The West Coast Ocean Acidification and Hypoxia Science Panel MAJOR FINDINGS, RECOMMENDATIONS, and ACTIONS
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Purification and Characterization of Bromocresol Purple for Spectrophotometric Seawater Alkalinity Titrations
University of Montana ScholarWorks at University of Montana Undergraduate Theses and Professional Papers 2016 PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS Taymee A. Brandon The University Of Montana, [email protected] Follow this and additional works at: https://scholarworks.umt.edu/utpp Part of the Analytical Chemistry Commons, and the Environmental Chemistry Commons Let us know how access to this document benefits ou.y Recommended Citation Brandon, Taymee A., "PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS" (2016). Undergraduate Theses and Professional Papers. 97. https://scholarworks.umt.edu/utpp/97 This Thesis is brought to you for free and open access by ScholarWorks at University of Montana. It has been accepted for inclusion in Undergraduate Theses and Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS By TAYMEE ANN MARIE BRANDON Undergraduate Thesis presented in partial fulfillment of the requirements for the University Scholar distinction Davidson Honors College University of Montana Missoula, MT May 2016 Approved by: Dr. Michael DeGrandpre Department of Chemistry and Biochemistry ABSTRACT Brandon, Taymee, B.S., May 2016 Chemistry Purification and Characterization of Bromocresol Purple for Spectrophotometric Seawater Alkalinity Titrations Faculty Mentor: Dr. Michael DeGrandpre The topic of my research is the purification of the sulfonephthalein indicator bromocresol purple (BCP). BCP is used as an acid-base indicator in seawater alkalinity determinations. Impurities in sulfonephthalein indicator salts often result in significant errors in pH values3. -
Geochemistry of Corals: Proxies of Past Ocean Chemistry, Ocean Circulation, and Climate
Proc. Natl. Acad. Sci. USA Vol. 94, pp. 8354–8361, August 1997 Colloquium Paper This paper was presented at a colloquium entitled ‘‘Carbon Dioxide and Climate Change,’’ organized by Charles D. Keeling, held November 13–15, 1995, at the National Academy of Sciences, Irvine, CA. Geochemistry of corals: Proxies of past ocean chemistry, ocean circulation, and climate ELLEN R. M. DRUFFEL Department of Earth System Science, University of California, Irvine, CA 92697 ABSTRACT This paper presents a discussion of the status Second, a synthesis is presented of the available proxy of the field of coral geochemistry as it relates to the recovery of records from corals as they relate to past climate, ocean past records of ocean chemistry, ocean circulation, and climate. circulation changes, and anthropogenic input of excess CO2. The first part is a brief review of coral biology, density banding, For some databases, the anthropogenic CO2 appears clear and and other important factors involved in understanding corals as globally distributed. For other databases it appears that vari- proxies of environmental variables. The second part is a syn- ability on interannual to decadal time scales complicates a thesis of the information available to date on extracting records straightforward attempt to separate natural perturbations of the carbon cycle and climate change. It is clear from these from the anthropogenic CO2 signal on the Earth’s environ- proxy records that decade time-scale variability of mixing pro- ment. Shen (4) presents a review of the types of coral archives cesses in the oceans is a dominant signal. That Western and available from the perspective of historical El Nin˜o-Southern Eastern tropical Pacific El Nin˜o-Southern Oscillation (ENSO) Oscillation (ENSO) influences on the tropical Pacific Ocean. -
Chemistry of the Oceans - Chen-Tung Arthur Chen
