An Introduction to the Nitrogen Cycle
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Water Cycle
Natural Resource Management Basic concepts and strategies 1 This publication was co-financed by the Catholic Relief Services (CRS) and the generous support of the American people through the United States Agency of International Development (USAID) Office of Acquisition and Assistance under the terms of Leader with Associates Cooperative Agreement No. AID-OAA-L-10-00003 with the University of Illinois at Urbana Champaign for the Modernizing Extension and Advisory Services (MEAS) Project. MEAS aims at promoting and assisting in the modernization of rural extension and advisory services worldwide through various outputs and services. The services benefit a wide audience of users, including developing country policymakers and technical specialists, development practitioners from NGOs, other donors, and consultants, and USAID staff and projects. Catholic Relief Services (CRS) serves the poor and disadvantaged overseas. CRS provides emergency relief in the wake of natural and man-made disasters and promotes the subsequent recovery of communities through integrated development interventions, without regard to race, creed or nationality. CRS’ programs and resources respond to the U.S. Bishops’ call to live in solidarity – as one human family – across borders, over oceans, and through differences in language, culture and economic condition. CRS provided co-financing for this publication. Catholic Relief Services 228 West Lexington Street Baltimore, MD 21201-3413 USA Illustrations: Jorge Enrique Gutiérrez Printed in the United States of America. ISBN x-xxxxxx-xx-x Download this publication and related material at http://crsprogramquality.org/ or at http://www.meas-extension.org/meas-offers/training © 20[nn] Catholic Relief Services – United States Conference of Catholic Bishops and MEAS project This work is licensed under a Creative Commons Attribution 3.0 Unported License. -
Ecological Principles and Function of Natural Ecosystems by Professor Michel RICARD
Intensive Programme on Education for sustainable development in Protected Areas Amfissa, Greece, July 2014 ------------------------------------------------------------------------ Ecological principles and function of natural ecosystems By Professor Michel RICARD Summary 1. Hierarchy of living world 2. What is Ecology 3. The Biosphere - Lithosphere - Hydrosphere - Atmosphere 4. What is an ecosystem - Ecozone - Biome - Ecosystem - Ecological community - Habitat/biotope - Ecotone - Niche 5. Biological classification 6. Ecosystem processes - Radiation: heat, temperature and light - Primary production - Secondary production - Food web and trophic levels - Trophic cascade and ecology flow 7. Population ecology and population dynamics 8. Disturbance and resilience - Human impacts on resilience 9. Nutrient cycle, decomposition and mineralization - Nutrient cycle - Decomposition 10. Ecological amplitude 11. Ecology, environmental influences, biological interactions 12. Biodiversity 13. Environmental degradation - Water resources degradation - Climate change - Nutrient pollution - Eutrophication - Other examples of environmental degradation M. Ricard: Summer courses, Amfissa July 2014 1 1. Hierarchy of living world The larger objective of ecology is to understand the nature of environmental influences on individual organisms, populations, communities and ultimately at the level of the biosphere. If ecologists can achieve an understanding of these relationships, they will be well placed to contribute to the development of systems by which humans -
Learning the Water, Carbon and Nitrogen Cycles Through the Effects of Intensive Farming Techniques
