The Aerodynamics Of Sail Interaction - Gentry Sailing

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.The Aerodynamics of Sail InteractionBy Arvel GentryProceedings of the Third AIAA Symposium on the Aero/Hydronautics of SailingNovember 20, 1971Redondo Beach, CaliforniaAbstractThis paper deals with the basic problem of the interaction between a mainsail and the jib. Since this paperDecemberis written for the sailor rather than the aerodynamicist, all aerodynamic terms and concepts are developedand explained as they are needed. The characteristics of the flow about the jib and mainsail airfoils whenthey are each used alone and when they are used together are discussed and illustrated. Results from theseflow field studies give a very complete and accurate description of the jib-mainsail interaction problem.1. IntroductionThe general subject of the interaction of sails, both onthe same boat and on boats sailing near each other, hasbeen of interest to competitive sailors for sometime. Thesailing literature abounds with attempts to explain justwhat is involved in the interaction between two sails. Suchterms as slot-effect, Bernoulli's equation, the venturieffect, mast effect, and even safe leeward position appearfrequently in what are apparently very rationalexplanations of this very basic sailing problem. However,the explanations are usually different in many respectsand as a result, this general problem has been the subject ofmuch argument and discussion over the years.As an aerodynamicist by profession and a weekendsailor (by preference), I have been interested, amazed andamused by this situation. After talking to a number ofsailors and reviewing both the sailing and aerodynamicliterature, I realized that there were several reasons whyarguments on this subject had persisted for so long.First, some of the difficulties of the sailor inunderstanding this problem stem from some completelyfalse and misleading ideas published in standard sailingreferences. Second, the explanations given in the literaturewere based on educated guesswork and practicalexperience and only a very limited amount of actualtheoretical calculations or measurements, not fromdetailed test measurements or valid and accuratetheoretical calculations. And third, attempts byaerodynamicists to properly explain the problem have notreached the sailor because of the technical language usedand also because the aerodynamicist's descriptions werenot always completely accurate themselves.Although it is recognized that a single paper such asthis cannot completely erase the years of argument toeveryone's satisfaction, the most important effects that arebrought about when two airfoils are used close togetherare illustrated and discussed. Important aerodynamicterms and concepts will be introduced and explained asthey are needed. The results shown in this paper wereobtained with the aid of some of the same techniques andC1999tools used by the aerodynamicist in the design of modernjet aircraft. Any educated guesswork will be avoided or, atthe least, clearly identified as such. Since this paper iswritten for the sailor, not the engineer, it will not dwell onthe mathematical details of the aerodynamic theories used(this type of information is well-covered in the referencedaerodynamic literature).2. Important Definitions and ConceptsA number of important terms and concepts should beclearly understood by the non-aerodynamicist before themain body of this paper is approached. A step-by-stepdevelopment of this fundamental aerodynamicknowledge is necessary before the reader can appreciatethe significance of the basic arguments and explanations tobe presented later.2.1 Division of Flow RegionsWhen the aerodynamicist studies the airflow about ashape, he recognizes that the flow can usually be dividedinto two basic types of flow areas, the external flow region,and the boundary layer region. These two flow regions areillustrated in Figure 1.lowal fnreExtTransitionalTurbulentLaminarFigure 1. Definition of flow regions about a thin airfoil.The boundary layer flow region is that layer of air thatlies very close to the airfoil. The thickness of this layer of airis greatly exaggerated in the Figure 1 for clarity. Air hasviscosity (even though it is very small when comparedwith other substances), and it is in the boundary layer thatthe viscous characteristics of air come into play. Because ofthis viscosity, the air that touches the airfoil is actuallycarried along by the airfoil (the air has zero speed withrespect to the surface of the airfoil). The air just a small1971 Arvel Gentry

