4.7 Article

A Century-Long Trajectory of Phosphorus Loading and Export From Mississippi River Basin to the Gulf of Mexico: Contributions of Multiple Environmental Changes

期刊

GLOBAL BIOGEOCHEMICAL CYCLES
卷 36, 期 6, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022GB007347

关键词

phosphorus loading; terrestrial ecosystems; aquatic ecosystems; climate; anthropogenic activities; biogeochemical model

资金

  1. NSF [1903722, 1922687]
  2. NOAA Grant [NA16NOS4780204]
  3. NASA [NNX12AP84G, NNX14AO73G, NNX10AU06G]
  4. Direct For Education and Human Resources
  5. Division Of Graduate Education [1922687] Funding Source: National Science Foundation
  6. NASA [14155, NNX10AU06G, 122594, NNX12AP84G] Funding Source: Federal RePORTER

向作者/读者索取更多资源

Phosphorus control is crucial in mitigating eutrophication in aquatic ecosystems. However, our understanding of phosphorus dynamics along the land-ocean aquatic continuum and the lack of well-developed process models hinder effective control of phosphorus export from soils. This study coupled riverine phosphorus biogeochemical processes and water transport with terrestrial processes to assess the impact of environmental changes on phosphorus loading and export in the Mississippi River Basin. The findings emphasize the importance of adopting effective phosphorus management strategies to reduce soil erosion and improve phosphorus use efficiency in crop production.
Phosphorus (P) control is critical to mitigating eutrophication in aquatic ecosystems, but the effectiveness of controlling P export from soils has been limited by our poor understanding of P dynamics along the land-ocean aquatic continuum as well as the lack of well-developed process models that effectively couple terrestrial and aquatic biogeochemical P processes. Here, we coupled riverine P biogeochemical processes and water transport with terrestrial processes within the framework of the Dynamic Land Ecosystem Model to assess how multiple environmental changes, including fertilizer and manure P uses, land use, climate, and atmospheric CO2, have affected the long-term dynamics of P loading and export from the Mississippi River Basin to the Gulf of Mexico during 1901-2018. Simulations show that riverine exports of dissolved inorganic phosphorus (DIP), dissolved organic phosphorus, particulate organic phosphorus (POP), and particulate inorganic phosphorus (PIP) increased by 42%, 53%, 60%, and 53%, respectively, since the 1960s. Riverine DIP and PIP exports were the dominant components of the total P flux. DIP export was mainly enhanced by the growing mineral P fertilizer use in croplands, while increased PIP and POP exports were a result of the intensified soil erosion due to increased precipitation. Climate variability resulted in substantial interannual and decadal variations in P loading and export. Soil legacy P continues to contribute to P loading. Our findings highlight the necessity to adopt effective P management strategies to control P losses through reductions in soil erosion, and additionally, to improve P use efficiency in crop production.

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