FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2092145499> ?p ?o ?g. }

• W2092145499 endingPage "1095" @default.
• W2092145499 startingPage "1073" @default.
• W2092145499 abstract "A model has been developed which describes the chemical processes occurring during the formation of hill cloud. This model has been applied to the study of four cases which should be typical of the chemical conditions which can exist during the formation of such cloud over hills in the N of England. The results show that a wide range of chemical behaviour is possible in cloud droplets, depending on the history of the airmass. The composition of the water-soluble aerosol is of importance in determining the chemical composition of cloud droplets, with most of the sulphate and large proportions of the other ions being derived from this source. Gas-phase chemistry is also important, not only because it dictates the initial concentrations of oxidants such as H2O2 and O3 and of acidic gases such as HNO3 at the onset of condensation, but also because of the chemical processes which occur concurrently with those in clouds. These are important sources of radicals, as well as of nitric acid, which continue to dissolve in solution. Gasphase HCl, HNO3 and NH3 are all of primary importance in describing the acidity of cloud droplets. The various oxidation mechanisms for SO2 can all be important, with their relative contributions varying from case to case. H2O2 does not invariably dominate this process, especially in winter when its concentration may be low. The chemistry of hill clouds is far from trivial and oversimplification can result in a misunderstanding of the behaviour which occurs. There is a need, rather, to consider a wide range of reactions if the nature of the overall processes and the impact of manmade emissions on the environment via this route are to be understood." @default.
• W2092145499 created "2016-06-24" @default.
• W2092145499 creator A5004691620 @default.
• W2092145499 date "1987-01-01" @default.
• W2092145499 modified "2023-09-24" @default.
• W2092145499 title "A computer modelling study of the chemistry occurring during cloud formation over hills" @default.
• W2092145499 cites W1545336444 @default.
• W2092145499 cites W1970652095 @default.
• W2092145499 cites W1976401550 @default.
• W2092145499 cites W1989054285 @default.
• W2092145499 cites W1998350080 @default.
• W2092145499 cites W1998914464 @default.
• W2092145499 cites W1999737743 @default.
• W2092145499 cites W2000807759 @default.
• W2092145499 cites W2003474111 @default.
• W2092145499 cites W2010192261 @default.
• W2092145499 cites W2019022438 @default.
• W2092145499 cites W2020678016 @default.
• W2092145499 cites W2020850022 @default.
• W2092145499 cites W2033743617 @default.
• W2092145499 cites W2035887063 @default.
• W2092145499 cites W2039325800 @default.
• W2092145499 cites W2045104811 @default.
• W2092145499 cites W2051593140 @default.
• W2092145499 cites W2064509426 @default.
• W2092145499 cites W2065817500 @default.
• W2092145499 cites W2066375491 @default.
• W2092145499 cites W2076741322 @default.
• W2092145499 cites W2078491194 @default.
• W2092145499 cites W2080675378 @default.
• W2092145499 cites W2081709688 @default.
• W2092145499 cites W2082045986 @default.
• W2092145499 cites W2088624829 @default.
• W2092145499 cites W2103073612 @default.
• W2092145499 cites W2148558371 @default.
• W2092145499 cites W2163719266 @default.
• W2092145499 cites W3042686910 @default.
• W2092145499 doi "https://doi.org/10.1016/0004-6981(87)90235-6" @default.
• W2092145499 hasPublicationYear "1987" @default.
• W2092145499 type Work @default.
• W2092145499 sameAs 2092145499 @default.
• W2092145499 citedByCount "35" @default.
• W2092145499 countsByYear W20921454992020 @default.
• W2092145499 crossrefType "journal-article" @default.
• W2092145499 hasAuthorship W2092145499A5004691620 @default.
• W2092145499 hasConcept C107872376 @default.
• W2092145499 hasConcept C111919701 @default.
• W2092145499 hasConcept C121332964 @default.
• W2092145499 hasConcept C124223222 @default.
• W2092145499 hasConcept C127313418 @default.
• W2092145499 hasConcept C149849071 @default.
• W2092145499 hasConcept C153294291 @default.
• W2092145499 hasConcept C177801218 @default.
• W2092145499 hasConcept C178790620 @default.
• W2092145499 hasConcept C185592680 @default.
• W2092145499 hasConcept C200093464 @default.
• W2092145499 hasConcept C2779345167 @default.
• W2092145499 hasConcept C33332676 @default.
• W2092145499 hasConcept C41008148 @default.
• W2092145499 hasConcept C49999975 @default.
• W2092145499 hasConcept C508106653 @default.
• W2092145499 hasConcept C79974875 @default.
• W2092145499 hasConcept C91586092 @default.
• W2092145499 hasConceptScore W2092145499C107872376 @default.
• W2092145499 hasConceptScore W2092145499C111919701 @default.
• W2092145499 hasConceptScore W2092145499C121332964 @default.
• W2092145499 hasConceptScore W2092145499C124223222 @default.
• W2092145499 hasConceptScore W2092145499C127313418 @default.
• W2092145499 hasConceptScore W2092145499C149849071 @default.
• W2092145499 hasConceptScore W2092145499C153294291 @default.
• W2092145499 hasConceptScore W2092145499C177801218 @default.
• W2092145499 hasConceptScore W2092145499C178790620 @default.
• W2092145499 hasConceptScore W2092145499C185592680 @default.
• W2092145499 hasConceptScore W2092145499C200093464 @default.
• W2092145499 hasConceptScore W2092145499C2779345167 @default.
• W2092145499 hasConceptScore W2092145499C33332676 @default.
• W2092145499 hasConceptScore W2092145499C41008148 @default.
• W2092145499 hasConceptScore W2092145499C49999975 @default.
• W2092145499 hasConceptScore W2092145499C508106653 @default.
• W2092145499 hasConceptScore W2092145499C79974875 @default.
• W2092145499 hasConceptScore W2092145499C91586092 @default.
• W2092145499 hasIssue "5" @default.
• W2092145499 hasLocation W20921454991 @default.
• W2092145499 hasOpenAccess W2092145499 @default.
• W2092145499 hasPrimaryLocation W20921454991 @default.
• W2092145499 hasRelatedWork W189050851 @default.
• W2092145499 hasRelatedWork W1992202389 @default.
• W2092145499 hasRelatedWork W2053997985 @default.
• W2092145499 hasRelatedWork W2130128720 @default.
• W2092145499 hasRelatedWork W2413765106 @default.
• W2092145499 hasRelatedWork W2565043716 @default.
• W2092145499 hasRelatedWork W2795827997 @default.
• W2092145499 hasRelatedWork W4246106773 @default.
• W2092145499 hasRelatedWork W849096085 @default.
• W2092145499 hasRelatedWork W2910548484 @default.
• W2092145499 hasVolume "21" @default.
• W2092145499 isParatext "false" @default.
• W2092145499 isRetracted "false" @default.

• next