Iowa Geological Survey, University of Iowa, 300 Trowbridge Hall, Iowa City, IA, 52242, USA.
Environ Monit Assess. 2021 Jul 21;193(8):500. doi: 10.1007/s10661-021-09297-3.
Agricultural drainage tiles are primary contributors to NO-N export from Iowa croplands. Saturated buffers are a relatively new conservation practice that diverts tile water into a distribution tile installed in a riparian buffer parallel to a stream with the intent of enhancing NO-N processing within the buffer. In this study, tile NO-N concentration reductions were characterized through two different saturated buffers at a working farm site in eastern Iowa. Study objectives were to (1) evaluate the hydrogeology and water quality patterns in the saturated buffer and (2) quantify the reduction in tile NO-N concentration from the saturated buffer installation. Results showed that the two saturated buffers are reducing NO-N concentrations in tile drainage water from input concentrations of approximately 15 mg/l to levels < 1.5 mg/l at the streamside well locations. The reduction occurs rapidly in the fine-textured and organic-rich alluvial soils with most of the reduction occurring within 1.5 m of the distribution line. Denitrification is hypothesized as being primarily responsible for the concentration reductions based on soil and water chemistry conditions, completion of a geophysical survey (quantifying low potential for N loss to deeper aquifers), and comparisons to other similar Iowa sites. The study provides more assurance to new adopters that this practice can be installed in many areas throughout the Midwestern Cornbelt region.
农业排水瓦是爱荷华州农田中硝酸盐氮(NO-N)输出的主要贡献者。饱和缓冲带是一种相对较新的保护措施,它将瓦排水引导到安装在与溪流平行的河岸缓冲带中的分配瓦中,目的是增强缓冲带内的硝酸盐氮处理。本研究通过爱荷华州东部一个工作农场现场的两个不同的饱和缓冲带来描述瓦中硝酸盐氮浓度的降低。研究目的是:(1)评估饱和缓冲带的水文地质和水质模式;(2)量化饱和缓冲带安装对瓦中硝酸盐氮浓度的降低。结果表明,两个饱和缓冲带将瓦排水中的硝酸盐氮浓度从约 15mg/L 的输入浓度降低到溪流侧井位的<1.5mg/L 水平。在细质地和富含有机质的冲积土壤中,还原过程迅速发生,大部分还原发生在分布线 1.5m 范围内。基于土壤和水化学条件、地球物理调查的完成(量化了向深层含水层损失氮的低潜力)以及与其他类似爱荷华州地点的比较,推测反硝化作用是导致浓度降低的主要原因。该研究为新采用者提供了更多保证,即这种做法可以在中西部玉米带地区的许多地区安装。