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International Journal of Antennas and Propagation

Volume 2012 (2012), Article ID 540649, 14 pages

http://dx.doi.org/10.1155/2012/540649

## Correlation and Capacity Calculations with Reference Antennas in an Isotropic Environment

Consultant, Azimuth Systems, Inc., 35 Nagog Park, Acton, MA 01720, USA

Received 5 January 2012; Revised 10 March 2012; Accepted 21 March 2012

Academic Editor: Moray Rumney

Copyright © 2012 Thorkild B. Hansen. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

#### Abstract

A reverberation chamber is a convenient tool for over-the-air testing of MIMO devices in isotropic environments. Isotropy is typically achieved in the chamber through the use of a mode stirrer and a turntable on which the device under test (DUT) rides. The quality of the isotropic environment depends on the number of plane waves produced by the chamber and on their spatial distribution. This paper investigates how the required sampling rate for the DUT pattern is related to the plane-wave density threshold in the isotropic environment required to accurately compute antenna correlations. Once the plane-wave density is above the threshold, the antenna correlation obtained through isotropic experiments agrees with the antenna correlation obtained from the classical definition, as has been proven theoretically. This fact is verified for the good, nominal, and bad reference antennas produced by CTIA. MIMO channel capacity simulations are performed with a standard base station model and the DUT placed in a single-tap plane-wave reverberation chamber model. The capacity curves obtained with the good, nominal, and bad reference antennas are clearly distinguishable.

#### 1. Introduction

The reverberation chamber [1] is a cost-efficient and convenient tool for creating an isotropic environment in which wireless devices can be tested. The field in a rectangular reverberation chamber can be described in terms of chamber modes that each can be expressed as a sum of eight plane waves [2, 3]. The chamber typically contains a mode stirrer and a turn table on which the device under test (DUT) rides. At any fixed turntable and stirrer position, the DUT sees a certain collection of plane waves. By rotating the stirrer and turntable, a new collection of plane waves illuminates the DUT (the turntable causes the DUT to see each plane wave from different angles). The isotropic test environment is thus achieved by rotating both the stirrer and turntable to illuminate the DUT with many different collections of plane waves. One can determine if a given reverberation chamber at a given frequency is isotropic by evaluating anisotropy coefficients obtained from three-axis dipole experiments [23, Annex J] and [4].

In the present paper we investigate the use of reverberation chambers for over-the-air testing of MIMO devices. Both antenna correlation (a quantity that is critically important for MIMO system performance) and MIMO capacity will be simulated in a plane-wave reverberation chamber model [5–9]. The simulations will be performed with a pair of Hertzian dipoles and with good, nominal, and bad reference antennas [10]. The classical antenna correlation is compared to the isotropic antenna correlation, and it is verified numerically that the two are equivalent, as proven by De Doncker and Meys [11].

To ensure accurate and reliable over-the-air test results, the test system must produce an accurate test environment in the entire physical region that contains the DUT. For example, in conventional 2D anechoic tests, the number of antennas in the ring surrounding the DUT must be large enough to accurately reproduce the desired channel conditions in the region occupied by the DUT. Similarly, the reverberation chamber must be large enough to supply enough plane waves to achieve an isotropic environment in the region occupied by the DUT.

By expressing the DUT pattern in terms of a spherical expansion (with a recently derived formula for truncation limit), we determine how closely the DUT pattern must be sampled to properly capture its variation. Using this sampling rate, we obtain rules that determine both the required number of antennas in the anechoic test and the required plane-wave density in the reverberation chamber test. As a byproduct of this investigation, we present accurate Fourier expansions of the DUT pattern that have been used in spherical near-field scanning for many years but appear to be relatively unknown in wireless communications.

The paper is organized as follows. Section 2 introduces the truncated spherical-wave expansion and derives the sampling theorems and Fourier expansions for the pattern of an arbitrary DUT. Section 3 deals with antenna correlations in both the reverberation chamber test and in a 2D anechoic chamber test. This section also relates the accuracy of simulated correlations to the sampling rate required for the pattern. In Section 4 we investigate the plane-wave distribution for realistic reverberation chambers by using the dyadic Green’s function for the rectangular box. We further simulate antenna correlations and compute anisotropy coefficients. Section 5 presents MIMO channel capacity simulations using a standard base station model and the plane-wave reverberation chamber model. Section 6 presents conclusions. Throughout, we assume time-harmonic fields that have time dependence with .

#### 2. Plane-Wave Receiving Characteristic and Far-Field Pattern

In this section we introduce the plane-wave receiving characteristic and far-field pattern of an arbitrary DUT-mounted antenna. (The term “pattern’’ will be used to refer to both the plane-wave receiving characteristic and to the far-field antenna pattern). A spherical expansion determines the spatial sampling rate required to “capture’’ the pattern of the antenna and provides a Fourier series expansion useful for computing any quantity involving the pattern. The standard spherical coordinates with unit vectors given by will be used throughout. Here, the unit vectors for the rectangular coordinates are , , and . Note that with and covers the unit sphere once. Figure 1 shows the spherical coordinates.

The DUT with a mounted antenna is shown in Figure 2 inside the minimum sphere with radius , defined such that the maximum value of the coordinate for all points on the DUT equals . Note that depends not only on the size of the DUT but also on its location with respect to the coordinate system. For example, a Hertzian dipole located at has despite the fact that its physical extent is vanishing. Also, even if the physical dimension of a DUT-mounted antenna is much smaller than the dimensions of the DUT (as in Figure 2), the antenna interacts with the DUT and therefore it is the entire DUT size that must be used when computing .

The plane-wave receiving characteristic is defined as follows. Assume that the incident plane wave with propagation direction illuminates the DUT. The direction of propagation is , and the constant vector satisfies . With this notation, the incident plane wave “comes’’ from the direction . For example, if , the plane wave is and propagates in the direction of the negative -axis. When the DUT is illuminated by this plane-wave field, its output is by definition , where is the plane-wave receiving characteristic satisfying .

If the DUT-mounted antenna satisfies reciprocity, its plane-wave receiving characteristic can be expressed in terms of its normalized far-field pattern as [12, equation (6.60)] (The spherical angles determining the plane-wave directions of propagation in [12] are different from those used in the present paper): where and are the free-space permeability and permittivity, respectively. Moreover, is the wavenumber and is the characteristic admittance of the propagating mode of a wave-guide feed assumed attached to the DUT antenna; see [12, Chapter 6]. In general, if the antenna is not reciprocal, the receiving characteristic can be related to the pattern of an adjoint antenna [13].

The electric far field of the DUT, when it is fed by an input voltage-amplitude , is [12, equation (6.35)] (The nonnormalized far-field pattern is defined in [12, equation (3.31)] in terms of the electric field through the limit . The normalized far-field pattern is in turn defined by , where is the input voltage amplitude of the signal that feeds the antenna. Note that the symbol “*~*’’ in (3) means “asymptotically equal to’’ in the limit .)
The far-field pattern determines the far field in the direction whereas determines the output due to a plane wave “coming in’’ from the direction . Hence, this incident plane wave propagates in the direction . Also, the normalized far-field pattern is dimensionless and the plane-wave receiving characteristic is a length.

These statements fully define the plane-wave receiving characteristic for any propagating plane wave that may illuminate the DUT. If the source of the incident field is close to the DUT, one must also specify the plane-wave receiving characteristic for evanescent plane waves [12, Chapters 3 and 6]. However, in this paper we consider only sources that are at least a few wavelengths away from the DUT so that evanescent waves are negligible.

Using (2) in conjunction with standard spherical-wave theory [14, 15] shows that the receiving characteristic can be expressed in terms of the transverse vector-wave functions and as where and are spherical expansion coefficients satisfying and when . The truncation number is determined from the radius of the minimum sphere as where the constant determines the number of digits of accuracy achieved [16, Section 3.4.2] and “int’’ denotes the integral part. The formula (5) is especially useful for small sources where the second term is on the same order of magnitude as the first term. (In older literature the following truncation formula is often used with the second term left unspecified: “ where is a small integer.’’)

The transverse vector-wave functions can be expressed in terms of the spherical harmonic [15, page 99] as [15, pages 742–746] and . The orthogonality relations [15] for the transverse vector-wave functions give the following well-known expressions for the spherical expansion coefficients and : where indicates complex conjugation. The formula (4) makes it possible to compute the plane-wave receiving characteristic in any direction from the spherical expansion coefficients and . However, in this paper we shall use (4) to derive Fourier expansions and sampling theorems that are useful for computing quantities like correlations that involve the plane-wave receiving characteristic.

The expressions for the transverse vector-wave functions and show that the and components of in (4) have the Fourier series (The expressions [15, page 98] for the associated Legendre function show that both the derivative and the fraction can be expanded in terms of with .): where and are Fourier coefficients. The Fourier expansions (8) define functions that are periodic in both and . Hence, the Fourier coefficients cannot be determined from the sampling theorem for periodic spatially bandlimited functions when is known only over the standard sphere , . We shall overcome this problem by continuing to the interval (see [17, 18], and [19, pages 111–113, 140–144]).

Since , the two points and correspond to the same point in space. Moreover, since the tangential spherical unit vectors satisfy and , we can analytically continue into a periodic in both and by use of One can show that the conditions (9) imply that the Fourier coefficients satisfy and .

Assume that and are known over the standard sphere , at , and , , where the sample rates are and , with and . Then the Fourier coefficients can be computed from the sampling theorem for periodic spatially bandlimited functions in conjunction with (9) as [19] and [20, Section IV]: Of course, (10) hold only for functions that satisfy (9). We summarize the results (which also hold for the antenna pattern ) as follows.(i)The plane-wave receiving characteristic should be sampled over the sphere and at a rate of at least , where , given by (5), depends on frequency, physical DUT size, and DUT location.(ii)The plane-wave receiving characteristic can be expressed in terms of the Fourier series (8) with Fourier coefficients computed through (10) from sampled values of .(iii)Integrals of the form where is a known function, occur in many places. For example, the expressions (7) for the spherical expansion coefficients have this form. Such integrals can be computed accurately by inserting the Fourier expansions (8) for . One can often compute the contribution from each Fourier term explicitly. Alternatively, by use of the Fourier series one can resample to a finer grid and then compute through numerical integration.(iv)In contrast, brute-force approximations of the form (with the original sampling rate retained) are often inaccurate, especially when the sampling is sparse (the antenna is electrically small). The lack accuracy is caused by the fact that the integral over does not involve a periodic spatially bandlimited function, so the trapezoidal rule is not guaranteed to work well [19, pages 111–113, 140–144, 372].

#### 3. Antenna Correlation in Isotropic Environment

In this section we describe the concept of antenna correlation in an isotropic environment like the one observed in a reverberation chamber. However, first we state the classical definition of antenna correlation in terms of the plane-wave receiving characteristics introduced in Section 2.

Consider two receiving antennas, possibly mounted on the same DUT, with plane-wave receiving characteristics and . The classical definition of the correlation between the two receiving antennas is In accordance with Section 2, the correlation (13) can be computed by inserting Fourier series expansions for and with Fourier coefficients obtained from sampled values.

A general specification of the isotropic environment can be found in Hill’s book [1, Section 7.1] and in the paper by De Doncker and Meys [11]. Here we consider a specific embodiment [5–9] involving plane waves propagating in a set of fixed directions. The points , , are roughly evenly distributed on the unit sphere as shown in Figure 3. More specifically, the points are on constant rings with the number of points on each ring dependent on . In particular, the top and bottom rings and consist of just one point each.

Assume that two plane waves are incoming in each of the directions . One of them is polarized with amplitude ; the other is polarized with amplitude , where . For a particular , the incident field is thus given by where , , and are the spherical unit vectors evaluated at . The plane-wave amplitudes and are uniformly distributed independent complex random variables with zero mean, and the corresponding outputs of the two receiving antennas are The isotropic environment is obtained as the collection of incident fields for , with a new set of amplitudes and selected for each . Thus, we can compute the outputs and for each of the two receiving antennas for . Section 5 presents MIMO capacity simulations with a receiving DUT placed in this isotropic environment.

It was shown by De Doncker and Meys [11] that the correlation between the outputs and in the isotropic environment is equal to the classical correlation (13): We shall now demonstrate through numerical simulations that this result is indeed correct and investigate the sampling rate (density of incident plane waves) required in the isotropic environment to make (16) accurate.

##### 3.1. Two Hertzian Dipoles

Consider two -directed Hertzian dipoles on the axis at and so that the radius of the minimum sphere is ; see Figure 4. The output of a Hertzian dipole is proportional to the incident electric field in the direction of the dipole. Hence, where is a constant length. The correlation between the dipoles is found from (13) to be Hill [1, equation (7.63)] confirms the general result (16) that the classical correlation (18) is the correlation obtained in an isotropic environment.

We compute the correlation from (16) for and with varying . Throughout, . As a measure of the density of incident plane waves, we use the “isotropic’’ spacing between constant rings on the unit sphere. Specifically, if there are constant rings (including the two at and ), we have .

Unlike the points with and spacing used in computing the Fourier coefficients in Section 2, the points do not lie on a rectangular grid. Hence, the number of plane-wave directions of incidence in the isotropic environment (denoted by ) is smaller than the number of grid points used to compute the Fourier coefficients in Section 2, even if .

Figure 5 shows the error: where is the exact correlation (18) and is the correlation obtained from the isotropic environment, as a function of . We set in the computation of in (5) and use .

For both and , the error becomes negligible when the ratio is about 0.7. In other words, accurate correlations are obtained when the isotropic sampling distance is about 1.4 times the sampling distance required to compute the Fourier coefficients in Section 2 with (). It is not surprising that accurate correlations are obtained in the isotropic environment when since the correlation (13) is an “average-over-an-entire-sphere’’ quantity whereas the expression for is derived to achieve the more demanding “point-by-point’’ accuracy.

To accurately reproduce the isotropic field conditions in a reverberation chamber, one must choose a chamber size large enough to ensure enough plane-wave directions of incidence for a given DUT size. We also note that these numerical simulations validate the general theorem by De Doncker and Meys [11].

Before leaving this section we investigate the sampling required for a 2D configuration where the correlation is based on incident fields from a small region of the unit sphere. This type of model will be used in Section 5 to simulate a transmitting base station that broadcasts according to a Laplacian distribution.

The two directed Hertzian dipoles are still on the axis at and as shown in Figure 6. The dipoles are now illuminated by a collection of plane waves that all propagate in the plane. 180 directions of incidence are selected according to the approximate Laplacian distribution [21, equation (18)] with centered on , as indicated in Figure 6. At any instant, each of the 180 plane waves is multiplied by a random phase to create a particular incident field. We achieve 10000 different incident fields by applying 10000 independent sets of random phases. The outputs and are thus obtained for , and the exact correlation in this experiment is .

We also compute an approximate correlation based on a fixed set of equally spaced directions of incidence illustrated by the ring in Figure 6. The angular spacing between two directions of incidence on this ring is . We simply replace the directions of incidence from the Laplacian distribution by the closest direction of incidence on this ring. The sampling theorem derived in Section 2 states that the angular spacing between these directions of incidence should be with computed from (5).

Figure 7 shows the error of the approximate correlation as a function of the ratio . We see that the error in this case with a limited range of directions of incidence only vanishes when is roughly equal to the spacing required by the sampling theorem. Hence, to accurately reproduce the model-specified field conditions in an anechoic-chamber tests system consisting of a ring of antennas, one must supply enough antennas to satisfy the sampling theorem.

##### 3.2. CTIA Reference Antennas

To expedite the baseline between laboratories participants of CTIA LTE round robin, a set of MIMO 2 × 2 reference antennas has been developed [10]. A subset of these antennas has dimension mm and operate at 751 MHz corresponding to mand . Hence, (5) gives when , and the required sampling is therefore .

We compute the isotropic correlation with 180 plane-wave directions of propagation corresponding to an isotropic sampling of . Table 1 shows the resulting correlations for three antennas: (i) good antenna with low correlation, (ii) nominal antenna with average correlation, and (iii) bad antenna with high correlation. The table validates the general theorem by De Doncker and Meys [11] in (16).

These results have also been verified experientially in a reverberation chamber at NIST [5–9].

#### 4. Isotropic Environment of a Rectangular Reverberation Chamber

A reverberation chamber provides a rich scattering environment that is ideal for over-the-air testing of wireless devices. The chamber typically contains a number of wall-mounted transmitting antennas, a mechanical mode stirrer, and a turntable on which the DUT is placed; see Figure 8. The turntable provides so-called platform stirring [22]. As we shall see, at any given position of stirrer and turntable, the DUT is illuminated by a large number of plane waves whose directions of propagation are determined by the modes of the chamber [1, 2]. We assume that the chamber is excited by a Hertzian dipole with frequency (as usual ).

##### 4.1. Modes in Terms of Plane Waves

Let the rectangular chamber have the dimensions , , and as shown in Figure 8. The dyadic Green’s function (field due to a Hertzian dipole source) can be expressed as a superposition of modes determined such that the tangential electric field vanishes on the chamber walls [3, pages 383-384]. Specifically, each rectangular field component can be expressed as a sum of terms of the form (we use the component for illustration purposes; the and components have similar expressions): where is independent of the observation point but dependent on the source location , the source strength, and the mode indices , , and , which can take on any nonnegative value.

There is one additional term (called an irrotational mode) that goes with the mode in (20) to ensure that the field satisfies the wave equation with wave number that corresponds to the medium in the chamber. The irrotational mode has an identical plane-wave representation, so analyzing (20) is sufficient. Also, the sum over can be performed in closed form to obtain a formula that involves just a double sum [3, page 384] and [1, page 34]. As usual, all losses (including wall losses) are accounted for by an effective lossy medium [3, page 389] and [1, page 35].

We associate a frequency and a propagation constant with each mode: where , , and . Note that and to convert (20) to where “7 more terms’’ indicate that the square bracket contains seven additional terms of the form . Hence, each mode can be expressed as the sum of eight plane waves with propagation vectors . The excitation factor can be written as where is independent of frequency and is the quality factor that accounts for wall and other losses in the chamber. is related to the RMS power delay time through . The 8 directions of incidence for a single mode are with the corresponding mode frequency given by (21).

The magnitude of the excitation factor (normalized) as a function of mode frequency for a 750 MHz driving signal and a 30 ns RMS delay is shown in Figure 9. We see that this factor has a peak at the diving frequency and that it falls off fairly slowly away from this frequency. For a chamber to work well, it must support a significant number of plane waves, which translates into the requirement that there must be a significant number of modes in the region where the excitation factor is significantly nonzero. One typically sets the threshold point where modes are considered “un-excitable’’ at the point where the excitation factor has fallen 3 dB. Notice that the width of the excitation factor depends on the quality factor. One of the benefits of using multiple wall-mounted transmitting antennas is that all excitable modes do actually get excited.

Let us now show the actual plane-wave directions of incidence for two reverberation chambers with 30 ns RMS delay that are driven by a 750 MHz source. One is electrically large (m, m, and m) at 750 MHz; the other is electrically small (m, m, and m) at 750 MHz. We include modes that lie in a 50 MHz band around 750 MHz. Figure 10(a) shows the plane-wave directions of incidence for the large chamber. The directions of incidence are nonuniformly distributed over the unit sphere with a maximum distance between points of and an average distance of . The largest gaps occur near the north and south poles.

As the stirrer in the reverberation chamber rotates, the amplitudes and phases of the plane waves change to produce an isotropic environment as discussed in the previous section. In addition to the stirrer, the chamber contains a turntable on which the DUT rides. As the turntable rotates, the DUT sees the plane waves from different angles, effectively creating additional directions of incidence. Figure 10(b) shows all the directions of incidence (see from the point of view of the DUT) for a turntable that rotates around a directed axis, as illustrated in Figure 8. The turntable thus multiplies the effective number of plane waves available. Of course, only plane waves corresponding to a single rotated version of Figure 10(a) are available at any instant.

Figure 11(a) shows the plane-wave directions of incidence for the small chamber. The directions of incidence are sparsely distributed with a maximum distance between points of and an average distance of . There are large gaps throughout the unit sphere. Figure 11(b) shows all the directions of incidence (see from the point of view of the DUT) for the turntable in Figure 8. Again, only plane waves corresponding to a single rotated version of Figure 11(a) are available at any instant.

##### 4.2. Correlation Simulations

Let us now investigate how these reverberation chambers perform when evaluating the correlation between the two directed Hertzian dipoles in Figure 4. The exact correlation is given by (18), and the error in (19) for the large chamber is shown in Figure 12 as a function of dipole separation. The “turntable off’’ simulation is performed by randomly changing the phase and amplitude of incident plane waves with directions of incidence in Figure 10(a) (the plane waves are given by with given by (25) and ). The “turntable on’’ simulation is performed by repeating the “turntable off” simulation with the plane-wave directions of incidence rotated by a fixed amount. In other words, the “turntable on’’ simulation accurately replicates the actual situation encountered by the DUT in a real reverberation chamber where only one set of plane waves (corresponding to a rotated version of the plane waves for a fixed DUT orientation) is available at any given instant. Figure 12 demonstrates that the turntable dramatically improves the accuracy of the computed correlation between the dipoles. This improved accuracy is achieved by illuminating the two dipoles from additional directions.

