Cowpea (Vigna ungiculata L. Walp) is a major food and fodder legume in poor countries, particularly Sub-Saharan Africa countries. It is generally produced in sandy, acid soils, deficient in phosphorus (P) which severely limits its production. Because processed phosphate fertilizers are expensive and poorly available to farmers, rock phosphate is viewed as a cheap alternative phosphate source. The present study evaluated 696 U.S Core Collection and IITA cowpea accessions for adaptation to low soil P environments and for response to rock phosphate application. Subsequently, organic acid exudation by selected cowpea genotypes as a mechanism for P acquisition from Fe-oxide and Ca bound P was investigated. A low P soil from Nacogdoches pine forest was used to grow plants. There were two P treatments: 0 and 300 mg P/kg of soil as Tahoua (Niger) rock phosphate. At harvest, plant height, shoot and root dry weights were determined and total biomass and shoot-to-root ratios were computed. Shoot P contents of 100 selected accessions were measured. Sixteen accessions reflecting the wide array of responses observed were selected for the organic acid study. Plants were grown in a growth chamber hydroponically with no P and +P nutrient solutions for 3 weeks. Organic acids were collected in a CaCl2-KCl solution. The nature and quantity of the collected organic acids was determined. Cowpea accessions were significantly different in their ability to adapt to Pdeficiency stress and to acquire P from rock phosphate. The parameters most effective in separating the accessions were shoot mass and total biomass. This data will be potentially useful in the selection of cowpea germplasm for (1) adaptation to West African soils of low P fertility, and (2) ability to utilize P from poorly soluble rock phosphate. The predominant organic acid exuded by cowpea roots was a tricarboxylic acid not yet identified. There was surprisingly more exudation of this acid under +P than under –P conditions. Exudation was more highly correlated to roots than to shoots.

The objective of this research was to investigate the retention of arsenate (iAsV), arsenite (iAsIII), monomethyl arsenate (MMAsV) and dimethyl arsenate (DMAsV) by calcite and assess the impact of dissolved Ca2+, Mg2+, phosphate and sulfate on arsenic solubility, adsorption and precipitation phenomena. Adsorption kinetics of iAsV, evaluated at a low and high concentration, was a relatively rapid process, with a fast initial reaction rate within the first few minutes and a subsequent slower reaction rate as equilibrium was approached. The relative adsorption of arsenicals decreased in the following order: iAsV > iAsIII > DMAV > MMAV. In no case was a clear adsorption maximum observed with increasing dissolved arsenic concentration. Dissolved 0.01 M Ca2+ resulted in an increase in iAsV adsorption; however, in the presence of 0.1 M Ca2+ adsorption of iAsV was decreased. The presence of Mg2+ as 0.01 M Mg(NO3)2 resulted in decreased iAsV adsorption probably the result of a lower iAsV affinity for adsorbed Mg2+ as compared to Ca2+. Phosphate and sulfate were highly competitive with iAsV in adsorption to calcite and both resulted in decreased iAsV adsorption. The total prevention of iAsV adsorption at initial equimolar arsenic/phosphate concentrations > 88 µM each could be from the consumption of available calcite surface sites by the specific adsorption of phosphate. Equilibrium modeling, using the geochemical and mineral speciation of equilibrium model (MINTEQA2), indicated that at low concentrations of arsenate or phosphate solid-phase precipitation was not likely and adsorption processes likely controlled solubility. At high concentrations of arsenate Ca3(AsO4)2 · 3 2/3 H2O and Ca3(AsO4)2 · 4 1/4 H2O solid phases could be controlling arsenate solubility. This study indicates that arsenic adsorption response by calcite was different than that of phosphate suggesting that arsenic may not be specifically adsorbed to calcium at the calcite surface. Reduction and biomethylation of arsenic decreased adsorption, suggesting that processes which could affect the speciation of arsenic in the environment, could increase arsenic mobility in environmental systems where calcite and dissolved aqueous calcium play a predominant role in controlling arsenic solubility. Dissolved aqueous concentrations of magnesium, phosphate and sulfate generally reduced the ability of arsenic to be adsorbed to calcite.

