Effectiveness of a Toothpaste and a Serum Containing Calcium Silicate on Protecting the Enamel After Interproximal Reduction
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More Information If you would like more information or help with this leaflet contact: Community Dental Service All Wales Special Interest Group Mouthcare For Or Children with Swallowing Problems (Dysphagia) Speak to the swallowing teams about suction equipment This booklet will support mouthcare for children with swallowing problems 16 Oral Health and Dysphagia CHILDREN April 14 If you would like moreOral Healthinformation and Dysphagia or CHILDREN help April 14 with this leaflet contact: What is a swallowing Dental Equipment problem Suction toothbrushes: Kimberly-Clark Kim Vent: Ready care A swallowing problem is when foods and oral care www.vap.kchealthcare.com liquids do not pass easily from the mouth down the throat. Oro-Care 2 www.intersurgical.co.uk It can lead to: choking Plak-Vac: USA ordering. dehydration poor feeding and chest infections There are lots of reasons why children have Dr Barman’s superbrush/duo-power this problem such as cerebral palsy or www.dentocare.co.uk trauma. How do we know if a child has a swallow Collis-curve toothbrushes problem? www.colliscurve.co.uk Here are some of the signs but they can be different from child to child: Dental shield www.dentocare.co.uk drooling hard to swallow coughing Open wide disposable mouth rest choking www.dentocare.co.uk gurgly voice after swallowing lots of chest infections 15 2 weight loss Oral Health and Dysphagia CHILDREN April 14 Oral Health and Dysphagia CHILDREN April 14 Toothpastes What is a Swallowing Toothpastes for children to use to problem stop tartar build-up: There can be other problems in the mouth such as: Aquafresh tartar-control whitening The tongue cannot push food down the throat Sensodyne Tartar-control plus whitening Lips cannot close together Keeping food in the mouth, in the cheek or under the tongue Unable to feel food or drink in the mouth Oral B Pro-expert Whitening/All-round protection A dry mouth can make these problems worse. -
Product Information Sheet
September 17, 2015 productISOVACTIN information AA PLUS Nutrients 8.5 fl oz (250mL) per 100mL SKU 37002 Calories 186 74 Calories From Fat 57 23 NET WEIGHT 2 GAL (7.5 L) Protein Equivalent, g 20 8 Free Amino Acids, g 22 9 SERVING SIZE 8.5 fl oz (250mL) Carbohydrates, g 13 5 Sugar, g 5 2 SERVINGS PER PACKAGE 30 Sugar Alcohols, g 0 0 Dietary Fiber, g 2.8 1 Fat, g 6 2.4 24359-0702-03 REIMBURSEMENT CODE Saturated Fat, g 0.5 0.2 (for USA only) Trans Fat, g 0.0 0.0 DHA, mg 150.0 60.0 Cholesterol, mg 0.4 0 MEDICAL FOOD PRODUCT Vitamin A, IU 1100.0 440.0 For the dietary management of Isovaleric Acidemia. Dispensed by prescription. Vitamin C, mg 40.0 16.0 Isovactin AA Plus is a ready-to-drink metabolic formula product for Isovaleric Acidemia Vitamin D, IU 620.0 248.0 patients, over 1 year of age. Isovactin contains an advanced fortification blend. Product Vitamin E, IU 10.0 4.0 Vitamin K1, mcg 20.0 8.0 comes in a 250 mL carton. Vitamin K2 (MK-7), mcg 20.0 8.0 Thiamin (B1), mg 0.5 0.2 Riboflavin (B2), mg 0.5 0.2 Niacin (B3), mg 6.6 2.6 PRECAUTIONS For the dietary management of Isovaleric Acidemia (IVA) and Vitamin B6, mg 0.5 0.2 other disorders of leucine metabolism. Use as directed by physician. Must be Folic acid, mcg 186.0 74.4 administered under medical supervision only. -
Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean. -
Brochure-Product-Range.Pdf
