## Encyclopedia of Physical Science and Technology, Volume 10 |

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Page 97

On a domain U in C , a meromorphic function F can be

continuous map of U into C = CU { 00 } ... the simplest examples , such as zı / 22 ,

show that indeterminate quotients 0 / 0 cannot be avoided , so the first

fails .

On a domain U in C , a meromorphic function F can be

**defined**either as acontinuous map of U into C = CU { 00 } ... the simplest examples , such as zı / 22 ,

show that indeterminate quotients 0 / 0 cannot be avoided , so the first

**definition**fails .

Page 326

Consider the case of one very simple property of a porous medium , its porosity (

w ) ,

regarded as a continuum , we must be able to

space .

Consider the case of one very simple property of a porous medium , its porosity (

w ) ,

**defined**as the ratio of the pore volume to the ... If a porous medium isregarded as a continuum , we must be able to

**define**its porosity at a point x inspace .

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

convolution of p ...

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 theconvolution of p ...

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### Contents

Seismology Observational 17 Stochastic Description | 325 |

Semiconductor Alloys LongRange and Karl Friedrich | 345 |

Sequency and Series 73 Solar Energy Engineering | 361 |

Copyright | |

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