Department of Geography, School of Environmental Science, University of Liverpool, Chatham Street, Liverpool, Merseyside, L69 7ZY, UK.
Water Res. 2010 Jul;44(14):4226-40. doi: 10.1016/j.watres.2010.05.026. Epub 2010 May 25.
River impoundment by dams has far-reaching consequences for downstream floodplains in terms of hydrology, water quality, geomorphology, ecology and ecosystem services. With the imperative of economic development, there is the danger that potential environmental impacts are not assessed adequately or monitored appropriately. Here, an investigation of sediment composition of two pans (floodplain wetlands) in the Pongolo River floodplain, KwaZulu-Natal, downstream of the Pongolapoort dam constructed in 1974, is considered as a method for post-hoc assessment of the impacts on river hydrology, sediment supply and water quality. Bumbe and Sokhunti pans have contrasting hydrological regimes in terms of their connection to the main Pongolo channel - Bumbe is a shallow ephemeral pan and Sokhunti is a deep, perennial water body. The results of X-ray fluorescence (XRF) geochemical analysis of their sediment records over a depth of >1 m show that whilst the two pans exhibit similar sediment composition and variability in their lower part, Bumbe pan exhibits a shift toward increased fine-grained mineral supply and associated nutrient influx at a depth of c. 45 cm whilst Sokhunti pan is characterised by increased biogenic productivity at a depth of c. 26 cm due to enhanced nutrient status. The underlying cause is interpreted as a shift in hydrology to a 'post-dam' flow regime of reduced flood frequencies with more regular baseline flows which reduce the average flow velocity. In addition, Sokhunti shows a greater sensitivity to soil influx during flood events due to the nature of its 'background' of autochthonous biogenic sedimentation. The timing of the overall shift in sediment composition and the dates of the mineral inwash events are not well defined, but the potential for these wetlands as sensitive recorders of dam-induced changes in floodplain hydrology, especially those with a similar setting to Sokhunti pan, is clearly demonstrated.
水坝的建造成就了对下游洪泛平原的水文、水质、地貌、生态和生态系统服务的深远影响。随着经济发展的迫切需要,存在着潜在环境影响未得到充分评估或监测的危险。在这里,我们对蓬戈洛河洪泛平原两个洼地(洪泛湿地)的沉积物组成进行了调查,该洼地位于 1974 年建造的蓬戈洛波尔特水坝下游,这被认为是事后评估对河流水文、泥沙供应和水质影响的一种方法。本比和索昆蒂洼地在与主要蓬戈洛河道的连接方面具有不同的水文状况-本比是一个浅而短暂的洼地,而索昆蒂是一个深而常年的水体。对它们的沉积物记录进行的 X 射线荧光(XRF)地球化学分析的结果表明,虽然这两个洼地在其下部具有相似的沉积物组成和可变性,但本比洼地在深度约 45 厘米处表现出向增加细粒矿物供应和相关养分涌入的转变,而索昆蒂洼地则在深度约 26 厘米处由于养分状况的改善而表现出生物生产力的增加。其根本原因被解释为水文学向“后坝”水流模式的转变,减少了洪水频率,增加了更规则的基线流量,从而降低了平均流速。此外,由于其自生生物沉积的“背景”性质,索昆蒂洼地在洪水事件中显示出对土壤输入的更大敏感性。沉积物组成总体转变的时间和矿物入侵事件的日期没有得到很好的定义,但这些湿地作为洪泛平原水文学变化的敏感记录者的潜力是显而易见的,特别是对于那些与索昆蒂洼地具有类似设置的湿地。