Learning the Water, Carbon and Nitrogen Cycles through the Effects of Intensive Farming Techniques Winnie Chan Furness High School Overview Rationale Objectives Strategies Classroom Activities Annotated Bibliography/Resources Appendices/Content Standards Overview Elements of natural substances are constantly cycling through Earth. Water, carbon, and nitrogen move through Earth’s many ecosystems in closed paths called the biogeochemical cycles. In this unit, students will learn about these cycles by understanding modern farming techniques used to produce enough food to feed a world population of 7.8 billion. Students will plan and carry out experiments, analyze and interpret data, and communicate the information learned. This curriculum unit is intended for Biology students in Grades 9 and 10. The lessons are meant to be incorporated into “Unit 10: Ecology” of the School District of Philadelphia’s Core Curriculum for Biology, which is typically taught at the end of the year (May/June). Rationale The biogeochemical cycles operate on a fixed amount of matter on Earth. While the total amounts of water, carbon and nitrogen do not change, these substances exist in many different forms. Water is found on Earth as solid ice, liquid water or gaseous vapor. Carbon and nitrogen both exist as in the atmosphere as carbon dioxide gas and nitrogen gas, respectively, or as an integrated part of living and non-living substances. The hydrologic or water cycle describes the constant movement of water through Earth and its atmosphere. Major processes of -
Biogeochemical Cycles
Biogeochemical Cycles Essential Knowledge Objectives 2.A.3 (a) Biogeochemical Cycles • Cycle inorganic and organic nutrients between organisms and the environment – Carbon cycle – Nitrogen cycle – Phosphorus cycle – Water cycle (also known as the hydrological cycle) Cycling of Matter • Organisms must exchange matter with the environment to grow, reproduce and maintain organization • Molecules and atoms from the environment are necessary to build new molecules Molecules Essential for Life • Carbohydrates – composed of C, H, and O, monomer is a monosaccharide • Lipids – composed of C, H, and O, monomers are fatty acids and glycerol • Proteins – composed of C, H, O, N, and S in trace amounts, monomers are amino acids • Nucleic Acids – composed of C, H, O, N and P, monomers are nucleotides Carbon • Carbon moves from the environment to organisms where it is used to build the essential organic molecules • Carbon is used in storage compounds and cell formation in all organisms Carbon in the Environment • Carbon found in something non-living is called inorganic carbon • Inorganic carbon is found in rocks (limestone), shells, the atmosphere and the oceans • Living organisms must “fix” inorganic carbon into organic carbon to build the organic compounds necessary for life Carbon Cycle Nitrogen and Phosphorus • Nitrogen moves from the environment to organisms where it is used to build proteins and nucleic acids • Phosphorus moves from the environment to organisms where it is used to build nucleic acids, certain lipids, and ATP (cell energy) Nitrogen -
Earth Systems and Interactions
The Earth System Earth Systems and Interactions Key Concepts • How do Earth systems What do you think? Read the three statements below and decide interact in the carbon whether you agree or disagree with them. Place an A in the Before column cycle? if you agree with the statement or a D if you disagree. After you’ve read • How do Earth systems this lesson, reread the statements to see if you have changed your mind. interact in the phosphorus Before Statement After cycle? 1. The amount of water on Earth remains constant over time. 2. Hydrogen makes up the hydrosphere. 3. Most carbon on Earth is in the atmosphere. 3TUDY#OACH Earth Systems Make a Table Contrast the carbon cycle and the Your body contains many systems. These systems work phosphorus cycle in a two- together and make one big system—your body. Earth is a column table. Label one system, too. Like you, Earth has smaller systems that work column Carbon Cycle and together, or interact, and make the larger Earth system. Four the other column Phosphorus of these smaller systems are the atmosphere, the Cycle. Complete the table hydrosphere, the geosphere, and the biosphere. as you read this lesson. The Atmosphere Reading Check The outermost Earth system is a mixture of gases and 1. Identify What systems particles of matter called the atmosphere. It forms a layer make up the larger Earth around the other Earth systems. The atmosphere is mainly system? nitrogen and oxygen. Gases in the atmosphere move freely, helping transport matter and energy among Earth systems. -
What Is the Water Cycle? Evapotranspiration the Water Cycle Describes the Existence and Movement of Water On, In, and Above the Earth
