Some time ago, I took my Key West up to Legg Lake. Prior to that, I had it running really well at Santee. It was loose and “flew” quite well. At Legg, it was just a dog. I was completely embarrassed by the way it ran. I had to skulk home with my head held down in shame.
What’s up with that? I know the guys that run IC engines have to worry about mixture control at different altitudes, whereas electrics don’t have that density altitude problem when producing power. So why did my KW run like crap at Legg?
Some discussion around this topic started on the RRR forum, and I thought I would bring that topic here as well.
The density (weight per volume) of a fluid is described by its specific gravity. Pure water has a specific gravity of 1.0000 at 60º F (by definition). The specific gravity of a fluid is determined by dividing the weight of a unit volume of that fluid by the weight of the same unit volume of pure water. Any change in temperature or composition of the water will change the specific gravity of that sample. Everybody knows that salt water has a lower specific gravity than does pure water. Could it be that the quality of water in different ponds results in markedly different performance results with the same setup? I have heard people say that at “X” pond, you need to prop down to keep temperatures in line, or that at “Y” pond the water was “faster”. Some ponds have a lot of suspended silt that may increase the density of the water (the specific gravity). Some may have soap or other chemical residue that may impact the way water “sticks to” or “slides off” of the boat’s planning surfaces (surface tension).
I found a website that sells highly accurate hydrometers (devices for measuring the specific gravity of a liquid). I may invest in a couple of these and see if there are significant variations in different ponds, and if these variations can be used to predict performance based on the specific gravity of the water in a particular pond.
For example: Your dialed-in setup runs an X642 prop with temperatures at 130º in your pond that has an S.G. of 1.0500. You travel to a neighboring pond that has an S.G. of 0.9500. Based on your research, you know that you can push a bigger prop in the less dense water, so you put on the X645. A quick test run confirms temperatures are “in the green arc”.
Voilá, you have a new tool for dialing-in your setups at different locations, just like your trusty thermometer.
What’s up with that? I know the guys that run IC engines have to worry about mixture control at different altitudes, whereas electrics don’t have that density altitude problem when producing power. So why did my KW run like crap at Legg?
Some discussion around this topic started on the RRR forum, and I thought I would bring that topic here as well.
The density (weight per volume) of a fluid is described by its specific gravity. Pure water has a specific gravity of 1.0000 at 60º F (by definition). The specific gravity of a fluid is determined by dividing the weight of a unit volume of that fluid by the weight of the same unit volume of pure water. Any change in temperature or composition of the water will change the specific gravity of that sample. Everybody knows that salt water has a lower specific gravity than does pure water. Could it be that the quality of water in different ponds results in markedly different performance results with the same setup? I have heard people say that at “X” pond, you need to prop down to keep temperatures in line, or that at “Y” pond the water was “faster”. Some ponds have a lot of suspended silt that may increase the density of the water (the specific gravity). Some may have soap or other chemical residue that may impact the way water “sticks to” or “slides off” of the boat’s planning surfaces (surface tension).
I found a website that sells highly accurate hydrometers (devices for measuring the specific gravity of a liquid). I may invest in a couple of these and see if there are significant variations in different ponds, and if these variations can be used to predict performance based on the specific gravity of the water in a particular pond.
For example: Your dialed-in setup runs an X642 prop with temperatures at 130º in your pond that has an S.G. of 1.0500. You travel to a neighboring pond that has an S.G. of 0.9500. Based on your research, you know that you can push a bigger prop in the less dense water, so you put on the X645. A quick test run confirms temperatures are “in the green arc”.
Voilá, you have a new tool for dialing-in your setups at different locations, just like your trusty thermometer.
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