Recent glacial recession in the Rwenzori Mountains of East Africa due to rising air temperature

Based on field surveys and analyses of optical spaceborne images (LandSat5, LandSat7), we report recent decline in the areal extent of glaciers in the Rwenzori Mountains of East Africa from 2.01 +/- 0.56 km(2) in 1987 to 0.96 +/- 0.34 km(2) in 2003. The spatially uniform loss of glacial cover at lower elevations together with meteorological trends derived from both station and reanalysis data, indicate that increased air temperature is the main driver. Clear trends toward increased air temperatures over the last four decades of similar to 0.5 degrees C per decade exist without significant changes in annual precipitation. Extrapolation of trends in glacial recession since 1906 suggests that glaciers in the Rwenzori Mountains will disappear within the next two decades

Geochemistry of the Potassic Basalts from the Bufumbira Volcanic Field in Southwestern Uganda

Bufumbira volcanic field is the southernmost of the four Ugandan small Pleistocene to Recent volcanic fields within the western branch of the East African rift system. The rocks consist of silica undersaturated and vesicular basalts with numerous primary structures. The rocks consist of basanites, leucitites, olivine basalts, trachytes, tephrites, trachyandesites and andesites. The basalts are picritic in the northern part of the field where they are dominated by olivine and are clinopyroxene rich in the southern part of the field. Leucite and plagioclase are common in the groundmass in varying proportions by volume for the entire field. Type 1 dunite and wehrlite upper mantle xenoliths characterize the northern part of the field whereas type II clinopyroxenite xenoliths are common in the southern part of the field. The various basalts are low in SiO2 wt %, Al2O3 wt % and Na2O wt % but high in MgO wt %, TiO2 wt %, CaO wt %, K2O wt % with K2O/Na2O = 1.08 to 2.07. These are potassic belonging to the kamafugite series. Plots discriminate two geochemical trends corresponding to the picritic and clinopyroxene rich basalts. The diagram of Na2O + K2O wt. % against SiO2 wt. % enables various rocks to plot in the designated fields for the different alkaline basalts. The field is enriched in trace, light rare earth (LREE) and high field trace elements (HFSE) where La/Yb = 31 – 55. The petrographic and geochemical studies elucidate enrichment of the upper mantle by both mineralogical (modal) and cryptic (geochemical) metasomatism.Keywords: Basalts, Enrichment, Mantle, Metasomatism, PotassicTanz. J. Sci. Vol 36 201

Hydrogeochemical processes in groundwater in Uganda: a national-scale analysis

Groundwater represents a vital source of freshwater to meet distributed, rapidly rising demands for safe drinking water, irrigation and industry in low-income countries across the tropics. The hydrochemistry of groundwater within deeply weathered crystalline rock aquifer systems that predominate at low latitudes, is determined primarily by long-term biogeochemical weathering of the parent bedrock. Here, we evaluate geochemical footprints and baseline chemical quality of groundwater that have developed from water-rock interactions across a range of geological environments in Uganda using a national database of hydrochemical and hydrogeological records from 3271 locations. Sampled groundwaters are mostly shallow (69% of samples from depths of <20 m below ground level), fresh at time of drilling (Electrical Conductivity <1000 μS cm−1 in 96% of samples), and of good quality (<8% of samples exceed WHO (2011) guidelines values for chemical parameters in drinking water). Unpalatably high concentrations of total soluble and suspended Fe are, however, common (21%) in meta-igneous, granitic and metamorphic formations. The dominant (95%) anionic facies of groundwater is bicarbonate (HCO3−), indicative of localized flow systems (i.e. discontinuous aquifers) in which chemical evolution of groundwater (e.g. as per Chebotarev sequence) is minimal. Low well yields (82% < 3.6 m3 h−1) and specific capacities (84% < 5 m2 d−1) support this inference; low aquifer transmissivities and storage serve to regulate naturally groundwater withdrawals (i.e. impacts of over-abstraction are localized). Overall, the results attest to the intrinsic high quality of groundwater that occurs in deeply weathered crystalline rock environments in Uganda, which may be expected across tropical Africa

Climate change and the aquatic ecosystems of the Rwenzori Mountains, Uganda

The Rwenzori Mountains are home to one of the last remaining tropical icefields outside of the Andes. Over the last century, equatorial icefields of the East African highlands have been steadily shrinking but the precise climate tropical alpine glaciers remain unclear. More than a decade had passed since the last detailed measurements of glacial cover were made in the Rwenzori Mountains. Recent evidence from Kilimanjaro suggests that its icecap will disappear entirely by the year 2020(1). The Rwenzori glaciers contribute meltwater flows to aquatic ecosystems of the Rwenzori Mountains National Park, a Word Heritage Site featuring spectacular, rare Afroalpine flora and fauna, and are headwaters of the River Nile. With the overall aim of assessing the impact of recent climate change on alpine aquatic ecosystems of the Rwenzori Mountains, a collaborative, international research team led by the University College London (United Kingdom) and Makerere University (Uganda), and involving the Institut für Geographie from the University of Innsbruck (Austria) and Water Resources Management Department (Uganda) was assembled in order to pursue three primary scientific objectives: • to assess the magnitude of current glacial recession; • to assess the impact of glacial recession on alpine riverflow; and • to assess recent environmental change from observational datasets and available, environmental archives stored in lake sediment and glacial ice

