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Liquid water test

Because of this extreme sensitivity, attention shifted to an acidic system, the phosphoric acid fuel cell (PAFC), for other applications. Although it is tolerant to CO, the need for liquid water to be present to facilitate proton migration adds complexity to the system. It is now a relatively mature technology, having been developed extensively for stationary power usage, and 200 kW units (designed for co-generation) are currently for sale and have demonstrated 40,000 hours of operation. An 11 MW model has also been tested. [Pg.528]

Figure 32.26 demonstrates a well-known method of correcting for fluid change from water for a centrifugal pump. This allows an engineer to predict change in performance if the kinematic viscosity of the liquid to be pumped is known and the water test data are available. [Pg.496]

Self-Tfst 6.11B When 0.338 g of pentane, C5H12, burns in an excess of oxygen to form carbon dioxide and liquid water in the same calorimeter as that used in Self-Test 6.1 1A, the temperature rises by 76.7°C. Write the thermochemical equation for the reaction. [Pg.362]

Seee-Test 7.17A Confirm that liquid water and water vapor are in equilibrium when the temperature is K)0.°C and the pressure is 1 atm. Data are available in Tables 6.3 and 7.2. [Pg.412]

When water is used as the immersion liquid, the test is essentially the ASTM Standard Test Method (D570) for Water Absorption of Plastics.( ) Determinations of the relative rate of water absorption are important in evaluating the effects of moisture exposure on such properties as mechanical strength, electrical resistivity, dielectric... [Pg.30]

Adiabatic compression test High pressure is applied rapidly to a liquid in a U-shaped metal tube. Bubbles of hot compressed gas are driven into the liquid and may cause explosive decomposition of the liquid. This test is intended to simulate water hammer and sloshing effects in transportation, such as humping of railway tank cars. It is very severe and gives worst-case results. [Pg.30]

When the hydrolysis is complete carefully wash out the condenser with 10-12 c.c. of water. Then distil up to 5 c.c. of liquid into a small conical quartz flask. Use the condenser in the downward position and if necessary add a few boiling capillaries to the liquid in the flask. Repeat the distillation three more times, each time adding 7 c.c. of water. Test the distillate (volume about 20 c.c.) with some barium chloride for sulphuric acid (none should be present), boil for seven to eight seconds and titrate at once with 0-033 N sodium hydroxide solution 1 from a micro-burette having 0-02 c.c. scale-divisions. Use phenolphthalein as indicator and continue the titration until the colour becomes just pink and remains so for a few seconds. For the second titration distil 2 x 7 or 3 x 7 c.c. and for the third and fourth titrations only about 7 c.c. on each occasion. [Pg.83]

After testing a number of DLs with and without MPLs, Lin and Nguyen [108] postulated that the MPL seemed to push more liquid water back to the anode through the membrane. Basically, the small hydrophobic pores in the MPL result in low liquid water permeability and reduce the water transport from the CL toward the DL. Therefore, more liquid water accumulated in the CL is forced toward the anode (back diffusion). This reduces the amount of water removed through the cathode DL, decreases the number of blocked pores within the cathode diffusion layer, and improves the overall gas transport from the DL toward the active zones. [Pg.238]

Peled ef al. [177] also designed a novel MEA in order to improve the water back diffusion from fhe cathode to the anode side. They used a liquid-water barrier layer (LWBL), which consisted of a paste, made out of PTFE and carbon black particles, fhat was inserted in the pores of fhe CFP to form a layer inside fhe paper. Up to seven layers were necessary in order to achieve a uniform layer of 20-50 pm in thickness. Testing showed that the LWBL on the cathode DL creates a hydraulic pressure that forces (or pushes) the water back from fhe cafhode toward the anode, thus improving the cell s water management at different operating conditions. [Pg.248]

Schmitz et al. [184] tested various carbon fiber papers with different thicknesses as cathode DLs in PEM fuel cells. It was observed that the cell resistance dropped when the thickness of the DL increased thus, thicker materials are desired in order to improve the electrical conductivity. It was also mentioned that the optimal thickness for the DL is usually between the thinnest and the thickest materials because the two extremes give the lowest performance. In fact, in thin DLs, the water produced can fill pores within the material, resulting in flooding and the blockage of available flow paths for the oxygen. Similarly, Lin and Nguyen [108] concluded that thinner DLs (without MPLs) were more prone to liquid water accumulation than thicker ones. [Pg.249]

