Integral formulas for transformation of potential field parameters in geosciences

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F49777513%3A23520%2F17%3A43929537" target="_blank" >RIV/49777513:23520/17:43929537 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.earscirev.2016.10.007" target="_blank" >http://dx.doi.org/10.1016/j.earscirev.2016.10.007</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.earscirev.2016.10.007" target="_blank" >10.1016/j.earscirev.2016.10.007</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Integral formulas for transformation of potential field parameters in geosciences

Popis výsledku v původním jazyce

In this article boundary-value problems of potential theory, that are required for transforming and continuing selected parameters of a potential field, are discussed. By the potential field parameters we understand the potential and its gradients (potential gradients) up to the third order. In particular, integral equations defined for a spherical boundary transforming potential gradients of different orders and continuing potential gradients of the same order through the 3-D space are reviewed and classified. This mathematical apparatus can be used for any harmonic potential, such as electric, magnetic or gravitational, under the assumption of its conservativeness, i.e., neglecting possible temporal variations. Integral transforms are discussed in context of geoscience applications, namely in terms of the Earth&apos;s gravitational field; however, the article can serve as a general reference for integral transforms of potential field parameters in any scientific or engineering area where potential fields are used

Název v anglickém jazyce

Integral formulas for transformation of potential field parameters in geosciences

Popis výsledku anglicky

In this article boundary-value problems of potential theory, that are required for transforming and continuing selected parameters of a potential field, are discussed. By the potential field parameters we understand the potential and its gradients (potential gradients) up to the third order. In particular, integral equations defined for a spherical boundary transforming potential gradients of different orders and continuing potential gradients of the same order through the 3-D space are reviewed and classified. This mathematical apparatus can be used for any harmonic potential, such as electric, magnetic or gravitational, under the assumption of its conservativeness, i.e., neglecting possible temporal variations. Integral transforms are discussed in context of geoscience applications, namely in terms of the Earth&apos;s gravitational field; however, the article can serve as a general reference for integral transforms of potential field parameters in any scientific or engineering area where potential fields are used

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

<a href="/cs/project/GA15-08045S" target="_blank" >GA15-08045S: Metody validace, zpracování a použití dat družicových misí v geodézii a geofyzice</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2017

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

EARTH-SCIENCE REVIEWS

ISSN

0012-8252

e-ISSN

—

Svazek periodika

164

Číslo periodika v rámci svazku

JAN 2017

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

23

Strana od-do

208-231

Kód UT WoS článku

000392777300009

EID výsledku v databázi Scopus

2-s2.0-85001968689