Agricultural and Biological Engineering Dep., Univ. of Florida, 287 Frazier Rogers Hall, P.O. Box 110570, Gainesville, FL 32611-0570, USA.
J Environ Qual. 2010 Sep-Oct;39(5):1570-84. doi: 10.2134/jeq2009.0375.
Floodplain forests provide unique ecological structure and function, which are often degraded or lost when watershed hydrology is modified. Restoration of damaged ecosystems requires an understanding of surface water, groundwater, and vadose (unsaturated) zone hydrology in the floodplain. Soil moisture and porewater salinity are of particular importance for seed germination and seedling survival in systems affected by saltwater intrusion but are difficult to monitor and often overlooked. This study contributes to the understanding of floodplain hydrology in one of the last bald cypress [Taxodium distichum (L.) Rich.] floodplain swamps in southeast Florida. We investigated soil moisture and porewater salinity dynamics in the floodplain of the Loxahatchee River, where reduced freshwater flow has led to saltwater intrusion and a transition to salt-tolerant, mangrove-dominated communities. Twenty-four dielectric probes measuring soil moisture and porewater salinity every 30 min were installed along two transects-one in an upstream, freshwater location and one in a downstream tidal area. Complemented by surface water, groundwater, and meteorological data, these unique 4-yr datasets quantified the spatial variability and temporal dynamics of vadose zone hydrology. Results showed that soil moisture can be closely predicted based on river stage and topographic elevation (overall Nash-Sutcliffe coefficient of efficiency = 0.83). Porewater salinity rarely exceeded tolerance thresholds (0.3125 S m(-1)) for bald cypress upstream but did so in some downstream areas. This provided an explanation for observed vegetation changes that both surface water and groundwater salinity failed to explain. The results offer a methodological and analytical framework for floodplain monitoring in locations where restoration success depends on vadose zone hydrology and provide relationships for evaluating proposed restoration and management scenarios for the Loxahatchee River.
泛滥平原森林提供了独特的生态结构和功能,但当流域水文学发生变化时,这些结构和功能往往会退化或丧失。受损生态系统的恢复需要了解泛滥平原地表水、地下水和包气带(不饱和)带水文学。在受海水入侵影响的系统中,土壤湿度和孔隙水盐分对于种子萌发和幼苗存活尤为重要,但这些因素很难监测,而且经常被忽视。本研究有助于了解佛罗里达州东南部最后一个巴尔的摩柏树[Taxodium distichum(L.)Rich.]泛滥平原沼泽地之一的泛滥平原水文学。我们调查了洛哈切奇河泛滥平原的土壤湿度和孔隙水盐分动态,这里的淡水流量减少导致了海水入侵和向耐盐、红树林占主导地位的群落的转变。沿两条横断面(一条在淡水上游位置,一条在下游潮汐区)安装了 24 个测量土壤湿度和孔隙水盐分的介电探头,每 30 分钟测量一次。这些独特的 4 年数据集补充了地表水、地下水和气象数据,量化了包气带水文学的空间变异性和时间动态。结果表明,土壤湿度可以根据河水位和地形高程(总体纳什-苏特克里夫效率系数= 0.83)进行密切预测。在上游的巴尔的摩柏树处,孔隙水盐分很少超过(0.3125 S m(-1))的耐受阈值,但在一些下游地区却超过了该阈值。这解释了观察到的植被变化,地表水和地下水盐分都无法解释这些变化。研究结果为依赖包气带水文学的泛滥平原监测提供了一种方法和分析框架,并为评估洛哈切奇河的拟议恢复和管理方案提供了关系。