Planning for Emotional Labor and Secondary Traumatic Stress in Child Welfare Organizations

This analysis provides an emergent framework that emphasizes a neglected component of both direct practice with families and organizational development. Human emotions, both beneficial (positive emotional labor) and harmful (negative emotional labor), have received short shrift in leadership development, supervision, direct practice preparation and supports, and workforce stabilization, and professionalization. Significantly, a key indicator of negative emotional labor—secondary traumatic stress (STS)—often has been ignored and neglected, despite the fact that it may be endemic in the workforce. STS typically results from traumatic events in practice, but it also stems from workplace violence. Often undetected and untreated, STS is at least a hidden correlate and perhaps a probable cause of myriad problems such as questionable practice with families, life-work conflicts, undesirable workforce turnover, and a sub-optimal organizational climate. Special interventions are needed. At the same time, new organizational designs are needed to promote and reinforce positive emotional labor. Arguably, positive emotional labor and the positive organizational climates it facilitates are requisites for harmonious relations between jobs and personal lives, desirable workforce retention, and better outcomes for children and families. What’s more, specialized interventions for positive emotional labor constitute a key component in the prevention system for STS. A dual design for positive emotional labor and STS (and other negative emotional labor) prevention/intervention is provided herewith. Early detection and rapid response systems for STS, with social work leadership, receive special attention. Guidelines for new organizational designs for emotional labor in child welfare are offered in conclusion.

Genome -wide and locus -specific instability

The discovery of expanded simple repeated sequences causing or associated with human disease has lead to a new area of research involved in the elucidation of how the expanded repeat causes disease and how the repeat becomes unstable. ^ To study the genetic basis of the (CTG)n repeat instability in the DMPK gene in myotonic dystrophy (DM1) patients, somatic cell hybrids were constructed between the lymphocytes of DM1 patients and a variety of Chinese hamster ovary (CHO) cell DNA repair gene deficient mutants. By using small pool PCR (SP-PCR), the instability of the (CTG)n can be quantitated for both the frequency and sizes of length change mutations. ^ Additional SP-PCR analysis on 2/11 subclones generated from this original hybrid showed a marked increase in large repeat deletions, ∼50%. A bimodal distribution of repeats was seen around the progenitor allele and at a large deleted product (within the normal range) with no intermediate products present. ^ To determine if the repair capacity of the CHO cell led to a mutator phenotype in the hamster and hybrid clones, SP-PCR was also done on 3 hamster microsatellites in a variety of hamster cell backgrounds. No variant alleles were seen in over 2500 genome equivalents screened. ^ Human-hamster hybrids have long been shown to be chromosomally unstable, yet information about the stability of repeated sequences was not known. To test if repeat instability was associated with either intact or non-intact human chromosomes, more than 300 microsatellite repeats on 13 human chromosomes (intact and non-intact) were analyzed in eight hybrid cells. No variants were seen between the hybrid and patient alleles in the hybrids. ^ To identify whether DM1 patients have a previously undetected level of genome wide instability or if the instability is truly locus specific, SP-PCR was done on 6 human microsatellites within the patient used to make the hybrid cells. No variants were seen in over 1000 genomes screened. ^ These studies show that the somatic cell hybrid approach is a genetically stable system that allows for the determination of factors that could lead to changes in microsatellite instability. It also shows that there is something inherent about the DM1 expanded (CTG)n repeat that it is solely targeted by, as of yet, and unknown mechanism that causes the repeat to be unstable. (Abstract shortened by UMI.)^

Sarna del manzano : detección de la forma sexual (Venturia inaequalis ) en Mendoza (Argentina)

El aumento de los daños provocados por la sarna del manzano [Fusicladium dendritichum (Wallr.) Fuckl.] en montes frutales de Mendoza (Argentina), motivó estudios para aclarar la biología del hongo y buscar la presencia de la forma sexual, no detectada aún en la provincia. Al momento de la brotación se muestrearon hojas del año anterior que se encontraban en el suelo de dichos montes. En el laboratorio fueron observadas bajo estereomicroscopio. Los cuerpos negros inmersos en el tejido de la hoja fueron montados en preparados microscópicos y observados para establecer su identidad. Se confirmó la presencia en la zona de la forma teleomórfica del agente causal de la sarna del manzano. Este hecho tiene importancia en la epidemiología de la enfermedad y en las estrategias de control.

