Parametric instability is investigated for planetary gears where the fluctuating stiffness results from the changing contact conditions at the multiple tooth meshes. The time-varying mesh stiffnesses of the sun-planet and ring-planet meshes are modeled as rectangular waveforms with different contact ratios and mesh phasing. The operating conditions leading to parametric instability are analytically identified. Using the well-defined properties of planetary gear vibration modes, the boundaries separating stable and unstable conditions are obtained as simple expressions in terms of mesh parameters. These expressions allow one to suppress particular instabilities by adjusting the contact ratios and mesh phasing. Tooth separation from parametric instability is numerically simulated to show the strong impact of this nonlinearity on the response.

### Introduction

Mesh stiffness variation as the number of teeth in contact changes is a primary excitation of gear vibration and noise. This excitation exists even when the gears are perfectly machined and assembled. In analytical gear vibration models, it is represented by time-varying mesh stiffnesses that parametrically excite the system. This parametric excitation causes instability under certain operating conditions. The ensuing vibration creates noise, increases dynamic loads, and potentially damages the gear teeth and bearings [1].

Parametric instability in single-pair gears governed by a single degree-of-freedom Mathieu equation has been extensively investigated [2-6]. For multi-stage gear systems, there are surprisingly few studies on parametric instabilities from multiple meshes. Tordion and Gauvin [7] and Benton and Seireg [8] analyzed the instabilities of two-stage gear systems with a mesh phasing between the two mesh stiffnesses. However, their instability conclusions are contradictory. This was recently clarified by Lin and Parker [9] using perturbation and numerical analyses. Lin and Parker also derived simple formulae that allow designers to suppress particular instabilities by properly selecting contact ratios and mesh phasing. For planetary gears ( Figure 1), which have multiple time-varying mesh stiffnesses, no systematic study on their parametric instability has been found in the literature. August and Kasuba [10] and Velex and Flamand [11] numerically computed dynamic responses to mesh stiffness variations for planetary gears with three sequentially phased planets. Their results showed the dramatic impact of mesh stiffness variation on dynamic response, tooth loads, and load sharing among planets. In addition, different contact ratios and phasing conditions that exist at the multiple meshes complicate the analytical examination of planetary gear parametric instability. How these factors affect instability conditions has not been investigated.

The objective of this study is to analyze parametric instability excited by multiple time-varying mesh stiffnesses in planetary gears [21]. The torsional vibration model used here considers the different contact ratios and planet phasing among multiple meshes, which are critical design parameters in planetary gears. The well-defined modal properties of planetary gears [12, 13] are used to derive simple expressions for instability boundaries separating the stable and unstable regions. From these expressions, the effects of contact ratios and mesh phasing are analytically determined. These results provide insight into planetary gear designs that avoid parametric instability. In practice, planet mesh-phasing schemes are often applied to cancel or neutralize resonant response at speeds where the mesh frequency is near a natural frequency [14-17]. In this same spirit, this study shows that particular parametric instabilities can be eliminated under certain phasing conditions that can be achieved by proper selection of design parameters. Tooth separation nonlinearity induced by parametric instability is numerically simulated and shown to have great impact on the unstable system response.

### System Model and Model Properties

The planetary gear dynamic model used is based on the one developed by Lin and Parker [12].Translational degrees of freedom in that model are eliminated, and only rotational motions of the gear bodies are considered ( Figure 1). Rotational motions of the carrier, ring, sun, and planets are denoted by θ* _{h}, h=c,r,s,1,…N*, where

*N*indicates the number of planets. The gear bodies are assumed rigid with moments of inertia

*I*. The sun-planet and ring-planet tooth meshes are modeled as linear springs with time-varying stiffnesses k

_{c}, I_{r}, I_{s}, I_{p}_{sn}(t), k

_{rn}(t), n=1,…N. Damping and clearance nonlinearity are not considered in the determination of instability boundaries, though they are added later in a numerical example for response calculation. The system equations of motion are

(1)

(2)

where the summation index *n* ranges from 1 to *N*. *u _{h}=r_{h}*θ

*are base radius deflections, and r*

_{h}, h=c,r,s,1,…N_{h}is the base circle radius for the sun, ring, and planets and the radius of the circle passing through the planet centers for the carrier.

