Alstad Karrin P, Hart Stephen C, Horton Jonathan L, Kolb Thomas E
School of Forestry and Merriam-Powell Center for Environmental Research, Northern Arizona University, Flagstaff, Arizona 86011, USA.
Ecol Appl. 2008 Mar;18(2):421-37. doi: 10.1890/06-1969.1.
Historical patterns of water source use by trees inferred from long-term records of tree-ring stable isotopic content could assist in evaluating the impact of human alterations to natural stream flow regimes (e.g., water impoundments, stream flow diversions, and groundwater extraction). Our objective was to assess the utility of the hydrogen stable isotopic composition (SD) of tree rings as an index of historical water source use by riparian trees. We investigated the influence of site conditions that varied in climate and hydrology on the relationship between deltaD of Populus xylem water (deltaD(xyl)) and tree-ring cellulose (deltaD(cell)). deltaD(xyl) and deltaD(cell) were strongly correlated across sites (r2 = 0.89). However, the slope of this relationship was less than 1, indicating that factors other than deltaD(xyl) influenced deltaD(cell). Inverse modeling with an isotopic fractionation model for tree-ring cellulose suggested that the lack of one-to-one correspondence between deltaD(xyl) and deltaD(cell) was due to the influence of the hydrogen isotopic content of the atmospheric water vapor (deltaD(atm)). Empirically measured values of deltaD(cell) were typically within the seasonal range of deltaD(cell) predicted from the fractionation model. Sensitivity analyses showed that changes in deltaD(xyl) generally had a greater influence at high-elevation montane sites, whereas deltaD(xyl) and deltaD(atm) had about equal influence on deltaD(cell) at low-elevation desert sites. The intrasite relationship between deltaD(cell) and deltaD(xyl) among individual trees was poor, perhaps because of the within-site spatial variation in hydrologic conditions and associated tree physiological responses. Our study suggests that historical variation in deltaD(cell) of Populus provides information on historical variation in both time-integrated water source use and atmospheric conditions; and that the influence of atmospheric conditions is not consistent over sites with large differences in temperature and humidity. Reconstruction of xylem water sources of Populus in riparian ecosystems from deltaD(cell) will be more direct at higher elevation mountain sites than at low-elevation desert sites.
从树木年轮稳定同位素含量的长期记录中推断出的树木水源利用历史模式,有助于评估人类活动对自然水流状态(如拦水、水流改道和地下水抽取)的影响。我们的目标是评估树木年轮的氢稳定同位素组成(δD)作为河岸树木历史水源利用指标的效用。我们研究了气候和水文条件各异的场地条件对杨树木质部水的δD(δD(xyl))与树木年轮纤维素的δD(δD(cell))之间关系的影响。δD(xyl)和δD(cell)在各场地间呈强相关(r2 = 0.89)。然而,这种关系的斜率小于1,表明除δD(xyl)外的其他因素影响了δD(cell)。利用树木年轮纤维素的同位素分馏模型进行的反演表明,δD(xyl)和δD(cell)之间缺乏一一对应关系是由于大气水汽的氢同位素含量(δD(atm))的影响。δD(cell)的实测值通常在分馏模型预测的δD(cell)季节范围内。敏感性分析表明,δD(xyl)的变化通常在高海拔山地场地影响更大,而在低海拔沙漠场地,δD(xyl)和δD(atm)对δD(cell)的影响大致相当。个体树木间δD(cell)和δD(xyl)的场地内关系较差,这可能是由于场地内水文条件的空间变化以及相关的树木生理反应。我们的研究表明,杨树δD(cell)的历史变化提供了关于时间积分水源利用和大气条件历史变化的信息;并且大气条件的影响在温度和湿度差异较大的场地间并不一致。从δD(cell)重建河岸生态系统中杨树的木质部水源,在高海拔山地场地比在低海拔沙漠场地更直接。