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ECOPHYSIOLOGY OF RIPARIAN COTTONWOODS <br />and consequently may not support phreatophytic cottonwoods <br />and willows. Cottonwoods become established when the chan- <br />nel flow is augmented, further demonstrating the reliance of <br />cottonwoods on stream water (Figure 2). <br />Isotopic analyses <br />Stable isotopes of oxygen and hydrogen occur naturally and, <br />because of fractionation accompanying evaporation and other <br />physical processes, specific water sources have particular iso- <br />topic compositions. Generally, there is minimal fractionation <br />in stem tissues, and thus xylem water reflects the isotopic com- <br />position of the source water taken up by roots (Dawson and <br />Ehleringer 1991). <br />Busch et al. (1992) used isotopic analyses to confirm the re- <br />liance of riparian cottonwoods on alluvial groundwater origi- <br />nating from river water. For both the Bill Williams and the <br />lower Colorado rivers in Arizona, 2H and 180 ratios consis- <br />tently showed that P. fremontii S. Watson xylem water was <br />1115 <br />Figure 1. Riparian zones along two <br />channels of the Big Lost River in Idaho <br />(July 1993). The upper photograph <br />shows a channel with continued flow <br />and healthy streamside sandbar wil- <br />lows (Salix exigua) and narrowleaf cot- <br />tonwoods (Populus angustifolia) <br />further back. The lower photograph <br />shows a channel in which flow is fully <br />diverted during the irrigation season, <br />which has led to woodland mortality <br />over a 5 -year period. <br />similar to alluvial groundwater, which was in turn similar to <br />river water (although evaporative enrichment of 2H occurred <br />over the summer). Other researchers have conducted isotopic <br />analyses that further demonstrate the reliance of riparian cot- <br />tonwoods on water originating from stream flow (Table 1). <br />However, there are several complications associated with <br />isotopic analyses (Dawson and Ehleringer 1991). For exam- <br />ple, along the Red Butte Creek near Salt Lake, Utah, ground- <br />water from hill -slope aquifers flows into the streamside zone <br />and supplements the water originating from the stream. A <br />study by Kolb et al. (1997) with box elder (Acer negundo L.), <br />another riparian phreatophyte, revealed seasonal differences. <br />The 's0 composition of xylem water indicated that large and <br />small trees along a stream in Arizona were solely reliant on <br />groundwater with an 180 composition similar to that of the ad- <br />jacent stream throughout the dry summer period, whereas, at <br />other times, these trees obtained up to one -half of their water <br />from shallow surface water that originated as recent, local pre- <br />TREE PHYSIOLOGY ONLINE at http: //heronpublishing.com <br />