To understand the soil microbial community structures of different locations and altitudes, as well as the fluctuation of microbial populations foward seasonal change, this study investigated the biodiversity of soil microbiota of eight sampling sites along the Lao-Nong River basin during 4/11/2003~3/21/2004. The results showed that the soil properties were different among these sampling sites. The soil temperatures were ranging in between 24~32¢J, except Tianchr, the highest altitude sampling site (7~19¢J) ; pH values were 4.00 (Tianchr) ~8.20 (Tauyuan) ; moisture contents were 2.31% (Liouguei) ~70.23% (Tianchr) ; total organic carbon contents were 0.38% (Linkou) ~36.21% (Tianchr) ; total organic nitrogen contents were 0.067% (Tauyuan) ~0.672% (Tianchr); the C/N ratio were 7.0~25.0, except Tianchr (42 in average) . In microbial community structures analysis, bacteria were the most abundant organisms among all soil samples (106~108 CFU per gram of soil) . The amount of other microbes were as follow: nitrogen-fixing microbes 105~107 CFU, actinomycetes 104~107 CFU, fungi 104~106 CFU, cellulolytic microbes 104~106 CFU, and the least one was phosphate- solubilizing microbes 103~105 CFU. For molecular biological microbiota analysis, the bead-beating DNA extraction method resulted the richest bacterial 16S rDNA DGGE profile. The16S rDNA DGGE profiles of various samples taken from different seasons showed somewhat seasonal variations that might relate to the specific climates of Taiwan, such as the plum rains and typhoons. Moreover, we also successfully cultured and preserved many microbes with specific biological functions. These microorganisms will provide a useful resource for further research and development in the biotechnology industries.

Tissue engineering is an interdisciplinary field that seeks to address the needs by applying the principles of chemistry, biology and engineering for the development of viable substitutes that restore and maintain the function of human bone and cartilage tissues. In tissue engineering, scaffolds play an important role as temporary supports for the transplantation of specific cells and tissues. In this study, poly(ester-urethane)urea (PEUU) and poly(caprolactone) (PCL) scaffolds were fabricated. Scaffolds were characterized by SEM. Porosities of scaffolds vary from 67 % to 80 %. Controlled drug delivery systems release drugs at predetermined rates for extended periods. In this study / firstly poly(lactic-co-glycolicolide/tricalcium phosphate) (PLGA/TCP) and poly(L-lactide)/tricalcium phosphate (PLLA/TCP) composites loaded with Gentamicin or Vancomycin were prepared as controlled drug delivery systems for the local treatment of osteomyelitis. The release behavior of drugs were monitored by UV-VIS spectrometer. It was shown that, Vancomycin loaded samples released higher amounts of drug than the samples loaded with Gentamicin. Secondly, porous ceramic samples were coated with PLGA and PLLA and they were loaded with dexamethasone. The release behavior of samples were monitored by UV-VIS spectrometer.The cubic ceramics released higher amounts of dexamethasone than cylindrical ceramics. When the mechanical properties of porous ceramic samples were concerned, PLLA coated samples had better mechanical properties.

In many organisms, trehalose protects against several environmental stresses, such as heat, desiccation and salt, probably by stabilizing protein structures and lipid membranes. Trehalose-6-phosphate synthase 1 (TPS1) is a subunit of trehalose synthase complex in fungi / it plays a key role in the biosynthesis of trehalose. In this study, a TPS1 gene fragment in R. oryzae was cloned successfully by PCR with primers designed according to eight hypothetical proteins found from BLAST search which was performed by using S. cerevisiae TPS1 gene template. The full length of R. oryzae TPS1 gene (designated RoTPS1) was attained by RTPCR with primers specific to the 3&amp / #8242 / and 5&amp / #8242 / end of the RoTPS1 cDNA. The RoTPS1cDNA was composed of 2505 bps encoding a protein of 834 amino acids with a molecular mass of 93.8 kDa. The amino acid sequence has relatively high homology with the TPS1s of several other organisms. RoTPS1 was further characterized by transformation into S. cerevisiae tps1 mutant. In galactose media, the growth curves of wild type, tps1 mutant and transformant S. cerevisiae cells had a comparable pattern in general, tps1 mutant reached to a higher maximum cell concentration compared to the others and wild type had a slightly lower specific growth rate compared to the tps1 mutant and transformed cells. Trehalose levels of transformant and wild type cells were increased up to 37 mg/gdw in the stationary phase.

ABSTRACT AN INVESTIGATION OF THE MICROSTRUCTURAL AND MECHANICAL PROPERTIES OF TRI-CALCIUM PHOSPHATES DOPED WITH ALUMINUM AND FLUORIDE IONS Tahmasebifar, Aydin M. Sc., Department of Engineering Sciences Supervisor: Assoc. Prof. Dr. Zafer Evis August / 88 Pages The aim of this study was to investigate the microstructure and mechanical properties of pure tricalcium phosphate (TCP) and tricalcium phosphates doped with aluminum (Al3+) and fluoride (F-) ions at different compositions. TCP was synthesized via precipitation method and sintered at 1100