Chemistry of biogenic sediments from the equatorial Pacific

To increase our understanding of the mechanisms that control the distribution of Al and Ti within marine sediment, we performed sequential extractions targeting the chemical signatures of the loosely bound, exchangeable, carbonate, oxide, organic, opal, and residual fraction of sediment from a carbonate-dominated regime (equatorial Pacific) and from a mixed opal-terrigenous regime (West Antarctic Peninsula). We observe a systematic partitioning of Al and Ti between sediment phases that is related to bulk Al/Ti. We show that, where we can quantify an Al(excess) component, the dissolved Al is preferentially affiliated with the oxide fraction, resulting in Al/Ti molar ratios of 500-3000. This is interpreted as the result of surface complexation in the water column of dissolved Al onto oxyhydroxides. We also observe a previously undetected Ti(excess) with as much as 80% of the total Ti in the organic fraction, which is most likely a function of metal-organic colloidal removal from the water column. In samples where the excess metals are obscured by the detrital load, the Al and Ti are almost exclusively found in the residual phase. This argues for the paired removal of Al (preferentially by the oxide component) and Ti (preferentially by the organic component) from the water column by settling particulate matter. This research builds upon earlier work that shows changes in the bulk ratio of Al to Ti in carbonate sediment from the central-equatorial Pacific that coincide with changes in the sedimentary bulk accumulation rate (BAR). The ratios that are observed are as much as three times higher than typical shale values, and were interpreted as the result of scavenging of dissolved Al onto particles settling in the water column. Because this non-terrigenous Al(excess) accounts for up to 50% of the total sedimentary Al inventory and correlates best with BAR, the bulk Al/Ti may be a sensitive tracer of particle flux and, therefore, export production. Because we show that the excess metals are the result of scavenging processes, the bulk Al/Ti may be considered a sensitive proxy for this region.

Isotopic record across the Aptian/Albian boundary of ODP Hole 171-1049C

Geochemical analyses of extraordinarily well preserved late Aptian-early Albian foraminifera from Blake Nose (Ocean Drilling Program Site 1049) reveal rapid shifts of d18O, d13C, and 87Sr/88Sr in the subtropical North Atlantic that may be linked to a major planktic foraminifer extinction event across the Aptian/Albian boundary. The abruptness of the observed geochemical shifts and their coincidence with a sharp lithologic contact is explained as an artifact of a previously undetected hiatus of 0.8-1.4 million years at the boundary contact, but the values before and after the hiatus indicate that major oceanographic changes occurred at this time. 87Sr/88Sr increase by ~0.000200, d13C values decrease by 1.5 per mil to 2.2 per mil, and d18O values decrease by ~1.0 per mil (planktics) to 0.5 per mil (benthics) across the hiatus. Further, both 87Sr/88Sr ratios and d18O values during the Albian are anomalously high. The 87Sr/88Sr values deviate from known patterns to such a degree that an explanation requires either the presence of inter-basin differences in seawater 87Sr/88Sr during the Albian or revision of the seawater curve. For d18O, planktic values in some Aptian samples likely reflect a diagenetic overprint, but preservation is excellent in the rest of the section. In well preserved material, benthic foraminiferal values are largely between 0.5 and 0.0 per mil and planktic samples are largely between 0.0 per mil to -1.0 per mil, with a brief excursion to -2.0 per mil during OAE 1b. Using standard assumptions for Cretaceous isotopic paleotemperature calculations, the d18O values suggest bottom water temperatures (at ~1000 -1500 m) of 8-10°C and surface temperatures of 10-14°C, which are 4-6°C and 10-16°C cooler, respectively, than present-day conditions at the same latitude. The cool subtropical sea surface temperature estimates are especially problematic because other paleoclimate proxy data for the mid-Cretaceous and climate model predictions suggest that subtropical sea surface temperatures should have been the same as or warmer than at present. Because of their exquisite preservation, whole scale alteration of the analyzed foraminifera is an untenable explanation. Our proposed solution is a high evaporative fractionation factor in the early Albian North Atlantic that resulted in surface waters with higher d18O values at elevated salinities than commonly cited in Cretaceous studies. A high fractionation factor is consistent with high rates of vapor export and a vigorous hydrological cycle and, like the Sr isotopes, implies limited connectivity among the individual basins of the Early Cretaceous proto-Atlantic ocean.

