Controls on transpiration in a semiarid riparian cottonwood forest

Cottonwood(Populus spp.)forestsareconspicuousandfunctionallyimportantelementsofriparianvegetationthroughoutmuchof the western U.S. Understanding how transpiration by this vegetation type responds to environmental forcing is important for determining the water balance dynamics of riparian ecosystems threatened by groundwater depletion. Transpiration was measured in semiarid riparian cottonwood (Populus fremontii) stands along a perennial and an intermittent reach of the San Pedro River in southeastern Arizona. Sap flow was measured using thermal dissipation probesandscaled to the standlevel to investigate standwater useinrelationtocanopystructure,depthtogroundwaterandclimateforcing.Thecottonwoodstandlocatedattheperennialstreamsite hadhigherleaf-to-sapwoodarearatio(0.31 � 0.04 m 2 cm � 2 ),leafareaindex(2.75)andshallowergroundwaterdepth(1.1‐1.8m)than the standattheintermittentstreamsite (0.21 � 0.04 m 2 cm � 2 , 1.75and3.1‐3.9 m,respectively).Moreover,totalannualtranspiration was higher at the perennial stream site (966 mm) than at the intermittent stream site (484 mm). The significant positive and linear correlation between transpiration and vapor pressure deficit indicated high hydraulic conductance along the root‐shoot pathway of cottonwoodtreesatthe perennialstreamsite.Duringthepeakdryperiodpriortothe summerrainyseason,the treesattheintermittent streamsiteexhibitedgreaterwaterstressastranspirationdidnotincreasebeyonditsmid-morningpeakwithincreasingvaporpressure deficit, which was likely due to leaf stomatal closure. However, this stress was alleviated after significant monsoonal rains and runoff events had recharged soil moisture and raised groundwater levels. Riparian cottonwood forests are exposed to extremefluctuations in water availability and transpiration demand throughout the growing season, and their access to shallow groundwater sources determines their structural and physiological responses to drought. Spatial and temporal variation in depth to groundwater induces drought stress in cottonwood threatening their productivity and existence along the river systems throughout much of western U.S. # 2006 Elsevier B.V. All rights reserved.

[1]  N. Breda,et al.  Water transfer in a mature oak stand (Quercus petraea) : Seasonal evolution and effects of a severe drought , 1993 .

[2]  L. Simmonds,et al.  Transpiration and water relations of poplar trees growing close to the water table. , 1999, Tree physiology.

[3]  Henry L. Gholz,et al.  Environmental Limits on Aboveground Net Primary Production, Leaf Area, and Biomass in Vegetation Zones of the Pacific Northwest , 1982 .

[4]  Angela M. Gurnell,et al.  Linking hydrology and ecology , 2000 .

[5]  J. Sparks,et al.  Regulation of water loss in populations of Populus trichocarpa: the role of stomatal control in preventing xylem cavitation. , 1999, Tree physiology.

[6]  Yann Kerr,et al.  Seasonal estimates of riparian evapotranspiration using remote and in situ measurements. , 2000 .

[7]  R. Oren,et al.  Sap-flux-scaled transpiration responses to light, vapor pressure deficit, and leaf area reduction in a flooded Taxodium distichum forest. , 1999, Tree physiology.

[8]  Thomas E. Kolb,et al.  Physiological response to groundwater depth varies among species and with river flow regulation , 2001 .

[9]  D. Cooper,et al.  Physiological and Morphological Response Patterns of Populus deltoides to Alluvial Groundwater Pumping , 2003, Environmental management.

[10]  Todd E. Dawson,et al.  Determining water use by trees and forests from isotopic, energy balance and transpiration analyses: the roles of tree size and hydraulic lift. , 1996, Tree physiology.

[11]  B. Legg Principles of Environmental Physics (second edition). By J. L. Monteith and M. H. Unsworth. Sevenoaks, Kent: Edward Arnold (1990), pp. 291, £14.95, hardback £30.00. , 1990, Experimental Agriculture.

[12]  F. Magnani,et al.  Response of a mature Pinus laricio plantation to a three-year restriction of water supply: structural and functional acclimation to drought. , 2002, Tree physiology.

[13]  A. Tyree,et al.  Vulnerability of Xylem to Cavitation and Embolism , 1989 .

