Comparison of Public Perception in Desert and Rainy Regions of Chile Regarding the Reuse of Treated Sewage Water
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Epidemiology of Dog Bite Incidents in Chile: Factors Related to the Patterns of Human-Dog Relationship
animals Article Epidemiology of Dog Bite Incidents in Chile: Factors Related to the Patterns of Human-Dog Relationship Carmen Luz Barrios 1,2,*, Carlos Bustos-López 3, Carlos Pavletic 4,†, Alonso Parra 4,†, Macarena Vidal 2, Jonathan Bowen 5 and Jaume Fatjó 1 1 Cátedra Fundación Affinity Animales y Salud, Universitat Autónoma de Barcelona, Parque de Investigación Biomédica de Barcelona, C/Dr. Aiguader 88, 08003 Barcelona, Spain; [email protected] 2 Escuela de Medicina Veterinaria, Facultad de Ciencias, Universidad Mayor, Camino La Pirámide 5750, Huechuraba, Región Metropolitana 8580745, Chile; [email protected] 3 Departamento de Ciencias Básicas, Facultad de Ciencias, Universidad Santo Tomás, Av. Ejército Libertador 146, Santiago, Región Metropolitana 8320000, Chile; [email protected] 4 Departamento de Zoonosis y Vectores, Ministerio de Salud, Enrique Mac Iver 541, Santiago, Región Metropolitana 8320064, Chile; [email protected] (C.P.); [email protected] (A.P.) 5 Queen Mother Hospital for Small Animals, Royal Veterinary College, Hawkshead Lane, North Mymms, Hertfordshire AL9 7TA, UK; [email protected] * Correspondence: [email protected]; Tel.: +56-02-3281000 † These authors contributed equally to this work. Simple Summary: Dog bites are a major public health problem throughout the world. The main consequences for human health include physical and psychological injuries of varying proportions, secondary infections, sequelae, risk of transmission of zoonoses and surgery, among others, which entail costs for the health system and those affected. The objective of this study was to characterize epidemiologically the incidents of bites in Chile and the patterns of human-dog relationship involved. The results showed that the main victims were adults, men. -
SURNAMES in CHILE a Study of the Population of Chile Through
Page 1 of 31 American Journal of Physical Anthropology 1 2 3 SURNAMES IN CHILE 4 5 A study of the population of Chile through isonymy 6 I. Barrai, A. Rodriguez-Larralde 2, J. Dipierri 1, E.Alfaro 1, N. Acevedo 3, 7 8 E. Mamolini, M. Sandri, A.Carrieri and C. Scapoli. 9 10 Dipartimento di Biologia ed Evoluzione, Università di Ferrara, 44121- Ferrara, Italy 11 1Instituto de Biología de la Altura, Universidad Nacional de Jujuy, 4600 – San Salvador De Jujuy, 12 13 Argentina. 14 2 15 Centro de Medicina Experimental, Laboratorio de Genetica Humana, IVIC, 1020A -Caracas, 16 Venezuela. 17 18 3Museo Nacional de Ciencias Naturales, Santiago, Chile 19 20 21 Running title: Surnames in Chile 22 23 24 25 26 Correspondence to: 27 Chiara Scapoli 28 Department of Biology and Evolution 29 30 University of Ferrara, 31 Via L. Borsari 46, - I-44121 Ferrara, Italy. 32 Telephone: +39 0532 455744; FAX: : +39 0532 249761 33 Email: [email protected] 34 35 36 Number of text pages: 15 37 Literature pages: 4 38 39 Number of Tables : 2 40 41 Number of Figures: 7 42 43 44 KEYWORDS : Chile, Population Structure, Isonymy, Inbreeding, Isolation by distance 45 46 47 ACKNOWLEDGMENTS: The authors are grateful to the Director of the Servicio Electoral de la 48 49 Republica de Chile Sr. Juan Ignacio Garcia Rodríguez, who made the data available, and to Sr. 50 51 Dr.Ginés Mario Gonzalez Garcia, Embajador de la Republica Argentina en Chile. The work was 52 supported by grants of the Italian Ministry of Universities and Research (MIUR) to Chiara Scapoli. -
The Evolution of the Location of Economic Activity in Chile in The
Estudios de Economía ISSN: 0304-2758 [email protected] Universidad de Chile Chile Badia-Miró, Marc The evolution of the location of economic activity in Chile in the long run: a paradox of extreme concentration in absence of agglomeration economies Estudios de Economía, vol. 42, núm. 2, diciembre, 2015, pp. 143-167 Universidad de Chile Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=22142863007 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative TheEstudios evolution de Economía. of the location Vol. 42 of -economic Nº 2, Diciembre activity in2015. Chile… Págs. / Marc143-167 Badia-Miró 143 The evolution of the location of economic activity in Chile in the long run: a paradox of extreme concentration in absence of agglomeration economies*1 La evolución de la localización de la actividad económica en Chile en el largo plazo: la paradoja de un caso de extrema concentración en ausencia de fuerzas de aglomeración Marc Badia-Miró** Abstract Chile is characterized as being a country with an extreme concentration of the economic activity around Santiago. In spite of this, and in contrast to what is found in many industrialized countries, income levels per inhabitant in the capital are below the country average and far from the levels in the wealthiest regions. This was a result of the weakness of agglomeration economies. At the same time, the mining cycles have had an enormous impact in the evolution of the location of economic activity, driving a high dispersion at the end of the 19th century with the nitrates (very concentrated in the space) and the later convergence with the cooper cycle (highly dispersed). -
Report on Cartography in the Republic of Chile 2011 - 2015
REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 ARMY OF CHILE MILITARY GEOGRAPHIC INSTITUTE OF CHILE REPORT ON CARTOGRAPHY IN THE REPUBLIC OF CHILE 2011 - 2015 PRESENTED BY THE CHILEAN NATIONAL COMMITTEE OF THE INTERNATIONAL CARTOGRAPHIC ASSOCIATION AT THE SIXTEENTH GENERAL ASSEMBLY OF THE INTERNATIONAL CARTOGRAPHIC ASSOCIATION AUGUST 2015 1 REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 CONTENTS Page Contents 2 1: CHILEAN NATIONAL COMMITTEE OF THE ICA 3 1.1. Introduction 3 1.2. Chilean ICA National Committee during 2011 - 2015 5 1.3. Chile and the International Cartographic Conferences of the ICA 6 2: MULTI-INSTITUTIONAL ACTIVITIES 6 2.1 National Spatial Data Infrastructure of Chile 6 2.2. Pan-American Institute for Geography and History – PAIGH 8 2.3. SSOT: Chilean Satellite 9 3: STATE AND PUBLIC INSTITUTIONS 10 3.1. Military Geographic Institute - IGM 10 3.2. Hydrographic and Oceanographic Service of the Chilean Navy – SHOA 12 3.3. Aero-Photogrammetric Service of the Air Force – SAF 14 3.4. Agriculture Ministry and Dependent Agencies 15 3.5. National Geological and Mining Service – SERNAGEOMIN 18 3.6. Other Government Ministries and Specialized Agencies 19 3.7. Regional and Local Government Bodies 21 4: ACADEMIC, EDUCATIONAL AND TRAINING SECTOR 21 4.1 Metropolitan Technological University – UTEM 21 4.2 Universities with Geosciences Courses 23 4.3 Military Polytechnic Academy 25 5: THE PRIVATE SECTOR 26 6: ACKNOWLEDGEMENTS AND ACRONYMS 28 ANNEX 1. List of SERNAGEOMIN Maps 29 ANNEX 2. Report from CENGEO (University of Talca) 37 2 REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 PART ONE: CHILEAN NATIONAL COMMITTEE OF THE ICA 1.1: Introduction 1.1.1. -
Unidades Sedimentarias Cenozoicas De La Cuenca Del Rio Loa En La Pampa Del Tamarugal, Region De Antofagasta, Chile
ESTRATlGRAFIA DE LAS -UNIDADES SEDIMENTARIAS CENOZOICAS DE LA CUENCA DEL RIO LOA EN LA PAMPA DEL TAMARUGAL, REGION DE ANTOFAGASTA, CHILE. JOSE A. NARANJO Servo Nac. Geol. y Minería, Casilla 10465, Santigo, Chile. ROLAND. P. PASKOFF Département de Géographie, Université de Tunis, 94, Bd. du 9 avril1938, Túnez. RESUMEN El relleno sedimentario de la cuenca del río Loa, en la Pampa del Tamarugal, es de gran complejidad. En él es posible distinguir al menos seis unidades diferentes. Su génesis se explicaría por la intervención e interacción de cambios climáticos en un ambiente árido, y de movimientos tectónicos durante el Cenozoico. ABSTRACT The sedimentary filling of the Pampa del Tamarugal in the Río Loa basin is compleXo At lcast six different units can be distinguished. Interferences between climatic changes in an arid environment and tectonic move ments account for their genesis. INTRODUCCION Durante mucho tiempo se ha pensado que el voluminoso relleno de depósitos aluviales y evapo ríticos de la depresión seguida por el río Loa, entre Calama y Quillagua (Fig. 1), correspondería a una sola formación, la Formación El Loa (Brüggen, 1950; Fuenzalida, 1957). Esta opinión prevalece todavía en estudios geológicos recientes (Boben rieth, 1980; Boric, 1980; Maksaev y Marinovic 1980), pese a que, en 1975, Rieu llamó la atención sobre la complejidad de los depósitos que rellenan la cuenca. Efectivamente, es posible distinguir va rias unidades estratigráficas, claramente separadas por discordancias de erosión (Fig. 2). Recientemente, Naranjo y Paskoff (1981) han caracterizado la estratigrafía del Cenozoico del sec tor comprendido entre Chiuchiu y Calama (22°20'- 22°27'S). -
Rethinking the Tiwanaku Phenomenon in San Pedro De
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Textile Society of America Symposium Proceedings Textile Society of America 9-2014 Rethinking the Tiwanaku Phenomenon in San Pedro de Atacama Through the Study of Textiles of Solcor 3 and Their Associated Contexts (400-1000 AD) Carolina Aguero Universidad Católica del Norte, [email protected] Mauricio Uribe Universidad de Chile Follow this and additional works at: http://digitalcommons.unl.edu/tsaconf Part of the Art and Design Commons, and the Art Practice Commons Aguero, Carolina and Uribe, Mauricio, "Rethinking the Tiwanaku Phenomenon in San Pedro de Atacama Through the Study of Textiles of Solcor 3 and Their Associated Contexts (400-1000 AD)" (2014). Textile Society of America Symposium Proceedings. 934. http://digitalcommons.unl.edu/tsaconf/934 This Article is brought to you for free and open access by the Textile Society of America at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Textile Society of America Symposium Proceedings by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Rethinking the Tiwanaku Phenomenon in San Pedro de Atacama Through the Study of Textiles of Solcor 3 and Their Associated Contexts (400-1000 AD) Carolina Agüero1 and Mauricio Uribe2 In this opportunity we will talk about the Tiwanaku problematic in San Pedro de Atacama because the interpretations so far are not substantial, and also now we have new information which forces us to rethink this phenomenon. The current state of the investigation keeps a conservative and hegemonic idea about the relation between both entities giving us simple explanations about the social complexity, in which the History of San Pedro depends on the existence of Tiwanaku and the social development of a State project. -
Hoyas Hidrográficas De Chile: Segunda Región