OCEANOGRAPHY – Vol.I - Chemistry of the Oceans - Chen-Tung Arthur Chen CHEMISTRY OF THE OCEANS Chen-Tung Arthur Chen Institute of Marine Geology and Chemistry, National Sun Yat-sen University, Kaohsiung 804, Taiwan, R.O.C. Keywords: Ωa, Ωc, alkalinity, anion, aragonite, bicarbonate, calcite, carbon, carbonate, CO2, colloids, conservative property, dielectric constant, euphotic zone, hydrogen bond, major elements, minor elements, nonconservative property, pCO2, pH, radionuclides, salinity, specific heat, surface tension, trace elements, viscosity. Contents 1. Introduction 2. General Chemistry of Seawater 3. Nutrients Cycling in the Oceans 4. Carbonate Chemistry of the Oceans 5. Natural and Anthropogenic Radionuclides 6. Human Perturbations 7. Non-Radioactive Ocean Pollution Glossary Bibliography Biographical Sketch Summary The oceans are filled with seawater which is mainly composed of water, a chemical compound composed of one oxygen and two hydrogen atoms. The polar nature of a water molecular, induced by a positive charge on the hydrogen side and a negative charge on the oxygen side, produces some unusual properties, one of the most important being water's remarkable ability to dissolve more substances than any other solvent. Although most solids and gases are soluble in water, the oceans are essentially in chemical equilibrium with as much material removed as that which enters every year. Each kilogram of typical seawater contains about 965 g water (857.8 g oxygen and 107.2 g hydrogen).UNESCO The major ions are chlo –ride EOLSS(18.98 g), sodium (10.56 g), sulfate (2.65 g), magnesium (1.27 g), calcium (0.40 g), potassium (0.38 g) and bicarbonate (0.14 g). -
Ocean Acidification in the Geological Past
UK Ocean Acidification programme synopsis Ocean acidification in the geological past www.oceanacidification.org.uk Lessons from the past Global-scale ocean acidification is happening now, as a result of human activities adding CO2 to the atmosphere. But ocean acidity has increased previously in the Earth’s history, as a result of natural changes in atmospheric composition. Of particular interest are past releases of CO2 that have occurred relatively rapidly in geological terms, since they may provide natural analogues for the effects of current acidification on chemical processes and marine life. Calcifying organisms (that construct their shells out of calcium carbonate) provide an important research focus, since they are preserved in the fossil record and are also likely to be especially sensitive to changes in ocean chemistry. Most of the palaeo-oceanographic Specific aims of the consortium study were: work in UKOA was carried out by a consortium project Abrupt ocean l To produce new estimates of seawater acidity and atmospheric CO2 levels for acidification events and their effects the period 40-65 million years ago in the Earth’s past, led by Paul l To study the response of the carbon cycle during the onset of the Paleocene - Pearson at Cardiff University. Formal Eocene thermal maximum (PETM) using new data from Tanzania and elsewhere partners were at Southampton, and new computer models University College London and the l To compare the PETM with other known ocean acidification events in the Open University, with additional Earth’s past contributions by researchers at Bristol, l To quantify the biotic response to ocean acidification events both directly Oxford, Yale and elsewhere. -
The Physical and Chemical Characteristics of Marine Primary Open Access Organic Aerosol: a Review Biogeosciences Biogeosciences Discussions B
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmos. Chem. Phys., 13, 3979–3996, 2013 Atmospheric Atmospheric www.atmos-chem-phys.net/13/3979/2013/ doi:10.5194/acp-13-3979-2013 Chemistry Chemistry © Author(s) 2013. CC Attribution 3.0 License. and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access The physical and chemical characteristics of marine primary Open Access organic aerosol: a review Biogeosciences Biogeosciences Discussions B. Gantt and N. Meskhidze Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, North Carolina, USA Open Access Open Access Correspondence to: N. Meskhidze ([email protected]) Climate Climate Received: 19 July 2012 – Published in Atmos. Chem. Phys. Discuss.: 23 August 2012 of the Past of the Past Revised: 5 March 2013 – Accepted: 24 March 2013 – Published: 18 April 2013 Discussions Open Access Open Access Abstract. Knowledge of the physical characteristics and 1 Introduction Earth System chemical composition of marine organic aerosols is needed Earth System for the quantification of their effects on solar radiation trans- Dynamics Dynamics fer and cloud processes. This review examines research per- One of the largest uncertainties of the aerosol-cloud sys- Discussions tinent to the chemical composition, size distribution, mixing tem is the background concentration of natural aerosols, es- state, emission mechanism, photochemical oxidation and cli- pecially over clean marine regions where cloud condensa- Open Access Open Access matic impact of marine primary organic aerosol (POA) asso- tion nuclei (CCN) concentrationGeoscientific ranges from less than 100 Geoscientific −3 ciated with sea-spray. -
