Environmental Studies (CYL-101) Unit-II: Ecosystems
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Biogeochemistry of Mediterranean Wetlands: a Review About the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions
water Review Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions Inmaculada de Vicente 1,2 1 Departamento de Ecología, Universidad de Granada, 18071 Granada, Spain; [email protected]; Tel.: +34-95-824-9768 2 Instituto del Agua, Universidad de Granada, 18071 Granada, Spain Abstract: Although Mediterranean wetlands are characterized by extreme natural water level fluctu- ations in response to irregular precipitation patterns, global climate change is expected to amplify this pattern by shortening precipitation seasons and increasing the incidence of summer droughts in this area. As a consequence, a part of the lake sediment will be exposed to air-drying in dry years when the water table becomes low. This periodic sediment exposure to dry/wet cycles will likely affect biogeochemical processes. Unexpectedly, to date, few studies are focused on assessing the effects of water level fluctuations on the biogeochemistry of these ecosystems. In this review, we investigate the potential impacts of water level fluctuations on phosphorus dynamics and on greenhouse gases emissions in Mediterranean wetlands. Major drivers of global change, and specially water level fluctuations, will lead to the degradation of water quality in Mediterranean wetlands by increasing the availability of phosphorus concentration in the water column upon rewetting of dry sediment. CO2 fluxes are likely to be enhanced during desiccation, while inundation is likely to decrease cumulative CO emissions, as well as N O emissions, although increasing CH emissions. Citation: de Vicente, I. 2 2 4 Biogeochemistry of Mediterranean However, there exists a complete gap of knowledge about the net effect of water level fluctuations Wetlands: A Review about the Effects induced by global change on greenhouse gases emission. -
The Global Marine Phosphorus Cycle: Sensitivity to Oceanic Circulation
Biogeosciences, 4, 155–171, 2007 www.biogeosciences.net/4/155/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. The global marine phosphorus cycle: sensitivity to oceanic circulation C. P. Slomp and P. Van Cappellen Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, The Netherlands Received: 4 September 2006 – Published in Biogeosciences Discuss.: 5 October 2006 Revised: 8 January 2007 – Accepted: 20 February 2007 – Published: 22 February 2007 Abstract. A new mass balance model for the coupled ma- stand long-term variations in marine biological activity, at- rine cycles of phosphorus (P) and carbon (C) is used to ex- mospheric composition and climate (Holland, 1984; Van amine the relationships between oceanic circulation, primary Cappellen and Ingall, 1996; Petsch and Berner, 1998; Bjer- productivity, and sedimentary burial of reactive P and partic- rum and Canfield, 2002). Important forcings include the sup- ulate organic C (POC), on geological time scales. The model ply of reactive P from the continents, oceanic circulation and explicitly represents the exchanges of water and particulate sea level fluctuations (Follmi,¨ 1996; Compton et al., 2000; matter between the continental shelves and the open ocean, Handoh and Lenton, 2003; Wallmann, 2003; Bjerrum et al., and it accounts for the redox-dependent burial of POC and 2006). the various forms of reactive P (iron(III)-bound P, particu- Upward transport of nutrient-rich water sustains biologi- late organic P (POP), authigenic calcium phosphate, and fish cal activity in marine surface waters. Vertical mixing, how- debris). Steady state and transient simulations indicate that ever, also controls the ventilation of the deeper ocean waters, a slowing down of global ocean circulation decreases pri- which in turn has a major effect on the sedimentary burial mary production in the open ocean, but increases that in the of phosphorus. -
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. -
Effects of Fertilisation on Phosphorus Pools in the Volcanic Soil of a Managed Tropical Forest
Forest Ecology and Management 258 (2009) 2199–2206 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Effects of fertilisation on phosphorus pools in the volcanic soil of a managed tropical forest Dean F. Meason a,*, Travis W. Idol a, J.B. Friday a, Paul G. Scowcroft b a Department of Natural Resources and Environmental Management, College of Tropical Agriculture and Human Resources, Sherman Laboratory, University of Hawaii, 1910 East West Road, Honolulu, HI 96822, USA b Institute of Pacific Islands Forestry, Pacific Southwest Research Station, USDA Forest Service, 60 Nowelo Street, Hilo, HI 96720, USA ARTICLE INFO ABSTRACT Article history: Acacia koa forests benefit from phosphorus fertilisation, but it is unknown if fertilisation is a short or long Received 31 July 2008 term effect on P availability. Past research suggests that P cycling in soils with high P sorption capacity, Received in revised form 30 March 2009 such as Andisols, was through organic pathways. We studied leaf P and soil P fractions in a tropical forest Accepted 2 April 2009 Andisol for 3 years after fertilisation with triple super phosphate. Leaf P concentration and labile P remained high after fertilisation. Fertilisation had increased all the inorganic P fractions over the length Keywords: of the study, while organic P fractions had not. The results suggested that the organic P fractions had a Hedley fractionation reduced role as a source of labile P after fertilisation. The size and dynamics of the sodium hydroxide- and Phosphorus fertilization hydrochloric acid-extractable P pools would suggest that either pool could be major sources of labile P. -
