Natural Resource Conservation Center, Watkinsville, GA 30677, USA.
J Environ Qual. 2011 May-Jun;40(3):969-79. doi: 10.2134/jeq2010.0411.
Approximately 11% of the Southern Piedmont (1.8 million ha) is used for pasture and hay production, mostly under low-input management. Few studies have investigated in the region long-term nitrogen and carbon losses in surface runoff, which can be significant. We present 1999 to 2009 hydrologic and water quality data from a rotationally grazed, 7.8-ha, zero-order pasture (W1) near Watkinsville in the Georgia Piedmont. Annual rainfall was 176 to 463 mm below the long-term average (1240 mm) in 7 of the 11 yr. There were 20 runoff events during 86 mo of below-average rainfall (deficit period), compared with 54 events during 46 mo of nondeficit period. Mean event flow-weighted concentration (in mg L) was 0.96 for nitrate-nitrogen (NO-N), 0.97 for ammonium-nitrogen (NH-N), 3.70 for total nitrogen (TN), and 9.12 for total organic carbon (TOC) ( = 43-47; limited due to instrument problem). Nutrient loads (in kg ha per event) averaged 0.04 for NO-N, 0.03 for NH-N, 0.19 for TN, and 0.54 for TOC. Total loads for N and TOC were 6 to 11 times greater from nondeficit than from deficit periods. The observed N concentrations, while well below maximum drinking water standard limits, could pose risk for eutrophication, which can be stimulated at lower concentrations. However, the ability of headwater streams, such as the one downstream of W1, to reduce nutrient concentrations might partially alleviate this concern. The results of this study point to the need to use a long-term dataset that includes measurements made in drought and wet years when evaluating the efficacy of water quality standards.
大约 11%的南皮德蒙特(180 万公顷)用于牧场和干草生产,主要采用低投入管理。该地区很少有研究调查地表水的长期氮和碳损失,而这些损失可能是显著的。我们展示了 1999 年至 2009 年佐治亚皮德蒙特沃特金斯维尔附近一个 7.8 公顷零级牧场(W1)的水文和水质数据。在 11 年中有 7 年的年降雨量低于长期平均水平(1240 毫米),降雨量为 176 至 463 毫米。在低于平均降雨量的 86 个月(亏缺期)内发生了 20 次径流事件,而在非亏缺期的 46 个月内发生了 54 次径流事件。平均事件流量加权浓度(mg/L)为硝酸盐氮(NO-N)0.96、铵氮(NH-N)0.97、总氮(TN)3.70 和总有机碳(TOC)9.12(=43-47;由于仪器问题而有限)。养分负荷(kg/ha/事件)平均为 NO-N0.04、NH-N0.03、TN0.19 和 TOC0.54。非亏缺期的氮和 TOC 总负荷比亏缺期高 6 至 11 倍。虽然观察到的氮浓度远低于最大饮用水标准限值,但可能对富营养化构成风险,而在较低浓度下就可以刺激富营养化。然而,像 W1 下游的源头溪流这样的溪流具有降低营养浓度的能力,可能会部分缓解这种担忧。本研究的结果表明,在评估水质标准的有效性时,需要使用包括干旱和湿润年份测量值的长期数据集。