Smith Douglas R, Warnemuende E A, Haggard B E, Huang C
USDA-ARS, National Soil Erosion Research Laboratory, 275 Russell Street, West Lafayette, IN 47907, USA.
J Environ Qual. 2006 Mar 1;35(2):611-6. doi: 10.2134/jeq2005.0301. Print 2006 Mar-Apr.
Managed drainage ditches are common in the midwestern United States. These ditches are designed to remove water from fields as quickly as possible, and sediment buildup necessitates dredging, to ensure adequate water removal. This laboratory study was conducted to determine the impact of ditch dredging on soluble phosphorus (P) transport. Ditch sediments were collected from a drainage ditch in northeastern Indiana immediately before and after dredging. The sediments were placed in a stream simulator, and stream water was loaded with 0.55 mM P for 5 d (adsorption experiment). Water was then removed, and "clean" water (no P added) was used for a desorption experiment, lasting 1 d. During the adsorption experiment, pre-dredged sediments were able to remove P from the water column quicker, and P concentrations 120 h after introduction of high P water were lower for the pre-dredged sediments (0.075 mM P) than the dredged sediments (0.111 mM P). During the desorption experiment, P was released to the water column slower in the pre-dredged treatment than the dredged treatment (instantaneous flux at t = 0 was 0.205 microM P h(-1) for pre-dredged and 0.488 microM P h(-1) for dredged). This occurred despite higher Mehlich 3-extractable P in the pre-dredged sediments than the dredged sediments. Equilibrium phosphorus concentrations (EPCo) were lower in the pre-dredged sediments during both adsorption and desorption experiments. Transport of soluble P immediately after dredging will likely increase in drainage ditches; however, dredging is a necessary management tool to ensure adequate discharge of water from surrounding fields.
在美国中西部,人工管理的排水沟很常见。这些排水沟旨在尽快排出田间积水,而沉积物的堆积需要进行疏浚,以确保排水顺畅。本实验室研究旨在确定沟渠疏浚对可溶性磷(P)迁移的影响。在疏浚前后,立即从印第安纳州东北部的一条排水沟中采集沟渠沉积物。将沉积物放入水流模拟器中,向水流中加入0.55 mM的磷,持续5天(吸附实验)。然后将水排出,使用“清洁”水(未添加磷)进行为期1天的解吸实验。在吸附实验中,疏浚前的沉积物能够更快地从水柱中去除磷,在引入高磷水120小时后,疏浚前沉积物中的磷浓度(0.075 mM P)低于疏浚后沉积物中的磷浓度(0.111 mM P)。在解吸实验中,疏浚前处理中磷向水柱中的释放速度比疏浚后处理慢(在t = 0时,疏浚前的瞬时通量为0.205 μM P h(-1),疏浚后的瞬时通量为0.488 μM P h(-1))。尽管疏浚前沉积物中Mehlich 3可提取磷的含量高于疏浚后沉积物,但仍出现了这种情况。在吸附和解吸实验中,疏浚前沉积物中的平衡磷浓度(EPCo)均较低。疏浚后,排水沟中可溶性磷的迁移可能会立即增加;然而,疏浚是确保周围田地排水顺畅的必要管理手段。