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John laing, mass media and misisi areas


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3.8waste disposal practices


There are two essential elements in the protection of groundwater, which include (i) strict regulation of human activity in the recharge zones, and (ii) Improvement and modernisation of solid waste and various systems of sewage accumulation facilities. In this regard, there are three important reasons for the significance of the underlying geology in areas like Lusaka to assure the provision of good quality water in quantities that can sustain human life and enhance development:

  1. Wastes are generated as a consequence of the use of earth materials. Thus, it is important to understand the properties of these materials, both individually and in combinations.

  2. Wastes and contaminants occur in, and travel through the geologic environment. Therefore, it is imperative that the nature of this environment, the transport process, and the potential for the dispersion of contaminants in this environment are understood.

  3. Most waste management schemes involve the use of geologic reservoirs for containment, or the use of geologic processes for dilution and dispersion of waste materials.

However, the manner in which both solid and liquid wastes are managed in the city is very unsatisfactory considering the interconnections of voids in the underlying rocks particularly with regard to groundwater contamination.

3.8.1Disposal of sewage and wastewater


Of the estimated two million inhabitants of Lusaka, about 25% are serviced by a sewer system, about 20% by septic tanks, while 55% rely on pit latrines to dispose of their sewage and waste water. The 55% consist of high-density residential townships that have generally developed in close proximity to areas of natural groundwater discharge or springs, where the groundwater table is very high (Fig. 17). Construction of pit latrines (Fig. 18) in areas with such a high water table implies that these structures are flooded during the rainy season. These excavations usually intersect the water table at depths of only two to three metres below ground surface in the dry season. Since they are excavated along solution features in the marbles, which are also conveyance lines for recharge to the groundwater store, they pose great risk of contaminating groundwater resources.

Further, because of a rapidly growing population, even the waterborne sewerage system initially designed for a population of about 300,000 inhabitants, is currently forced to cope with numbers in excess of 600,000 (Nkhuwa, 1996). Consequently, the system is overloaded, resulting in occasional spillage of sewage on the ground surface.

Since most of this spillage occurs over the vulnerable and differentially dissolved marble terrain, it has the likely consequence of percolating quickly down to the water table, thereby posing more threats of contamination to groundwater resources.

Figure 17: The shallow water table situation in Misisi compound


Fig. 18: The (inappropriate) siting and construction of pit latrines in Misisi Compound


3.8.2Disposal of Solid Waste


It is currently estimated that 800,000 Kg of solid waste are generated in Lusaka per day. According to source of generation (ECZ/LCC, 1997), there are three main categories of waste generated in Lusaka are shown in Table 5 below.

Table 5: Forms of waste produced in Lusaka on the basis of source of generation



TYPE OF WASTE

SOURCE OF GENERATION

Domestic

Households in residential areas

Trade and Industry

Hotels, Restaurants, Markets, Processing commercial and Industrial Plants, Public Institutions, etc.

Other

Clinics, Hospitals, other hazardous chemical-based industries, used oils, old motor vehicle bodies, etc.

Source: ECZ/LCC Report (1997)

An indication of some types of waste produced by about 130 industries located in the heavy industrial area along Buyantanshi and Mungwi Roads is given in Table 6.

Table 6: Types of industrial activities, wastes produced and potential pollutants generated

Type of industrial Activity

Potential pollutant

Tannery and leather shoe manufacturers.

Chromium, phenols, heavy metals, biological waste, sulphides

Drug manufacturers/suppliers

Drugs

Paint manufacturers

Petroleum products

Detergent manufacturers

Acids and bases

Fertiliser, pesticides and herbicide suppliers/ manufacturers

Phosphates, nitrates & other organic compounds

Food, dairy and tobacco processing

Organic wastes, inorganic acids, detergents

Timber products

Saw dust, paint, solvents, petroleum products, etc.

Refrigerant dealers and plastic manufacturers

Halogen hydrogen compounds

Chemical and cleaning agencies

Inorganic acids and organic compounds

Drink manufacturers (alcoholic and non—alcoholic)

Organic wastes and bases

Source: Gibb (Eastern Africa Limited) Report (1999)

However, only about 10 % of the generated wastes are freighted to ‘designated’ dumpsites each day, with the larger part of the remaining waste being randomly dumped into unofficial sites scattered over the city. Most of these sites are sinkholes and surface depressions, which have formed by either ground collapse or mining activities of in-filling laterite or outright mining of marbles for construction purposes. Even the now abandoned official dumpsite at Libala utilised such dugout solution conduits (Fig. 19). As such, it comprised numerous scattered excavations into which all forms of waste were dumped, and which usually filled-up with water during the rainy season. With the envisaged subterranean channel-network in the marbles underlying these sites, there is little control, if at all, for outward migration of leachate (or wash-outs) from the waste-bedrock boundary into the underlying strata. As water levels in the city aquifer are quite shallow (from about 2 to 13 metres below ground surface) and generally unprotected, leachate from these waste-dumps has the likelihood of finding unhindered and un-attenuated access to the groundwater store (Fig. 20), thereby posing great threats of groundwater contamination.



Fig. 19: Excavations that have been used for the disposal of waste at the Libala dumpsite




A

B

Fig. 20: (A) Water pond at the abandoned Libala dumpsite and (B) a Schematic model of leachate migration at the waste-bedrock boundary into the underlying strata.

Since the site was licensed by the Environmental Council of Zambia (ECZ) in 1993 as a temporal site until its closure in February 2001, the Libala dumpsite utilised to tip all types of waste without exception as indicated in Fig. 21.

Since the water table in the area is only about 3 – 15 metres below ground surface there is little doubt that water in these boreholes is also chemically impaired considering that cones of depression created by pumping are capable of tapping leachate as recharge at the edges of these cones of depression. The presence of highly permeable coarse gravels overlying this area exacerbates the problem of contamination in that they have the capacity to permit unhindered access of contaminants to the groundwater store.

In this regard, there is need for quality monitoring of boreholes in the vicinity of the dumpsite, which must generate comprehensive data that will show whether or not the tipping site has had any impact on the quality of groundwater and the severity of this impact.



Industrial waste

Industrial waste



Clinical/Hospital waste

Industrial waste


Clinical/Hospital waste



Industrial waste

Fig. 21: Examples of types of waste dumped at the Libala site (showing mainly industrial and clinical/hospital waste)


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