Department of Biology, University of Utah, Salt Lake City, Utah 84112, USA.
Ecol Appl. 2010 Mar;20(2):347-61. doi: 10.1890/09-0492.1.
Riparian cottonwood/willow forest assemblages are highly valued in the southwestern United States for their wildlife habitat, biodiversity, and watershed protection. Yet these forests are under considerable threat from climate change impacts on water resources and land-use activities to support human enterprise. Stream diversions, groundwater pumping, and extended drought have resulted in the decline of cottonwood/willow forests along many riparian corridors in the Southwest and, in many cases, the replacement of these forests with less desirable invasive shrubs and trees. Nevertheless, ecophysiological responses of cottonwood and willow, along with associated ecohydrological feedbacks of soil water depletion, are not well understood. Ecophysiological processes of mature Fremont cottonwood and coyote willow stands were examined over four consecutive growing seasons (2004-2007) near Salt Lake City, Utah, USA. The tree stands occurred near the inlet of a reservoir that was drained in the spring of 2005 and remained empty until mid-summer of 2006, effectively removing the primary water source for most of two growing seasons. Stem sap flux density (Js) in cottonwood was highly correlated with volumetric soil moisture (theta) in the upper 60 cm and decreased sevenfold as soil moisture dropped from 12% to 7% after the reservoir was drained. Conversely, Js in willow was marginally correlated with 0 and decreased by only 25% during the same period. Opposite patterns emerged during the following growing season: willow had a lower whole-plant conductance (kt) in June and higher leaf carbon isotope ratios (delta13C) than cottonwood in August, whereas k(t) and delta13C were otherwise similar between species. Water relations in both species recovered quickly from soil water depletion, with the exception that sapwood area to stem area (As:Ast) was significantly lower in both species after the 2007 growing season compared to 2004. Results suggest that cottonwood has a greater sensitivity to interannual reductions in water availability, while willow is more sensitive to longer periods of soil water depletion. These data shed light on the linkage between soil water deficits and ecophysiological processes of threatened riparian forests given potential land-use and long-term drought impacts on freshwater resources.
河岸棉白杨/柳树林组合在美国西南部因其野生动物栖息地、生物多样性和流域保护而备受重视。然而,这些森林受到气候变化对水资源和支持人类企业的土地利用活动的巨大威胁。溪流改道、地下水抽取和长期干旱导致西南地区许多河岸走廊的棉白杨/柳树林减少,在许多情况下,这些森林被不太理想的入侵灌木和树木所取代。然而,棉白杨和柳树的生理生态响应以及土壤水分消耗的相关生态水文反馈还没有得到很好的理解。在美国犹他州盐湖城附近,连续四个生长季节(2004-2007 年)对成熟弗里蒙特棉白杨和郊狼柳树林的生态生理过程进行了研究。这些树木生长在一个水库的入口附近,该水库在 2005 年春季被排空,直到 2006 年夏中一直空着,有效地消除了两个生长季节中大部分时间的主要水源。棉白杨的茎液流密度(Js)与上 60 厘米处的体积土壤水分(θ)高度相关,当水库排空后土壤水分从 12%降至 7%时,Js 降低了七倍。相反,柳树的 Js 与 0 呈边缘相关,在此期间仅下降了 25%。在下一个生长季节出现了相反的模式:柳树在 6 月的整株植物导度(kt)较低,8 月的叶片碳同位素比值(δ13C)较高,而物种之间的 k(t)和δ13C则相似。除了 2007 年生长季后两种物种的边材面积与茎面积比(As:Ast)显著低于 2004 年外,两种物种的水分关系均从土壤水分亏缺中迅速恢复。结果表明,棉白杨对年际水资源减少更为敏感,而柳树对较长时间的土壤水分亏缺更为敏感。这些数据阐明了在潜在土地利用和长期干旱对淡水资源的影响下,土壤水分亏缺与受威胁河岸林的生态生理过程之间的联系。