What is the water cycle? Evapotranspiration The water cycle describes the existence and movement of water on, in, and above the Earth. Earth's water is always in movement and is always changing states, from liquid to vapor to ice and back again. In general, evapotranspiration is the sum of evaporation and transpiration. Evapotranspiration is defined as the Precipitation water lost to the atmosphere from the ground surface, evaporation from the Precipitation is water capillary fringe of the groundwater released from clouds in the table, and the transpiration of form of rain, freezing rain, groundwater by plants whose roots sleet, snow, or hail. It is tap the capillary fringe of the the primary connection in groundwater table. the water cycle that The transpiration aspect of evapotranspiration is essentially provides for the delivery of evaporation of water from plant leaves. Transpiration accounts atmospheric water to the for about 10 percent of the moisture in the atmosphere, with Earth. Most precipitation oceans, seas, and other bodies of water (lakes, rivers, falls as rain. streams) providing nearly 90 percent, and a tiny amount coming from sublimation (ice changing into water vapor Infiltration without first becoming liquid). Anywhere in the world, a portion of the water that falls as rain and snow infiltrates into the subsurface Evaporation soil and rock. How much infiltrates depends greatly on a number of factors, such as ground cover or soil Evaporation is the type. process by which water changes from a liquid to a Some water that infiltrates will remain in the shallow gas or vapor. Evaporation soil layer, where it will gradually move vertically and is the primary pathway horizontally through the soil and subsurface material. -
Human Alteration of the Global Nitrogen Cycle
What is Nitrogen? Human Alteration of the Nitrogen is the most abundant element in Global Nitrogen Cycle the Earth’s atmosphere. Nitrogen makes up 78% of the troposphere. Nitrogen cannot be absorbed directly by the plants and animals until it is converted into compounds they can use. This process is called the Nitrogen Cycle. Heather McGraw, Mandy Williams, Suzanne Heinzel, and Cristen Whorl, Give SIUE Permission to Put Our Presentation on E-reserve at Lovejoy Library. The Nitrogen Cycle How does the nitrogen cycle work? Step 1- Nitrogen Fixation- Special bacteria convert the nitrogen gas (N2 ) to ammonia (NH3) which the plants can use. Step 2- Nitrification- Nitrification is the process which converts the ammonia into nitrite ions which the plants can take in as nutrients. Step 3- Ammonification- After all of the living organisms have used the nitrogen, decomposer bacteria convert the nitrogen-rich waste compounds into simpler ones. Step 4- Denitrification- Denitrification is the final step in which other bacteria convert the simple nitrogen compounds back into nitrogen gas (N2 ), which is then released back into the atmosphere to begin the cycle again. How does human intervention affect the nitrogen cycle? Nitric Oxide (NO) is released into the atmosphere when any type of fuel is burned. This includes byproducts of internal combustion engines. Production and Use of Nitrous Oxide (N2O) is released into the atmosphere through Nitrogen Fertilizers bacteria in livestock waste and commercial fertilizers applied to the soil. Removing nitrogen from the Earth’s crust and soil when we mine nitrogen-rich mineral deposits. Discharge of municipal sewage adds nitrogen compounds to aquatic ecosystems which disrupts the ecosystem and kills fish. -
Nitrogen Metabolism in Phytoplankton - Y
MARINE ECOLOGY – Nitrogen Metabolism in Phytoplankton - Y. Collos, J. A. Berges NITROGEN METABOLISM IN PHYTOPLANKTON Y. Collos Laboratoire d'Hydrobiologie CNRS, Université Montpellier II, France J. A. Berges School of Biology and Biochemistry, Queen's University of Belfast, UK Keywords: uptake, reduction, excretion, proteases, chlorophyllases, cell death. Contents 1. Introduction 2. Availability and use of different forms of nitrogen 2.1 Nitrate 2.2. Nitrite 2.3. Ammonium 2.4. Molecular N2 2.5. Dissolved organic N (DON) 2.6. Particulate nitrogen (PN) 3. Assimilation pathways 4. Accumulation and storage 4.1. Inorganic compounds 4.2. Organic compounds 5. Nutrient classification and preferences 6. Plasticity in cell composition 7. Overflow mechanisms: excretion and release processes 8. Recycling of N within the cell 9. Degradation pathways 9.1. Requirements for and roles of degradation 9.2. How is degradation accomplished? 