Summary of Gallstone
Transcript for Gallstone
When you eat some real fatty foods, like say some delicious french fries, they make their way to through the stomach and into the small intestine. At this point they aren’t really french fries anymore, but since they’re high in fat, they’re still a little more difficult to absorb, and that’s where your gallbladder comes in.
This high fat food stimulates the gallbladder to squeeze out some bile into the small intestine, that bile emulsifies the fat, or basically mixes the fat up, and makes it easier to absorb.
This is pretty much your gallbladder’s job—store and concentrate bile until the time comes to send it to the small intestine. It’s not the most glamorous of jobs, but hey, gotta start somewhere.
If we take a closer look at this magical substance, we’d get a rough breakdown that’s something like the following: ~70% bile salts and acids, ~10% cholesterol ~5% phospholipids, ~5% proteins, and 1% conjugated bilirubin, and the rest, small amounts of various other compounds like water, electrolytes, and bicarbonate.
Bile salts and acids are mostly a product of cholesterol metabolism, so an acid might look something like this and its salt is the anionic form, something like this (ROO-) group.
These acids and their salts have both hydrophobic and hydrophilic sides, making them amphiphilic, which help them make cholesterol and fat in the gut more soluble in bile.
The phospholipids are mostly lecithin, also amphiphilic, and also help make cholesterol and fats more soluble in bile.
Gall-stones are these round and solid stones you can find inside your gallbladder, and they’re made from the components of bile, and so they’re categorized depending on what they’re made of, the most common ones are cholesterol stones, but there’s also bilirubin stones, which are sometimes called pigmented stones.
The first type, as you might guess, are made mostly of cholesterol that has precipitated out of the bile as a solid and formed these solid stones. These account for around 75 to 90% of cases.
This cholesterol precipitation can happen in a couple ways, first, the bile can become supersaturated with cholesterol, meaning that the bile has so much cholesterol that the bile salts and acids or phospholipids can’t hold any more in solution, because remember that these all help make the cholesterol more soluble in bile, and so the cholesterol comes out of solution as a solid.
Another, somewhat similar way, is if you don’t have enough of these bile salts or acids and phospholipids to help keep the cholesterol in solution, so the less you have, the less cholesterol can be in solution and the more precipitates out.
Gallbladder stasis, or inactivity, has also been linked to forming stones, if the bile just sits there it can cause the solid to separate and precipitate out, kind of like when the oil in your peanut butter jar separates from the peanuts if it just sits too long.
Stones that’re made of cholesterol can’t be seen on x-ray, but rarely are the stones only cholesterol, and usually you’ll see a bit of a mixed composition; if they have enough calcium carbonate they might be able to be seen on x-ray.
Remember that we said there’s a small amount of electrolytes and bicarbonate? Well some of those electrolytes are calcium ions, and calcium ions tend to form insoluble precipitates with bicarbonate as calcium carbonate, which would be radio-opaque, and visible on x-ray, but usually there’s not enough calcium carbonate and the cholesterol stones will be radiolucent on x-ray and you won’t be able to see them.
Alright, so the other type is bilirubin or pigmented gallstones.
These ones, again, are pretty self-explanatory and are made mostly of bilirubin and therefore are pigmented.
These are made when there’s too much bilirubin in the bile and it has combined with calcium to form the solid precipitate calcium bilirubinate.