Yellow laser light generation by frequency doubling of the output from a master oscillator fiber power amplifier system

We present a power-scalable approach for yellow laser-light generation based on standard Ytterbium (Yb) doped fibers. To force the cavity to lase at 1154 nm, far above the gain-maximum, measures must be taken to fulfill lasing condition and to suppress competing amplified spontaneous emission (ASE) in the high-gain region. To prove the principle we built a fiber-laser cavity and a fiber-amplifier both at 1154 nm. In between cavity and amplifier we suppressed the ASE by 70 dB using a fiber Bragg grating (FBG) based filter. Finally we demonstrated efficient single pass frequency doubling to 577 nm with a periodically poled lithium niobate crystal (PPLN). With our linearly polarized 1154 nm master oscillator power fiber amplifier (MOFA) system we achieved slope efficiencies of more than 15 % inside the cavity and 24 % with the fiber-amplifier. The frequency doubling followed the predicted optimal efficiency achievable with a PPLN crystal. So far we generated 1.5 W at 1154nm and 90 mW at 577 nm. Our MOFA approach for generation of 1154 nm laser radiation is power-scalable by using multi-stage amplifiers and large mode-area fibers and is therefore very promising for building a high power yellow laser-light source of several tens of Watt.

Geochemistry and sea-surface temperature reconstruction for sediment cores of the Iberian Margin

Biogenic records of the marine palaeoproductivity (carbonates, organic carbon, and C37 alkenones) and the molecular stratigraphy of past sea surface temperatures (SSTs; UK'37) were studied at high resolution in two cores of the Iberian Margin. The comparison of these records indicates that the oceanographic conditions switched abruptly during the past 160 kyr between three kinds of regimes. A first regime with high (17-22°C) SST and low productivity typifies the interglacial periods, marine isotopic stages (MIS) 5 and 1. Several periods during MIS 6, 2, and the terminations II and I are characterised by about 4-5°C colder SST and a higher organic matter accumulation, both of which define the second regime. This anticorrelation between SST and marine productivity suggests that these variations are related to the intensity of the coastal upwelling. By contrast with this upwelling behaviour, extremely low biological productivity and very cold SST (6-12°C) occurred during short phases of glacial MIS 6, 4, and 2, and as abrupt events (~1 kyr or less) during MIS 3. The three oceanographic regimes are consistent with micropalaeontological changes in the same cores based on foraminifera and diatoms. The general trend of these hydrologic changes follows the long-term glacial/interglacial cycle, but the millennium scale variability is clearly related to Heinrich events and Dansgaard-Oeschger cycles. Strengthening of the upwelling corresponds probably to an intensification of the subtropical atmospheric circulation over the North Atlantic which was influenced by the presence of continental ice sheets. However, extreme glacial conditions due to massive discharges of icebergs interrupted the upwelling. Interestingly, both terminations II and I coincided with strong but transient intensification of the upwelling.

Stable isotopes, Mg/Ca ratios and sea surface temperatures on foraminifera from sediment cores off equatorial Peru during the last ~17kyr

The complex deglacial to Holocene oceanographic development in the Gulf of Guayaquil (Eastern Equatorial Pacific) is reconstructed for sea surface and subsurface ocean levels from (isotope) geochemical proxies based on marine sediment cores. At sea surface, southern sourced Cold Coastal Water and tropical Equatorial Surface Water/Tropical Surface Water are intimately related. In particular since ~10 ka, independent sea surface temperature proxies capturing different seasons emphasize the growing seasonal contrast in the Gulf of Guayaquil, which is in contrast to ocean areas further offshore. Cold Coastal Water became rapidly present in the Gulf of Guayaquil during the austral winter season in line with the strengthening of the Southeast Trades, while coastal upwelling off Peru gradually intensified and expanded northward in response to a seasonally changing atmospheric circulation pattern affecting the core locations intensively since 4 ka BP. Equatorial Surface Water, instead, was displaced and Tropical Surface Water moved northward together with the Equatorial Front. At subsurface, the presence of Equatorial Under Current-sourced Equatorial Subsurface Water was continuously growing, prominently since ~10-8 ka B.P. During Heinrich Stadial 1 and large parts of the Bølling/Allerød, and similarly during short Holocene time intervals at ~5.1-4 ka B.P. and ~1.5-0.5 ka B.P., the admixture of Equatorial Subsurface Water was reduced in response to both short-term weakening of Equatorial Under Current strength from the northwest and emplacement by tropical Equatorial Surface Water, considerably warming the uppermost ocean layers.

