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Monterey

B. R. White, "Reclamation and Recycling of Propellants and Explosive," ia J TNN TF Safety and Environmental Protection Subcommittee Meeting, Monterey, Calif., May 1988. [Pg.27]

Fig. 14. Preferred Hquefaction-coking Hquid yields in the EDS process for various coals where Hrepresents Flexicoking Hquids and , Hquefaction Hquids (124). A, Ireland (West Virginia) B, Monterey (Illinois) C, Burning Star (Illinois) D, Wyodak (Wyoming) and E, Big Brown (Texas). Fig. 14. Preferred Hquefaction-coking Hquid yields in the EDS process for various coals where Hrepresents Flexicoking Hquids and , Hquefaction Hquids (124). A, Ireland (West Virginia) B, Monterey (Illinois) C, Burning Star (Illinois) D, Wyodak (Wyoming) and E, Big Brown (Texas).
J. E. Besser, Proceedings of the 7th Vertebrate Pest Control Conference, Monterey, Calif., 1976, p. 11. [Pg.123]

California contains the largest formation of diatomite in the United States the Monterey Formation extends from Point Arena in Mendocino County in the north to San Onofre in the south (7). The most extensive deposit is near Lompoc, Santa Barbara County, and is of marine origin. A freshwater deposit is being mined near Burney, Shasta County. Other important deposits (not mined as of this writing) are located in Monterey, Fresno, Inyo, Kem, Orange, San Bemadino, San Joaquin, Sonoma, and San Luis Obispo counties. [Pg.56]

A. Soutar, S. R. Johnson, and T. R. Baumgartner, in C. Isaacs and J. Garison, eds.. The Monterey Formation and Related Siliceous Rocks of California, Society of Economic Paleontologists and Mineralogists, 1981, p. 123. [Pg.59]

Capital Costs A typical medium-scale RO seawater plant might produce 0.25 mVs (6 MGD). For a plant with an open sea intake, seawater salinity of 38 g/1, and conversion of 45 percent, the overall cost woiild be 26.5 miUiou (1996). A capital breakdown is given in Table 22-18. Capital charges are site specific, and are sensitive to the salinity of the feed. A plant of this size would likely contain six trains. For seawater RO, the Best estimate for the slopes of the family of lines in Fig. 22-55 is —0.6 for the equipment and 0.95 for the membranes. Capital charges, shown in TaBle 22-19, usually dominate the overall economics the numbers presented are only an example. Seawater economics are based on Shields and Moch, Am. Desalination Assn. Conf. Monterey CA (1996). [Pg.2037]

Jeanloz, R., and Grover, R. (1988), Birch-Murnaghan and Us-Up Equations of State, in Proceedings of the American Physical Society Topical Conference on Shock Waves in Condensed Matter, Monterey, CA, 1987 (edited by Schmidt S.C. and N.C. Holmes), Plenum, New York, pp. 69-72. [Pg.112]

Williams, J. C., 1989, A Data-Based Method for Assessing and Reducing Human Error to Improve Operational Performance, Proceedings of the 1988 IEEE Fourth Conference on Human Factors and Power Plants, Monterey, CA, June 5-9, pp 436-450, IEEE. [Pg.491]

Fifth, 1987 Monterey Schmidt and Flolmes North-FIolland 1988... [Pg.11]

Maiiahan, S. E. (1984). Enviroumeiitil Chemistry, 4th ed. Monterey, CA Brooks/Cole Publishing Company. [Pg.251]

Wemgarten, L., and Weingarten, S. (1992). The Water Heater Handbook A Hands-On Guide to Water Heaters. Monterey, CA Elemental Enterprises. [Pg.1218]

Chul Kim, U. R. and van Rooyen, D., Strain rate and temperature effects on the stress corrosion cracking of Inconel 600 steam generator tubing in the (PWR) primary water conditions , Proc. 2nd Int. Conf. on Environmental Degradation of Materials in Nuclear Power Systems-VIalet Reactors, Monterey, USA, 9-12 Sept. 1985, American Nuclear Society, pp. 448-55 (1986)... [Pg.1326]

Wolfson, R. G., Application Specific Electronic Materials by Ion Implantation and MOCVD, Proc. of Conf. on High Performance Inorganic Coatings, Monterey, CA, G.A.M.I., Gorham, ME 04038 (1988)... [Pg.365]

Environmental Sciences Division, Oak Ridge National Laboratory, P.O. Box 2008, Oak Ridge, TN 37831-0335 Monterey Bay Aquarium Research Institute, 160 Central Avenue, Pacific Grove, CA 93950-0020... [Pg.392]

Fessenden and Fessenden, Organic Chemistry , 6th ed., Brooks/Cole, Monterey, CA, 1998. [Pg.1625]

Schomburg CJ, Glotfelty DW, Seiber JN. 1991. Pesticide occurrence and distribution in fog collected near Monterey, California. Environ Sci Technol 25 155-160. [Pg.230]

