Practical_Antenna_Handbook_0071639586
A p p e n d i x A : U s e f u l M a t h 717 The other important point to take away from Eq. (A.3.6) is that the higher the frequency f of the sinusoidal driving force, the larger the coefficient of the acceleration terms in front of the sin or cos term. As we discuss in Chap. 3, electromagnetic radiation is caused by accelerated charges; it is clear from this equation that the propensity for EM radiation increases with increasing frequency f. A.4 Triangles In plane geometry we find three kinds of triangles, as shown in Fig. A.4.1: • Equilateral (where all three sides are of equal length) • Isosceles (where two sides are of equal length) • Scalene (where no two sides are the same length) All three types share a common trait: The sum of their three interior angles (a, b, and g) is always 180 degrees. We can also categorize triangles by their interior angles: • Acute (where no interior angle is 90 degrees or greater) • Right (where one interior angle is exactly 90 degrees) • Obtuse (where one interior angle is greater than 90 degrees) Right Triangles In a right triangle, one angle is always 90 degrees, so the sum of the other two angles must also be 90 degrees. The side opposite the right angle is perpendicular to neither of the other two sides, and it is always the longest side of the three; it is called the hypotenuse. If we place a right triangle on an x-y grid so that the two perpendicular sides are on the x and y axes as shown in Fig. A.4.2, the relative lengths of the sides and the three interior angles are related as shown in the figure. For a right triangle—and only for a right triangle—the square of the hypotenuse is equal to the sum of the squares of the other two sides: 2 2 2 h = a + b (A.4.1) a a a a a c Figure A.4.1 Types of plane triangles. a (A) Equilateral b (B) Isosceles b (C) Scalene
718 A p p e n d i x A : U s e f u l M a t h y hypotenuse h b Symbol indicating a right triangle a h 2 = a 2 + b 2 a = h sin b = h sin x Figure A.4.2 Right triangle relationships. so it follows that h = a 2 + b 2 and a = h 2 − b 2 and b = h 2 − a 2 (A.4.2) Sometimes it is helpful to think of the sides a and b as the projections of h onto the x and y axes, respectively. For instance, if the sun is directly overhead, a is the shadow projected by a stick having the length and orientation of h onto the ground directly beneath it. The sides and interior angles of a right triangle are related by the following equations: sin α = a h or a = h sin α (A.4.3a) sinβ = b h or b = h sin β (A.4.3b) For completeness, we list the following additional relationships in a right triangle: cosα = b h or b = h cosα (A.4.3c) cosβ = a h or a = h cosβ (A.4.3d)
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718 A p p e n d i x A : U s e f u l M a t h<br />
y<br />
hypotenuse<br />
<br />
h<br />
b<br />
Symbol indicating a<br />
right triangle<br />
<br />
a<br />
h 2 = a 2 + b 2<br />
a = h sin <br />
b = h sin <br />
x<br />
Figure A.4.2 Right triangle relationships.<br />
so it follows that<br />
h = a 2 + b 2 and a = h 2 − b 2 and b = h 2 − a<br />
2<br />
(A.4.2)<br />
Sometimes it is helpful to think of the sides a and b as the projections of h onto the x<br />
and y axes, respectively. For instance, if the sun is directly overhead, a is the shadow<br />
projected by a stick having the length and orientation of h onto the ground directly beneath<br />
it.<br />
The sides and interior angles of a right triangle are related by the following equations:<br />
sin α = a h or a = h sin α<br />
(A.4.3a)<br />
sinβ = b h<br />
or b = h sin β (A.4.3b)<br />
For completeness, we list the following additional relationships in a right triangle:<br />
cosα = b h<br />
or b = h cosα (A.4.3c)<br />
cosβ = a h<br />
or a = h cosβ (A.4.3d)