The study was conducted to determine if aquatic insect production was significantly different between high and low alkalinity mountain streams and if any differences were associated with food availability factors. The major objectives included determining: (1) if annual production differences occur between high and low alkalinity streams; (2) if processing rates of terrestrial detritus differs between high and low alkalinity streams; (3) if detrital processing rates are related to stream insect productivities; (4) if primary productivity varies between high and low alkalinity streams; (5) if toxic effects or micronutrient limitations exist in high or low alkalinity streams that could limit insect survivals. A high alkalinity stream was defined as one having over 150 milligrams per liter average total alkalinity. Six study sites on four high alkalinity streams were located in the Wasatch National Forest near Logan in northern Utah. Six study sites on four low alkalinity streams were located in the Shoshone National Forest near Yellowstone National Park in northern Wyoming. Sites from each region were shown to not differ significantly for all physical parameters tested. The mean annual production of 22 of the 29 invertebrate taxa analyzed were significantly higher in the high alkalinity streams, while 2 taxa were significantly more productive in the low alkalinity streams. The mean annual production of all taxa summed was significantly higher in the high alkalinity streams. All high alkalinity sites had significantly higher production than any low alkalinity site. Alder leaf packs left open to allow invertebrate activity had a significantly higher rate of weight loss in the high alkalinity stream. Alder leaf packs placed inside fine mesh bags to exclude invertebrate activity showed no significant differences in weight loss when the experiments were terminated. The patterns of weight loss for these mesh packs did differ between the two stream types. In the high alkalinity stream, the leaves had a early rapid weight loss phase followed by a period of reduced weight loss. In the low alkalinity stream, the leaves experienced little weight loss during the early phase of the study but lost weight rapidly during the latter phase. The survivorships of all taxa tested did not differ significantly between high and low alkalinity water. Estimates of detrital inputs based on drift measurements and standing crops of detritus collected with invertebrate samples showed no significant differences between regions. The following conclusions resulted from the study. The high alkalinity streams had a significantly much higher production of aquatic invertebrates than did the low alkalinity streams. The high alkalinity streams also had significantly higher standing crops of attached algae and faster processing of alder leaves. Algae and processed allochthonous detritus are two major food sources for many aquatic invertebrates. It is concluded that a major reason for the great difference in invertebrate production between the physically similar high and low alkalinity streams in this study was the availability difference of these two food sources. The insects in the high alkalinity streams had much more of both food types available to them so a much higher annal production of aquatic invertebrates was supported.

High bicarbonate (HCO3-) content and associated high pH of irrigation water is detrimental to plant growth. Sustain ableagricultural/horticultural production will increasingly have to rely on economically feasible and environmentally sound solutions to the problems associated with high levels of HCO3- in irrigation water. The ability of a mixed Glomus Tulasne & Tulasne species inoculum of arbuscular mycorrhizal fungi (AMF), Glomus ZAC-19 (containing Glomus albidum Walker & Rhodes, Glomus claroideum Schenck & Smith, and Glomus diaphanum Morton & Walker), to enhance plant tolerance to HCO3- was tested on the growth and nutrient uptake of Rosa multiflora Thunb. ex J. Murr. cv. Burr (rose). Arbuscular mycorrhizal colonized and non-inoculated (non-AMF) R. multiflora cv. Burr were treated with 0, 2.5, 5, and 10 mM HCO3-. Increasing HCO3- concentration and associated high pH reduced R. multiflora cv. Burr growth, nutrient uptake, and acid phosphatase activity (ACP), while increasing alkaline phosphatase activity (ALP). Inoculation with AMF enhanced plant tolerance to HCO3- as indicated by greater growth, nutrient uptake, leaf chlorophyll content, higher mycorrhizal inoculation effect (MIE), lower root iron reductase activity, and generally lower soluble and wall-bound ALP activity. While AMF colonization (arbuscules, vesicles, and hyphae formation) was reduced by increasing HCO3- concentration, colonization still occurred at high HCO3- concentration. At 2.5 mM HCO3-, AMF plant growth was comparable to plants at 0 mM HCO3-, further indicating the beneficial effect of AMF for alleviation of HCO3- plant stress.

No description available.

