Coastal outwelling of organic carbon from mangrove wetlands contributes to near-shore productivity and influences biogeochemical cycling of elements. I used a flume to measure fluxes of dissolved organic carbon (DOC) between a mangrove forest and adjacent tidal creek along Shark River, Florida. Shark River’s hydrology is influenced by diurnal tides and seasonal rainfall and wind patterns. Samplings were made over multiple tidal cycles in 2003 to include dry, wet, and transitional seasons. Surface water [DOC], temperature, salinity, conductivity and pH were significantly different among all sampling periods. [DOC] was highest during the dry season (May), followed by the wet (October) and transitional (December) seasons. Net DOC export was measured in October and December, inferring the mangrove forest is a source of DOC to the adjacent tidal creek during these periods. This trend may be explained by high rates of rainfall, freshwater inflow and subsequent flushing of wetland soils during this period of the year.

Marine aggregates are an important means of carbon transfers downwards to the deep ocean as well as an important nutritional source for benthic organism communities that are the ultimate recipients of the flux. During these last 10 years, data on size distribution of particulate matter have been collected in different oceanic provinces using an Underwater Video Profiler. The cruise data include simultaneous analyses of particle size distributions as well as additional physical and biological measurements of water properties through the water column. First, size distributions of large aggregates have been compared to simultaneous measurements of particle flux observed in sediment traps. We related sediment trap compositional data to particle size (d) distributions to estimate their vertical fluxes (F) using simple power relationships (F=Ad^b). The spatial resolution of sedimentation processes allowed by the use of in situ particle sizing instruments lead to a more detailed study of the role of physical processes in vertical flux. Second, evolution of the aggregate size distributions with depth was related to overlying primary production and phytoplankton size-distributions on a global scale. A new clustering technique was developed to partition the profiles of aggregate size distributions. Six clusters were isolated. Profiles with a high proportion of large aggregates were found in high-productivity waters while profiles with a high proportion of small aggregates were located in low-productivity waters. The aggregate size and mass flux in the mesopelagic layer were correlated to the nature of primary producers (micro-, nano-, picophytoplankton fractions) and to the amount of integrated chlorophyll a in the euphotic layer using a multiple regression technique on principal components. Finally, a mesoscale area in the North Atlantic Ocean was studied to emphasize the importance of the physical structure of the water column on the horizontal and vertical distribution of particulate matter. The seasonal change in the abundance of aggregates in the upper 1000 m was consistent with changes in the composition and intensity of the particulate flux recorded in sediment traps. In an area dominated by eddies, surface accumulation of aggregates and export down to 1000 m occured at mesoscale distances (<100 km).

A preliminary study shows that Submarine Groundwater Discharge (SGD) exists around Taiwan even though groundwater overdrawing is serious. Only five of the 20 sites studied did not record any SGD signal. Two nearly fresh SGD samples were obtained, providing strong and direct evidence for the existence of SGD in Taiwan. SGD is the submarine seepage of all fluids from coastal sediments into the overlying coastal areas. It has been well documented that SGD may contribute much nutrients to the coasts (Burnett et al.,2001, 2003; Church, 1996; Taniguchi et al., 2002; Zhang and Satake, 2002). Because of its difficulty in measurement, there are few reports on the characteristics of groundwater seepage, such as the flow rate and the water chemistry. In Taiwan, the only report was published in the Japanese journal Geochemistry (Chen et al. , 2005 ). In this study, samples were collected monthly from May, 2004 to June, 2006 at Xiziwan and Caishan in Kaohsiung. A flux chamber was also used in the observation of the SGD seepage rates. Further, samples were collected from 20 different places around Taiwan. The SGD collecting device, the SGD-Flux chamber and the Lee type seepage meter (Zhang et al., 2005) were used in this study, the latter being the first time used to explore the SGD flux in Taiwan. Salinity, dissolved oxygen saturation (%), nutrients (NO3, NO2, PO4, SiO2, NH3), total alkalinity, pH and major ions were analyzed. We averaged all seepage rate data at Xiziwan and Caishan to estimated the SGD seepage rate at about 1.32¡Ó1.57 L/m2/hr. The average concentrations of inorganic nitrogen (NO3+NO2+NH3), PO4 and SiO2 are, respectively, 48.6¡Ó86.3 (n=85), 0.78¡Ó1.26 (n=110) and 55.1¡Ó39.8

Rapport de stage DESS : Réseaux d'information et document électronique : Villeurbanne, ENSSIB : 2002.

Reproduction de : Thèse doctorat : Médecine. Immunologie et biologie parasitaire : Reims : 2005. / Titre provenant de l'écran-titre. Bibliogr. p.121-141.

Reproduction de : Thèse doctorat : Médecine. Biologie cellualire : Reims : 2006. / Titre provenant de l'écran-titre. Bibliogr. p.163-218.