.distance fromthe airfoil moves with some finite velocityRanger23 Newsletterwith respect to the airfoil. The air at the edge of theboundary layer moves with the speed of the external air atthat point on the airfoil. The remainder of the airflow willbe identified as the external flow. The viscosity of the airdoes not affect the aerodynamic calculations for this part ofthe flow. The techniques used by the engineer incalculating what happens to the air in these two types offlow are different.The boundary layer itself is usually divided into threeseparate types of flow. Near the leading edge of an airfoilthere is a very smooth change of airspeed within theboundary layer from the airfoil surface to the edge of theboundary layer. This is the laminar boundary layer.Eventually, because of the development ofunsteadiness within the boundary layer and because ofdisturbances introduced into the flow by roughnesses (jibhanks, cloth seams, etc.), the smooth changes in speedwithin the laminar boundary layer start to give way to amuch more erratic type of flow. This is called thetransitional region of the boundary layer. After this shorttransitional region, the boundary layer becomes fullyturbulent.The external flow is not appreciably affected by this sothe lift on the airfoil does not change much. The mostsignificant effect is that the skin friction drag is greater inthe turbulent area of the flow than it is in the laminarportion. For the portions of the boat that are underwater,great care is usually taken to keep the bottom clean andsmooth to delay the transition from laminar flow toturbulent flow as far back on the hull or keel as is possible.Laminar separationTrubulentSeparationFigure 2. Separation flow areas on a thin airfoil.Figure 2 shows another part of the airflow about a sail ,separated flow. Separated flow regions occur when theboundary layer is no longer able to follow the surface of theairfoil. When this point is reached, the boundary layerseparates from the surface and a very confused and mixedup type of flow is formed. (Note that from theaerodynamic standpoint, we refrain from calling this typeof flow turbulent, since the word turbulent is reserved foruse in describing the turbulent boundary layer. Instead,we will use to the term, “separated flow”).There are two types of separation: laminar separationand turbulent separation. A boundary layer will separatewhen the external pressure along the surface starts toincrease too rapidly. The more rapid the increase inpressure, the more likely it is that the boundary layer willseparate. The rate of change of pressure along the surfaceis called the pressure gradient. When the pressure is-2-increasing, the pressure gradient is called an adversepressure gradient.Whether or not the boundary layer separates whensubjected to a given adverse pressure gradient dependsupon: the character of the boundary layer, laminar orturbulent, what has happened to the boundary layerbefore reaching the adverse pressure gradient, and whatthe speed of the airflow is a the edge of the boundary layer.The speed-distance factor is expressed by theaerodynamicist in a term called the Reynolds number.In general, the laminar boundary layer is more proneto separation than the turbulent boundary layer. In somecases the separated flow will reattach itself to the surface ofthe airfoil. This is frequently the case for a laminarseparation where a small separated bubble may form andthe flow reattach as a turbulent boundary layer.If the flow separates from the airfoil (either a laminaror turbulent separation) and does not reattach, weexperience what is defined as a stalled condition. The lifton the airfoil no longer increases with angle of attack butactually reduces. We spot this situation by watching theyarn telltails on the lee side of our jib start to twirl wildly aswe bear off from a close-hauled course.The most important fact to remember from the abovediscussion is that we need an increase in pressure (anadverse pressure gradient) to cause separation. If thesteepness of this gradient is decreased, then theprobability of getting separation will be reduced. We willsee the importance of this later on when we examine theinfluence of the jib on the mainsail.2.2 Potential FlowThe term potential flow is used by the aerodynamicistto describe airflow that is not affected by viscous effects(the boundary layer or by separation). Potential flowtheory is a way of solving the external flow when we areable to neglect the boundary layer or separation. Since wealways try to shape our airfoils (sails) so as to avoidseparation and since the boundary layer is relatively thin,we will find that potential flow solutions have many veryuseful applications.By the use of potential flow theory, we will be able todetermine completely how the air flows past a singleairfoil or around a combination of airfoils such as amainsail and a jib. Potential flow solutions my be obtainedwith elaborate and advanced digital computer programssuch as in Reference 1, or by the use of the rheoelectricanalogy as applied with the analog field plotter. The use ofthe field plotter will be discussed in more detail later.2.3 StreamlinesThe concept of a streamline is very simple and weneed only to look briefly at the example in Figure 3 on thenext page to get the basic idea. The streamlines tell thedirection of the airflow at different points in the flow fieldabout an airfoil. The airflow between two particularstreamlines will always stay between the two streamlines.The stagnation streamline is the streamline that separatesthe airflow that goes on one side of the airfoil (the top orleeward side) from the airflow that goes on the other side

