Hydrochemical Atlas of the Arctic Ocean

Introduction: Chemical composition of water determines its physical properties and character of processes proceeding in it: freezing temperature, volume of evaporation, density, color, transparency, filtration capacity, etc. Presence of chemical elements in water solution confers waters special physical properties exerting significant influence on their circulation, creates necessary conditions for development and inhabitance of flora and fauna, and imparts to the ocean waters some chemical features that radically differ them from the land waters (Alekin & Liakhin, 1984). Hydrochemical information helps to determine elements of water circulation, convection depth, makes it easier to distinguish water masses and gives additional knowledge of climatic variability of ocean conditions. Hydrochemical information is a necessary part of biological research. Water chemical composition can be the governing characteristics determining possibility and limits of use of marine objects, both stationary and moving in sea water. Subject of investigation of hydrochemistry is study of dynamics of chemical composition, i.e. processes of its formation and hydrochemical conditions of water bodies (Alekin & Liakhin 1984). The hydrochemical processes in the Arctic Ocean are the least known. Some information on these processes can be obtained in odd publications. A generalizing study of hydrochemical conditions in the Arctic Ocean based on expeditions conducted in the years 1948-1975 has been carried out by Rusanov et al. (1979). The "Atlas of the World Ocean: the Arctic Ocean" contains a special section "Hydrochemistry" (Gorshkov, 1980). Typical vertical profiles, transects and maps for different depths - 0, 100, 300, 500, 1000, 2000, 3000 m are given in this section for the following parameters: dissolved oxygen, phosphate, silicate, pH and alkaline-chlorine coefficient. The maps were constructed using the data of expeditions conducted in the years 1948-1975. The illustrations reflect main features of distribution of the hydrochemical elements for multi-year period and represent a static image of hydrochemical conditions. Distribution of the hydrochemical elements on the ocean surface is given for two seasons - winter and summer, for the other depths are given mean annual fields. Aim of the present Atlas is description of hydrochemical conditions in the Arctic Ocean on the basis of a greater body of hydrochemical information for the years 1948-2000 and using the up-to-date methods of analysis and electronic forms of presentation of hydrochemical information. The most wide-spread characteristics determined in water samples were used as hydrochemical indices. They are: dissolved oxygen, phosphate, silicate, pH, total alkalinity, nitrite and nitrate. An important characteristics of water salt composition - "salinity" has been considered in the Oceanographic Atlas of the Arctic Ocean (1997, 1998). Presentation of the hydrochemical characteristics in this Hydrochemical Atlas is wider if compared with that of the former Atlas (Gorshkov, 1980). Maps of climatic distribution of the hydrochemical elements were constructed for all the standard depths, and seasonal variability of the hydrochemical parameters is given not only for the surface, but also for the underlying standard depths up to 400 m and including. Statistical characteristics of the hydrochemical elements are given for the first time. Detailed accuracy estimates of initial data and map construction are also given in the Atlas. Calculated values of mean-root deviations, maximum and minimum values of the parameters demonstrate limits of their variability for the analyzed period of observations. Therefore, not only investigations of chemical statics are summarized in the Atlas, but also some elements of chemical dynamics are demonstrated. Digital arrays of the hydrochemical elements obtained in nodes of a regular grid are the new form of characteristics presentation in the Atlas. It should be mentioned that the same grid and the same boxes were used in the Atlas, as those that had been used by creation of the US-Russian climatic Oceanographic Atlas. It allows to combine hydrochemical and oceanographic information of these Atlases. The first block of the digital arrays contains climatic characteristics calculated using direct observational data. These climatic characteristics were not calculated in the regions without observations, and the information arrays for these regions have gaps. The other block of climatic information in a gridded form was obtained with the help of objective analysis of observational data. Procedure of the objective analysis allowed us to obtain climatic estimates of the hydrochemical characteristics for the whole water area of the Arctic Ocean including the regions not covered by observations. Data of the objective analysis can be widely used, in particular, in hydrobiological investigations and in modeling of hydrochemical conditions of the Arctic Ocean. Array of initial measurements is a separate block. It includes all the available materials of hydrochemical observations in the form, as they were presented in different sources. While keeping in mind that this array contains some amount of perverted information, the authors of the Atlas assumed it necessary to store this information in its primary form. Methods of data quality control can be developed in future in the process of hydrochemical information accumulation. It can be supposed that attitude can vary in future to the data that were rejected according to the procedure accepted in the Atlas. The hydrochemical Atlas of the Arctic Ocean is the first specialized and electronic generalization of hydrochemical observations in the Arctic Ocean and finishes the program of joint efforts of Russian and US specialists in preparation of a number of atlases for the Arctic. The published Oceanographic Atlas (1997, 1998), Atlas of Arctic Meteorology and Climate (2000), Ice Atlas of the Arctic Ocean prepared for publication and Hydrochemical Atlas of the Arctic Ocean represent a united series of fundamental generalizations of empirical knowledge of Arctic Ocean nature at climatic level. The Hydrochemical Atlas of the Arctic Ocean was elaborated in the result of joint efforts of the SRC of the RF AARI and IARC. Dr. Ye. Nikiforov was scientific supervisor of the Atlas, Dr. R. Colony was manager on behalf of the USA and Dr. L. Timokhov - on behalf of Russia.

