By Stephen Coonts, William H. Keith Jr.
Within the Arctic, American intelligence operatives are abducted whereas investigating Russian submarines—a consistent, covert presence underneath the ice caps. In Washington, ex-Marine Charlie Dean and his group at table 3 hint the kidnapping again to the Russian mafiya, who've their attractions set at the titanic reserves of oil that lie millions of toes lower than the ocean’s floor.
While Dean is shipped to the Arctic to rescue the hostages, the attractive Lia DeFrancesca penetrates a seriously guarded dacha at the beaches of the Black Sea. the following she learns the explosive fact approximately Russia and its Arctic oil—one which could rate Dean and his Deep Black workforce their lives…and force the world’s superpowers to the edge of conflict.
Read Online or Download Arctic Gold (Stephen Coonts' Deep Black, Book 7) PDF
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Extra resources for Arctic Gold (Stephen Coonts' Deep Black, Book 7)
Here, the integration reduces to multiplication by an observation surface area of 4πr2. The result is P= ∫∫ I (r )r 2dr sin(ϑ )dϑ dϕ = ρ 0Qˆ 2 2 ⋅ω . 12) Thus we find the relation I= P . 13) In practice, sound power is also expressed in decibels with reference to P0 = 10–12 W: LW = 10 log P . 14) These findings can be applied to any kind of small volume-moving sound source. 1. Sound power and sound power levels of typical sources Sound source Speech Human voice, maximal Grand piano Orchestra, fortissimo Aircraft at takeoff Sound power P/W 10–5 10–2 10–1 100 103–104 Sound power level Lw / dB 70 100 110 140 150–160 26 2 Sound sources Sound power levels are part of the characterization of sources.
By this approach, the scattering cross section is defined. For an incidence plane wave with intensity I0, the scattering cross section is (λ « a) Q= Ps . 19) In a more general approach, the theoretical model is based on superposition of the undisturbed incident field, p0, and the scattered wave, ps, p = p0 + ps 7 Plane wave approximation. 3 Scattering 43 =2 a 3 =2 a =2 a 5 Fig. 7. Sound scattering at a sphere with radius a (after (Morse and Ingard 1968)) ps must fulfil the boundary condition at the object’s surface.
Depending on the size of the objects compared with the wavelength, the scattered field has large amplitudes in the forward direction (“forward scattering”), in the reverse direction (“reflection”) or in any other direction following a specific distribution. The exact formulation and solution of the scattered field amplitude is a difficult problem, except in academic cases of objects such as spheres, cylinders, etc. An efficient strategy for addressing the problem in practical cases is to map the scattered field to an equivalent field created by a spherical scatterer.