HOYAS HIDROGRÁFICAS DE CHILE: SEGUNDA REGIÓN REALIZADO POR: HANS NIEMEYER F. HOVA DEL RlO LOA La hoya hidrográfica del río Loa~ con una superf! cie tota~'de 33 570 km2 , se desarrolla en el tercio norte de la IIa R~ gión de Chile, entre latitudes extremas 20Q52' y 22Q57' L.S. ylongit~ des 68QOO' y 7oQ02' L.o. El río Loa nace en la falda norte del Vn. Mi ño~ en los Ojos del Hiño, casi en los límites entre la la y IIa Regio nes de Chile, en 21Q15' L.S. y 70Q L.O~ Su longitud total se acerca a 440 km. A pesar de su extensa hoya, los recursos h!dricos provienen de la cuenca alta que comprende alrededor del 20% de la su~ perficie total. Con curso aproximadamente norte-sur~ el Loa reco rre casi 150 km en un profundo cañón de altura variable, desde su nací miento hasta el oasis de Chiu ~hiu, pueblo que se levanta en su margen izquierda. En este trayecto recibe sus dos tributarios más importantes que le caen del este: el río San Pedro o Inacaliri y el río Salado. En Chiu Chiu dobla su curso sensiblemente hacia el oeste para alcanzar en un recorrido de 115 km el punto denominado Chacance. En él se le reúne por la derecha el río San Salvador. En Chacance,el Loa toma franca di= recci6n sur-norte hasta fertilizar el oasis de Quillagua, despu~s de una trayectoria de 80 km. A partir de Quillagua el Loa describe un gran arco y luego desemboca en el Pacífico~ en Caleta Huel~n, despu~8 de trasponer el macizo costero en un tajo profundo~ de más de 500 m de al tura. -
Manufacturing Landscape It's a Sunny Morning in Santiago, Chile's Capital. Tamara Pérez and Antonella Mele Are Standing In
Manufacturing Landscape Words Frederico Duarte Photographs Cristóbal Olivares It’s a sunny morning in Santiago, Chile’s capital. Tamara Pérez and Antonella Mele are standing in what was once the dining room of a pretty 1960s apartment building in Providencia, a mainly residential quarter of the Chilean capital. Stood in silence, they are slowly and gently applying a black, grainy substance to a bulky stoneware object placed on the table in front of them. 72 Duarte, Frederico. “Manufacturing Landscape,” Disegno, April 2017. Tamara Pérez examining the lava In the adjacent room – surely a former living room – fabric, as if held by a kind hand. In 2016, three of products in GT2P’s studio, Santiago. the other members of the design studio Great Things these vases were included in the Italian furniture to People (GT2P) sit at laptops, scribbling on a brand Cappellini’s Progetto Oggetto collection, whiteboard-top table, talking on the phone, chatting. and are currently being manufactured in &OHMBOE A breeze flows through the many open windows and The second direction is CPP No2: Porcelain vs Lava doors of the ground-floor apartment, which is Lights, a series of wall lamps and chandeliers for sparsely furnished, and whose somewhat disorderly which GT2P perfected the casting process by rooms reveal models, materials, bits of prototypes, controlling the clay layers and therefore the tools, books, magazines. In one of these rooms a 3D thickness and translucency of the resulting shallow, porcelain printer is being installed. In the kitchen creamy white porcelain bowls. While working on there’s instant coffee and the odd ceramic cup on these lights the studio began to experiment with the counter, another porcelain printer and a kiln, lava samples collected from Chile’s Chaitén and where Pérez and Mele will soon place the object Villarrica volcanoes, performing heating and they have been working on. -
Diagnostico Regional De Suelos Abandonados Con Potencial Presencia De Contaminantes”
