The ecological and social context of mammal hunting in the coastal savanna of Ghana

This article argues that insufficient attention has been paid in the recent literature to the social and environmental factors which regulate hunting in Ghanaian savannas, and to how this may influence the sustainability of their livelihoods. Despite the vital significance of this issue, the emphasis in the literature and media has been on the destructive impacts of hunting and the bushmeat trade on wildlife. Taking a case study from the coastal savanna of Ghana, a region commonly regarded as a degraded relict of former deciduous forest with a richer wildlife past, it investigates the hypothesis that structure/actor dualities, manifested by socio-cultural change, local environmental knowledge and livelihood activity options, are the primary regulators of hunting intensity and possible sustainability. Such an evaluation is effective if done from a structuration perspective. The integrated methodology incorporates social surveys, GIS based time series image analysis, ecological field methods and statistical analysis. The results provide evidence that the direct and indirect regulatory functions of the socioenvironmental context provide a core feature of the sustainability of hunting. It is concluded that local strategies of resource management may provide an effective complement to conservation policy.     

Poverty and HIV prevalence in Ghana: a geographical perspective

There is a widespread belief that poverty leads to the spread of HIV/AIDS. However, intra-country comparisons of the phenomenon have been limited. This study seeks to fill this gap by examining the relationship between poverty and HIV prevalence amongst the 10 administrative regions of Ghana. Based on the available data for poverty and HIV, certain distinct patterns emerge. For example, poverty levels are the highest in the three northern regions (Upper East, Upper West and Northern region) even though their HIV prevalence is one of the lowest. It clearly follows that there are more complex forces at work than just the effects of poverty alone. To unravel some of these puzzles, the paper proposes a key role for culture, globalization and geographical accessibility. In addition, it is suggested that local level studies in a multivariate framework have much to contribute to the identification and quantification of relevant relationships.     

Hydrogeologic and hydrochemical framework of the shallow groundwater system in the southern Voltaian Sedimentary Basin, Ghana

 The southern Voltaian Sedimentary Basin underlies an area of about 5000 km² in east-central Ghana. Groundwater in the basin occurs in fractures in highly consolidated siliciclastic aquifers overlain by a thin unsaturated zone. Aquifer parameters were evaluated from available aquifer-test data on 28 shallow wells in the basin. Hydraulic-conductivity values range from 0.04–3.6 m/d and are about two orders of magnitude greater than the hydraulic conductivity calculated using Darcy's Law and the average groundwater velocity estimated from carbon-14 dating. Linear-regression analysis of the transmissivity and specific-capacity data allowed the establishment of an empirical relationship between log transmissivity and log specific capacity for the underlying aquifers. Groundwater chemistry in the basin is controlled by the weathering of albitic plagioclase feldspar. The weathering rates of various minerals were estimated using ¹⁴C-derived average velocity in the basin. The weathering rate of albite was calculated to be 2.16 μmol L^–1 yr^–1 with the resulting formation of 3.3 μmol L^–1 yr^–1 of kaolinite and 0.047 μmol L^–1 yr^–1 of calcite. The low porosity and permeability of the aquifers in the basin are attributed to the precipitation of secondary minerals on fracture surfaces and interlayer pore spaces. Received, September 1997 Revised, July 1998, August 1998 Accepted, August 1998     

Hydrochemical characterization of groundwater in the Accra plains of Ghana

Chemical and isotopic analyses are used to characterize and identify the relevant water-rock interactions, which are responsible for the poor groundwater quality in the Accra Plains. Four main water types are identified. Processes that singly or in combination influence the chemical composition of each water type include halite dissolution carbonate dissolution and precipitation, seawater intrusion, cation exchange, evaporative concentration of solutes and aluminosilicates dissolution. These processes contribute considerably to the concentration of major ions in the groundwater. Stable isotope contents of the groundwater suggest mainly direct integrative recharge. A few samples plot along the meteoric-seawater mix line which is coincidentally the evaporative line. The Cl⁻/Br⁻ ratios of some of these are close to 300 confirming marine origin, others probably concentrated by evaporation have their Cl⁻/Br⁻ ratios significantly lower than 300. Groundwater is qualitatively good for drinking purposes only along the foothills of the Akwapim Togoland ranges.     

