Reproducción de documentación perteneciente a Miguel José Garmendia Aldaz, Asesor Jurídico y Secretario Particular del Consejero de Gobernación del Gobierno Vasco durante la Guerra en el Norte, y Mayor Jefe de la Demarcación de Fronteras en Cataluña a partir de octubre de 1938, y en enero de 1939 Delegado de Orden Público adscrito a la Comandancia Militar de Figueras.

Fecha: 10-10-1936/31-1-1939 / Unidad de instalación: Carpeta 25 - Expediente 21 / Nº de pág.: 33 (28 mecanografiadas, 5 manuscritas)

Reproducción de Tarjetas de Visita remitidas por D. Sabino de Arana y Goiri a D. Estanislao de Aranzadi.

Fecha: 6-10-1898 (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-1 / Nº de pág.: 2 (manuscritas)

Reproducción del certificado extendido por el Consul Español en Hendaya a Carlos Solano.

Fecha: 20-4-1943 (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-3 / Nº de pág.: 1 (mecanografiada)

Reproducción de Tarjeta de visita de Eliodoro de la Torre.

Fecha: s.f. (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-5 / Nº de pág.: 1 (mecanografiada)

Reproducción de Esquela de la Misa de Requiem conmemorativa del 43º Aniversario del fallecimiento del Fundador del Nacionalismo Vasco, Sabino de Arana y Goiri.

Fecha: 25-11-1944 (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-6 / Nº de pág.: 1 (mecanografiada)

Reproducción del Modelo de Ficha del "Censo de los Vascos Refugiados en el Estado Francés".

Fecha: 1944 (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-7 / Nº de pág.: 1 (mecanografiada)

Reproducción de la carta remitida por el Subprefecto de Bayona a J. Gortazar.

Fecha: 22-12-1944 (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-8 / Nº de pág.: 1 (mecanografiada)

Study of the turbulence in the air-side and water-side boundary layers in experimental laboratory wind induced surface waves

This study detailed the structure of turbulence in the air-side and water-side boundary layers in wind-induced surface waves. Inside the air boundary layer, the kurtosis is always greater than 3 (the value for normal distribution) for both horizontal and vertical velocity fluctuations. The skewness for the horizontal velocity is negative, but the skewness for the vertical velocity is always positive. On the water side, the kurtosis is always greater than 3, and the skewness is slightly negative for the horizontal velocity and slightly positive for the vertical velocity. The statistics of the angle between the instantaneous vertical fluctuation and the instantaneous horizontal velocity in the air is similar to those obtained over solid walls. Measurements in water show a large variance, and the peak is biased towards negative angles. In the quadrant analysis, the contribution of quadrants Q2 and Q4 is dominant on both the air side and the water side. The non-dimensional relative contributions and the concentration match fairly well near the interface. Sweeps in the air side (belonging to quadrant Q4) act directly on the interface and exert pressure fluctuations, which, in addition to the tangential stress and form drag, lead to the growth of the waves. The water drops detached from the crest and accelerated by the wind can play a major role in transferring momentum and in enhancing the turbulence level in the water side.On the air side, the Reynolds stress tensor's principal axes are not collinear with the strain rate tensor, and show an angle α σ≈=-20°to-25°. On the water side, the angle is α σ≈=-40°to-45°. The ratio between the maximum and the minimum principal stresses is σ a/σ b=3to4 on the air side, and σ a/σ b=1.5to3 on the water side. In this respect, the air-side flow behaves like a classical boundary layer on a solid wall, while the water-side flow resembles a wake. The frequency of bursting on the water side increases significantly along the flow, which can be attributed to micro-breaking effects - expected to be more frequent at larger fetches. © 2012 Elsevier B.V.

