Yeah, that's a good question. You know, there's a there's a couple of different entry points, I guess you could say. And depending on the angle that we take to start the conversation. Shock will end up going down any number of deep dives and rabbit holes, because humic substances are very complex, but there's also aspects about them that are simple. So maybe we should start by first establishing what are some of the simple ways to understand humic acids. And the idea basically is as follows, when plants are growing through their photosynthetic activity, really what they're trying to do is capture carbon out of the air. They're using the power of the sun. They have water as a fuel, and they've kind of figured out this really clever way to pull carbon out of the air. In its default state, the carbon is always going to be oxidized because we've got so much oxygen in the air that you and I are breathing. It's about 200 maybe 210,000 parts per million, compared to about only 420 ish ppms of CO two. So there's a lot more oxygen than there is carbon dioxide. And this creates an atmosphere or an environment because it's so rich in oxygen that things tend to exist in oxidized forms, that oxygen really likes to steal the electrons. And so plants have this problem or this challenge they have to overcome. It's how do I take this carbon that's oxidized in form of CO two out of the air, and how do I reduce it through photosynthesis? And how do I really capture and store it over long periods of time? And this is where humic acids kind of come into play, because as plants photosynthesize, and they produce things like root exudates. Those root exudates may actually contribute to building up organic matter in soils. And what this means is that they're pulling the carbon out of the air, and they're figuring out really clever ways to make those carbon bonds very stable and very persistent over long periods of time. They resist oxidative degradation, and they hang out in the soil with particular arrangement of bonds that is a source of trapped energy. It's potential energy versus kinetic energy. So over long periods of time, what ends up happening is, as the plants grow year over year, there's more and more organic matter that progressively gets sunk into the soil. And over a very long period of time, this combination of root exudates that are being produced the activities of microbes and fungi and also the remnants of all of them, plants, as they die, they'll drop the leaves those contribute to mix ups formation, certainly as microbial colonies turn over, there are carcasses And there's remnants of microbes that used to exist those can contribute towards building up cumic substances in soils over long periods of time. And same thing with fun fungal colonies as well. When the actual fungi, you know, my ceiling network is growing it, they too are capable of producing compounds, like polysaccharides, for example, that will kind of promote soil aggregation, and it will form clumps in the soil, which is a very desirable property to have if you have very crumbly soil. And it can, you know, hold on to water very well. It just kind of contributes to the overall physical properties and chemical properties of the soil. So, you know, to tie this back into humic substances. You know, simply put, it's just the result of what plants and microbes and fungi do in coordination with each other over very long periods of time. It builds up organic matter in the soil. It's very slow to break down, and so it kind of contributes to building up carbon. Now, you should also mention that there's physical properties that I'm kind of talking about with just the sequestration of carbon from the air and burying it into the soil. But there's also some kind of chemical properties that are associated with humic substances too. And you know, because by definition, humic substances don't have a specific molecular formula, their specific composition is going to vary greatly depending on a few factors, like we just talked about, the plants that are growing. Well, which plants, where are they growing? If they're growing in northern regions versus equatorial regions, there's different species of plants, and those plants produce different exudates, and those exudates have different molecular formulas and different rates of degradation, different chelation capacities, all of these wonderful things. When that stuff gets buried into the soil, it contributes to this weird property that there's no two humic substance fractions that are really going to be the same. There's some that are going to be similar enough. But certainly the further and further out you go and you kind of look at a global scale, all humic substances, by definition, are different because they're ultimately made up of plants. So there's a huge amount of variation that can occur on the specific chemistry of root exudates, soil chemistry, is it a clay soil? Is it, you know, subject to floods? Is it rich in organic matter? Are there microbial and fungal activities, and if so, to what extent all of these things will contribute to the formation of stable residues that accumulate over millions of years, and as the total pool of organic matter increases, so too does this chemical diversity. So