Perspectives on Chemical Oceanography in the 21St Century
Old Dominion University ODU Digital Commons OEAS Faculty Publications Ocean, Earth & Atmospheric Sciences 2018 Perspectives on Chemical Oceanography in the 21st Century: Participants of the COME ABOARD Meeting Examine Aspects of the Field in the Context of 40 Years of DISCO Andrea J. Fassbender Hilary I. Palevsky Todd R. Martz Anitra E. Ingalls Martha Gledhill See next page for additional authors Follow this and additional works at: https://digitalcommons.odu.edu/oeas_fac_pubs Part of the Environmental Chemistry Commons, and the Oceanography Commons Repository Citation Fassbender, Andrea J.; Palevsky, Hilary I.; Martz, Todd R.; Ingalls, Anitra E.; Gledhill, Martha; Fawcett, Sarah E.; Brandes, Jay A.; Aluwihare, Lihini I.; The aP rticipants of COME ABOARD; and DISCO XXV, "Perspectives on Chemical Oceanography in the 21st Century: Participants of the COME ABOARD Meeting Examine Aspects of the Field in the Context of 40 Years of DISCO" (2018). OEAS Faculty Publications. 343. https://digitalcommons.odu.edu/oeas_fac_pubs/343 Original Publication Citation Fassbender, A. J., Palevsky, H. I., Martz, T. R., Ingalls, A. E., Gledhill, M., Fawcett, S. E., . Aluwihare, L. I. (2017). Perspectives on chemical oceanography in the 21st century: Participants of the COME ABOARD meeting examine aspects of the field in the context of 40 years of DISCO. Marine Chemistry, 196, 181-190. doi: 10.1016/j.marchem.2017.09.002 Authors Andrea J. Fassbender, Hilary I. Palevsky, Todd R. Martz, Anitra E. Ingalls, Martha Gledhill, Sarah E. Fawcett, Jay A. Brandes, Lihini I. Aluwihare, The aP rticipants of COME ABOARD, and DISCO XXV This article is available at ODU Digital Commons: https://digitalcommons.odu.edu/oeas_fac_pubs/343 Marine Chemistry 196 (2017) 181–190 Contents lists available at ScienceDirect Marine Chemistry ELSEVIER journal homepage: www.elsevier.com/locate/marchem Perspectives on Chemical Oceanography in the 21st century: Participants of CrossMark the COME ABOARD Meeting examine aspects of the field in the context of 40 years of DISCO ⁎ Andrea J. -
Distribution and Sedimentary Characteristics of Tsunami Deposits
Sedimentary Geology 200 (2007) 372–386 www.elsevier.com/locate/sedgeo Distribution and sedimentary characteristics of tsunami deposits along the Cascadia margin of western North America ⁎ Robert Peters a, , Bruce Jaffe a, Guy Gelfenbaum b a USGS Pacific Science Center, 400 Natural Bridges Drive, Santa Cruz, CA 95060, United States b USGS 345 Middlefield Road, Menlo Park, CA 94025, United States Abstract Tsunami deposits have been found at more than 60 sites along the Cascadia margin of Western North America, and here we review and synthesize their distribution and sedimentary characteristics based on the published record. Cascadia tsunami deposits are best preserved, and most easily identified, in low-energy coastal environments such as tidal marshes, back-barrier marshes and coastal lakes where they occur as anomalous layers of sand within peat and mud. They extend up to a kilometer inland in open coastal settings and several kilometers up river valleys. They are distinguished from other sediments by a combination of sedimentary character and stratigraphic context. Recurrence intervals range from 300–1000 years with an average of 500–600 years. The tsunami deposits have been used to help evaluate and mitigate tsunami hazards in Cascadia. They show that the Cascadia subduction zone is prone to great earthquakes that generate large tsunamis. The inclusion of tsunami deposits on inundation maps, used in conjunction with results from inundation models, allows a more accurate assessment of areas subject to tsunami inundation. The application of sediment transport models can help estimate tsunami flow velocity and wave height, parameters which are necessary to help establish evacuation routes and plan development in tsunami prone areas. -
Non-Radioactive Ocean Pollution - Chen-Tung Arthur Chen