Nitrogen isotope gradients off Peru and Ecuador related to upwelling, productivity, nutrient uptake and oxygen deficiency

We present new nitrogen isotope data from the water column and surface sediments for paleo-proxy validation collected along the Peruvian and Ecuadorian margins between 1°N and 18°S. Productivity proxies in the bulk sediment (organic carbon, total nitrogen, biogenic opal, C37 alkenone concentrations) and 15N/14N ratios were measured at more than 80 locations within and outside the present-day Peruvian oxygen minimum zone (OMZ). Microbial N-loss to N2 in subsurface waters under O2 deficient conditions leaves a characteristic 15N-enriched signal in underlying sediments. We find that phytoplankton nutrient uptake in surface waters within the high nutrient, low chlorophyll (HNLC) regions of the Peruvian upwelling system influences the sedimentary signal as well. How the d15Nsed signal is linked to these processes is studied by comparing core-top values to the 15N/14N of nitrate and nitrite (d15N[NOx]) in the upper 200 m of the water column. Between 1°N and 10°S, subsurface O2 is still high enough to suppress N-loss keeping d15NNOx values relatively low in the subsurface waters. However d15N[NOx] values increase toward the surface due to partial nitrate utilization in the photic zone in this HNLC portion of the system. d15N[sed] is consistently lower than the isotopic signature of upwelled [NO3]-, likely due to the corresponding production of 15N depleted organic matter. Between 10°S and 15°S, the current position of perennial upwelling cells, HNLC conditions are relaxed and biological production and near-surface phytoplankton uptake of upwelled [NO3]- are most intense. In addition, subsurface O2 concentration decreases to levels sufficient for N-loss by denitrification and/or anammox, resulting in elevated subsurface d15N[NOx] values in the source waters for coastal upwelling. Increasingly higher production southward is reflected by various productivity proxies in the sediments, while the north-south gradient towards stronger surface [NO3]- utilization and subsurface N-loss is reflected in the surface sediment 15N/14N ratios. South of 10°S, d15N[sed] is lower than maximum water column d15N[NOx] values most likely because only a portion of the upwelled water originates from the depths where highest d15N[NOx] values prevail. Though the enrichment of d15N[NOx] in the subsurface waters is unambiguously reflected in d15N[sed] values, the magnitude of d15N[sed] enrichment depends on both the depth of upwelled waters and high subsurface d15N[NOx] values produce by N-loss. Overall, the degree of N-loss influencing subsurface d15N[NOx] values, the depth origin of upwelled waters, and the degree of near-surface nitrate utilization under HNLC conditions should be considered for the interpretation of paleo d15N[sed] records from the Peruvian oxygen minimum zone.

Empleo de biomarcadores para la reconstrucción paleoclimática. El registro pleistoceno del Mar de Fuentillejo (Ciudad Real)

