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Stream systems

If back-pressure is too low or demand too high, the compressor will be unable to provide sufficient volume or pressure to the down-stream systems. In this instance, the discharge pressure will be noticeably lower than designed. [Pg.561]

This type of compressor will continue to compress the air volume in the down-stream system until (1) some component in the system fails, (2) the brake horsepower exceeds the driver s capacity, or (3) a safety valve opens. Therefore, the operator s primary control input should be the compressor s discharge pressure. If the discharge pressure is below the design point, it is a clear indicator that the total down-stream demand is greater than the unit s capacity. If the discharge pressure is too high, the demand is too low and excessive unloading will be required to prevent failure. [Pg.561]

Reddy KR, Flaig E, Scinto LJ, Diaz O, Debusk TA (1996) Phosphorus assimilation in a stream system of the Lake Okeechobee. J Am Water Resour Assoc 32 901-915... [Pg.196]

Fig. 12. On-line enzyme reactor system designs, merging stream system (Top) and immobilized-enzyme reactor system (Bottom). A = mobile phase, B = enzyme solution... Fig. 12. On-line enzyme reactor system designs, merging stream system (Top) and immobilized-enzyme reactor system (Bottom). A = mobile phase, B = enzyme solution...
Method A packed-bed throwaway system to remove organic pollutants from oily waste stream. System component A contactor system, and a pump station designed for a contact time of 30 min and hydraulic loading of 162 L/min/m2 (4gpm/ft2). [Pg.378]

We developed a staggered parallel HPLC system with a CTC HTS PAL autosampler equipped with trio valves. The system consists of four (six if gradient is needed) independent HPLC pumps. Parallel analysis is achieved by an offset dual-stream system with a time delay that allows efficient staggering of MS acquisition times. [Pg.77]

Table 1. Concentrations and estimated daily fluxes of Al, Cd, and F through the Banyu Pahit stream system, based on approximate stream discharges of 60 L/s (from the Crater Lake) and 4000 L/s (near Blawan from Delmelle Bernard, 2000). ... Table 1. Concentrations and estimated daily fluxes of Al, Cd, and F through the Banyu Pahit stream system, based on approximate stream discharges of 60 L/s (from the Crater Lake) and 4000 L/s (near Blawan from Delmelle Bernard, 2000). ...
Maioloni B, Lencioni V (2001) Longitudinal distribution of macroinvertebrate assemblages in a glacially influenced stream system in the Italian Alps. Freshw Biol 46 1625... [Pg.192]

Zah R, Uehlinger U (2001) Particulate organic matter inputs to a glacial stream system in the Swiss Alps. Freshw Biol 46 1597... [Pg.221]

Process Stream System Constituents Wastestream Constituent... [Pg.208]

Mariner 9 tly-by of Mars revealed a surface remain of massive blocks of tumbled character cut by ridges and grahen-type troughs Huge volcanic peaks dominate a pock-marked landscape. Extensive channels characierislrc of concentrated erosive powers of torrential floods were also evident, as were braided stream systems emanating front what were resolved to be plateau-type elevations. [Pg.1011]

The Blue Stream sub-sea pipeline (BS) project was constructed to deliver gas from the Russian Black Sea region to Turkey without involving any transit country. Gas might be Russian, Turkmen or Kazakhstani. However, in contrast to Gazprom s expectation the delivery through the Blue Stream system has been delayed for a long time because of disputes with Turkey. To resolve this Blue Stream problem, the Russian presidential envoy to the Caspian Region, Mr. Viktor Kalyuzhnyi, offered to build a gas... [Pg.12]

Barium carbonate 154 fluid jet stream system To remove C02 from waste... [Pg.285]

The main significance of the terminal velocity lies in the fact that it defines the minimum gas velocity requested. The particle enters the system at Point 1 at zero velocity. If a gas velocity is employed so that u, < uh the particle cannot get into but drops out of the system if the gas velocity makes the relative velocity equal the terminal velocity, i.e., u, = it, the particle will move with a constant velocity of zero with respect to the ground, and so will remain at Point 1 while if the gas velocity makes the relative velocity greater than the terminal velocity, i.e., u,> it, the particle will be accelerated by the gas flow to the terminal velocity and will then move towards Point 2 at that velocity. Therefore, the terminal velocity is necessary for the determination of the operational range of the gas flow velocity for a specific vertical gas-solid impinging stream system. [Pg.59]

A Side-stream systems - airlift [Norit X-flow) B Ultra-Flo - side-stream dead-end setup... [Pg.390]

Figure 16.17 Examples of side-stream systems based on airlift or deadend mode. Figure 16.17 Examples of side-stream systems based on airlift or deadend mode.
Pusey BJ, Arthington AH, MacClean J. 1994. The effects of a pulsed application of chlor-pyrifos on macroinvertebrate communities in an outdoor artificial stream system. Ecotoxicol Environ Safety 27 221-250. [Pg.355]

Reactor Model. The design of an industrial packed-bed reactor requires a reactor model as well as the chemical and the heat and mass transfer parameters of the catalyst bed - gas stream system. Since these parameters are model-specific, it seemed advisable to employ a continuum model for the reactor calculation. This is the only model to date for which the literature contains consistent data for calculating heat and mass transfer parameters (5,6,7). This model in its... [Pg.4]

The main objective of design is the flowsheet architecture. We mean by this type of units, performance and connections by material and energy streams. Systemic techniques are capable of calculating optimal targets for subsystems and components without the need of the detailed sizing of equipment. [Pg.15]

Figure 12.1. Illustration of the major pathways linking terrestrial and stream ecosystems in the Amazon basin and the main physicochemical processes operating in each ecosystem. Processes identified by an asterix have been examined in Amazon stream systems, although the number of these studies and diversity of terrain types examined is generally very limited. Figure 12.1. Illustration of the major pathways linking terrestrial and stream ecosystems in the Amazon basin and the main physicochemical processes operating in each ecosystem. Processes identified by an asterix have been examined in Amazon stream systems, although the number of these studies and diversity of terrain types examined is generally very limited.
The lithologic control of baseflow chemistry extends also to dissolved organic carbon (DOC). In a one-year comparison of Clearwater (Oxisol on Barreiras formation) and blackwater stream systems (Spodosol on sand deposits), McClain et al. (1997) reported consistent groundwater DOC contents of near 3000 pM in the blackwater system and 100 to 300 pM in the clearwater system (Fig 12.6). Baseflow in the two systems reflected this large difference in DOC content, which McClain et al. (1997) attributed to the different DOC sorption characteristics of Spodosols and Oxisols. [Pg.193]

Question What are the biogeochemical consequences of anthropogenic activities to streams in the Amazon (that is, how do these activities alter the natural functioning of stream systems), and what management practices best minimize adverse effects ... [Pg.200]


See other pages where Stream systems is mentioned: [Pg.298]    [Pg.189]    [Pg.266]    [Pg.233]    [Pg.252]    [Pg.261]    [Pg.218]    [Pg.568]    [Pg.662]    [Pg.511]    [Pg.511]    [Pg.166]    [Pg.253]    [Pg.87]    [Pg.88]    [Pg.270]    [Pg.367]    [Pg.389]    [Pg.64]    [Pg.87]    [Pg.1174]    [Pg.298]    [Pg.420]    [Pg.10]    [Pg.10]    [Pg.185]    [Pg.201]   
See also in sourсe #XX -- [ Pg.188 ]




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