FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4220805739> ?p ?o ?g. }

• W4220805739 abstract "&lt;p&gt;Land cover change and its effect on water resources has been a continuous concern in south-central Chile. In this regard, we use two methodologies to study the effect of different land covers on the hydrological processes in several experimental catchments (&lt;100km&lt;sup&gt;2&lt;/sup&gt;) located between 36&amp;#176;S to 39&amp;#176;S. These experimental catchments include native forest and commercial plantations (Monterrey Pine and Eucalyptus) land covers. The first methodology is the use of hydrological modelling to analyze the land cover influence on the water yield of a catchment. [1] compared hydrological and evapotranspiration models and selected the best which represented daily stream flow. The best results were obtained through the more complex model (i.e GR6J and Oudin PET model) which can account for groundwater interaction. The second methodology is the use of the recession coefficient (a) as a metric for baseflow recession analysis, which is a good index of the risk of flow decreasing below a threshold. This coefficient represents the rate of decrease in streamflow after a rainfall event. [2] investigated through mathematical modelling how (a) differs between land cover within the same study sites as [1] study mentioned above. This coefficient did not differ in winter, indicating a similar soil saturation, but some differences were found in summer.&amp;#160; It was determined that (a) was similar between land cover types. Considering both methodological approaches we can conclude that at the experimental catchment scale geology and the fractured rock system play a crucial role in surface-groundwater interactions in these ecosystems. Therefore, future investigations should be focused on subsoil processes and surface-groundwater interaction. Due to its Mediterranean climate, rainfall in Chile is concentrated during winter months, when trees are dormant, meaning that they do not significantly transpire, and a larger proportion of rainfall can infiltrate into the soil. Therefore, metrics such as (a) can help develop landscape planning strategies to increase water availability in conjunction with hydrological modelling.&amp;#160;&lt;/p&gt;&lt;p&gt;References:&lt;/p&gt;&lt;p&gt;[1] Flores, N., Rodr&amp;#237;guez, R., Y&amp;#233;pez, S., Osores, V., Rau, P., Rivera, D., &amp; Balocchi, F. (2021). Comparison of Three Daily Rainfall-Runoff Hydrological Models Using Four Evapotranspiration Models in Four Small Forested Watersheds with Different Land Cover in South-Central Chile. Water, 13(22), 3191.&lt;/p&gt;&lt;p&gt;[2] Balocchi, F., Flores, N., Arum&amp;#237;, J. L., Iroum&amp;#233;, A., White, D. A., Silberstein, R. P., &amp; Ram&amp;#237;rez de Arellano, P. (2021a). Comparison of streamflow recession between plantations and native forests in small catchments in Central&amp;#8208;Southern Chile. Hydrological Processes, 35(6), e14182.&lt;/p&gt;" @default.
• W4220805739 created "2022-04-03" @default.
• W4220805739 creator A5028506164 @default.
• W4220805739 creator A5046899714 @default.
• W4220805739 creator A5068395030 @default.
• W4220805739 creator A5083393978 @default.
• W4220805739 date "2022-03-27" @default.
• W4220805739 modified "2023-10-17" @default.
• W4220805739 title "Understanding land cover influence on water resources in south-central Chile: A hydrological modelling with baseflow recession analysis approach&#160;" @default.
• W4220805739 doi "https://doi.org/10.5194/egusphere-egu22-1842" @default.
• W4220805739 hasPublicationYear "2022" @default.
• W4220805739 type Work @default.
• W4220805739 citedByCount "0" @default.
• W4220805739 crossrefType "posted-content" @default.
• W4220805739 hasAuthorship W4220805739A5028506164 @default.
• W4220805739 hasAuthorship W4220805739A5046899714 @default.
• W4220805739 hasAuthorship W4220805739A5068395030 @default.
• W4220805739 hasAuthorship W4220805739A5083393978 @default.
• W4220805739 hasConcept C126645576 @default.
• W4220805739 hasConcept C127313418 @default.
• W4220805739 hasConcept C176783924 @default.
• W4220805739 hasConcept C187320778 @default.
• W4220805739 hasConcept C18903297 @default.
• W4220805739 hasConcept C205649164 @default.
• W4220805739 hasConcept C2776740192 @default.
• W4220805739 hasConcept C2780648208 @default.
• W4220805739 hasConcept C39432304 @default.
• W4220805739 hasConcept C4792198 @default.
• W4220805739 hasConcept C53739315 @default.
• W4220805739 hasConcept C58640448 @default.
• W4220805739 hasConcept C76856003 @default.
• W4220805739 hasConcept C76886044 @default.
• W4220805739 hasConcept C86803240 @default.
• W4220805739 hasConceptScore W4220805739C126645576 @default.
• W4220805739 hasConceptScore W4220805739C127313418 @default.
• W4220805739 hasConceptScore W4220805739C176783924 @default.
• W4220805739 hasConceptScore W4220805739C187320778 @default.
• W4220805739 hasConceptScore W4220805739C18903297 @default.
• W4220805739 hasConceptScore W4220805739C205649164 @default.
• W4220805739 hasConceptScore W4220805739C2776740192 @default.
• W4220805739 hasConceptScore W4220805739C2780648208 @default.
• W4220805739 hasConceptScore W4220805739C39432304 @default.
• W4220805739 hasConceptScore W4220805739C4792198 @default.
• W4220805739 hasConceptScore W4220805739C53739315 @default.
• W4220805739 hasConceptScore W4220805739C58640448 @default.
• W4220805739 hasConceptScore W4220805739C76856003 @default.
• W4220805739 hasConceptScore W4220805739C76886044 @default.
• W4220805739 hasConceptScore W4220805739C86803240 @default.
• W4220805739 hasLocation W42208057391 @default.
• W4220805739 hasOpenAccess W4220805739 @default.
• W4220805739 hasPrimaryLocation W42208057391 @default.
• W4220805739 hasRelatedWork W108006107 @default.
• W4220805739 hasRelatedWork W1984179614 @default.
• W4220805739 hasRelatedWork W2024616223 @default.
• W4220805739 hasRelatedWork W2358964058 @default.
• W4220805739 hasRelatedWork W2373233278 @default.
• W4220805739 hasRelatedWork W3012605768 @default.
• W4220805739 hasRelatedWork W4220805739 @default.
• W4220805739 hasRelatedWork W4232043328 @default.
• W4220805739 hasRelatedWork W4255467712 @default.
• W4220805739 hasRelatedWork W4320506528 @default.
• W4220805739 isParatext "false" @default.
• W4220805739 isRetracted "false" @default.
• W4220805739 workType "article" @default.