.met all the requirements of the governing equations, butthe calculations indicated that the airfoil had no lift. Thetypes of streamlines that resulted are shown in Figure 4.(the bottom or windward side). The stagnation streamlineleaving the trailing edge or leech of the airfoil divides theairflow coming off the top of the airfoil from the air comingoff the bottom. It is also called a stagnation streamline.SSFigure 4. Flow field without circulation (no viscosity).SSNote that these mathematically determinedstreamlines make very sharp turns in getting around theleading edge and trailing edge of the airfoil. For a thinairfoil this means infinite velocities at these points. Thevelocities around the leading edge can be reduced bybending the airfoil down into the flow (cambering theairfoil) but what about the trailing edge? In real life, wefind that the flow around the trailing edge changes as theair first begins to move past the airfoil so that it leaves theairfoil in the same direction on the top and the bottom.This requirement that the airflow leave the airfoilsmoothly at the trailing edge and in a directiondetermined by an imaginary slight extension of the airfoil,is known as the Kutta condition.It has been found that the Kutta condition can besatisfied mathematically by superimposing another typeof flow solution, called circulation, onto that alreadydetermined above. The superposition of these twodifferent types of solutions is illustrated in Figure 5.Circula tionNon-LiftingSolutionFigure 3. Streamlines about a thin airfoil with boundarylayer and separation neglected.2.4 Effect of Streamline SpacingOnce a complete set of streamlines are determined, wecan make some very useful judgments as to how the windspeed and pressure vary in the flow field about the airfoil.It is quite obvious that when two streamlines get very closetogether, the air will have to speed up to get through thesmaller area. Where the streamlines get closer together theair speeds up, and where the streamlines get farther apart,the air slows down. The next question is, what happens tothe pressure as the air speed changes? The relationshipbetween speed and pressure is provided by Bernoulli'sequation:P 1/2 rV2 Hwhere P pressurer density of air (rho)V2 local velocity squaredH constant within a streamtubeThe trade-off of air speed and pressure along a givenstreamline is governed by Bernoulli's equation and the factthat H, and therefore the sum of pressure P and ½ rV2 mustremain constant. Now this is all quite simple, but it isimportant to note that, before we can apply Bernoulli'sequation, we must first know how the air flows about theairfoil. We must know where the streamlines go. All toooften in the sailing literature, Bernoulli's equation isapplied with only guessed streamlines and theconclusions drawn can be grossly wrong.The aerodynamicist usually converts velocity orpressure into a pressure coefficient as follows:2Cp (P -P ) / ( ½ rV ) or Cp 1 - (V/V )2Where Cp pressure coefficientP and V conditions well in front of the airfoil2.5 The Generation of LiftWe will now take a look at just how a sail generates lift.Here too, we find that some of the simple explanations inthe sailing literature are wrong. One explanation of how awing of an airplane gives lift is that as a result of the shapeof the airfoil, the air flows faster over the top than it doesover the bottom because it has farther to travel. Of course,with our thin-airfoil sails, the distance along the top is thesame as along the bottom so this explanation of lift fails.In the first early attempts by aerodynamicists to comeup with a solution to the flow around airfoils, they foundthat their results were not very realistic. Their solutionsOOOO OOOOFigure 5. Superposition of circulation and non-circulationsolution to give lift.The strength of the circulation is adjusted so that theKutta condition at the trailing edge is satisfied. Since thevelocities from the circulation solution are smaller than thenon-circulation solution, it is easy to see that when the twoairflows are added together, the air on the top of the airfoilwill be accelerated and that on the lower side will beretarded slightly. With slow speed flow on the bottom ofthe airfoil and high speed flow on the top, we get high-3-

.pressure on the bottom and low pressure on the top, andthe necessary pressure difference across the sail tomaintain the cambered shape and to give the lifting forceto drive the boat.3. The Analog Field PlotterBefore we start examining the flow field results aboutsome typical airfoils, a piece of equipment will bedescribed that is capable of providing direct solutions ofthe potential flow problem. This equipment is called the“Analog Field Plotter” and uses what is referred to as therheoelectric analogy. A picture and diagram of theequipment setup are shown in Figures 6 and 7.Figure 6. Analog field plotter equipment.rapeCirculationinputSlide wireCpinguctdnoVoltage dividing potentiometerSilver painted conducting stripsTeberotPNull detectorSilver painted conducting stripFigure 7. Diagram of analog field plotter.-4-

