Our recentÌýÌýhasÌýexplored how long-term changes in land use, agriculture, atmospheric pollution and human waste generation and management has changed the flows of nutrients through our waterways.
Centuries of nutrient changeÌý
The past two centuries have seen huge changes in our landscapes and ways of lifeÌýthat haveÌýdrivenÌýbig changesÌýinÌýthe flows of macronutrients,Ìýcarbon nitrogen and phosphorus,Ìýin our environment.ÌýAgricultural expansion has changed plant cover, disrupting plant-soil nutrient cycles, and with the Green Revolution and the widespread adoption of inorganic fertilizer use came large additions of nitrogen and phosphorusÌýto the environment. Natural ecosystems too have been affected by large additions of nitrogen from atmospheric pollution, driven by rising fertilizer use and fossil fuel burning.ÌýRisingÌýpopulations, the introduction of the toilet,Ìýand the use of new products in the home such as detergents,ÌýhaveÌýalsoÌýmeant thatÌýwastewater has changed the flow of nutrients around our environment.ÌýÌý
A nutrient puzzleÌý
All thisÌýsimultaneous,Ìýlong-term,ÌýwidespreadÌýchange presents us with puzzleÌý– how can we understand how these various drivers have contributed to nutrientÌýcycleÌýchangeÌýandÌýthe consequences for terrestrial and aquatic ecosystems, and what can we learn that helps us manage nutrient flows and the negative knock-on effects in future? Computer modelling offers us a way to unpick this puzzle.ÌýÌý
The Long-Term Large-Scale project, funded by the Natural Environment Research Council’s Macronutrient ResearchÌýProgramme,Ìýbrought togetherÌýa diverse set ofÌýresearchersÌýto build an integrated model that interconnectsÌýnutrient processesÌýfrom atmosphere to plants and soils to waterways.ÌýJohn Quinton and Jess Davies were part of this modelling effort contributing key components in plant-soil biogeochemical and soil erosion modelling.ÌýÌý
Modelling the past to understand theÌýfutureÌý
TheÌý, published in Science of the Total Environment, communicates some of our findings from a freshwater perspective. Our modelling analysis indicatesÌýthat the rapid increase in the use of agriculturalÌýfertilisersÌýafter the second world war, and the rising human population, led to a rapid rise inÌýnitrogenÌýand phosphorusÌýfluxes to rivers, with nitrogen export to rivers quadruplingÌýand phosphorus increasing by a factor of 10Ìý(see figure exert below).ÌýDuring this period, the modelling shows that the dominant source ofÌýnitrogenÌýtoÌýriversÌýswitchedÌýfromÌýintenseÌýgrasslandsÌýto arable, the dissolved N export to rivers quadrupled, and P from human wasteÌýentering our waterwaysÌýincreased by ~600%, despiteÌýwaste waterÌýtreatment.ÌýÌý
This work highlights the extent to which we as humans have modified our nutrient worldÌýin the past, but it can also help us make a better future. This research and the modelling tools producedÌýcanÌýhelpÌýinform national nutrient budgets and targeting of water qualityÌýmeasures, andÌýhelp us set realistic targets for nutrient export and water quality status.Ìý

Exert from figure in Bell et al 2021: Export of carbon, nitrogen and phosphorus to UK waterways from soils 1800–2010.
If you are interested in other findings form the Long-Term Large Scale Macronutrient Change project, more outputs from the project are listed below:Ìý
- Measured estimates of semi-natural terrestrial NPP in Great Britain: comparison with modelled values, and dependence on atmospheric nitrogen deposition. Edward Tipping, Jessica A. C. Davies, Peter A. Henrys, Susan G. Jarvis, Edwin C. Rowe, Simon M. Smart, Michael G. Le Duc, Robert H. Marrs, Robin J.ÌýPakemanÌý(2019) Biogeochemistry 144, 215–227.ÌýÌýÌý
- Impact of two centuries of intensive agriculture on soil carbon, nitrogen and phosphorus cycling in the UK.ÌýS.E.Muhammed, K. Coleman,ÌýLianhaiÌýWu, V.A. Bell, J.A.C. Davies, J.N. Quinton, E.J. Carnell, S.J. Tomlinson, A.J. Dore, U.ÌýDragosits, P.S. Naden, M.J.ÌýGlendining, E. Tipping, A.P. Whitmore (2018). Science of the Total Environment 634, 1486–1504.ÌýÌýÌý
- Long-term increases in soil carbon due to ecosystem fertilization by atmospheric nitrogen deposition demonstrated by regional-scale modelling and observations.Ìý E. Tipping, J. A. C. Davies, P. A. Henrys, G. J. D. Kirk, A. Lilly, U.ÌýDragosits, E. J. Carnell, A. J. Dore, M. A. Sutton & S. J. Tomlinson.Ìý Scientific Reports 7, Article number: 1890 (2017)ÌýÌýÌý
- 150 years of macronutrient change in unfertilized UK ecosystems: Observations vs simulations.Ìý JAC Davies, E Tipping, AP Whitmore.Ìý Science of the Total Environment (2016)ÌýÌýÌý
- Long-term P weathering and recent N deposition control contemporary plant-soil C, N, and P. J.A.C. Davies,ÌýE.Tipping, E.C. Rowe, J.F. Boyle,ÌýE.GrafÌýPannatier, V. Martinsen (2016) Global Biogeochemical Cycles 30, 231-249.ÌýÌýÌý