Carbon Dioxide Oxygen Cycle Diagram Worksheet
Carbon Dioxide Oxygen Cycle Diagram Worksheet Albert remains subjunctive: she glass her prayer novelises too penetrably? Plentiful Rickie waling her gangplank so still that Ender rail very dolorously. Puffingly needed, Dominic sleeved half-pike and cooperate epicenter. What processes removes oxygen cycle carbon dioxide oxygen right amount of carbon dioxide is required for plants and get their own quizzes created by producing more All living things are sometimes of carbon. Carbon Dioxide Oxygen Cycle Worksheet. Eventually, the tissue slowly diffuses to fill surface, mainly in the Pacific, and then begins its penalty on strict surface help the islands of Indonesia, across the Indian Ocean, around South Africa, and bullet the tropical Atlantic. Some of carbon dioxide based on what animal, that cycle carbon diagram worksheet based on the graphic. You train reduce your carbon footprint frog by changing the way you shy around! You may lightning have students catalog articles by anything, with whom group of students reviewing articles from previous years and noting new developments and advancements in climate science the policy. Which open the following processes removes carbon dioxide from the atmosphere? It down the wide common element of subsequent human body. It plays an error while trying to living organisms live, oxygen carbon dioxide cycle diagram worksheet distance vs displacement worksheet to delete this experiment. Trees that oxygen when crops or comments or cool your worksheet. Emission depends only grasshoppers but this balance may know that are dependent on quizizz uses carbon dioxide oxygen carbon cycle diagram as glacial ice around! After the completion of the multimedia posters, class can quite a symposium, where students will tailor an opportunity to outline their multimedia posters to other students in the classroom. -
Flows and Human Interferences
P1: FXZ/VEN October 16, 2000 12:3 Annual Reviews AR118-03 Annu. Rev. Energy Environ. 2000. 25:53–88 Copyright c 2000 by Annual Reviews. All rights reserved PHOSPHORUS IN THE ENVIRONMENT: Natural Flows and Human Interferences Vaclav Smil Department of Geography, University of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada; e-mail: [email protected] Key Words biogeochemical cycling, phosphates, fertilizers, eutrophication ■ Abstract Phosphorus has a number of indispensable biochemical roles, but it does not have a rapid global cycle akin to the circulations of C or N. Natural mobilization of the element, a part of the grand geotectonic denudation-uplift cycle, is slow, and low solubility of phosphates and their rapid transformation to insoluble forms make the element commonly the growth-limiting nutrient, particularly in aquatic ecosystems. Human activities have intensified releases of P.By the year 2000 the global mobilization of the nutrient has roughly tripled compared to its natural flows: Increased soil erosion and runoff from fields, recycling of crop residues and manures, discharges of urban and industrial wastes, and above all, applications of inorganic fertilizers (15 million tonnes P/year) are the major causes of this increase. Global food production is now highly dependent on the continuing use of phosphates, which account for 50–60% of all P supply; although crops use the nutrient with relatively high efficiency, lost P that reaches water is commonly the main cause of eutrophication. This undesirable process affects fresh and ocean waters in many parts of the world. More efficient fertilization can lower nonpoint P losses. Although P in sewage can be effectively controlled, such measures are often not taken, and elevated P is common in treated wastewater whose N was lowered by denitrification. -
Fate and Reactivity of Natural and Manufactured Nanoparticles in Soil/Water Environments Allison Vandevoort Clemson University, [email protected]
