Comparison of interception, forest floor evaporation and transpiration in Pinus radiata and Eucalyptus globulus plantations

被引:43
作者
Benyon, R. G. [1 ,2 ]
Doody, T. M. [1 ]
机构
[1] CSIRO Land & Water, Urrbrae, SA, Australia
[2] Univ Melbourne, Parkville, Vic 3010, Australia
关键词
interception; evaporation; transpiration; leaf area index; Pinus; Eucalyptus; WATER-USE; RAINFALL INTERCEPTION; CANOPY CONDUCTANCE; VEGETATION CHANGES; EVAPOTRANSPIRATION; CATCHMENT; BALANCE; ENERGY; YIELD; TREES;
D O I
10.1002/hyp.10237
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Studies of evapotranspiration (ET) processes in forests often only measure one component of total ET, most commonly interception. This study examined all three components of annual ET (interception, evaporation from the forest floor and transpiration) and the correlations between them at 18 plantation forest sites in two species. All plantations had closed canopies, and sparse or no understorey. Single-sided leaf area index averaged 3.5 (standard deviation 0.5) in Eucalyptus globulus Labill. and 6.1 (0.8) in Pinus radiata D.Don. Measurements included annual totals of rainfall in the open and under the canopy, stem flow (four sites only), evaporation from the forest floor and transpiration by the overstorey. Interception (I) averaged 19% (+/- 4.9) of annual rainfall in E.globulus compared with 31% (+/- 11.1) in P.radiata. However, higher annual interception in P.radiata did not result in higher total ET because annual evaporation from the forest floor (E) averaged 29% (+/- 4.9) of rainfall in E.globulus but only 15% (+/- 3.5) in P.radiata. Hence, the relative contribution of annual I plus E to ET did not differ significantly between the two species, averaging 48% (+/- 7.3) of annual rainfall in E.globulus compared with 46% (+/- 11.8) in P.radiata. As reported previously, transpiration did not differ significantly between the two species either, but was strongly related to depth-to-groundwater. In closed canopy plantations, mean annual ET did not differ between the two species. We conclude that when grown in plantations under similar soil and climatic conditions, conifer and broad-leaved tree species can have similar annual ET, once the canopy of the plantation has closed. Lower average annual interception in broad-leaved trees was offset by higher soil evaporation. These results highlight the importance of measuring all components of ET in studies of vegetation water use. Copyright (c) 2014 John Wiley & Sons, Ltd.
引用
收藏
页码:1173 / 1187
页数:15
相关论文
共 46 条
[1]   Future long-term changes in global water resources driven by socio-economic and climatic changes [J].
Alcamo, Joseph ;
Floerke, Martina ;
Maerker, Michael .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2007, 52 (02) :247-275
[2]   Growth and water balance of Eucalyptus grandis hybrid plantations in Brazil during a rotation for pulp production [J].
Almeida, Auro C. ;
Soares, Joao V. ;
Landsberg, Joe J. ;
Rezende, Gabriel D. .
FOREST ECOLOGY AND MANAGEMENT, 2007, 251 (1-2) :10-21
[3]   On measuring and modeling energy fluxes above the floor of a homogeneous and heterogeneous conifer forest [J].
Baldocchi, DD ;
Law, BE ;
Anthoni, PM .
AGRICULTURAL AND FOREST METEOROLOGY, 2000, 102 (2-3) :187-206
[4]  
Baldocchi DD, 1996, TREE PHYSIOL, V16, P5
[5]   TRACE GAS-EXCHANGE ABOVE THE FLOOR OF A DECIDUOUS FOREST .1. EVAPORATION AND CO2 EFFLUX [J].
BALDOCCHI, DD ;
MEYERS, TP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D4) :7271-7285
[6]   Modelling evapotranspiration at three boreal forest stands using the class: Tests of parameterizations for canopy conductance and soil evaporation [J].
Bartlett, PA ;
McCaughey, JH ;
Lafleur, PM ;
Verseghy, DL .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2003, 23 (04) :427-451
[7]   Spatial Variability in Forest Water Use from Three Contrasting Regions of South-Eastern Australia [J].
Benyon, R. G. ;
Lane, P. N. J. ;
Theiveyanathan, S. ;
Doody, T. M. ;
Mitchell, P. J. .
VIII INTERNATIONAL SYMPOSIUM ON SAP FLOW, 2012, 951 :233-240
[8]   Impacts of tree plantations on groundwater in south-eastern Australia [J].
Benyon, RG ;
Theiveyanathan, S ;
Doody, TM .
AUSTRALIAN JOURNAL OF BOTANY, 2006, 54 (02) :181-192
[9]  
Benyons R, 2009, QUANTIFYING GROUNDWA
[10]  
Benyons RG, 2009, PNC0640607 FOR WOOD