加纳水井钻完井施工技术

饮用水问题是关系到加纳人民健康和社会经济发展的重要问题。为解决这一问题,包括中国在内的世界多国政府和世界组织提供资金,建设了一批水井项目以改善该国的饮用水现状。湖北省地质工程有限公司在加纳历经21年的野外工作,克服各种技术问题,共完成4000多口水文水井的施工任务,积累了丰富的水文水井施工经验。本文介绍了加纳的水文地质概况及当地的施工技术要求,提出了一套适合于当地环境的施工机械设备配套方案。针对该国花岗岩、千枚岩和石英砂岩3大类地层特点,各提出了一套含开孔、钻进、扩孔和下滤管、投滤料等工序的钻完井施工工艺技术方案。     

Hydrogeologic framework and borehole yields in Ghana

In Ghana, 68% of the population live in rural communities, which are scattered and remote. Groundwater is the most feasible source of potable water supply for most of these dispersed and remote settlements. To meet the present and future challenges of population expansion vis-à-vis the observed declining rainfall in most parts of Africa including Ghana, it is necessary to assess, efficiently manage, and utilize the groundwater resources. The objective of this paper is therefore to describe the hydrogeologic framework and analyze borehole yields as part of the groundwater-resources assessment of Ghana. The hydrogeologic units are broadly categorized as: (1) the Basement Complex (crystalline rocks), which underlies about 54% of the country; (2) the Voltaian System, which underlies about 45%; and (3) the Cenozoic, Mesozoic, and Paleozoic sedimentary strata (Coastal Provinces), which underlie the remaining 1% of the country. The Basement Complex and the Coastal Provinces have higher groundwater potential than the Voltaian System. This is particularly significant, because the Basement Complex and the Coastal Provinces underlie the most densely populated areas of the country and can hence be tapped for human use. The average borehole yields of the Basement Complex, the Coastal Provinces and the Voltaian System range from 2.7–12.7, 3.9–15.6, and 6.2–8.5?m3/h, respectively.     

Water quality analysis of groundwater in crystalline basement rocks,Northern Ghana

Hydrochemical data are presented for groundwater samples, collected from fractured aquifers in parts of northern Ghana. The data was collected to assess the groundwater suitability for domestic and agricultural use. Results of the study reveal that the pH of the groundwater in the area is slightly acidic to slightly alkaline. The electrical conductivity values, total dissolved solids (TDS) values and calcium, magnesium and sodium concentrations in the groundwater are generally below the limit set by the WHO for potable water supply. On the basis of activity diagrams, groundwater from the fractured aquifers appears to be stable within the montmorillonite field, suggesting weathering of silicate minerals. An inverse distance weighting interpolator with a power of 2 was applied to the data points to produce prediction maps for nitrate and fluoride. The distribution maps show the presence of high nitrate concentrations (50–194 mg/l) in some of the boreholes in the western part of the study area indicating anthropogenic impact on the groundwater. Elevated fluoride level (1.5–4 mg/l), higher than the WHO allowable fluoride concentration of 1.5, is recorded in the groundwater underlying the northeastern part of the study area, more specifically Bongo and its surrounding communities of the Upper East region. Results of this study suggest that groundwater from the fractured aquifers in the area exhibit low sodicity–low salinity (S1–C1), low sodicity–medium salinity (S1–C2) characteristics [United States Salinity Laboratory (USSL) classification scheme]. All data points from this study plot within the ‘Excellent to good’ category on a Wilcox diagram. Groundwater in this area thus appears to provide irrigation water of excellent quality. The hydrochemical results indicate that, although nitrate and fluoride concentrations in some boreholes are high, the groundwater in the study area, based on the parameters analyzed, is chemically potable and suitable for domestic and agricultural purposes.     

Spessartine Garnets in a Manganiferous Carbonate Formation from Nsuta, Ghana

Abstract: Manganese carbonate ore beds and host rock manganiferous phyllites at the Nsuta mine, western Ghana, contain well developed garnet crystals. Individual crystals are idioblastic, sometimes porphyroblastic, and homogeneous, and are associated with rhodochrosite (with or without kutnahorite), quartz and muscovite. The conspicuous absence of chlorite in garnet-rich assemblages, and of garnet in chlorite-rich rocks, suggest chemical constraints may have been important in the formation of the two minerals. Gondite bands within carbonate ores are interpreted to have resulted from localised processes in which manganese carbonates, in environments rich in alumino-silicate minerals, may have been completely exhausted during metamorphic reactions.     

