An Introduction to Photosynthesis and Cellular Respiration
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Comparing Aerobic Vs. Anaerobic Respiration
Comparing Aerobic vs. Anaerobic Respiration Objective: Students will compare the two types of cellular respiration: aerobic respiration and anaerobic respiration (fermentation). Students will note similarities and differences between the two processes including when, where, and how each process occurs. Students will develop a concept map using Inspiration indicating the criteria for aerobic and anaerobic respiration. This concept map will indicate: Three similarities between the two processes. Two types of cells that perform each process. Location in the cell where each process occurs. Oxygen requirements for each process. Reactants and products for each process. Energy output for each process. Two different types of anaerobic respiration. Reactants and products for each. Types of cells that perform each process. Introduction: This activity will follow a fermentation (anaerobic respiration) lab using yeast. This lab will address the process of alcoholic fermentation. Students will perform push-ups to experience lactic acid build-up in muscle cells. These activities will gain interest in the process of anaerobic respiration. Students will have already studied the detailed process of aerobic cellular respiration. Procedure: Students will work in pairs or trios to answer questions (as seen in benchmarks) on aerobic and anaerobic respiration. Students will use previous notes and lab activities to summarize main ideas for aerobic and anaerobic respiration. Individually, students will create a concept map using Inspiration to further integrate and separate the two processes. Accommodations: Instructions will be provided in written format as well as read orally. Instructions will also be on an overhead. One example will be provided for students on how to summarize data. -
Cellular Respiration +
Reference 3 Cellular Respiration Cellular respiration is a critical biochemical process for life on Earth. All cells require a continuous supply of energy to maintain order, build organic molecules, grow, and carry on all their other activities. Plants and other organisms can recover the solar energy stored in the molecular bonds of glucose by breaking down the sugar. Energy can then be stored in the bonds of ATP, which is used for a variety of processes that a cell must carry out to live. Cellular respiration is the most efficient way that glucose can be broken down to generate energy for other cellular reactions. In a sense, cellular respiration can be thought of as a type of controlled burning. When something is burned, a great deal of energy is released. The process requires oxygen and releases carbon dioxide and water and produces ATP. Cellular respiration can be summarized as: C6H12O6 + 6 O2 6 CO2 + 6 H2O + 32 ATP & heat carbohydrate oxygen carbon dioxide water energy During cellular respiration, the energy stored in a glucose molecule is released slowly as the molecule is broken down (figure R3.1). Cellular respiration occurs in three phases. In the first steps, known as glycolysis, glucose is split into two 3- carbon molecules. This releases energy, some of which is transferred to ATP. Glycolysis takes place in the cell cytoplasm. The second stage is called the Krebs cycle. During the Krebs cycle, each of the 3-carbon molecules is disassembled in a series of reactions to form six carbon dioxide molecules. Hydrogen atoms are also released. -
Energy Metabolism: Gluconeogenesis and Oxidative Phosphorylation
International Journal for Innovation Education and Research www.ijier.net Vol:-8 No-09, 2020 Energy metabolism: gluconeogenesis and oxidative phosphorylation Luis Henrique Almeida Castro ([email protected]) PhD in the Health Sciences Graduate Program, Federal University of Grande Dourados Dourados, Mato Grosso do Sul – Brazil. Leandro Rachel Arguello Dom Bosco Catholic University Campo Grande, Mato Grosso do Sul – Brazil. Nelson Thiago Andrade Ferreira Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Geanlucas Mendes Monteiro Heath and Development in West Central Region Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Jessica Alves Ribeiro Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Juliana Vicente de Souza Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Sarita Baltuilhe dos Santos Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Fernanda Viana de Carvalho Moreto MSc., Nutrition, Food and Health Graduate Program, Federal University of Grande Dourados Dourados, Mato Grosso do Sul – Brazil. Ygor Thiago Cerqueira de Paula Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. International Educative Research Foundation and Publisher © 2020 pg. 359 International Journal for Innovation Education and Research ISSN 2411-2933 September 2020 Vanessa de Souza Ferraz Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. Tayla Borges Lino Motion Science Graduate Program, Federal University of Mato Grosso do Sul Campo Grande, Mato Grosso do Sul – Brazil. -
