DOCSLIB.ORG

Chemical Equilibrium Chemistry (H) 1St Year SEM-II, Dated: 7Th April 2020

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Chemical Equilibrium Chemistry (H) 1St Year SEM-II, Dated: 7Th April 2020 Remarks of Assignment 2: Chemical Equilibrium Chemistry (H) 1st Year SEM-II, Dated: 7th April 2020 Grades: A (Excellent); B+ (Very good); B (Good) and C (Poor) S. NAME Roll No. Grade Remarks No. 1. Sejal Jain 1931210 Resubmission: Not submitted or misplaced 2. Harshita 1931206 A In Q.6. no need to discuss the situations, according to figure 1 it is NO and Q.8. Try to write concisely 3. Yogesh Kumar 1931152 B+ Q. 6. Not correct 4. Pooja 1931132 B+ Q. 6. Not correct 5. Riddhima 120 A Excellent 6. Jyoti 112 B+ Q. 6. Not correct 7. Vivek 146 B+ Q. 6. Not correct 8. Vikash 154 B+ Q. 6. Not correct 9. Nidhi 150 A Excellent 10. Mehak Vaish 136 B+ Q. 6. Not correct 11. Rinka* 122 B+ Q. 6. Not correct 12. Sheenu 202 A Excellent 13. Bhupendra 104 B+ Q. 6. Not correct Maurya 14. Deepanshu 142 B+ Q. 6. Not correct 15. Diksha Rathi 204 A Excellent 16. Khushboo Mittal 256 A Q. 6. Not correct 17. Amit Patwa 252 B+ Q. 6. Not correct 18. Aman Tomar 246 A Excellent 19. Vinay Sharma 176 B+ Q. 6. Not correct 20. Garima Nveen 128 B+ Q. 6. Not correct and Q. 8. Answer in terms of number of moles, 21. Yatin Kumar 254 B+ Q. 6. Not correct 22. Ajay Kumar 238 B+ Q. 6. Not correct 23. Divya Yadav 214 A Excellent, Kindly check Q.6. not properly scanned but I think you want to say NO 24. Kushagra Malik 174 B+ Q. 6. Not correct 25. Megha Dhingra 184 B+ Q. 6. Not correct 26. Prerna Mahajan 186 B+ Q. 6. Not correct 27. Ramkrishna 230 B+ Q. 6. Not correct Bidika 28. Ramsha 218 B+ Q. 6. Not correct 29. Rinku Rathee 236 B+ Q. 6. Not correct 30. Riya Singh 248 B+ Q. 6. Not correct 31. Rohit Pawar 200 A Q. 6. Not correct 32. Saachi Sood 148 B+ Q. 6. Not correct and Q.8. partially correct 33. Sachin Yadav 140 A Q. 6. Not correct 34. Satwik Gupta 130 A Excellent 35. Shivendra Singh 158 B+ Q. 6. Not correct 36. Simran Giri 198 B+ Q. 6. Not correct 37. Somya Chawla 216 B+ Q. 6. Not correct 38. Tarnija Midha 126 A Excellent 1 39. Yousuf Khan 208 B+ Q. 6. Not correct 40. Mubarak Ali 250 B+ Q. 6. Not correct 41. Vijay Bhasin 172 B+ Q. 6. Not correct 42. Rishav Kumar 118 Resubmission: Not submitted or misplaced 43. Divyansh 226 B+ Q. 6. Not correct Chaudhary 44. Rohit Yadav 234 B+ Q. 6. Not correct 45. Shekhar Yadav 178 B+ Q. 6. Not correct 46. Yesh Vardhan 190 Resubmission: Not submitted or misplaced 47. Abhishek Meena 244 B+ Q. 6. Not correct 48. Abhishek Singh 220 B+ Q. 6. Not correct 49. Ajeet Kumar 242 B+ Q. 6. Not correct 50. Madhusoodan P 224 B+ Q. 6. Not correct Meghwal 51. Chahal Kohli 188 B+ Q. 6. Not correct Notes: (i) Absent: 182,194, 232, and 240 (Resubmission for all) (ii) Consult Atkins Book for answers. Answers: Figure 1. Ans: Q.6. & Q.7.: No, the given figure 1 (pair of weights joined by a string) does not represent a chemical