An assessment of the extent and causes of food insecurity in northern Ghana using a livelihood vulnerability framework

The article describes the food insecurity situation in three villages in northern Ghana. A livelihood approach is used emphasising the vulnerability of the peasants’ adaptation to a marginal and remote area. The peasant households are grouped according to level of food insecurity. It is argued that multiple income sources including non-farm activities are necessary to reduce food insecurity for all but a small part of the peasant households.     

RETRACTED ARTICLE: The hydrochemical framework of surface water basins in southern Ghana

Surface water resources play a crucial role in the domestic water delivery system in Ghana. In addition, sustainable food production is based on the quality and quantity of water resources available for irrigation purposes to supplement rain-fed agricultural activities in the country. The objective of this research was to determine the main controls on the hydrochemistry of surface water resources in the southern part of Ghana and assess the quality of water from these basins for irrigation activities in the area. R-mode factor and cluster analyses were applied to 625 data points from 6 river basins in southern Ghana after the data had been log transformed and standardized for homogeneity. This study finds that surface water chemistry in the south is controlled by the chemistry of silicate mineral weathering, chemistry of rainfall, fertilizers from agricultural activities in the area, as well as the weathering of carbonate minerals. A Gibb’s diagram plotted with total dissolved solids (TDS) on the vertical axis against (Na⁺ + K⁺)/(Ca²⁺ + K⁺ + Na⁺) on the horizontal axis indicates that rock weathering plays a significant role in the hydrochemistry. Activity diagrams for the CaO–Na₂O–Al₂O–SiO₂–H₂O and CaO–MgO–Al₂O₃–SiO₂–H₂O systems suggest that kaolinite is the most stable clay mineral phase in the system. In addition, an assessment of the irrigation quality of water from these basins suggests that the basins are largely low sodium—low to medium salinity basins, delivering water of acceptable quality for irrigation purposes.     

热带雨林景观土壤测量采样深度与样品粒级试验研究——以加纳国雅卡锰金矿为例

加纳国雅卡锰金矿床位于著名的阿散蒂金矿带上。在该成矿带进行土壤测量采样深度、样品粒级试验以及方法技术的适应性和有效性研究,可为下一步开展大面积土壤地球化学测量提供技术依据,从而圈定可靠土壤地球化学异常。本文采用的工作方法为土壤垂向剖面法,选择有代表性的地段进行试验研究,结果显示在已知矿上方获得了明显的土壤地球化学异常。通过实验研究,选取土壤测量采样深度60～80 cm,截取样品粒级-4～+20目,获得了可靠、明显的土壤地球化学异常。研究证明该方法具有显著的地球化学找矿效果。     

河西走廊干旱荒漠区盐碱化土地修复与调控研究--以石羊河灌区为例

近年来，由于自然因素和人为因素的共同作用，石羊河灌区盐碱化土地面积逐年增加，盐碱化程度不断加深，严重影响到该区国民经济、社会和生态环境的可持续发展。文章分析了造成石羊河灌区盐碱化的自然因素和人为因素．认为自然因素主要是：①．气候干旱，降水稀少，蒸发量强烈；②．水资源量逐年减少；③．地势上位于我国现代地形的第二阶梯，为内陆河流；④．地下水质矿化度高。人为因素是：①．过度开荒，灌区大量超采地下水；②．植被大量减少，加剧了土地盐碱化；③．灌溉技术落后，有灌无排。同时从四个方面探索建立了科学合理的石羊河灌区盐碱化土地综合调控措施：①．水资源合理配置；②．以水盐平衡理论为指导，调控地上水位和盐分的时空分布；③．加强以节水灌溉为核心的灌区配套建设，推广节水防盐的灌水技术；④．扩大牧草种植，逐步实现农业三元结构。     

Transitions to adulthood among young entrepreneurs in the informal mobile telephony sector in Accra,Ghana

