 This is our tabletop rainfall simulator. It really is kind of a nice simulation because it's actually taking a 3 1⁄2 inch sample right out of the field and gives us a really good handle on soil structure and infiltration. So we like to use this. And in fact, why don't we go through and actually do this demonstration. This is a Enet loam. This is a long-term no-till with, of course, it's got a rye cover crop on it. And then this soil structure over here has been destroyed with tillage, long-term tillage, conventionally tilled, corn-sulivian rotation. Structure is just so much different. And of course, this little test actually shows us that difference is in infiltration and runoff. So just to be clear, both of these are Enet loams. Enet loams, yeah. But same soil series, different management. Exactly, yep. All right, well, let's do this. All right, we're going to put this infiltration tray up on the top, get that leveled out. And then it's just a matter of adding water. So we'll go ahead and do that. Wow. So what's happening now? Oh, my goodness. Well, I think you can see there's a substantial difference. And in fact, it appears that all the water and that runoff in the conventionally tillage is basically runoff. And you can see the differences in the color. That is the amount of sediments that's actually removed. And it's hard to see, but you can see there's a large amount of infiltrated water here. And there's really no infiltrated water over here. And that's really what we see. And when we start talking about soil structure, what makes it so important. I didn't actually expect that everything would runoff. There's literally one drop in here. That's amazing. And that came up from around the side of Beth.