Long‐Term Trajectory of Nitrogen Loading and Delivery From Mississippi River Basin to the Gulf of Mexico. Issue 5 (25th April 2020)

• Record Type: Journal Article
• Authors: Tian, Hanqin; Xu, Rongting; Pan, Shufen; Yao, Yuanzhi; Bian, Zihao; Cai, Wei‐Jun; Hopkinson, Charles S.; Justic, Dubravko; Lohrenz, Steven; Lu, Chaoqun; Ren, Wei; Yang, Jia
• Is Part Of: Global biogeochemical cycles. Volume 34:Issue 5(2020:May)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-04-25
• Subjects: Biogeochemical cycles -- Periodicals; Electronic journals; 577.1405
• DOI: 10.1029/2019GB006475
• Languages: English
• ISSNs: 0886-6236

Abstract

Abstract: The large areal extent of hypoxia in the northern Gulf of Mexico has been partially attributed to substantial nitrogen (N) loading from the Mississippi River basin, which is driven by multiple natural and human factors. The available water quality monitoring data and most of the current models are insufficient to fully quantify N load magnitude and the underlying controls. Here we use a process‐based Dynamic Land Ecosystem Model to examine how multiple factors (synthetic N fertilizer, atmospheric N deposition, land use changes, climate variability, and increasing atmospheric CO2 ) have affected the loading and delivery of total nitrogen (TN) consisting of ammonium and nitrate (dissolved inorganic N) and total organic nitrogen from the Mississippi River basin during 1901–2014. The model results indicate that TN export during 2000–2014 was twofold larger than that in the first decade of twentieth century: Dissolved inorganic N export increased by 140% dominated by nitrate; total organic nitrogen export increased by 53%. The substantial enrichment of TN export since the 1960s was strongly associated with increased anthropogenic N inputs (synthetic N fertilizer and atmospheric N deposition). The greatest export of TN was in the spring. Although the implementation of N reduction has been carried out over the past three decades, total N loads to the northern Gulf of Mexico have not decreased significantly. Due to the legacy effect from historical N accumulation in soils and riverbeds, a larger reduction in synthetic N fertilizer inputs as well as improved N management practices are needed to alleviate ocean hypoxia in the northern Gulf of Mexico. Key Points: Over the period 1901‐2014, DIN and TON export from the Mississippi River basin increased by 85% and 60%, respectively. The Ohio River basin was largest contributor to the increase among seven subbasins Synthetic N fertilizer application was the dominant contributor to increases in the export of DIN (70%) and TON (40%) since the 1970s The highest DIN and TON export occurred in the spring, accounting for 39% and 36% of the total export from the MRB during 1990‐2014