Cation Exchange

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Excellent video! Thanks for sharing

👍︎︎ 3 👤︎︎ u/Basicallysteve 📅︎︎ Feb 26 2018 🗫︎ replies

I will walk into traffic to never take another soil science class agian.

👍︎︎ 3 👤︎︎ u/SouthernSerf 📅︎︎ Feb 26 2018 🗫︎ replies

I had to watch it twice.

👍︎︎ 1 👤︎︎ u/Iskandar11 📅︎︎ Feb 26 2018 🗫︎ replies

I'm a bot, bleep, bloop. Someone has linked to this thread from another place on reddit:

 If you follow any of the above links, please respect the rules of reddit and don't vote in the other threads. (Info / Contact)

👍︎︎ 1 👤︎︎ u/TotesMessenger 📅︎︎ Feb 26 2018 🗫︎ replies
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-[narrator] Not all soils are created equal. And if it weren't for chemistry we wouldn't be able to grow many crops here, nor here, nor here. It's like this, soils are composed of sand, silt, clay, and organic matter. Some have more sand, others more clay. Each soils unique blend determines its color, texture, and storage capacity for nutritious chemicals. Although incredibly small, nutrients still need their space and by space we mean the area surrounding the soils tiny particles. Keep in mind that surface area is not the same as particle size. For example, clay particles are tiny compared to sand, but they have more than 1,000 times as much external surface area as the particles in an equal volume of sand. However, if a nutrient just sits there unattached it will likely leach out from the soils and grains, and will not be available for plants. Remember that time when you rub the balloon on your best friend's hair and stuck it to a wall? Well a similar phenomenon occurs in the soil. Through their electrostatic energy, nutrients cling on to clay particle surfaces. Nutrients like calcium, magnesium, potassium, and ammonium are all positively charged chemicals or cations. And as it turns out, most clay particles and organic matter in soil are negatively charged. So, many nutrients are positive and particles are negative. Perfect! In chemistry, as in romance, opposites attract. Good! No more leaching! But like the balloon on the wall, the nutrients are only temporarily held. In fact, there's actually a shell of water molecules that forms around the cation. Preventing it from bonding permanently. This shell is often called a hydration sphere, but that's a whole other video. So, back to cations. Basically if a plant wants a nutritious cation like potassium, it will need to exchange it for another cation or cations of equal charge. Luckily, plants produce hydrogen cations that they can exchange. One hydrogen cation for one potassium cation, easy enough. But for nutrients with a positive charge of two like calcium, two hydrogen cations are needed. The higher the positive charge, the harder it gets to exchange or trade cations. That's because a cation with high positive charge and small size is preferentially held by the soil over those with lower charge or larger size. Meaning that a large cation with a positive charge of one will be the first to be released. A divalent cation having a charge of two will be released more easily than a cation with a positive charge of three. Whether they are held tightly or not, the nutrients are available to the plant in exchange for other cations. Not all nutrients are cations, however. Some are actually negatively charged compounds or anions. Since anions like nitrate are sulfate have a negative charge they are unable to attach themselves to negatively charged particles, and as a result leech out when watered. Of course, all soils are different. There are soils in the tropics, for example, that have positively charged soil particles. And in that case, it's the anions not cations that are held temporarily and then exchanged with other anions. Most soils, however, have negatively charged particles. The more negatively charged the soil is and the more surface area a soil has, the more cation exchange capacity it has. This is such an important factor for plant growth that scientists measure a soils cation exchange capacity, CEC, in order to help farmers determine how much and how often fertilization is needed. That's because CEC is sort of like a cup size at a fast food joint. Some soils are super sized, but others have a kiddy cup. Pouring too much will just cause a mess, but if you refill several times and still quench your thirst. Farming and low CEC soils works almost the same way. Even though the soil has lower capacity, you can fertilize more often using smaller amounts and the plants will grow healthy and strong. And it's a good thing too! Otherwise, we'd have very little land to farm. So the fact that farmers can grow crops almost anywhere kind of seems like superhero powers. But really it's just knowing about chemistry. [music playing]
Info
Channel: LearningGamesLab
Views: 257,055
Rating: 4.9402022 out of 5
Keywords: nutrients, soils, cation exchange capacity, CEC, fertilizer, fertilization timing, particle size, sand, clay, silt, cations, anions, Low CEC, High CEC, potassium, magnesium, calcium, ammonium, iron, hydrogen, electrostatic energy, agriculture
Id: HmEyymGXOfI
Channel Id: undefined
Length: 5min 49sec (349 seconds)
Published: Tue Sep 13 2016
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