*T*are external torques. Each mesh stiffness is represented by where

_{c}, T_{r}, T_{s}*k*are mean values and

_{sp}, k_{rp}*k*are time-varying components of the

_{1n}, k_{2n}*n*-th sun-planet and ring-planet meshes. Expansion of

*k*in Fourier series yields

_{1n}, k_{2n}(3)

where *k _{sp}, k_{rp}* are mean values and

*k*are time-varying components of the

_{1n}, k_{2n}*n*-th sun-planet and ring-planet meshes. Expansion of

*k*in Fourier series yields

_{1n}, k_{2n}(4)

For spur gears, rectangular waves are often used to approximate mesh stiffnesses alternating between *d* and *d+1* pairs of teeth in contact. Figure 2 shows the mesh stiffness variations *k _{1n}*,

*k*with peak-to-peak amplitudes

_{2n}*2k*,

_{vs}*2k*contact ratios c

_{vr},_{s}, c

_{r}, and phasing angles ϒ

*, (ϒ*

_{sn}T*ϒ*

_{sr}+*. The sun-planet and ring-planet meshes have the identical mesh frequency Ω*

_{rn})T*=2*π

*/T*. The sun-planet mesh stiffnesses between planets differ only by a time translation (or phase), i.e.

*k*ϒ

_{sn}(t)=k_{s1}(t-*. Likewise,*

_{sn}T)*k*ϒ

_{rn}(t)=k_{r1}(t-*for the ring-planet meshes. Mesh phasing between planets is determined by planet position angles ψ*

_{rn}T)*and the numbers of teeth*

_{n}*z*for the sun and ring [15]. ϒ

_{s}, z_{r}*ψ*

_{sn}=*/(2π) denotes the mesh phasing between the first and n-th sun-planet meshes (ϒ*

_{n}z_{s}*ϒ*

_{s1}=0);*ψ*

_{rn}=-*/(2π) is the mesh phasing between the first and*

_{n}z_{r}*n*-th ring-planet meshes (ϒ

*); for any planet, ϒ*

_{r1}=0*is the phasing between the sun-planet and ring-planet meshes for a given planet; It is the same for each planet. The Fourier coefficients in (4) are*

_{sr}(5)

Mesh stiffnesses depend on many parameters including the number of teeth in contact, gear facewidth, material properties, profile modifications, and applied load [18]. Let and be the relative amplitudes of mesh stiffness variation. In the simplest approximation, mesh stiffnesses are assumed proportional to the number of tooth pairs in contact, that is, *k _{sp}=c_{s} k_{1t}, k_{rp}=c_{r} k_{2t}* and

*k*, where

_{vs}= k_{1t}/2, k_{vr}= k_{2t}/2*k*are one-pair tooth bending stiffnesses of the sun-planet and ring-planet meshes. With this simplifying assumption, the nominal amplitudes of stiffness variations are ε

_{1t}, k_{2t}*ε*

_{1}=1/(2c_{s}),*2=1/(2c*and one obtains the explicit relation ε

_{r}),*ε*

_{2}=*In practice and in the analysis that follows, however, ε*

_{1}c_{s}/c_{r}.*and ε*

_{1}_{2}are not constrained to these “nominal” values but vary independently of the contact ratios to account for the many factors influencing mesh stiffness variation amplitudes. For this modeling, we let ε

*ε*

_{1}=*ε where*

_{2}/g=*g=O(1) (and g=c*under the simplifying assumption noted above). Substitution of (3) and (4) into (2) yields

_{s}/c_{r}(6)

where the average stiffness matrix **K**_{0} has the same form as (2) with *k _{sn}*,

*k*substituted by

_{rn}*k*. The Fourier coefficient matrices are also in the form (2) with

_{sp}, k_{rp}*k*substituted by for for and substituted by

_{sn}, k_{rn}For the time-invariant case, the eigenvalue problem associated with (1) is

(7)

where ω_{i }are the natural frequencies. The vibration modes φ* _{i}* are normalized as Φ

^{T}

**M**Φ=I with Φ=[φ

*,…,φ*

_{1}*]. The natural frequencies and vibration modes have unique properties due to the cyclic symmetry of planetary gears [12, 13]. We specialize these properties for the case of a rotational vibration model with fixed ring and*

_{L}*L=N+2*degrees of freedom. In this case, all vibration modes can be classified into one of three categories: (1) a rigid body mode (ω

*), (2) two modes with distinct natural frequencies (ω*

_{1}=0*, ω*

_{2}*), and (3) a group of degenerate modes with multiplicity*

_{L}*N*–

*1*(ω

*=…=ω*

_{3}*). In the distinct modes, including the rigid body mode, all planets have identical motion*

_{N+1}(8)

In the degenerate modes, the carrier, ring, and sun have no motion, and the planet rotations satisfy

