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JO URNAL OF RESEARCH of the Nati ona l Bu reau of Standa rds-C. Engineering and Instrumentation Vol. 64C, No. 2, Apr il- June 1960 The Functional Synthesis of Linear Plots I J. P. Vinti and R. F. Dressler 2 (J a nu ary 26, 1960) In pract i cal en 9 in eering or experimen tal wo rk one oft en enco un te rs a fun ct ion F of many vari ables, F IX'S, V's, z's), represen te d only by t he families of c ur ves ob tained by pl ott in g Ji' aga in st each of t he x's on Car tes ian gra ph paper, again st each of the V's on semi- log paper, and again st each of the z's on double-log paper. It frequ ently ha pp ens th at these cur ves are a ll a pprox imately st raight lines over a limi te d ra nge of in te rest. On the ass ump tion t hat th ey are all t ru e st raight lines, t he present n ote shows how to sy nthesize a ll the gr ap hi ca l represen tat ion s, for any numb er of paramete rs, in to the most general formul a poss ibl e, e xpr essing F as t he produ ct of a multilin ea r fun ct ion of the x's a nd the exponent ial of a constant-free mul t ilin ea r fun ct ion of the V's a nd of the log z's, t he coeffi - cien ts in bot h mul t ilin ear fun ct ions being ind ependent of the x's, V's, a nd z's. 1. Introduction In an invest igat ion by one of tbe aut hors on assembl ages of elastic shell s, the various r es ults for cer tain components of str ess and displa cement exhibi te d approximately linear behavior over th e limited ranges of interest of the rel evant parameter s, wh en plotte d on Car- tesian graph pap er, semi -l og paper, or double-log paper. Th ese r es ul ts, d erived from various num eri cal calculations a nd corroboratory experiments, are fun ctions of many param eter s, such as t he various geometrical r at io s defining shell shapes, the shell thickness, Poisson's r at io, the num- ber of coupled shells, and other significan t quantities. Ra ther than to retain these extensive r es ult s in the form of cumb ersome families of graphs, it was d es irable and useful to combine them in such a way as to obt ain a single explicit formula for each depend en t qu antity, in terms of th e abov e-mentioned ind epend ent parameters. Th e problem of combining such r es ult s is, of course, not peculiar to investi gat ions in elasticit y bu t of te n arises in experimen tal or engineering work of any n at ur e. One can very easily cons tru ct simple functions which will ex hibit some of these " lin ear" prop er ties, bu t the most general answer to tbe inverse problem is less obvious, es pecially when tb e numb er of parameters is lar ge. Th en an unsystemati c attempt to eff ect such a synth es is m ay prove infeasible or in complete, and furnish no assurance th at one has ind eed co n st ructed the mo st general fun ction wi t h th ese proper ties. Our pr esent note, therefore, formul ates the gene ral problem for any numb er of variables in a precise mann er and deri ves its most general so lu tion. For the simple case of only t hr ee parameter s, the solution is illust r ate d by a few exampl es. 2. The General Problem In th e following developments we shall ass ume t hat all the pertinent quan tities ha ve been grouped into ind epend ent dimensionless combinations, so as to tak e ad va ntage of wh ate ver infor- mation is provid ed by th e Bu ckingham Pi theorem. 3 Let us then consider a dimensionless func- tion F of th e dimensionless ind ep endent variables X l, X2, . .. , Xm ; Yl , Y 2, .. . , y p; 21, 22, .. . , 2 Q; and U l , U 2, ... , U r, such th at a st raight line result s wb en we plot F again st any X on ordinary Cart esian gr aph paper, against any Y on semi-log pap er, or against any 2 on double-l og paper. Let the u's denote all other dimensionless variabl es on which F may depend, bu t for which no such "linear " proper ty exists. It is und er stood, of course, th at in pra ctice such linearit y m ay hold only approximately, and only for a certain bound ed range of the vari able used as ab scissa, a nd only for certain bound ed ranges of the remaining vari ables, which a pp ear as parameters. With no lo ss of generality, however, we relax th ese rest ri ct ions, assuming t hat each plot is a straight line for all values of abscissa a nd pa rameters. I Th is research was supported by tbe Un ited States Air Force, t hrough t he Oflice of Scien tifi c Research of the Research and Development Command. , On leave to Inst itu te of M athematical Sciences, New York Uni versity, New Yo rk , N.Y. , P. W. Bridgman, Dimensional analYS iS, p. 36 (Yale Uni v. Press, New II aven, Conn ., 1 931) . 115
Transcript

JO URNAL OF RESEARCH of the National Bureau of Standa rds-C. Engineering and Instrumentation Vol. 64C, No. 2, April- June 1960

The Functional Synthesis of Linear Plots I

J. P. Vinti and R. F. Dressler 2

(J anuary 26, 1960)