PRODUCT RANGE 2015 edition ANSI Standard 60 NSF® CERTIFIED HALAL M ISLAMIC FOOD AND NUTRITION ® COUNCIL OF AMERICA Rue Joseph Wauters, 144 ISO 9001:2008 (Quality) / OHSAS 18001:2007 (Health/ B-4480 Engis Safety) / ISO 14001:2004 (Environment) / ISO 22000:2005 www.globulebleu.com (Food Safety) / FSSC 22000:2013 (Food Safety). Tel. +32 (0) 4 273 93 58 Our food grade phosphates are allergen free, GMO free, Fax. +32 (0) 4 275 68 36 BSE/TSE free. www.prayon.com mail. [email protected] Design by www.prayon.com PRODUCT RANGE | 11 TABLE OF CONTENTS HORTICULTURE APPLICATIONS HORTIPRAY® RANGE FOR HORTICULTURE* FOOD AND INDUSTRIAL APPLICATIONS PRODUCT NAME Bulk density P O pH N-NH Made 2 5 4 MONOAMMONIUM PHOSPHATE - NH4H2PO4 in 3 3 % 1% % Sodium orthophosphates ................................................................................... 03 g/cm lbs/ft indicative indicative indicative Water-soluble fertilisers. Sodium pyrophosphates .................................................................................... 04 HORTIPRAY® MAP Horticultural Grade 0.9 56 61 4.5 12 Sodium tripolyphosphates ................................................................................. 05 HORTIPRAY® MAP 12.60 Horticultural Grade 0.9 56 60 5 12.1 Water-soluble fertilisers; Sodium polyphosphates ..................................................................................... 06 HORTIPRAY® MAP anticalc Horticultural Grade 0.9 56 61 4.5 12 preventive action against clogging. Potassium orthophosphates ............................................................................. -
Paleoceanographical Proxies Based on Deep-Sea Benthic Foraminiferal Assemblage Characteristics
CHAPTER SEVEN Paleoceanographical Proxies Based on Deep-Sea Benthic Foraminiferal Assemblage Characteristics Frans J. JorissenÃ, Christophe Fontanier and Ellen Thomas Contents 1. Introduction 263 1.1. General introduction 263 1.2. Historical overview of the use of benthic foraminiferal assemblages 266 1.3. Recent advances in benthic foraminiferal ecology 267 2. Benthic Foraminiferal Proxies: A State of the Art 271 2.1. Overview of proxy methods based on benthic foraminiferal assemblage data 271 2.2. Proxies of bottom water oxygenation 273 2.3. Paleoproductivity proxies 285 2.4. The water mass concept 301 2.5. Benthic foraminiferal faunas as indicators of current velocity 304 3. Conclusions 306 Acknowledgements 308 4. Appendix 1 308 References 313 1. Introduction 1.1. General Introduction The most popular proxies based on microfossil assemblage data produce a quanti- tative estimate of a physico-chemical target parameter, usually by applying a transfer function, calibrated on the basis of a large dataset of recent or core-top samples. Examples are planktonic foraminiferal estimates of sea surface temperature (Imbrie & Kipp, 1971) and reconstructions of sea ice coverage based on radiolarian (Lozano & Hays, 1976) or diatom assemblages (Crosta, Pichon, & Burckle, 1998). These à Corresponding author. Developments in Marine Geology, Volume 1 r 2007 Elsevier B.V. ISSN 1572-5480, DOI 10.1016/S1572-5480(07)01012-3 All rights reserved. 263 264 Frans J. Jorissen et al. methods are easy to use, apply empirical relationships that do not require a precise knowledge of the ecology of the organisms, and produce quantitative estimates that can be directly applied to reconstruct paleo-environments, and to test and tune global climate models. -
Silicate Weathering in Anoxic Marine Sediment As a Requirement for Authigenic Carbonate Burial T
Earth-Science Reviews 200 (2020) 102960 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Silicate weathering in anoxic marine sediment as a requirement for authigenic carbonate burial T Marta E. Torresa,*, Wei-Li Hongb, Evan A. Solomonc, Kitty Millikend, Ji-Hoon Kime, James C. Samplef, Barbara M.A. Teichertg, Klaus Wallmannh a College of Earth, Ocean and Atmospheric Science, Oregon State University, Corvallis OR 97331, USA b Geological Survey of Norway, Trondheim, Norway c School of Oceanography, University of Washington, Seattle, WA 98195, USA d Bureau of Economic Geology, University of Texas at Austin, Austin, TX 78713, USA e Petroleum and Marine Research Division, Korea Institute of Geoscience and Mineral Resources, Daejeon, South Korea f School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA g Geologisch-Paläontologisches Institut, Wilhelms-Universität Münster, Corrensstr. 