(9)

These well-defined properties are valid not only for equally spaced planets with position angles ψ* _{n} =2*π

*(n-1)/N*, but also for diametrically opposed planets with ψ

*ψ*

_{n+N/2}=*π [13].*

_{n}+### General Expresion for Instability Boundries

Parametric instabilities occur when harmonics of the mesh frequency are close to particular combinations of the natural frequencies. We determine the operating conditions (that is, mesh frequency Ω and stiffness variation amplitude ε) that lead to instability when *l *Ω≈ω_{p}+ω_{q} for integer *l*. The results are illustrated as stable and unstable regions in the (Ω, ε) parameter plane (Figure 3, for example). Primary (l=1, p=q), secondary (*l=2, p=q*), and combination (*l=1, pq)* instabilities are of most interest as higher order instabilities have much smaller instability regions and are unlikely to occur in practice. The rigid body mode (ω* _{1}=0*) is not excited under operating conditions and does not affect the instabilities of other modes. Only the two distinct modes and the group of degenerate modes are considered in what follows. Applying the modal transformation q=Φz to (1) and using (6), the free vibration equations become

(10)

where the matrices and . Using the method of multiple scales, the solution of (10) is expressed as

(11)

where τ*=*ε*t* and . Substitution of (11) into (10) yields

(12)

(13)

The general solutions of (12) are

(14)

where cc represents the complex conjugate of preceding terms. Insertion of (14) into (13) yields

(15)

The parametric instability when *l *Ω≈ω* _{p}*+ω

*is considered. Let , where σ is a detuning parameter to be determined. When ω*

_{q}*and ω*

_{p}*are both distinct, the instability boundaries are [9]*

_{q}single mode instability: (16)

combination instability: (17)

where.

When ω* _{p}* or ω

*is degenerate, the complexity of instability boundary solutions depends on the multiplicity of the degenerate natural frequencies. We first study the case with multiplicity two for three-planet systems, say ω*

_{q}*=ω*

_{p}*. For the single-mode instability , vanishing of the terms in (15) leading to unbounded response requires*

_{q}(18)

(19)

The nontrivial solutions of (18) and (19) have the form

(20)

where R* _{p}*, R

*, I*

_{q}*, I*

_{p}*are real. With these solutions, (18) and (19) yield*

_{q}(21)

For bounded solutions, the eigenvalues of the coefficient matrix have non-positive real parts, which requires

(22)

Thus, the single-mode instability boundaries for ω* _{p}*=ω

*are*

_{q}(23)

Now consider the combination instability where ω* _{p}*=ω

*are degenerate but ω*

_{q}*is distinct. Vanishing of the terms in (15) leading to unbounded response requires*

_{r}(24)

(25)

(26)

With the solutions (20) and , (24)-(26) give

(27)

Requiring the eigenvalues of the coefficient matrix to have non-positive real parts gives the instability boundaries

(28)

When the degenerate natural frequencies ω* _{3}*=…=ω

*have multiplicity m > 2, vanishing of the terms in (15) leading to unbounded response for*

_{m+2}*l*yields

*m*coupled equations

(29)

Similar to (21), a *2mÃ—2m* coefficient matrix is obtained from (29)

(30)

where* * are *mxm *submatrices of including rows and columns *3, …, m+2*. The σ for bounded solutions is obtained by requiring the real parts of the eigenvalues of this coefficient matrix to be non-positive. Generally, no closed-form solution can be derived for these single-mode instabilities, but numerical evaluation can determine σ and the instability boundaries unless have special features (e.g., diagonal matrices) as discussed later. More is possible for combination instabilities. For combination instability of distinct ω* _{r}* and degenerate ω

*=…=ω*

_{3}*of any multiplicity*

_{m+2}*m*, the same procedure as led to (28) yields instability boundaries

(31)

All results so far apply for a general system (10) with degenerate natural frequencies. These results reduce to simple forms when specialized to planetary gears.

### Planetary Gear Parametric Instability

Planetary gears′ well-defined modal properties are now used to simplify the above instability conditions to compact expressions suitable for use in applications. Expansion of in (10) gives

(32)

where is the deformation of the *n*-th sun-planet mesh in mode φ_{p} and is the deformation of the *n*-th ring-planet mesh. For different spacing and phasing of planets, matrices have special features that simplify the instability conditions. Note the following analysis considers mesh stiffness of any waveform as represented by the Fourier coefficients *a, b* in (32). As the most appropriate analytical idealization for spur gears, rectangular waveforms (5) are used to get simplified expressions and investigate the effects of contact ratio and phasing.