.The flow field recording surface is a special sheet ofblack conducting paper. An electrically conducting paint isused to paint a conducting strip across the top and bottomof the paper. The electrical control box contains a powersupply that is attached to the painted strips across the topand bottom of the paper so that current flows through thepaper from one strip to the other. Because of the resistanceof the paper, we will get a voltage drop between the twostrips. If nothing else is painted on the paper between thetwo border strips, the voltage across a horizontal linethrough the center of the paper would be halfwaybetween the voltage at the top and the bottom. The controlbox contains a sensitive potentiometer, a null-meter and aprobe device so that very accurate traces may be made ofthe lines of constant potential (voltage) within the paper.These lines may be marked with white chalk.The airfoil shape to be studied is painted in the centerof the paper at the proper angle as though the airflow wereflowing from left to right across the paper. The presence ofthis highly conducting painted shape placed at an angle onthe paper will cause all of the constant potential lines to bedistorted. What we have accomplished at this stage of theequipment hook-up is to construct an exact analog to theflow about an airfoil with zero circulation (see Figure 4).The mathematical equations necessary to solve the airflowabout the airfoil are exactly the same as the equations thatdescribe the flow of electricity through the conductingpaper.However, the airfoil still has zero circulation as wehave done nothing to assure that the Kutta condition issatisfied at the trailing edge of the airfoil. To do this, we firstrun a special resistance wire between the top and bottomstrips. We then tap off of this with a conducting wire that isattached to the airfoil painted onto the paper. By slidingthis tap-point to different spots on the resistance wire wecan cause the airfoil to be at any potential (voltage)between the top and bottom strips.By a trial and error process, we keep adjusting thepotential of the painted airfoil and each time trace theshape of the constant potential line that leaves the trailingedge of the airfoil. When we find the right setting that letsthe streamline leave the airfoil smoothly at the trailingedge, we will have satisfied the Kutta condition. Themathematical equations that now describe the flow ofelectricity through the paper are exactly the same as thosethat are used to describe the airflow about the airfoil withcirculation and, therefore, with lift.Once this situation is achieved in our experimentalapparatus we can proceed to use the sensing probe todetermine complete pictures of the streamlines about theairfoil. Any number of airfoils may be studied simply bypainting them on the paper in the proper relative positionsand by attaching a wire to each airfoil so that the Kuttacondition on each is satisfied.The accuracy of the results obtained with the fieldplotter have been verified by the use of a potential flowdigital computer program. The field plotter is also a veryuseful teaching device.4. The Single Thin AirfoilNow that we have the necessary aerodynamicbackground and the experimental apparatus we will lookat the basic aerodynamics of the airfoils that are formed byour sails. The characteristics of the flow about a singleairfoil representing a jib will be discussed first. The nextsection then deals with the flow about two airfoils such as ajib and a mainsail.The airfoil shapes and relative position and sizes asselected for these studies approximate the airfoil sectionson a mainsail and a genoa jib (both taken at the level of thefirst batten on the main). Of course, the thickness of theairfoils on our sails is virtually zero, while the thickness ofthe airfoils painted onto the field plotter paper is somefinite value (about 1.5 to 3% thick) because of the size of thepaintbrush used. This approximation will not significantlyaffect our answers. The initial discoveries for this studywere made with the analog field plotter. The actual resultspresented here were determined later with a potentialflow computer program.Figure 8 shows the streamline patterns about an airfoilat two different relative wind angles for the boat. In thefirst case, the angle of the centerline of the boat was 25degrees from the relative wind. This sail had a sheetingangle of 20.6 degrees from the centerline of the boat, so theairfoil itself had an angle of attack of 4.4 degrees. In thesecond case the angle of the centerline of the boat from therelative wind was set at 35 degrees. Still using the samesheeting a

The Aerodynamics of Sail Interaction By Arvel Gentry Proceedings of the Third AIAA Symposium on the Aero/Hydronautics of Sailing November 20, 1971 Redondo Beach, California Abstract This paper deals with the basic problem of the int

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