The rapid expansion of the mobile telephony sector in African countries has been accompanied by the establishment of a wide range of informal support businesses, mostly run by young people. Little is known, however, about the lived experiences of young entrepreneurs working in this rapidly changing, technologically-driven sector. Drawing on qualitative research conducted in Accra, this paper explores young people's experiences of running informal businesses within the mobile telephony sector, including the sale of mobile phones and accessories, repair and technical support services, and the sale of airtime and mobile money services. Fateful and critical moments relating to personal and family events, as well as social networks and structural factors, are shown to mediate young entrepreneurs' chances of success in this new ‘niche' economic sub-sector. Despite the challenges they face, the paper illustrates how many of these young people have been able to achieve financial independence, afford rental accommodation, provide support for family members, and establish and sustain households. The mobile telephony sector is shown to be offering young people the opportunity to carve out a living, facilitate transitions into adulthood, and even enable some to move up the social ladder. By highlighting the agency of this group of young people, and for some their success in achieving the status of adulthood through their hard work and ingenuity, this study offers an important counter balance to images of young people in sub-Saharan Africa as being ‘stuck' or in ‘waithood'.     

Changing rainfall inputs in the Volta basin: implications for water sharing in Ghana

We present evidence from the analysis of gridded annual rainfall data that, increased variability and declining rainfall totals are the main cause of declining lake levels in the Volta basin above the Akosombo Dam. West Africa has undergone a period of diminished rainfall, punctuated by a series of severe droughts and marked by a shift in rainfall regime. As a result, lake levels behind the hydro-electric impoundment have fluctuated so widely at times that, power has had to be rationed. The trends in the spatial and temporal variability of annual rainfall in the riparian nations explain the low impoundment levels frequent in recent decades. The drying of Burkina Faso and Mali is particularly marked and synchronous to an apparent shift in the rainfall regime in Ghana towards a longer dry season and vanishing short dry spell, the effects which tend to negate each other. The various regional and temporal associations between El Niño-Southern Oscillation phenomenon (ENSO) are investigated as a possible cause of variation across the basin. The strengths of these associations and low frequency shifts suggest an unfortunate correspondence between national and climatological boundaries which may serve to heighten regional political tensions resulting from ENSO effects. Lack of re-investment in the Akosombo Dam as a result of management policies, political and pre-construction contractual agreements have all conspired in recent decades to make these hydro-climatological changes more devastating.     

Geochemistry, genesis, and health implications of fluoriferous groundwaters in the upper regions of Ghana

 The most appropriate and widely used source of drinking water for the populations of the upper regions of Ghana is groundwater. In general, groundwater quality is acceptable except for some parts of the Bolgatanga and Bongo Districts, where there are occurrences of elevated levels of natural groundwater fluoride. Concentrations of groundwater fluoride in excess of the World Health Organization (WHO) maximum guideline value (1.5 mg/l) in the Bongo area have been known since 1978. However, the effect of fluoride on people ingesting the water did not receive public and medical attention until October 1993, when health personnel were asked to investigate the cause of stained teeth in school children. The investigation established that 62% of the total population of school children in the Bongo area had dental fluorosis. Against this background, a study was initiated to understand the geochemistry, genesis, and distribution of fluoride in relation to the geology of the area. Groundwater fluoride in the upper regions ranges from 0.11 to 4.60 ppm, with the highest concentrations associated with the fluorine-enriched Bongo coarse-grained hornblende granite and syenite suite. The source of groundwater fluoride within the Bongo granitoids is dissolution of the mineral fluorite and dissolution of and anion exchange with micaceous minerals and their clay products. Applying the WHO recommended guideline values for fluoride in drinking water reveals that 49% of wells in the area deliver water below the optimum level of 0.5 mg/l F^–; these populations are thus prone to dental caries. Twenty-eight percent of the wells fall within the optimum interval for good dental health (0.5–1.5 mg/l F^–). Twenty-three percent of the wells have concentrations above the recommended maximum guideline limit of 1.5 mg/l F^–; this population is susceptible to dental and possibly skeletal fluorosis. Climatic conditions of the area suggest that the individual water consumption is in the order of 3 to 4 l which is higher than the WHO estimate of 2 l/adult/day. In addition, dietary intake for the upper region population is probably higher than WHO baseline values (0.2–0.5 mg/day). This implies that a much higher population is susceptible to developing dental and skeletal fluorosis than originally suspected. Geochemical symbol plot maps help geochemists understand factors controlling the distribution and uptake of fluoride in the upper regions, but they are of minimal value to health officials responsible for planning epidemiological studies and dental health education programs in the region. By casting fluoride data into contoured 'geochemical health-risk maps' using intake interval guidelines more closely aligned to regional climatic and dietary conditions, health officals can better judge the impacts (regional and population based) of fluoride on segments of the population, such as various sex and age groups. Received: 11 March 1997 · Accepted: 17 June 1997     

