Download Arctic Gold (Stephen Coonts' Deep Black, Book 7) by Stephen Coonts, William H. Keith Jr. PDF

By Stephen Coonts, William H. Keith Jr.

ISBN-10: 0312946953

ISBN-13: 9780312946951

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 crew at table 3 hint the kidnapping again to the Russian mafiya, who've their attractions set at the gigantic reserves of oil that lie millions of ft lower than the ocean’s floor.

While Dean is distributed to the Arctic to rescue the hostages, the attractive Lia DeFrancesca penetrates a seriously guarded dacha at the seashores of the Black Sea. right here she learns the explosive fact approximately Russia and its Arctic oil—one which could rate Dean and his Deep Black group their lives…and force the world’s superpowers to the threshold of struggle.

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Additional resources for Arctic Gold (Stephen Coonts' Deep Black, Book 7)

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This mode describes a velocity modulation in the direction of motion. 33), the sound waves have frequency w = -Janok sin 7/J and speed s = w/k = Yanosin7/J. We see that this speed depends on the propagation direction, decreasing for the sound waves that propagate closer to the x-axis. The speed s vanishes and the respective modes become purely dissipative at 7/J = o. This behavior is different from the properties of sound waves in classical isotropic fluids, where the Galilean invariance prohibits any dependence of the sound on the angle between the wavevector and the flow direction.

Suppose that each particle represents a solid disk of radius Ro. The surfactant is continuously produced at rate J per unit time inside the particle and released into the liquid through a small hole located at the center of the disk bottom. This surfactant diffuses through the liquid with the diffusion constant D and modifies its surface tension. The capillary coefficient T, which gives the magnitude of the capillary force acting per unit length of the solid-liquid contact line, depends as T = To - J-LC on the local surfactant concentration c.

In reality, the pheromone concentration in the air close to the ground fluctuates because of the turbulence in the atmosphere. This can be taken phenomenologically into account by replacing the calculated concentration field c(r, t) with c(r, t)(l+c~(r, t)), where ~(r, t) is white noise of unit intensity and c is a parameter that specifies the mean amplitude of fluctuations. The ants sense the pheromone concentration in a thin air layer close to the surface (z -+ 0). e. tlC = l(k· V'c), where l is the distance between the left and right antennae and k is the unit vector with the components kx = sin () and ky = - cos ().

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Arctic Gold (Stephen Coonts' Deep Black, Book 7) by Stephen Coonts, William H. Keith Jr.


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