FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313647464> ?p ?o ?g. }

• W4313647464 abstract "Abstract. Throughfall heterogeneity induced by the redistribution of precipitation in vegetation canopies has repeatedly been hypothesized to affect the variation of soil water content and runoff behavior, especially in forests. However, we are not aware of any observational study relating the spatial variation of soil water content directly to net precipitation to confirm modelling hypotheses. Here, we investigate whether throughfall patterns affect the spatial heterogeneity of soil water response in the main rooting zone. We assessed rainfall, throughfall and soil water contents (two depths: 7.5 cm and 27.5 cm) on a 1‐ha temperate mixed beech forest plot in Germany 2015–2016 during the growing seasons in independent high‐resolution stratified random designs. Because throughfall and soil water content cannot be measured at the same location, we used kriging to derive the throughfall values at the locations where soil water content was measured. We first explore the spatial variation and temporal stability of throughfall and soil water patterns, and next evaluate the effects of input (throughfall), soil properties (field capacity and air capacity), and vegetation parameters (canopy cover and distance to the next tree) on soil water content and dynamics. Throughfall spatial patterns were related to canopy density. Although spatial auto-correlation decreased with increasing event sizes, temporally stable throughfall patterns emerged, leading to reoccurring high and lower input locations across precipitation events. A linear mixed effect model analysis showed, that soil water content patterns were only poorly linked to throughfall spatial patterns, and it was rather shaped by unidentified but time constant factors. Instead of soil water content itself, the patterns of its increase after rainfall corresponded more closely to throughfall patterns, in that more water was stored in the soil where throughfall was elevated. Furthermore, soil moisture patterns themselves enhanced or decreased water storage in the soil, and probably fast drainage and runoff components. Locations with low topsoil water content tended to store less of the input water, indicating preferential flow. In contrast in subsoil, locations with high water content stored less water. Also, distance to the next tree and air capacity modified how much water was retained in soil storage. In this comprehensive study we show that throughfall patterns imprint less on soil water contents and more on soil water dynamics shortly after rainfall events, therefore only partly confirming previous modelling with data. Our findings highlight at the same time systematic patterns of times and locations where the capacity to store water is reduced and water probably conducted quickly to greater depth. Our results indicate that not soil moisture patterns but rather percolation may depend on small scale spatial heterogeneity of canopy input patterns." @default.
• W4313647464 created "2023-01-07" @default.
• W4313647464 creator A5008314512 @default.
• W4313647464 creator A5053532418 @default.
• W4313647464 creator A5061754760 @default.
• W4313647464 creator A5065197357 @default.
• W4313647464 creator A5083432491 @default.
• W4313647464 date "2023-01-06" @default.
• W4313647464 modified "2023-10-03" @default.
• W4313647464 title "Throughfall spatial patterns translate into spatial patterns of soil moisture dynamics – empirical evidence" @default.
• W4313647464 doi "https://doi.org/10.5194/hess-2022-418" @default.
• W4313647464 hasPublicationYear "2023" @default.
• W4313647464 type Work @default.
• W4313647464 citedByCount "0" @default.
• W4313647464 crossrefType "posted-content" @default.
• W4313647464 hasAuthorship W4313647464A5008314512 @default.
• W4313647464 hasAuthorship W4313647464A5053532418 @default.
• W4313647464 hasAuthorship W4313647464A5061754760 @default.
• W4313647464 hasAuthorship W4313647464A5065197357 @default.
• W4313647464 hasAuthorship W4313647464A5083432491 @default.
• W4313647464 hasBestOaLocation W43136474641 @default.
• W4313647464 hasConcept C101000010 @default.
• W4313647464 hasConcept C105795698 @default.
• W4313647464 hasConcept C127313418 @default.
• W4313647464 hasConcept C158709400 @default.
• W4313647464 hasConcept C159390177 @default.
• W4313647464 hasConcept C159750122 @default.
• W4313647464 hasConcept C187320778 @default.
• W4313647464 hasConcept C18903297 @default.
• W4313647464 hasConcept C24939127 @default.
• W4313647464 hasConcept C2779705648 @default.
• W4313647464 hasConcept C33923547 @default.
• W4313647464 hasConcept C39432304 @default.
• W4313647464 hasConcept C39807119 @default.
• W4313647464 hasConcept C50477045 @default.
• W4313647464 hasConcept C76886044 @default.
• W4313647464 hasConcept C86803240 @default.
• W4313647464 hasConcept C91586092 @default.
• W4313647464 hasConcept C94747663 @default.
• W4313647464 hasConceptScore W4313647464C101000010 @default.
• W4313647464 hasConceptScore W4313647464C105795698 @default.
• W4313647464 hasConceptScore W4313647464C127313418 @default.
• W4313647464 hasConceptScore W4313647464C158709400 @default.
• W4313647464 hasConceptScore W4313647464C159390177 @default.
• W4313647464 hasConceptScore W4313647464C159750122 @default.
• W4313647464 hasConceptScore W4313647464C187320778 @default.
• W4313647464 hasConceptScore W4313647464C18903297 @default.
• W4313647464 hasConceptScore W4313647464C24939127 @default.
• W4313647464 hasConceptScore W4313647464C2779705648 @default.
• W4313647464 hasConceptScore W4313647464C33923547 @default.
• W4313647464 hasConceptScore W4313647464C39432304 @default.
• W4313647464 hasConceptScore W4313647464C39807119 @default.
• W4313647464 hasConceptScore W4313647464C50477045 @default.
• W4313647464 hasConceptScore W4313647464C76886044 @default.
• W4313647464 hasConceptScore W4313647464C86803240 @default.
• W4313647464 hasConceptScore W4313647464C91586092 @default.
• W4313647464 hasConceptScore W4313647464C94747663 @default.
• W4313647464 hasFunder F4320320879 @default.
• W4313647464 hasLocation W43136474641 @default.
• W4313647464 hasOpenAccess W4313647464 @default.
• W4313647464 hasPrimaryLocation W43136474641 @default.
• W4313647464 hasRelatedWork W1972435682 @default.
• W4313647464 hasRelatedWork W1980610457 @default.
• W4313647464 hasRelatedWork W2014313475 @default.
• W4313647464 hasRelatedWork W2061115122 @default.
• W4313647464 hasRelatedWork W2084918940 @default.
• W4313647464 hasRelatedWork W2295010903 @default.
• W4313647464 hasRelatedWork W2369966870 @default.
• W4313647464 hasRelatedWork W2778576106 @default.
• W4313647464 hasRelatedWork W2791539677 @default.
• W4313647464 hasRelatedWork W3111363341 @default.
• W4313647464 isParatext "false" @default.
• W4313647464 isRetracted "false" @default.
• W4313647464 workType "article" @default.