Oxygen and hydrogen sulfide concentration of Nootka Sound bottom water

Senior thesis written for Oceanography 445

The Activity of Breast Milk and Monoclonal HIV-specific Antibodies in Mother-to-Child Transmission

Mother-to-child transmission of HIV is a unique setting that allows us to explore both the correlates of protective immunity and the characteristics of transmitted variants. This thesis first describes the levels and functional capacity of breast milk HIV-specific antibodies in 19 women with high plasma viral loads. Neutralizing antibodies (Nabs) were detected in breast milk supernatant (BMS) of 4 of 19 women examined, were of low potency and were not associated with infant infection. The low NAb activity in BMS was reflected in binding antibody levels with HIV envelope specific IgG titers being 2.2 log10 lower in BMS versus plasma. In contrast, non- neutralizing antibodies (nNAbs) capable of antibody dependent cell-mediated cytotoxicity (ADCC) were detected in the BMS from all 19 women. BMS ADCC activity was associated with envelope-specific IgG titers (p = 0.014) and was inversely associated with infant infection risk (p = 0.039). Our data indicate that BMS has limited HIV neutralizing activity, however, BMS ADCC activity is a correlate of transmission that may impact infant infection risk. In the second part of this thesis the neutralization sensitivity of 111 variants of diverse subtypes obtained from mothers and infants was determined against 7 HIVspecific broadly neutralizing monoclonal antibodies (mAbs) (NIH45-46w, VRC01, PGT128, PGT121, PG9 PGT145 and b12). Maternal and infant variants did not differ in their neutralization sensitivity to these mAbs and neither did variants from transmitting versus those from non-transmitting women. However, subtype A viruses were iii significantly more sensitive to neutralization by NIH45-46w and VRC01 (p= 0.0001 in both cases) and PGT145 (p=0.03) compared to non-subtype A viruses. Together, NIH45- 46w and PGT128 neutralization profiles resulted in 100% coverage of the variants tested. These data suggest that the epitopes targeted by these mAbs are present and accessible in both circulating and transmitted variants and that a combination of antibodies would provide maximum coverage against diverse subtypes commonly found in HIV endemic regions. Overall, this data suggest that an antibody based HIV vaccine capable of eliciting antibodies of multiple specificities that can mediate ADCC and/or neutralizing activity can provide protection and conquer the genetic diversity displayed by HIV.

Analysis of the Hydrogeological Conditions and the Effects of Development on the Hydraulic Head at Redmond Ridge East

Redmond Ridge East (RRE) is a large-scale master plan community in East King County, WA. In this report, I evaluate the spatial variability of the Quaternary Advance Outwash (Qva) at RRE and the time-series data for 16 water wells with the intent to better understand groundwater below the RRE area. I investigate changes between pre- and post-development conditions through the determination of temporal changes in annual water level, annual water level fluctuations, hydraulic head response to precipitation, and ambient drainage of the aquifer. I also perform a basic analysis of the annual aquifer recharge and a determination for the storage through the implementation of the water table fluctuation (WTF) method. Associated Earth Sciences (AESI) was tasked with monitoring the geological and environmental impacts during the development of RRE and collected the data I use in this report. AESI involvement in monitoring began in 1998 and extends to the present. Sixteen wells were identified in the RRE area with adequate temporal data to conduct the analysis. A comparison of the well logs and aquifer testing data allowed local variations in the Qva to be mapped. The WTF was used to determine a range of reasonable specific yield values for locations where the Qva was unconfined. Yearly average of the seasonal water level high and lows, and the fluctuations were quantified. Temporal relationships were established through linear regression. The average water level was found to be increasing in some locations, and the corresponding fluctuations were found to decrease. However, no clear change between pre- and post-development was observed. The response of hydraulic head to precipitation was investigated through an analysis of hydrographs for ten wells. Periods of consistent response and the corresponding precipitation during each period were delineated. A linear relationship between precipitation and water level change was determined. The threshold precipitation under which there is a positive response in the hydraulic head was established. No observable changes were apparent between pre- and post-development conditions. The ambient drainage for the Qva was calculated using recessional periods on the hydrograph. The transmissivity of Qva varies with thickness of the overlying lodgment till and thickness of the Qva, itself. Water level fluctuations observed in the Qva are consistent with regional observations. Localized areas in the Qva display the large 10 foot fluctuations and these anomalies are likely due to a combination of the local variability in the storativity as well as the concentration and channeling of water due to geographical variations in the Qva and the overlying topography. All trends seen in the RRE area remained relatively constant through time. There was no evidence showing an effect of development on the hydraulic head at RRE. This implies that the style and distribution of infiltration has not changed as a result of development, and that any measures in place are properly mitigating the effects of development on the RRE region.

Mixing Regimes in the Amundsen Basin of the Arctic Ocean

Thesis (Ph.D.)--University of Washington, 2016-06