7.014 Handout PRODUCTIVITY: the “METABOLISM” of ECOSYSTEMS
7.014 Handout PRODUCTIVITY: THE “METABOLISM” OF ECOSYSTEMS Ecologists use the term “productivity” to refer to the process through which an assemblage of organisms (e.g. a trophic level or ecosystem assimilates carbon. Primary producers (autotrophs) do this through photosynthesis; Secondary producers (heterotrophs) do it through the assimilation of the organic carbon in their food. Remember that all organic carbon in the food web is ultimately derived from primary production. DEFINITIONS Primary Productivity: Rate of conversion of CO2 to organic carbon (photosynthesis) per unit surface area of the earth, expressed either in terns of weight of carbon, or the equivalent calories e.g., g C m-2 year-1 Kcal m-2 year-1 Primary Production: Same as primary productivity, but usually expressed for a whole ecosystem e.g., tons year-1 for a lake, cornfield, forest, etc. NET vs. GROSS: For plants: Some of the organic carbon generated in plants through photosynthesis (using solar energy) is oxidized back to CO2 (releasing energy) through the respiration of the plants – RA. Gross Primary Production: (GPP) = Total amount of CO2 reduced to organic carbon by the plants per unit time Autotrophic Respiration: (RA) = Total amount of organic carbon that is respired (oxidized to CO2) by plants per unit time Net Primary Production (NPP) = GPP – RA The amount of organic carbon produced by plants that is not consumed by their own respiration. It is the increase in the plant biomass in the absence of herbivores. For an entire ecosystem: Some of the NPP of the plants is consumed (and respired) by herbivores and decomposers and oxidized back to CO2 (RH). -
Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-Rich, Geothermal Spring 2 3 Lewis M
bioRxiv preprint doi: https://doi.org/10.1101/428698; this version posted September 27, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-rich, Geothermal Spring 2 3 Lewis M. Ward1,2,3*, Airi Idei4, Mayuko Nakagawa2,5, Yuichiro Ueno2,5,6, Woodward W. 4 Fischer3, Shawn E. McGlynn2* 5 6 1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA 7 2. Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, 152-8550, Japan 8 3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 9 91125 USA 10 4. Department of Biological Sciences, Tokyo Metropolitan University, Hachioji, Tokyo 192-0397, 11 Japan 12 5. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 13 152-8551, Japan 14 6. Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth 15 Science and Technology, Natsushima-cho, Yokosuka 237-0061, Japan 16 Correspondence: [email protected] or [email protected] 17 18 Abstract 19 Hydrothermal systems, including terrestrial hot springs, contain diverse and systematic 20 arrays of geochemical conditions that vary over short spatial scales due to progressive interaction 21 between the reducing hydrothermal fluids, the oxygenated atmosphere, and in some cases 22 seawater. At Jinata Onsen, on Shikinejima Island, Japan, an intertidal, anoxic, iron- and 23 hydrogen-rich hot spring mixes with the oxygenated atmosphere and sulfate-rich seawater over 24 short spatial scales, creating an enormous range of redox environments over a distance ~10 m. -
A Study of Differences in Vertical Phosphorus Profiles Within the Sediments of Selected Florida Lakes As Related to Trophic Dynamics
University of Central Florida STARS Retrospective Theses and Dissertations 1976 A Study of Differences in Vertical Phosphorus Profiles Within the Sediments of Selected Florida Lakes as Related to Trophic Dynamics Edgar Allen Stewart III University of Central Florida, [email protected] Part of the Engineering Commons Find similar works at: https://stars.library.ucf.edu/rtd University of Central Florida Libraries http://library.ucf.edu This Masters Thesis (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Stewart, Edgar Allen III, "A Study of Differences in Vertical Phosphorus Profiles Within the Sediments of Selected Florida Lakes as Related to Trophic Dynamics" (1976). Retrospective Theses and Dissertations. 258. https://stars.library.ucf.edu/rtd/258 • A STUDY OF DIFFEREilCES IN VERTICAL PHOSPHORUS PRO FILES WliHIN THE SEDIMENTS OF SELECTED FLORIUA LAKES AS [{ELATED TO °fROPfiiC DYNArHCS BY EDGAR ALLE N STEHART III B.S., University of Florida, 1971 THESIS SubmHted o'n partial fulfiliment of the requirements for the degree of Mdster of Science °in the Graduate Studies Program of the Co 11 eye of Engi neer i ng of Florida Technological University , Or l ando, Florida 1976 • A STUDY OF DIFFERENCES IN VERTICAL PHOSPHOROUS PROFILES WITHIN THE SEDIMENTS OF SELECTED FLORIDA LAKES AS RELATED TO TROPHIC DYNAMICS BY E. ALLEIJ STEWART I II \ ABSTRACT Seve"a 1 Flori da 1akes with different docu'llcnted traphi c sta te indi ces were se lected for sediment analysis . -
Cellular Respiration Process by Which Cells Transfer Energy from Food To