Diamond-like Carbon (DLC) film exhibits an extreme hardness, low friction coefficient, chemical stability, heat conductivity, and high resistance. Their properties lead to remarkable applications on industry. In the experiment, we use electrondeposition to deposit the DLC film on Si substrate. Different concentrations of electrolyte were used to deposit on the of silicon substrates with different roughness surface. KOH solution was used to etch and to get the different roughness on the surface of silicon substrates. the morphology of surface were observed by SEM and AFM. Composition and microstructure of the DLC film were characterized by the Raman spectroscopy and XPS, repectively. The optical properties of DLC film were investigated by the N&K analyzer. From the AFM results, the surface morphology observed by KOH etching on the surface of silicon substrates during etching time as 0¡B20¡B40¡B60 min, the surface roughness increased from 2.64 to 14.07 nm. Based on thevariation of surface roughness, the growth rate was observed more quicker than the non etch surface. Moreover, to deposit the DLC film on the alkalinity solution was better then acid solution. However, the ID/IG ratio and the sp2/sp3 ratio obtained from Raman and XPS increase with the roughness surface from 1.09 to 1.82 and 0.985 to 2.15, respectively. It is because that the microstructure of DLC film varies and exchange to graphitization. The mixed the ammonia water and ammonium acetate into acetic acid solution was used to deposit DLC film on Si surface, and film shows with lower ID/IG ratio. Additionally, as the amount of ammonium acetate was varied in the solution, the ID/IG ratio of the films observed as decrease from 1.2 to 0.93 with increasing amount of ammonium acetate 10g to 40g. It was due to the methyl radicals increase in the solution. Besides, we can find the optical band gap decreased with DLC films changing to graphitization.

High bicarbonate (HCO3-) content and associated high pH of irrigation water is detrimental to plant growth. Sustain ableagricultural/horticultural production will increasingly have to rely on economically feasible and environmentally sound solutions to the problems associated with high levels of HCO3- in irrigation water. The ability of a mixed Glomus Tulasne & Tulasne species inoculum of arbuscular mycorrhizal fungi (AMF), Glomus ZAC-19 (containing Glomus albidum Walker & Rhodes, Glomus claroideum Schenck & Smith, and Glomus diaphanum Morton & Walker), to enhance plant tolerance to HCO3- was tested on the growth and nutrient uptake of Rosa multiflora Thunb. ex J. Murr. cv. Burr (rose). Arbuscular mycorrhizal colonized and non-inoculated (non-AMF) R. multiflora cv. Burr were treated with 0, 2.5, 5, and 10 mM HCO3-. Increasing HCO3- concentration and associated high pH reduced R. multiflora cv. Burr growth, nutrient uptake, and acid phosphatase activity (ACP), while increasing alkaline phosphatase activity (ALP). Inoculation with AMF enhanced plant tolerance to HCO3- as indicated by greater growth, nutrient uptake, leaf chlorophyll content, higher mycorrhizal inoculation effect (MIE), lower root iron reductase activity, and generally lower soluble and wall-bound ALP activity. While AMF colonization (arbuscules, vesicles, and hyphae formation) was reduced by increasing HCO3- concentration, colonization still occurred at high HCO3- concentration. At 2.5 mM HCO3-, AMF plant growth was comparable to plants at 0 mM HCO3-, further indicating the beneficial effect of AMF for alleviation of HCO3- plant stress.

Mississippi River affects the carbon dynamics in the northern Gulf of Mexico (N-GoM) significantly. Hence, total alkalinity (TA) algorithms developed for major ocean basins produce inaccurate estimations for this region. A TA algorithm was developed, which addresses the local effects of coastal processes and complex spatial influences. In-situ data collected during numerous previous research cruises in the N-GoM were compiled and used to calculate the efficiency of an existing TA algorithm that uses Sea-Surface-Temperature (SST) and Sea-Surface-Salinity (SSS) as explanatory variables. To improve this algorithm, statistical analyses were performed to improve the coefficients and functional form of this algorithm. Then, chlorophyll-a (Chla) was included as an additional explanatory variable. Chla worked as a proxy for addressing the organic carbon pump’s pronounced effects on coastal waters. Finally, a Geographically Weighted Regression (GWR) algorithm was developed to address spatial non-stationarity, which apparently could not be addressed in the previously developed global algorithm.

