Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand

The major fraction of water reaching the forest floor is throughfall, which consists of free throughfall, splash throughfall and canopy drip. Research has shown that forest canopies modify the isotopic composition of throughfall by means of evaporation, isotopic exchange, canopy selection and mixing of rainfall waters. However, the effects of these factors in relation to throughfall isotopic composition and the throughfall drop size reaching the soil surface are unclear. Based on research in a mountainous Scots pine stand in northeastern Spain, this study sought to fill this knowledge gap by examining the isotopic composition of throughfall in relation to throughfall drop size. In the experimental stand, throughfall consisted on average of 65 % canopy drip, 19 % free throughfall and 16 % splash throughfall. The dynamics of the isotopic composition of throughfall and rainfall showed complex behaviour throughout events. The isotopic shift showed no direct relationship with meteorological variables, number of drops, drop velocities, throughfall and rainfall amount, or raindrop kinetic energy. However, the experiment did reveal that the isotopic shift was higher at the beginning of an event, decreasing as cumulative rainfall increased, and that it also increased when the median volume drop size of throughfall (D50_TF) approached or was lower than the median volume drop size of rainfall (D50_RF). This finding indicates that the major contribution of splash throughfall at the initial phase of rain events matched the highest vapour pressure deficit (VPD) and, at the same time, corresponded to higher isotopic enrichment, which implies that splash droplet evaporation occurred. Future applications of our approach will improve understanding of how throughfall isotopic composition may vary with drop type and size during rainfall events across a range of forest types.

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Bibliographic Details
Main Authors: Pinos, Juan, Latron, Jérôme, Nanko, Kazuki, Levia, Delphis F., Llorens, Pilar
Other Authors: Ministerio de Ciencia e Innovación (España)
Format: artículo biblioteca
Language:English
Published: European Geosciences Union 2020-09-28
Subjects:Mediterranean Scots pine stand, Water fraction, Forest floor,
Online Access:http://hdl.handle.net/10261/222937
http://dx.doi.org/10.13039/501100004837
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spelling dig-idaea-es-10261-2229372020-11-17T02:23:14Z Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand Pinos, Juan Latron, Jérôme Nanko, Kazuki Levia, Delphis F. Llorens, Pilar Ministerio de Ciencia e Innovación (España) Llorens, Pilar [0000-0003-4591-5303] Mediterranean Scots pine stand Water fraction Forest floor The major fraction of water reaching the forest floor is throughfall, which consists of free throughfall, splash throughfall and canopy drip. Research has shown that forest canopies modify the isotopic composition of throughfall by means of evaporation, isotopic exchange, canopy selection and mixing of rainfall waters. However, the effects of these factors in relation to throughfall isotopic composition and the throughfall drop size reaching the soil surface are unclear. Based on research in a mountainous Scots pine stand in northeastern Spain, this study sought to fill this knowledge gap by examining the isotopic composition of throughfall in relation to throughfall drop size. In the experimental stand, throughfall consisted on average of 65 % canopy drip, 19 % free throughfall and 16 % splash throughfall. The dynamics of the isotopic composition of throughfall and rainfall showed complex behaviour throughout events. The isotopic shift showed no direct relationship with meteorological variables, number of drops, drop velocities, throughfall and rainfall amount, or raindrop kinetic energy. However, the experiment did reveal that the isotopic shift was higher at the beginning of an event, decreasing as cumulative rainfall increased, and that it also increased when the median volume drop size of throughfall (D50_TF) approached or was lower than the median volume drop size of rainfall (D50_RF). This finding indicates that the major contribution of splash throughfall at the initial phase of rain events matched the highest vapour pressure deficit (VPD) and, at the same time, corresponded to higher isotopic enrichment, which implies that splash droplet evaporation occurred. Future applications of our approach will improve understanding of how throughfall isotopic composition may vary with drop type and size during rainfall events across a range of forest types. This research has