Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Reservoir direction

The Ubbelohde viscometer is shown in Figure 24c. It is particularly useful for measurements at several different concentrations, as flow times are not a function of volume, and therefore dilutions can be made in the viscometer. Modifications include the Caimon-Ubbelohde, semimicro, and dilution viscometers. The Ubbelohde viscometer is also called a suspended-level viscometer because the Hquid emerging from the lower end of the capillary flows down only the walls of the reservoir directly below it. Therefore, the lower Hquid level always coincides with the lower end of the capillary, and the volume initially added to the instmment need not be precisely measured. This also eliminates the temperature correction for glass expansion necessary for Cannon-Fen ske viscometers. [Pg.181]

Each solvent passes from its reservoir directly to a pump and from the pump to a mixing manifold. After mixing, the solvents pass to the sample valve and column. The pumps control the actual program and are usually driven by stepping motors. The volume delivery of each solvent is controlled by the speed of the respective pump. In turn, the speed of each motor is precisely determined by the frequency of its power supply which can be either generated by external oscillators or, if the chromatograph is computer controlled, directly from the computer itself. [Pg.126]

Commercial bakeries and doughnut shops normally use a system that extrudes a batter from a reservoir directly into the deep fat fryer (Figure 5). In such a system the rheology of the batter is vitally important. The batter must flow and spread as needed. The major influence on the batter viscosity is the water content, which is around 70% of the flour or around 40% of the dry mix. Various gums are sometimes added to the dry mix to bind water, reduce fat absorption, and control the viscosity. Examples of these gums are guar gum, locust bean gum and carboxymethyl cellulose. [Pg.230]

In living cells, proteins account for a major fraction of the cellular C and most of the N. We therefore expect that DON released from living organisms will contain proteins. In addition, the prominent amide resonance in the N-NMR spectrum of HMWDON could be derived from peptides and therefore, it is reasonable to hypothesize that proteins dominate the DON reservoir. Direct quantification of proteins in DOM has proven to be difficult (as seen later), so to test the above hypothesis many studies have focused on identifying and quantifying total hydro-lysable amino acids (THAA) in DOM. Amino acids are released from DOM following hydrolysis of peptides and proteins, and most marine DOM studies have used similar methods of hydrolysis and subsequent quantification (i.e., 6M HCl hydrolysis with variable temperature and hydrolysis times, followed by HPLC... [Pg.107]

Agent Index A292 Class Index C25 Chikungunya Type Virus Arthritis in wrist, knee, ankle and small joints of extremities. A rash may develop in 1 to 10 days. May present hemorrhagic symptoms. Recovery may be prolonged. Routes Vector (Mosquitoes) Secondary Hazards Vector Cycle Incubation 3 to 11 days Mortality Rate 0% Reservoir — Direct Person-to-Person Transmission does not occur. [Pg.204]

Figure 22.1 depicts the major reservoirs in the biogeochemical cycle of sulfur, with estimated quantities [in Tg(S)] in each reservoir. Directions of fluxes between the reservoirs are indicated by arrows. The major pathways of sulfur compounds in the atmosphere are depicted in Figure 22.2. The numbers on each arrow refer to the description of the process given in the caption to the figure (not to fluxes). Note the small amount of sulfur in the atmosphere relative to that in the other reservoirs. Also note the significant amount of sulfur in the marine atmosphere this is the result of dimethyl sulfide (DMS) emissions from the sea. Figure 22.1 depicts the major reservoirs in the biogeochemical cycle of sulfur, with estimated quantities [in Tg(S)] in each reservoir. Directions of fluxes between the reservoirs are indicated by arrows. The major pathways of sulfur compounds in the atmosphere are depicted in Figure 22.2. The numbers on each arrow refer to the description of the process given in the caption to the figure (not to fluxes). Note the small amount of sulfur in the atmosphere relative to that in the other reservoirs. Also note the significant amount of sulfur in the marine atmosphere this is the result of dimethyl sulfide (DMS) emissions from the sea.
The objective of any exploration venture is to find new volumes of hydrocarbons at a low cost and in a short period of time. Exploration budgets are in direct competition with acquisition opportunities. If a company spends more money finding oil than it would have had to spend buying the equivalent amount in the market place there is little Incentive to continue exploration. Conversely, a company which manages to find new reserves at low cost has a significant competitive edge since it can afford more exploration, find and develop reservoirs more profitably, and can target and develop smaller prospects. [Pg.15]