Detection histories for eight species of Amazona parrots in Venezuela during the NeoMaps bird surveys in 2010

Documenting changes in distribution is necessary for understanding species' response to environmental changes, but data on species distributions are heterogeneous in accuracy and resolution. Combining different data sources and methodological approaches can fill gaps in knowledge about the dynamic processes driving changes in species-rich, but data-poor regions. We combined recent bird survey data from the Neotropical Biodiversity Mapping Initiative (NeoMaps) with historical distribution records to estimate potential changes in the distribution of eight species of Amazon parrots in Venezuela. Using environmental covariates and presence-only data from museum collections and the literature, we first used maximum likelihood to fit a species distribution model (SDM) estimating a historical maximum probability of occurrence for each species. We then used recent, NeoMaps survey data to build single-season occupancy models (OM) with the same environmental covariates, as well as with time- and effort-dependent detectability, resulting in estimates of the current probability of occurrence. We finally calculated the disagreement between predictions as a matrix of probability of change in the state of occurrence. Our results suggested negative changes for the only restricted, threatened species, Amazona barbadensis, which has been independently confirmed with field studies. Two of the three remaining widespread species that were detected, Amazona amazonica, Amazona ochrocephala, also had a high probability of negative changes in northern Venezuela, but results were not conclusive for Amazona farinosa. The four remaining species were undetected in recent field surveys; three of these were most probably absent from the survey locations (Amazona autumnalis, Amazona mercenaria and Amazona festiva), while a fourth (Amazona dufresniana) requires more intensive targeted sampling to estimate its current status. Our approach is unique in taking full advantage of available, but limited data, and in detecting a high probability of change even for rare and patchily-distributed species. However, it is presently limited to species meeting the strong assumptions required for maximum-likelihood estimation with presence-only data, including very high detectability and representative sampling of its historical distribution.

Distribution of Cycladophora davisiana davisiana in upper Pliocene and Pleistocene sediments of the North Atlantic and Labrador Sea