Seulamurskaimen murskausominaisuuksien tutkiminen ja kehittäminen

Työn tavoitteena oli kehittää seulamurskaimen murskausprosessia selvittämällä murskaukseen vaikuttavia tekijöitä. Murskausprosessin sisäistämisen myötä voidaan saavuttaa parempi jaekoon hallinta, parantaa kapasiteettia sekä luoda tehokkaampia murskaussovelluksia. Murskausprosessia tutkittiin aluksi murskaukseen vaikuttavien teorioiden kautta. Teoriapohjaista tietoa ja murskaustapahtumaa tutkittiin käytännön testeillä, joissa testattiin seulamurskainta useilla eri materiaaleilla ja erilaisilla tuotevariaatioilla. Testeissä kerättiin näytteitä jaekoon jatkotutkimusta varten sekä saatujen tulosten pohjalta vertailtiin eri tuotevariaatioiden keskeisiä eroja. Saavutettuja tuloksia analysoitiin ja kehitettiin uusia potentiaalisia ratkaisuja seulamurskaimiin. Seulamurskaimen nykyinen rakenne on kehitetty ennen kaikkea seulontasovelluksiin ja sen toiminta perustuu rungon sisällä materiaalin pyörivään liikkeeseen. Murskausprosessissa on kuitenkin oleellista pyrkiä vähentämään sisäistä pyörintäliikettä, joka on hidasteena kappaleiden murskaukselle. Lisäksi seulamurskaimessa on useita rakenteita, jotka on kehitetty erityisesti seulontaa varten ja niiden uudenlaisella rakennesuunnittelulla voitaisiin saavuttaa huomattavasti parempia tuloksia murskauksen kannalta. Nämä tekijät kuitenkin vaativat huomattavan paljon tehoa, mikä puolestaan saattaa asettaa uusia haasteita suunnitteluun, sillä seulamurskaimessa käytettävissä oleva teho on varsin rajallinen.

La Asociación de Amistad Islamo-Cristiana de España.

Título anterior de la publicación : Boletín de la Comisión Española de la UNESCO

Jesús y Muhammad en el Año Internacional del Niño.

Título anterior de la publicación : Boletín de la Comisión Española de la UNESCO

Results from the CERN pilot CLOUD experiment

During a 4-week run in October–November 2006, a pilot experiment was performed at the CERN Proton Synchrotron in preparation for the Cosmics Leaving OUtdoor Droplets (CLOUD) experiment, whose aim is to study the possible influence of cosmic rays on clouds. The purpose of the pilot experiment was firstly to carry out exploratory measurements of the effect of ionising particle radiation on aerosol formation from trace H2SO4 vapour and secondly to provide technical input for the CLOUD design. A total of 44 nucleation bursts were produced and recorded, with formation rates of particles above the 3 nm detection threshold of between 0.1 and 100 cm−3 s−1, and growth rates between 2 and 37 nm h−1. The corresponding H2SO4 concentrations were typically around 106 cm−3 or less. The experimentally-measured formation rates and H2SO4 concentrations are comparable to those found in the atmosphere, supporting the idea that sulphuric acid is involved in the nucleation of atmospheric aerosols. However, sulphuric acid alone is not able to explain the observed rapid growth rates, which suggests the presence of additional trace vapours in the aerosol chamber, whose identity is unknown. By analysing the charged fraction, a few of the aerosol bursts appear to have a contribution from ion-induced nucleation and ion-ion recombination to form neutral clusters. Some indications were also found for the accelerator beam timing and intensity to influence the aerosol particle formation rate at the highest experimental SO2 concentrations of 6 ppb, although none was found at lower concentrations. Overall, the exploratory measurements provide suggestive evidence for ion-induced nucleation or ion-ion recombination as sources of aerosol particles. However in order to quantify the conditions under which ion processes become significant, improvements are needed in controlling the experimental variables and in the reproducibility of the experiments. Finally, concerning technical aspects, the most important lessons for the CLOUD design include the stringent requirement of internal cleanliness of the aerosol chamber, as well as maintenance of extremely stable temperatures (variations below 0.1 _C).