Reproduction de : Habilitation à diriger des recherches : Sciences économiques : Lille 1 : 2006. / Synthèse des travaux. N° d'ordre (Lille 1) : 502. Curriculum vitae. Titre provenant de la page de titre du document numérisé. Bibliogr. p. 42-48. Liste des publications.

The effects of neutron displacement damage on materials are sensitive to neutron energy spectra. In controlled neutron damage experiments, a well characterized neutron flux spectrum is critical in determining the equivalent dose for displacement damage. Two techniques were used to characterize the neutron flux spectra in the University of Texas at Austin TRIGA research nuclear reactor. The first technique uses a standard method of measuring the reaction rates of two identical metal foils, one of which was irradiated in a Cd cover, the other of which was irradiated bare. Assuming an analytic form of the neutron spectrum the reaction rates were used to determine an approximate spectrum. The second technique uses the reaction rates measured from a set of activated metal foils along with two spectral unfolding techniques to approximate and then refine the neutron spectrum. A Matlab code was developed which fits radiative capture reaction rates to an approximate spectrum using a least squares approach. The result was used as an initial guess in a second Matlab code which refines the epithermal and fast energy ranges of the spectrum using reaction rates from threshold reactions. Errors in the reaction rates calculated from the resulting spectrum to the measured reaction rates were used to assess the accuracy of the final neutron spectrum. / text

Climate models forecast lower and less frequent precipitation in the next 50 years. This is especially pronounced in the central United States, where Texas is expected to lose a week’s worth of rain every summer. Water availability is a primary driver of carbon flux in terrestrial ecosystems – controlling photosynthesis and organic matter decomposition. Thus, under proposed rainfall shifts, understanding the potential ecosystem response is key to predicting the future of terrestrial productivity. Terrestrial nutrient cycling is also driven by microbial saprotrophs, which are the chief decomposers of organic matter. Understanding the microbial response to rain shifts is key in predicting the ecosystem response. Research supports both microbial community specialization to local environment, and that the microbial communities may have the ability to rapidly acclimate to environmental change. To address this question of microbial response, we used a steep natural rainfall gradient along the Edwards Plateau in central Texas. The Edwards Plateau is an ideal field site in which to test these ideas because nearly identical grassland habitat and soils are found across its entirety, while mean annual precipitation ranges from 45 cm to 91 cm. To understand how soil microbial communities varied as a result of historical rainfall differences, we divided the gradient into four isoclines based on precipitation (46-56 cm, 56-66 cm, 66-76 cm, and 76-86 cm), and examined soil and soil microbial community characteristics at three sites in each isocline. We further used soils from the same sites for a reciprocal soil moisture experiment, where we asked how soil microbial communities responded to altered moisture conditions. Using a full factorial design, soils from each site in each isocline were exposed to one of four soil moisture treatments: soil moisture from the ‘home’ isocline and the three other ‘away’ isoclines. The moisture treatments were maintained for one year. Microbial respiration was measured at regular intervals throughout the experiment; fungal hyphal abundance and inorganic nitrogen were measured at the final harvest. The soils collected from the gradient decreased in both soil moisture and hyphal abundance from the wet to the dry end of the gradient, but there was no trend in inorganic nitrogen. In the reciprocal moisture experiment, microbial CO2 respiration was affected by both home isocline and soil moisture treatment. Drier sites had a narrower response to wetter treatments and did not achieve the same activity as wetter sites regardless of soil moisture treatment. In contrast, soils from the wettest isocline experienced severe reductions in activity with drying, with activity at the driest moisture treatment below that found in soils that were from the driest isocline. These patterns are consistent with some degree of local specialization, which may constrain the ability of microbial communities to rapidly acclimate to altered precipitation regimes. This experiment did not include immigration, however, and shifts in community composition in the presence of dispersal may be able to counteract local specialization. Given expected future increases in drought intensity microbial decomposition activity is likely to decrease and local specialization may create a lag in acclimation to the new condition. Thus, local specialization of microbial communities should be considered when predicting ecosystem responses to future climate change and their potential feedbacks to ecosystem productivity and carbon storage. / text

Using cross-correlation analysis, we demonstrate that flux measurements at observation locations during hydraulic tomography (HT) surveys carry non-redundant information about heterogeneity that are complementary to head measurements at the same locations. We then hypothesize that a joint interpretation of head and flux data can enhance the resolution of HT estimates. Subsequently, we use numerical experiments to test this hypothesis and investigate the impact of stationary and non-stationary hydraulic conductivity field, and prior information such as correlation lengths, and initial mean models (uniform or distributed means) on HT estimates. We find that flux and head data from HT have already possessed sufficient heterogeneity characteristics of aquifers. While prior information (as uniform mean or layered means, correlation scales) could be useful, its influence on the estimates is limited as more non-redundant data are used in the HT analysis (see Yeh and Liu [2000]). Lastly, some recommendation for conducting HT surveys and analysis are presented.