Upper Pliocene and Pleistocene abundance fluctuations of the radiolarian Cycladophora davisiana (Ehrenberg) davisiana (Petrushevskaya) are documented from North Atlantic (Site 609) and Labrador Sea (Site 646B) to provide the first long-term correlation of its abundance fluctuations to oxygen isotope stages 1-114. Also examined are temporal and regional fluctuations in abundances C. d. davisiana and the global dispersal routes of the species. The first occurrence of C. d. davisiana in the eastern North Atlantic Ocean (Site 609) occurred between 2.586 and 2.435 Ma (oxygen isotope stages 109.66-102.19). During the early Matuyama Chron, prior to oxygen isotope stage 63, C. d. davisiana abundances were less than 1% and never greater than 12%, while abundances of greater than 5% are found in stages 65.71-73, 74, and 83-84. The initial major abundance peak (35.7%) of C. d. davisiana was noted near the stage 63/62 boundary. Abundance peaks of greater than 15%, between oxygen isotope stages 35 and 63, are limited to stages 63.02, 58.07, 55.07-54.26, and 50.76-50.22. These represent the only such abundance peaks detected during the first c. 1.5 million years of the species within the North Atlantic. The character of C. d. davisiana abundance fluctuations in Site 609 changes after oxygen isotope stage 35; average abundances are greater (7.7% vs. 4.3%) and abundance maxima of more than 15% are more frequent. Many, but not all, peak abundances of C. d. davisiana occur in glacial stages (e.g., 8, 14, 18, 20, 26, 30, 34, 50, 54, and 58). Increased abundances of the species are also noted in weak interglacial stages (e.g., stages 3, 23, 39, and 41), and significant cool periods of robust interglacial periods (e.g., late stage 11). Sample spacing is adequate in some stages to note some rapid changes in abundance near stage transitions (e.g., stages 4/5, 25/26, 62/63). The sample density in Holes 609 and 611 and the upper portion of 646B is sufficient to detect a synchroneity of many abundance maxima and minima among sites. Some abundance peaks are undetected in one or more of the two holes, warranting further sampling to obtain a more accurate record of regional abundance fluctuations. Prior to stage 36, few ages of Hole 611 peaks are the same as those in the more precisely dated Hole 609. The highest abundances of C. d. davisiana were noted in Labrador Sea Hole 646B where the earliest known occurrence of the species is documented (3.08-2.99 Ma). C. d. davisiana is inferred to have evolved in the Labrador Sea (or Arctic), and migrated next through the Arctic into the North Pacific (2.62-2.64 Ma, stage 114) before migrating into the Norwegian Sea (2.63-2.53 Ma) and North Atlantic (2.59-2.44 Ma, stages 109-102). Additional migration of C. d. dauisiana into the southern South Atlantic (Site 704) occurred much later (2.06 Ma, stage 83).

Benthic foraminiferal biofacies and stable isotopic record of St. Stephens Quarry, Alabama

We integrate upper Eocene-lower Oligocene lithostratigraphic, magnetostratigraphic, biostratigraphic, stable isotopic, benthic foraminiferal faunal, downhole log, and sequence stratigraphic studies from the Alabama St. Stephens Quarry (SSQ) core hole, linking global ice volume, sea level, and temperature changes through the greenhouse to icehouse transition of the Cenozoic. We show that the SSQ succession is dissected by hiatuses associated with sequence boundaries. Three previously reported sequence boundaries are well dated here: North Twistwood Creek-Cocoa (35.4-35.9 Ma), Mint Spring-Red Bluff (33.0 Ma), and Bucatunna-Chickasawhay (the mid-Oligocene fall, ca. 30.2 Ma). In addition, we document three previously undetected or controversial sequences: mid-Pachuta (33.9-35.0 Ma), Shubuta-Bumpnose (lowermost Oligocene, ca. 33.6 Ma), and Byram-Glendon (30.5-31.7 Ma). An ~0.9 per mil d18O increase in the SSQ core hole is correlated to the global earliest Oligocene (Oi1) event using magnetobiostratigraphy; this increase is associated with the Shubuta-Bumpnose contact, an erosional surface, and a biofacies shift in the core hole, providing a first-order correlation between ice growth and a sequence boundary that indicates a sea-level fall. The d18O increase is associated with a eustatic fall of ~55 m, indicating that ~0.4 per mil of the increase at Oi1 time was due to temperature. Maximum d18O values of Oi1 occur above the sequence boundary, requiring that deposition resumed during the lowest eustatic lowstand. A precursor d18O increase of 0.5 per mil (33.8 Ma, midchron C13r) at SSQ correlates with a 0.5 per mil increase in the deep Pacific Ocean; the lack of evidence for a sea-level change with the precursor suggests that this was primarily a cooling event, not an ice-volume event. Eocene-Oligocene shelf water temperatures of ~17-19 °C at SSQ are similar to modern values for 100 m water depth in this region. Our study establishes the relationships among ice volume, d18O, and sequences: a latest Eocene cooling event was followed by an earliest Oligocene ice volume and cooling event that lowered sea level and formed a sequence boundary during the early stages of eustatic fall.

