FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2950510147> ?p ?o ?g. }

• W2950510147 endingPage "1277" @default.
• W2950510147 startingPage "1277" @default.
• W2950510147 abstract "Soil moisture is a central theme in eco-hydrology. Topography, soil characteristics, and vegetation types are significant factors impacting soil moisture dynamics. However, water loss (evapotranspiration and leakage) and its factors of the self-organized vegetation pattern are not clear, which has significant ecologic functions and contributes to different hydrological ecosystem services. From an eco-hydrological point of view, we relied on the observation of rainfall, soil moisture, and soil temperature in the growing season of a drought year to compare soil moisture and temperature dynamics in terms of frequency/probability distribution and water loss among three typical vegetation types in the Qilian Mountains, China. The results indicated that shrubland (the semi-shaded slope) had the highest average soil moisture at the surface soil (0–40 cm) and soil profile during the growing season, while grassland (the south-facing slope) had the lowest daily average soil moisture and highest daily average soil temperature at the surface soil and soil profile. Spruce forest (the shaded slope) had the lowest daily average soil temperature at the surface soil and soil profile (p < 0.001). Water loss among the three vegetation types has a clear positive relationship with soil water content and a negative relationship with soil temperature. The values of water loss between values of water loss at the wilting point and maximum evapotranspiration point tend to occur in wetter soil moisture under the spruce forest and shrubland, whereas that of grassland emerges in drier soil moisture. The spruce forest and shrubland experienced higher water loss than the grassland. Although the spruce forest and shrubland had a better capacity to retain soil water, they also consumed more soil water than the grassland. Soil moisture may be the main factor controlling the difference in water loss among the three vegetation types. These findings may contribute to improving our understanding of the relationship between the soil moisture dynamics and vegetation pattern, and may offer basic insights for ecosystem management for upstream water-controlled mountainous areas." @default.
• W2950510147 created "2019-06-27" @default.
• W2950510147 creator A5039326489 @default.
• W2950510147 creator A5045037838 @default.
• W2950510147 creator A5058794904 @default.
• W2950510147 creator A5068106562 @default.
• W2950510147 creator A5083758760 @default.
• W2950510147 creator A5089824454 @default.
• W2950510147 date "2019-06-19" @default.
• W2950510147 modified "2023-10-15" @default.
• W2950510147 title "Soil Hydrothermal Characteristics among Three Typical Vegetation Types: An Eco-Hydrological Analysis in the Qilian Mountains, China" @default.
• W2950510147 cites W1548298781 @default.
• W2950510147 cites W1551433475 @default.
• W2950510147 cites W1564860500 @default.
• W2950510147 cites W1752442883 @default.
• W2950510147 cites W1793886366 @default.
• W2950510147 cites W1917537995 @default.
• W2950510147 cites W1966645910 @default.
• W2950510147 cites W1970957530 @default.
• W2950510147 cites W1973946685 @default.
• W2950510147 cites W1978122243 @default.
• W2950510147 cites W1982931704 @default.
• W2950510147 cites W1993908563 @default.
• W2950510147 cites W1999350237 @default.
• W2950510147 cites W2001305958 @default.
• W2950510147 cites W2003299037 @default.
• W2950510147 cites W2008337587 @default.
• W2950510147 cites W2008963807 @default.
• W2950510147 cites W2028181163 @default.
• W2950510147 cites W2028979033 @default.
• W2950510147 cites W2036247824 @default.
• W2950510147 cites W2052001969 @default.
• W2950510147 cites W2052225688 @default.
• W2950510147 cites W2055963580 @default.
• W2950510147 cites W2062555598 @default.
• W2950510147 cites W2064251579 @default.
• W2950510147 cites W2070817134 @default.
• W2950510147 cites W2071911694 @default.
• W2950510147 cites W2086980364 @default.
• W2950510147 cites W2091438967 @default.
• W2950510147 cites W2092284888 @default.
• W2950510147 cites W2106435400 @default.
• W2950510147 cites W2111169586 @default.
• W2950510147 cites W2117325793 @default.
• W2950510147 cites W2119893173 @default.
• W2950510147 cites W2135694410 @default.
• W2950510147 cites W2136238095 @default.
• W2950510147 cites W2138277837 @default.
• W2950510147 cites W2146291222 @default.
• W2950510147 cites W2148989614 @default.
• W2950510147 cites W2158957260 @default.
• W2950510147 cites W2163712639 @default.
• W2950510147 cites W2164935596 @default.
• W2950510147 cites W2172956642 @default.
• W2950510147 cites W2578608718 @default.
• W2950510147 cites W2593099842 @default.
• W2950510147 cites W2621219463 @default.
• W2950510147 cites W2794421688 @default.
• W2950510147 cites W2886134084 @default.
• W2950510147 cites W2890756997 @default.
• W2950510147 cites W2906595379 @default.
• W2950510147 doi "https://doi.org/10.3390/w11061277" @default.
• W2950510147 hasPublicationYear "2019" @default.
• W2950510147 type Work @default.
• W2950510147 sameAs 2950510147 @default.
• W2950510147 citedByCount "3" @default.
• W2950510147 countsByYear W29505101472020 @default.
• W2950510147 countsByYear W29505101472023 @default.
• W2950510147 crossrefType "journal-article" @default.
• W2950510147 hasAuthorship W2950510147A5039326489 @default.
• W2950510147 hasAuthorship W2950510147A5045037838 @default.
• W2950510147 hasAuthorship W2950510147A5058794904 @default.
• W2950510147 hasAuthorship W2950510147A5068106562 @default.
• W2950510147 hasAuthorship W2950510147A5083758760 @default.
• W2950510147 hasAuthorship W2950510147A5089824454 @default.
• W2950510147 hasBestOaLocation W29505101471 @default.
• W2950510147 hasConcept C110872660 @default.
• W2950510147 hasConcept C127313418 @default.
• W2950510147 hasConcept C142724271 @default.
• W2950510147 hasConcept C144144481 @default.
• W2950510147 hasConcept C159390177 @default.
• W2950510147 hasConcept C159750122 @default.
• W2950510147 hasConcept C176783924 @default.
• W2950510147 hasConcept C187320778 @default.
• W2950510147 hasConcept C18903297 @default.
• W2950510147 hasConcept C24939127 @default.
• W2950510147 hasConcept C2775835988 @default.
• W2950510147 hasConcept C2776133958 @default.
• W2950510147 hasConcept C2778898053 @default.
• W2950510147 hasConcept C27934549 @default.
• W2950510147 hasConcept C39432304 @default.
• W2950510147 hasConcept C59898753 @default.
• W2950510147 hasConcept C6557445 @default.
• W2950510147 hasConcept C71924100 @default.
• W2950510147 hasConcept C76886044 @default.
• W2950510147 hasConcept C86803240 @default.
• W2950510147 hasConceptScore W2950510147C110872660 @default.
• W2950510147 hasConceptScore W2950510147C127313418 @default.

• next