Clemson University TigerPrints All Dissertations Dissertations 12-2012 Fate and Reactivity of Natural and Manufactured Nanoparticles in Soil/Water Environments Allison Vandevoort Clemson University, [email protected] Follow this and additional works at: https://tigerprints.clemson.edu/all_dissertations Part of the Environmental Sciences Commons Recommended Citation Vandevoort, Allison, "Fate and Reactivity of Natural and Manufactured Nanoparticles in Soil/Water Environments" (2012). All Dissertations. 1018. https://tigerprints.clemson.edu/all_dissertations/1018 This Dissertation is brought to you for free and open access by the Dissertations at TigerPrints. It has been accepted for inclusion in All Dissertations by an authorized administrator of TigerPrints. For more information, please contact [email protected]. FATE AND REACTIVITY OF NATURAL AND MANUFACTURED NANOPARTICLES IN SOIL/WATER ENVIRONMENTS A Dissertation Presented to the Graduate School of Clemson University In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy Plant and Environmental Sciences by Allison René Rick VandeVoort December 2012 Accepted by: Dr. Yuji Arai, Committee Chair Dr. John Andrae Dr. Cindy Lee Dr. Horace Skipper ABSTRACT Nanoparticles (NPs), < 100 nm in diameter, make up the smallest component of solid material. This small size often causes increased reactivity in soil/water environments, which is true for both natural NPs, such as very fine clay particles, and for manufactured nanoparticles, such as silver nanoparticles (AgNPs). -
The Carbon Cycle High School Environmental Science Instructional Sequence
District of Columbia Office of the State Superintendent of Education The Carbon Cycle High School Environmental Science Instructional Sequence 1 This high school environmental science instructional sequence was created to support teaching the Next Generation Science Standards through the Biological Sciences Curriculum Study (BSCS) 5E instructional model. Developed by District of Columbia teachers, these lessons include real-world contexts for learning about environmental science through a lens that encourages student investigation of local issues. The lessons also support Scope and Sequence documents used by District local education agencies: Unit 1: Ecosystems: Interactions, Energy and Dynamics Advisory 1 and 2 Acknowledgements: Charlene Cummings, District of Columbia International School This curriculum resource can be downloaded online: https://osse.dc.gov/service/environmental-literacy-program-elp 2 Overview and Goal of the Lesson: In this sequence of lessons, students will go into depth via investigations about what processes drive the carbon cycle. Students are first introduced to the carbon cycle in an interactive game that triggers prior knowledge and touches on how carbon moves through Earth’s interconnected spheres. Students then investigate and gather evidence of the carbon transformation that carbon atoms encounter throughout the cycle. Since carbon is seen in students’ everyday lives, they will calculate their carbon footprint, calculate ways to deduct their carbon footprint, and trace carbon interaction throughout a typical school day. Essential Question(s): How are the cycles of matter and energy transferred in ecosystems? What processes drive the carbon cycle? NGSS Emphasized and Addressed in this Lesson Sequence: Carbon Cycle PERFORMANCE SCIENCE AND ENGINEERING DISCIPLINARY CORE IDEAS CROSSCUTTING CONCEPTS EXPECTATIONS PRACTICES HS-LS2-3. -
Ecological Succession and Biogeochemical Cycles
Chapter 10: Changes in Ecosystems Lesson 10.1: Ecological Succession and Biogeochemical Cycles Can a plant really grow in hardened lava? It can if it is very hardy and tenacious. And that is how succession starts. It begins with a plant that must be able to grow on new land with minimal soil or nutrients. Lesson Objectives ● Outline primary and secondary succession, and define climax community. ● Define biogeochemical cycles. ● Describe the water cycle and its processes. ● Give an overview of the carbon cycle. ● Outline the steps of the nitrogen cycle. ● Understand the phosphorus cycle. ● Describe the ecological importance of the oxygen cycle. Vocabulary ● biogeochemical cycle ● groundwater ● primary succession ● carbon cycle ● nitrogen cycle ● runoff ● climax community ● nitrogen fixation ● secondary succession ● condensation ● phosphorus cycle ● sublimation ● ecological succession ● pioneer species ● transpiration ● evaporation ● precipitation ● water cycle Introduction Communities are not usually static. The numbers and types of species that live in them generally change over time. This is called ecological succession. Important cases of succession are primary and secondary succession. In Earth science, a biogeochemical cycle or substance turnover or cycling of substances is a pathway by which a chemical substance moves through both biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) compartments of Earth. A cycle is a series of change which comes back to the starting point and which can be repeated. The term "biogeochemical" tells us that biological, geological and chemical factors are all involved. The circulation of chemical nutrients like carbon, oxygen, nitrogen, phosphorus, calcium, and water etc. through the biological and physical world are known as biogeochemical cycles. In effect, the element is recycled, although in some cycles there may be places (called reservoirs) where the element is accumulated or held for a long period of time (such as an ocean or lake for water). -
Cycles Worksheet Please Answer the Following Using the Words in the Text Box
