<a href=showthread.php?s=&postid=7828092#post7828092 target=_blank>Originally posted</a> by King-Kong
I forget who, but they reported an initial drop in Ca/Alk demand of 80% upon switching from their sandbed. This later levelled out to around 50% once the corals picked up the pace.
<a href=showthread.php?s=&postid=7830349#post7830349 target=_blank>Originally posted</a> by crypticghost
Ok, some explain to me why this is...does the sand trap CA...cause sand does not grow...but I have heard that if you have CA levels to high sand can become hard...so does the sand trap it or something?
<a href=showthread.php?s=&postid=7830349#post7830349 target=_blank>Originally posted</a> by crypticghost
Ok, some explain to me why this is...does the sand trap CA...cause sand does not grow...but I have heard that if you have CA levels to high sand can become hard...so does the sand trap it or something?
<a href=showthread.php?s=&postid=7835888#post7835888 target=_blank>Originally posted</a> by LFS_worker
Dr. Ronald shimek Refers to this kind of massive precipitation as very rare ... the binding of an oolitic sand is usually caused by a natural bacteria bloom but they are non calcifying bacteria .. they make a sugar like substance that binds the sand together.
for the record this type of clumping of sand is not healthy for a DSB. and is usually the reason for polution spikes in tanks.
refer to "sand bed secrets" by ronald shimek for more totally awesome info
Brian
<a href=showthread.php?s=&postid=7823270#post7823270 target=_blank>Originally posted</a> by deansreef
Just wondering if a reactor is still needed?
Deean