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[email protected] wrote:
>John Albergo <
[email protected]> writes:
>
>
>
>>>Unfortunately the last drawing in this URL, the drop should have a line across the bottom,
>>>showing that it is the cross section of a nearly a complete "soap bubble". Soap bubble leave a
>>>wet ring on the surface where they land. If that surface is moving relative to the bubble, the
>>>ring will be elliptical.
>>>
>>>
>
>
>
>>>The unanswered question that I have is, why they all have nearly the same aspect ratio of major
>>>to minor axis, regardless of size. They range from 20 to 200mm in length. It means that they all
>>>have the same velocity to the road when they burst, but why?
>>>
>>>
>
>
>>Assuming that most oils have the same surface tension, then I'd guess that most oil drips would be
>>about the same size, and "pop" at about the same airspeed (relative wind). Perhaps the size of the
>>resulting road ring is due to the "altitude" of the burst?
>>
>>
>
>After thinking about it some more and looking at oil drops on Sierra mountain passes this weekend,
>I am convinced by the number of oil splotches and oil mist on roads that the oil bubble forms only
>in a narrow range of wind speed. Wind speed being vehicle speed. These ellipses are formed
>relatively rarely in the genersal environment of vehicle oil drips. That seems the most reasonable
>conclusion I can find. High seed routes have only oil fog. Driveways, only drops.
>
>
After further reflection I think the error is in thinking of these in terms of soap bubbles. From
the diagram presented earlier, the air-buffeted droplet forms a ring, with a thinner "parachute"
at the back that provides cohesion and pulling force against the ring closing. This is unlike a
soap bubble that has relatively uniform thickness because it has escaped the turbulence that
formed it and claimed a spherical shape. I think the oil bubble in question is not allowed to
complete the sphere.
Further, the relative wind experienced by the droplet is coming from the direction of travel. So I
can see the resulting ring oriented more nearly vertical to the road. If this object settles with
some forward velocity you get an eliptical ring. The thin film forming the parachute would either
break and retreat to the ring from surface tension, or perhaps deposit on the road but its much
lower mass would leave a much fainter mark. I'd guess that parachute breakage at impact would be
common. The ring itself would last longer under those conditions, perhaps long enough to deposit the
elipse. On those occasions where the ring lost cohesion before complete deposition, you would get
the open-ended elipse you've observed with the opening in the direction of travel.
Instead of my altitude-burst hypothesis I now think the various sizes are simply caused by the
amount of inflation of the object prior to contact. The previous idea was based again on soap
bubbles and the idea that an equivalent mass of soapy water would yield bubbles of about the
same size. however, with the object we're talking about, the predominant mass can be contained
in the annular ring, and more can be pulled into the parachute, and the ring opening expanded to
various sizes.
finally, the uniform ratio of length and width suggests *settling* at a fairly uniform forward
speed, and this should be caclulable by assuming a reasonable fall height for the drop, giving the
vertical acceleration. It seems that would be a fairly low forward speed. The forward speed will
have degraded significantly once the drop hits the oncoming wind. It is probably the initial
encounter with the airstream that determines whether the drop is volatized, remains a drop, or
forms the ring/parachute. Figuring that initial airspeed from the elipse I KNOW takes more math
than I have.
Now that I've hedged my bets with contradictory hypotheses some testing is in order. I don't know if
I can generate enough windspeed with my household fans though I'll probably give it a shot. Perhaps
someone with a leafblower would like to try. My other option would seem to be deliberately dripping
oil from a moving vehicle, which would probably get me a citation as opposed to the millions of
"honest" oil drippers. My preference would be a stationary test and try to get some images or at
least some oil rings on a newspaper.