INFORME FINAL. Versión 4 “DIAGNOSTICO REGIONAL DE SUELOS ABANDONADOS CON POTENCIAL PRESENCIA DE CONTAMINANTES” CONTRATO NO 618775-3-LP13 31-Marzo-2014 Informe Final-versión 4 Página 1 INDICE GENERAL GLOSARIO DE TERMINOS UTILIZADOS EN ESTE INFORME. 4 ALCANCE Y PRESENTACION DEL INFORME 7 PARTE 1.- PRESENTACION DEL PROBLEMA. 10 1.1.- INTRODUCCIÓN GENERAL. 10 1.1.1 ESTADO DEL ARTE DE LA GESTION DE SUELOS CON POTENCIAL 12 PRESENCIA DE CONTAMINANTES. 1.2.- OBJETIVOS 15 1.2.1 Objetivo General 15 1.2.2 Objetivos Específicos 15 1.3.- GENERALIDADES DE LA METODOLOGIA DE TRABAJO 16 1.3.1Gestión de suelos con potencial presencia de contaminantes: identificación 16 y priorización. PARTE 2.- RECOPILACION Y SISTEMATIZACION DE LA INFORMACION 20 DISPONIBLE. 2.1 LA REGION DE ANTOFAGASTA Y LOS SUELOS CON POTENCIAL 20 PRESENCIA DE CONTAMINANTES. 2.1.1. Breve descripción de la región 20 2.1.2Estrategia de desarrollo regional 2009-2020 22 2.2 LEVANTAMIENTO DE INFORMACION 23 PARTE 3: PRIORIZACION Y JERARQUIZACION DE SUELOS 32 ABANDONADOS CON POTENCIAL PRESENCIA DE CONTAMINANTES. 3.1.- RESULTADOS DE LA PRIORIZACION DE SAPPC. 32 3.2.- RESULTADOS DE LA INSPECCION DE LOS SAPPC. 37 3.3 RESULTADOS DE LA JERARQUIZACION DE SAPPC. 41 PARTE 4.- INVESTIGACION PRELIMINAR Y CONFIRMATORIA. 48 4.1- INVESTIGACION PRELIMINAR 48 4.2- INVESTIGACION CONFIRMATORIA 48 4.2.1 DEFINICION DE CONTAMINANTES DE INTERES POTENCIAL. 49 4.2.2 HIPOTESIS DE DISTRIBUCION DE LOS CONTAMINANTES 52 4.2.3 TAMAÑO DEL SPPC. 53 4.2.4 COMPONENTES AMBIENTALES A MUESTREAR; NÚMERO Y TIPO DE 53 MUESTRAS. 4.2.5 MUESTRAS BLANCO O BACKGROUND 54 4.2.6 ANALISIS QUIMICO DE MUESTRAS AMBIENTALES 62 4.2.7 PROCEDIMIENTOS DE CONTROL Y ASEGURAMIENTO DE CALIDAD 72 4.2.8 COMPARACION CON VALORES DE REFERENCIA. -
Volcán Olca - Paruma
Volcán Olca - Paruma Región: Antofagasta Provincia: El Loa Comuna: Ollagüe Coordenadas: 20°56’32’’S – 68°30’12’ W Poblados más cercanos: Collahuasi – Cosca – Ollagüe Ranking de riesgo específico: 35 Altura: 5407 m snm Diámetro basal: 17 km Área basal: 227 km2 Volumen estimado: 74 km3 Última actividad: 03/1990 Última erupción mayor: 1865 - 1867 Volcán Olca desde el suroeste (Fotografía: Daniel Bertin) Corresponde a un complejo elongado de unos 15 km de largo orientado en dirección este-oeste, conformado por lavas dacíticas y andesíticas, que se encontraría activo desde hace unos 80 mil años. Dentro de este complejo destacan dos centros eruptivos: Olca, en el extremo oeste, y Paruma, en el extremo este, separados entre sí por alrededor de 8 km. Además de estos dos volcanes principales, existen a lo menos doce centros eruptivos, algunos con cráteres muy bien preservados. Desde el volcán Olca fueron emitidas lavas andesíticas a dacíticas que se extienden hasta 5 km al oeste del cráter central, las que se encuentran recubiertas por lavas de morfologías más recientes. Desde el volcán Paruma, numerosos flujos de lava de probable composición andesítica-basáltica fueron emitidos alcanzando casi 7 km tanto hacia el norte como hacia el sur. Al este de la cima principal del volcán Paruma se emitió una lava dacítica, la cual parece ser posterior a las morrenas glaciares desarrolladas en el flanco sur. Destacan depósitos de azufre principalmente en torno al volcán Olca, los que fueron explotados intensamente durante los siglos pasados. No hay certeza respecto a cuál es el sector actualmente activo. Existen reportes no confirmados de una erupción de flanco en el volcán Olca entre 1865 y 1867, mientras que en 1990 se reportó actividad fumarólica en el volcán Paruma la que estuvo acompañada de sismicidad menor. -
Statistical SYNTHESIS of CHILE 2008-2012 Statistical SYNTHESIS of CHILE 2008-2012