Cellular Respiration Process by which cells transfer energy from food to ATP Cells rely heavily on Oxygen Can be Aerobic or Anaerobic Brain cells cannot produce energy anaerobicly Heart Cells have a minimal ability to produce energy anaerobicly Glycolysis, Krebs cycle, Electron Transport Carb Metabolism Only food the can create energy through Anaerobic metabolism Preferred food of the body, uses least amount of oxygen Glucose- 6-carbon sugar C6H12O6 Break down= Glucose + Oxygen = Water + Carbon Dioxide + Energy Excess Glucose stored as Glycogen stored in the liver & muscles Stage 1- Glycolysis Prepares glucose to enter the next stage Converts Glucose to Pyruvic Acid (Aerobic) or Lactic Acid (Anaerobic) ATP is produced 2 ATP used in the first steps (Only 1 if glycogen) 2 ATP produced end steps 2 NAD FAD & NAD similar to a taxi (Transport Oxygen) 6 Carbon Glucose broken down to 2 3-carbon cells Lactic Acid- Glycogen (Anaerobic) Pyruvic acid- Glucose (Aerobic) Stage 2- Formation of Acetyl Coenzyme A Converts Pyruvate to Acetyl Coenzyme A No ATP is used or produced 2 NAD (4 NAD) Stage 3- Krebs Cycle Begins & ends with the same substance No ATP is used 2 ATP Made (2 Cells) Hydrogen’s spilt for Electron Transport 6 NAD Stage 4- Electron Transport System Hydrogen taken from FAD & NAD to make water Electrons are dropped off and then pick up- repeats 3 times One ATP for each for each pair of Hydrogen’s Each NAD makes 3ATP Each FAD makes 2 ATP Total Stage 1 – Glycolysis-2 ATP, NAD but can’t be used in skeletal muscle (FAD uses electron in skeletal -
Chapter 20 Electrochemistry
Chapter 20 Electrochemistry Learning goals and key skills: Identify oxidation, reduction, oxidizing agent, and reducing agent in a chemical equation Complete and balance redox equations using the method of half-reactions. Sketch a voltaic cell and identify its cathode, anode, and the directions in which electrons and ions move. o Calculate standard emfs (cell potentials), E cell, from standard reduction potentials. Use reduction potentials to predict whether a redox reaction is spontaneous. o o Relate E cell to DG and equilibrium constants. Calculate emf under nonstandard conditions. Identify the components of common batteries. Describe the construction of a lithium-ion battery and explain how it works. Describe the construction of a fuel cell and explain how it generates electrical energy. Explain how corrosion occurs and how it is prevented by cathodic protection. Describe the reactions in electrolytic cells. Relate the amounts of products and reactants in redox reactions to electrical charge. Electrochemistry Electrochemistry is the study of the relationships between electricity and chemical reactions. • It includes the study of both spontaneous and nonspontaneous processes. 1 Redox reactions: assigning oxidation numbers Oxidation numbers help keep track of what species loses electrons and what species gains them. • An element is oxidized when the oxidation number increases • An element is reduced when the oxidation number decreases • an oxidizing agent causes another element to be oxidized • a reducing agent causes another element to be reduced. Assigning oxidation numbers (sect. 4.4) 1. Elemental form, each atom has ox. # = 0. Zn O2 O3 I2 S8 P4 2. Simple ions, = charge on ion. -1 for Cl-, +2 for Mg2+ 3. -
Unique Properties of Water!
Name: _______ANSWER KEY_______________ Class: _____ Date: _______________ Unique Properties of Water! Word Bank: Adhesion Evaporation Polar Surface tension Cohesion Freezing Positive Universal solvent Condensation Melting Sublimation Dissolve Negative 1. The electrons are not shared equally between the hydrogen and oxygen atoms of water creating a Polar molecule. 2. The polarity of water allows it to dissolve most substances. Because of this it is referred to as the universal solvent 3. Water molecules stick to other water molecules. This property is called cohesion. 4. Hydrogen bonds form between adjacent water molecules because the positive charged hydrogen end of one water molecule attracts the negative charged oxygen end of another water molecule. 5. Water molecules stick to other materials due to its polar nature. This property is called adhesion. 6. Hydrogen bonds hold water molecules closely together which causes water to have high surface tension. This is why water tends to clump together to form drops rather than spread out into a thin film. 7. Condensation is when water changes from a gas to a liquid. 8. Sublimation is when water changes from a solid directly to a gas. 9. Freezing is when water changes from a liquid to a solid. 10. Melting is when water changes from a solid to a liquid. 11. Evaporation is when water changes from a liquid to a gas. 12. Why does ice float? Water expands as it freezes, so it is LESS DENSE AS A SOLID. 13. What property refers to water molecules resembling magnets? How are these alike? Polar bonds create positive and negative ends of the molecule. -
Ocean Storage