In practical en9ineerin g or experimental work one often encounters a fun ction F of ma ny variables, F IX'S, V's, z's), r epresented only by t he families of curves obtained by plottin g Ji' against each of t he x's on Cartesian graph paper, against each of t he V's on semi­log paper, a nd against each of t he z's on double-log p aper. It frequently happens t hat t hese curves are all approximately st raight lines over a limi ted ra nge of interest. On t he assumption t hat t hey a re all t rue straight lines, t he present n ote shows how to sy nt hesize all t he graphi cal representations, for any number of pa ra meters, in to t he most general formula poss ibl e, expressing F as t he product of a mul t ilinear fun ction of the x's and t he exponent ia l of a constant -free mul t ilinear fun ction of t he V's and of t he log z's, t he coeffi­cients in both mult ilinear fun ctions bein g independent of t he x's, V's, and z's.

1. Introduction In an investigation by one of tbe au thors on assemblages of elastic shells, the variou s

r esul ts for cer tain componen ts of stress and displacement exhibited approximately linear behavior over the limi ted ranges of in terest of the relevant parameters, wh en plotted on Car­tesian graph paper , semi-log paper , or double-log paper . These resul ts, derived from various numeri cal calcula tions and corrobora tory experimen ts, are functions of m any parameters, such as t he various geometrical ratios defining shell shapes, the shell thickness, Poisson's ratio, the num­ber of coupled sh ells, and other significan t qu an tities. Ra ther than to r eta in these extensive results in the form of cumbersome families of graphs, it was desirable and useful to combine them in such a way as to obtain a single explicit formula for each dependen t quan tity, in terms of the above-mention ed independen t parameters .

The problem of combining such results is, of course, not peculiar to investigations in elasticity bu t often arises in experimental or engineering work of any nature. One can very easily construct simple fun ctions which will exhibi t some of these "linear " proper ties, but the most general answer to tbe inverse problem is less obvious, especially when tbe number of parameters is large. Then an unsystematic attempt to effect such a synthesis may prove infeasible or incomplete, a nd furnish no assurance that one has indeed constru cted the most general function with th ese proper ties. Our present no te, therefore, formulates t he general problem for any number of variables in a precise manner and derives its most general solu tion. For the simple case of only three parameters, the solution is illustrated by a few examples.

2. The General Problem In the following developments we shall assume that all the pert inent quantities have been

grouped into independent dimensionless combina tions, so as to take advantage of wh atever infor­mation is provided by the Buckingham Pi theorem .3 Let us then consider a dimensionless fun c­t ion F of the dimensionless independent variables Xl, X2, . .. , Xm ; Yl , Y 2, .. . , y p; 21, 22, .. . , 2 Q;

and U l , U 2, ... , U r , such tha t a straigh t line results wb en we plot F against any X on ordinary Cartesian graph paper , against any Y on semi-log paper , or against any 2 on double-log paper. Let the u 's deno te all other dimensionless variables on which F may depend, but for which no such "linear" proper ty exists. It is understood, of course, that in practice such linearity may hold only approximately, and only for a certain bounded range of t he variable used as abscissa , and only for certain bounded ranges of the remaining varia bles, which appear as parameters. With no loss of generality , however , we r elax these r estri ctions, assuming that each plot is a straigh t line for all values of abscissa and parameters.

I Th is research was supported by tbe United States Air Force, through t he Oflice of Scien tifi c Research of the Research and Develop ment Command.

, On leave to Institu te of M athematical Sciences, New York Un i versity, New York, N .Y. , P. W. Bridgman , Dimensional analYSiS, p. 36 (Yale Univ. Press, New IIaven, Conn., 1931) .

115

We put ... , ln zq = YlI, (n=p+q); (1 )

then F(xJ, ... Xm, Yl , ... Yn, u) is a function such that the plot of F against any x or of lnF against any Y is a straight line on Cartesian graph paper. Here u denotes the set Ul, U2, . , U T •

Then (k =1 ,2, ... , n ) (2)

where Ak and B k are functions of Xl ... Xm, Yl ... Yk- J, Yk+J ... Yn, and of the u's. ~Te then ask: if InF is linear in each y when the other V's are all beld constant, what is the most general form for lnF, as a function of the V's, that will represent such a property?

To answer tbis preliminary question, we first recall tbe definition of a multih'near function G, of several variables tl , t2 , • •. , ts) as a function which is the sum of a constant and a linear combination of all the products of the t's taken one at a time, two at a tim e, ... , s at a time, without repetition. For example, if 8= 3,

(3)

Any such multilin ear function satisfies the differential equations

(k = I,2, ... , s). (4 )

(~Th en the constant term vanishes, we term G a constant-free multilinear function. ) I t is then easily shown by indu ction that G(tJ,t2' ... , ts) is the most general function of t J,t2 , •.• , ts which is linear in each t.

2.1. The Synthesis for the y's Alone

On a,pplying these considerations to (2), we find that

(5)

where Ntx• u) denotes a general constant-free multilinear function of the V's, with coefficients which are, a priori, fun ctions of XJ, •.. , Xm , U. On placing

(6)

we obtain (7)

which gives the synthesis of the linearities of lnF versus the V's.