STATISTICAL SYNTHESIS OF CHILE 2008-2012 STATISTICAL SYNTHESIS OF CHILE 2008-2012 STATISTICAL SYNTHESIS OF CHILE • 2008-2012 TABLE OF CONTENTS MAP OF CHILE BY REGIONS 4 Chile its regions, provinces, and communes, as at 31 December 2012 5 GENERAL BACKGROUND 9 Location and area 9 Boundaries, climate and natural resources, temperature, rainfall of main Chilean towns 10 Air pollution statistics by sampling station in Greater Santiago 14 POPULATION 16 SYSTEM OF GOVERNMENT, AND POLITICAL AND ADMINISTRATIVE ORGANIZATION 18 ECONOMIC AND SOCIAL INDICATORS 21 Main indicators of domestic economy 21 National accounts 22 Public finance 27 Agriculture, forestry, woodland production and consumption, livestock and fishing 29 Mining 37 Manufacturing 38 Construction 41 Energy 42 Transport 44 Communications 45 Tourism 45 Prices 46 Money and banking 51 Interest rates 52 Balance of payments 54 Balance of trade by product 55 Gross foreign debt by maturity 59 Direct foreign investment under decree law 600 60 Employment 61 Wages 62 Social indicators 63 3 CENTRAL BANK OF CHILE MAP OF CHILE BY REGIONS Región (Capital) 72° 68° XV Arica y Parinacota (Arica) 19° 19° I Tarapacá (Iquique) II Antofagasta (Antofagasta) III Atacama (Copiapó) IV Coquimbo (La Serena) 32° V Valparaíso (Valparaíso) 32° RMS Metropolitana de Santiago (Santiago) VI Libertador Gral. Bdo. O´Higgins (Rancagua) VII Maule (Talca) VIII Biobío (Concepción) IX La Araucanía (Temuco) XIV Los Ríos (Valdivia) 43° X Los Lagos (Puerto Montt) 43° Chilean Antartic Territory 90° 53° XI Aysén del Gral.Carlos Ibáñez del Campo (Coihaique) (*) South Pole XII Magallanes y de La Antártica Chilena (Punta Arenas) 72° 68° 0 300 600 km 56° 56° (*) Agreement between Chile and Argentina to precisely trace the common boundary between Fitz Roy and Daudet mountains. -
Exposure to Arsenic of the Atacameno Population in Northern Chile
Assessing and Managing Health Risks from Drinking Water Contamination: Approaches and Applications (ProccedingsoftheRomeSymposium,Septemberl994).IAHSPubl.no.233, 1995. 141 Exposure to arsenic of the Atacameno population in northern Chile ANA MARIA SANCHA & DANIEL RODRIGUEZ Universidad de Chile, Depto. de Ingenieria Civil, Blanco Encalada 2120, 4° Piso, Of 17 Santiago, Chile, Casilla 228-3 FLAVIO VEGA & SERGIO FUENTES Institute de Salud Pûblica, Marathon 1000, Santiago, Chile ANA MARIA SALAZAR Asociaciôn Chilena de Seguridad, Vicuna Mackenna 152, Santiago, Chile VENTURWO HERNAN CODELCO-Chile, Division Chuquicamata, Chuquicamata, Chile VERONICA MORENO & ANA MARIA BARON San Pedro de Atacama, Chile Abstract Results are reported from a study of inhabitants of Atacameno settlements in northern Chile, who consume water with naturally high arsenic (As) concentrations. Of the 3000 inhabitants residing in the Atacameno zone, 761 participated voluntarily in the study. The clinical study revealed that the only sign of chronic arsenic poisoning of the exposed population was the presence of leukomelanodermic plaques in varying degrees, with a clear exposure-response relationship between arsenic concentration in drinking water and frequency of this dermal lesion. The urine of the exposed populations contained arsenic concentra tions higher than the normal reference value recommended by WHO for non-occupationally exposed populations. The paucity of observed health effects may be explained by the difference in Atacameno susceptibility to arsenic due to increased detoxification by methylation, which may be influenced by genetic or dietary and other lifestyle factors. INTRODUCTION In northern Chile, in the zone between 17°S and 26°S, 67°E and the Pacific Ocean, water supplies are naturally contaminated with arsenic due to the chemical process of solubilization of volcanic geological material (Enriquez, 1978).