Iowa County Precipitation Estimates, Departure from Normal 2008

Report produced by the The Department of Agriculture and Land Stewardship, Climatology Bureau.

Iowa County Precipitation Estimates, Departure from Normal 2008

Report produced by the The Department of Agriculture and Land Stewardship, Climatology Bureau.

Time constant of the cerebral arterial bed in normal subjects.

The time constant of cerebral arterial bed (in brief time constant) is a product of brain arterial compliance (C(a)) and resistance (CVR). We tested the hypothesis that in normal subjects, changes in end-tidal CO(2) (EtCO(2)) affect the value of the time constant. C(a) and CVR were estimated using mathematical transformations of arterial pressure (ABP) and transcranial Doppler (TCD) cerebral blood flow velocity waveforms. Responses of the time constant to controlled changes in EtCO(2) were compared in 34 young volunteers. Hypercapnia shortened the time constant (0.22 s [0.17, 0.26] vs. 0.16 s [0.13, 0.20]; p = 0.000001), while hypocapnia lengthened the time constant (0.22 s [0.17, 0.26] vs. 0.23 s [0.19, 0.32]; p < 0.0032). The time constant was negatively correlated with changes in EtCO(2) (R(partial) = -0.68, p < 0.000001). This was associated with a decrease in CVR when EtCO(2) increased (R(partial) = -0.80, p < 0.000001) and C(a) remained independent of changes in EtCO(2). C(a) was negatively correlated with mean ABP (R(partial) = -0.68, p < 0.000001). In summary, the time constant shortens with increasing EtCO(2). Its potential role in cerebrovascular investigations needs further studies.

A High-Resolution 2D/3D Seismic Study of a Thrust Fault Zone in Lake Geneva, Switzerland

P130 A HIGH-RESOLUTION 2D/3D SEISMIC STUDY OF A THRUST FAULT ZONE IN LAKE GENEVA SWITZERLAND M. SCHEIDHAUER M. BERES D. DUPUY and F. MARILLIER Institute of Geophysics University of Lausanne 1015 Lausanne, Switzerland Summary A high-resolution three-dimensional (3D) seismic reflection survey has been conducted in Lake Geneva near the city of Lausanne Switzerland where the faulted molasse basement (Tertiary sandstones) is overlain by complex Quaternary sedimentary structures. Using a single 48-channel streamer an area of 1200 m x 600 m was surveyed in 10 days. With a 5-m shot spacing and a receiver spacing of 2.5 m in the inline direction and 7.5 m in the crossline direction, a 12-fold data coverage was achieved. A maximum penetration depth of ~150 m was achieved with a 15 cu. in. water gun operated at 140 bars. The multi-channel data allow the determination of an accurate velocity field for 3D processing, and they show particularly clean images of the fault zone and the overlying sediments in horizontal and vertical sections. In order to compare different sources, inline 55 was repeated with a 30/30 and a 15/15 cu. in. double-chamber air gun (Mini GI) operated at 100 and 80 bars, respectively. A maximum penetration depth of ~450 m was achieved with this source.

Effets d'une perfusion de facteur natriurétique auriculaire humain chez des volontaires sains [Effects of perfusion of human atrial natriuretic factor in normal volunteers]

The renal and systemic effects of a synthetic atrial natriuretic peptide (ANP) corresponding to the sequence of the human hormone was investigated in normal volunteers. Each subject was infused for 4 hours on 3 different days at a one week interval with either ANP (0.5 or 1 microgram/min) or its vehicle. ANP enhanced natriuresis without simultaneously modifying glomerular filtration rate. ANP did, however, reduce effective renal plasma flow. In spite of the increased natriuresis, the activity of the renin-angiotensin-aldosterone system was reduced during ANP infusion. ANP induced a transient increase in skin blood flow. No change in blood pressure and heart rate occurred in the course of the experiment.

Immunohistochemical expression of endothelial markers CD31, CD34, von Willebrand Factor and Fli-1 in normal human tissues

