right? Yeah, they're different. But let's say, if we just want to have the large molecules from coal, that's a much easier job to do, because majority of them is very large molecules of what we call that polyphenolic structure. It's the skeleton, huge skeleton, of those carbonaceous compounds mixed together. Nobody can even draw a molecular formula for it. It's so complicated, but that's they're very stable. That's why they're still there. And I would bet, if you just take coal and grind it and apply that to soil, it's going to still, still going to be there for, you know, 1000s of years, right, right? But from that perspective, you can use lignite, you can use anthracycle, any coal, it would have that fraction. But what's different is that's the only fraction you have. What we try to do in Guyana is, and the reason we use lignite and sub bituminous coal, these are the two, only two species we're using is because of the other good stuff trapped in the coal. In this kind of coal that we use a, you know, it's basically a train of process of electrochemical digestion, plus a biological digestion, and we use these two processes to weaken the bonds of our feed stock. We're breaking apart, breaking it apart partially, and then so we can release these compounds out. So the end product of guy in eight is basically some very large humic substances, which is very similar to biochar. I can't even say it's the same as biochar for that fraction. But then, in addition to that, we have a large pool of intermediate compounds, almost like compost, but it's not made from compost, because it's just partially digested from coal. So we're making that that middle range molecules that can stay in soil and serve as food to microbes and some to plants. For a long time, it's like a slow releasing source. And in addition to that, some of the fractions are very small organic compounds, we have actually detected eight different organic acids in Guyana. And these compounds are highly water soluble. It's, they're just like fulbric acid, you know. And and more than that, we have, we even found acetic acid in there. And then they can feed microbes immediately. Some of them get into the plant metabolism, you know, so they can actually enhance plants growth directly, but most of them would enhance the soil microbes. And in addition to that, because of the mineralization or codification process of coal, some soil microbes got into that cosine and you also have mineral compounds formed within that, lignite and submiss coal. So we have lot of a trace amount of mineral elements. Is a very important stuff, actually. Now more and more studies are on the food quality and food nutrient intensity, and data are showing that actually these two parameters are closely related to the trace elements in soil and in that's a different topic, but I just want to mention that quickly, because you probably noticed that nowadays. Is even, you know, comparing to, you know, just a few decades ago, where we were kids, we didn't have that many different kinds of allergies, but now we have so many different kinds of allergies. People are allergic to weird stuff. But do you have, you know, all sorts of allergies that's that's an indication of the degradation of immune system? Yeah, absolutely. And which is related to our microbiome in our guts, right? And it all starts in the soil. You can track it all the way to soil, yeah, soil, to food, to ourselves. Now