Integrated Science Name ____________________________ Cycles worksheet Please answer the following using the words in the text box. Carbon Cycle Coal Oil Natural Gas burning of fossil fuels volcanoes Photosynthesis Respiration ocean sugar Greenhouse decayed 1. Plants use CO2 in the process of ___________________ to make ___________ and oxygen. 2. Animals use oxygen in the process of _______________ and make more CO2. 3. The ____________ is the main regulator of CO2 in the atmosphere because CO2 dissolves easily in it. 4. In the past, huge deposits of carbon were stored as dead plants and animals __________. 5. Today these deposits are burned as fossil fuels, which include _____________, _______________, and ______________. 6. More CO2 is released in the atmosphere today than in the past because of _________ ___________________ . 7. Another natural source for CO2 is __________________. 8. Too much CO2 in the atmosphere may be responsible for the _______________ effect. 9. Write the equation for photosynthesis. 10. Draw a simple diagram of the Carbon Cycle using the words in the text box above. Oxygen Cycle Photosynthesis Ozone Waste Crust Oceans Respiration 1. Plants release 430-470 billion tons of oxygen during process of _________________. 2. Atmospheric oxygen in the form of ___________ provides protection from harmful ultraviolet rays. 3. Oxygen is found everywhere on Earth, from Earth’s _____________ (rocks) to the ______________ where it is dissolved. 4. Oxygen is vital for ________________ by animals, a process which produces CO2.and water. 5. Oxygen is also necessary for the decomposition of ______________ into other elements necessary for life. 6. Write the equation for respiration. -
Chapter 15 Biogeochemical Cycles
Climate Change Impacts in the United States CHAPTER 15 BIOGEOCHEMICAL CYCLES Convening Lead Authors James N. Galloway, University of Virginia William H. Schlesinger, Cary Institute of Ecosystem Studies Lead Authors Christopher M. Clark, U.S. Environmental Protection Agency Nancy B. Grimm, Arizona State University Robert B. Jackson, Duke University Beverly E. Law, Oregon State University Peter E. Thornton, Oak Ridge National Laboratory Alan R. Townsend, University of Colorado Boulder Contributing Author Rebecca Martin, Washington State University Vancouver Recommended Citation for Chapter Galloway, J. N., W. H. Schlesinger, C. M. Clark, N. B. Grimm, R. B. Jackson, B. E. Law, P. E. Thornton, A. R. Townsend, and R. Martin, 2014: Ch. 15: Biogeochemical Cycles. Climate Change Impacts in the United States: The Third National Climate Assessment, J. M. Melillo, Terese (T.C.) Richmond, and G. W. Yohe, Eds., U.S. Global Change Research Program, 350-368. doi:10.7930/J0X63JT0. On the Web: http://nca2014.globalchange.gov/report/sectors/biogeochemical-cycles INFORMATION DRAWN FROM THIS CHAPTER IS INCLUDED IN THE HIGHLIGHTS REPORT AND IS IDENTIFIED BY THIS ICON 350 15 BIOGEOCHEMICAL CYCLES KEY MESSAGES 1. Human activities have increased atmospheric carbon dioxide by about 40% over pre-industrial levels and more than doubled the amount of nitrogen available to ecosystems. Similar trends have been observed for phosphorus and other elements, and these changes have major consequences for biogeochemical cycles and climate change. 2. In total, land in the United States absorbs and stores an amount of carbon equivalent to about 17% of annual U.S. fossil fuel emissions. U.S. forests and associated wood products account for most of this land sink. -
Global Oceanic and Atmospheric Oxygen Stability Considered In
..... ~- OCEANOLOGICA ACTA- VOL. 17- N°2 Global oceanic and atmospheric oxygen Air-sea ex ge CyC4 photosynthesis stability considered in relation to the Global change Oxygène carbon cycle and to different time scales Dioxide de carbone Échange air-mer Photosynthèse C3/C4 Changement global i, Egbert K. DUURSMA a and Michel P.R.M. BOISSON b 1 le ( a Résidence Les Marguerites, Appartement 15, 1305, Chemin des Revoires, 06320 La Turbie, France. '·•· b Service de l'Environnement, Ministère d'État, 3, avenue de Fontvieille, MC 98000 Monaco. Received 12/03/93, in revised form 20/01194, accepted 23/01/94. ABSTRACT This paper constitutes an overview and synthesis conceming atmospheric and oceanic oxygen and related carbon dioxide, particular attention being paid to potential regulation mechanisms on different time scales. The world atmospheric oxygen reserve is remarkably large, so that a lack of oxygen will not easily occur, whether in confined spaces or in major conurbations. On "short" scales, measured in hundreds or thousands of years, feedback processes with regard to oxygen regulation, solely based on atmospheric oxygen variations, would have to be so highly sensitive as to be barely conceivable. Only oxygen in the oceans can vary between zero and about twice the saturation - a fact which suggests that here, at !east potentially, there exist possibilities for a feedback based on oxygen changes. Atmospheric oxygen production began sorne 3.2 billion years ago, and has resul ted in a net total amount of 5.63 x 1020 mol (1.8 x 1022 g) of oxygen, of which 3.75 x I019 mol is present as free oxygen in the atmosphere and 3.1 x I017 mol as dissolved oxygen in the oceans, the remainder being stored in a large number of oxidized terrestrial and oceanic compounds.