I'm curious about the process of "cooking" (NOT curing) rock. I'm no biologist, but as a former long-time techie slave to corporate America, I absolutely LOVE the concepts of hard resets and clean installs. As I said, I'm certainly not a biologist, so please feel free to edumacate me if I'm missing the point here.
As I understand it, the process of "cooking" dry rock is based on the principle of bacterial solubilization of inorganic phosphate. This means that the bound phosphate ions from insoluble calcium phosphate and other minerals that are created by other sequestration methods throughout the existence of the "rock" as a living organism's skeleton or later as a host to other organisms are freed. Is this about the gist of it? In this process, are the bacteria consuming the calcium and leaving phosphates as free waste?
If I understand this right, the reason for starting the process with acid/vinegar soaks is to remove as much organic material from the rock as possible. Is this done to expose the actual rock surface area as much as possible to these bacteria, or to control the growth of other bacteria that would simply continue the process of sequestering phosphate back into the rock?
My final queries are about the bacteria themselves. Are these types of bacteria commonly found outside of marine environments? It seems to me that there would be similar bacteria almost everywhere life is found, considering so many creatures are full of calcium phosphate minerals. The reason I'd like to know more is because I'm curious about wether or not saltwater is actually necessary to the cooking process. I wonder about this bacteria and wether it can survive a cooking process using ro/di water instead of saltwater. Since the rock has been dry for a long time, and successively soaked in vats of acid, is it safe to assume that these mystical phosphate munching bacteria are being introduced from outside the marine environment? If so, shouldn't it be possible to achieve the same effect in freshwater?
Anyhoo, thanks for reading my ramblings, and hopefully for shedding some more light on an interesting topic.
As I understand it, the process of "cooking" dry rock is based on the principle of bacterial solubilization of inorganic phosphate. This means that the bound phosphate ions from insoluble calcium phosphate and other minerals that are created by other sequestration methods throughout the existence of the "rock" as a living organism's skeleton or later as a host to other organisms are freed. Is this about the gist of it? In this process, are the bacteria consuming the calcium and leaving phosphates as free waste?
If I understand this right, the reason for starting the process with acid/vinegar soaks is to remove as much organic material from the rock as possible. Is this done to expose the actual rock surface area as much as possible to these bacteria, or to control the growth of other bacteria that would simply continue the process of sequestering phosphate back into the rock?
My final queries are about the bacteria themselves. Are these types of bacteria commonly found outside of marine environments? It seems to me that there would be similar bacteria almost everywhere life is found, considering so many creatures are full of calcium phosphate minerals. The reason I'd like to know more is because I'm curious about wether or not saltwater is actually necessary to the cooking process. I wonder about this bacteria and wether it can survive a cooking process using ro/di water instead of saltwater. Since the rock has been dry for a long time, and successively soaked in vats of acid, is it safe to assume that these mystical phosphate munching bacteria are being introduced from outside the marine environment? If so, shouldn't it be possible to achieve the same effect in freshwater?
Anyhoo, thanks for reading my ramblings, and hopefully for shedding some more light on an interesting topic.
Last edited: