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Ecology in Palau Chapter 1
ECOLOGY IN PALAU CHAPTER 1 CHAPTER 1 also has the largest tract of tropical lowland Ecology in Palau forest in the Pacific (Kitalong, 2014). In 1979, nearly 218 km2 or 52% of Palau’s land was The landscape of Palau is one of a medium to covered with lowland forests. Yet, slowly, forests low volcanic island chain with large fringing ECOLOGY IN PALAU are being cut for homesteads, development and/or barrier reefs. The Palauan island chain and roads. Forest trees and plants are valued as has all three-island types: volcanic, limestone Christopher Kitalong, David Mason sources of timber, food, medicine, habitat for and atolls. Palau’s proximity to the Asian other species, and for their cultural and aesthetic continent, Philippines, and Indonesia results Settings value (Kitalong, 2008). in increased radiation of plant taxa compared The archipelago of Palau was formed during to other islands in Micronesia. Despite being the Eocene epoch, 40 million years ago by the closest Micronesian island to larger land the subduction of the Pacific Plate beneath masses, Palau is still relatively isolated. Due the Philippine Plate along the Kyushu-Palau to these factors, Palau has the greatest number Ridge (PALARIS, 2009). Palau lies on the of endemics and highest species richness in east edge of the Andesite Line, which divides the Micronesian island chain (Canfield, 1981). the deeper basalts of the Central Pacific Basin However, the amount of arable soil is very from the partially submerged continental areas limited and very prone to erosion. As suggested of andesite. Volcanism ceased 20 million years by the USDA report deposited at Forestry ago and was succeeded by submergence of Service in Palau, islands and formation of the barrier reef began. -
Provenance Studies of Polynesian Basalt Adze Material: a Review and Suggestions for Improving Regional Data Bases
Provenance Studies of Polynesian Basalt Adze Material: A Review and Suggestions for Improving Regional Data Bases MARSHALL 1. WEISLER PACIFIC ARCHAEOLOGISTS have long been interested in the settlement of Polyne sia, the origin of colonizing groups at distant archipelagoes, and subsequent social interaction between island societies (see, for example, Howard 1967; Irwin 1990; Kirch and Green 1987). Early material studies in Polynesia inferred migration routes and social interaction from the distribution of similar architecture, especially marae (Emory 1943; also R. Green 1970), adzes (Emory 1961), and fishhooks (Sinoto 1967). The identification of exotic raw materials and finished artifacts throughout Polynesia eliminates the ambiguity often presented by linking stylistic similarities across space and through time. In relation to the long history of identifying exotic lithic materials from archaeological sites (see, for example, Grimes 1979), the compositional analysis of oceanic obsidians was begun quite recently (Key 1968). The efficacy of chemical characterization of artifacts and quarry material in New Zealand provided the in centive to apply similar techniques to obsidian of the southwest Pacific, where several large sources were known and where the archaeological distribution of this material was tl)ought to be widespread (Ambrose 1976). Although it has been possible to define the spread and interaction of human groups in the southwest Pacific by determining the spatial and temporal distribution of obsidian and pot tery, these materials are restricted to a few areas in Polynesia. Consequently, the effort to document prehistoric interaction throughout Polynesia must proceed without using obsidian or pottery. This leaves only basalt (debitage, formed arti facts, and oven stones), pearlshell, and volcanic glass as material for distributional studies (Best et al. -
Extraction of Alumina from Local Clays Using Hydrochloric Acid
International Journal of Scientific Research and Engineering Development-– Volume 2 Issue 4, July – Aug 2019 Available at www.ijsred.com Extraction of Alumina from Local Clays Using Hydrochloric Acid 1Eze, J.U., 2Anyakwo, C.N., 3Osoka, E.C. 4Nnodum, A.N., 5Onuoha, C., 6Anusi, M.O., 1,2,4,5Department of Material and Metallurgical Engineering, Federal University of Technology, Owerri 3,6 Department of Chemical Engineering, Federal University of Technology, Owerri -------------------------------------- ************************ -------------------------------- Abstract The present work investigates the extraction of alumina from different local clay samples; Ihiala clay (sample A), Nsu clay (sample B), and Umuhu clay (sample C), which contain 27.83%, 29.93%, and 28.31% of Al 2O3 respectively and are extremely abundant in the Eastern part of Nigeria. The clay samples were crushed, ground and sieved using 100 mesh standard tyler screens and were further calcined at a temperature of 700 0C, held for 1hr and then leached with 5ml of concentrated hydrochloric acid at different leaching temperatures (25 0C,50 0C,75 0C, 100 0C) and time (10,30,60,80,100 and 120mins). A relatively large increase in percentage extraction of Al 2O3 was also observed with increasing leaching temperature in the range of 25 0C to 100 0C. The effects of the leaching time and temperatures were investigated using response surface methodology. A pure- quadratic model fit well to experimental data for the three clay samples. The surface plot revealed a linear relationship with temperature, which had more effect of percentage alumina extracted, and a quadratic relationship with time. An estimated optimum extraction condition for the three clay samples would be a leaching time of 76minutes and temperature of 100 OC. -
The Cultural Landscapes of the Pacific Islands Anita Smith 17
World Heritage Convention Cultural Landscapes of the Pacific Islands ICOMOS Thematic study Anita Smith and Kevin L. Jones December 2007 ICOMOS 49-51 rue de la Fédération – 75015 Paris Tel +33 (0)1 45 67 67 70 – Fax +33 (0)1 45 66 06 22 www.icomos.org – [email protected] Contents Part 1: Foreword Susan Denyer 3 Part 2: Context for the Thematic Study Anita Smith 5 - Purpose of the thematic study 5 - Background to the thematic study 6 - ICOMOS 2005 “Filling the Gaps - An Action Plan for the Future” 10 - Pacific Island Cultural Landscapes: making use of this study 13 Part 3: Thematic Essay: The Cultural Landscapes of the Pacific Islands Anita Smith 17 The Pacific Islands: a Geo-Cultural Region 17 - The environments and sub-regions of the Pacific 18 - Colonization of the Pacific Islands and the development of Pacific Island societies 22 - European contact, the colonial era and decolonisation 25 - The “transported landscapes” of the Pacific 28 - Principle factors contributing to the diversity of cultural Landscapes in the Pacific Islands 30 Organically Evolved Cultural Landscapes of the Pacific 31 - Pacific systems of horticulture – continuing cultural landscapes 32 - Change through time in horticultural systems - relict horticultural and agricultural cultural landscapes 37 - Arboriculture in the Pacific Islands 40 - Land tenure and settlement patterns 40 - Social systems and village structures 45 - Social, ceremonial and burial places 47 - Relict landscapes of war in the Pacific Islands 51 - Organically evolved cultural landscapes in the Pacific Islands: in conclusion 54 Cultural Landscapes of the Colonial Era 54 Associative Cultural Landscapes and Seascapes 57 - Storied landscapes and seascapes 58 - Traditional knowledge: associations with the land and sea 60 1 Part 4: Cultural Landscape Portfolio Kevin L. -
Nanoparticle Catalytic Enhancement of Carbon Dioxide Reforming of Methane for Hydrogen Production Nicholas Groden
Louisiana Tech University Louisiana Tech Digital Commons Doctoral Dissertations Graduate School Fall 11-17-2018 Nanoparticle Catalytic Enhancement of Carbon Dioxide Reforming of Methane for Hydrogen Production Nicholas Groden Follow this and additional works at: https://digitalcommons.latech.edu/dissertations Part of the Nanoscience and Nanotechnology Commons, Other Chemical Engineering Commons, and the Other Materials Science and Engineering Commons Recommended Citation Groden, Nicholas, "" (2018). Dissertation. 3. https://digitalcommons.latech.edu/dissertations/3 This Dissertation is brought to you for free and open access by the Graduate School at Louisiana Tech Digital Commons. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of Louisiana Tech Digital Commons. NANOPARTICLE CATALYTIC ENHANCEMENT OF CARBON DIOXIDE REFORMING OF METHANE FOR HYDROGEN PRODUCTION by Nicholas Groden, M.S., B.S. A Dissertation Presented in Partial Fulfillment of the Requirements of the Degree Doctor of Philosophy COLLEGE OF ENGINEERING AND SCIENCE LOUISIANA TECH UNIVERSITY November 2018 LOUISIANA TECH UNIVERSITY THE GRADUATE SCHOOL JUNE 16, 2018 Date We hereby recommend that the dissertation prepared under our supervision by xxxxxxxxxxxxxxx Nicholas Groden, M.S., B.S. entitled Nanoparticle Catalytic Enhancement of Carbon Dioxide Reforming of Carbon Dioxide Reforming of Methane for Hydrogen Production be accepted in partial fulfillment of the requirements for the Degree of Doctor of Philosophy in Engineering Micro and Nanoscale Systems Supervisor of Dissertation Research Head of Department Department Recommendation concurred in: _____________________________ _____________________________ Advisory Committee _____________________________ _____________________________ Approved: Approved: __________________________________ ______________________________ Director of Graduate Studies Dean of the Graduate School __________________________________ Dean of the College GS Form 13 (8/10) ABSTRACT The U.S. -
Geology of Saipan Mariana Islands Part 2
Geology of Saipan Mariana Islands Part 2. Petrology and Soils GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-B-D Geology of Saipan Mariana Islands Part 2. Petrology and Soils GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-B-D Chapter B. Petrology of the Volcanic Rocks By ROBERT GEORGE SCHMIDT Chapter C. Petrography of the Limestones By J. HARLAN JOHNSON Chapter D. Soils By RALPH J. McCRACKEN UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR Fred A. Seaton, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS OF PART 2 Page Chapter B. Petrology of the Volcanic Rocks .... 127 Chapter C. Petrography of the Limestones ...... 177 Chapter D. Soils ................................ 189 m GEOLOGICAL SURVEY PROFESSIONAL PAPER 280 Geology of Saipan, Mariana Islands Part 1. General Geology Chapter A. General Geology By PRESTON E. CLOUD, JR., ROBERT GEORGE SCHMIDT, and HAROLD W. BURKE Part 2. Petrology and Soils Chapter B. Petrology of the Volcanic Rocks By ROBERT GEORGE SCHMIDT Chapter C. Petrography of the Limestones By J. HARLAN JOHNSON Chapter D. Soils By RALPH J. McCRACKEN Part 3. Paleontology Chapter E. Calcareous Algae By J. HARLAN JOHNSON Chapter F. Discoaster and Some Related Microfossils By M. N. BRAMLETTE Chapter G. Eocene Radiolaria By WILLIAM RIEDEL Chapter H. Smaller Foraminifera By RUTH TODD dhapter I. Larger Foraminifera By W. STORRS COLE ^Chapter J. Echinoids By C. WYTHE COOKE ~Part 4. Submarine Topography and Shoal-Water Ecology ^Chapter K. Submarine Topography and Shoal-Water Ecology By PRESTON E. CLOUD, JR. -
The European Union Aluminium Industry the Impact of the Eu Trade Measures on the Competitiveness of Downstream Activities
THE EUROPEAN UNION ALUMINIUM INDUSTRY THE IMPACT OF THE EU TRADE MEASURES ON THE COMPETITIVENESS OF DOWNSTREAM ACTIVITIES June 2019 GRUPPO DI RICERCHE INDUSTRIALI E FINANZIARIE - GRIF “FABIO GOBBO” LUISS GUIDO CARLI UNIVERSITY The EU aluminium industry. The impact of the EU trade measures on the competitiveness of downstream activities 1 The EU aluminium industry. The impact of the EU trade measures on the competitiveness of downstream activities Authors and contributors Ernesto Cassetta, GRIF “Fabio Gobbo”, University of Udine Umberto Monarca, GRIF “Fabio Gobbo”, University of Foggia Cesare Pozzi, GRIF “Fabio Gobbo”, LUISS University Davide Quaglione, GRIF “Fabio Gobbo”, D’Annunzio University of Chieti-Pescara Alessandro Sarra, GRIF “Fabio Gobbo”, D’Annunzio University of Chieti-Pescara GRUPPO DI RICERCHE INDUSTRIALI E FINANZIARIE - GRIF “FABIO GOBBO” Department of Business and Management LUISS Guido Carli University Viale Romania, 32 00197 Roma (Italia) 2 The EU aluminium industry. The impact of the EU trade measures on the competitiveness of downstream activities 3 The EU aluminium industry. The impact of the EU trade measures on the competitiveness of downstream activities Disclaimer This project has been funded with support from FACE - The Federation of Aluminium Consumers in Europe. We were asked by FACE to carry out an independent study with the aim of establishing a constructive and transparent exchange of views on the competitiveness of the aluminium value chain in the European Union with a specific focus on trade policies on unwrought aluminium and their impact on manufacturers of aluminium semi-finished products. To have consistent information and to ensure the robustness and the comparability of the quantitative analysis for well-informed design of policies, the study only relies on data provided by institutional sources and independent third parties, having market recognition for reliability. -
Stone Tools from the Ancient Tongan State Reveal Prehistoric Interaction Centers in the Central Pacific
Stone tools from the ancient Tongan state reveal prehistoric interaction centers in the Central Pacific Geoffrey R. Clarka,1, Christian Reepmeyera, Nivaleti Melekiolab, Jon Woodheadc, William R. Dickinsond, and Helene Martinsson-Walline aArchaeology and Natural History, College of Asia and the Pacific, Australian National University, Canberra, ACT 0200, Australia; bLapaha Town Council, Lapaha Village, Tongatapu, Kingdom of Tonga; cSchool of Earth Sciences, The University of Melbourne, Parkville, VIC 3010, Australia; dDepartment of Geoscience, University of Arizona, Tucson, AZ 85721; and eDepartment of Archaeology and Ancient History, Gotland Campus, Uppsala University, 75105 Uppsala, Sweden Edited by Patrick V. Kirch, University of California, Berkeley, CA, and approved June 10, 2014 (received for review April 2, 2014) Tonga was unique in the prehistoric Pacific for developing a mari- involved control and distribution of prestige exotic goods by elites time state that integrated the archipelago under a centralized and whether the polity’s interaction sphere was only one of several authority and for undertaking long-distance economic and political prehistoric networks responsible for the movement of people, exchanges in the second millennium A.D. To establish the extent goods, and ideas in the Central Pacific. of Tonga’s maritime polity, we geochemically analyzed stone tools This article reports the analysis of a significant lithic artifact excavated from the central places of the ruling paramounts, par- assemblage recovered during recent excavations of sites of the ticularly lithic artifacts associated with stone-faced chiefly tombs. Tongan polity, which was manifested by the construction of The lithic networks of the Tongan state focused on Samoa and Fiji, religo-political centers containing monumental architecture on with one adze sourced to the Society Islands 2,500 km from Ton- the island of Tongatapu (297 km2), where the political hier- gatapu. -
A Hundred Years of the Bayer Process for Alumina Production*
Essential Readings in Light Metals: Alumina and Bauxite. Edited by Don Donaldson and Benny E. Raahauge. 2013 The Minerals, Metals & Materials Society. Published 2013 by John Wiley & Sons, Inc. 2. BAYER PROCESS This section includes five significant areas: 1. Bayer Process Design. This first area includes the fundamental principles of Bayer process design as well as the history of the development of the Bayer pro- cess. The basic process has not changed but the development of its application for more than a century is truly remarkable. What is even more remarkable is that sig- nificant further improvement is feasible. 2. Physical Data. Contains much of the materials and liquor data needed to prepare flow sheets and heat and material balances. 3. Calcium Chemistry. Included are papers that discuss the effects and use of lime in the process as well as using lime to re-causticize (react) sodium carbonate back to sodium hydroxide. 4. Silica Chemistry. These papers discuss the dissolution of bauxite silica during digestion and the subsequent reaction that forms solid sodium aluminum silicate (desilication product). 5. Organic Removal. These papers deal with the important subject of removing accumulated sodium organates (originating from organic carbon compounds in the bauxite) from Bayer liquor to enhance alumina product quality and to improve pro- cess productivity of alumina. Equally good papers in the list of recommended readings could not be included as published papers because of the limitation on the size of the book. Fred Williams 83 Essential Readings in Light Metals: Alumina and Bauxite. Edited by Don Donaldson and Benny E. -
Volcanoes Flying Through Volcanic Ash Can Be
Volcanoes Flying through volcanic ash can be hazardous to your plane! ⇒ 1982 British Airways ⇒ 1989 KLM Boeing 247 from Alaskan Volcano ⇒ 1991 Mount Pinatubo ⇒ Since 1990 damage to at least 15 aircraft Volcanoes are not all bad: 1) Esthetic beauty 2) Skiing and hiking 3) Soils can be productive However, of course they can kill. Who Should Worry? In short – People who live on plate boundaries. ⇒ Most dangerous, convergent plate boundaries with subduction zones ⇒ 900/1350 volcanoes that have erupted are on the Pacific ring of fire (N.Z., Japan, Alaska, Mexico, C.A., Chile) Mt. Erebus of Antarctica is the farthest south ⇒ Other famous: Mediterranean – Vesuvius, Etna, Stromboli Stromboli - “Lighthouse of the Mediterranean” ⇒ Most active – mild eruption of fluid lava, typically at Divergent Plate Boundaries ⇒ 2x more volcanoes north of the equator Can affect world climate Examples: Tamboru (1815), El Chichon (1982), Mt. Pinatubo (1991) ⇒ Us- no one east of New Mexico (Figure 5.2 &5.3) – tectonics Main mainland U.S. zone – Cascadia Subduction Zone ⇒ WA, OR, CA “Alaska is the second most active volcanic region in the world, and Hawaii is not far behind.” Nature of the Problem VEI – Volcanic Explosivity Index (Figures 5.4 & 5.5) ⇒ Related to volume of stuff erupted, height it rises, and duration of eruption ⇒ Mount St. Helens (1980) – Explosive to Cataclysmic – 4 ⇒ VEI can increase with time ⇒ Magnitude and frequency – Yellowstone (cataclysmic book) ⇒ Magma’s viscosity is important T↑, V↓ or T↓, V↑ Silica: the more siliceous, the more viscous Felsic vs. Mafic and the Andesite Line Andesite Line: From Alaska to east of N.Z. -
The Geology of Tofua Island, Tonga!