The error in (19) for the small chamber is shown in Figure 13 as a function of dipole separation. With the sparse coverage of plane-wave directions of incidence (Figure 11(a)), the correlation obtained with the turntable off is very inaccurate. The error is above 0.3 for certain values of the dipole separation. Remarkably, with the turntable on, the error falls dramatically to an almost tolerable level.

##### 4.3. Anisotropy Coefficients

One of the most important statistical properties of the field in the chamber is the degree to which it is isotropic, that is, how evenly distributed are the directions of propagation and polarizations of the incoming plane waves at the location of the DUT. With the isotropy test developed by the international standards committee (ICE) [23], field anisotropy coefficients measure the bias of the average direction of polarization of the electric field in the chamber. The bias is computed by comparing three components of the electric field obtained from dipole-antenna measurements. The degree of isotropy of an actual chamber is determined by comparing the observed and ideal (known from theory) distributions of the anisotropy coefficients. We shall next compute the anisotropy coefficients for the large and small reverberation chambers introduced above.

Three orthogonal components of the electric field recorded at the location of the DUT are required to compute the field anisotropy coefficients [23]: where and denote the three orthogonal directions. The quantity is the net input power (forward minus reflected) injected into the chamber, and is an index that determines the position of the turntable, the position of the mechanical stirrer, and the active transmit antenna. In addition to the three anisotropy coefficients defined by (26), the test in [23] also employs a total anisotropy coefficient that we shall not investigate here. For a perfectly isotropic chamber, is uniformly distributed between −1 and 1. Pages 195 and 196 of [23] show plots of anisotropy coefficients for well-stirred and poorly stirred reverberation chambers.

When the DUT is placed near the edge of the turntable in Figure 8, the three relevant orthogonal directions for the isotropy test are (i) the direction normal to the turn table, (ii) the direction tangential to the edge of the turntable, and (iii) the direction radial to the turntable. Hence, in a standard cylindrical coordinate system centered on the turntable, and can take the values , , and .

Figures 14 and 15 show the histograms for the anisotropy coefficients of the large (m, m, and m) and small (m, m, and m) reverberation chambers (both with the turntable active). We see that the anisotropy coefficients for the large chamber closely follow a uniform distribution, whereas the anisotropy coefficients for the small chamber show a significant deviation from a uniform distribution. We conclude that the small chamber does not produce enough plane waves, even though the turntable is active.

##### 4.4. Remarks

We have now described the plane-wave environment in a reverberation chamber using the mode expansion of the dyadic Green’s function for the rectangular box. We have seen how the plane-wave directions of incidence as seen from the DUT depend on the dimensions of the chamber and on whether or not a turntable is active. Through numerical simulations, we evaluated the accuracy of correlation experiments in the chamber. It would be nice to have a theory that explicitly determined the accuracy of the chamber as a function of chamber dimension and chamber loading (quality factor ). Such a theory does not exist, and at the present moment the accuracy can only be determined by numerical simulations like the ones presented here. Moreover, if a precise theory existed, it would have to be fairly complicated because accuracy depends not only on mode density (which is largely determined by chamber volume [1, page 30]) but also on the actual plane-wave directions of incidence, which depend on all 3 rectangular chamber dimensions. For example, a large chamber may have a large “plane-wave gap’’ near the poles, which in turn can make it less accurate than a smaller chamber.

#### 5. MIMO Capacity Simulations

In this section we perform MIMO capacity simulations with a two-antenna DUT receiver in an isotropic environment. The transmitter is a standard two-antenna base station. We employ the good, nominal, and bad reference antennas described in Section 3.2 and show that they produce clearly distinguishable throughput curves. The approach taken in this section was inspired by [5–9].