been supported by the Spanish Ministry of Science and Innovation (grant nos. CGL2016- 75957-R AEI/FEDER UE, PID2019-106583RB-I00 and BES2017-082234) and the Japan Society for the Promotion of Science (grant no. JP15H05626). The publication fee for this article was covered by the CSIC Open Access Publication Support Initiative through its Unit of Information Resources for Research (URICI). Peer reviewed 2020-11-16T10:02:25Z 2020-11-16T10:02:25Z 2020-09-28 artículo http://purl.org/coar/resource_type/c_6501 Hydrology and Earth System Sciences 24: 4675–4690 (2020) http://hdl.handle.net/10261/222937 10.5194/hess-24-4675-2020 http://dx.doi.org/10.13039/501100004837 en #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/CGL2016- 75957-R AEI/FEDER UE info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2019-106583RB-I00 info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/BES2017-082234 Publisher's version https://doi.org/10.5194/hess-24-4675-2020 Sí open European Geosciences Union
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Mediterranean Scots pine stand
Water fraction
Forest floor
Mediterranean Scots pine stand
Water fraction
Forest floor
spellingShingle Mediterranean Scots pine stand
Water fraction
Forest floor
Mediterranean Scots pine stand
Water fraction
Forest floor
Pinos, Juan
Latron, Jérôme
Nanko, Kazuki
Levia, Delphis F.
Llorens, Pilar
Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
description The major fraction of water reaching the forest floor is throughfall, which consists of free throughfall, splash throughfall and canopy drip. Research has shown that forest canopies modify the isotopic composition of throughfall by means of evaporation, isotopic exchange, canopy selection and mixing of rainfall waters. However, the effects of these factors in relation to throughfall isotopic composition and the throughfall drop size reaching the soil surface are unclear. Based on research in a mountainous Scots pine stand in northeastern Spain, this study sought to fill this knowledge gap by examining the isotopic composition of throughfall in relation to throughfall drop size. In the experimental stand, throughfall consisted on average of 65 % canopy drip, 19 % free throughfall and 16 % splash throughfall. The dynamics of the isotopic composition of throughfall and rainfall showed complex behaviour throughout events. The isotopic shift showed no direct relationship with meteorological variables, number of drops, drop velocities, throughfall and rainfall amount, or raindrop kinetic energy. However, the experiment did reveal that the isotopic shift was higher at the beginning of an event, decreasing as cumulative rainfall increased, and that it also increased when the median volume drop size of throughfall (D50_TF) approached or was lower than the median volume drop size of rainfall (D50_RF). This finding indicates that the major contribution of splash throughfall at the initial phase of rain events matched the highest vapour pressure deficit (VPD) and, at the same time, corresponded to higher isotopic enrichment, which implies that splash droplet evaporation occurred. Future applications of our approach will improve understanding of how throughfall isotopic composition may vary with drop type and size during rainfall events across a range of forest types.
author2 Ministerio de Ciencia e Innovación (España)
author_facet Ministerio de Ciencia e Innovación (España)
Pinos, Juan
Latron, Jérôme
Nanko, Kazuki
Levia, Delphis F.
Llorens, Pilar
format artículo
topic_facet Mediterranean Scots pine stand
Water fraction
Forest floor
author Pinos, Juan
Latron, Jérôme
Nanko, Kazuki
Levia, Delphis F.
Llorens, Pilar
author_sort Pinos, Juan
title Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
title_short Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
title_full Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
title_fullStr Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
title_full_unstemmed Throughfall isotopic composition in relation to drop size at the intra-event scale in a Mediterranean Scots pine stand
title_sort throughfall isotopic composition in relation to drop size at the intra-event scale in a mediterranean scots pine stand
publisher European Geosciences Union
publishDate 2020-09-28
url http://hdl.handle.net/10261/222937
http://dx.doi.org/10.13039/501100004837
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AT nankokazuki throughfallisotopiccompositioninrelationtodropsizeattheintraeventscaleinamediterraneanscotspinestand
AT leviadelphisf throughfallisotopiccompositioninrelationtodropsizeattheintraeventscaleinamediterraneanscotspinestand
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