Jackson P C, Cavelier J, Goldstein G, Meinzer F C, Holbrook N M
Department of Biology and Laboratory of Structural Biology and Molecular Medicine, University of California, 900 Veteran Ave., 90024-1786, Los Angeles, CA, USA.
Departamento de Biología, Universidad de Los Andes, Bogotá, Colombia.
Oecologia. 1995 Feb;101(2):197-203. doi: 10.1007/BF00317284.
Source water used by plants of several species in a semi-evergreen lowland tropical forest on Barro Colorado Island, Panama, was assessed by comparing the relative abundance of deuterium, D, versus hydrogen, H (stable hydrogen isotope composition, δD) in xylem sap and in soil water at different depths, during the dry season of 1992. Ecological correlates of source water were examined by comparing xylem water δD values with leaf phenology, leaf water status determined with a pressure chamber, and rates of water use determined as mass flow of sap using the stem heat balance method. Soil water δD values decreased sharply to 30 cm, then remained relatively constant with increasing depth. Average δD values were-13‰, for 0-30 cm depth and-36.7‰ for 30-100 cm depth. Soil water δD values were negatively associated with soil water content and soil water potential. Concurrent analyses of xylem water revealed a high degree of partitioning of water resources among species of this tropical forest. Xylem water δD of deciduous trees (average=-25.3±1.4‰) was higher than that of evergreen trees (average=-36.3±3.5‰), indicating that evergreen species had access to the more abundant soil water at greater depth than deciduous species. In evergreen shade-tolerant and high-light requiring shrubs and small trees, δD of xylem water was negatively correlated with transpiration rate and leaf water potential indicating that species using deeper, more abundant water resources had both higher rates of water use and more favorable leaf water status.
1992年旱季期间,通过比较巴拿马巴罗科罗拉多岛半常绿低地热带森林中几种植物木质部汁液和不同深度土壤水中氘(D)与氢(H)的相对丰度(稳定氢同位素组成,δD),评估了这些植物所使用的源水。通过将木质部水δD值与叶物候、用压力室测定的叶水状况以及用茎热平衡法测定的作为汁液质量流的水分利用速率进行比较,研究了源水的生态相关性。土壤水δD值在30厘米深度处急剧下降,然后随深度增加保持相对恒定。0 - 30厘米深度的平均δD值为 - 13‰,30 - 100厘米深度的平均δD值为 - 36.7‰。土壤水δD值与土壤含水量和土壤水势呈负相关。对木质部水的同步分析表明,该热带森林物种间水资源分配程度较高。落叶树的木质部水δD(平均 = - 25.3±1.4‰)高于常绿树(平均 = - 36.3±3.5‰),这表明常绿树种比落叶树种能获取更深层更丰富的土壤水。在耐荫和喜光的常绿灌木及小乔木中,木质部水δD与蒸腾速率和叶水势呈负相关,这表明利用更深层、更丰富水资源的物种具有更高的水分利用速率和更有利的叶水状况。