FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2086061626> ?p ?o ?g. }

• W2086061626 endingPage "267" @default.
• W2086061626 startingPage "253" @default.
• W2086061626 abstract "Monthly, seasonal and annual water balances of Eucalyptus urophylla plantations on the Leizhou Peninsula, southeastern China were estimated in 40m×40 m plots at two sites with contrasting soil types. The Jijia site is located on basalt-derived clay rich soils, while the Hetou site is characterised by coarse textured soils formed on Quaternary sediments. Observations of evaporative processes (overstorey canopy interception and transpiration, and soil evaporation), soil moisture dynamics, and climate variables were collected at both sites over 2 years. Canopy interception was measured by throughfall troughs and stemflow collectors, daily transpiration was measured by the heat pulse technique in year 1 and estimated from regressions with potential evapotranspiration and available soil water in year 2, soil evaporation was measured by periodic microlysimetry and used to derive a daily soil surface resistance—matric potential relationship for estimation of daily soil evaporation throughout the study period. Soil moisture storage was measured to 4 m depth and drainage estimated as the residual term in a water balance equation. Total annual evapotranspiration (Et) was similar at 1118 and 1150 mm at Jijia and 969 and 1024 mm at Hetou for years 1 and 2, respectively, despite 20–30% higher rainfall in year 2. These values represent 71 and 66% of annual rainfall in year 1, and 54 and 50% in year 2. Transpiration did not exceed 600 mm in either year and annual soil evaporation was 15–26% of Et, with the higher values from Jijia. The higher rainfall in year 2 was predicted to produce an increase in drainage and runoff rather than tree water use. Dry season water balances showed Et exceeded or approached rainfall, indicating water use from deep soil or ground water storages following soil water depletion, particularly at Hetou. However, storages were replenished by high wet season recharge. The differences in soil properties between the sites resulted in a three-fold greater soil water store at Jijia that provided a supply for Es, and the sandier Hetou soils with poor water holding capacity had greater wet season drainage and higher dry season abstraction from deep storages. The water use of the eucalypts does not appear to be seriously deleterious for water supply in this area." @default.
• W2086061626 created "2016-06-24" @default.
• W2086061626 creator A5007587623 @default.
• W2086061626 creator A5027234207 @default.
• W2086061626 creator A5029459507 @default.
• W2086061626 creator A5065830770 @default.
• W2086061626 creator A5087570263 @default.
• W2086061626 creator A5074424513 @default.
• W2086061626 date "2004-08-01" @default.
• W2086061626 modified "2023-10-17" @default.
• W2086061626 title "Water balance of tropical eucalypt plantations in south-eastern China" @default.
• W2086061626 cites W1562339465 @default.
• W2086061626 cites W1976095361 @default.
• W2086061626 cites W1979336368 @default.
• W2086061626 cites W1990839466 @default.
• W2086061626 cites W2001674519 @default.
• W2086061626 cites W2003879041 @default.
• W2086061626 cites W2006579364 @default.
• W2086061626 cites W2007517891 @default.
• W2086061626 cites W2015659077 @default.
• W2086061626 cites W2017280679 @default.
• W2086061626 cites W2019274022 @default.
• W2086061626 cites W2027953186 @default.
• W2086061626 cites W2029113687 @default.
• W2086061626 cites W2034297167 @default.
• W2086061626 cites W2043728752 @default.
• W2086061626 cites W2050201618 @default.
• W2086061626 cites W2052368806 @default.
• W2086061626 cites W2060057443 @default.
• W2086061626 cites W2062623210 @default.
• W2086061626 cites W2065500676 @default.
• W2086061626 cites W2072135353 @default.
• W2086061626 cites W2083504662 @default.
• W2086061626 cites W2100557629 @default.
• W2086061626 cites W2116991286 @default.
• W2086061626 cites W2127615053 @default.
• W2086061626 cites W2148750799 @default.
• W2086061626 cites W2153873785 @default.
• W2086061626 cites W2163426811 @default.
• W2086061626 cites W2332536414 @default.
• W2086061626 doi "https://doi.org/10.1016/j.agrformet.2004.01.015" @default.
• W2086061626 hasPublicationYear "2004" @default.
• W2086061626 type Work @default.
• W2086061626 sameAs 2086061626 @default.
• W2086061626 citedByCount "68" @default.
• W2086061626 countsByYear W20860616262012 @default.
• W2086061626 countsByYear W20860616262013 @default.
• W2086061626 countsByYear W20860616262014 @default.
• W2086061626 countsByYear W20860616262015 @default.
• W2086061626 countsByYear W20860616262016 @default.
• W2086061626 countsByYear W20860616262017 @default.
• W2086061626 countsByYear W20860616262018 @default.
• W2086061626 countsByYear W20860616262019 @default.
• W2086061626 countsByYear W20860616262020 @default.
• W2086061626 countsByYear W20860616262021 @default.
• W2086061626 countsByYear W20860616262022 @default.
• W2086061626 countsByYear W20860616262023 @default.
• W2086061626 crossrefType "journal-article" @default.
• W2086061626 hasAuthorship W2086061626A5007587623 @default.
• W2086061626 hasAuthorship W2086061626A5027234207 @default.
• W2086061626 hasAuthorship W2086061626A5029459507 @default.
• W2086061626 hasAuthorship W2086061626A5065830770 @default.
• W2086061626 hasAuthorship W2086061626A5074424513 @default.
• W2086061626 hasAuthorship W2086061626A5087570263 @default.
• W2086061626 hasConcept C127313418 @default.
• W2086061626 hasConcept C157517311 @default.
• W2086061626 hasConcept C159390177 @default.
• W2086061626 hasConcept C159750122 @default.
• W2086061626 hasConcept C176783924 @default.
• W2086061626 hasConcept C183688256 @default.
• W2086061626 hasConcept C187320778 @default.
• W2086061626 hasConcept C18903297 @default.
• W2086061626 hasConcept C24939127 @default.
• W2086061626 hasConcept C2776679863 @default.
• W2086061626 hasConcept C2779705648 @default.
• W2086061626 hasConcept C39432304 @default.
• W2086061626 hasConcept C55157361 @default.
• W2086061626 hasConcept C59822182 @default.
• W2086061626 hasConcept C61270487 @default.
• W2086061626 hasConcept C66465714 @default.
• W2086061626 hasConcept C76886044 @default.
• W2086061626 hasConcept C86803240 @default.
• W2086061626 hasConceptScore W2086061626C127313418 @default.
• W2086061626 hasConceptScore W2086061626C157517311 @default.
• W2086061626 hasConceptScore W2086061626C159390177 @default.
• W2086061626 hasConceptScore W2086061626C159750122 @default.
• W2086061626 hasConceptScore W2086061626C176783924 @default.
• W2086061626 hasConceptScore W2086061626C183688256 @default.
• W2086061626 hasConceptScore W2086061626C187320778 @default.
• W2086061626 hasConceptScore W2086061626C18903297 @default.
• W2086061626 hasConceptScore W2086061626C24939127 @default.
• W2086061626 hasConceptScore W2086061626C2776679863 @default.
• W2086061626 hasConceptScore W2086061626C2779705648 @default.
• W2086061626 hasConceptScore W2086061626C39432304 @default.
• W2086061626 hasConceptScore W2086061626C55157361 @default.
• W2086061626 hasConceptScore W2086061626C59822182 @default.
• W2086061626 hasConceptScore W2086061626C61270487 @default.
• W2086061626 hasConceptScore W2086061626C66465714 @default.

• next