The basic data gathering methods are direct methods which allow visual inspection or at least direct measurement of properties, and indirect methods whereby we infer reservoir parameters from a number of measurements taken in a borehole. The main techniques available within these categories are summarised in the following table ... [Pg.125]

To gain an understanding of the composition of the reservoir rock, inter-reservoir seals and the reservoir pore system it is desirable to obtain an undisturbed and continuous reservoir core sample. Cores are also used to establish physical rock properties by direct measurements in a laboratory. They allow description of the depositional environment, sedimentary features and the diagenetic history of the sequence. [Pg.126]

Other logs employed to determine N/G ratio include the spontaneous potential (SP) log and the microlog, which differentiate permeable from non-permeable intervals. The N/ G ratio can also be measured directly on cores if there is visible contrast between the reservoir and non-reservoir sections, or from permeability measurements on core samples, providing sample coverage is sufficient. [Pg.145]

Reservoir porosity can be measured directly from core samples or indirectly using logs. However as core coverage is rarely complete, logging is the most common method employed, and the results are compared against measured core porosities where core material is available. [Pg.145]

Formation permeability around the wellbore can be measured directly on core samples from the reservoir or from well testing (see Section 8.4), or indirectly (estimated) from logs. [Pg.151]

Applying this directly to the reservoir, when a volume of fluid (dV) is removed from the system through production, the resulting drop in pressure (dP) will be determined by... [Pg.183]

The air may be collected directly into a Hempel gas-burette (Fig. 76) and there measured. This burette consists of a glass tube H calibrated in ml. from the tap E downwards, and connected by a piece of rubber tubing to the reservoir R, the height of which can be adjusted. The tap E is a 3-way tap. by which the tube H can be connected directly through to the capillary tube above, or either tube can be connected through the left- hand end of the tap to the atmosphere. [Pg.427]

Another development arising from FAB has been its transformation from a static to a dynamic technique, with a continuous flow of a solution traveling from a reservoir through a capillary to the probe tip. Samples are injected either directly or through a liquid chromatography (LC) column. The technique is known as dynamic or continuous flow FAB/LSIMS and provides a convenient direct LC/MS coupling for the on-line analysis of mixtures (Figure 40.2). [Pg.288]

Batch inlet. The historic term for a reservoir inlet. The term reservoir inlet is preferred because a direct-inlet probe is also a form of batch inlet. Batch gas inlet or batch vapor inlet are, however, completely descriptive terms. [Pg.432]

Continuous inlet. An inlet in which sample passes continuously into the mass spectrometer ion source, as distinguished from a reservoir inlet or a direct-inlet probe. [Pg.432]

Sources of water for aquaculture include municipal suppHes, wells, springs, streams, lakes, reservoirs, estuaries, and the ocean. The water may be used directly from the source or it may be treated in some fashion prior to use (see Water). [Pg.19]


See other pages where Reservoir direction is mentioned: [Pg.194]    [Pg.288]    [Pg.276]    [Pg.154]    [Pg.223]    [Pg.370]    [Pg.368]    [Pg.523]    [Pg.524]    [Pg.100]    [Pg.51]    [Pg.223]    [Pg.155]    [Pg.376]    [Pg.194]    [Pg.288]    [Pg.276]    [Pg.154]    [Pg.223]    [Pg.370]    [Pg.368]    [Pg.523]    [Pg.524]    [Pg.100]    [Pg.51]    [Pg.223]    [Pg.155]    [Pg.376]    [Pg.49]    [Pg.50]    [Pg.83]    [Pg.116]    [Pg.283]    [Pg.198]    [Pg.52]    [Pg.144]    [Pg.649]    [Pg.652]    [Pg.246]    [Pg.279]    [Pg.405]    [Pg.176]   
See also in sourсe #XX -- [ Pg.3 , Pg.134 , Pg.152 ]




SEARCH



© 2024 chempedia.info