FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2124129085> ?p ?o ?g. }

• W2124129085 endingPage "955" @default.
• W2124129085 startingPage "943" @default.
• W2124129085 abstract "A number of mathematical distributions have been proposed for the description of the particle size distribution of unconsolidated sediments. However, few studies have mathematically described aeolian dust particle size distributions. Recent work has shown mathematically how the sequential fragmentation of materials leads to a Weibull distribution. Since the breakage of aggregates by saltating grains is a primary mode of aeolian dust production, we test the hypothesis that the Weibull distribution may be used to describe airborne soil grains. Surface samples were collected from 52 sites including soils, dirt roads and roadside ditches in the Southern High Plains of west Texas. The samples were tumbled in the Lubbock dust generation, sampling and analysis system to generate a dust cloud. The particle size distribution of the dust was measured in situ by laser diffraction and PM10 concentration was determined gravimetrically (PM10 = airborne particulate matter with diameter ≤10 µm). This study demonstrated that the Weibull cumulative distribution function (c.d.f.) is an excellent choice to describe the particle size distribution of dust suspended from mineral sediment. A Weibull c.d.f. used to describe the dust cloud size distribution, accounted for 94 per cent of the variation in estimates of particles ≤50 µm diameter. The fraction of dust particles ≤10 µm diameter, as estimated using the Weibull, was not correlated to suspended PM10 concentration. However, the fraction of particles ≤10 µm was correlated with properties of the sediment from which the airborne dust was derived. As clay content increased, the total amount of suspended dust increased and the fraction of suspended particles ≤10 µm in the dust cloud decreased. Analyses of variance showed no significant differences (P < 0·05) among sampling locations (roads vs ditches vs soils) for cumulative fraction values for ≤2·5, ≤10, ≤25, ≤30 and ≤50 µm diameter particles. However, the PM10 concentration values were significantly different among dust generated from these locations. The road samples produced about twice the amount of PM10 (490 mg m−3) as the soil or ditch samples (235 mg m−3). Published in 1999 by John Wiley & Sons, Ltd." @default.
• W2124129085 created "2016-06-24" @default.
• W2124129085 creator A5003383802 @default.
• W2124129085 creator A5035772448 @default.
• W2124129085 creator A5088654091 @default.
• W2124129085 date "1999-09-01" @default.
• W2124129085 modified "2023-10-18" @default.
• W2124129085 title "A two-parameter Weibull function to describe airborne dust particle size distributions" @default.
• W2124129085 cites W1974751079 @default.
• W2124129085 cites W1977836620 @default.
• W2124129085 cites W1979170340 @default.
• W2124129085 cites W1983199601 @default.
• W2124129085 cites W1996453555 @default.
• W2124129085 cites W1999472158 @default.
• W2124129085 cites W2006402821 @default.
• W2124129085 cites W2009110968 @default.
• W2124129085 cites W2019765564 @default.
• W2124129085 cites W2019884924 @default.
• W2124129085 cites W2031003095 @default.
• W2124129085 cites W2039099309 @default.
• W2124129085 cites W2045040003 @default.
• W2124129085 cites W2053272187 @default.
• W2124129085 cites W2058476323 @default.
• W2124129085 cites W2062689653 @default.
• W2124129085 cites W2075535441 @default.
• W2124129085 cites W2075903087 @default.
• W2124129085 cites W2077727077 @default.
• W2124129085 cites W2086673345 @default.
• W2124129085 cites W2087484271 @default.
• W2124129085 cites W2110868782 @default.
• W2124129085 cites W2121846972 @default.
• W2124129085 cites W2127353896 @default.
• W2124129085 cites W2129900821 @default.
• W2124129085 cites W2132993449 @default.
• W2124129085 cites W2312820985 @default.
• W2124129085 cites W2727420541 @default.
• W2124129085 cites W4250950666 @default.
• W2124129085 cites W4251615374 @default.
• W2124129085 doi "https://doi.org/10.1002/(sici)1096-9837(199909)24:10<943::aid-esp30>3.0.co;2-9" @default.
• W2124129085 hasPublicationYear "1999" @default.
• W2124129085 type Work @default.
• W2124129085 sameAs 2124129085 @default.
• W2124129085 citedByCount "50" @default.
• W2124129085 countsByYear W21241290852012 @default.
• W2124129085 countsByYear W21241290852013 @default.
• W2124129085 countsByYear W21241290852014 @default.
• W2124129085 countsByYear W21241290852015 @default.
• W2124129085 countsByYear W21241290852016 @default.
• W2124129085 countsByYear W21241290852017 @default.
• W2124129085 countsByYear W21241290852018 @default.
• W2124129085 countsByYear W21241290852019 @default.
• W2124129085 countsByYear W21241290852020 @default.
• W2124129085 countsByYear W21241290852021 @default.
• W2124129085 countsByYear W21241290852022 @default.
• W2124129085 countsByYear W21241290852023 @default.
• W2124129085 crossrefType "journal-article" @default.
• W2124129085 hasAuthorship W2124129085A5003383802 @default.
• W2124129085 hasAuthorship W2124129085A5035772448 @default.
• W2124129085 hasAuthorship W2124129085A5088654091 @default.
• W2124129085 hasConcept C105795698 @default.
• W2124129085 hasConcept C111368507 @default.
• W2124129085 hasConcept C114793014 @default.
• W2124129085 hasConcept C127313418 @default.
• W2124129085 hasConcept C151730666 @default.
• W2124129085 hasConcept C159390177 @default.
• W2124129085 hasConcept C159985019 @default.
• W2124129085 hasConcept C173291955 @default.
• W2124129085 hasConcept C180093795 @default.
• W2124129085 hasConcept C187530423 @default.
• W2124129085 hasConcept C192562407 @default.
• W2124129085 hasConcept C199289684 @default.
• W2124129085 hasConcept C2778517922 @default.
• W2124129085 hasConcept C2779015675 @default.
• W2124129085 hasConcept C2816523 @default.
• W2124129085 hasConcept C33923547 @default.
• W2124129085 hasConcept C39432304 @default.
• W2124129085 hasConcept C60448018 @default.
• W2124129085 hasConcept C91586092 @default.
• W2124129085 hasConceptScore W2124129085C105795698 @default.
• W2124129085 hasConceptScore W2124129085C111368507 @default.
• W2124129085 hasConceptScore W2124129085C114793014 @default.
• W2124129085 hasConceptScore W2124129085C127313418 @default.
• W2124129085 hasConceptScore W2124129085C151730666 @default.
• W2124129085 hasConceptScore W2124129085C159390177 @default.
• W2124129085 hasConceptScore W2124129085C159985019 @default.
• W2124129085 hasConceptScore W2124129085C173291955 @default.
• W2124129085 hasConceptScore W2124129085C180093795 @default.
• W2124129085 hasConceptScore W2124129085C187530423 @default.
• W2124129085 hasConceptScore W2124129085C192562407 @default.
• W2124129085 hasConceptScore W2124129085C199289684 @default.
• W2124129085 hasConceptScore W2124129085C2778517922 @default.
• W2124129085 hasConceptScore W2124129085C2779015675 @default.
• W2124129085 hasConceptScore W2124129085C2816523 @default.
• W2124129085 hasConceptScore W2124129085C33923547 @default.
• W2124129085 hasConceptScore W2124129085C39432304 @default.
• W2124129085 hasConceptScore W2124129085C60448018 @default.
• W2124129085 hasConceptScore W2124129085C91586092 @default.
• W2124129085 hasIssue "10" @default.

• next