Age determination and model of sediment core RAPiD-15-4P

Greenland ice core records indicate that the last deglaciation (~7-21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C-10°C within decades. However, the cause behind many of these events is uncertain. A likely candidate may have been the input of deglacial meltwater, from the Laurentide ice sheet (LIS), to the high-latitude North Atlantic, which disrupted ocean circulation and triggered cooling. Yet the direct evidence of meltwater input for many of these events has so far remained undetected. In this study, we use the geochemistry (paired Mg/Ca-d18O) of planktonic foraminifera from a sediment core south of Iceland to reconstruct the input of freshwater to the northern North Atlantic during abrupt deglacial climate change. Our record can be placed on the same timescale as ice cores and therefore provides a direct comparison between the timing of freshwater input and climate variability. Meltwater events coincide with the onset of numerous cold intervals, including the Older Dryas (14.0 ka), two events during the Allerød (at ~13.1 and 13.6 ka), the Younger Dryas (12.9 ka), and the 8.2 ka event, supporting a causal link between these abrupt climate changes and meltwater input. During the Bølling-Allerød warm interval, we find that periods of warming are associated with an increased meltwater flux to the northern North Atlantic, which in turn induces abrupt cooling, a cessation in meltwater input, and eventual climate recovery. This implies that feedback between climate and meltwater input produced a highly variable climate. A comparison to published data sets suggests that this feedback likely included fluctuations in the southern margin of the LIS causing rerouting of LIS meltwater between southern and eastern drainage outlets, as proposed by Clark et al. (2001, doi:10.1126/science.1062517).

A robust procedure for damage detection from strain measurements based on principal component analysis

FBGs are excellent strain sensors, because of its low size and multiplexing capability. Tens to hundred of sensors may be embedded into a structure, as it has already been demonstrated. Nevertheless, they only afford strain measurements at local points, so unless the damage affects the strain readings in a distinguishable manner, damage will go undetected. This paper show the experimental results obtained on the wing of a UAV, instrumented with 32 FBGs, before and after small damages were introduced. The PCA algorithm was able to distinguish the damage cases, even for small cracks. Principal Component Analysis (PCA) is a technique of multivariable analysis to reduce a complex data set to a lower dimension and reveal some hidden patterns that underlie.

Caracterización de la necrosis sistémica inducida por la interacción sinérgica entre el Virus X de la patata y potyvirus en Nicotiana benthamiana

