Toor Gurpal S, Occhipinti Marti L, Yang Yun-Ya, Majcherek Tammy, Haver Darren, Oki Lorence
Soil and Water Quality Laboratory, Gulf Coast Research and Education Center, University of Florida, Institute of Food and Agricultural Sciences, Wimauma, FL, United States of America.
South Coast Research & Extension Center, University of California Cooperative Extension, 7601 Irvine Blvd, Irvine, CA, United States of America.
PLoS One. 2017 Jun 12;12(6):e0179151. doi: 10.1371/journal.pone.0179151. eCollection 2017.
Sources and mechanisms of nutrient transport in lawn irrigation driven surface runoff are largely unknown. We investigated the transport of nitrogen (N) and phosphorus (P) in lawn irrigation driven surface runoff from a residential neighborhood (28 ha) of 56% impervious and 44% pervious areas. Pervious areas encompassing turfgrass (lawns) in the neighborhood were irrigated with the reclaimed water in common areas during the evening to late night and with the municipal water in homeowner's lawns during the morning. The stormwater outlet pipe draining the residential neighborhood was instrumented with a flow meter and Hach autosampler. Water samples were collected every 1-h and triple composite samples were obtained at 3-h intervals during an intensive sampling period of 1-week. Mean concentrations, over 56 sampling events, of total N (TN) and total P (TP) in surface runoff at the outlet pipe were 10.9±6.34 and 1.3±1.03 mg L-1, respectively. Of TN, the proportion of nitrate-N was 58% and other-N was 42%, whereas of TP, orthophosphate-P was 75% and other-P was 25%. Flow and nutrient (N and P) concentrations were lowest from 6:00 a.m. to noon, which corresponded with the use of municipal water and highest from 6:00 p.m. to midnight, which corresponded with the use of reclaimed water. This data suggests that N and P originating in lawn irrigation driven surface runoff from residential catchments is an important contributor of nutrients in surface waters.
草坪灌溉驱动的地表径流中养分运输的来源和机制在很大程度上尚不清楚。我们调查了一个住宅区(28公顷)草坪灌溉驱动的地表径流中氮(N)和磷(P)的运输情况,该住宅区不透水面积占56%,透水面积占44%。住宅区中包括草坪草(草坪)的透水区域,在傍晚至深夜期间使用再生水进行灌溉,而在早晨则使用市政供水灌溉业主的草坪。排放该住宅区雨水的排水管道安装了流量计和哈希自动采样器。在为期1周的密集采样期间,每1小时采集一次水样,并每隔3小时获取一次三联复合样本。在56次采样事件中,排水管道处地表径流中总氮(TN)和总磷(TP)的平均浓度分别为10.9±6.34和1.3±1.03毫克/升。在TN中,硝酸盐氮的比例为58%,其他氮为42%;而在TP中,正磷酸盐磷为75%,其他磷为25%。流量和养分(N和P)浓度在上午6:00至中午最低,这与市政供水的使用相对应,而在下午6:00至午夜最高,这与再生水的使用相对应。这些数据表明,来自住宅集水区草坪灌溉驱动的地表径流中的N和P是地表水中养分的重要来源。