2.2. The Complete Synthesis

Since F is linear in each x, it follows from the property of multilinear functions that

(8)

where P (v. u) is a general multilinear function of the x's, the coefficients b eing functions of the V's and the u's. Then

where by (4) o2Njoy%= 0

o2PjoX] = 0

(k=I,2,

(j= I ,2,

116

,n)

,m).

(9)

(10)

(1 1)

We next show that f is a multilinear fun ction of the x's . To do so, pu t every y equal to zero in (9) . Since N contains no constan t term, it then vanishes, so that (9) becomes

(12)

H ere Jypu ) is simply the expression for P (v. u) with each coefficient evaluated at each y = O, so tha t it is a mul tilinear fu nction of the x's wi th coefficien ts depending only upon the u's.

vVe now show that the coeffi cients in N (x.u) are independ ent of the x's, as follows. Insert (12) in to (7), so that

F = M (u) exp N (x. u) (13}

and require that (13) satisfy (11 ). I t follows that

(14).

whcre we havc omit ted tbe superscrip ts for convenience. Since M is mul tilinear in the x's , i t follows from (4) that

so that

(16}

If wc now difj'eren tiaLe (16) t wi cc wi th respect Lo Yk, wc find wi th usc of (10) t hat

(l7}

wh encc ~ (o N ) = o { j = 1,2, . .. , m, 0Yk oXj k= 1,2, . .. ,n.

(IS}

Equation (I S) mcans that oN joxj can bc a function only of the x's and the u's. But Nand oN joxj are constan t-free multilinear fun ct ions of the V's, wi th coefficients tllat are, a pnon,. fun ctions of t he x's a nd Lhe u's. Th csc rcs ul ts are compatible if and only if

(j= 1,2, .. . ,m) (19}

so that each coefficien t in the consta nt-free multilinear function N must be independent of the x's.

We may thus rewrite (13) as

(20}

When we return to the original formula tion of the problem in terms of the x's, V's, and z's,. i t follows tha t the most general functional form for F is given by

(21 }

where J.11. (u) is a general multilinear function of the x's and N (u) a general constant-free mul ti­linear function of the V's and ln z's, the coefficien ts in both being functions only of the u's .

3. Some Elementary Examples

As short illustrations of the general result (21), we append a few cases where F has linear plo ts against only three variables. For each we list the specific form tha t (21 ) assumes and thc slopes and intercepts on the appropriate plots. By comparing the behavior of the slopes.

117

L

and intercepts in the various experimentally given families of curves that define the function F with these listed formulas, one can readily determine which coefficients vanish, if any, and thus obtain a specific formula for F in any actual case. Here "In" denotes a natural logarithm and "log" a common logarithm. For an x or a Y the intercept is taken at zero, while for a z it is taken at Z= 1. For the logarithmic plots the slopes and intercepts are those of log F. In the following formulas, it is understood that the constants may be functions of the u's .

(a) x, YI' Y2 F = (k1x+ k2) exp(alYI + a2Y2 + bYJY2)

Cartesian plot versus" x:

slope S = kl exp(aJYI + a2Y2 + bYIY2)

intercept I = k2 exp(aIYI + a2Y2 + bYIY2)

S emi-log plot versus YI :

slope S = 0.4343 (al + by,)

intercept I = log(klx+ k2) + 0.4343azY2

(b) x, y, z F= (klx+ k2 )ealllz"2+by

Cartesian plot versus x :

slope S = kleaIYza,+by

intercept I = k2e"I Yz' 2+by

S emi-log plot versus y:

slope S = 0.4343al + b log z

intercept I=log(klx+ k2) + a2 log z

Double-log plot versus z :

slope S = a2+ by

intercept I = log(klx+ k2) + 0.4343aIY

(c) YI, Y2' Z F = kealYI +U2Y2+b3YI Y2 ZU3+b I YI +b2Y2+ CYI Y2

Semi-log plot versus YI:

slope S = 0.4343 (aJ + b3Y2) + (bl + CY2) log z

intercept 1= log k + 0 .4343a2Y2 + (a3 + b2Y2) log z

Double-log plot versus z :

slope S = a3 + bIYI + b2Y2 + CYIY2

intercept I = log k + 0 .4343 (alYI + a2Y2 + b3YIY2)

(d) y, Zl' Z2 F = keaIYzlu,+b IYZ2a3+b2YH

118

where

S emi-log plo t versus y:

slope

inter cept I = log lc+ a2log zl+ a3log z2+ 2.303b3 Iog ZI log Z2

Double-log plot versus 2 1 :

slope S = a2+ b1y+ 2. 303(b3+ cy)log Z2

intercept

VVA SHl NG'l'ON, D.C.

5398 9- 60- 3 119

(Paper 64C2-31)


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