Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022896074> ?p ?o ?g. }
Showing items 1 to 78 of
78
with 100 items per page.
- W2022896074 endingPage "148" @default.
- W2022896074 startingPage "123" @default.
- W2022896074 abstract "A quantitative soil development index based on field morphologic data has been applied to a chronosequence of six soils at Honcut Creek in central California. The soils range from 600 yr to 1.6 m.y. in age and exist in a xeric-thermic soil climatic regime. Plots of the development of individual properties versus the log of soil age are generally linear. Of the eight soil properties used in the index, clay films, texture plus wet consistence, structure, and rubification (color hue and chroma), are most highly correlated with soil age (correlation coefficients for linenar regression of 0.96−0.87). Dry consistence, moist consistence, melanization (color value), and pH lowering are not as highly correlated with soil age (correlation coefficients of 0.68−0.55), although correlation coefficients for all eight soil properties are significant at α = 0.01 or 0.05 level. Depth functions of a horizon index that incorporates all eight soil properties chart the development of the A-horizons in Holocene soils and the development of the cambic and then argillic horizons in older soils. Total depth of soil development increases from about 60 cm in Holocene soils to more than 5 m in the oldest soils. Lithologic discontinuities and stratification are brought out in the horizon index because of their effects on soil development. Soils on the alluvial terraces of Honcut Creek have developed systematically over the 1.6 m.y. age span of the chronosequence: correlation coefficients for regressions of the profile index versus the log of soil age are ⩾0.97 (significant at α = 0.01 level). The coefficient of variation of replicate profiles decreases with increasing soil age. The soil development index substantiates the geologic and pedologic correlations made during geologic mapping and soil survey of the area, although differences among soils in parent material and topographic factors complicate the age trends." @default.
- W2022896074 created "2016-06-24" @default.
- W2022896074 creator A5000120512 @default.
- W2022896074 date "1987-12-01" @default.
- W2022896074 modified "2023-10-18" @default.
- W2022896074 title "Pedogenesis of a chronosequence in the Sacramento Valley, California, U.S.A., I. Application of a soil development index" @default.
- W2022896074 cites W1977730813 @default.
- W2022896074 cites W1990625716 @default.
- W2022896074 cites W1991762835 @default.
- W2022896074 cites W2011946898 @default.
- W2022896074 cites W2041621264 @default.
- W2022896074 cites W2045971761 @default.
- W2022896074 cites W2067250759 @default.
- W2022896074 doi "https://doi.org/10.1016/0016-7061(87)90032-2" @default.
- W2022896074 hasPublicationYear "1987" @default.
- W2022896074 type Work @default.
- W2022896074 sameAs 2022896074 @default.
- W2022896074 citedByCount "42" @default.
- W2022896074 countsByYear W20228960742013 @default.
- W2022896074 countsByYear W20228960742014 @default.
- W2022896074 countsByYear W20228960742015 @default.
- W2022896074 countsByYear W20228960742016 @default.
- W2022896074 countsByYear W20228960742017 @default.
- W2022896074 countsByYear W20228960742020 @default.
- W2022896074 countsByYear W20228960742021 @default.
- W2022896074 countsByYear W20228960742022 @default.
- W2022896074 countsByYear W20228960742023 @default.
- W2022896074 crossrefType "journal-article" @default.
- W2022896074 hasAuthorship W2022896074A5000120512 @default.
- W2022896074 hasConcept C114793014 @default.
- W2022896074 hasConcept C127313418 @default.
- W2022896074 hasConcept C152494472 @default.
- W2022896074 hasConcept C156634047 @default.
- W2022896074 hasConcept C159390177 @default.
- W2022896074 hasConcept C159750122 @default.
- W2022896074 hasConcept C184269829 @default.
- W2022896074 hasConcept C187320778 @default.
- W2022896074 hasConcept C2778948613 @default.
- W2022896074 hasConcept C39432304 @default.
- W2022896074 hasConcept C53706860 @default.
- W2022896074 hasConcept C5589519 @default.
- W2022896074 hasConcept C69823785 @default.
- W2022896074 hasConcept C76886044 @default.
- W2022896074 hasConceptScore W2022896074C114793014 @default.
- W2022896074 hasConceptScore W2022896074C127313418 @default.
- W2022896074 hasConceptScore W2022896074C152494472 @default.
- W2022896074 hasConceptScore W2022896074C156634047 @default.
- W2022896074 hasConceptScore W2022896074C159390177 @default.
- W2022896074 hasConceptScore W2022896074C159750122 @default.
- W2022896074 hasConceptScore W2022896074C184269829 @default.
- W2022896074 hasConceptScore W2022896074C187320778 @default.
- W2022896074 hasConceptScore W2022896074C2778948613 @default.
- W2022896074 hasConceptScore W2022896074C39432304 @default.
- W2022896074 hasConceptScore W2022896074C53706860 @default.
- W2022896074 hasConceptScore W2022896074C5589519 @default.
- W2022896074 hasConceptScore W2022896074C69823785 @default.
- W2022896074 hasConceptScore W2022896074C76886044 @default.
- W2022896074 hasIssue "1-2" @default.
- W2022896074 hasLocation W20228960741 @default.
- W2022896074 hasOpenAccess W2022896074 @default.
- W2022896074 hasPrimaryLocation W20228960741 @default.
- W2022896074 hasRelatedWork W1981965234 @default.
- W2022896074 hasRelatedWork W2045815763 @default.
- W2022896074 hasRelatedWork W2081114255 @default.
- W2022896074 hasRelatedWork W2093536092 @default.
- W2022896074 hasRelatedWork W2543198176 @default.
- W2022896074 hasRelatedWork W3096526332 @default.
- W2022896074 hasRelatedWork W3146209675 @default.
- W2022896074 hasRelatedWork W3182517280 @default.
- W2022896074 hasRelatedWork W4223434120 @default.
- W2022896074 hasRelatedWork W4308862766 @default.
- W2022896074 hasVolume "41" @default.
- W2022896074 isParatext "false" @default.
- W2022896074 isRetracted "false" @default.
- W2022896074 magId "2022896074" @default.
- W2022896074 workType "article" @default.