277 6 Ocean storage Coordinating Lead Authors Ken Caldeira (United States), Makoto Akai (Japan) Lead Authors Peter Brewer (United States), Baixin Chen (China), Peter Haugan (Norway), Toru Iwama (Japan), Paul Johnston (United Kingdom), Haroon Kheshgi (United States), Qingquan Li (China), Takashi Ohsumi (Japan), Hans Pörtner (Germany), Chris Sabine (United States), Yoshihisa Shirayama (Japan), Jolyon Thomson (United Kingdom) Contributing Authors Jim Barry (United States), Lara Hansen (United States) Review Editors Brad De Young (Canada), Fortunat Joos (Switzerland) 278 IPCC Special Report on Carbon dioxide Capture and Storage Contents EXECUTIVE SUMMARY 279 6.7 Environmental impacts, risks, and risk management 298 6.1 Introduction and background 279 6.7.1 Introduction to biological impacts and risk 298 6.1.1 Intentional storage of CO2 in the ocean 279 6.7.2 Physiological effects of CO2 301 6.1.2 Relevant background in physical and chemical 6.7.3 From physiological mechanisms to ecosystems 305 oceanography 281 6.7.4 Biological consequences for water column release scenarios 306 6.2 Approaches to release CO2 into the ocean 282 6.7.5 Biological consequences associated with CO2 6.2.1 Approaches to releasing CO2 that has been captured, lakes 307 compressed, and transported into the ocean 282 6.7.6 Contaminants in CO2 streams 307 6.2.2 CO2 storage by dissolution of carbonate minerals 290 6.7.7 Risk management 307 6.2.3 Other ocean storage approaches 291 6.7.8 Social aspects; public and stakeholder perception 307 6.3 Capacity and fractions retained -
Introduction to Chemistry
Introduction to Chemistry Author: Tracy Poulsen Digital Proofer Supported by CK-12 Foundation CK-12 Foundation is a non-profit organization with a mission to reduce the cost of textbook Introduction to Chem... materials for the K-12 market both in the U.S. and worldwide. Using an open-content, web-based Authored by Tracy Poulsen collaborative model termed the “FlexBook,” CK-12 intends to pioneer the generation and 8.5" x 11.0" (21.59 x 27.94 cm) distribution of high-quality educational content that will serve both as core text as well as provide Black & White on White paper an adaptive environment for learning. 250 pages ISBN-13: 9781478298601 Copyright © 2010, CK-12 Foundation, www.ck12.org ISBN-10: 147829860X Except as otherwise noted, all CK-12 Content (including CK-12 Curriculum Material) is made Please carefully review your Digital Proof download for formatting, available to Users in accordance with the Creative Commons Attribution/Non-Commercial/Share grammar, and design issues that may need to be corrected. Alike 3.0 Unported (CC-by-NC-SA) License (http://creativecommons.org/licenses/by-nc- sa/3.0/), as amended and updated by Creative Commons from time to time (the “CC License”), We recommend that you review your book three times, with each time focusing on a different aspect. which is incorporated herein by this reference. Specific details can be found at http://about.ck12.org/terms. Check the format, including headers, footers, page 1 numbers, spacing, table of contents, and index. 2 Review any images or graphics and captions if applicable. -
Titanium Dioxide Production Final Rule: Mandatory Reporting of Greenhouse Gases
Titanium Dioxide Production Final Rule: Mandatory Reporting of Greenhouse Gases Under the Mandatory Reporting of Greenhouse Gases (GHGs) rule, owners or operators of facilities that contain titanium dioxide production processes (as defined below) must report emissions from titanium dioxide production and all other source categories located at the facility for which methods are defined in the rule. Owners or operators are required to collect emission data; calculate GHG emissions; and follow the specified procedures for quality assurance, missing data, recordkeeping, and reporting. How Is This Source Category Defined? The titanium dioxide production source category consists of any facility that uses the chloride process to produce titanium dioxide. What GHGs Must Be Reported? Each titanium dioxide production facility must report carbon dioxide (CO2) process emissions from each chloride process line. In addition, each facility must report GHG emissions for other source categories for which calculation methods are provided in the rule. For example, facilities must report CO2, nitrous oxide (N2O), and methane (CH4) emissions from each stationary combustion unit on site by following the requirements of 40 CFR part 98, subpart C (General Stationary Fuel Combustion Sources). Please refer to the relevant information sheet for a summary of the rule requirements for calculating and reporting emissions from any other source categories at the facility. How Must GHG Emissions Be Calculated? Reporters must calculate CO2 process emissions using one of two methods, as appropriate: • Installing and operating a continuous emission monitoring system (CEMS) according to the requirements specified in 40 CFR part 98, subpart C. • Calculating the process CO2 emissions for each process line using monthly measurements of the mass and carbon content of calcined petroleum coke.