[14]  David G. Williams,et al.  Water sources used by riparian trees varies among stream types on the San Pedro River, Arizona. , 2000 .

[15]  Thomas Kolb,et al.  Responses of riparian trees to interannual variation in ground water depth in a semi‐arid river basin , 2001 .

[16]  Ram Oren,et al.  Transpiration in Upper Amazonia Floodplain and Upland Forests in Response to Drought‐Breaking Rains , 1996 .

[17]  Stan D. Wullschleger,et al.  A review of whole-plant water use studies in tree. , 1998, Tree physiology.

[18]  W. J. Shuttleworth,et al.  Interannual and seasonal variation in fluxes of water and carbon dioxide from a riparian woodland ecosystem , 2004 .

[19]  J. Monteith,et al.  Principles of Environmental Physics , 2014 .

[20]  P. Shafroth,et al.  Responses of Riparian Cottonwoods to Alluvial Water Table Declines , 1999, Environmental management.

[21]  A. P. O'Grady,et al.  Transpiration increases during the dry season: patterns of tree water use in eucalypt open-forests of northern Australia. , 1999, Tree physiology.

[22]  D. Whitehead Regulation of stomatal conductance and transpiration in forest canopies. , 1998, Tree physiology.

[23]  J. Flexas,et al.  Regulation of photosynthesis of C3 plants in response to progressive drought: stomatal conductance as a reference parameter. , 2002, Annals of botany.

[24]  David G. Williams,et al.  Response of tree ring holocellulose δ 13 C to moisutre availability in Populus fremontii at perennial and intermittent stream reaches , 2004 .

[25]  J. Cleverly,et al.  Evapotranspiration at the land/water interface in a semi‐arid drainage basin , 2002 .

[26]  S. Patiño,et al.  Vulnerability to drought-induced cavitation of riparian cottonwoods in Alberta: a possible factor in the decline of the ecosystem? , 1994, Tree physiology.

[27]  A. Granier,et al.  Evaluation of transpiration in a Douglas-fir stand by means of sap flow measurements. , 1987, Tree physiology.

[28]  A. S. Evans,et al.  Variation in carbon isotope composition among years in the riparian tree Populus fremontii , 1999, Oecologia.

[29]  S. McCutcheon,et al.  Phytoremediation: Transformation and control of contaminants , 2003 .

[30]  J. Vose,et al.  Measuring and Modeling Tree Stand Level Transpiration , 2003 .

[31]  David C. Goodrich,et al.  Transpiration of cottonwood/willow forest estimated from sap flux , 2000 .

[32]  D. Goodrich,et al.  Hydrologic requirements of and consumptive ground-water use by riparian vegetation along the San Pedro River, Arizona. Chapters A-D. , 2006 .

[33]  M. Cherry,et al.  The influence of drought on the relationship between leaf and conducting sapwood area in Eucalyptus globulus and Eucalyptus nitens , 1998, Trees.

[34]  J. Roberts The influence of physical and physiological characteristics of vegetation on their hydrological response , 2000 .

[35]  T. Kolb,et al.  Leaf gas exchange characteristics differ among Sonoran Desert riparian tree species. , 2001, Tree physiology.

[36]  M. Wu,et al.  Principles of environmental physics , 2004, Plant Growth Regulation.

[37]  D. Marks,et al.  Components and Controls of Water Flux in an Old-growth Douglas-fir–Western Hemlock Ecosystem , 2004, Ecosystems.

[38]  Donald R. Pool,et al.  Hydrogeologic investigations of the Sierra Vista subwatershed of the Upper San Pedro Basin, Cochise County, southeast Arizona , 1999 .

[39]  J. Vose,et al.  Measuring and Modeling Tree and Stand Level Transpiration , 2005 .

[40]  J. Stromberg,et al.  Effects of Groundwater Decline on Riparian Vegetation of Semiarid Regions: The San Pedro, Arizona , 1996 .

[41]  D. Wolf Phytoremediation: Transformation and Control of Contaminants , 2005 .

[42]  J. Cleverly,et al.  Seasonal estimates of actual evapo-transpiration from Tamarix ramosissima stands using three-dimensional eddy covariance , 2002 .