The Geology of Tofua Island, Tonga! GLENN R. BAUER2 ABSTRACT: Tofua Island is an oval, steep-sided composite volcano, 5 miles by 6 miles in diameter, the summit of which has collapsed to form a caldera. Within the caldera, Lofia cone is still active. Four units have been mapped: (1) the Hamatua Formation, of precaldera age, includes basaltic andesites, pyroxene andesites, and pyroxene dacites; (2 ) the Hokula Froth Lava, a microvesiculated lava flow of andesite; ( 3) the Kolo Formation, composed of air-laid lapilli tuff-breccia, tuff, unconsolidated ash and cinder, small basaltic andesite lava flows, and one thick pyroxene andesite lava flow; and (4) the Lofia Formation, composed of air-laid tuff, ash, basaltic andesite lava flows, and andesite lava flows. An erosional unconformity separates the Hamatua Formation from the Hokula Froth Lava, and another lies between the froth lava and the Kolo Formation. The rocks are typical orogenic andesites and related types, unusually high in CaO, which is reflected in the calcic nature of the plagioclase. The pyroxenes of the groundmass are usually pigeonite and pigeonitic augite, whereas the phenocrysts are augite. Hypersthene is less common and occurs only as phenocrysts surrounded by reaction rims of pigeonite and/or pigeonitic augite. Concentric normal faults associated with caldera collapse are common on the northern, eastern, and southern rims of the caldera. Some of the faults have served as conduits for rising magma of the Kolo Formation; others, on which caldera collapse is continuing, do not exhibit .associared volcanism. Tensional cracks are abundant along the southern rim. THE GEOLOGICAL INVESTIGATION of Tofua foot contour intervals was drawn up primarily Island is part of a larger study of the Tonga and for the gravimetric work, but it was also used as the Lau islands by the Hawaii Institute of Geo a base for the geologic mapping (Fig. -
Shipboard Report, Capricorn Expedition 26 September 1952-21
University of California Scripps Institution of Oceanography Shipboard Report, Capricorn Expedition 26 September 1952 – 21 February 1953 Sponsored by Office of Naval Research and Bureau of Ships SIO Reference 53-15 25 February 1953 ― ii ― ― iii ― ― iv ― PREFACE CAPRICORN was the fourth of a series of oceanographic expeditions into the deep Pacific sponsored by the Navy Department and the University of California. In 1950, the MID-PACIFIC Expedition was devoted largely to exploration of the sea floor in the area between Cape Mendocino, the Marshall Islands, and the Equator. In 1951, NORTHERN HOLIDAY conducted hydrographic and geologic studies in the eastern North Pacific between San Diego and the Aleutian Islands. Hydrographic exploration of the eastern Central Pacific was the principal objective of SHELLBACK, in 1952. On the present expedition we ventured farther south than on any of our previous cruises, and most of the work was done between the Equator and the Tropic of Capricorn. Hence the name, CAPRICORN. CAPRICORN, like the preceding expeditions, was generously supported by the Office of Naval Research and the Bureau of Ships of the Navy Department. The meteorological program was supported by the Air Force Cambridge Research Center. FIGURE 1 CAPRICORN station chart. The chart shows BAIRD's position on seismic stations and also stations for both HORIZON and BAIRD where a temperature probe, hydrographic series, core, or dredge haul was taken or where a dive was made. BT lowerings, GEK observations, echo soundings and magnetometer surveys, net hauls, SOFAR bomb drops, and meteorological observations are not indicated. The stations in the Tonga area are shown on chart in Figure 2.