24, 48149 Münster, Germany h IFM-GEOMAR Leibniz Institute of Marine Sciences, Wischhofstrasse 1-3, 24148 Kiel, Germany ARTICLE INFO ABSTRACT Keywords: We emphasize the importance of marine silicate weathering (MSiW) reactions in anoxic sediment as funda- Silicate weathering mental in generating alkalinity and cations needed for carbonate precipitation and preservation along con- Authigenic carbonate tinental margins. We use a model that couples thermodynamics with aqueous geochemistry to show that the CO2 Organogenic dolomite released during methanogenesis results in a drop in pH to 6.0; unless these protons are buffered by MSiW, Alkalinity carbonate minerals will dissolve. We present data from two regions: the India passive margin and the active Carbon cycling subduction zone off Japan, where ash and/or rivers supply the reactive silicate phase, as reflected in strontium isotope data. -
The Silicate Structure Analysis of Hydrated Portland Cement Paste
The Silicate Structure Analysis of Hydrated Portland Cement Paste CHARLES W. LENTZ, Research Department, Dow Corning Corporation, Midland, Michigan A new technique for recovering silicate structures as trimeth- ylsilyl derivatives has been used to study the hydration of port- land cement. By this method only the changes iii the silicate portion of the structure can be determined as a function of hydration time. Cement pastes ranging in age from one day to 14. 7 years were analyzedfor the study. The hydration reaction is shown to be similar to a condensation type polymerization. The orthosilicate content of cement paste (which probably rep- resents the original calcium silicates in the portland cement) gradually decreases as the paste ages. Concurrentiy a disilicate structure is formed which reaches a maximum quantity in about four weeks and then it too diminishes as the paste ages. Minor quantities of a trisiicate and a cyclic tetrasiicate are shown to be present in hydrated cement paste. An unidentified polysilicate structure is produced by the hydration reaction which not only increases in quantity throughout the age period studied, but also increases in molecular weight as the paste ages. THE SILICON atoms in silicate minerals are always in fourfold coordination with oxygen. These silicon-oxygen tetrahedra can be completely separated from each other, as in the orthosilicates, they can be paired, as in the pyrosilicates, or they can be in other combinations with each other to give a variety of silicate structures. If the min- eral is composed only of Si and 0, then there is a three-dimensional network of silicate tetrahedra. -
(12) Patent Application Publication (10) Pub. No.: US 2017/0143022 A1 Wicker Et Al
US 20170143022A1 (19) United States (12) Patent Application Publication (10) Pub. No.: US 2017/0143022 A1 Wicker et al. (43) Pub. Date: May 25, 2017 (54) COMPOSITIONS INCORPORATING AN (52) U.S. Cl. UMLAM FLAVORAGENT CPC ............... A2.3L 27/20 (2016.08); A23L 27/88 (2016.08); A23L 2/56 (2013.01); A23L 2780 (71) Applicant: Senomyx, Inc., San Diego, CA (US) (2016.08); A23L 27/30 (2016.08); A23K 20/10 (2016.05); A23K 50/40 (2016.05); A61K 47/22 (72) Inventors: Sharon Wicker, Carlsbad, CA (US); (2013.01) Tanya Ditschun, San Diego, CA (US) (21) Appl. No.: 14/948,101 (57) ABSTRACT The present invention relates to compositions containing (22) Filed: Nov. 20, 2015 flavor or taste modifiers, such as a flavoring or flavoring agents and flavor or taste enhancers, more particularly, Publication Classification savory (“umami”) taste modifiers, savory flavoring agents (51) Int. Cl. and savory flavor enhancers, for