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And then we have a Dead Eutrophocation. And so this is where that algae is getting over-nourished. Once this algae dies, and it starts to float down, that can be food for bacteria. We talked about that in the nitrogen and the phosphorous cycle videos.

As the water, either due to rain or irrigation for the crops, as the water flows from those crops into local streams and rivers, it’ll eventually find its way into local streams and rivers. The bacteria will consume all of the wutrophication in the water.

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Science Biology Ecology Biogeochemical cycles. And because of that, we humans have added a lot of nitrogen and especially phosphates to plants in order to grow them better, because we need the plants to live, to have more food. We’ve already talked about the role of oxygen in respiration. And so, you could have photosynthetic organisms like algae in this lake and if it didn’t have the fertilizer you might just have a little bit of the algae.

And this is, let’s say that’s a farm, right over there on the land where we’re growing our crops. In order to ensure that the crops grow as much as they can, we add fertilizer to it, and a lot of that fertilizer might be nitrogen, it might be phosphorous in the form of phosphates, so we add fertilizer.

It’s getting way more phosphates than would have typically happened just if there wasn’t fertilizer, if there wasn’t this runoff happening. But now all of a sudden, if this bacteria, because they’re able to decompose all this algae that is dying, if they’re consuming all of the oxygen, well it depletes the oxygen from the water so that the ocean animals can’t live there anymore. It’s really happening because there’s extra nutrients that are allowing these algal blooms or aldral algo, I don’t know, to go out of control and when they decompose the bacteria is sopping up all the oxygen, nothing else can live.


So, right over here is a satellite image of the Caspian Sea and you can see the eutrophication. It’s making the water less clear. Let’s say this is a lake of it and we already know that things like phosphates are the rate-limiting factors for plants.

Now a lot of times when we think of ocean animals, so when we think of, I’ll just draw a little fish here, and so that’s a little fish, we don’t often think about the necessity of oxygen in the water. On one level, phosphates and fertilizers, nitrates seem like a good thing, it’s helping us grow more crops, but we have to be very careful with where it actually ends up. That helps the plants grow more, which seems like a good thing, but there’s another side effect that happens because of this.

So this fish is going to die and other animals like it aren’t going to live because there’s not gonna be enough oxygen in that water. So these are all the crops that we’re growing. And the biggest culprit here tends to be phosphates, the phosphorous in them, and that helps the plants grow more. So this is a serious ecological thing that we have to think about. This is another one, and you’ve probably seen this, especially in places that might have sewage runoff.

You can see the algeal, algal blooms throughout this area. Let me show you some more. And so you might think that this is a good thing but as we’ll see over the course of this video, this is really about over-nourishment, and over-nourishment to the point that it’s actually eutrophicatiob very bad things to happen in our biosphere.

Eutrophication and dead zones. Eu referring to well and then trophic or trophia, referring to nourished, or nourishment. So right over here is kind of a global picture of dead zones eutrophicatin we have and you see them all through the world. And this is happening on a macro scale.

Intro to biogeochemical cycles.

Eutrophication and dead zones

It could just make the surface of the water a little bit less clear, a little bit green, but hey, eutropjication living things here. And if you were to zoom in, let’s say on the Caspian Sea, you can see this in more detail, you can visually see this. That could be food for bacteria, and as the bacteria consume it, they also use oxygen.


And so the irony here is, by having this fertilizer runoff, by having these extra phosphates, this eutrophication, by allowing one thing to eutrophicatoin far more than it would have otherwise, it actually ends up depleting the oxygen that keeps other things from growing.

pogil activities for ap biology eutrophication – NetFind – Content Results

And you might say okay, well why is this bad? But now since they’re getting all of these phosphates, the algae can go crazy. The algae can go crazy and grow all over the surface of the lake.

But ocean animals need oxygen just like we do, and they get that oxygen, waves can crash and as the waves crash it brings in oxygen from the surface that ocean animals can use in order to live, in order to do their respiration. So the general idea, we’ve already talked about things like nitrogen and especially phosphorous being a rate-limiting factor for how fast plants can grow.

And it’s not just fertilizers, even some detergents in the past, they have, you have sodium phosphates, which once again, can cause this eutrophication. And this is a serious problem. And it actually creates what we call dead zones.

Well the issue is what happens once this algae dies. Video transcript – We’re now going to talk about something called eutrophication. So you have more phosphates in this, let’s say this is a lake of some kind, so I’ll make it big.

So what has happened is, so let’s say that this right over here is some land.

Read sac/eutrophication-pogil

And you see they are typically concentrated where we have more industrialized nations, where we have either more agriculture happening, more industrial agriculture, where they might be using more fertilizer and also where you might have more runoff from cities that will have nutrients like the phosphates, that will cause this eutrophication to happen.

This is potential eutrophication in this picture. We have some pictures here. And it comes from, or it’s derived from, the Greek for well nourished.