Résumé du travail de thèse Introduction : Les différentes cellules endothéliales du lit vasculaire ont de nombreuses similitudes fonctionnelles et morphologiques. Cependant, elles présentent également une importante hétérogénéité structurelle et fonctionnelle qui peut avoir des implications notamment dans l'angiogenèse et le développement des maladies cardio-vasculaires. Peu d'études ont été publiées au sujet de l'expression et de la distribution des marqueurs endothéliaux dans les tissus humain normaux. Objectif : Nous avons étudié l'expression immunohistochimique des marqueurs endothéliaux CD31, CD34, vWF et Fli-1 dans les vaisseaux périphériques du rein, du poumon, de la rate, du foie, du cour et des gros vaisseaux ; incluant l'aorte, la veine cave inférieure, l'artère rénale ainsi que les artères et veines pulmonaires et fémorales. Matériel et méthodes : Les échantillons tissulaires ont été obtenus à partir de matériel d'autopsie et de biopsies. Le matériel a été fixé en formaline et inclus en paraffine. Les coupes de paraffine ont été colorées immunohistochimiquement avec CD31, CD34 et vWF. Les biopsies ont également été colorées immunohistochimiquement avec Fli-1, D2-40 et Lyve-1. Résultats : L'expression immunohistochimique de ces marqueurs est hétérogène dans les différents organes étudiés. Dans le rein, l'endothélium fenêtré des glomérules exprime fortement CD31 et CD34. Par contre, il n'exprime pas ou alors de manière faible et focale vWF. Dans le poumon, les capillaires alvéolaires expriment fortement CD31 et CD34 mais sont habituellement négatifs pour le vWF. L'expression de vWF augmente graduellement avec le calibre vasculaire dans le poumon. Les sinusoïdes de la rate expriment CD31 de manière diffuse mais ils n'expriment pas CD34. Les sinusoïdes du foie expriment CD31 de part et d'autre des lobules. Par contre, CD34 est exprimé seulement dans la région périportale. L'expression de Fli-1 dans les cellules endothéliales est ubiquitaire et ne varie pas suivant le type de vaisseau ou d'organe. Fli-1 est également exprimé dans d'autres types de cellules, essentiellement des lymphocytes. D2-40 est exprimé seulement dans l'endothélium des vaisseaux lymphatiques. L'expression de Lyve-1 dans ce matériel de routine était inconstante et non reproductible. Conclusion : Ces résultats indiquent que l'expression des marqueurs endothéliaux CD31, CD34 et vWF est hétérogène dans le lit vasculaire et qu'elle varie entre différents vaisseaux et différents compartiments anatomiques du même organe. D2-40 ne marque que les cellules endothéliales lymphatiques.

Adubação nitrogenada na cultura do milho no sistema plantio direto em ano com precipitação pluvial normal e com "El Niño"

O objetivo deste estudo foi avaliar a aplicação parcelada e antecipada de nitrogênio no milho no sistema plantio direto em sucessão à aveia preta, em dois regimes hídricos. Os tratamentos foram: (a) aplicação de 150 kg ha-1 de N em pré-semeadura e 30 kg ha-1 de N na semeadura, com aplicação de precipitações pluviais do "El Niño" de 1997/98; (b) aplicação da adubação nitrogenada, sendo 30 kg ha-1 de N na semeadura, 30 kg ha-1 de N aos 31 e 57 dias após a emergência (DAE), com aplicação do "El Niño"; (c) testemunha, sem nitrogênio e com aplicação do "El Niño", e (d) aplicação da adubação nitrogenada (tratamento b), com aplicação de precipitações pluviais normais. O experimento foi realizado no ano agrícola de 1998/99 na Universidade Federal de Santa Maria, no delineamento experimental inteiramente casualizado, com duas repetições. Utilizaram-se oito lisímetros de drenagem, que foram protegidos das precipitações pluviais naturais por meio de uma cobertura móvel. Determinaram-se a altura de plantas, o índice de área foliar (IAF), a massa seca da parte aérea, o rendimento de grãos, a percentagem de N e o N total na massa seca e nos grãos. A aplicação de N em ambos os regimes hídricos não influenciou o IAF, altura de plantas, rendimento de grãos, percentagem de N na massa de grãos e N total translocado para os grãos. A produção de massa seca de folhas e colmos e o N total translocado para estas partes da planta foram menores com a aplicação das precipitações pluviais consideradas normais, em relação aos tratamentos com adubação nitrogenada e "El Niño".

Role of high normal gamma-glutamyltransferase level in identifying heavy alcohol use in young men.