Tam, W.F.S. and Bell, M., in AIAA-93-2211, 29th AIAA/ASME/SAE/ASEE Joint Propulsion Conf and Exhibit, Monterey, CA, June 28-30, 1993. [Pg.394]

P. radiata (Little) D. Don P. remota (Little) Bailey Hawksworth Monterey pine Cool and Zavarin (1992) Snajberk and Zavarin (1986)... [Pg.157]

Crews, P., Campbell, L. and Heron, E. 1977. Different chemical types of Plocamium violaceum (Rhodophyta) from the Monterey Bay Region, California. J. Phycol. 13 297-301. [Pg.308]

Fig. 4.14. Tracing climate change in the Miocene. Shown here are records of ice volume and temperature (based on foraminiferal S 0) and relative organic carbon burial (based on foraminiferal S C), compared with the CO2 estimates of Pagani et al. (1999), and tectonic events that may have affected ocean heat transport. Trends in CO2 are consistent with organic carbon burial and CO2 drawdown during the Monterey Excursion, but cannot explain the Miocene Climatic Optimum (MCO) or expansion of the East Antarctic Ice Sheet (EAIS). Fig. 4.14. Tracing climate change in the Miocene. Shown here are records of ice volume and temperature (based on foraminiferal S 0) and relative organic carbon burial (based on foraminiferal S C), compared with the CO2 estimates of Pagani et al. (1999), and tectonic events that may have affected ocean heat transport. Trends in CO2 are consistent with organic carbon burial and CO2 drawdown during the Monterey Excursion, but cannot explain the Miocene Climatic Optimum (MCO) or expansion of the East Antarctic Ice Sheet (EAIS).
The studies by Pagani et al. (1999), Pearson and Palmer (2000) and Kashiwagi et al. (2000) suggest that Pqo did not decrease from the Miocene to the present time. This view is not in agreement with that was favored by previous works such as Raymo s hypothesis (Raymo et al., 1988) and Monterey s hypothesis (Vincent and Berger, 1985). If their estimates are correct, it is inferred that PcOa is not an important factor affecting cooling from the middle Miocene to present. [Pg.443]

Vincent, E. and Berger, W.H. (1985) Carbon dioxide and polar cooling in the Miocene The Monterey Hypothesis. In Sundquist, E.T. and Broecker, W.S. (eds.). The Carbon Cycle and Atmospheric CO2 Natural Variations Archean to Present. Washington D.C. Am. Geophysical Union, pp. 455 68. [Pg.447]

F. Hofler and G. Alt, Proceedings 11th International Symposium on Capillary Chromatography, Monterey, CA (1990). [Pg.566]

From the 323 MTBE treatment profiles, eight projects were identified where MTBE was treated using phytoremediation. These projects used various approaches, including hybrid poplar trees, Monterey pine, oak, eucalyptus, and engineered wetlands. [Pg.1045]

Deeb, R.A. and Kavanaugh, M., In-Situ biological destruction of MTBE Field engineering solutions, Remediation of Chlorinated and Recalcitrant Compounds Conference, Monterey, CA, May 23, 2002. [Pg.1052]

Landmeyer, J.E., Vrblosky, D.A., and Bradley, P.M., MTBE and BTEX in trees above contaminated groundwater, Battelle International Conference on Remediation of Chlorinated and Recalcitrant Compounds, Monterey, CA, 2000. [Pg.1054]

Monterey Peninsula Landfill, Marina, CA (ACAP project) Nonhazardous waste site Operational May 2000... [Pg.1083]

In the solvent-refined coal pilot plant at Wilsonville, Alabama, the coal slurry is heated to reaction temperature in 3-4 minutes residence time in the preheater. The slurry is then held in the dissolver for an additional 40 minutes before it is filtered to obtain specification solvent-refined coal. By bypassing the dissolver and going directly to the filters, samples of short-contact time (SCT) SRC were produced from Illinois 6 (Monterey) and West Kentucky coals. [Pg.179]

Figure 1. Elemental composition of short-contact-time and regular Monterey SRC (C )> regular contact time short contact time. Figure 1. Elemental composition of short-contact-time and regular Monterey SRC (C )> regular contact time short contact time.

See other pages where Monterey is mentioned: [Pg.175]    [Pg.422]    [Pg.1130]    [Pg.332]    [Pg.338]    [Pg.732]    [Pg.85]    [Pg.107]    [Pg.174]    [Pg.238]    [Pg.285]    [Pg.286]    [Pg.287]    [Pg.928]    [Pg.135]    [Pg.138]    [Pg.138]    [Pg.138]    [Pg.181]   
See also in sourсe #XX -- [ Pg.152 ]




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California Monterey Formation

High-sulfur Monterey kerogens, pyrolysis

Liquefaction Monterey bituminous

Monterey Bay Aquarium

Monterey Bay Aquarium Research Institute

Monterey Formation

Monterey Pine

Monterey coal

Monterey coal , liquefaction

Monterey coal , liquefaction bituminous

Monterey concentrations

Pyrolysis of high-sulfur Monterey kerogens

Shale Monterey

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