babyblues71
New member
Okay, I have an advanced question.  Calcite and Dolomite are two of the most abundant carbonate materials that are found and are slowly but surely broken down via rivers in the hydrologic cycle right before this mineral-rich water makes its way into the ocean.  Now then, since calcite is more abundant than dolomite, and easier to break down, why is it that there’s a greater reading of magnesium in the ocean, which is more apparent within dolomite?  Am I missing another source, or when the magnesium “is†managed to be broken down from the dolomite is it in a greater quantity ppm-wise for some reason, or are the readings from the ocean like that because not as much magnesium is “needed†in the ocean when compared to calcium, and that’s why calcium tests out at 411 ppm and magnesium 1290?  I've always been curious about that.....  
 
http://www.seafriends.org.nz/oceano/seawater.htm
 
Brent
				
			http://www.seafriends.org.nz/oceano/seawater.htm
Brent
 
	 
 
		 Other significant sources are volcanic activity such as the deep sea rifts
 Other significant sources are volcanic activity such as the deep sea rifts 
 
 
		 
 
		 
 
		