A schematic of the channel model is shown in Figure 16. The base station employs two antennas separated by and radiating through a standard 3-sector pattern [24, page 9]. The voltage input amplitudes for the two base station antennas are denoted and . Each base station antenna broadcasts in the directions , according to the Laplacian distribution approximation [21, equation (18)] with . We have now complex numbers for base station antenna 1, and complex numbers for base station antenna 2,

In practice, the two-antenna 2D Laplacian base station output would be fed to the reverberation chamber through two or more wall antennas. The directions of propagation from the base station are thus distributed randomly into plane waves in the chamber, and the Laplacian distribution is not preserved. In other words, the chamber does not reproduce the Laplacian distribution. However, the correlation imposed on the two information streams by the base station is preserved. Further, one often feeds a reverberation chamber from a channel emulator that is programmed to produce advanced spatial channel models, which can include both Doppler spectra, long time delays (much longer than the one produced by the chamber alone), and specified directions of incidence. When such channel models are fed to the reverberation chamber, the channel model is said to be evaluated isotropically. In such situations, the specified directions of propagation dictated by the channel model are not preserved. However, if the emulator and reverberation chamber are adjusted properly, the time delays and Doppler spectra of the channel model are preserved in the chamber. The use of advanced channel models adds a lot of flexibility to the reverberation chamber as an over-the-air test tool.

Next we select a set of evenly distributed points , , on the unit sphere as described in Section 3 to obtain incoming plane-wave propagation directions for illuminating the DUT. For we compute a set of random permutations of the numbers given by . In addition, for , we compute two sets of uniformly distributed random variables and in the range from 0 to . The permutations facilitate the random pairing between point on the base station pattern and plane-wave directions of incidence. The variables and provide random phase adjustments for each pair.

We now have different propagation channels that result in the following DUT antenna outputs: which can be written in matrix form as where is the channel matrix. The corresponding channel capacities are where the superscript indicates the transpose complex conjugate, is the receiver noise, and the transmitter power.

Figure 17 shows the capacity curves as functions of the signal to noise ratio (SNR) for the good, nominal, and bad reference antennas computed with and . These curves are obtained by computing the mean capacity for varying SNR. The mean is taken over all propagation channels. To achieve a capacity of 7 bps/Hz, the three reference antennas require very different SNR values: the bad reference antenna requires an SNR of 19 dB, whereas the good reference antenna requires only an SNR of 13 dB. The difference in SNR between good and bad reference antennas is in this case 6 dB. Similarly, to achieve a capacity of 12.5 bps/Hz, the difference in SNR between good and bad reference antennas is 7 dB. Hence, the capacity curves are clearly distinguishable, thereby confirming the capability of the isotropic environment for over-the-air MIMO testing. However, given the large variation in correlation of the three antennas (see Table 1), it is no surprise that the capacity curves are very different. Most practical antennas would likely fall in the nominal category.

#### 6. Conclusions

We investigated the use of reverberation chambers for over-the-air testing of MIMO devices by examining antenna correlation and throughput in isotropic environments. A truncated spherical-wave expansion was used to derive sampling theorems and the Fourier expansions for the pattern of an arbitrary DUT. The required sampling rate of the pattern depends on the frequency, the physical size of the entire DUT (not just its antenna), and the relative location of the DUT to the spherical coordinate system.

Through numerical investigations involving Hertzian dipoles, it was shown how the sampling rate for the pattern determines the plane-wave density required in the isotropic environment to obtain accurate values for the correlation between antennas. It was also demonstrated that antenna correlation in the isotropic environment is equivalent to the classical definition of antenna correlation, as was proven theoretically by De Doncker and Meys [11]. In particular, the correlations computed for the CTIA reference antennas [10] in isotropic simulations agree with the correlations obtained from the classical definition.

Using the dyadic Green’s function for the rectangular box, we computed the plane-wave distribution for realistic reverberation chambers, which were in turn used in simulations of antenna correlations and anisotropy coefficients. No general theory that explicitly determined the accuracy of the chamber as a function of chamber dimension and chamber loading was found. Instead we explained how one can determine accuracy estimates through simulations.

We performed MIMO channel capacity simulations using a standard base station model and the DUT (employing the CTIA reference antennas) placed in a single-tap plane-wave reverberation chamber model. The capacity curves obtained with the good, nominal, and bad reference antennas were clearly distinguishable, as would be expected given the vast difference between the correlations of these antennas; see Table 1.

Hence, we conclude that isotropic tests performed in a reverberation chamber can distinguish between DUTs that employ the different CTIA reference antennas. It would be interesting to perform link-level simulations with multitap isotropic channel models to further investigate this over-the-air test method.

#### Acknowledgments

The author would like to thank R. J. Pirkl and K. A. Remley of the NIST for numerous helpful discussions. I. Szini of Motorola is thanked for providing the patterns for the reference antennas.

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