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Feature topography

Surface topography features of the scolex and strobila of the cysticercus of Hydatigera taeniaeformis. IRCS Medical Science Microbiology, Parasitology and Infectious Diseases, 8 28-9. [Pg.329]

Making a comprehensive analysis from the landslide slope s topography features, lithology, soil structure, deformation and failure characteristics, the landslide s deformation and failure mode is excavated the foot of the slope and then the slope lose support—surface precipitation and water pipe leakage due to slope body weight gain, strength... [Pg.862]

For both of the PFOM concentration studies shown in fig. 4.3a, the PFOM thickness linearly extrapolated to zero PFOM concentration intercepts the vertical axis at about 1.5-2.0 nm. This thickness is nearly the same as the length of the monomer unit of the PFOM polymer shown in fig. 4.11a. Since the PFOM thickness-vs.-con-centration curve must pass through zero, it seems that a layer of the PFOM forms ou the surface at a very low concentration. The PFOM film thickness is also relatively independent of withdrawal rates between 0.2 to 1.6 mm/s, as shown in fig. 4.3b. The interpretation of the rapid layer formation, which is nearly one monomer unit thick, can be extended to suggest that the formation of a uniform layer may be possible at very low PFOM concentrations. An apparent nonzero intercept of the film thickness-vs.-concentration plot, and the film thickness being relatively independent of withdrawal rate, can also arise from rapid evaporation at the meniscus of a solvent that does not wet the substrate. It would be of interest to explore the region of even lower concentration to avoid excess PFOM deposit on surface topography features of the slider that accumulate a meniscus or pendant drops of solution. [Pg.80]

Solid-wa.ste-filling plan. The specific method of filling will depend on the characteristics of the site, such as the amount of available cover material, the topography, and local hydrology and geology. To assess future development plans, it will be necessary to prepare a detailed plan for the layout of the individual solid-waste cells. On the basis of the characteristics of the site or the method of operation (e.g., gas recovery), it may be necessaiy to incorporate special features for the control of the movement of gases and leachate from the landfill. [Pg.2257]

Many of the factors that influence the c.xtcnt of contamination are site specific, cither climatic or hydrogeological. Other factors that influence the extent of contamintition relate to land surface features such as topography or dcNclopmcnt, which determine exposure routes. Additional important... [Pg.363]

Ikonopisov284 has conducted a systematic study of breakdown mechanisms in growing anodic oxides. He has enumerated factors significantly affecting the breakdown (nature of the anodized metal, electrolyte composition and resistivity) as well as those of less importance (current density, surface topography, temperature, etc.). By assuming a mechanism of avalanche multiplication of electrons injected into the oxide by the Schottky mechanism, Ikonopisov has correctly predicted the dependence of Ub on electrolyte resistivity and other breakdown features. [Pg.481]

The GR15 and T42 topography originate from the ET0P05 [NOAA (1988)] data set interpolated onto the model grid. Hereby, specific topographic features, such as the important conduits of overflows and throughflows, were adjusted to observed depths [Marsland et al (2003)]. [Pg.26]

In situations with no observed data, one possible means to evaluate status is to use a similar analogous site for which data are available, and to assume that the assessment made from the observed data can be applied validly to both sites. The site for which data are available must have good status according to the WFD. For instance, bodies subject to similar pressures and with similar characteristics could be grouped. It is noteworthy that proximity cannot be taken on its own as an indication of similarity since the features of the catchments, such as climate, topography and ecology, can change abruptly. [Pg.384]


See other pages where Feature topography is mentioned: [Pg.556]    [Pg.26]    [Pg.209]    [Pg.911]    [Pg.31]    [Pg.1404]    [Pg.911]    [Pg.698]    [Pg.112]    [Pg.859]    [Pg.281]    [Pg.214]    [Pg.556]    [Pg.26]    [Pg.209]    [Pg.911]    [Pg.31]    [Pg.1404]    [Pg.911]    [Pg.698]    [Pg.112]    [Pg.859]    [Pg.281]    [Pg.214]    [Pg.235]    [Pg.87]    [Pg.198]    [Pg.381]    [Pg.701]    [Pg.119]    [Pg.321]    [Pg.17]    [Pg.106]    [Pg.232]    [Pg.253]    [Pg.258]    [Pg.165]    [Pg.158]    [Pg.229]    [Pg.680]    [Pg.55]    [Pg.65]    [Pg.571]    [Pg.80]    [Pg.266]    [Pg.192]    [Pg.179]    [Pg.231]    [Pg.200]    [Pg.104]    [Pg.186]    [Pg.470]    [Pg.383]    [Pg.46]   
See also in sourсe #XX -- [ Pg.137 ]




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