9.3. Variation in degradation 9.4. Pathogenesis and Cell Death 10. From uptake to growth: time-lag phenomena 11. Relationships with carbon metabolism 12. Future directions AcknowledgementsUNESCO – EOLSS Glossary Bibliography SAMPLE CHAPTERS Biographical Sketches Summary Phytoplankton use a large variety of nitrogen compounds and are extremely well adapted to fluctuating environmental conditions by a high capacity to change their chemical composition.Degradation and turnover of nitrogen within phytoplankton is essential for many processes including normal cell maintenance, acclimations to changes in light, salinity, and nutrients, and cell defence against pathogens. The ©Encyclopedia of Life Support Systems (EOLSS) MARINE ECOLOGY – Nitrogen Metabolism in Phytoplankton - Y. Collos, J. A. Berges pathways by which N degradation is accomplished are very poorly understood, but based on work in higher plant species, protein degradation is likely to be of central importance. -
Human Alteration of the Global Nitrogen Cycle: Causes And
Published by the Ecological Society of America Number 1, Spring 1997 Causes andConsequences Human Alterationofthe Issues in EcologyGlobal NitrogenCycle: Photo by Nadine Cavender Issues in Ecology Number 1 Spring 1997 Human Alteration of the Global Nitrogen Cycle: Causes and Consequences SUMMARY Human activities are greatly increasing the amount of nitrogen cycling between the living world and the soil, water, and atmosphere. In fact, humans have already doubled the rate of nitrogen entering the land-based nitrogen cycle, and that rate is continuing to climb. This human-driven global change is having serious impacts on ecosystems around the world because nitrogen is essential to living organisms and its availability plays a crucial role in the organization and functioning of the worlds ecosystems. In many ecosystems on land and sea, the supply of nitrogen is a key factor controlling the nature and diversity of plant life, the population dynamics of both grazing animals and their predators, and vital ecologi- cal processes such as plant productivity and the cycling of carbon and soil minerals. This is true not only in wild or unmanaged systems but in most croplands and forestry plantations as well. Excessive nitrogen additions can pollute ecosystems and alter both their ecological functioning and the living communities they support. Most of the human activities responsible for the increase in global nitrogen are local in scale, from the production and use of nitrogen fertilizers to the burning of fossil fuels in automobiles, power generation plants, and industries. However, human activities have not only increased the supply but enhanced the global movement of various forms of nitrogen through air and water. -
Chapter 3. Nutrient Cycling by Fungi in Wet Tropical Forests
Chapter 3 Nutrient cycling by fungi in wet tropical forests D. Jean Lodge U.S.D.A. Forest Service, Forest Products Laboratory, Center for Forest Mycology Reseach, PO Box B, Palmer, Pueto Rico 00721, U.S.A. Introduction Fungi are primarily responsible for the recycling of mineral nutrients through decomposition of organic matter (Swift, Heal & Anderson, 1979) and the uptake and transfer of these nutrients into plants via mycorrizal fungi (Janos, 1983). In addition, fungi and other soil microorganisms serve alternately as sources and sinks of labile nutrients that are necessary for plant growth (Marumoto, Anderson & Domsch 1983 Yang & Insam 1991). Thus, fungal and microbial biomass can control significant fractions of the labile nutrient pools in some humid and wet tropical forests (Marumoto et al., 1982; Lodge, 1985; Yang & Insam, 1991), and regulate the availability of nutrients that may limit plant growth (Jordan 1985; Hilton, 1987; Singh et al., 1989 Lee, Han & Jordan 1990 Behera Pati & Basu, 1991; Yang & Insam, 1991). The term biomass normally refers only to living organisms, but it is used more broadly in this chapter to refer to dead as well as living microorganisms as both contain nutrients. Although humid tropical forests often have large stature and an abundance of vegetation, their growth and productivity is frequently limited by the availability of mineral nutrients. A diversity of soils occurs in the wet tropics so it is difficult to generalise about nutrient limitation. However, the availability of phosphorus to higher plants is generally limited because phosphorus combines with aluminium and iron oxides in the highly weathered soils to form insoluble complexes (Sanchez 1976). -
