Air bubble suspension - homogenized mud
Posted: Tue Aug 03, 2010 8:46 pm
This is a technical moot point that I've been wondering about recently.
I know from my own experience with silt deposit mudflats that the density tends to vary (and therefore, the 'sinkability') in spots that are in close proximity to each other. Why that should occur is a mystery to me, but is not especially relevant here. I distinctly recall my surpise upon returning to an area that I agitated and then semi-liquified a year before, by adding water, and contrary to my expectations the mud was remarkably solid - as if the churning process had released all the microscopic air bubbles that were orginally laid down with the deposits. This is an area of intertidal mudflats, incidentally.
It got me thinking that it might be possible to mechanically introduce tiny air bubbles into a gelationous mud mixture (clay, for example), as it was being pumped through a pipe under high pressure, just before entering the prepared pit. I would speculate that providing the air bubbles were sufficiently small, they would not escape to the surface without fairly vigorous agitation. I would imagine that such apparatus exists for some industrial purpose. And once the mud had dehydrated and thickened up a bit, it would be even harder for the air particles to escape. I don't know how many cubic inches per cubic yard (or PPM) would be required to make a substantial difference in density, but I understand the compressive nature of pneumatics.
The practical upshot of this would be (at least theoretically) to make it easier to sink into more viscous mud (thick and deep is a winning combination IMO) without first having to water it down.
I'm guessing this is why it is easier to sink into peat bogs, because they appear much less dense than clay.
I know from my own experience with silt deposit mudflats that the density tends to vary (and therefore, the 'sinkability') in spots that are in close proximity to each other. Why that should occur is a mystery to me, but is not especially relevant here. I distinctly recall my surpise upon returning to an area that I agitated and then semi-liquified a year before, by adding water, and contrary to my expectations the mud was remarkably solid - as if the churning process had released all the microscopic air bubbles that were orginally laid down with the deposits. This is an area of intertidal mudflats, incidentally.
It got me thinking that it might be possible to mechanically introduce tiny air bubbles into a gelationous mud mixture (clay, for example), as it was being pumped through a pipe under high pressure, just before entering the prepared pit. I would speculate that providing the air bubbles were sufficiently small, they would not escape to the surface without fairly vigorous agitation. I would imagine that such apparatus exists for some industrial purpose. And once the mud had dehydrated and thickened up a bit, it would be even harder for the air particles to escape. I don't know how many cubic inches per cubic yard (or PPM) would be required to make a substantial difference in density, but I understand the compressive nature of pneumatics.
The practical upshot of this would be (at least theoretically) to make it easier to sink into more viscous mud (thick and deep is a winning combination IMO) without first having to water it down.
I'm guessing this is why it is easier to sink into peat bogs, because they appear much less dense than clay.