Championing urban farmers in Kampala. Influences on local policy change in Uganda. Process and partnership for pro-poor policy change

This working paper presents an analysis of actors, events and influences affecting a policy change on urban agriculture in Kampala. It reviews the policy and institutional changes related to urban agriculture that occurred in Kampala from 1990 to 2006, and examines how and why they came about. The approach used here combined elements of three established methodologies, viz, episode studies; case study analysis; and outcome mapping. For this case study, the episode study component was central, with the case study and outcome mapping components used to cross-check and deepen the analysis. This information was assembled into three overlapping narratives: 1. A timeline of activities that played a role in changing attitudes and behaviour towards urban agriculture. 2. An analysis of the development of policies affecting urban agriculture in Kampala including the new ordinances. 3. A description of behaviour change of key actors related to the policy change These were summarised in a visual representation of the process and influences and analysed using a framework emphasising political context and the roles of evidence, linkages and external environment

Vorkommen von Spurenelementen in Flusssedimenten und Grund- und Oberflächenwasser in der Bergbauregion von Gatumba, Ruanda

Aufgrund der intensiven Landnutzung durch Bergbau und Landwirtschaft sind die Gewässer im Gatumba Mining District durch Stoffaustrag aus Abraumhalden und Erosion stark geprägt. Untersuchungen während einer Trocken- und Regenzeit hinsichtlich der Konzentration von Spurenelemente haben gezeigt, dass von einer Gesundheitsgefährdung der lokalen Bevölkerung derzeit nicht ausgegangen werden kann. In der Regel weisen die Wasserproben der Trockenzeit gegenüber denen der Regenzeit tendenziell höhere Konzentrationen auf. Die Konzentrationen der Sedimente zeigen keinen entsprechenden Trend

The impact of maternal infection with Mycobacterium tuberculosis on the infant response to bacille Calmette-Guérin immunization.

Bacille Calmette-Guérin (BCG) immunization provides variable protection against tuberculosis. Prenatal antigen exposure may have lifelong effects on responses to related antigens and pathogens. We therefore hypothesized that maternal latent Mycobacterium tuberculosis infection (LTBI) influences infant responses to BCG immunization at birth. We measured antibody (n = 53) and cellular (n = 31) responses to M. tuberculosis purified protein derivative (PPD) in infants of mothers with and without LTBI, in cord blood and at one and six weeks after BCG. The concentrations of PPD-specific antibodies declined between birth (median [interquartile range (IQR)]) 5600 ng ml(-1) [3300-11 050] in cord blood) and six weeks (0.00 ng ml(-1) [0-288]). Frequencies of PPD-specific IFN-γ-expressing CD4(+)T cells increased at one week and declined between one and six weeks (p = 0.031). Frequencies of IL-2- and TNF-α-expressing PPD-specific CD4(+)T cells increased between one and six weeks (p = 0.019, p = 0.009, respectively). At one week, the frequency of PPD-specific CD4(+)T cells expressing any of the three cytokines, combined, was lower among infants of mothers with LTBI, in crude analyses (p = 0.002) and after adjusting for confounders (mean difference, 95% CI -0.041% (-0.082, -0.001)). In conclusion, maternal LTBI was associated with lower infant anti-mycobacterial T-cell responses immediately following BCG immunization. These findings are being explored further in a larger study

Effects of maternal and infant co-infections, and of maternal immunisation, on the infant response to BCG and tetanus immunisation.

Some vaccines show poor efficacy in tropical countries. Within a birth cohort in Uganda, we investigated factors that might influence responses to BCG and tetanus immunisation. Whole blood assay responses to crude culture filtrate proteins of Mycobacterium tuberculosis (cCFP)) and tetanus toxoid (TT) were examined among 1506 and 1433 one-year-olds, respectively. Maternal Mansonella perstans infection was associated with higher interleukin (IL)-10 responses to both immunogens but no reduction in gamma interferon (IFN-γ), IL-5 and IL-13 responses; other maternal helminth infections showed little effect. Tetanus immunisation during pregnancy was associated with higher infant responses to TT; maternal BCG scar (from past immunisation) with lower infant IL-5 and IL-13 responses to cCFP. IFN-γ, IL-5 and IL-13 to TT were reduced in HIV-exposed-uninfected infants; infant malaria and HIV were associated with lower IFN-γ, IL-5 and IL-13 responses to both immunogens. We conclude that maternal helminth infections are unlikely to explain poor vaccine efficacy in the tropics. Effects of maternal immunisation on infant responses to vaccines should be explored. Prevention of infant malaria and HIV could contribute to effectiveness of immunisation programmes