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Capturing CO2 from ambient air - David Keith

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the <strong>CO2</strong> capture rate in a spray system.<br />

The equations presented so far address mass transport of <strong>CO2</strong>. In principle, numerical methods may<br />

be used to estimate evaporative water loss in a contactor as well. As discussed in Section 3.2, it turns<br />

out that Equation 3.1 is not the correct model for <strong>CO2</strong>, which appears to instead follow Equation 3.3<br />

(<strong>CO2</strong>mass transfer is liquid-side limited). However, Equation 3.1 can be applied to the evaporation of<br />

water (Seinfeld and Pandis, 1998). If we define RH2O/<strong>CO2</strong> as the molar ratio of water evaporated to <strong>CO2</strong><br />

captured, then we can estimate it by the ratio of mass transfer equations:<br />

RH2O/<strong>CO2</strong> = kg(C∞,H2O −Cs,H2O)<br />

�<br />

Dlk[OH− ]<br />

C0<br />

The calculation is complicated because the vapor pressure of water at the drop surface, Cs,H2O, is a<br />

function of drop temperature, [OH − ], and [CO 2−<br />

3 ] (the concentration of <strong>CO2</strong> already absorbed in mol/L).<br />

For a sense of scale, we plug in initial conditions for temperature, relative humidity, and apply other<br />

reasonable parameters. Equation 3.7 then evaluates to the order of 10 3 , which is quite large (though it is<br />

clearly an overestimate because it does not account for changing temperature and other dynamic effects).<br />

It is large enough to suggest that the <strong>air</strong> leaving a full-scale contactor will be saturated with water vapor.<br />

Thus we can estimate evaporative water loss by assuming the <strong>air</strong> leaving the contactor has water partial<br />

pressure equal to the vapor pressure of water at the surface of the drops.<br />

For simplicity we assume that <strong>air</strong> and liquid reach the bottom of the contactor at the same temperature,<br />

so that an energy balance yields the temperature at the outlet:<br />

Tout = Tin − ΔCH2OΔHvap<br />

ρ<strong>air</strong>cp,<strong>air</strong> + ρlcl<br />

where mvap is the mass of water evaporated per units contactor volume, cp,<strong>air</strong> and cl are the heat capacities<br />

of <strong>air</strong> and the liquid solution (assumed equivalent to water), and ρ<strong>air</strong> and ρl are the bulk densities of <strong>air</strong><br />

and suspended solution. The quantity of water evaporated, ΔCH2O, is the difference between inlet water<br />

concentration and outlet vapor pressure of the solution:<br />

ΔCH2O = Cs,H2O(T = Tout) −CH2O,in<br />

Equations 3.8 and 3.9 can be solved simultaneously by iteration to yield ΔCH2O. Assuming an overall<br />

capture efficiency for the contactor of <strong>CO2</strong> <strong>from</strong> <strong>air</strong> allows a calculation of RH2O/<strong>CO2</strong> . The results of this<br />

calculation for reasonable conditions in the contactor are presented in the next section.<br />

3.1.2 Experimental methods<br />

We constructed a prototype contactor in order to demonstrate the feasibility of <strong>CO2</strong> capture by NaOH<br />

spray and to allow us to measure the energy requirements in a way such that the results could be scaled up<br />

to a full size contactor. Details of the design choices and experimental procedure are given in Appendix<br />

B along with additional photographs of the structure. We required (1) a tower diameter large enough to<br />

19<br />

(3.7)<br />

(3.8)<br />

(3.9)

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