OCEANOGRAPHY – Vol.I - Non-Radioactive Ocean Pollution - Chen-Tung Arthur Chen NON-RADIOACTIVE OCEAN POLLUTION Chen-Tung Arthur Chen Institute of Marine Geology and Chemistry, National Sun Yat-sen University, Kaohsiung 804, Taiwan, Republic of China. Keywords: ASEAN, dumping, emulsification, heavy metals, marine pollution, organic compounds, pesticides, pollution, resins, SEAPOL sewage, sludge, trace metals, United Nations Convention on the Law of the sea, UNDP, UNEP. Contents 1. Introduction 2. Trace Metals 3. Pesticides and Organic Compounds 4. Sewage 5. Temporal Trend Glossary Bibliography Biographical Sketch Summary The pollution of the marine environment has been a major focus of concern in the international community. To illustrate the seriousness of the problem, of the 320 articles of the United Nations Convention on the Law of the Sea, the very first addresses the issue of marine pollution. The most important sources of pollution and, thus, the major threat to the marine environment come from the land and this includes the continuous discharges through rivers, runoff, ocean outfalls and groundwater discharges. The marine environment in some areas, notably the enclosed and semi-enclosed seas surrounded by very dense populations, has large run-offs from rivers and sewers that contain fertilizers, detergents, pesticides and industrial wastes. Untreated sewage pouring into coastal waters directly, or via rivers or ocean outfalls, can carry hepatitis, cholera, typhoid and a wide rangeUNESCO of other diseases and infections –. Simply EOLSS said, in many coastal areas pollution has reached intolerable aesthetic, ecological and social levels. In the deep seas, tar balls on the surface, mercury in the tuna and the dumping of noxious wastes present problems although, surprisingly,SAMPLE usually less important CHAPTERS or critical than pollution from certain nutrients. -
States Vulnerable to Ocean Acidification
PACIFIC NORTHWEST IS AT HIGH RISK FOR ECONOMIC HARM DUE TO OCEAN ACIDIFICATION According to a new assessment of the U.S. communities most vul- nerable to ocean acidification, the Date Water Pacific Northwest is at high risk of Unfavorable Economic Sensitivity To Shellfish Score Other Factors economic harm. Communities and 2006 - 2030 High Algae Blooms 2031 - 2050 Medium High River Inputs governments can still take action, 2051 - 2070 Medium Upwelling 2071 - 2099 Medium Low researchers say. 2099 + Low MAP LEFT: The long-term economic impacts of ocean acidification are expected to be most severe in regions where ocean areas are acidifying soonest (black) and where the residents rely most on local shellfish for their livelihood (red). Local factors such as algae blooms from nutrient pollu- tion, local upwelling currents, and poorly buffered rivers (green, purple, blue) can amplify acidification locally. adapted by NRDC from Ekstrom et al., 2015 adapted by NRDC from Ekstrom et al., 2015 WHY IS THE PACIFIC NORTHWEST A HOTSPOT? ECONOMIC DEPENDENCE OCEAN VULNERABILITY A SALTY GOLDMINE. Shelled Some believe Puget Sound is the greatest oyster-growing mollusk fisheries in Washington region on the planet. Cold, clean and Oregon produce slightly water from deep currents off the more than $100 million annu- coast, a winding coastline with ally in direct sales. Though the thousands of inlets with sheltered economic benefits extend well water, and an abundant supply of beyond the value of the harvest. The estimated mountain-fed rivers all contribute to this perception. But this same formula has also total annual economic impact of aquaculture in put the region at risk from ocean acidification. -
Ocean Acidification Due to Increasing Atmospheric Carbon Dioxide
Ocean acidification due to increasing atmospheric carbon dioxide Policy document 12/05 June 2005 ISBN 0 85403 617 2 This report can be found at www.royalsoc.ac.uk ISBN 0 85403 617 2 © The Royal Society 2005 Requests to reproduce all or part of this document should be submitted to: Science Policy Section The Royal Society 6-9 Carlton House Terrace London SW1Y 5AG email [email protected] Copy edited and typeset by The Clyvedon Press Ltd, Cardiff, UK ii | June 2005 | The Royal Society Ocean acidification due to increasing atmospheric carbon dioxide Ocean acidification due to increasing atmospheric carbon dioxide Contents Page Summary vi 1 Introduction 1 1.1 Background to the report 1 1.2 The oceans and carbon dioxide: acidification 1 1.3 Acidification and the surface oceans 2 1.4 Ocean life and acidification 2 1.5 Interaction with the Earth systems 2 1.6 Adaptation to and mitigation of ocean acidification 2 1.7 Artificial deep ocean storage of carbon dioxide 3 1.8 Conduct of the study 3 2 Effects of atmospheric CO2 enhancement on ocean chemistry 5 2.1 Introduction 5 2.2 The impact of increasing CO2 on the chemistry of ocean waters 5 2.2.1 The oceans and the carbon cycle 5 2.2.2 The oceans and carbon dioxide 6 2.2.3 The oceans as a carbonate buffer 6 2.3 Natural variation in pH of the oceans 6 2.4 Factors affecting CO2 uptake by the oceans 7 2.5 How oceans have responded to changes in atmospheric CO2 in the past 7 2.6 Change in ocean chemistry due to increases in atmospheric CO2 from human activities 9 2.6.1 Change to the oceans -