reaction in equilibrium. We can compare the figure 1 with a chemical reaction as: Explanation: Spontaneity does not represent a chemical reaction in equilibrium. Means, a reaction can be spontaneous but not in equilibrium. Equilibrium means the rate of forward reaction is equal to the rate of backward reaction. As we know that the conditions or criteria for spontaneity and equilibrium are as: 2 SPONTANEOUS EQUILIBRIUM NON-SPONTANEOUS ∆G < 0 ∆G = 0 ∆G ˃ 0 ∆S ˃ 0 ∆S = 0 ∆S < 0 Q < K Q = K Q ˃ K Where ∆G is free energy of the reaction; ∆S is entropy of the reaction; Q is the reaction quotient and K is the equilibrium constant (See Q.4. of assignment 1 which depicts the relationship between ∆G, Q and K). In figure 1, the heavier weight moves downward (a natural tendency) due to gravity. Means, this downward movement is spontaneous. At the same time, the movement of lighter weight is due to the downward movement of heavier weight and against the gravity. Therefore, the movement of lighter weight is non-spontaneous and its movement is driven by heavier weight. Thus, figure 1 justifies that a spontaneous process drives a non- spontaneous process. Hence, we can say that “Reactions at equilibrium are spontaneous in neither direction: they are neither spontaneous (exergonic) nor non-spontaneous (endergonic)”. Figure 2. Ans: Q.8.: The equilibrium constant, K depends on ∆G0, which is defined at standard pressure. The value of ∆G0, and hence of K, is therefore independent of the pressure (P) at which the equilibrium is actually established. Therefore, (∂K/∂P)T = 0, this shows that K is independent of P and this does not necessarily mean that equilibrium composition is independent of P, and its effect depends on how the pressure is applied. Figure 2 justifies this condition. Mathematically: A ↔ 2 B The equilibrium constant is: ퟐ ퟎ 푲 = 풑푩 /풑푨풑 ………………… (1) 3 In this case, since the reaction is at equilibrium, and is compressed from (a) to (b), the system responds by reducing the no. of molecules in gas phase in order to minimize the increase in pressure. Let amount of A present initially = n and no B is present that is, A ↔ 2 B Initially: n 0 At equilibrium: (1 - α) n 2αn Where α is extent of dissociation of A into 2B. Mole fractions at equilibrium are: 푥 (1−훼)푛 (1−훼) and 퐴= = (1−훼)푛 +2훼푛 (1+훼) 2훼푛 2훼 푥퐵= = (1−훼)푛 +2훼푛 (1+훼) Equation (1) becomes: ퟐ ퟐ ퟐ ퟐ ퟎ 풑푩 풙푩 푷 ퟒ훼 (푷⁄풑 ) 푲 = ퟎ = ퟎ = ퟐ 풑푨풑 풙푨푷풑 1−훼 where P = total pressure; (Partial pressure = mole fraction × total pressure) 1 1/2 훼 = ( ) 1 + ퟒ푷⁄푲풑ퟎ This formula shows that, even though K is independent of pressure, the amounts of A and B do depend on pressure. It also shows that as 푷 is increased, α decreases, in accord with Le Chatelier’s principle. Note: Most of the answers (except 2-3 students) are without this mathematical derivation. They answered in terms of no. of moles, volumes and pressure which is also right. Md. Merajul Islam (Name of Teacher) Dated: 21st April 2020 4 .
