Impacts of the Nitrogen Cascade on Ecosystems Presentation to NYSERDA October 8, 2003 William Moomaw Fletcher School, Tufts University
Reactive N and Unreactive N 2 Unreactive N is N 2 (78% of earth’s atmosphere) Reactive N (Nr) includes all biologically, chemically and physically active N compounds in the atmosphere and biosphere of the Earth N controls productivity of most natural ecosystems N 2 is converted to Nr by biological nitrogen fixation (BNF) N 2 is converted to Nr by humans fossil fuel combustion, the Haber Bosch process, and cultivation-induced BNF.
Reactive N and Unreactive N 2 Unreactive N is N 2 (78% of earth’s atmosphere) Reactive N (Nr) includes all biologically, chemically and physically active N compounds in the atmosphere and biosphere of the Earth N controls productivity of most natural ecosystems N 2 is converted to Nr by b iological nitrogen fixation (BNF) N 2 is converted to Nr by humans f ossil fuel combustion , the Haber Bosch process , and cultivation-induced BNF. Bottom Lines – Humans create more Nr than do natural terrestrial processes. – Nr is accumulating in the environment. – Nr accumulation contributes to most environment issues of the day. – Challenge is to reduce anthropogenic Nr creation.
Reactive N and Unreactive N 2 Unreactive N is N 2 (78% of earth’s atmosphere) Reactive N (Nr) includes all biologically, chemically and physically active N compounds in the atmosphere and biosphere of the Earth N controls productivity of most natural ecosystems N 2 is converted to Nr by b iological nitrogen fixation (BNF) N 2 is converted to Nr by humans f ossil fuel combustion , the Haber Bosch process , and cultivation-induced BNF. Bottom Lines – Humans create more Nr than do natural terrestrial processes. – Nr is accumulating in the environment. – Nr accumulation contributes to most environment issues of the day. – Challenge is to reduce anthropogenic Nr creation. But, this is complicated by fact that Nr creation sustains most of the world’s food needs. – The real challenge is how can we provide food (and energy) while also reducing Nr creation rates and arresting the nitrogen cascade ?
zyxwvutsrqponmlkjihgfedcbaWUTSRPONMLKJIHGFEDCBA Reactive Nitrogen Cuts Across Multiple Global Issues and Environmental Agreements Regional air quality (LRTAP) Climate change (UNFCCC & Kyoto Prot.) Ozone Depletion (Montreal Protocol) Biodiversity loss (CBD) Transboundary water quality (Non-navigational Uses of International Water Courses Estuary damage (Regional Seas) Fisheries loss (Law of the Sea?)
Need for an Integrated Analytical Policy Approach to Reactive Nitrogen First explain history of human alteration of nitrogen cycle Identify the reasons why reactive nitrogen cascades through so many segments of the global ecosystem Describe the International Nitrogen Initiative
The History of Nitrogen --Global Population & Discovery of N-- 7,000 6,000 5,000 4,000 3,000 2,000 N-Discovered 1,000 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
The History of Nitrogen --Major N processes-- 7,000 6,000 5,000 4,000 3,000 2,000 BNF N-Discovered N-Nutrient 1,000 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
Nr Creation by Cultivation --So that’s why we plant soybeans-- 7,000 200 6,000 150 5,000 4,000 100 3,000 2,000 BNF 50 N-Discovered N-Nutrient 1,000 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Legumes/Rice, Tg N Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
Nr Creation by Fossil Fuel Combustion --Nr produced by accident-- 7,000 200 6,000 150 5,000 4,000 100 3,000 2,000 BNF 50 N-Discovered N-Nutrient 1,000 N 2 + O 2 --> 2NO 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Legumes/Rice, Tg N NOx emissions, Tg N zyxwvutsrqponmlkjihgfedcbaWVUTSRQPONMLIHGFEDCBA Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
The History of Nitrogen --A British chemists view-- 7,000 200 6,000 150 5,000 4,000 100 World is running out of N * 3,000 2,000 BNF 50 N-Discovered N-Nutrient 1,000 N 2 + O 2 --> 2NO 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Legumes/Rice, Tg N NOx emissions, Tg N zyxwvutsrqponmlkjihgfedcbaWVUTSRQPONMLIHGFEDCBA * 1898, Sir William Crookes, president of the British Association for the Advancement of Science Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