foods, beverages, and other AOIN 25/00 (2006.01) comestible compositions. Compositions comprising an A23K2O/It (2006.01) umami flavor agent or umami taste-enhancing agent in A6 IK 47/22 (2006.01) combination with one or more other food additives, prefer A2.3L 2/56 (2006.01) ably including a flavorant, herb, Spice, fat, or oil, are A23K 50/40 (2006.01) disclosed. US 2017/O 143022 A1 May 25, 2017 COMPOSITIONS INCORPORATING AN tions WO 02/06254, WO 00/63166 art, WO 02/064631, and UMAM FLAVORAGENT WO 03/001876, and U.S. Patent publication US 2003 0232407 A1. The entire disclosures of the articles, patent BACKGROUND OF THE INVENTION applications, -
Soares, R. Et Al
Original Article DOI: 10.7860/JCDR/2017/23594.9758 Assessment of Enamel Remineralisation After Treatment with Four Different Dentistry Section Remineralising Agents: A Scanning Electron Microscopy (SEM) Study RENITA SOARES1, IDA DE NORONHA DE ATAIDE2, MARINA FERNANDES3, RAJAN LAMBOR4 ABSTRACT these groups were remineralised using the four remineralising Introduction: Decades of research has helped to increase our agents. The treated groups were subjected to pH cycling over a knowledge of dental caries and reduce its prevalence. However, period of 30 days. This was followed by assessment of surface according to World Oral Health report, dental caries still remains microhardness and SEM for qualitative evaluation of surface a major dental disease. Fluoride therapy has been utilised in changes. The results were analysed by One-Way Analysis Of a big way to halt caries progression, but has been met with Variance (ANOVA). Multiple comparisons between groups were limitations. This has paved the way for the development of performed by paired t-test and post-hoc Tukey test. newer preventive agents that can function as an adjunct to Results: The results of the study revealed that remineralisation of fluoride or independent of it. enamel was the highest in samples of Group E (Self assembling Aim: The purpose of the present study was to evaluate the ability peptide P11-4) followed by Group B (CPP-ACPF), Group C (BAG) of Casein Phosphopeptide-Amorphous Calcium Phosphate and Group D (fluoride enhanced HA gel). There was a significant Fluoride (CPP ACPF), Bioactive Glass (BAG), fluoride enhanced difference (p<0.05) in the remineralising ability between the self assembling peptide P -4 group and BAG and fluoride Hydroxyapatite (HA) gel and self-assembling peptide P11-4 to 11 remineralise artificial carious lesions in enamel in vitro using enhanced HA gel group. -
University of Nevada Reno SILICATE and CARBONATE SEDIMENT
University of Nevada Reno /SILICATE AND CARBONATE SEDIMENT-WATER RELATIONSHIPS IN WALKER LAKE, NEVADA A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Geochemistry by Ronald J. Spencer MINES 2 - UBKAKY %?: The thesis of Ronald James Spencer is approved: University of Nevada Reno May 1977 ACKNOWLEDGMENTS The author gratefully acknowledges the contributions of Dr. L. V. Benson, who directed the thesis, and Drs. L. C. Hsu and R. D. Burkhart, who served on the thesis ccmnittee. A special note of thanks is given to Pat Harris of the Desert Research Institute, who supervised the wet chemical analyses on the lake water and pore fluids. I also would like to thank John Sims and Mike Rymer of the U. S. Geological Survey, Menlo Park, for their effort in obtaining the piston core; and Blair Jones of the U. S. Geological Survey, Reston, for the use of equipment and many very helpful suggestions. Much of the work herein was done as a part of the study of the "Dynamic Ecological Relationships in Walker Lake, Nevada", and was supported by the Office of Water Research and Technology through grant number C-6158 to the Desert Research Institute. I thank the other members involved in the study; Drs. Dave Koch and Roger Jacobson, and Joe Mahoney, Jim Cooper, and Jim Hainiine; for advice in their fields of expertise and help in sample collection. Special thanks are extended to my wife, Laurie, without whose help and support this thesis could not have been completed. A final note of thanks to Tina Nesler, who advised Laurie in the typing of the manuscript. -
