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22-Elec-A7 Electromagnetics · December 2013

Question 5 of 8: Circular Polarization from Two Crossed Current Elements

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format. National Examinations, December 2013 — 07-Elec-A7 Electromagnetics. Three hours, closed book, one approved calculator. Eight questions of equal value (20 marks each); the paper states that any five constitute a complete paper, but all eight are solved here so the set works as a complete study resource. Aids printed on the paper: $\epsilon_0 = 8.85\times10^{-12}$ F/m and $\mu_0 = 4\pi\times10^{-7}$ H/m.

Reference texts. Sadiku, Elements of Electromagnetics, 7th ed.; Hayt & Buck, Engineering Electromagnetics, 9th ed.; Ulaby & Ravaioli, Fundamentals of Applied Electromagnetics, 8th ed.; Pozar, Microwave Engineering, 4th ed.; Balanis, Antenna Theory: Analysis and Design, 4th ed.

Free-space quantities follow from the printed aids: $c = 1/\sqrt{\mu_0\epsilon_0} \approx 3\times10^{8}$ m/s and $\eta_0 = \sqrt{\mu_0/\epsilon_0} = 376.8\ \Omega$.

Question 5: Circular Polarization from Two Crossed Current Elements (20 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. Two co-located short current elements — one vertical, one horizontal along north–south — driven in quadrature with the vertical element carrying twice the current.

Given data
QuantitySymbolValue
Frequency$f$10 MHz
Free-space wavelength$\lambda$30 m
Element length (each)$l$1 m
Vertical element current$I_v$$2I$
Horizontal (N–S) element current$I_h$$I$
Relative phase$\Delta\varphi$$90^{\circ}$

Find. At least one direction of propagation in which the two radiated fields combine into a circularly polarised wave.

upESvertical element, 2IN-S element, I30°E rotates:circularray: 30° from verticalEqual amplitudes: 2 sin 30° = 1 sin 90° = 1Ray lies in the vertical E-W plane, 60° above the horizon
Figure 5.1 — The crossed elements and one direction giving circular polarization: 30° from the vertical, in the vertical east–west plane.

Approach. Circular polarization needs two orthogonal field components of equal amplitude in quadrature. The quadrature is already supplied by the currents, so the task reduces to finding a direction where the two $\sin\theta$ patterns equalise the amplitudes while the field directions stay perpendicular.

  1. Check the short-element approximation. At 10 MHz the wavelength is $\lambda = c/f = 30$ m, so each 1 m element is $\lambda/30$ long and the supplied formula $E = Z_0 I l k \sin\theta\,e^{-jkr}/(4\pi r)$, with $k = 2\pi/\lambda = 0.2094$ rad/m, applies. Both elements share the same $l$, $k$ and $r$, so only the products $I\sin\theta$ differ.
  2. Radiation patterns of the two elements. Each element radiates as $\sin\theta$ measured from its own axis, with the field lying along the local $\hat{\boldsymbol{\theta}}$ direction. Writing $\theta_v$ for the angle from the vertical and $\theta_h$ for the angle from the north–south axis,$$|E_v| \propto 2I\sin\theta_v,\qquad |E_h| \propto I\sin\theta_h .$$
  3. Equal-amplitude condition. Circular polarization demands the two components be equal in magnitude:$$2\sin\theta_v = \sin\theta_h .$$The right-hand side can be at most 1, so $\sin\theta_v \leq 1/2$: the direction must lie well away from the horizon, where the stronger vertical element would otherwise dominate.
  4. Choose the convenient solution. Take the equality case $\sin\theta_h = 1$, which means the direction is perpendicular to the north–south element, i.e. it lies in the vertical east–west plane. Then$$\sin\theta_v = \tfrac{1}{2}\;\Longrightarrow\;\theta_v = 30^{\circ}\ \text{from the vertical},$$so the ray sits 60° above the horizon, pointing east (or west).
  5. Confirm the two fields are orthogonal. Along that ray $\hat{\mathbf{r}} = (\sin 30^{\circ},\,0,\,\cos 30^{\circ})$ in (east, north, up) coordinates. The vertical element radiates a field in the plane of $\hat{\mathbf{z}}$ and $\hat{\mathbf{r}}$ — the vertical east–west plane — while the north–south element, being perpendicular to $\hat{\mathbf{r}}$, radiates a field along $\hat{\mathbf{y}}$ (due north). Those two directions are at right angles, so the components are genuinely orthogonal:$$\mathbf{E}_v \cdot \mathbf{E}_h = 0 .$$
  6. Combine. Equal magnitudes ($2\sin 30^{\circ} = 1\cdot\sin 90^{\circ} = 1$ in units of $Z_0 I l k/4\pi r$), perpendicular directions, and the $90^{\circ}$ current phase difference carried straight through to the fields: the tip of the total E vector traces a circle. Hence$$\boxed{\theta = 30^{\circ}\ \text{from the vertical, in the vertical E--W plane}}$$By symmetry the same holds due west, and for the two mirror directions 30° from the downward vertical, so there are four such rays in all. The sense (right- or left-hand) is set by the sign of the 90° phase and reverses between the eastward and westward rays.

Check: elements at the same point are assumed, so no path-length difference adds to the 90° current phase. The wave is elliptically polarised in every other direction; due east on the horizon, for example, the amplitude ratio is 2:1, giving an axial ratio of 2 (6 dB) rather than unity.

Final Results
QuantitySymbolValue
Free-space wavelength$\lambda$30 m
Wavenumber$k$0.2094 rad/m
Required amplitude condition—$2\sin\theta_v = \sin\theta_h$
Angle from the vertical$\theta_v$$30^{\circ}$
Angle from the N–S element$\theta_h$$90^{\circ}$
One direction giving circular polarization—due east, 60° above the horizon
Total number of such directions—four (east/west, above/below the horizon)