The History of Nitrogen --German science at the forefront-- 7,000 200 6,000 150 5,000 N 2 + 3H 2 4,000 --> 2NH 3 100 3,000 2,000 BNF 50 N-Discovered N-Nutrient 1,000 N 2 + O 2 --> 2NO 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Legumes/Rice, Tg N NOx emissions, Tg N zyxwvutsrqponmlkjihgfedcbaWVUTSRQPONMLIHGFEDCBA Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
Nr Creation by Haber-Bosch --most used for fertilizer-- 7,000 200 6,000 150 5,000 N 2 + 3H 2 --> 2NH 3 4,000 100 3,000 H-B 2,000 BNF 50 N-Discovered N-Nutrient 1,000 N 2 + O 2 --> 2NO 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Haber Bosch Legumes/Rice, Tg N NOx emissions, Tg N zyxwvutsrqponmlkjihgfedcbaWVUTSRQPONMLIHGFEDCBA Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
N r Creation by Food and Energy Production 7,000 200 6,000 150 5,000 4,000 100 3,000 BNF H-B 2,000 50 N-Nutrient N-Discovered 1,000 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Energy Production Food Production Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
N r Creation by Food and Energy Production 7,000 200 6,000 150 5,000 4,000 { 100 3,000 Nr, natural H-B 2,000 BNF 50 N-Nutrient N-Discovered 1,000 0 0 1750 1800 1850 1900 1950 2000 2050 Humans, millions Total N Fixed, Tg Galloway JN and Cowling EB. 2002; Galloway et al., 2002a
N Drivers in 1860 Grain Production Meat Production Energy Production
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 N 2 N NO y NO NH x NH 2 y x 1860 120 120 Galloway et al., 2002b
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 N 2 N NO y NO NH x NH 2 y x 1860 120 120 15 15 0.3 0.3 Galloway et al., 2002b
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 6 N 2 6 N NO y NO NH x NH 2 y x 9 9 8 6 8 6 1860 120 120 8 11 8 7 7 11 15 15 6 6 0.3 0.3 27 27 Galloway et al., 2002b
Nitrogen Drivers in 1860 & 1995 Grain Production Meat Production Energy Production
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 6 N 2 6 N NO y NO NH x NH 2 y x 9 9 8 6 8 6 1860 120 120 8 11 8 7 7 11 15 15 6 6 0.3 0.3 27 27 5 5 mid-1990s N 2 N NO y NO NH x NH 2 y x 110 110 Galloway et al., 2002b
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 6 N 2 6 N NO y NO NH x NH 2 y x 9 9 8 6 8 6 1860 120 120 8 11 8 7 7 11 15 15 6 6 0.3 0.3 27 27 5 5 mid-1990s N 2 N NO y NO NH x NH 2 y x 33 33 110 110 100 100 25 25 N 2 + 3H 2 2NH 3 Galloway et al., 2002b
The Global Nitrogen Budget in 1860 and mid-1990s, TgN/yr 5 5 6 N 2 6 N NO y NO NH x NH 2 y x 9 9 8 6 8 6 1860 120 120 8 11 8 7 7 11 15 15 6 6 0.3 0.3 27 27 5 5 6 6 mid-1990s N 2 N NO y NO NH x NH 2 y x 26 23 26 33 16 16 33 23 18 18 110 21 110 21 25 39 25 39 100 100 25 25 N 2 + 3H 2 48 48 2NH 3 Galloway et al., 2002b
zyxwvutsrqponmlkjihgfedcbaWVUTSRQPONMLIHGFEDCBA Nr Riverine Fluxes 1860 (left) and 1990 (right) TgN/yr 9.1 21.8 5 7.8 4.4 8.3 7.7 8.5 7.4 9.7 zyxwvutsrqponmlkjihgfedcbaWUTSRPONMLKJIHGFEDCBA 2.1 2 -> all regions increase riverine fluxes -> Asia becomes dominant Galloway et al, 2002b; Boyer et al., in preparation
Nitrogen Deposition Past and Present mg N/m 2 /yr 5000 2000 1000 750 zyxwvutsrqponmlkjihgfedcbaWUTSRPONMLKJIHGFEDCBA 500 250 100 50 25 5 1993 1860 Galloway and Cowling, 2002; Galloway et al., 2002b
Mid-Course Summary Summary Next Questions Humans mobilize ~50% What are the consequences more Nr than natural of Nr accumulation? terrestrial ecosystems. – Food production accounts What is projected for future? for 75% Nr is widely dispersed How can science and policy – Atmospheric Nr emissions respond? have increased 3-fold since 1860; NH 3 twice as important as NO x Nr is accumulating in ecosystems and the atmosphere.
Nr and Agricultural Ecosystems Haber-Bosch has facilitated agricultural intensification 40% of world’s population is alive because of it An additional 3 billion people by 2050 will be sustained by it Most N that enters agroecosystems is released to the environment.
Nr and the Atmosphere NO x emissions contribute to OH, which defines the oxidizing capacity of the atmosphere NO x emissions are responsible for tens of thousands of excess- deaths per year in the United States O 3 and N 2 O contribute to atmospheric warming N 2 O emissions contribute to stratospheric O 3 depletion
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