Transpiration of cottonwood/willow forest estimated from sap flux.
Authors:
Schaeffer, S.M. Williams, D.G. Goodrich, D.C. USDA, ARS
Source:
Agricultural and forest meteorology. Nov 20, 2000. v. 105 (1/3), p. 257-270.
NALT Subjects:
Populus fremontii Salix transpiration sap sap flow estimation methodology tree age vegetation riparian forests streams floodplains velocity seasonal variation canopy ecological succession leaf area index sapwood diameter basal area Arizona
Other Subjects:
salix gooddingii ratios evaluation size
Issue Date:
20-Nov-2000
Abstract:
Cottonwood/willow forests in the American Southwest consist of discrete, even-aged vegetation patches arranged in narrow strips along active and abandoned stream channels of alluvial flood plains. We used the heat-pulse velocity technique in this study to estimate transpiration in 12 such forest patches along a perennially flowing reach of the San Pedro River in southeastern Arizona, USA during five periods from April to October 1997. Transpiration per unit sapwood area was consistently higher for the larger cottonwood trees found on outer secondary channels compared to that of smaller cottonwood trees along the active channel, but statistically significant differences were found only in August and October. Conversely, transpiration per unit sapwood area in willow was markedly higher for trees along the primary channel than for those few larger trees that were sampled on the outer margins of the forest. Average daily transpiration at the canopy scale among the patches in July was 4.8±0.7 mm per day and ranged from 5.7±0.6 mm per day in young forest patches adjacent to the primary stream channel to 3.1±0.6 mm per day in more successionally advanced patches on secondary channels. Differences in our estimates of transpiration between forest patches along primary and secondary stream channels were related to differences in the ratio of sapwood area to ground area of the forest patches, and leaf area index. Estimates of transpiration from this forest type, and projections of transpiration and groundwater flux over larger areas on the San Pedro River, should take into account structural variation in these forests that relate to population dynamics of dominant trees.