Submitted by (edna.saturno@ufrpe.br) on 2017-02-07T11:34:15Z No. of bitstreams: 1 Alexandre Duarte Rodrigues da Silva.pdf: 439100 bytes, checksum: 1b2fd1350f22fda3959acac92bbccf28 (MD5) / Made available in DSpace on 2017-02-07T11:34:15Z (GMT). No. of bitstreams: 1 Alexandre Duarte Rodrigues da Silva.pdf: 439100 bytes, checksum: 1b2fd1350f22fda3959acac92bbccf28 (MD5) Previous issue date: 2010-06-14 / Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPq / Culture of Litopenaeus vannamei in freshwater (0.0 g L-1) and low alkalinity and hardness (<50 mg L-1 CaCO3) were performed during 2008 to 2009, with the aim of evaluating the influence of adding of lime, to maximize production indices of shrimp. Post-larvae of this species, with 10 to 12 days (PL10-12), were initially acclimated to fresh water and then stored at density of 17 PL m-2, 12 experimental ponds of 60 m2. The concentrations of lime (4.0, 8.0, 12.0 and 16.0 t ha-1 cycle-1) were evaluated in the presence or absence of fertilizer-based K+ and Mg2+, in completely randomized. The diet was formed based pelleted feed, shrimp with 32% protein, and administered at feeders. The monitoring of physical and chemical qualities of water was carried out in different phases. After 60 days of cultivation,the best survival were observed in treatments of 8.0 and 12.0 t ha-1 without fertilizer, and application of 4.0 t ha-1 in crops with fertilizer. It was concluded that the use of lime favors the growth of L. vannamei in freshwater. / Cultivos do Litopenaeus vannamei, em água doce (0,0 g L-1) e com baixa alcalinidade e dureza (< 50 mg L-1 CaCO3) foram realizados no período de 2008 a 2009, com o objetivo de avaliar a influência da adição de calcário dolomítico, para maximizar os índices zootécnicos desses camarões. Pós-larvas dessa espécie, com 10 a 12 dias (PL10-12), foram inicialmente aclimatadas a água doce e, posteriormente, estocados a densidade de 17 PL m-2, em 12 viveiros experimentais de 60 m2. As concentrações de calcários (4,0, 8,0, 12,0 e 16,0 t ha-1 ciclo-1) foram avaliadas na presença ou não de fertilizantes a base de K+ e Mg2+, em experimentos inteiramente casualizados. A dieta foi constituída a base de ração peletizada,para camarão com 32% de proteína, e administrada em comedouros. O monitoramento das qualidades físicas e químicas da água foi realizado, nas diferentes fases experimentais. Após 60 dias de cultivo, as melhores sobrevivências foram observadas nos tratamentos de 8,0 e 12,0 t ha-1, sem fertilizante, e na aplicação de 4,0 t ha-1 em cultivos com fertilizante. Concluiu-se que a utilização do calcário dolomítico favorece o cultivo do L. vannamei em água doce.

Coastal zones receive massive terrestrial inputs of nutrients and organic matter, and play an important role in biogeochemical cycles. The interactions of river inputs, ocean currents, atmospheric exchanges, anthropogenic influences, and biologically active ecosystems make CO2 system studies in coastal waters highly challenging. This work focuses on improving our understanding of the CO2 system in coastal waters through (1) development of a new methodology for measurements of CO2 system parameters in the field; (2) observations of large spatial and temporal CO2 system variations in coastal waters; and (3) characterization of the influence of organics on CO2 system behavior in coastal waters. A novel portable light-emitting-diode (LED) photometer was developed to provide low-cost seawater pH measurements in the field. With meta cresol purple (mCP) as the indicator, the photometer produces pHT measurements within ± 0.01 units of state-of-the-art spectrophotometric measurements (7.6 ≤ pH ≤ 8.2, 30 ≤ S ≤ 36.2, and 15 oC ≤ t ≤ 30 oC). With a simple “do-it-yourself” (DIY) construction design, a hundredfold reduction in cost relative to benchtop spectrophotometric systems, and routine calibration-free operation in the field, the DIY photometer is an ideal replacement for pH test strips or consumer-level potentiometric probes. Applications of special interest include education, citizen science, coastal zone monitoring, and aquaculture and aquarium management. Subannual variability of total alkalinity (TA) distributions in the northeastern Gulf of Mexico (GOM) was examined through the use of TA data from ship-based water sampling, historical records of riverine TA, and contemporaneous model output of surface currents and salinity. Variability of TA observed in the upper 150 m of the GOM water column was primarily controlled by subannual variations in the extent of mixing between seawater and river water. A transition in TA distribution patterns between the river-dominated northern margin (near the Mississippi–Atchafalaya River System) and the ocean current-dominated eastern margin (West Florida Shelf) was observed. A riverine alkalinity input index was developed to highlight riverine TA contributions. Contributions of organic alkalinity (Org-Alk) to TA were investigated in coastal waters from three different environments (estuary, urban, mangrove) and offshore sites in the Gulf of Mexico. The difference in alkalinity (∆TA) between TA measured by direct titration (TAmeas) and calculated (TAcal) from observations of DIC and pH was used as an estimate of Org-Alk. Average values of ∆TA were 0.1 ± 5.0 µmol kg-1 at coastal sample sites outside the Mississippi-Atchafalaya River Estuary (n = 17), 1.9 ± 5.2 µmol kg-1 in offshore waters (n = 14) in the northern Gulf of Mexico, 33.6 ± 18.0 µmol kg-1 in the Suwannee River Estuary (n = 17), and 16.0 ± 25.4 µmol kg-1 in sites that included Tampa Bay, the Caloosahatchee River, and the Ten Thousand Islands area (n = 55). In addition to Org-Alk assessments based on measurements of ∆TA, a novel two-step spectophotometric titration method was developed for the characterization of Org-Alk. Direct titrations showed substantial Org-Alk in coastal samples (n = 5), and the Org-Alk values obtained from the two-step titrations showed good agreement with results from ∆TA calculations. The spectrophotometric titration data were used in model fits to evaluate the dissociation constants (pKi) of the natural organic acids. The pKi of the organic acids were within the previously reported range for riverine fulvic acids.

