FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2093120894> ?p ?o ?g. }

• W2093120894 endingPage "40" @default.
• W2093120894 startingPage "30" @default.
• W2093120894 abstract "The longitudinal electric field along the axis and the channel core conductivity of a straight, vertical lightning channel above ground has been calculated by using different return stroke models. The lightning channel is modeled by a negatively charged corona sheath that stretches around a thin, very conductive central core. It is commonly held that the majority of the leader charge is located within the corona sheath radius, which is of the order of meters, while the highly conductive channel core, with a diameter assessed at around 1 cm, in effect transports the whole of the axial current. An inhomogeneous channel line charge density generates as strong radial as well as vertical electric field inside the corona sheath. Transmission-line-type models and the generalized traveling current source model, representing the “engineering” return stroke models, are used for the calculation of the vertical field and the core conductivity in the channel. For the purpose of the present study only the influence of the charge in the corona sheath on the vertical electric field are taken into account while all other effects are neglected. For comparison purposes, the same channel-base current for all models is assumed. First, we calculated the vertical electric field along the axis on the channel. Knowing the axial current density profile along the channel determined by the particular return stroke model and the assumed channel core diameter, the core conductivity is calculated using simple scalar relationship. The conductivity is compared between the models and with the values found in the existing literature. It is concluded that all considered models give the maximum value of the core conductivity more or less in accordance with the predictions in the literature (of the order of 104 S/m). Some discrepancies (negative conductivity) are observed for two transmission-line-type models at the very bottom of the channel. They can be explained by the great amount of injected positive charge in zone 1 of the channel sheath and by the presence of the image charge, small changes in input parameters could diminished or avoid it. Due to the big charge accumulation near the ground the generalized traveling current source model gives greater discrepancies regarding negative conductivity at 25–35 m above ground. It is concluded that the removing of these discrepancies requires a more complex approach, the inclusion of the new physical mechanisms during the discharge (for example the magnetic field generated by the core current in the channel), that is a more accurate calculation of the channel discharge function. On the other hand our results are consistent with the 1 cm core diameter value found in the literature." @default.
• W2093120894 created "2016-06-24" @default.
• W2093120894 creator A5004723106 @default.
• W2093120894 creator A5014201292 @default.
• W2093120894 creator A5025656597 @default.
• W2093120894 creator A5038367669 @default.
• W2093120894 date "2014-08-01" @default.
• W2093120894 modified "2023-09-27" @default.
• W2093120894 title "Vertical electric field inside the lightning channel and the channel-core conductivity during discharge – Comparison of different return stroke models" @default.
• W2093120894 cites W1974567881 @default.
• W2093120894 cites W1977496415 @default.
• W2093120894 cites W1977620062 @default.
• W2093120894 cites W1984610292 @default.
• W2093120894 cites W1990565206 @default.
• W2093120894 cites W2007055985 @default.
• W2093120894 cites W2014545616 @default.
• W2093120894 cites W2032359864 @default.
• W2093120894 cites W2036991652 @default.
• W2093120894 cites W2039553597 @default.
• W2093120894 cites W2082308266 @default.
• W2093120894 cites W2082774835 @default.
• W2093120894 cites W2091386671 @default.
• W2093120894 cites W2093228035 @default.
• W2093120894 cites W2107353187 @default.
• W2093120894 cites W2115116327 @default.
• W2093120894 cites W2119401457 @default.
• W2093120894 cites W2141921834 @default.
• W2093120894 cites W2147642306 @default.
• W2093120894 cites W2154389969 @default.
• W2093120894 cites W2166422828 @default.
• W2093120894 doi "https://doi.org/10.1016/j.epsr.2014.02.026" @default.
• W2093120894 hasPublicationYear "2014" @default.
• W2093120894 type Work @default.
• W2093120894 sameAs 2093120894 @default.
• W2093120894 citedByCount "7" @default.
• W2093120894 countsByYear W20931208942015 @default.
