FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2460140982> ?p ?o ?g. }

• W2460140982 endingPage "680" @default.
• W2460140982 startingPage "670" @default.
• W2460140982 abstract "In terms of formation mechanisms of linear dunes, there are open arguments for their widespread distribution and multi-morphological diversities. In order to clarify the formation mechanism of linear dunes of Qarhan Salt Lake, we used pattern analysis method to analyze the statistical characteristics and spatial variation of their pattern parameters. Except at the west-northwest margin, the pattern parameters showed regular spatial variation from the up-middle part towards the downwind end of the dune field. Based on the cumulative probability plots for inter-crest spacing and crest length, we divided the linear dunes into three groups, which corresponding to the three evolution stages of these dunes. The first group comprises erosional relics, with shorter crests, smaller inter-crest spacing and more random dune orientation. The second group comprises dunes whose sand supply is just sufficient to maintain stability and these dunes are approaching the net erosion stage. The crest length and inter-crest spacing of these dunes are much larger than those of the first group, and dune orientation is closer to the resultant drift direction (RDD). The last group comprises linear dunes that are still undergoing vertical accretion and longitudinal elongation, which follows the RDD of the modern wind regime. The presence of regular spatial variation of pattern parameters and a similar geometry with the vegetated linear dunes suggest that deposition and erosion coexist in the development and evolution of linear dunes of Qarhan Salt Lake, i.e. deposition predominates at the downwind end of linear dunes in the vertical accretion and longitudinal elongation stage, whereas erosion mainly occurs at the upwind end of linear dunes in the degradation stage. Therefore, the formation mechanism of linear dunes in Qarhan Salt Lake can be reasonably explained by the combination of depositional and erosional theories." @default.
• W2460140982 created "2016-07-22" @default.
• W2460140982 creator A5002998830 @default.
• W2460140982 creator A5007530486 @default.
• W2460140982 creator A5015753506 @default.
• W2460140982 creator A5016847702 @default.
• W2460140982 creator A5036726873 @default.
• W2460140982 creator A5045056678 @default.
• W2460140982 creator A5053297901 @default.
• W2460140982 date "2016-06-02" @default.
• W2460140982 modified "2023-09-25" @default.
• W2460140982 title "Pattern analysis of a linear dune field on the northern margin of Qarhan Salt Lake, northwestern China" @default.
• W2460140982 cites W1483380491 @default.
• W2460140982 cites W1964573299 @default.
• W2460140982 cites W1977217597 @default.
• W2460140982 cites W1980474487 @default.
• W2460140982 cites W1981215178 @default.
• W2460140982 cites W1991430203 @default.
• W2460140982 cites W2001992966 @default.
• W2460140982 cites W2003522741 @default.
• W2460140982 cites W2006261488 @default.
• W2460140982 cites W2018281579 @default.
• W2460140982 cites W2020297532 @default.
• W2460140982 cites W2023648948 @default.
• W2460140982 cites W2026546350 @default.
• W2460140982 cites W2047412183 @default.
• W2460140982 cites W2058955612 @default.
• W2460140982 cites W2066999391 @default.
• W2460140982 cites W2067627484 @default.
• W2460140982 cites W2069801708 @default.
• W2460140982 cites W2077861238 @default.
• W2460140982 cites W2098624449 @default.
• W2460140982 cites W2105228813 @default.
• W2460140982 cites W2114837653 @default.
• W2460140982 cites W2140061839 @default.
• W2460140982 cites W2145486493 @default.
• W2460140982 cites W2150260315 @default.
• W2460140982 cites W2154098731 @default.
• W2460140982 cites W2166394847 @default.
• W2460140982 cites W2222985393 @default.
• W2460140982 cites W4253489545 @default.
• W2460140982 doi "https://doi.org/10.1007/s40333-016-0052-5" @default.
• W2460140982 hasPublicationYear "2016" @default.
• W2460140982 type Work @default.
• W2460140982 sameAs 2460140982 @default.
• W2460140982 citedByCount "13" @default.
• W2460140982 countsByYear W24601409822016 @default.
• W2460140982 countsByYear W24601409822018 @default.
• W2460140982 countsByYear W24601409822019 @default.
• W2460140982 countsByYear W24601409822020 @default.
• W2460140982 countsByYear W24601409822021 @default.
• W2460140982 countsByYear W24601409822022 @default.
• W2460140982 crossrefType "journal-article" @default.
• W2460140982 hasAuthorship W2460140982A5002998830 @default.
• W2460140982 hasAuthorship W2460140982A5007530486 @default.
• W2460140982 hasAuthorship W2460140982A5015753506 @default.
• W2460140982 hasAuthorship W2460140982A5016847702 @default.
• W2460140982 hasAuthorship W2460140982A5036726873 @default.
• W2460140982 hasAuthorship W2460140982A5045056678 @default.
• W2460140982 hasAuthorship W2460140982A5053297901 @default.
• W2460140982 hasBestOaLocation W24601409822 @default.
• W2460140982 hasConcept C100970517 @default.
• W2460140982 hasConcept C108497213 @default.
• W2460140982 hasConcept C111368507 @default.
• W2460140982 hasConcept C114793014 @default.
• W2460140982 hasConcept C121332964 @default.
• W2460140982 hasConcept C123157820 @default.
• W2460140982 hasConcept C127313418 @default.
• W2460140982 hasConcept C167110946 @default.
• W2460140982 hasConcept C180093795 @default.
• W2460140982 hasConcept C187320778 @default.
• W2460140982 hasConcept C205649164 @default.
• W2460140982 hasConcept C2524010 @default.
• W2460140982 hasConcept C2776401274 @default.
• W2460140982 hasConcept C2816523 @default.
• W2460140982 hasConcept C33923547 @default.
• W2460140982 hasConcept C44870925 @default.
• W2460140982 hasConcept C48880136 @default.
• W2460140982 hasConcept C62520636 @default.
• W2460140982 hasConcept C64297162 @default.
• W2460140982 hasConcept C76886044 @default.
• W2460140982 hasConcept C94700167 @default.
• W2460140982 hasConceptScore W2460140982C100970517 @default.
• W2460140982 hasConceptScore W2460140982C108497213 @default.
• W2460140982 hasConceptScore W2460140982C111368507 @default.
• W2460140982 hasConceptScore W2460140982C114793014 @default.
• W2460140982 hasConceptScore W2460140982C121332964 @default.
• W2460140982 hasConceptScore W2460140982C123157820 @default.
• W2460140982 hasConceptScore W2460140982C127313418 @default.
• W2460140982 hasConceptScore W2460140982C167110946 @default.
• W2460140982 hasConceptScore W2460140982C180093795 @default.
• W2460140982 hasConceptScore W2460140982C187320778 @default.
• W2460140982 hasConceptScore W2460140982C205649164 @default.
• W2460140982 hasConceptScore W2460140982C2524010 @default.
• W2460140982 hasConceptScore W2460140982C2776401274 @default.
• W2460140982 hasConceptScore W2460140982C2816523 @default.
• W2460140982 hasConceptScore W2460140982C33923547 @default.
• W2460140982 hasConceptScore W2460140982C44870925 @default.

• next