Load more

Recommended publications
  • Introduction to Co2 Chemistry in Sea Water
    INTRODUCTION TO CO2 CHEMISTRY IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego Mauna Loa Observatory, Hawaii Monthly Average Carbon Dioxide Concentration Data from Scripps CO Program Last updated August 2016 2 ? 410 400 390 380 370 2008; ~385 ppm 360 350 Concentration (ppm) 2 340 CO 330 1974; ~330 ppm 320 310 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015 Year EFFECT OF ADDING CO2 TO SEA WATER 2− − CO2 + CO3 +H2O ! 2HCO3 O C O CO2 1. Dissolves in the ocean increase in decreases increases dissolved CO2 carbonate bicarbonate − HCO3 H O O also hydrogen ion concentration increases C H H 2. Reacts with water O O + H2O to form bicarbonate ion i.e., pH = –lg [H ] decreases H+ and hydrogen ion − HCO3 and saturation state of calcium carbonate decreases H+ 2− O O CO + 2− 3 3. Nearly all of that hydrogen [Ca ][CO ] C C H saturation Ω = 3 O O ion reacts with carbonate O O state K ion to form more bicarbonate sp (a measure of how “easy” it is to form a shell) M u l t i p l e o b s e r v e d indicators of a changing global carbon cycle: (a) atmospheric concentrations of carbon dioxide (CO2) from Mauna Loa (19°32´N, 155°34´W – red) and South Pole (89°59´S, 24°48´W – black) since 1958; (b) partial pressure of dissolved CO2 at the ocean surface (blue curves) and in situ pH (green curves), a measure of the acidity of ocean water.
    [Show full text]
  • 3-D Surface Visualization of Ph Titration “Topos”: Equivalence Point Cliffs, Dilution Ramps and Buffer Plateaus
    University of Montana ScholarWorks at University of Montana Water Topos: A 3-D Trend Surface Approach to Viewing and Teaching Aqueous Equilibrium Open Educational Resources (OER) Chemistry 11-2020 Chapter 1.1: 3-D Surface Visualization of pH Titration “Topos”: Equivalence Point Cliffs, Dilution Ramps and Buffer Plateaus Garon C. Smith University of Montana, Missoula Md Mainul Hossain North South University, Bangladesh Patrick MacCarthy Colorado School of Mines Follow this and additional works at: https://scholarworks.umt.edu/topos Part of the Chemistry Commons Let us know how access to this document benefits ou.y Recommended Citation Smith, Garon C.; Hossain, Md Mainul; and MacCarthy, Patrick, "Chapter 1.1: 3-D Surface Visualization of pH Titration “Topos”: Equivalence Point Cliffs, Dilution Ramps and Buffer Plateaus" (2020). Water Topos: A 3-D Trend Surface Approach to Viewing and Teaching Aqueous Equilibrium Chemistry. 2. https://scholarworks.umt.edu/topos/2 This Book is brought to you for free and open access by the Open Educational Resources (OER) at ScholarWorks at University of Montana. It has been accepted for inclusion in Water Topos: A 3-D Trend Surface Approach to Viewing and Teaching Aqueous Equilibrium Chemistry by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Part 1: Acid-Base Equilibrium Chapter 1.1 3-D Surface Visualization of pH Titration “Topos”: Equivalence Point Cliffs, Dilution Ramps and Buffer Plateaus Garon C. Smith1, Md Mainul Hossain2 and Patrick MacCarthy3 1Department of Chemistry and Biochemistry, The University of Montana, Missoula, MT 59812, Department of Biochemistry and Microbiology, North South University, Dhaka, Bangladesh, and 2Department of Chemistry and Geochemistry, Colorado School of Mines, Golden, CO 80401 Abstract 3-D topographic surfaces (“topos”) can be generated to visualize how pH behaves during titration and dilution procedures.
