Curling clubs,
curling rocks, curling ice, curling technology |
| CHAPTER TS 2, page2.10
of The Book which is now free on the web. WHY ROCKS MAY CURL/MOVE IN THE "WRONG" DIRECTION
I did curl again at GPCC and the rocks again "wore out" soon after the "in-place" sand paper job. I will now curl at the Valleyview club this year, competitive league, because they will not curl at a club,GPCC, with such "bad rocks." Destroy your club, Buy
porcelain rocks We don't want to introduce
thermal factors to the surface so we use a porcelain gear with
similar insulation/thermal conductivity qualities of granite. No analog rock that is made of a
non-wettable substance/surface will work like granite. A rubber tire tossed flat ways down a highway spinning right would do the same. It would move left, laterally opposite to the normal curling rock turn/curl direction, due to the high friction environment until the initial turn energy had dissipated and then it would skid ahead in the projected direction. In a game situation, after the first two ends, (pebble tops knocked/sheared off/down) a curling rock will move in the direction of rotation because the snowplow slow side friction is higher than the net of front and rear cup edge lateral shear friction. When you brush a rock, you minimize snowplow slow side friction and the remaining shear friction has a greater influence and may stop curl or even cause a lateral rock movement opposite to the original "curl" direction. The curl is reduced. You "illegal" corner brushers can do your job now that you know where to brush? The so-called illegal or short or corner brushing is no longer illegal.
Analog Rock/Gear |
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Shear Friction Zone that Causes
Gear/Rock to resist "slow Side" friction and will make gear
rock move left and maybe a
granite rock in
first two ends. GEAR/ROCK TEETH
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"Gear" teeth grab/"shear" pebble and make the gear/rock move left in the high friction environment -- like a granite rock's leading and cup edges biting new pebble in the first two ends. It is clear that the net of leading edge less/minus trailing cup edge lateral friction is great enough to cause the rock to move left contra to normal curl. The net effect is less because of two reasons. 1. Normal load is higher in front (nose dive effect -rotational torque/force about cg. due to slowing) and more importantly -- 2. The projected radial contact surface is less for the trailing cup edge Vs. leading edge giving less "biting" edge and hence less friction for the rear. Vibration from uneven pebble heights dumps friction causing snow out the momentary trailing edge and vibration breaks the molecular bond of ice on the rocks running surface and sheet ice and is THE reason the rock slides so easily on pebbled ice. Without pebble, there is no curl. Without some frost on pebble tops and valleys, there is no curl. This fact is why you can slow or even stop curl by brushing!!
Side thrust opposite to curl direction, "shear friction," can overcome
slow side snowplow friction when the ice is very cold (pebble hard) and when new tall
pebble is present giving the rock edges friction material to bite on causing the
rock to curl minimally or even "backup.".
The rock will run straighter or may even "curl" to the left in a rock
turning right scenario. Brushers can level and polish the tops of pebble and
valleys reducing shear
friction enabling the rock to travel further and with more curl (Especially in
the EARLY TWO ENDS) when the
rock is in a high friction new pebble (pebble not clipped) environment.
After the pebble reaches a more uniform height (tops
are flatter) to support rock weight, the net lateral forces of leading and cup edge pebble shearing is
reduced allowing curl. The rock will continue to "shave" the frost buildup and
drag it to the slow side to effect -- curl.
Across the face brushing will make the rock slide further and make it run
straighter (reducing net shear force difference of leading edge and cup edge -- shearing which act in
opposite directions) and slow side friction become more equal because slow side friction
is reduced (due to momentary brushing of large crystals/frost into small/ballbearing
frost) in the new "low friction" environment of "keen" ice. Shortside
brushing on the slow side of a "draw" can stop curl and can make the rock actually curl in the
opposite direction (backup) by up to 6". Brushing the fast side will increase curl!!