Los virus de plantas pueden causar enfermedades severas que conllevan serias pérdidas económicas a nivel mundial. Además, en la naturaleza son comunes las infecciones simultáneas con distintos virus que conducen a la exacerbación de los síntomas de enfermedad, fenómeno al que se conoce como sinergismo viral. Una de las sintomatologías más severas causadas por los virus en plantas susceptibles es la necrosis sistémica (NS), que incluso puede conducir a la muerte del huésped. Este fenotipo ha sido comparado en ocasiones con la respuesta de resistencia de tipo HR, permitiendo establecer una serie de paralelismos entre ambos tipos de respuesta que sugieren que la NS producida en interacciones compatibles sería el resultado de una respuesta hipersensible sistémica (SHR). Sin embargo, los mecanismos moleculares implicados en el desarrollo de la NS, su relación con procesos de defensa antiviral o su relevancia biológica aún no son bien entendidos, al igual que tampoco han sido estudiados los cambios producidos en la planta a escala genómica en infecciones múltiples que muestran sinergismo en patología. En esta tesis doctoral se han empleado distintas aproximaciones de análisis de expresión génica, junto con otras técnicas genéticas y bioquímicas, en el sistema modelo de Nicotiana benthamiana para estudiar la NS producida por la infección sinérgica entre el Virus X de la patata (PVX) y diversos potyvirus. Se han comparado los cambios producidos en el huésped a nivel genómico y fisiológico entre la infección doble con PVX y el Virus Y de la patata (PVY), y las infecciones simples con PVX o PVY. Además, los cambios transcriptómicos y hormonales asociados a la infección con la quimera viral PVX/HC‐Pro, que reproduce los síntomas del sinergismo entre PVX‐potyvirus, se han comparado con aquellos producidos por otros dos tipos de muerte celular, la PCD ligada a una interacción incompatible y la PCD producida por la disfunción del proteasoma. Por último, técnicas de genética reversa han permitido conocer la implicación de factores del huésped, como las oxilipinas, en el desarrollo de la NS asociada al sinergismo entre PVXpotyvirus. Los resultados revelan que, respecto a las infecciones con solo uno de los virus, la infección doble con PVX‐PVY produce en el huésped diferencias cualitativas además de cuantitativas en el perfil transcriptómico relacionado con el metabolismo primario. Otros cambios en la expresión génica, que reflejan la activación de mecanismos de defensa, correlacionan con un fuerte estrés oxidativo en las plantas doblemente infectadas que no se detecta en las infecciones simples. Además, medidas en la acumulación de determinados miRNAs implicados en diversos procesos celulares muestran como la infección doble altera de manera diferencial tanto la acumulación de estos miRNAs como su funcionalidad, lo cual podría estar relacionado con los cambios en el transcriptoma, así como con la sintomatología de la infección. La comparación a nivel transcriptómico y hormonal entre la NS producida por PVX/HC‐Pro y la interacción incompatible del Virus del mosaico del tabaco en plantas que expresan el gen N de resistencia (SHR), muestra que la respuesta en la interacción compatible es similar a la que se produce durante la SHR, si bien se presenta de manera retardada en el tiempo. Sin embargo, los perfiles de expresión de genes de defensa y de respuesta a hormonas, así como la acumulación relativa de ácido salicílico (SA), ácido jasmonico (JA) y ácido abscísico, en la interacción compatible son más semejantes a la respuesta PCD producida por la disfunción del proteasoma que a la interacción incompatible. Estos datos sugieren una contribución de la interferencia sobre la funcionalidad del proteasoma en el incremento de la patogenicidad, observado en el sinergismo PVX‐potyvirus. Por último, los resultados obtenidos al disminuir la expresión de 9‐LOX, α‐DOX1 y COI1, relacionados con la síntesis o con la señalización de oxilipinas, y mediante la aplicación exógena de JA y SA, muestran la implicación del metabolismo de las oxilipinas en el desarrollo de la NS producida por la infección sinérgica entre PVXpotyvirus en N. benthamiana. Además, estos resultados indican que la PCD asociada a esta infección, al igual que ocurre en interacciones incompatibles, no contiene necesariamente la acumulación viral, lo cual indica que necrosis e inhibición de la multiplicación viral son procesos independientes. ABSTRACT Plant viruses cause severe diseases that lead to serious economic losses worldwide. Moreover, simultaneous infections with several viruses are common in nature leading to exacerbation of the disease symptoms. This phenomenon is known as viral synergism. Systemic necrosis (SN) is one of the most severe symptoms caused by plant viruses in susceptible plants, even leading to death of the host. This phenotype has been compared with the hypersensitive response (HR) displayed by resistant plants, and some parallelisms have been found between both responses, which suggest that SN induced by compatible interactions could be the result of a systemic hypersensitive response (SHR). However, the molecular mechanisms involved in the development of SN, its relationship with antiviral defence processes and its biological relevance are still unknown. Furthermore, the changes produced in plants by mixed infections that cause synergistic pathological effects have not been studied in a genome‐wide scale. In this doctoral thesis different approaches have been used to analyse gene expression, together with other genetic and biochemical techniques, in the model plant Nicotiana benthamiana, in order to study the SN produced by the synergistic infection of Potato virus X (PVX) with several potyviruses. Genomic and physiological changes produced in the host by double infection with PVX and Potato virus Y (PVY), and by single infection with PVX or PVY have been compared. In addition, transcriptional and hormonal changes associated with infection by the chimeric virus PVX/HC‐Pro, which produces synergistic symptoms similar to those caused by PVX‐potyvirus, have been compared with those produced by other types of cell death. These types of cell death are: PCD associated with an incompatible interaction, and PCD produced by proteasome disruption. Finally, reverse genetic techniques have revealed the involvement of host factors, such as oxylipins, in the development of SN associated with PVX‐potyvirus synergism. The results revealed that compared with single infections, double infection with PVX‐PVY produced qualitative and quantitative differences in the transcriptome profile, mainly related to primary metabolism. Other changes in gene expression, which reflected the activation of defence mechanisms, correlated with a severe oxidative stress in doubly infected plants that was undetected in single infections. Additionally, accumulation levels of several miRNAs involved in different cellular processes were measured, and the results showed that double infection not only produced the greatest variations in miRNA accumulation levels but also in miRNA functionality. These variations could be related with transcriptomic changes and the symptomatology of the infection. Transcriptome and hormone level comparisons between SN induced by PVX/HCPro and the incompatible interaction produced by Tobacco mosaic virus in plants expressing the N resistance gene (SHR), showed some similarities between both responses, even though the compatible interaction appeared retarded in time. Nevertheless, the expression profiles of both defence‐related genes and hormoneresponsive genes, as well as the relative accumulation of salicylic acid (SA), jasmonic acid (JA) and abscisic acid in the compatible interaction are more similar to the PCD response produced by proteasome disruption. These data suggest that interference with proteasome functionality contributes to the increase in pathogenicity associated with PVX‐potyvirus synergism. Finally, the results obtained by reducing the expression of 9‐LOX, α‐DOX1 and COI1, related with synthesis or signalling of oxylipins, and by applying exogenously JA and SA, revealed that oxylipin metabolism is involved in the development of SN induced by PVX‐potyvirus synergistic infections in N. benthamiana. Moreover, these results also indicated that PVX‐potyvirus associated PCD does not necessarily restrict viral accumulation, as is also the case in incompatible interactions. This indicates that both necrosis and inhibition of viral multiplication are independent processes.