    [Show full text]
  • Atmospheric Chemistry
    Atmospheric Chemistry John Lee Grenfell Technische Universität Berlin Atmospheres and Habitability (Earthlike) Atmospheres: -support complex life (respiration) -stabilise temperature -maintain liquid water -we can measure their spectra hence life-signs Modern Atmospheric Composition CO2 Modern Atmospheric Composition O2 CO2 N2 CO2 N2 CO2 Modern Atmospheric Composition O2 CO2 N2 CO2 N2 P 93bar 1bar 6mb 1.5bar surface CO2 Tsurface 735K 288K 220K 94K Early Earth Atmospheric Compositions Magma Hadean Archaean Proterozoic Snowball CO2 Early Earth Atmospheric Compositions Magma Hadean Archaean Proterozoic Snowball Silicate CO2 CO2 N2 N2 Steam H2ON2 O2 O2 CO2 Additional terrestrial-type atmospheres Jurassic Earth Early Mars Early Venus Jungleworld Desertworld Waterworld Superearth Modern Atmospheric Composition Today we will talk about these CO2 Reading List Yuk Yung (Caltech) and William DeMore “Photochemistry of Planetary Atmospheres” Richard P. Wayne (Oxford) “Chemistry of Atmospheres” T. Gredel and Paul Crutzen (Mainz) “Chemie der Atmosphäre” Processes influencing Photochemistry Photons Protection Delivery Escape Clouds Photochemistry Surface OCEAN Biology Volcanism Some fundamentals… ALKALI METALS The Periodic Table NOBLE GASES One outer electron Increasing atomic number 8 outer electrons: reactive Rows called PERIODS unreactive GROUPS: similar Halogens chemical C, Si etc. have 4 outer electrons properties SO CAN FORM STABLE CHAINS Chemical Structure and Reactivity s and p orbitals d orbitals The Aufbau Method works OK for the first 18 elements
    [Show full text]
  • Analytical I
    ANALYTICAL I Analytical I (unable to fetch text document from uri [status: 0 (UnableToConnect), message: "Error: TrustFailure (Ssl error:1000007d:SSL routines:OPENSSL_internal:CERTIFICATE_VERIFY_FAILED)"]) TABLE OF CONTENTS 1: INTRODUCTION TO ANALYTICAL CHEMISTRY 1.1: WHAT IS ANALYTICAL CHEMISTRY? 1.2: THE ANALYTICAL PERSPECTIVE 1.3: COMMON ANALYTICAL PROBLEMS 1.4: INTRODUCTION TO ANALYTICAL CHEMISTRY (EXERCISES) 1.5: INTRODUCTION TO ANALYTICAL CHEMISTRY (SUMMARY) 2: BASIC TOOLS OF ANALYTICAL CHEMISTRY In the chapters that follow we will explore many aspects of analytical chemistry. In the process we will consider important questions such as “How do we treat experimental data?”, “How do we ensure that our results are accurate?”, “How do we obtain a representative sample?”, and “How do we select an appropriate analytical technique?” Before we look more closely at these and other questions, we will first review some basic tools of importance to analytical chemists. 2.1: MEASUREMENTS IN ANALYTICAL CHEMISTRY 2.2: CONCENTRATION 2.3: STOICHIOMETRIC CALCULATIONS 2.4: BASIC EQUIPMENT 2.5: PREPARING SOLUTIONS 2.6: SPREADSHEETS AND COMPUTATIONAL SOFTWARE 2.7: THE LABORATORY NOTEBOOK 2.8: BASIC TOOLS OF ANALYTICAL CHEMISTRY (EXERCISES) 2.9: BASIC TOOLS OF ANALYTICAL CHEMISTRY (SUMMARY) 3: THE VOCABULARY OF ANALYTICAL CHEMISTRY If you leaf through an issue of the journal Analytical Chemistry, you will soon discover that the authors and readers share a common vocabulary of analytical terms. You are probably familiar with some of these terms, such as accuracy and precision, but other terms, such as analyte and matrix may be less familiar to you. In order to participate in the community of analytical chemists, you must first understand its vocabulary.