>
>
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<br> <br> <a class="moz-txt-link-abbreviated"
href="
mailto:[email protected]">
[email protected]</a> wrote:<br>
<blockquote type="cite" cite="
[email protected]"> <pre wrap="">John
Albergo <a class="moz-txt-link-rfc2396E"
href="
mailto:[email protected]"><
[email protected]></a> writes:
</pre> <blockquote type="cite"> <blockquote type="cite"> <pre wrap="">Unfortunately the last
drawing in this URL, the drop should have a line across the bottom, showing that it is the cross
section of a nearly a complete "soap bubble". Soap bubble leave a wet ring on the surface where
they land. If that surface is moving relative to the bubble, the ring will be elliptical. </pre>
</blockquote> </blockquote> <pre wrap=""><!----> </pre> <blockquote type="cite"> <blockquote
type="cite"> <pre wrap="">The unanswered question that I have is, why they all have nearly the
same aspect ratio of major to minor axis, regardless of size. They range from 20 to 200mm in
length. It means that they all have the same velocity to the road when they burst, but why? </pre>
</blockquote> </blockquote> <pre wrap=""><!----> </pre> <blockquote type="cite"> <pre
wrap="">Assuming that most oils have the same surface tension, then I'd guess that most oil drips
would be about the same size, and "pop" at about the same airspeed (relative wind). Perhaps the
size of the resulting road ring is due to the "altitude" of the burst? </pre> </blockquote> <pre
wrap=""><!----> After thinking about it some more and looking at oil drops on Sierra mountain
passes this weekend, I am convinced by the number of oil splotches and oil mist on roads that the
oil bubble forms only in a narrow range of wind speed. Wind speed being vehicle speed. These
ellipses are formed relatively rarely in the genersal environment of vehicle oil drips. That seems
the most reasonable conclusion I can find. High seed routes have only oil fog. Driveways, only
drops. </pre> </blockquote> <blockquote type="cite"
cite="
[email protected]"> </blockquote> <pre wrap="">
After further reflection I think the error is in thinking of these in terms of soap bubbles. From
the diagram presented earlier, the air-buffeted droplet forms a ring, with a thinner "parachute" at
the back that provides cohesion and pulling force against the ring closing. This is unlike a soap
bubble that has relatively uniform thickness because it has escaped the turbulence that formed it
and claimed a spherical shape. I think the oil bubble in question is not allowed to complete the
sphere.</pre> Further, the relative wind experienced by the droplet is coming from the direction of
travel. So I can see the resulting ring oriented more nearly vertical to the road. If
this object settles with some forward velocity you get an eliptical ring. The thin film
forming the parachute would either break and retreat to the ring from surface tension, or perhaps
deposit on the road but its much lower mass would leave a much fainter mark. I'd guess that
parachute breakage at impact would be common. The ring itself would last longer under those
conditions, perhaps long enough to deposit the elipse. On those occasions where the ring lost
cohesion before complete deposition, you would get the open-ended elipse you've observed with the
opening in the direction of travel.<br> <br> Instead of my altitude-burst hypothesis I now think
the various sizes are simply caused by the amount of inflation of the object prior to contact.
The previous idea was based again on soap bubbles and the idea that an equivalent mass of
soapy water would yield bubbles of about the same size. however, with the object we're
talking about, the predominant mass can be contained in the annular ring, and more can be pulled
into the parachute, and the ring opening expanded to various sizes.<br> <br> finally, the uniform
ratio of length and width suggests *settling* at a fairly uniform forward speed, and this should be
caclulable by assuming a reasonable fall height for the drop, giving the vertical acceleration.
It seems that would be a fairly low forward speed. The forward speed will have degraded
significantly once the drop hits the oncoming wind. It is probably the initial encounter with
the airstream that determines whether the drop is volatized, remains a drop, or forms the
ring/parachute. Figuring that initial airspeed from the elipse I KNOW takes more math than I
have.<br> <br> Now that I've hedged my bets with contradictory hypotheses some testing is in order.
I don't know if I can generate enough windspeed with my household fans though I'll probably
give it a shot. Perhaps someone with a leafblower would like to try. My other option
would seem to be deliberately dripping oil from a moving vehicle, which would probably get me a
citation as opposed to the millions of "honest" oil drippers. My preference would be a
stationary test and try to get some images or at least some oil rings on a newspaper.<br> <br> <br>
<blockquote type="cite" cite="
[email protected]"> <pre wrap=""> </pre>
</blockquote> <br> </body> </html>
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