URS Corporation, Morrisville, North Carolina, USA.
Int J Phytoremediation. 2013;15(3):232-44. doi: 10.1080/15226514.2012.687195.
Poplar and willow tree stands were installed in 2003 at a site in Raleigh, North Carolina containing total petroleum hydrocarbon - contaminated groundwater. The objective was groundwater uptake and plume control. The water table was 5 to 6 m below ground surface (bgs) and therefore methods were used to encourage deep root development. Growth rates, rooting depth and sap flow were measured for trees in Plot A located in the center of the plume and in Plot B peripheral to the plume. The trees were initially sub-irrigated with vertically installed drip-lines and by 2005 had roots 4 to 5 m bgs. Water balance calculations suggested groundwater uptake. In 2007, the average sap flow was higher for Plot B (approximately 59 L per day per tree) than for Plot A (approximately 23 L per day per tree), probably as a result of TPH-induced stress in Plot A. Nevertheless, the estimated rate of groundwater uptake for Plot A was sufficient, relative to the calculated rate of groundwater flux beneath the stand, that a high level of plume control was achieved based on MODFLOW modeling results. Down-gradient groundwater monitoring wells installed in late 2011 should provide quantitative data for plume control.
2003 年,在美国北卡罗来纳州罗利市的一个含有总石油烃污染地下水的地点安装了杨树和柳树林。目的是地下水摄取和羽流控制。地下水位在地面以下 5 到 6 米处,因此采用了一些方法来鼓励深根的发展。在位于羽流中心的 A 区和位于羽流外围的 B 区测量了树木的生长速度、根系深度和液流。这些树木最初通过垂直安装的滴灌线进行亚灌溉,到 2005 年,根系已经长到 4 到 5 米深。水量平衡计算表明地下水的摄取。2007 年,B 区(每棵树每天约 59 升)的平均液流高于 A 区(每棵树每天约 23 升),这可能是由于 A 区的 TPH 诱导压力。然而,相对于模型计算的地下水位下的地下水通量,A 区的地下水摄取率估计是足够的,基于 MODFLOW 模型结果,实现了高程度的羽流控制。2011 年末安装的下游地下水监测井应提供羽流控制的定量数据。