    [Show full text]
  • Seepage Chemistry Manual
    RECLAMManagAingTWateIr iOn theNWest Report DSO-05-03 Seepage Chemistry Manual Dam Safety Technology Development Program U.S. Department of the Interior Bureau of Reclamation Technical Service Center Denver, Colorado December 2005 Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 The public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing the burden, to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE (DD-MM-YYYY) 2. REPORT TYPE 3. DATES COVERED (From - To) 12-2005 Technical 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER Seepage Chemistry Manual 5b. GRANT NUMBER 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER Craft, Doug 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT Bureau of Reclamation, Technical Service Center, D-8290, PO Box 25007, NUMBER Denver CO 80225 DSO-05-03 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESS(ES) 10.
    [Show full text]
  • Modeling of Aqueous Equilibrium: Three-Dimensional Trend Surfaces (Topos)
    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2014 MODELING OF AQUEOUS EQUILIBRIUM: THREE-DIMENSIONAL TREND SURFACES (TOPOS) Mohammad Mainul Hossain The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Hossain, Mohammad Mainul, "MODELING OF AQUEOUS EQUILIBRIUM: THREE-DIMENSIONAL TREND SURFACES (TOPOS)" (2014). Graduate Student Theses, Dissertations, & Professional Papers. 4413. https://scholarworks.umt.edu/etd/4413 This Dissertation is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. MODELING OF AQUEOUS EQUILIBRIUM: THREE-DIMENSIONAL TREND SURFACES (TOPOS) By MOHAMMAD MAINUL HOSSAIN MSc, Chemistry, Jahangirnagar University, Dhaka, Bangladesh, 2000 Dissertation Presented in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Chemistry The University of Montana Missoula, MT July 2014 Approved by: J. B. Alexander (Sandy) Ross, Dean of the Graduate School Graduate School and Committee Member Garon C. Smith, Chair Department of Chemistry and Biochemistry Edward Rosenberg Department of Chemistry and Biochemistry Richard
    [Show full text]
  • Chemistry (CHEM) 1
    Chemistry (CHEM) 1 Chemistry (CHEM) CHEM 117. Chemical Concepts and Applications. 3 Credits. Introduction to general and organic chemistry, with applications drawn from the health, environmental, and materials sciences. Prereq or Coreq: MATH 103, MATH 104 or MATH 107 or Math placement. CHEM 117L. Chem Concepts and Applications Lab. 1 Credit. Introduction to general and organic chemistry, with applications drawn from the health, environmental, and materials sciences. Prereq or Coreq: MATH 103, MATH 104, MATH 107 or Math placement. CHEM 121L. General Chemistry I Laboratory. 1 Credit. Matter, measurement, atoms, ions, molecules, reactions, chemical calculations, thermochemistry, bonding, molecular geometry, periodicity, and gases. Prereq or Coreq: MATH 103 or MATH 107 or Math placement. CHEM 121. General Chemistry I. 3 Credits. Matter, measurement, atoms, ions, molecules, reactions, chemical calculations, thermochemistry, bonding, molecular geometry, periodicity, and gases. Prereq or Coreq: MATH 103 or MATH 107 or Math placement. CHEM 122L. General Chemistry II Laboratory. 1 Credit. Intermolecular forces, liquids, solids, kinetics, equilibria, acids and bases, solution chemistry, precipitation, thermodynamics, and electrochemistry. Prereq: CHEM 121L. CHEM 122. General Chemistry II. 3 Credits. Intermolecular forces, liquids, solids, kinetics, equilibria, acids and bases, solution chemistry, precipitation, thermodynamics, and electrochemistry. Prereq: CHEM 121. CHEM 140. Organic Chemical Concepts and Applications. 1 Credit. Introduction to organic chemistry for pre-nursing and other students who need to meet the prerequisite for CHEM 260. CHEM 150. Principles of Chemistry I. 3 Credits. Chemistry for students with good high school preparation in mathematics and science. Electronic structure, stoichiometry, molecular geometry, ionic and covalent bonding, energetics of chemical reactions, gases, transition metal chemistry.
