Showing posts with label Stability. Show all posts
Showing posts with label Stability. Show all posts

Friday, 27 May 2016

Stability at last

The End of Stability

Work, work, work! No time for blogging until now.

Let's look at a really round bottom boat first.


So first we'll join the chines which leaves us with a trapezoid, and finding the centre of that is described here (centre already marked). If we join the centre of that line with the centre of the curve we essentially have two almost triangles and finding the centre of those is described here.

Once we have the centre of each almost triangle



We can join those centres with a line.



Where that line crosses the line join the center of the curve and the chine line is the centre of the area as both almost triangles are the same size.



We then join the two centres of area and do the math set out here and that gives us the centre of buoyancy



Again if you overlay this hull with the other two the centres of buoyancy are almost the same.



Well what about a boat with no parallel sides. That's even easier than our square boat.

You can divide the underwater area into two triangles and we already know how to find the centers there so I won't go into detail. What is most amazing is that an overlay of this dory type hull onto the other three puts the CB in almost the same place as all the others.



The only thing that is the same about the four hulls is their waterline at the beam. The dory shape is very much smaller displacement although the other three are about the same. I'm going to investigate this further and will comment on it at some later date.

Next time aesthetics or does it look good?

Wednesday, 6 April 2016

Stability Again

The stable Farmer

In his book, My Old Boat Shop,WestonFarmer observed that he had discovered a rule of thumb target for comfort at sea and that was the pounds per square foot loading of the waterplane. He surmised that the optimum loading was 64 pounds per square foot of the waterplane, or to put it another way the underwater volume should be the area of the waterplane times 1 foot. He theorized that this would make the vessel the same weight as the sea surrounding it and thus the vessel would move with the sea not out of sync with it as would a lighter or heavier vessel. But what about the stability of such a vessel?

This idea intrigued me so I did some follow up. To dissect this theory we'll use a closed box 10' long by 4' wide and 2' deep. In the first iteration the box weighs 64 lbs per cubic foot or 128lbs per sqft of waterplane.


The green line is the waterline, the centre of gravity and the centre of buoyancy coincide. Logic tells you that this arrangement would not be very stable as it would rotate about the centres completely underwater. Add some sides,

Stability increases but comfort doesn't as the boat would move out of sync with the movement of the water. A wave passing through would start the boat moving upwards but not at the speed of the wave. As the wave passed and the trough arrived the boat would continue upwards due to inertia and then start to fall as the next wave arrived creating a very uncomfortable motion.

So what would happen if we loaded the boat as Mr. Farmer suggests?

Here it is,

Mr. Farmer's theory is that this loading would be very comfortable as the boat would move in sync with the water, Stability is much improved as the centre of bouyancy is now below the center of gravity and would move outboard as the boat heeled. Let's take a look at how that would work.

Here is our box boat at 40 degrees of heel,

However the immersed volume is too great so we must adjust the waterline (WL) and then determine the center of buoyancy, which is a piece of cake with a triangle.



You all remember your basic geometry of course. From that we can determine the metacentric height for that angle of heel and the righting arm.



But what did I discover? Here it is - If you look at the diagram above where we found the center of the triangle you'll notice that the line from the top left to the middle of the right side cuts though the deck line exactly in the centre, from that we can deduce that the center of buoyancy falls on a line joining the mid points of the two parallel sides. But where on that line?

Jim Michalak in a post here,  http://www.jimsboats.com/1dec15.htm shows you how to find the centre of effort of a four sided sail, that same method can be used with the above knowledge to find the center of buoyancy of a four sided immersed section but without the math. Here we go.

Here's our boat at 15 degrees of heel, the immersed volume is four sided.



First we join the two mid points,



Then divide the four sided figure into two triangles, find the centre of each and join the two centres.



Where the two lines joining centres and midpoints cross is the center of buoyancy.



But will it work for boats that don't have two parallel sides or a round bottom boats. Next time.

Saturday, 2 April 2016

Stability One

Staying upright or at least afloat

Here's the real deal on stability in small boats, modern sail boat design http://www.wavetrain.net/boats-a-gear/471-modern-sailboat-design-quantifying-stability. Which is perfect for larger boats with decks and a mostly fixed centre of gravity. But what about small open boats such as the one we've just been working on. Well here is the stability curve for RMSQ&D assuming a fixed centre of gravity.



So degrees of heel are on the X axis and righting arm, in inches, on the y axis. The reason we've only gone to 45 degrees is because beyond that water is coming in over the gunwale and you're going down.

You can see that this boat has a pretty good level of stability up to 45 degrees which is great. However the fact is that you, the person in the boat, has a huge influence on the stability through your ability to move the centre of gravity by moving yourself about.

The question is how did I calculate the data for this curve? It is mind numbing work involving drawing and redrawing waterlines at various degrees of heel and then calculating the centre of buoyancy using stations and Simpson's rule. It is not for the faint of heart. Information on the process is here, www.mi.mun.ca/media/mi/boatrace/files/shipcalculations2.pdf , and here, http://koti.kapsi.fi/hvartial/stab/stab.htm.

The one thing to remember is when you draw in the new waterline at a different angle of heel the displacement must remain the same. With the boat dead level the displacement of station 5 is 109.118 cubic inches, or .7578 cu ft or 48 lbs However when you heel the boat 10 degrees without altering the waterline the displacement is 136.706 cu in, or .9493 cu ft. So we must reduce that displacement by .1915 cu ft, so the waterline must go down but by how much?

If we measure the new waterline it is 3.4 ft, 3.4 into .1915 is .056 ft or .675 inches so we draw in the new waterline .675 inches below the old water line and measure the difference in volume which works out to 28.642 cu in which brings our displaced volume down to 108.064 which is close enough.

We then divide the new waterline into 10 sections, making sure one station line passes through the centre of gravity, giving us the measures for applying Simpsons rule and calculate the transverse centre of bouyancy for station 5.

And then we do it all again for different angles of heel.

Westlawn recommends using the trapezoidal rule instead of Simpson's I don't think there is much difference in the end result.

The thing to remember is that beam is directly proportional to initial stability. But too much beam can create problems with dynamic stability.

We'll talk more about stability next time and about a discovery I have made whilst working on this.