The objective of the current study was to determine the predictive value of high normal gamma-glutamyltransferase (GGT) level as an indication of heavy drinking in young men. In a sample of 577 men attending a one-day army recruitment process mandatory for all Swiss men at age 19 years, GGT level was evaluated as the dependent variable for each of eight dichotomous classifications of individuals on the basis of meeting cut-off criteria for five indexes of alcohol use, two indexes of alcohol-related problems, and one index of body mass. The sensitivity, specificity, and predictive values of GGT level in identifying subjects as either heavy drinkers or being overweight were determined. Compared with findings for their counterparts, GGT level was higher in subjects reporting consumption of more than 14 drinks per week (20.5 +/- 7.81 vs. 18.9 +/- 7.60, P <.05), in those reporting being drunk at least once during the past 30 days (20.3 +/- 7.80 vs. 18.3 +/- 7.43, P <.001), and in individuals with body mass indexes >or=25 kg/m(2) (25.8 +/- 10.84 vs. 18.3 +/- 6.59, P <.001). At a GGT level cut-off of 20 U/l, the sensitivity, specificity, and positive and negative predictive values of either being a heavy drinker or overweight were 48.2%, 70.2%, 67.7%, and 51.2%, respectively. Exclusion of subjects with body mass indexes of >or=25 kg/m(2) revealed similar results. High normal GGT level in young men is indicative of heavy alcohol use or being overweight; when present, subjects should be screened further for potential concomitant drinking problems.

A Dose-Response Strategy Reveals Differences between Normal-Weight and Obese Men in Their Metabolic and Inflammatory Responses to a High-Fat Meal.

A dose-response strategy may not only allow investigation of the impact of foods and nutrients on human health but may also reveal differences in the response of individuals to food ingestion based on their metabolic health status. In a randomized crossover study, we challenged 19 normal-weight (BMI: 20-25 kg/m(2)) and 18 obese (BMI: >30 kg/m(2)) men with 500, 1000, and 1500 kcal of a high-fat (HF) meal (60.5% energy from fat). Blood was taken at baseline and up to 6 h postprandially and analyzed for a range of metabolic, inflammatory, and hormonal variables, including plasma glucose, lipids, and C-reactive protein and serum insulin, glucagon-like peptide-1, interleukin-6 (IL-6), and endotoxin. Insulin was the only variable that could differentiate the postprandial response of normal-weight and obese participants at each of the 3 caloric doses. A significant response of the inflammatory marker IL-6 was only observed in the obese group after ingestion of the HF meal containing 1500 kcal [net incremental AUC (iAUC) = 22.9 ± 6.8 pg/mL × 6 h, P = 0.002]. Furthermore, the net iAUC for triglycerides significantly increased from the 1000 to the 1500 kcal meal in the obese group (5.0 ± 0.5 mmol/L × 6 h vs. 6.0 ± 0.5 mmol/L × 6 h; P = 0.015) but not in the normal-weight group (4.3 ± 0.5 mmol/L × 6 h vs. 4.8 ± 0.5 mmol/L × 6 h; P = 0.31). We propose that caloric dose-response studies may contribute to a better understanding of the metabolic impact of food on the human organism. This study was registered at clinicaltrials.gov as NCT01446068.

Al voltant del servei bibliotecari a zones rurals: tres oportunitats de canvi

Les autores del llibre Els serveis bibliotecaris en les zones rurals: una proposta d'actuació viable fan un breu repàs a les idees principals de la seva obra. Els elements que cal tenir en compte a l¿hora de dissenyar un servei que cobreixi les necessitats específiques del món rural són tres: l¿estructura del sistema de lectura pública, la facilitat d¿accés a la informació i les possibilitats que ofereixen les noves tecnologies. El paper dels bibliotecaris ha de ser el d'impulsors, dissenyadors i productors de serveis d'informació, formació i lectura.

Isolation and characterization of carcinoembryonic antigen (CEA) extracted from normal human colon mucosa.

Carcinoembryonic antigen (CEA) was identified in perchloric acid (PCA)_extract from normal colon mucosa by 2 immunological criteria: a line of identity in double diffusion and a parallel inhibition curve in radioimmunoassay (RIA), both with reference colon carcinoma-CEA (CEA-Tu). The average concentration of CEA in normal colon mucosa (CEA-No) was 35 times lower than in primary large bowel carcinomas and 230 times lower than in metastatic colon or rectum carcinomas. CEA-No was purified from PCA extracts of normal colon mucosa by Sephadex G-200 filtration and immunoadsorbent columns. Purified CEA-No had quatitatively the same inhibition activity in RIA as the British Standard CEA coded 73/601. Purified CEA-No was labelled with 125I. The percentage of binding of labelled CEA-No to a specific goat anti-CEA-Tu antiserum was similar to that of CEA-Tu. Labelled CEA-No could be used as radioactive tracer in RIA as well as labelled CEA-Tu. The physico-chemical properties of purified CEA-Tu as demonstrated by Sepharose 6 B filtration, SDS Polyacrylamide gel analysis and cesium chloride density gradient, were found to be almost identical to those of reference CEA-Tu. Preliminary results showed that CEA-No and CEA-Tu contained the same types of carbohydrates in similar proportions. A rabbit antiserum against CEA-No was obtained which demonstrated the same specificity as conventional anti-CEA-Tu antisera.