    [Show full text]
  • The Physics and Chemistry of Nebular Evolution 209
    Ciesla and Charnley: The Physics and Chemistry of Nebular Evolution 209 The Physics and Chemistry of Nebular Evolution F. J. Ciesla and S. B. Charnley NASA Ames Research Center Primitive materials in the solar system, found in both chondritic meteorites and comets, record distinct chemical environments that existed within the solar nebula. These environments would have been shaped by the dynamic evolution of the solar nebula, which would have affected the local pressure, temperature, radiation flux, and available abundances of chemical reactants. In this chapter we summarize the major physical processes that would have affected the chemis- try of the solar nebula and how the effects of these processes are observed in the meteoritic record. We also discuss nebular chemistry in the broader context of recent observations and chemical models of astronomical disks. We review recent disk chemistry models and discuss their applicability to the solar nebula, as well as their direct and potential relevance to meteor- itical studies. 1. INTRODUCTION ent facets of disk evolution may have been and discuss what effects this evolution may have had on nebular chemistry. Condensation calculations have been used as the basic (For example, we will discuss the effect of mass transport guides for understanding solar nebula chemistry over the through the solar nebula even though the driving mecha- last few decades. As reviewed by Ebel (2006), condensa- nism for this transport remains an area of ongoing research.) tion calculations provide information about the direction of It should be the goal of future studies and future generations chemical evolution, telling us what the end products would of meteoriticists, astronomers, and astrophysicists to im- be in a system given a constant chemical inventory, infinite prove upon the overviews provided here and make greater time, and ready access of all chemical species to one an- strides toward developing a coherent, unified model for the other.
    [Show full text]
  • RSC Macrocyclic and Supramolecular Chemistry Meeting Th Th 16 - 17 December 2019
    RSC Macrocyclic and Supramolecular Chemistry Meeting th th 16 - 17 December 2019 The organisers than the generous support of the following sponsors: Practical Information Venue The lecture and poster programme will take place in the Sibson building (Lecture Theatre 3). Tea, Coffee and Lunch will be served in the Sibson Foyer on both days. The meeting dinner will be held in the Darwin Conference Suite. Poster sessions will be also be held in the seminar rooms on the group floor of the Sibson Building. Buses The Unibus service (Uni 1 and Uni 2) runs every 8-15 minutes and bus service 4 runs every 30 minutes, all from Canterbury Bus Station (Bay B1). All services stop at the University campus and both railway stations. Alight at the bus turning circle on University Road. Parking Please park cars in the designated Visitor Car Parks – P (see campus map on the next page) to avoid being fined. Taxis The main taxi rank on campus is situated on University Road outside the Venue/ Student Media Centre. Local taxi services provide accessible vehicles and offer both male and female drivers. Local Taxi operators: Canterbury Taxis: 01227 444 444 Longleys Cab Company: 01227 710 777 Cab Line 6: 01227 666 666 Cabco Taxis: 01227 455 455 Programme: RSC Macrocyclic and Supramolecular Chemistry Meeting University of Kent: 16th - 17th December 2019 Event harassment officers: Cally Haynes, Anna McConnell and Claudia Caltagirone Monday 16th December 2019 09.30-10.20 Arrival, registration, poster setup, coffee 10.20-10.30 Welcome and opening remarks Session
    [Show full text]
  • One-Dimensional Transport with Equilibrium Chemistry (OTEQ) — a Reactive Transport Model for Streams and Rivers
    One-Dimensional Transport with Equilibrium Chemistry (OTEQ) — A Reactive Transport Model for Streams and Rivers Techniques and Methods Book 6, Chapter B6 U.S. Department of the Interior U.S. Geological Survey Cover. Upper workings of the Pennsylvania Mine in the headwaters of Peru Creek, Colorado. Photograph by Robert L. Runkel, U.S. Geological Survey, September 2009. One-Dimensional Transport with Equilibrium Chemistry (OTEQ): A Reactive Transport Model for Streams and Rivers By Robert L. Runkel Toxic Substances Hydrology Program Techniques and Methods Book 6, Chapter B6 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1–888–ASK–USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1–888–ASK–USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Runkel, R.L., 2010, One-dimensional transport with equilibrium chemistry (OTEQ) — A reactive transport model for streams and rivers: U.S. Geological Survey Techniques and Methods Book 6, Chapter B6, 101 p. iii Contents Abstract .