The Collaborative on Oceanography and Chemical Analysis (COCA) and Suggestions for Future Instrumental Analysis Methods in Chemical Oceanography
The Collaborative on Oceanography and Chemical Analysis (COCA) and suggestions for future instrumental analysis methods in chemical oceanography COCA Working Group*1 *Corresponding author Chris Measures, Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, HI, 96822, USA. Tel +1 808-956-8693 Email: [email protected] 1 The members of the COCA Working group are listed in Appendix I Submitted to a special issue of Marine Chemistry June, 2014. Abstract The ability to make measurements accurately and precisely is the sine qua non of chemical oceanography. The development of theory and its transformation into modeling is completely dependant on the understanding gained through accurate measurements of oceanic properties. Chemical oceanographers, by making measurements of various chemical elements in ocean water, seek to discover, understand, and quantify ocean processes and use them in conjunction with other branches of oceanography to understand how the oceans interact with Earth system processes. We use this information to understand how the planetary biogeochemical systems affect and interact with the climate and use the chemical record in the sediments to understand how these systems operated in the past. With this knowledge we can build accurate models to predict responses to future climate forcing events. The primary inputs to chemical oceanography are dominantly provided by applied analytical chemistry. The construction of large networked observing systems and the development of a variety of autonomous vehicles have provided an unprecedented opportunity to study the ocean at spatial and temporal scales that have not been previously available to the ocean research community. However, as a result of power availability, mass and size constraints, and the limited ability to service instruments on these platforms, there are only a few parameters of interest to chemical oceanographers that can take advantage of this expensive infrastructure. -
EA for Cascadia Spring/Summer Survey 2020
Draft Environmental Assessment/Analysis of a Marine Geophysical Survey by R/V Marcus G. Langseth of the Cascadia Subduction Zone in the Northeast Pacific Ocean, Late Spring/Summer 2020 Prepared for Lamont-Doherty Earth Observatory 61 Route 9W, P.O. Box 1000 Palisades, NY 10964-8000 and National Science Foundation Division of Ocean Sciences 4201 Wilson Blvd., Suite 725 Arlington, VA 22230 by LGL Ltd., environmental research associates 22 Fisher St., POB 280 King City, Ont. L7B 1A6 21 November 2019 LGL Report FA0186-01A Table of Contents TABLE OF CONTENTS LIST OF FIGURES .......................................................................................................................................... iv LIST OF TABLES ............................................................................................................................................. v ABSTRACT .................................................................................................................................................... vi LIST OF ACRONYMS ..................................................................................................................................... ix I PURPOSE AND NEED ................................................................................................................................... 1 1.1 Mission of NSF ................................................................................................................................ 1 1.2 Purpose of and Need for the Proposed Action ................................................................................