LouNathanson
Petroleum
- Oct 11, 2010
- 1
In the discussion of glycol gas dehydration systems in the GPSA Databook, there is a graph of equilibrium dew point versus TEG concentration (fig 20-54 in the current version). The numbers here are generally in agreement with what I come up with in a Hysys simulation using very many theoretical stages. (Using Peng-Robinson, Hysys dew points are perhaps 15 F higher, presumably due to hydrate versus metat-stable dew point calculationis.) So far, so good.
However, the GPSA suggests that approaches to equilibrium of 10-20 F are the norm in the field. However, most contactors that I've seen have about 12 trays. Tray efficiency in this service is generally 25-30% -- per GPSA, per equipment vendors, and per what I've generally found by backcalculating from field data.
Given that tray efficiency, Hysys generally tells me that my gas dewpoint is about 50 F higher than obtainable with infinite stages. This is also what I generally find in the field.
I do find that my dew points measured in the field (using a FRESHLY CLEANED panametrics portable analyzer) agree with the water content that I calculate from a material balance using my sampled rich TEG concentration and circulation rate.
So my questions:
Does anyone know where GPSA comes up with the assertion that approaches to equilibrium of 10-20 F are typical?
What approaches to equilibrium are other folks finding in the field?
Thanks,
-Lou
However, the GPSA suggests that approaches to equilibrium of 10-20 F are the norm in the field. However, most contactors that I've seen have about 12 trays. Tray efficiency in this service is generally 25-30% -- per GPSA, per equipment vendors, and per what I've generally found by backcalculating from field data.
Given that tray efficiency, Hysys generally tells me that my gas dewpoint is about 50 F higher than obtainable with infinite stages. This is also what I generally find in the field.
I do find that my dew points measured in the field (using a FRESHLY CLEANED panametrics portable analyzer) agree with the water content that I calculate from a material balance using my sampled rich TEG concentration and circulation rate.
So my questions:
Does anyone know where GPSA comes up with the assertion that approaches to equilibrium of 10-20 F are typical?
What approaches to equilibrium are other folks finding in the field?
Thanks,
-Lou