Carbon–Nitrogen Interactions in Idealized Simulations with JSBACH (Version 3.10)
Geosci. Model Dev., 10, 2009–2030, 2017 www.geosci-model-dev.net/10/2009/2017/ doi:10.5194/gmd-10-2009-2017 © Author(s) 2017. CC Attribution 3.0 License. Carbon–nitrogen interactions in idealized simulations with JSBACH (version 3.10) Daniel S. Goll1,a, Alexander J. Winkler2,3, Thomas Raddatz2, Ning Dong3,5, Ian Colin Prentice4,6, Philippe Ciais1, and Victor Brovkin2 1Le Laboratoire des Sciences du Climat et de l’Environnement, IPSL-LSCE CEA/CNRS/UVSQ Saclay, Gif sur Yvette, France 2Max Planck Institute for Meteorology, Hamburg, Germany 3International Max Planck Research School on Earth System Modeling, Hamburg, Germany 4Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia 5Faculty of Agriculture and Environment, Department of Environmental Sciences, University of Sydney, NSW 2006, Australia 6AXA Chair in Biosphere and Climate Impacts, Department of Life Sciences, Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, UK aformerly at: Max Planck Institute for Meteorology, Hamburg, Germany Correspondence to: Daniel S. Goll ([email protected]) Received: 17 December 2016 – Discussion started: 9 January 2017 Revised: 7 April 2017 – Accepted: 14 April 2017 – Published: 22 May 2017 Abstract. Recent advances in the representation of soil car- The strengths of the land carbon feedbacks of the re- −1 bon decomposition and carbon–nitrogen interactions imple- cent version of JSBACH, with βL D 0:61 Pgppm and γL D mented previously into separate versions of the land sur- −27:5 Pg ◦C−1, are 34 and 53 % less than the averages of face scheme JSBACH are here combined in a single version, CMIP5 models, although the CMIP5 version of JSBACH which is set to be used in the upcoming 6th phase of coupled simulated βL and γL, which are 59 and 42 % higher than model intercomparison project (CMIP6). -
The Importance of Soil Food Web for Healthy Environment and Sustainable Development
International Journal of Applied Research 2015; 1(3): 15-20 ISSN Print: 2394-7500 ISSN Online: 2394-5869 Impact Factor: 3.4 The importance of soil food web for healthy IJAR 2015; 1(3): 15-20 www.allresearchjournal.com environment and sustainable development Received: 18-01-2015 Accepted: 08-02-2015 Rajeev Ranjan, M. Divya and M. Bavitha Rajeev Ranjan Abstract PG Research Scholar, Soil food web is a natural network of consumer resource interactions among different functional Dept. of Aquaculture, groups of soil organisms which are occur in the soil ecosystem. Soil is a complex, unconsolidated Fisheries College & Research mixture of inorganic, organic, and living material that is found on the immediate surface of the earth Institute, TNFU, that supports many important functions for plants, animals, and humans. The soil food web is very Thoothukudi-8, dynamic, complex and interchanging depending on its ecosystem. Nutrients in soil in their most basic Tamil Nadu, India. form come from fully decomposed organic matter which we call compost. Decomposition of organic matter is largely a biological process that occurs naturally. The organisms found in the soil food web M. Divya PG Research Scholar, carry out a large amount of microbial processes such as decomposition, mineralization, Dept. of Aquatic environment immobilization, respiration, and fixation along with many others. Without soil food web, plants management, would not obtain the nutrients which are necessary for growth. Nutrient exchanges between organic Fisheries College & Research matter, water and soil are essential to soil fertility and need to be maintained for sustainable Institute, TNFU, Thoothukudi- production. A diverse and complete soil food web where soils are well structured and fertile through 8, T.N.