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Hydrophobic interaction chromatography (HIC) is a common purification method for biological drug substances. For continuous monitoring the quality of the purification, a column performance test is carried out to test the packing of the resin. The packing integrity is commonly tested between runs by measuring the Hight Equivalent to a Theoretical Plate (HETP) by injecting a small volume of a tracer solution (spike) that gives a change in conductivity. The column performance test provides useful information regarding the packing quality that could be used for troubleshooting before a purification is performed since a well packed gel is essential for an effective purification. During this thesis project a screening of suitable test conditions for a HETP test for a HIC column was performed. The developed HETP test were then investigated if it could be combined with the storage of the resin or if the packing is affected by the test conditions. Factors such as spike volume, flow rate and the concentration of the elute and spike solution, were considered. 0.1 M NaOH elute and 0.15 M NaCl as spike solution gave the best result based on HETP and the asymmetry of the conductivity peak. A test purification with the new HETP test conditions compared with the old method were then carried out to verify that the quality of the purification is not affected. The purification showed promising result and implementation of a more convenient storage solution and HETP test would be possible without changing the product quality.

Made available in DSpace on 2014-10-09T12:35:21Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:06:18Z (GMT). No. of bitstreams: 0 / Dissertação (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP

Made available in DSpace on 2014-10-09T12:35:21Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:06:18Z (GMT). No. of bitstreams: 0 / A Amazônia armazena em sua floresta na ordem de 95 a 120 PgC de biomassa viva e mais 160 PgC no solo, que podem ser rapidamente liberados para a atmosfera por meio da queima de biomassa e, também, pela mudança do uso da terra. Este estudo foi desenvolvido com o objetivo de elucidar a contribuição da Bacia Amazônica nas emissões de carbono no ano de 2010. A quantificação do CO2 foi realizada por meio da coleta do ar atmosférico utilizando aviões de pequeno porte que descreveram um perfil vertical em quatro locais, estrategicamente posicionado na Bacia Amazônica, e utilizando sistemas semiautomáticos de coleta de ar em 17 ou 12 altitudes diferentes. O Fluxo de emissão/absorção foi calculado pelo método de integração de coluna, que consiste na determinação da concentração de CO2 no perfil vertical, subtraído da concentração de entrada no continente, levando-se em conta o tempo que a massa de ar despende entre a costa e o local de amostragem. Para a determinação da concentração de entrada, foram utilizadas as concentrações medidas pela NOAA nas Ilhas de Ascencion e Barbados e, como traçador de massas de ar, o SF6. Foi encontrado um caráter emissor da Amazônia em território brasileiro para o ano de 2010, em torno de 0,41 PgC, considerando a média ponderada das quatro regiões estudadas, sendo a queima de biomassa a principal responsável. Para a determinação da emissão proveniente da queima de biomassa foi utilizado o CO, como traçador, e a razão CO:CO2. Apesar de possuir um perfil emissor neste ano anormalmente seco, foi possível observar um caráter sumidor de carbono. / Dissertação (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP

Natural organic matter (NOM) is a diverse blend of decomposed animal and plant material found in different natural water sources. Due to its large and complex structure, NOM is difficult to both remove and characterize in water. Therefore, there is a need to separate NOM into its components before it can be characterized. The aim of this project was to fractionate NOM through a novel size exclusion chromatography (SEC) composite (poly (styrene-divinyl benzene) (PS-DVB) and Polysilsesquioxane (PSQ)) packed column. Raw and final water samples from Mid-Vaal (MV), Olifantspoort (LO), Mtwalume (MT) and Preekstoel (P) were investigated. Poly (styrene-divinyl benzene) (PS-DVB) and polysilsesquioxane were both synthesized and optimized at various temperatures, compositions and time periods. An end-capping material such as hexamethyldisilizane (HMDS) was added on the PSQ to prevent active silanol groups on the polysilsesquioxane (PSQ) from reacting with active sites of NOM (our analyte). The E-PSQ (end-capped PSQ) and PS-DVB materials were packed in eight different SPE cartridges first, before the materials could be packed in the SEC column. This packing was done to check for the best mass composition of the E-PSQ and PS-DVB. From the obtained SPE results, both the EPSQ and PS-DVB were packed in one SEC/GPC column at a ratio of 1:1 in order to form the composite hybrid material. The packed SEC column was connected to an HPLC instrument and various column efficiency tests were evaluated. The results for the test of interactions with acidic compounds implied that the column can be used for the acidic analytes such as those forming NOM composition (humic acids, fulvic acids) and the column had minimum silanol groups. For hydrophobic interactions the stationary phase strength was different to that of the commercial columns and it could selectively elute molecules based on their different masses. The steric selectivity test showed that the stationary phase could separate and distinguish between molecules with similar hydrophobicity and structure but different shapes (o-terphenyl and triphenylene). The Hydrogen bonding capacity (HBC) test showed that the column had minimum silanol groups and the end-capping was successful on the E-PSQ. After fractionation of all the water samples, the MT raw showed NOM peaks around 1.8 mins, 3.4 mins and 5.3, and the final showed NOM peaks around 1.8 mins and 5.5 mins. The Mid-Vaal (MV) raw and final samples shows NOM peaks at around 1.8 mins and 6 mins. The Preekstoel (P) final water had one NOM peak at around 1.8 mins and raw samples had two NOM peaks around 1.8 mins and 6 mins. / Chemistry / M. Sc. (Chemistry)