Meixner T, Fenn M E, Wohlgemuth P, Oxford M, Riggan P
Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona 85721, USA.
Environ Sci Technol. 2006 May 1;40(9):2887-94. doi: 10.1021/es051268z.
Fire is a critical ecosystem process in many landscapes and is particularly dominant in the chaparral shrublands of southern California which are also exposed to high levels of atmospheric N deposition. Few studies have addressed the combined effects of these two disturbance factors. In this study we evaluate the hydrologic and biogeochemical response of a control and a prescribed burn catchment over a 15-year period. Streamwater nitrate concentrations and export in the burned catchment were higher than those in the unburned catchment for 7-10 years after the burn and concentrations remained high in both catchments during the entire study. Therefore, fire is not an effective mitigation tool for N deposition in these semi-arid systems. Additionally, the extended N export in this system indicates that chaparral ecosystems do not recovertheir N retention capabilities as rapidly as humid systems do when subjected to disturbance.
在许多地貌中,火灾是一个关键的生态系统过程,在南加州的矮林灌丛中尤为显著,这些地区还面临着高水平的大气氮沉降。很少有研究探讨这两种干扰因素的综合影响。在本研究中,我们评估了一个对照流域和一个规定燃烧流域在15年期间的水文和生物地球化学响应。燃烧后7至10年内,燃烧流域的溪流硝酸盐浓度和输出量高于未燃烧流域,并且在整个研究期间,两个流域的浓度都保持在较高水平。因此,在这些半干旱系统中,火灾不是减轻氮沉降的有效工具。此外,该系统中氮的持续输出表明,矮林生态系统在受到干扰后,其氮保留能力的恢复速度不如湿润系统快。