El registro sedimentario del lago volcánico conocido como maar de Fuentillejo (Centro de España) ofrece la oportunidad de determinar la evolución paleoambiental durante el Pleistoceno medio y superior de la parte Centro-Sur de la Península Ibérica, objetivo principal de esta Tesis Doctoral. Se ha recopilado información sobre otras reconstrucciones paleoambientales en maares de todo el mundo y estudios paleoclimáticos realizados en el registro de la turbera de Padul, relativamente próxima al maar de Fuentillejo. Con ello, se pudo realizar el estado del arte.A lo largo del sondeo continuo (142,25 m) perforado en la parte central del maar de Fuentillejo en el año 2002, se han tomando un total de 613 muestras a intervalos de 20 cm para el análisis de biomarcadores. Los biomarcadores se obtuvieron mediante un equipo de extracción acelerada de disolventes (Dionex ASE 200) y fueron analizados con un cromatógrafo de gases (HP 6890) con detector selectivo de masas (HP 5973). La datación de sedimentos del maar de Fuentillejo ha sido complicada debido a la ausencia de restos orgánicos terrestres. Se seleccionaron seis muestras de sedimento para intentar datar por el método de racemización de aminoácidos: los resultados obtenidos no fueron buenos. Finalmente, el modelo de edad-profundidad se ha llevado a cabo mediante paleomagnetismo, dataciones 14C y U/Th. En base a una interpolación lineal de las edades medias calibradas se ha datado la base del registro en aproximadamente 355 ka. Se han identificado y cuantificado los n-alcanos, n-metil cetonas, ácidos n- alcanoicos y azufre orgánico del sedimento a lo largo del registro. La interpretación de los diferentes índices establecidos a partir de éstos permite independizar tres Unidades Geoquímicas generales (UG) y nueve Subunidades (S) que definen condiciones paleoambientales distintas (predominio en el aporte de vegetación terrestre/de macrofitas/acuática, lámina de agua más alta vs. más baja, periodos más húmedos vs. más secos).A partir de análisis estadísticos de los índices de n-alcanos (matriz de correlación y análisis de agrupaciones) se han definido tres asociaciones: Grupo 1 (condiciones ambientales más húmedas y fase con lámina de agua elevada), Grupo 2 (con condiciones intermedias) y Grupo 3 (las fases más secas y con lámina de agua más baja). Además, se establece un Indicador Paleoambiental (I.P.) que muestra variaciones notables correlacionables con escenarios paleoambientales distintos (más húmedos vs. más secos) distinguiendo veintiséis Episodios (E): cinco Secos, nueve Húmedos y doce Intermedios.En general, se encuentra una buena correspondencia entre estos Episodios (E) y los eventos paleoclimáticos cortos descritos por Vegas et al. (2010) en este registro, en base a la palinología y geoquímica, así como los Episodios del Oxígeno Marino (MIS) y Eventos Heinrich, que permiten suponer que las oscilaciones paleoclimatológicas registradas en el maar tienen un origen global. Esta correspondencia se confirma por el análisis espectral, que revela que los ciclos interpretados (103, 41, 26 y 23 ka) evidencian influencia orbital. Además, se ha realizado una correlación tentativa entre los episodios paleoambientales de larga duración obtenidos a partir del perfil suavizado del porcentaje relativo de C27 de la Cuenca de Padul (Granada, Sur de la Península Ibérica) y el perfil I.P. suavizado del maar de Fuentillejo, aunque hay diferencias que podrían ser explicadas por la vecindad de Padul a la zona de nieves perpetuas de Sierra Nevada lo que origina marcadas diferencias hidrológicas entre ambos sitios. El análisis por cadenas de Markov ha permitido determinar que los cambios paleoambientales reflejados por los biomarcadores no fueron, en la mayoría de los casos, bruscos pasando, normalmente, por estados transicionales.

Assessing user bias in affect detection within context-based spoken dialog systems

This paper presents an empirical evidence of user bias within a laboratory-oriented evaluation of a Spoken Dialog System. Specifically, we addressed user bias in their satisfaction judgements. We question the reliability of this data for modeling user emotion, focusing on contentment and frustration in a spoken dialog system. This bias is detected through machine learning experiments that were conducted on two datasets, users and annotators, which were then compared in order to assess the reliability of these datasets. The target used was the satisfaction rating and the predictors were conversational/dialog features. Our results indicated that standard classifiers were significantly more successful in discriminating frustration and contentment and the intensities of these emotions (reflected by user satisfaction ratings) from annotator data than from user data. Indirectly, the results showed that conversational features are reliable predictors of the two abovementioned emotions.

Electrificación rural fotovoltaica "Solar Home Systems". Fiabilidad y costes de mantenimiento

La electrificación rural fotovoltaica ha experimentado últimamente un salto de escala tanto en la dimensión de sus programas como en sus sistemas de gestión. Garantizar la calidad técnica ya no se reduce solamente a la fase de dise~o e instalación, sino también a la de operación y mantenimiento. El estudio del Instituto de Energfa Solar de la Universidad Politécnica de Madrid trata de caracterizar la fase de ope ración del programa de electrificación rural fotovoltaico de Marruecos sobre el cual se ha llevado a cabo un exhaustivo estudio de fiabilidad de los distintos componentes que integran los denominados Solar Heme 5ysrems (SHS). Ase como una evaluación de los costes unitarios ligados al mantenimiento, analizando su impacto en la estructura general de costes del programa. Los resultados van dirigidos hacia la caracterización de un modelo de la estructura de mantenimiento que logre asegurar la sostenibilidad de este tipo de programas energéticos.