Estructuras de hormigón armado bajo carga dinámica severa. Parte I: Aspectos teóricos

En el ámbito de las estructuras de protección, tales como polvorines o refugios de protección civil, el hormigón armado es el material más empleado, fundamentalmente por su masividad, sus buenas características de absorción de energía y, cuando está adecuadamente reforzado, por su comportamiento dúctil. En ambos tipos de estructuras, la principal amenaza proviene de las explosiones causadas por armas de guerra, en particular, por armas convencionales. Por otro lado, en España viene actuando la organización terrorista ETA desde finales de los años 60, a lo que últimamente hay que añadir el denominado terrorismo internacional. En ambos casos, sus apariciones se manifiestan, generalmente, mediante la detonación de explosivos, aspecto que ha hecho que tanto entidades públicas como privadas hayan estado seriamente interesadas por el comportamiento de las estructuras cerramientos, etc. A título de ejemplo, se puede recordar el atentado perpetrado el día 31 de diciembre de 2008 en la sede de EITB de Bilbao, o el perpetrado el día 9 de febrero de 2009 en la sede de la empresa constructora Ferrovial-Agroman situada en el Campo de las Naciones de Madrid.

Los plásticos en el diseño de la maquinaria agrícola. Plásticos I: Qué son y para que se usan

El importante avance de los componentes de la maquinaria agrícola que se construyen con materiales ‘plásticos’ permite abrir una serie de cuatro artículos en los que se analizan de manera conceptual lo que pueden ofrecer los plásticos y algunas de las realizaciones sobre las máquinas que se encuentran en el mercado.

Demostración del sentido verdadero de las autoridades de que se vale el Doctor Don Juan Antonio de Llorente, canónigo de la Catedral de Toledo, en el tomo I de "Las noticias históricas de las tres provincias vascongadas" : y de lo que en verdad resulta de los historiadores que cita, con respecto solamente al Muy Noble y Muy Leal Señorío de Vizcaya / por Francisco de Aranguren y Sobrado.

Digitalización Vitoria-Gasteiz Archivos y Bibliotecas Abril 1994 18-6

Bauen I, la cabaña de Martin Heidegger

El espacio de lo doméstico se debate, como las casas de Heidegger en Todtnauberg (el refugio del pensador - 1922) y Friburgo (la casa del personaje publico - 1928), entre la construcción de la intimidad y la proyección hacia lo público.

Els plà nols de l’església nova i el plà nol geomètric de Santa Pola

La recerca històrica i geogràfi ca a vegades dóna resultats sorprenents. Aquest és el cas de la troballa del Proyecto de Iglesia Parroquial para el pueblo de Santa Pola, en què s’inclou, a més dels plànols originals de la coneguda com a «església rota» (l’actual mercat central), un «Plano Topográfi co de Santa Pola» de gran transcendència per a conéixer els inicis de l’evolució urbana de la localitat, tots signats per Francisco Morell y Gómez el 1863. Primer, tractem el projecte de l’església, analitzem les dades del projecte i els plànols. Després, el més interessant és el plànol topogràfi c inèdit esmentat. Fem una comparació amb el signat el 1863 pel també arquitecte José Ramon Mas y Font. Són iguals? Tenen diferències? Quines són i quina importància tenen? El plànol esdevé un instrument de recerca de primer ordre per a donar resposta a aquestes preguntes.

El plano geométrico de Crevillent: un pla urbanístic de sanejament i reforma interior de José Guardiola Picó el 1877

El present article analitza i situa en el context l’expedient urbanístic sobre la reforma interior del nucli urbà de Crevillent que l’ajuntament d’aquesta ciutat intentà dur a terme en l’últim quart del segle xix i que, en part, constitueix el plànol geomètric parcial d’aquesta vila. Es tracta d’un expedient municipal en què se succeeixen les actes del consistori per a la seua tramitació administrativa (entre 1876 i 1878) i en què s’intercala el projecte urbà de reforma interior, que consta de tres documents (memòria i dos planols: geomètric i de perfils), firmats el 12 de gener de 1877 per l’arquitecte José Guardiola y Picó (1836-1909), i que es tanca amb un plànol solt del 9 de gener de 1884 de firma no molt llegible.