longinelli 1984 Luz et al. 1984 Ayliffe and Chivas 1990 D Angela and Longinelli 1990 Yoshida and Miyazaki 1991 Huertas et al. 1995). For comparison, plotted as filled circles, are 8 0 values for tooth enamel analyzed by laser fluorination (six humans, one shark, and one wolf Kohn et al. 1996). 

Fig. 3. Rate of CO2 assimilation. A, and leaf conductance, g, in Zea mays on various days after withholding watering. Data are those shown in Fig. 2 with 30.5 Pa ambient partial pressure of CO2 (after Wong et al., 1985).

Figure 5. Evolution of cathodic response to 10 pA cm" galvanostatic pulse as Ecorr increases during biofouling of 316L stainless steel in fresh river water. Data shown by solid lines and circles indicate points generated from curve lit to Eq. (6). (Reprinted from Ref. 12 with permission from NACE International.)...

CONSTANT STD1=2287,4 CONSTANT STD2=-1.4657E4 CONSTANT STD3=4.3092E5 WATER DATA CONSTANT cpw=l CONSTANT RHOw=62.3... 

W.W. Lapham, F.D. Wilde, and M. T. Koterba, Ground-Water Data-Collection Protocols and Procedures for the National Water-Quality Assessment Program Selection, Installation, and Documentation of Wells and Collection of Related Data, Open-File Report 95-398, US Geological Survey, Reston, VA (1995). 

Rard (1992) reported the results of isopiestic vapor-pressure measurements for the aqueous solution of high-purity NiCl2 solution form 1.4382 to 5.7199 mol/kg at 298.1510.005 K. Based on these measurements he calculated the osmotic coefficient of aqueous NiCb solutions. He also evaluated other data from the literature and finally presented a set of smoothed osmotic coefficient and activity of water data (see Table IV in original reference). 

Caffeine contained in tea beverage is absorbed at about the same rate as caffeine in coffee, cola drinks, or in pure water. Data to support this conclusion was obtained in a human feeding experiment.109 The theory that complexation of caffeine with the polyphenolic material in tea retards absorption110-111 is not borne out. 

Table 24.1 Limiting cooling water data for four operations.

The shifted limiting cooling water data are given in Table 24.2. 

Malenkov claimed that Eq. (2-67) effectively correlated five sets of water data, three sets of methanol data, and one each of ethanol, w-pentane, and carbon tetrachloride—all obtained at 1 atm—in 11 different investigations. 

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