### Equally Spaced Planets

For equally spaced planets (ψ_{n}*=2*π*(n-1)/N)*, the vibration modes have structured properties (8) and (9). In this case, *(z _{s}+z_{r})*/N = integer and the planet meshes have phasing ϒ

*and ϒ*

_{sn}=(n-1)z_{s}/N*. The two possible phasing conditions are examined below.*

_{rn}=-(n-1)z_{r}/N, n=1,…,N#### (1) In-phase Planet Meshes

Consider the case when all the sun-planet meshes are in-phase (ϒ* _{sn}=0, n=1,…,N)* and all the ring-planet meshes are in-phase (ϒ

*This design is typical when optimizing load sharing among planets and results when*

_{rn}=0, n=1,…,N).*z*and

_{s}*z*are each integer multiples of

_{r}*N*. There is, however, a constant phasing ϒ

*between the sun-planet and ring-planet meshes for each planet. The Fourier coefficients*

_{sr}*in (4) and (32) are independent of the planet index*

*n*for in-phase planet meshes.

For a distinct natural frequency ω* _{p}*, vibration mode property (8) leads to

*for any planet*

*n*. Using rectangular form (5) and (32) in (16), the primary instability boundaries are governed by

(33)

Obviously, * = 0 when **c _{s}, c_{r}* are integers and all instabilities vanish. If

*c*integer, a second choice to reduce the instability regions is to make the third term in (33) negative by adjusting

_{s}, c_{r}*c*, and ϒ

_{s}, c_{r}*. The combination instability boundaries for two distinct modes can be obtained from (17).*

_{sr}For the degenerate natural frequencies ω* _{3}=…=*ω

*, vibration mode property (9) results in*

_{N+1}(34)

where the following identities are used to derive (34)

(35)

Use of (34) in (32) gives

(36)

For the simple form of * in (36), the eigenvalues of (30) can be expressed in closed-form for any multiplicity **m=N-1*. In this case, the single-mode instability boundaries are the same as (23) with * . For the rectangular waveforms (5),*

(37)

Equation (37) applies for any number of planets *N*.

For the combination instability of degenerate ω* _{3}*=…=ω

*and distinct ω*

_{N+1}*, use of properties (8) and (9) in (32) yields*

_{r}(38)

where C* _{i}* and β

*are constants independent of*

_{i}*n*. For in-phase planet meshes

*(z*are integers) and

_{s}/N, z_{r}/N*l=1*, (35) guarantees

*=0 and similarly*

*=0. It follows from (31) that the combination instabilities (*

*l=1*) of a distinct mode and a degenerate mode

*always*vanish for any

*N*when the planet meshes are in-phase. A more general condition for vanishing of these combination instabilities is that each of

*(lz*integer.

_{s}±1)/N, (lz_{r}±1)/NAs an example, Figure 3 shows the instability boundaries for a planetary gear with three equally spaced planets. The parameters and nominal natural frequencies are given in Table 1 and the vibration modes are shown in Figure 4. The mesh phasing ϒ* _{sn}=*ϒ

*, ϒ*

_{rn}=0*and the contact ratios c*

_{sr}=1/2*=1.4, c*

_{s}*=1.6. We specify ε*

_{r}*=ε*

_{1}*=ε (that is, g=1). The slight downward drift in the instability regions results from natural frequencies frequency changes as ε varies, which occur because the average mesh stiffnesses depend on k*

_{2}*and k*

_{vs}*; (the central line between the peak-to-peak mesh stiffnesses in (Figure 2) are kept constantsheld constant) in the example (Figure 2). The analytical solutions (solid lines) from (16), (17), (23), and (28) agree well with the numerical solutions using Floquet theory and numerical integration. Note the combination instabilities at ω*

_{vr}*+ω*

_{2}*, ω*

_{3}*+ω*

_{3}*vanish because they involve the distinct (ω*

_{5}*,ω*

_{2}*) and degenerate (ω*

_{5}*=ω*

_{3}*) natural frequencies. Figure 5 shows the primary instability regions for different contact ratios c*

_{4}*, c*

_{s}*; the stiffness variation amplitude ε*

_{r}*=0.3*and phasing ϒ

*. All instabilities vanish when the contact ratios are integers. The size of the*