• W2093120894 countsByYear W20931208942020 @default.
• W2093120894 countsByYear W20931208942021 @default.
• W2093120894 countsByYear W20931208942022 @default.
• W2093120894 crossrefType "journal-article" @default.
• W2093120894 hasAuthorship W2093120894A5004723106 @default.
• W2093120894 hasAuthorship W2093120894A5014201292 @default.
• W2093120894 hasAuthorship W2093120894A5025656597 @default.
• W2093120894 hasAuthorship W2093120894A5038367669 @default.
• W2093120894 hasConcept C119599485 @default.
• W2093120894 hasConcept C121332964 @default.
• W2093120894 hasConcept C127162648 @default.
• W2093120894 hasConcept C127413603 @default.
• W2093120894 hasConcept C131540310 @default.
• W2093120894 hasConcept C163258240 @default.
• W2093120894 hasConcept C178635117 @default.
• W2093120894 hasConcept C202374169 @default.
• W2093120894 hasConcept C2524010 @default.
• W2093120894 hasConcept C2776779350 @default.
• W2093120894 hasConcept C2779900269 @default.
• W2093120894 hasConcept C30475298 @default.
• W2093120894 hasConcept C33441834 @default.
• W2093120894 hasConcept C33923547 @default.
• W2093120894 hasConcept C38652104 @default.
• W2093120894 hasConcept C41008148 @default.
• W2093120894 hasConcept C57879066 @default.
• W2093120894 hasConcept C60799052 @default.
• W2093120894 hasConcept C62520636 @default.
• W2093120894 hasConcept C69398868 @default.
• W2093120894 hasConcept C87355193 @default.
• W2093120894 hasConceptScore W2093120894C119599485 @default.
• W2093120894 hasConceptScore W2093120894C121332964 @default.
• W2093120894 hasConceptScore W2093120894C127162648 @default.
• W2093120894 hasConceptScore W2093120894C127413603 @default.
• W2093120894 hasConceptScore W2093120894C131540310 @default.
• W2093120894 hasConceptScore W2093120894C163258240 @default.
• W2093120894 hasConceptScore W2093120894C178635117 @default.
• W2093120894 hasConceptScore W2093120894C202374169 @default.
• W2093120894 hasConceptScore W2093120894C2524010 @default.
• W2093120894 hasConceptScore W2093120894C2776779350 @default.
• W2093120894 hasConceptScore W2093120894C2779900269 @default.
• W2093120894 hasConceptScore W2093120894C30475298 @default.
• W2093120894 hasConceptScore W2093120894C33441834 @default.
• W2093120894 hasConceptScore W2093120894C33923547 @default.
• W2093120894 hasConceptScore W2093120894C38652104 @default.
• W2093120894 hasConceptScore W2093120894C41008148 @default.
• W2093120894 hasConceptScore W2093120894C57879066 @default.
• W2093120894 hasConceptScore W2093120894C60799052 @default.
• W2093120894 hasConceptScore W2093120894C62520636 @default.
• W2093120894 hasConceptScore W2093120894C69398868 @default.
• W2093120894 hasConceptScore W2093120894C87355193 @default.
• W2093120894 hasLocation W20931208941 @default.
• W2093120894 hasOpenAccess W2093120894 @default.
• W2093120894 hasPrimaryLocation W20931208941 @default.
• W2093120894 hasRelatedWork W1844540554 @default.
• W2093120894 hasRelatedWork W2046017672 @default.
• W2093120894 hasRelatedWork W2136413936 @default.
• W2093120894 hasRelatedWork W230035678 @default.
• W2093120894 hasRelatedWork W2353665340 @default.
• W2093120894 hasRelatedWork W2387517784 @default.
• W2093120894 hasRelatedWork W2569605742 @default.
• W2093120894 hasRelatedWork W3041446543 @default.
• W2093120894 hasRelatedWork W3158277747 @default.

• next