Rate and processes of river network rearrangement during incipient faulting: The case of the Cahabon river, Guatemala

Deeply incised river networks are generally regarded as robust features that are not easily modified by erosion or tectonics. Although the reorganization of deeply incised drainage systems has been documented, the corresponding importance with regard to the overall landscape evolution of mountain ranges and the factors that permit such reorganizations are poorly understood. To address this problem, we have explored the rapid drainage reorganization that affected the Cahabon River in Guatemala during the Quaternary. Sediment-provenance analysis, field mapping, and electrical resistivity tomography (ERT) imaging are used to reconstruct the geometry of the valley before the river was captured. Dating of the abandoned valley sediments by the Be-10-Al-26 burial method and geomagnetic polarity analysis allow us to determine the age of the capture events and then to quantify several processes, such as the rate of tectonic deformation of the paleovalley, the rate of propagation of post-capture drainage reversal, and the rate at which canyons that formed at the capture sites have propagated along the paleovalley. Transtensional faulting started 1 to 3 million years ago, produced ground tilting and ground faulting along the Cahabon River, and thus generated differential uplift rate of 0.3 +/- 0.1 up to 0.7 +/- 0.4 mm . y(-1) along the river's course. The river responded to faulting by incising the areas of relative uplift and depositing a few tens of meters of sediment above the areas of relative subsidence. Then, the river experienced two captures and one avulsion between 700 ky and 100 ky. The captures breached high-standing ridges that separate the Cahabon River from its captors. Captures occurred at specific points where ridges are made permeable by fault damage zones and/or soluble rocks. Groundwater flow from the Cahabon River down to its captors likely increased the erosive power of the captors thus promoting focused erosion of the ridges. Valley-fill formation and capture occurred in close temporal succession, suggesting a genetic link between the two. We suggest that the aquifers accumulated within the valley-fills, increased the head along the subterraneous system connecting the Cahabon River to its captors, and promoted their development. Upon capture, the breached valley experienced widespread drainage reversal toward the capture sites. We attribute the generalized reversal to combined effects of groundwater sapping in the valley-fill, axial drainage obstruction by lateral fans, and tectonic tilting. Drainage reversal increased the size of the captured areas by a factor of 4 to 6. At the capture sites, 500 m deep canyons have been incised into the bedrock and are propagating upstream at a rate of 3 to 11 mm . y(-1) deepening at a rate of 0.7 to 1 5 mm . y(-1). At this rate, 1 to 2 million years will be necessary for headward erosion to completely erase the topographic expression of the paleovalley. It is concluded that the rapid reorganization of this drainage system was made possible by the way the river adjusted to the new tectonic strain field, which involved transient sedimentation along the river's course. If the river had escaped its early reorganization and had been given the time necessary to reach a new dynamic equilibrium, then the transient conditions that promoted capture would have vanished and its vulnerability to capture would have been strongly reduced.

Localization and characterization of an active fault in an urbanized area in central Guatemala by means of geoelectrical imaging

The Polochic and Motagua faults define the active plate boundary between the North American and Caribbean plates in central Guatemala. A splay of the Polochic Fault traverses the rapidly growing city of San Miguel Uspantan that is periodically affected by destructive earthquakes. This fault splay was located using a 2D electrical resistivity tomography (ERT) survey that also characterized the fault damage zone and evaluated the thickness and nature of recent deposits upon which most of the city is built. ERT images show the fault as a similar to 50 m wide, near-vertical low-resistivity anomaly, bounded within a few meters by high resistivity anomalies. Forward modeling reproduces the key aspects of the observed electrical resistivity data with remarkable fidelity thus defining the overall location, geometry, and internal structure of the fault zone as well as the affected lithologies. Our results indicate that the city is constructed on a similar to 20 m thick surficial layer consisting of poorly consolidated, highly porous, water-logged pumice. This soft layer is likely to amplify seismic waves and to liquefy upon moderate to strong ground shaking. The electrical conductivity as well as the major element chemistry of the groundwater provides evidence to suggest that the local aquifer might, at least in part, be fed by water rising along the fault. Therefore, the potential threat posed by this fault splay may not be limited to its seismic activity per se, but could be compounded its potential propensity to enhance seismic site effects by injecting water into the soft surficial sediments. The results of this study provide the basis for a rigorous analysis of seismic hazard and sustainable development of San Miguel Uspantan and illustrate the potential of ERT surveying for paleoseismic studies.