Pulse-Shape Analysis of PDM-QPSK Modulation Formats for 100 and 200 Gb/s DWDM transmissions

Advanced optical modulation format polarization-division multiplexed quadrature phase shift keying (PDM-QPSK) has become a key ingredient in the design of 100 and 200-Gb/s dense wavelength-division multiplexed (DWDM) networks. The performance of this format varies according to the shape of the pulses employed by the optical carrier: non-return to zero (NRZ), return to zero (RZ) or carrier-suppressed return to zero (CSRZ). In this paper we analyze the tolerance of PDM-QPSK to linear and nonlinear optical impairments: amplified spontaneous emission (ASE) noise, crosstalk, distortion by optical filtering, chromatic dispersion (CD), polarization mode dispersion (PMD) and fiber Kerr nonlinearities. RZ formats with a low duty cycle value reduce pulse-to-pulse interaction obtaining a higher tolerance to CD, PMD and intrachannel nonlinearities.

Inorganic polyphosphate and the induction of rpoS expression

Inorganic polyphosphate [poly(P)] levels in Escherichia coli were reduced to barely detectable concentrations by expression of the plasmid-borne gene for a potent yeast exopolyphosphatase [poly(P)ase]. As a consequence, resistance to H2O2 was greatly diminished, particularly in katG (catalase HPI) mutants, implying a major role for the other catalase, the stationary-phase KatE (HPII), which is rpoS dependent. Resistance was restored to wild-type levels by complementation with plasmids expressing ppk, the gene for PPK [the polyphosphate kinase that generates poly(P)]. Induction of expression of both katE and rpoS (the stationary-phase σ factor) was prevented in cells in which the poly(P)ase was overproduced. Inasmuch as this inhibition by poly(P)ase did not affect the levels of the stringent-response guanosine nucleotides (pppGpp and ppGpp) and in view of the capacity of additional rpoS expression to suppress the poly(P)ase inhibition of katE expression, a role is proposed for poly(P) in inducing the expression of rpoS.

Targeted ablation of the 25-hydroxyvitamin D 1α-hydroxylase enzyme: Evidence for skeletal, reproductive, and immune dysfunction

The active form of vitamin D, 1α,25-dihydroxyvitamin D [1α,25(OH)2D], is synthesized from its precursor 25 hydroxyvitamin D [25(OH)D] via the catalytic action of the 25(OH)D-1α-hydroxylase [1α(OH)ase] enzyme. Many roles in cell growth and differentiation have been attributed to 1,25(OH)2D, including a central role in calcium homeostasis and skeletal metabolism. To investigate the in vivo functions of 1,25(OH)2D and the molecular basis of its actions, we developed a mouse model deficient in 1α(OH)ase by targeted ablation of the hormone-binding and heme-binding domains of the 1α(OH)ase gene. After weaning, mice developed hypocalcemia, secondary hyperparathyroidism, retarded growth, and the skeletal abnormalities characteristic of rickets. These abnormalities are similar to those described in humans with the genetic disorder vitamin D dependent rickets type I [VDDR-I; also known as pseudovitamin D-deficiency rickets (PDDR)]. Altered non-collagenous matrix protein expression and reduced numbers of osteoclasts were also observed in bone. Female mutant mice were infertile and exhibited uterine hypoplasia and absent corpora lutea. Furthermore, histologically enlarged lymph nodes in the vicinity of the thyroid gland and a reduction in CD4- and CD8-positive peripheral T lymphocytes were observed. Alopecia, reported in vitamin D receptor (VDR)-deficient mice and in humans with VDDR-II, was not seen. The findings establish a critical role for the 1α(OH)ase enzyme in mineral and skeletal homeostasis as well as in female reproduction and also point to an important role in regulating immune function.