5 ms·
One of the holy grails of solar is syngas: using solar thermal power to convert CO2/water to a mix of hydrogen and methane. If you can do it efficiently enough,
by ndonnellan 9y ago
One of the holy grails of solar is syngas: using solar thermal power to convert CO2/water to a mix of hydrogen and methane. If you can do it efficiently enough, the gas is the energy storage and you can either pipe it or use it to fuel a NG turbine/combined-cycle plant which will be more thermodynamically efficient than a simpler solar->steam cycle plant.
The reason it's a holy grail is because there are some major materials science breakthroughs that need to happen before it's feasible. Since the sun's energy cycles rapidly on the minute/second timescale, whatever receiver you're using to convert inputs to syngas needs to not be destroyed by that periodic, rapid temperature (and thus stress) cycling.
- petre 9y agoSyngas can be easily converted to DME (dimethyl ether), which is a cleaner diesel replacement. It's stored just like LNG, in pressurized containers at 0.5 MPa - typical roadbike tyre pressure.
- neltnerb 9y ago> The reason it's a holy grail is because there are some major materials > science breakthroughs that need to happen before it's feasible. Since > the sun's energy cycles rapidly on the minute/second timescale, whatever > receiver you're using to convert inputs to syngas needs to not be > destroyed by that periodic, rapid temperature (and thus stress) cycling. What do you mean here? What aspect of the sun's energy cycles on the minute/second timescale? And why would variability at that time scale do anything to a solar thermal system? I'm pretty sure the reason it is hard is because you need to go above and below phase transitions that change the oxidation state, achieve high rates of oxygen absorption and release, and maintain a high enough surface area to not lose your oxygen diffusion rate. Or are you talking about some new issue?
- ndonnellan 9y agoHaha, yes. The sun doesn't cycle. But sun reaching your receivers does because of clouds :-). Last time I worked in solar, the processes needed for the conversion typically worked above 600C (or much higher). If you can do conversion at atmospheric pressure, then you don't need pressure vessels (which are susceptible to fatigue because of cycling from 100C to 600C+ when a 5 minute cloud passes overhead, for example), but then your gas is at a lower density and now your process is less efficient. Also, the higher the temperature, the higher the radiative heat losses become. T1^4 - T2^4 = much much higher. So you want to minimize the view factor of the heat transfer tubes/materials. Which means you want a cavity receiver...yada yada. Google solar air receiver and you'll get some interesting reading material, for example: http://www.sciencedirect.com/science/article/pii/S1876610214005074 http://www.sciencedirect.com/science/article/pii/S1876610214... I'm a lot more familiar with salt systems, tbh: http://www.esolar.com/wp-content/uploads/2013/10/SolarPACES-2013.pdf http://www.esolar.com/wp-content/uploads/2013/10/SolarPACES-...
- neltnerb 9y agoOh, I see. Cyclic thermal stresses from clouds then? Yeah, the stuff I'm familiar with is solar thermal water splitting using iron oxide at ~1000C, though I can see why the Caltech group preferred ceria (my favorite ceramic). I think my favorite cute trick with solar thermal is solar thermal reforming of biomass. By piggybacking on the existing chemical reaction you actually end up with solar energy directly added to the chemical energy! First time I saw that I was struck by how clever it was. I imagine using CO2 as a reactant is a lot more difficult, that's not a simple molecule to break apart so I very much appreciated that the solar thermal reforming process takes advantage of the plants to do the hard part while extracting even more solar energy.
- Symmetry 9y agoAdding enough storage capacity to the electrical grid to handle the day/night fluctuations in solar is currently in feasibly expensive. Adding enough storage for minute by minute fluctuations is pretty easy, though.