Automatic fault detection on BIPV systems without solar irradiation data

BIPV systems are small PV generation units spread out over the territory, and whose characteristics are very diverse. This makes difficult a cost-effective procedure for monitoring, fault detection, performance analyses, operation and maintenance. As a result, many problems affecting BIPV systems go undetected. In order to carry out effective automatic fault detection procedures, we need a performance indicator that is reliable and that can be applied on many PV systems at a very low cost. The existing approaches for analyzing the performance of PV systems are often based on the Performance Ratio (PR), whose accuracy depends on good solar irradiation data, which in turn can be very difficult to obtain or cost-prohibitive for the BIPV owner. We present an alternative fault detection procedure based on a performance indicator that can be constructed on the sole basis of the energy production data measured at the BIPV systems. This procedure does not require the input of operating conditions data, such as solar irradiation, air temperature, or wind speed. The performance indicator, called Performance to Peers (P2P), is constructed from spatial and temporal correlations between the energy output of neighboring and similar PV systems. This method was developed from the analysis of the energy production data of approximately 10,000 BIPV systems located in Europe. The results of our procedure are illustrated on the hourly, daily and monthly data monitored during one year at one BIPV system located in the South of Belgium. Our results confirm that it is possible to carry out automatic fault detection procedures without solar irradiation data. P2P proves to be more stable than PR most of the time, and thus constitutes a more reliable performance indicator for fault detection procedures. We also discuss the main limitations of this novel methodology, and we suggest several future lines of research that seem promising to improve on these procedures.