Nguyen et al. [205] designed a volume displacement technique that was used to measure the capillary pressures for both hydrophobic and hydrophilic materials. One requirement for this method is that the sample material must have enough pore volume to be able to measure the respective displaced volume. Basically, while the sample is filled wifh water and then drained, the volume of water displaced is recorded. In order for the water to be drained from fhe material, it is vital to keep the liquid pressure higher than the gas pressure (i.e., pressure difference is key). Once the sample is saturated, the liquid pressure can be reduced slightly in order for the water to drain. From these tests, plots of capillary pressure versus water saturation corresponding to both imbibitions and drainages can be determined. A similar method was presented by Koido, Furusawa, and Moriyama [206], except they studied only the liquid water imbibition with different diffusion layers. [Pg.259]

Koido, Furusawa, and Moriyama [206] used a technique based on the steady-state test method for reservoir rock, sandstone, and other porous media. In this method, a DL is sandwiched between similar DLs on the inlet and outlet sides. The material on the inlet is used to guarantee homogeneous distribution of liquid water in the planar direction, while the material at the outlet minimizes the flow in the outlet. Liquid water is introduced first and then a constant flow rate of air is injected. Once it is at steady state, the pressure difference between the inlet and outlet is measured. The sample is then weighed and the permeability is calculated in a way similar to that of Nguyen and colleagues [205]. [Pg.266]

Park and Li [267] also performed an experimental and numerical study in which a serpentine FF with and without diffusion layers was analyzed (see Figure 4.30). For the case in which a DL was not used, an impermeable plate was placed between the anode and cathode plates in order to perform the pressure drop tests. It was observed that the pressure difference between the two cases was as large as 80% of the pressure drop in the case without the DL. It was also explained that the reason for the large pressure difference between both cases was due to the cross-flow phenomena between adjacent channels through the porous diffusion layer. These researchers also performed the pressure drop tests when the fuel cell was running it was observed that the pressure drops were higher in this case than when the cell was inactive. It was believed that this pressure difference was a result of liquid water blocking reactant flow in either the channels or the DLs. [Pg.283]

When a generator is driven by an HPRT on a gas-rich process stream, the generator should be generously sized. The output power of HPRTs can be as much as 20 to 30 percent or more over that predicted by water tests, as a result of the effects of evolved gas or flashed liquid. [Pg.115]

The results of both liquid water and water vapor tests show that acetylation of lignocellulosic materials greatly improves dimensional stability of composites made from these materials. [Pg.248]

NASA has designed and contracted a water testing, purification, and retest (certification) system that is a self-contained unit about the size of a small automobile. Human involvement is restricted to putting hose A into a puddle, polluted stream, saltwater bay, or almost any other liquid source, and to drinking pure water from liose B. The fully automated laboratory (and processing) system is intended for an eventual Mars base. It is currently used on navy ships and some desert warfare army units. [Pg.226]

Materials red cabbage, pot, strainer, household liquids to test (ammonia, vinegar, tap water, lemon juice, etc.)... [Pg.316]

Fig. 5. Variation of the Sl80 and 8D values of the fluid delivered from well 131, located 500 m away from the re-injection site, during an injection test conducted in the peripheral area of Serrazzano in the Larderello field (open squares). The figure also shows graphically, and in arbitrary units, the flow rate Q of water re-injected into the well as a function of time, and the position of each sample collected. Theoretical isotopic pattern of the steam produced by re-injected water, assuming continuous steam separation at depth, is also reported. Since the actual evaporation temperature and the fraction of residual water are unknown, calculations were made for three different temperatures (140, 160, and 180 °C) and fractions (/w) of residual liquid water after boiling. Dashed line represents the hypothetical mixing between deep geothermal steam (W) and completely evaporated re-injected water (R). Fig. 5. Variation of the Sl80 and 8D values of the fluid delivered from well 131, located 500 m away from the re-injection site, during an injection test conducted in the peripheral area of Serrazzano in the Larderello field (open squares). The figure also shows graphically, and in arbitrary units, the flow rate Q of water re-injected into the well as a function of time, and the position of each sample collected. Theoretical isotopic pattern of the steam produced by re-injected water, assuming continuous steam separation at depth, is also reported. Since the actual evaporation temperature and the fraction of residual water are unknown, calculations were made for three different temperatures (140, 160, and 180 °C) and fractions (/w) of residual liquid water after boiling. Dashed line represents the hypothetical mixing between deep geothermal steam (W) and completely evaporated re-injected water (R).

See other pages where Liquid water test is mentioned: [Pg.344]    [Pg.344]    [Pg.275]    [Pg.238]    [Pg.2308]    [Pg.2313]    [Pg.146]    [Pg.80]    [Pg.251]    [Pg.251]    [Pg.272]    [Pg.194]    [Pg.200]    [Pg.203]    [Pg.204]    [Pg.222]    [Pg.84]    [Pg.273]    [Pg.100]    [Pg.119]    [Pg.431]    [Pg.195]    [Pg.197]    [Pg.137]    [Pg.108]    [Pg.169]    [Pg.256]    [Pg.511]    [Pg.275]    [Pg.24]    [Pg.218]   


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