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进入墨西哥湾的氮输入。

Nitrogen input to the Gulf of Mexico.

作者信息

Goolsby D A, Battaglin W A, Aulenbach B T, Hooper R P

机构信息

U.S. Geological Survey, MS406, DFC, Lakewood, CO 80225, USA.

出版信息

J Environ Qual. 2001 Mar-Apr;30(2):329-36. doi: 10.2134/jeq2001.302329x.

Abstract

Historical streamflow and concentration data were used in regression models to estimate the annual flux of nitrogen (N) to the Gulf of Mexico and to determine where the nitrogen originates within the Mississippi Basin. Results show that for 1980-1996 the mean annual total N flux to the Gulf of Mexico was 1,568,000 t yr-1. The flux was about 61% nitrate N, 37% organic N, and 2% ammonium N. The flux of nitrate N to the Gulf has approximately tripled in the last 30 years with most of the increase occurring between 1970 and 1983. The mean annual N flux has changed little since the early 1980s, but large year-to-year variations in N flux occur because of variations in precipitation. During wet years the N flux can increase by 50% or more due to flushing of nitrate N that has accumulated in the soils and unsaturated zones in the basin. The principal source areas of N are basins in southern Minnesota, Iowa, Illinois, Indiana, and Ohio that drain agricultural land. Basins in this region yield 1500 to more than 3100 kg N km-2 yr-1 to streams, several times the N yield of basins outside this region.

摘要

历史流量和浓度数据被用于回归模型,以估算流入墨西哥湾的氮(N)年通量,并确定氮在密西西比河流域内的来源地。结果表明,1980 - 1996年期间,流入墨西哥湾的年均总氮通量为156.8万吨/年。该通量中约61%为硝酸盐氮,37%为有机氮,2%为铵态氮。在过去30年里,流入墨西哥湾的硝酸盐氮通量大约增加了两倍,大部分增加发生在1970年至1983年之间。自20世纪80年代初以来,年均氮通量变化不大,但由于降水量的变化,氮通量存在较大的逐年波动。在湿润年份,由于流域土壤和非饱和带中积累的硝酸盐氮被冲刷,氮通量可增加50%或更多。氮的主要来源地是明尼苏达州南部、爱荷华州、伊利诺伊州、印第安纳州和俄亥俄州的流域,这些流域排水的是农业用地。该地区的流域向河流输送的氮量为1500至超过3100千克氮/平方千米·年,是该地区以外流域氮产量的几倍。

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