David Mark B, Wall Lareina G, Royer Todd V, Tank Jennifer L
University of Illinois, Department of Natural Resources and Environmental Sciences, W-503 Turner Hall, 1102 S. Goodwin Avenue, Urbana 61801, USA.
Ecol Appl. 2006 Dec;16(6):2177-90. doi: 10.1890/1051-0761(2006)016[2177:datnbo]2.0.co;2.
Denitrification is an important process in aquatic sediments, but its role has not been assessed in the N mass balance of upper-Midwestern (USA) reservoirs that receive large agricultural riverine N inputs. We used a 4400-ha reservoir to determine the role of denitrification in the N mass balance and effectiveness in reducing downstream transport of NO(3-)N. Sediment denitrification was (1) measured monthly (March 2002-March 2003) at eight sites in the Lake Shelbyville reservoir in central Illinois using the acetylene inhibition, chloramphenicol technique, (2) scaled to the overall reservoir and compared to N not accounted for in a mass balance, and (3) estimated indirectly using long-term (1981-2003) mass balances of N in the reservoir. Denitrification rates in the reservoir were high during spring and early summer of 2002, when maximum NO(3-)N concentrations were measured (10-14 mg NO(3-)N/L). We estimated that denitrification for the year was between 2580 and 5150 Mg N. Missing N from the mass balance was 3004 Mg N, suggesting that sediment denitrification was the sink. Areal rates of sediment denitrification in the reservoir ranged from 62 to 225 g N x m(-2) x yr(-1), with rates a function of both denitrification intensity (microg N x g dry mass x h(-1)) and the overall mass of sediment present. From 1981 to 2003 the average NO(3-)N inlet flux was 8900 Mg N/yr. About 58% of the total NO(3-)N input was removed, and annual NO(3-)N removed as a percentage of inputs was significantly related to reservoir retention time (average = 0.36 yr for the 23 years, range = 0.21-0.84 yr). By scaling denitrification in Lake Shelbyville to other reservoirs in Illinois, we estimated a sink of 48900 Mg N/yr. When combined with estimated in-stream denitrification, 60900 Mg N/yr was estimated to be removed by sediment denitrification. This reduces riverine export from Illinois to the Gulf of Mexico, where the flux during the 1990s was about 244000 Mg N/yr, and illustrates the importance of reservoir denitrification as an N sink in Midwestern agricultural landscapes.
反硝化作用是水生沉积物中的一个重要过程,但在美国中西部上游那些接纳大量农业河流氮输入的水库的氮质量平衡中,其作用尚未得到评估。我们利用一个面积为4400公顷的水库来确定反硝化作用在氮质量平衡中的作用以及减少下游硝酸根氮输送的有效性。沉积物反硝化作用通过以下方式进行研究:(1)2002年3月至2003年3月期间,每月在伊利诺伊州中部谢尔比维尔湖水库的8个地点,采用乙炔抑制、氯霉素技术进行测量;(2)将测量结果按比例推算至整个水库,并与质量平衡中未计入的氮进行比较;(3)利用该水库长期(1981 - 2003年)的氮质量平衡进行间接估算。2002年春季和初夏期间,水库中的反硝化速率较高,此时测量到的硝酸根氮浓度最高(10 - 14毫克硝酸根氮/升)。我们估算该年的反硝化量在2580至5150公吨氮之间。质量平衡中缺失的氮为3004公吨氮,这表明沉积物反硝化作用是氮的汇。水库中沉积物反硝化的面积速率在62至225克氮×平方米⁻²×年⁻¹之间,速率是反硝化强度(微克氮×克干质量×小时⁻¹)和沉积物总量的函数。1981年至2003年,硝酸根氮的平均入流通量为8900公吨氮/年。约58%的总硝酸根氮输入被去除,作为输入百分比的年度硝酸根氮去除量与水库滞留时间显著相关(23年的平均值为0.36年,范围为0.21 - 0.84年)。通过将谢尔比维尔湖的反硝化作用按比例推算至伊利诺伊州的其他水库,我们估算氮汇为48900公吨氮/年。当与估算的河道内反硝化作用相结合时,估算沉积物反硝化作用去除的氮为60900公吨氮/年。这减少了从伊利诺伊州向墨西哥湾的河流输出,20世纪90年代期间该通量约为244000公吨氮/年,说明了水库反硝化作用作为中西部农业景观中氮汇的重要性。