An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity 2 3 ACKNOWLEDGEMENTS
P a g e | 1 DRAFT FOR CBD PEER-REVIEW ONLY; NOT TO QUOTE; NOT TO CIRCULATE 1 An updated synthesis of the impacts of ocean acidification on marine biodiversity 2 3 ACKNOWLEDGEMENTS ....................................................................................................... 3 4 5 EXECUTIVE SUMMARY ....................................................................................................... 4 6 7 1. Background and introduction ............................................................................................... 8 8 1.1. Mandate of this review .......................................................................................................... 8 9 1.2. What is ocean acidification? ........................................................................................ 9 10 1.3. Re-visiting key knowledge gaps identified in the previous CBD review ................... 14 11 12 2. Scientific and policy framework ........................................................................................ 17 13 2.1. Steps towards global recognition and international science collaboration ................. 17 14 2.2. Intergovernmental interest in ocean acidification and actions to date ........................ 19 15 16 3. Global status and future trends of ocean acidification ....................................................... 23 17 3.1. Variability .................................................................................................................. 23 18 3.2. Modelled simulations of future ocean -
DENTAL EROSION Dental Erosion, Also Known As Erosive Tooth Wear, Is Caused by Acid Contacting and Dissolving the Tooth Surface
Caring for your teeth OCTOBER 2018 DENTAL EROSION Dental erosion, also known as erosive tooth wear, is caused by acid contacting and dissolving the tooth surface. This creates thinning of the enamel which can weaken the tooth and make it sensitive. As the outer protective layer of enamel dissolves from the tooth surface, the dentine underneath is exposed which can make the tooth sensitive. The dentine is softer than enamel and dissolves much easier in acid. Preventing dental erosion is very important for protecting our teeth. Where does the acid come from? What else can increase dental The acid that causes erosion mainly comes from food or erosion? drink. Common sources of dietary acids that have been As well as frequent exposure to acid, low salivary flow (dry linked to dental erosion are: mouth) can increase the risk of dental erosion. A healthy flow • Soft drinks of saliva protects the teeth by washing away and neutralising • Energy drinks acid. Dry mouth can be caused by: • Sports drinks • Medications and taking multiple medications together • Vinegar • Radiotherapy to the head/neck • Citrus fruits • Stress • Fruit juices • Sjogren’s syndrome (an auto-immune disease) • Fruit-flavoured water • Smoking • Fruit-flavoured tea (e.g. lemon, peach, rosehip) • Diabetes • Cordial • Alcoholic drinks • Sour (acidic) sweets/lollies • Chewable Vitamin C tablets • Effervescent or dissolvable vitamins/medications Remember, even sugar-free food or drink can cause dental erosion if it’s high in acid. Common acidic food additives to be aware of are: • Citric acid (food acid acidity regulator/antioxidant 330) • Sodium citrate (food acid/acidity regulator/antioxidant 331) • Malic acid (food acid/preservative 296) • Ascorbic acid (Vitamin C/antioxidant 300) • Fruit juice concentrate.