The New Zealand Institute for Plant & Food Research Limited, Ruakura Research Centre, Hamilton.
J Environ Sci Health B. 2012;47(1):30-41. doi: 10.1080/03601234.2012.606416.
In the Mezquital Valley, Mexico, crops have been irrigated with untreated municipal wastewater for more than a century. Atrazine has been applied to maize and alfalfa grown in the area for weed control for 15 years. Our objectives were to analyse (i) how wastewater irrigation affects the filtering of atrazine, and (ii) if the length of irrigation has a significant impact. We compared atrazine sorption to Phaeozems that have been irrigated with raw wastewater for 35 (P35) and 85 (P85) years with sorption to a non-irrigated (P0) Phaeozem soil under rainfed agriculture. The use of bromide as an inert water tracer in column experiments and the subsequent analysis of the tracers' breakthrough curves allowed the calibration of the hydrodynamic parameters of a two-site non equilibrium convection-dispersion model. The quality of the irrigation water significantly altered the soils' hydrodynamic properties (hydraulic conductivity, dispersivity and the size of pores that are hydraulically active). The impacts on soil chemical properties (total organic carbon content and pH) were not significant, while the sodium adsorption ratio was significantly increased. Sorption and desorption isotherms, determined in batch and column experiments, showed enhanced atrazine sorption and reduced and slower desorption in wastewater-irrigated soils. These effects increased with the length of irrigation. The intensified sorption-desorption hysteresis in wastewater-irrigated soils indicated that the soil organic matter developed in these soils had fewer high-energy, easily accessible sorption sites available, leading to lower and slower atrazine desorption rates. This study leads to the conclusion that wastewater irrigation decreases atrazine mobility in the Mezquital valley Phaeozems by decreasing the hydraulic conductivity and increasing the soil's sorption capacity.
在墨西哥的梅斯基特山谷,农作物已经用未经处理的城市废水灌溉了一个多世纪。莠去津已被用于该地区种植的玉米和苜蓿的杂草控制,已有 15 年。我们的目标是分析:(i)废水灌溉如何影响莠去津的过滤,以及(ii)灌溉时间的长短是否有显著影响。我们比较了用未经处理的废水灌溉 35 年(P35)和 85 年(P85)的黑钙土与雨养农业下未灌溉的黑钙土(P0)对莠去津的吸附。溴化物作为惰性水示踪剂在柱实验中的使用,以及随后对示踪剂突破曲线的分析,使我们能够校准双位点非平衡对流-弥散模型的水动力参数。灌溉水的质量显著改变了土壤的水动力性质(水力传导率、弥散度和水力作用的孔隙大小)。对土壤化学性质(总有机碳含量和 pH 值)的影响并不显著,而钠离子吸附比则显著增加。批量和柱实验中确定的吸附和解吸等温线表明,在废水灌溉的土壤中,莠去津的吸附增强,解吸减少且更慢。这些影响随着灌溉时间的延长而增加。在废水灌溉的土壤中,吸附-解吸滞后现象加剧,表明这些土壤中形成的土壤有机质具有较少的高能、易接近的吸附位点,导致莠去津解吸速率降低且更慢。本研究得出的结论是,废水灌溉通过降低水力传导率和增加土壤的吸附能力,降低了梅斯基特山谷黑钙土中莠去津的迁移性。