Department of Biological and Agricultural Engineering, North Carolina State University, Raleigh, North Carolina 27695, United States.
Environ Sci Technol. 2012 Sep 18;46(18):9956-63. doi: 10.1021/es3011783. Epub 2012 Aug 28.
Nitrogen losses in drainage water from coastal forest plantations can constrain the long term sustainability of the system and could negatively affect adjacent nutrient sensitive coastal waters. Based on long-term (21 years) field measurements of hydrology and water quality, we investigated the temporal variations and controlling factors of nitrate and dissolved organic nitrogen (DON) export from an artificially drained coastal forest over various time scales (interannual, seasonal, and storm events). According to results of stepwise multiple linear regression analyses, the observed large interannual variations of nitrate flux and concentration from the drained forest were significantly (p < 0.004) controlled by annual mean water table depth, and annual drainage or precipitation. Annual precipitation and drainage were found to be dominant factors controlling variations of annual DON fluxes. Temporal trends of annual mean DON concentration could not be explained explicitly by climate or hydrologic factors. No significant difference was observed between nitrogen (both nitrate and DON) export during growing and nongrowing seasons. Nitrate exhibited distinguished export patterns during six selected storm events. Peak nitrate concentrations during storm events were significantly (p < 0.003) related to 30-day antecedent precipitation index and the minimum water table depth during individual events. The temporal variations of DON export within storm events did not follow a clear trend and its peak concentration during the storm events was found to be significantly (p < 0.006) controlled by the short-term drying and rewetting cycles.
沿海人工林排水水中的氮素损失会限制系统的长期可持续性,并可能对相邻的营养敏感沿海水域产生负面影响。本研究基于对水文和水质的长期(21 年)野外测量,调查了人工排水沿海林在不同时间尺度(年际、季节性和风暴事件)下硝酸盐和溶解有机氮(DON)输出的时间变化及其控制因素。逐步多元线性回归分析的结果表明,排水林硝酸盐通量和浓度的观测到的大的年际变化主要受年平均地下水位深度、年排水量或年降水量控制。研究发现,年降水量和排水量是控制年 DON 通量变化的主要因素。年平均 DON 浓度的时间趋势不能通过气候或水文因素来明确解释。在生长季和非生长季,氮(硝酸盐和 DON)的输出没有明显差异。在六次选定的风暴事件中,硝酸盐表现出明显的输出模式。风暴事件期间的硝酸盐峰值浓度与 30 天前期降水指数和个别事件中的最低地下水位深度显著相关(p < 0.003)。风暴事件中 DON 输出的时间变化没有明显的趋势,其在风暴事件期间的峰值浓度主要受短期干湿循环控制(p < 0.006)。