Environmental concerns of poor households in low-income cities: the case of the Tamale Metropolis,Ghana

The Tamale Metropolitan Area (TMA), as a low-income city in a heavily indebted poor country, is at the first stage of the urban environmental transition where most of the environmental problems tend to occur close to the home. Some of the more severe household environmental problems are poor housing, inadequate potable water supply, unsanitary conditions, uncollected garbage, indoor air pollution and pest infestation. Those usually exposed to these environmental burdens are the less wealthy households who have benefited less from development planning and infrastructure provision. Using questionnaire survey and focus group discussions, this study explored the environmental anxieties of households in the metropolis. A stratified sample of residential areas of the city was employed, and the study is able to examine city-wide disparities. The results indicate that problems of water supply are the concern of all groups. Sanitation and garbage disposal services are problems faced mainly by the poor in low-income areas. Other problems faced by the poor are overcrowding, indoor air pollution and pest infestation, but these problems are not highlighted by the poor reflecting a misplaced lack of concern for these problem areas and ignorance of the health risks posed by these hazards. The finding suggests a considerable demand for improvements in environmental service provision and a general willingness to pay for such improvements.

Investigation of hydrochemical characteristics of groundwater from the Cretaceous-Eocene limestone aquifer in southern Ghana and southern Togo using hierarchical cluster analysis

The most relevant controls on the water quality within the Cretaceous-Eocene limestone aquifer of the Keta Basin, Ghana, and the coastal sedimentary basin of Togo were assessed using Q-mode hierarchical cluster analysis (HCA) and mass-balance modelling. The pattern recognition technique of HCA was employed for partitioning hydrochemical data from a total of 65 surface and borehole samples from the study area into water groups. A spatial plot of the water groups consisting of samples from the limestone aquifer shows that the vast majority of samples belonging to the same group are located in close proximity to one another, suggesting the same processes and/or flow paths in the limestone aquifer system. Geochemical reaction models of selected water groups were constructed using PHREEQC-2. The hydrochemical compositions of the water groups and the mass-balance calculations indicate that the dominant processes and reactions responsible for the hydrochemical evolution in the system are: (1) carbonate equilibria, (2) silicate weathering reactions, (3) limited mixing with saline water, and (4) ion exchange. The combined use of HCA and mass-balance modelling has shown to be a useful approach in interpreting groundwater hydrochemistry in an area where large uncertainties exist in the understanding of the groundwater flow system.     

Understanding land-use/cover change process for land and environmental resources use management policy in Ghana

Accurate information on land-use/cover change is a critical input for natural resource use management policy decisions. In Ghana, however, land-use/cover change is premised on the assumption that there has been a historically simple, linear, and uniform degradation of vegetation across all landscapes. The Kintampo and neighboring districts have become a subject of intense debate as to the real nature of prevailing land cover changes .It is commonly assumed that there is ubiquitously progressive irreversible woody vegetation loss across the area. The paper reports on the process and amount of land-use/cover changes that have prevailed in specific localities across the area within a 10-year period. It is hoped this will improve understanding and management of land-use/cover change in Ghana. Remote sensing and Geographic information systems technologies were used for the investigation. A multi-site satellite imagery approach was adopted to ensure that inductive inferences could be made. The outcome of the study indicated that, in space and time, there have been significant land-use/cover changes. Variability in change was a constant, rather than occasional feature across these human dominated landscapes. The conversion and transformation processes indicated that the traditional land-use strategies are self-sustaining. Any effective land-use/cover management strategy should be built upon the existing traditional farming system knowledge and practices.