_{sr}=0*2*ω

*instability region is primarily affected by*

_{2}*c*while insensitive to changes in

_{r}*c*. This is because the dominant deformation of mode φ

_{s}*occurs in the ring-planet meshes (Figure 4). The*

_{2}*2*ω

*instability region is mostly affected by*

_{5}*c*because most deformation occurs in the sun-planet meshes for this mode. The primary instability of the degenerate modes at

_{s}*2*ω

*ω*

_{3}=2*is influenced by both*

_{4}*c*and

_{s}*c*. The primary instability regions are maximized for

_{r}*c*, which is expected from (33) and (37). The relative phasing ϒ

_{s}=c_{r}=1.5*between the sun-planet and ring-planet meshes can have a major impact. When the phasing ϒ*

_{sr}*( Figure 5), the*

_{sr}=1/2*2*ω

*ω*

_{3}=2*instability vanishes for any*

_{4 }*c*because Γ

_{s}=c_{r}*in this case.*

^{(1)}=0 in (37)#### (2) Sequentially Phased Planet Meshes

Here we consider equally spaced planet systems where the sun-planet and ring-planet meshes are sequentially phased with ϒ_{sn}=(n-1)z_{s}*/N* and ϒ* _{rn}=-(n-1)z_{r} /N*. This case corresponds to

*z*integer but

_{s}/N, z_{r}/N*(z*=integer. A constant phasing ϒ

_{s}+z_{r})/N*exists between the sun-planet and ring-planet meshes for each planet. Using (35) and the sequential phasing, the Fourier coefficients in (32) satisfy*

_{sr}(39)

when* lz _{s} /N, lz_{r} /N *are non-integer. Equation (39) applies for any waveform of mesh stiffness variation waveform.

For distinct natural frequencies ω* _{p}*, using

*and (39) in (32) yields*

*. It follows from (16) that the primary instabilities*

*(l=1)*of distinct modes

*always*vanish when the planets are sequentially phased. Physically, it means that these instabilities are not excited because the resultant modal excitations from the sun-planet and ring-planet meshes each are zero. The secondary instabilities

*(l=2)*of distinct modes also vanish when

*2z*are non-integer. Similarly, for combination instability

_{s}/N, 2z_{r}/N*(l=1)*of distinct ω

*and ω*

_{p}*,*

_{q}*in (17). Thus, combination instabilities of two distinct modes*

*always*vanish in this case.

For instabilities involving the degenerate modes, it is difficult to obtain simple expressions for the instability boundaries; their instability conditions can be calculated from (23), (30), and (31). A special case is the combination instability *(l=1)* of degenerate ω* _{3}*=…=ω

*and distinct ω*

_{N+1}*when*

_{r }*(z*each is non-integer. In this case,

_{s}±1)/N, (z_{r}±1)/N*because of (35) and (38), and the combination instabilities of distinct and degenerate modes vanish.*

*=**=0, p=3,…,N+1*Figure 6 shows the instability boundaries for the same system as in Figure 3 , except the three planets are sequentially phased with ϒ* _{sn}= [0, 1/3, 2/3],* ϒ

*Note the primary, secondary, and combination instability regions vanish for the distinct natural frequencies ω*

_{rn}= [0, -2/3, -1/3].*, ω*

_{2}*; only instabilities involving the degenerate modesω*

_{5}*=ω*

_{3}*exist.*

_{4}The above analyses show that contact ratios and mesh phasing significantly affect the operating condition instability regions. In practice, particular instabilities can be minimized by proper selection of contact ratios and mesh phasing, which are adjusted by center distance, diametral pitch, pressure angle, tooth addendum, numbers of teeth, and other parameters. The foregoing results for equally spaced planets and any mesh stiffness waveform (not just rectangular) are summarized in Table 2.

### Unequally Spaced Planets

When the planets are arbitrarily spaced, the structured modal properties do not exist and the general expressions for instability boundaries cannot be further simplified. For the practically important case of diametrically opposed planets, however, the vibration modes retain the well-defined properties (8) and (9). For the sun-planet meshes, each of the *N/2* pairs of diametrically opposed planets are in-phase *(*ϒ* _{s(n+N/2)} =*ϒ

*for even zs and counter-phased (ϒ*

_{sn})*=ϒ*

_{s(n+N/2)}*for odd*

_{sn}+1/2)*z*. An analogous rule applies for the ring-planet mesh phasing. Note that adjacent planets have arbitrary mesh phasing defined by their circumferential position, ϒ

_{s}*Ψ*

_{sn}=*/*

_{n}z_{s}*(2*π

*),*ϒ

*=-Ψ*

_{rn}

_{n}z_{r}*/(2*π

*)*,

*n=1,…,N/2.*

When the sun-planet and ring-planet meshes are both counter-phased (odd *z _{s}, z_{r}*), equation (39) holds for odd

*l*because

*and similar relations for*

*. Recalling modal property (8),*

*for distinct ω*

*, ω*

_{p}*and odd*

_{q}*l*. From (16) and (17), primary and combination

*(l=1)*instabilities of distinct modes

*always*vanish in the counter-phased case. Physically, these instabilities are eliminated because the modal excitations from each pair of diametrically opposed planets always cancel each other. The instability regions involving degenerate modes are obtained from numerical evaluation of the eigenvalues of (30).

