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Measurement cont

TABLE 1.5.1 Disasters and Their Effects on Safety Measures (cont d)... [Pg.23]

B. Lake measurements cont.) Crater Lake, Oregon USA 380 ... [Pg.72]

Table 7.2 Matrix of Enabling Elements, Processes Process Owners, and Number of Performance Measures—cont d... [Pg.144]

Potential of zero charge cont.) contribution of the solvent, 158 Conway and Colledan, and the determination of, 34 on copper, and aqueous solution, 89 crystal phase and, 44 crystal face specificity of, 21 and the crystal surface specificity, 152 DeLevie, on the effect of the density of broken bonds on, 75 dependence upon crystal phase, 154 dependence upon time of measurement, 150,151... [Pg.639]

J.P. Steyer, J.C. Bouvier, T. Conte, P. Gras, J. Harmand, and J.P. Delgenes. On-line measurements of COD, TOC, VPA, total and partial alkalinity in anaerobic digestion process using infra-red spectrometry. Wat. Sci. TechnoL, 45(10) 133-138, 2002. [Pg.163]

Caramella, C., Colombo, P., Conte, U. Ferrari, F., and La Marma, A., Water uptake and disintegrating force measurements Towards a general understanding of disintegration mechanisms. Drug Dev. Ind. Pharm., 12 1749-1766 (1986). [Pg.290]

J. R. Koseff. Plume dispersion in a stratified, near-coastal flow Measurements and modeling. Cont. Shelf Res. 20, 637-663 (2000). [Pg.129]

Stacey, M. T., E. A. Cowen, T. M. Powell, E. Dobbins, S. G. Monismith, and J. R. Koseff. Plume dispersion in a stratified, near-coastal flow Measurements and modeling. Cont. Shelf Res. 20, 637-663 (2000). [Pg.346]

DeMaster, D.J., McKee, B.A., Nittrouer, C.A., Jiangchu, Q., and Quodong, C. (1985) Rates of sediment accumulation and particle reworking based on radiochemical measurements from the continental shelf deposits in the East China Sea. Cont. Shelf Res. 4, 143-158. [Pg.572]

Bristol, E. H., "On a New Measure of Interaction for Multi-variable Process Control," IEEE Trans. Auto. Cont., 1966, AC-11, 133. [Pg.116]

We thank the Union Carbide Corp. for permission to publish this work. Acknowledgment also goes to J. J. Bohan and L. B. Conte for thgir technical assistance to A. D. Hammerich for the NMR measurements and to L. M. Robeson for the dynamic mechanical data. [Pg.575]

Holligan PM, Fernandez E, Aiken J, Balch WM, Boyd P, Burkill PH, Finch M, Groom SB, Malin G, Muller K, Purdie DA, Robinson C, Trees CC, Turner SM, Vander-wal P (1993) A Biogeochemical Study Of The Cocco-lithophore, Emiliania-Huxleyi, In The North-Atlantic. Global Biogeochem Cycles 7 879-900 Holligan PM, Turner SM, Liss PS (1987) Measurements of dimethyl sulphide in frontal regions. Cont Shelf Res 7 213-224... [Pg.273]

Figure. 10.7. Cont d. (C) 15%. Marks are the measured results while full lines are the reference values. (D) Particle size information measured to obtain a reference velocity by applying Lloys and Berry s multiple scattering theory. (Reproduced with permission of Elsevier, Ref [77].)... Figure. 10.7. Cont d. (C) 15%. Marks are the measured results while full lines are the reference values. (D) Particle size information measured to obtain a reference velocity by applying Lloys and Berry s multiple scattering theory. (Reproduced with permission of Elsevier, Ref [77].)...
The various read-out techniques, as described before, for linear PSD s can be applied for two-dimensional systems too. One should however bear in mind that, when complete diffraction patterns have to be measured, the conting rate capability plays an even more important role. A linear detector is exposed to only a fraction of the total flux of a pattern, as compared to a two-dimensional detector, which is intended to measure the entire area at once. [Pg.77]

The relationship observed in sediments closely mimics the relation measured between unsaturation in photic zone particulates (Conte et al. in press) and in situ temperature. We should note, however, that the calibration of sedimentary U 7 to mean annual SST represents a statistical relationship and should not be interpreted in too simphstic a manner. We have seen above that this relation holds for sediments because alkenone synthesis generally occurs in the mixed layer, and because alkenone production by selected hapto-phyte algae is less seasonal than many other planktonic groups. Lurthermore, temperatures during the season of maximal alkenone production generally come close to mean annual SST. The index, therefore, is a quite robust proxy for mean annual temperature. It should be kept in mind that regional variations in the factors that control the depth and seasonality of alkenone production can cause the index to deviate from mean annual SST. [Pg.3272]

Table 3.5. Measuring techniques for the investigation of monolayers (cont.). Table 3.5. Measuring techniques for the investigation of monolayers (cont.).

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Glass, inorganic (Cont measurement

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