## Encyclopedia of Physical Science and Technology, Volume 1 |

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Page 97

On a domain U in C, a meromorphic function F can_be

continuous map of U into C = C U {»} [with F-'(C) 4- 0], which is holomorphic on F"

'(C); or as a quotient fig, where /e sMJ) and g 6 si(t/)\{const. 0} have no common

zero.

On a domain U in C, a meromorphic function F can_be

**defined**either as acontinuous map of U into C = C U {»} [with F-'(C) 4- 0], which is holomorphic on F"

'(C); or as a quotient fig, where /e sMJ) and g 6 si(t/)\{const. 0} have no common

zero.

Page 326

that of the change of scale: at the microscopic pore scale the physics of the

interactions between fluid and solid are well understood and documented, but at

any larger scale, it is necessary to perform an integration in order to

that of the change of scale: at the microscopic pore scale the physics of the

interactions between fluid and solid are well understood and documented, but at

any larger scale, it is necessary to perform an integration in order to

**define**the ...Page 329

ume (p), we will similarly extend the

unit volume p (zero in the grains) to the entire space. But then p is discontinuous

at the solid-liquid interface. If (p) was simply

...

ume (p), we will similarly extend the

**definition**of the microscopic fluid mass perunit volume p (zero in the grains) to the entire space. But then p is discontinuous

at the solid-liquid interface. If (p) was simply

**defined**by the convolution of p by m,...

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#### Encyclopedia of physical science and technology

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### Contents

Daniel Hillel | 303 |

Seismology Observational 17 Stochastic Description | 325 |

Seismology Theoretical 47 Solar Chimneys | 335 |

Copyright | |

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