Epitopes close to the apolipoprotein B low density lipoprotein receptor-binding site are modified by advanced glycation end products

Advanced glycation end products (AGEs) are thought to contribute to the abnormal lipoprotein profiles and increased risk of cardiovascular disease of patients with diabetes and renal failure, in part by preventing apolipoprotein B (apoB)-mediated cellular uptake of low density lipoproteins (LDL) by LDL receptors (LDLr). It has been proposed that AGE modification at one site in apoB, almost 1,800 residues from the putative apoB LDLr-binding domain, may be sufficient to induce an apoB conformational change that prevents binding to the LDLr. To further explore this hypothesis, we used 29 anti-human apoB mAbs to identify other potential sites on apoB that may be modified by in vitro advanced glycation of LDL. Glycation of LDL caused a time-dependent decrease in its ability to bind to the LDLr and in the immunoreactivity of six distinct apoB epitopes, including two that flank the apoB LDLr-binding domain. ApoB appears to be modified at multiple sites by these criteria, as the loss of glycation-sensitive epitopes was detected on both native glycated LDL and denatured, delipidated glycated apoB. Moreover, residues directly within the putative apoB LDLr-binding site are not apparently modified in glycated LDL. We propose that the inability of LDL modified by AGEs to bind to the LDLr is caused by modification of residues adjacent to the putative LDLr-binding site that were undetected by previous immunochemical studies. AGE modification either eliminates the direct participation of the residues in LDLr binding or indirectly alters the conformation of the apoB LDLr-binding site.

Blind separation of auditory event-related brain responses into independent components

Averaged event-related potential (ERP) data recorded from the human scalp reveal electroencephalographic (EEG) activity that is reliably time-locked and phase-locked to experimental events. We report here the application of a method based on information theory that decomposes one or more ERPs recorded at multiple scalp sensors into a sum of components with fixed scalp distributions and sparsely activated, maximally independent time courses. Independent component analysis (ICA) decomposes ERP data into a number of components equal to the number of sensors. The derived components have distinct but not necessarily orthogonal scalp projections. Unlike dipole-fitting methods, the algorithm does not model the locations of their generators in the head. Unlike methods that remove second-order correlations, such as principal component analysis (PCA), ICA also minimizes higher-order dependencies. Applied to detected—and undetected—target ERPs from an auditory vigilance experiment, the algorithm derived ten components that decomposed each of the major response peaks into one or more ICA components with relatively simple scalp distributions. Three of these components were active only when the subject detected the targets, three other components only when the target went undetected, and one in both cases. Three additional components accounted for the steady-state brain response to a 39-Hz background click train. Major features of the decomposition proved robust across sessions and changes in sensor number and placement. This method of ERP analysis can be used to compare responses from multiple stimuli, task conditions, and subject states.

Interaction of the β sliding clamp with MutS, ligase, and DNA polymerase I

The β and proliferating cell nuclear antigen (PCNA) sliding clamps were first identified as components of their respective replicases, and thus were assigned a role in chromosome replication. Further studies have shown that the eukaryotic clamp, PCNA, interacts with several other proteins that are involved in excision repair, mismatch repair, cellular regulation, and DNA processing, indicating a much wider role than replication alone. Indeed, the Escherichia coli β clamp is known to function with DNA polymerases II and V, indicating that β also interacts with more than just the chromosomal replicase, DNA polymerase III. This report demonstrates three previously undetected protein–protein interactions with the β clamp. Thus, β interacts with MutS, DNA ligase, and DNA polymerase I. Given the diverse use of these proteins in repair and other DNA transactions, this expanded list of β interactive proteins suggests that the prokaryotic β ring participates in a wide variety of reactions beyond its role in chromosomal replication.