Knight Inlet

In addition to raising waves on the water surface, winds will set the surface layers of water in motion in the direction of the wind stress or, if the water is sufficiently shallow, set up a circulation pattern extending to the bottom. Pickard and Rodgers (1959) have shown, for example, how an up-estuary wind can set the surface layer of water in the Knight Inlet (B.C.) in motion against the estuarine circulation. Elliott (1978) has demonstrated the importance of wind stress in determining the circulation in the Potomac estuary. To have much influence on estuarine sedimentary processes, however, the wind-driven circulation must penetrate to the bottom, which is likely to happen only in relatively shallow estuaries. In... 

Pickard, G. L., and Rodgers, K. (1959), Current measurements in Knight Inlet, British Columbia. J. Fish. Res. Board Can. 16, 635-678. 

Inlet, Santa Barbara Basin, and the Miocene Monterey Formation. Mar Geol 174 159-176 Jnrinak JJ, Dndley LM, Allen MF, Knight WG (1986) The role of calcium oxalate in the availability of phosphoras in soils of semiarid regions A thermodynamic study. Soil Sci 142 255-261 Kaz ov AV (1937) The phosphorite facies and the genesis of phosphorites. Soviet Geol 8 33-47 Kemp AES, Baldanf JG (1993) Vast Neogene laminated diatom mat deposits from the eastern equatorial Pacific Ocean. Natnre 362 141-144... 

Reactant flow strategies, such as coimter-flow design to transfer water from the wetter outlet region of the cathode into the drier fuel flow at the anode inlet (Knights et al, 2004). 

Time to significant gas cross-over (>10 cm /min at 2 bar pressure differential) as a function of inlet gas humidification for a non-optimized cell design. Air/hydrogen operation, current density = 540 mA/cm, coolant temperature = 75 °C, humidification levels of reactant streams as indicated. (Source Knights etal., 2004, reprinted with permission from Elsevier.)... 

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