    [Show full text]
  • The Effect of Cooperative Learning Methods and Individual
    Educational Policy Analysis and Strategic Research, V 15, N 3, 2020 © 2020 INASED The Effect of Cooperative Learning Methods and Individual Learning Method on Pre- Service Science Teachers’ Sub-Micro Level Conceptual Understanding at Equilibrium Chemistry Seda OKUMUŞ1 Atatürk University Zehra ÖZDİLEK2 Bursa Uludağ University Aysel ARSLAN3 Atatürk University Abstract The purpose of the study is to investigate the effect of cooperative and individual learning methods on the conceptual understanding at sub-micro level of pre-service science teachers (PST) in equilibrium chemistry. The study was conducted on 52 PSTs. A pre-test/posttest non-equivalent quasi- experimental design was used in this study. Data collection instruments used as pre- and posttest as a Module Test (MT) consisted of seven open-ended questions developed by the researchers. Although, participants were identified with a convenience sampling method, each group were randomly assigned. For this reason, three study groups were selected, and each implementation was randomly assigned. Groups was determined as Cooperative Student Teams-Achievement Divisions (STAD, E1) and Reading-Writing-Application (RWA, E2) methods, and Individual Learning (IL, E3) method. The data gathered with the MT were evaluated using content analysis. According to findings, there was not a significance difference among groups related to conceptual understandings at equilibrium chemistry. However, some misconceptions related to topic were decreased. Consequently, when three learning methods are used that it is more likely to misconceptions of the PSTs will be treated, while at the same time micro level understanding will improve. Keywords: Cooperative learning, STAD, RWA, individual learning, equilibrium chemistry, conceptual understanding DOI: 10.29329/epasr.2020.270.19 1Seda Okumuş, Assis.
    [Show full text]
  • An Investigation of the Kinetics and Equilibrium Chemistry of Cold-Brew
    An Investigation of the Kinetics and Equilibrium Chemistry of Cold-brew Coffee Caffeine and Chlorogenic Acid Concentrations as a Function of Roasting Temperature and Grind Size Niny Z. Rao, PhD1, Megan Fuller, PhD1, Nicholas Parenti1, Samantha Ryder1, Nelly Setchie Tchato1 1College of Health, Science, and the Liberal Arts, Philadelphia University, Philadelphia PA Abstract Method Recently, both small and large commercial coffee brewers have begun offering cold-brew coffee drinks to customers with the claims that these cold-water extracts contain fewer bitter acids due to brewing conditions (Toddy Cold Brew website, 2016) while still retaining the flavor profile. Dunkin Donuts’ website suggests that the cold-water and long brewing times allow the coffee to reach “... its purest form.” With very little research existent on the Coarse and medium grinds of both dark and medium roasts were analyzed by mixing 350mL of chemistry of cold brew coffee consumers are left to the marketing strategies of Starbucks and other companies regarding the contents of cold-brew coffee. This research analyzes the caffeine and chlorogenic acid (3-CGA) filtered water with 35g of coffee grinds under constant stirring at 20°C. Sampling was content of cold-brew coffee as a function of brewing time, grind size, and roasting temperature of coffee beans sourced from the Kona region of Hawaii using high pressure liquid chromatography (HPLC). Coarse and medium performed every 15 minutes for the first hour, then every 30 minutes for the next ten to twelve grinds of both dark and medium roasts were analyzed by mixing 350mL of filtered water with 35g of coffee grinds under constant stirring at 20°C.
    [Show full text]