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The study was to investigate the changes in (1) triacylglycerol (TAG) contents and its relationship to (2) lipid synthesis- and metabolism-related enzyme activity and (3) their gene expression in cobia (Rachycentron canadum) during the fast growth period (from October 2006 to April 2007) in ventral muscle and liver in Hsiao-Lu-Chiao island in southwestern Taiwan. The crude lipid was 12% for fed diet, 30-40% for liver while 13% in February and 11% to 9% in other month for muscle. The TAG content of crude lipid was 36 % for fed diets, and from 22% (December) to 40% (February) for muscle, and from 63% (October to February) to 47% (March) for liver. Oil red-O (ORO) staining showed that TAG accumulated in muscle in February but in December in liver. Muscle TAG contents and enzyme activities and mRNA levels of GPDH and FAS increased in February. A decrease in GPDH enzyme activity and mRNA levels but an increase in PEPCK enzyme activity and mRNA levels indicate the increased supply of acetyl-CoA for fatty acid synthesis is in muscle. An increase in FATP2 mRNA levels suggest the influx of fatty acid also contributes to increased fatty acid accumulation in muscle.In liver, TAG and fatty acid contents decreased in March April but increased FAS and PEPCK enzyme activity and mRNA levels. It is possible that fatty acid synthesis is enhanced in March, but a fast transport to other organs results in a net decline in liver fatty acid contents and subsequently a decrease in TAG contents. FATP contents decreased in March-April mRNA, indicating that the influx of fatty acid in decreasing in liver in adult fish. GPDH and GAPDH were not related to lipid metabolism in liver. These data from enzyme activity and mRNA level, demonstrated that a potentially increase in acetyl-CoA via PEPCK contributes to fatty acid synthesis and GPDH-mediated synthesis of G-3-P provide the C skeleton for TAG synthesis.

This work focuses on the chemical substitution of cations and anions in the frameworks of materials that have been known to exhibit negative thermal expansion (NTE). Zr2(PO4)2(SO4) is a member of the A(2)M(3)O(12) family which has been known to exhibit NTE. We have shown that Zr2(PO4)2(SO4) exhibits anisotropic positive thermal expansion. We have also shown that this material has been characterized in the wrong space group. Hf2(PO4)2(SO4) behaves similarly to Zr2(PO4)2(SO4) and follows this trend. Under pressure, Hf2(PO4)2(SO4) appears to undergo a phase transition. We have still yet to determine what space group the materials transitions to. While many members of the AX(2)O(7) family of frameworks have been fully characterized, the thermal expansion of PbP2O7 has yet to be reported. We were unable to obtain a reproducible procedure for synthesis of PbP2O7 from its precursor. Finally, variable temperature and variable pressure studies were performed on ZrMo2O8 in an attempt to learn more about the local structure. We found that space groups P213 and Pa-3 gave poor fits of the local structure at low r. Behavior of the nearest neighbor Zr-Mo distance was very similar to the bulk CTE. On compression, pressure induced amorphization is observed in ZrMo2O8. All interatomic correlations above 4 angstroms are washed out. Zr-O-Mo linkages remain well defined and do not massively deform as the pressure is increased. Finally, we we observed that Zr-O-Mo linkages change geometry reversibly as the pressure is increased.

Phosphorus (P) is a requirement for biological growth, but this vital nutrient is present at low or limiting concentrations across vast areas of the global surface ocean. Inorganic polyphosphate (poly-P), a linear polymer of at least three orthophosphate units, is one component of the marine P cycle that has been relatively overlooked as compared to other P species, owing in part to a lack of routine analytical techniques that cleanly evaluate it within samples. This thesis demonstrates that inorganic poly-P is a quantitatively significant and dynamic component of the global marine P cycle while also establishing two new techniques for its analysis in biological and environmental samples. In Chapter 2, experiments using the freshwater algae Chlamydomonas sp. and Chlorella sp. illustrate X-ray fluorescence spectromicroscopy as a powerful tool for the sub-micron scale assessment of poly-P composition in organisms. This method enabled the discovery, detailed in Chapter 3, of a mechanism for the long-term sequestration of the vital nutrient P from marine systems via the initial formation of poly-P in surface waters and its eventual transformation into the mineral apatite within sediments. The importance of marine poly-P is furthermore established in Chapter 3 by observations showing that naturally-occurring poly-P represents 7-11% of total P in particles and dissolved matter in Effingham Inlet, a eutrophic fjord located on Vancouver Island, British Columbia. In Chapter 4, a new fluorometric protocol based on the interaction of inorganic poly-P with 4',6-diamidino-2-phenylindole (DAPI) is established as a technique for the direct quantification of poly-P in environmental samples. Chapter 5 presents work from Effingham Inlet utilizing this method that show that inorganic poly-P plays a significant role in the redox-sensitive cycling of P in natural systems.