Eastern Base Section

The base sections had begun to report stock status to the theater and SOS chemical sections in April under the increased reporting requirement. However, their reports were little more comprehensive than the earlier informal reports until June, when comprehensive reports from ABS and MBS and a partial report from Eastern Base Section permitted the theater and SOS chemical sections to compile the first full-scale stock status report. Even then, quantity in the hands of troops was known for only one item, the eyeshield, which had been reported 500,000 short. The theater chemical section assumed... 

The Eastern, Western, Southern, and Northern Ireland Base Sections were organized by SOS ETO on 20 July 1942, but only with skeleton staffing. Ruppenthal, Logistical Support, I, 84-83. 

The Geochemical Ocean Section Program (GEOSECS) has produced data from which it is possible to profile the saturation state of seawater with respect to calcite and aragonite in the Atlantic and Pacific oceans. Representative north-south calcite saturation profiles for the Western Atlantic and Central Pacific oceans are presented in Figures 5 and 6 (based on 39). It was observed that the saturation state of seawater with respect to calcite at the CCD was close to constant ( 2 = 0.70 I" 0,05) except in the southern extremes (39). Broecker and Takahashi (31) have recently found that the carbonate ion concentration is close to constant at the FL, when appropriate corrections are made for pressure. The saturation state of seawater at the FL, calculated by the method presented in this paper, is 0.80 0.05. Berger (40) has presented profiles for Rq, FL, CCD and CSL (calcite saturation level) in the eastern and western Atlantic ocean (see... 

Figure 14.14 Vertical sections of (A) N2O (nM) and (B) AN2O/AOU (x 10 along the 90°E transect in the eastern Indian Ocean based on observations in May-July 1987 (from Butler et al, 1989 and Nevison etal., 2003).

Figures 15-17 show how this composition compares to other estimates of crust composition. Figure 15 shows that our new composition has generally higher MgO, CaO, and FeO, and lower Na20 and K2O than most other seismically based models. The differences between our model and that of Wedepohl (1995) and Gao et al. (1998a) likely reflect the regional character of these latter models (western Europe, eastern China), where the crust is thinner and more evolved than the global averages (Chirstensen and Mooney, 1995, and Rudnick and Fountain, 1995). The lower MgO and higher alkali elements in Christensen and Mooney s model compared to ours must stem from the differences in the chemical databases used to construct these two models, as the lithological proportions of the deep crust are very similar (Section 3.01.3).

This model has been exercised on a variety of AQCR s for which an accurate emission inventory, meteorological data base, and measured ground level pollutant concentrations are available. The results discussed in this paper represent analyses of the New York, Philadelphia, Niagara Frontier, St. Louis, and Milwaukee AQCRs 13, 14). These AQCRs represent a reasonable cross-section of the eastern urban AQCRs where the primary sulfur dioxide ambient air quality problem exists. The results of these analyses indicate that the level of control required by emission source to achieve ambient air quality standards can be forecast with greatly increased assurance. The following conclusions from this exercise should be considered in the near-term achievement of ambient air quality standards. 

Applied to the Michigan Basin in east-west cross section, the "lower black" shale (A) represents the Antrim Shale of western Michigan and that part of the eastern Antrim Shale identified by Subunits 1A, IB, 1C and 2. The "green-gray" facies (C) is the Ellsworth Shale, and the "upper black" (B) is represented by all Antrim Shale above Unit 2 and below the base of the Bedford Shale. The uniformity of the lower beds of the Antrim Shale has been noted by several others (20, 23), and a westward source for the Ellsworth has been postulated by several (20, 23-25) Nevertheless, the westward source seems more applicable to those beds above the western Antrim Shale, i.e., above the beds termed "lower black" in this paper. 

Figure 4, Cross-section of the thicknesses of the stratigraphic units above the base of the Cleveland HGZ (top), and variation in hydrogen and carbon for the Sunbury shale and Cleveland HGZ in eastern Kentucky (bottom).

Zeolitized tuffs from the Eastern Rhodopes Paleogene volcanic area have been studied. Na-mordenite and Ca-clinoptilolite are the main products of the acid glass alteration. Erionite, analcime and stilbite are also identified. Opal and adularia are most abundant at the base of tuff succession. Zeolite content increases upward mordenite is prevailing in the middle and ciinoptilolite in the topmost levels of the studied section. Compared with fresh perlite zeolitized tuffs are depleted in Na20, Y, Rb, Ba and Mn and enriched in CaO and Sr. C.E.C. coefficient ranges from 60.66 to 94.53 meq/lOOg. Low-temperature hydrothermal solutions, heated by the initially hot pyroclastic material are the inferred cause of the zeolite formation. 

Based on the previous studies, the following questions are raised What about women s situation in urban design of cities in the Middle Eastern world How are their needs and values being met in cities What role do they have in desigrting and managing cities These issues will be investigated in the next section which is concerned with women s needs in designing Middle Eastern cities, with partictrlar attention to women s requirement for privacy. 

The chapters in this section focus on the structural transformation of engineering education in historical and contemporary perspective, with a focus on processes around the globe. Based largely on country and region-specific case studies, these chapters discuss developments in the United States, Western and Eastern Europe, Brazil, India, and Latin America, respectively. They also provide the broad canvas upon which the subsequent sections of this two-volume edited compilation can be interpreted. 

In 8 seconds, the LFL envelope s SE extremity has impacted the northwest corner of the Main Office building and has commenced exiting from the eastern domain boundary between the southern ends of section 25A and 7 and the northern wall of the office building. The base of the LFL footprint has progressed northward to the base of R1 with the northern boundary of the UFL just past the base of R4. 

Successful plastic wheels have been produced, in the context of sports vehicles. Wheels moulded from polycarbonate were in use for rallying in the former USSR and other Eastern Bloc countries in the 1970s, based on a Bulgarian process for injection moulding very thick sections without voids. Wheels of this type however would probably not pass modem specifications... 

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