When pairs of opposing sun-planet or ring-planet meshes are in-phase (even *z _{s}* or even

*z*), no simple expression for instabilities regions is available; numerical solutions are obtained from (16), (17), (30), and (31).

_{r}### Dynamic Response and Contact Loss

When planetary gears operate inside an instability region, damping and nonlinearities from friction, tooth separation, etc. bound the unstable linear model motion. Figure 7a shows the RMS steady-state planet response amplitude versus mesh frequency for the same system as in Figure 3 and the stiffness variation ε*=0.3*. Rayleigh damping **C***=(0.07)****M***+(0.07)****K** is added to system (1) and the force vector is **F***=[-2000 1000 0 0 0] ^{T} N*. The solutions are obtained from numerical integration of (10) using mesh stiffnesses in rectangular waveforms (Figure 7b). The instabilities near ω

*=ω*

_{3}*, 2ω*

_{4}*=2ω*

_{3}*, and ω*

_{4}*+ω*

_{2}_{5}grow to instability very slowly so that their parametric instabilities are not apparent in Figure 7a (and Figure 8a). The instability excited by the primary instability 2ω

*grows extremely large because tooth separation (that is, vanishing mesh stiffness) is*

_{5}*not*considered; the mesh stiffnesses are pre-specified functions of time (Figure 7b). In practice, tooth separation (clearance nonlinearity) occurs for large dynamic responses and its effects are dramatic. Figure 8a shows the response for the same system as in Figure 7a but tooth separations are modeled. The mesh stiffness k

*or k*

_{sn}*is set to zero if the corresponding tooth deformation δ*

_{rn}*<0 or δ*

_{sn}*<0 at any step of the integration. The response amplitude of the 2ω*

_{rn}*primary instability is*

_{5}*significantly*reduced from that in Figure 7a. Moreover, a softening jump phenomenon occurs. Sun-planet tooth separation (k

*=0) is apparent in Figure 8b for a mesh frequency in the primary instability region of 2ω*

_{sp}*. The interactions of mesh stiffness variation and clearance nonlinearity has been studied by Kahraman and Blankenship [19, 20] for single-mesh gears. Their effects on multi-mesh planetary gears need additional investigation.*

_{5}### Conclusions

This work analytically investigates the parametric instabilities from mesh stiffness variation in planetary gears. Instability boundaries are obtained for systems with equally spaced (summarized in Table 2) and diametrically opposed planets. The main points are:

1. Using the structured properties of vibration modes, the instability boundaries are reduced to simple, closed-form expressions for several planet phasing conditions. The instability boundaries are sensitive to contact ratios and mesh phasing, and the simple expressions are useful in design to suppress instabilities by adjusting these parameters.

2. Certain parametric instabilities always vanish for particular mesh phasing conditions, including (1) combination instabilities of distinct and degenerate modes when equally spaced planets are in-phase, (2) primary and combination instabilities of distinct modes when equally spaced planets are sequentially phased, and (3) primary and combination instabilities of distinct modes when diametrically opposed planets are counter-phased. These features come from the well-defined modal properties and apply to any form of mesh stiffness variation.

3. Instability boundaries relate directly to mesh deformations in the vibration modes. The mesh parameters (e.g, *c _{s} *and

*c*) that are most critical to a particular instability are those of the tooth meshes with dominant deformations in the unstable vibration modes.

_{r}4. When a parametric instability is excited under operating conditions, tooth separation occurs. This nonlinearity dramatically changes the dynamic response. More analysis is needed to reveal the interaction of mesh stiffness variation and backlash nonlinearity in multi-mesh gear systems.

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**Acknowledgment**

The authors would like to thank Timothy L. Krantz of the Army Research Lab at NASA Glenn Research Center for his support and advice on the project. This material is based upon work supported by the U.S. Army Research Office under grant DAAD19-99-1-0218.