Résumé : La technologie des armatures en matériaux composites de polymères renforcés de fibre (PRF) reste relativement récente (moins de 20 ans) et souffre d’une moins bonne réputation en termes de durabilité, ce qui tend à freiner son acceptation par les professionnels du secteur. Les travaux présentés dans ce mémoire ont pour but d’étudier les effets de l’humidité et de l’alcalinité sur les performances mécaniques et thermomécaniques de barres d’armature en PRF. Si de nos jours l’évolution des propriétés des armatures de PRF a été largement étudiée par différents chercheurs, nous n’avons que peu d’informations sur les modes de dégradation qui entrainent ces pertes de performances. Le but des travaux entrepris dans ce mémoire est de trouver des pistes d’investigation pour la compréhension de ces mécanismes de dégradation qui pourraient éventuellement par la suite être reprises dans le cadre de travaux de thèse. Les travaux qui ont été entrepris s’articulent autour de deux projets. Le premier s’intéresse à l’étude du vieillissement accéléré de barres de polymère renforcé de fibres de verre (PRFV) de différents diamètres et soumis à un environnement humide. Le second s’intéresse à l’étude de barres de PRFV et de polymère renforcé de fibres de basalte (PRFB) de même diamètre soumis à un environnement alcalin qui simule le milieu interstitiel du béton. / Abstract : The FRP rebars technology remains relatively recent and suffers from a bad reputation in terms of durability which slows its acceptation among the professionals of the construction field. The aim of the work presented in this essay is to study the effects of moisture and alkalinity on the mechanical and thermo mechanical performances of FRP rebars. Nowadays, the progressions of FRP performances have been widely studied by different researchers but we still have few knowledge about the modes of degradation which lead to performance losses. The final goal of this work is to find investigation trails for the understanding of those degradation mechanisms which could possibly be taken over as part of a thesis work. The work is divided into two projects. The first one is the study of accelerated aging of glass fibers reinforced polymer (GFRP) rebars, of different diameters, conditioned in a moist environment. The second one concerns the behavior of GFRP and basalt fibers reinforced polymer (BFRP) rebars, of same diameter, conditioned in an alkaline environment which simulates the interstitial solution of concrete.

This thesis uses palaeolimnological records to reconstruct Holocene ontogeny trends from four lakes in south western Greenland. The research addresses four hypotheses investigating how Holocene lake ontogeny trends vary under different climatic settings, how long-term changes in ontogeny relate to periods of established climatic change in the region, the similarities between proxies within the lakes and between the lakes, and the role of vegetation in lake ontogeny. The study region occupies the widest ice-free area of south western Greenland and is characterised by a climatic gradient. The area inland and nearer to the ice-margin is arid, receives less precipitation and is warmer relative to the coastal areas. A paired lake approach, using lake records from two inland lakes and two coastal lakes, was adopted to examine the role of climatic setting upon lake development trajectories. Specifically, diatoms were used to reconstruct DI-alkalinity from the lakes using a DI-alkalinity model created from existing training sets in the region (WA Cla model, r2boot = 0.76, RMSEP = 0.28 log alkalinity units), sedimentary pigments to investigate trends in production and sedimentary parameters to reconstruct organic and minerogenic accumulation rates. All four lakes experienced comparable Holocene long-term ontogeny trajectories; maximum alkalinity in the first ~ 1000 cal. year BP of deglaciation followed by maximum production during the peak of Holocene Thermal Maximum (HTM) warming (~7000 -6000 cal. years BP). Following the HTM, all lakes demonstrated oligotrophication and a decline in pH. Vegetation development and catchment stabilisation at the end of the HTM may be important in determining the onset of oligotrophication in vegetated catchments. However, the impact of vegetation development on lake ontogeny cannot be isolated from the changes in the lakes associated with the colder and wetter climate which occurred at the end of the peak HTM warming. The timings of the large transitions in the ontogeny trajectories are comparable with established periods of Holocene climatic variability in the region; climate forcing drives ontogeny in these lakes. However, there are short-term differences between the lakes indicating that lakes have different thresholds of ecological change and may respond differently to the same climate forcing. It is concluded that ontogeny is driven by climate but lakes may respond differently to forcing depending on catchment specific characteristics which can filter out the climate signal or cause climate to influence the lake in a more direct way.