Octa Journal of Environmental Research International Peer-Reviewed Journal
Oct. Jour. Env. Res. Vol. 1(1):48-51
Available online http://www.sciencebeingjournal.com January - March, 2013
Octa Journal of Environmental Research
ISSN: 2321-3655
Research Article ADOPTABLE TECHNIQUE(S) FOR MANAGING GHANAIAN SALINE SOILS
Akwasi Asamoaha, Charles Antwi-Boasiakoa, Kwasi Frimpong-Mensahc and Dohan Mariam Somac a,b,cFaculty of Renewable Natural Resources, Kwame Nkrumah University of Sci. & Tech. Kumasi, Ghana
dInstitut de l’Environnement et de Recherches Agricoles, Ouagaduoguo, Burkina Faso
*Corresponding author’s Email: asamoah38@yahoo.com
Received: 15th Feb 2013 Revised: 5th March 2013 Accepted: 12th March 2013
Abstract: Salinization of Ghanaian soils is on the rise. Organic matter application has not proved an effective and feasible technique for curbing this rise. Hence this paper seeks to review techniques that Ghana is using to manage its saline soils and further recommend a feasible, cost effective and beneficial technique for exhaustive research and possible adoption in the future. Halophytes appear to be the most feasible, cost effective and beneficial technique which could be adopted for the effective management of Ghanaian saline soils. But where halophytes are exotic, care must be taken to avoid competition with native species and allow preservation of agro-biodiversity.
Keywords: Halophytes, Organic matter, Salinity, Salinization,
Postal Address: P. O Box 2770, Kumasi, Ghana Phone: 00233-244605483
INTRODUCTION
Ghana’s agriculture goes as far back as the 10th century when the first settlers from the old Mali Empire made entry (Stride and Ifeke, 1971) and now accounts for 33% of GDP (CIA World Fact book, 2011). Ghana with a total area of 23.8 million ha has only 13.6 million ha of arable land which is mostly rain-fed (Adiku et al., 1997) of which only 5.3 million ha is cultivated to produce sufficient food even at an annual population growth rate of 2.6% (FAO, 2000). With a growth in GDP of 5.2% in 2004 to 11.9% in 2008, agriculture’s contribution to GDP is also expected to grow with it. Increased agriculture contribution cannot be realized without a conscious effort to grow crops year round. Year-round agricultural production is only achievable through increased irrigation. Nonetheless, irrigation is normally the major cause of salinization of soils (Rietz and Haynes, 2003). The more irrigation extends the more salinity of soils significantly alters (González-Núñez et al., 2004 and Siadat, 1998). Therefore, it does not come as a surprise that from 1989 (Szabolcs in Choukr-Allah, 2004) to 2000 (FAO in Geressu and Gezaghegne, 2008), there has been an increase in the expanse of Ghanaian saline soils from 318,000ha to 790,000ha. This indicates that the techniques that Ghana is using for managing its saline soils are not very effective. Thus, the need to survey technique(s) that Ghana is using widely to manage its saline soils. Hence this paper seeks to survey technique(s) that Ghana is using widely to manage its saline soils and further recommend a most feasible, cost effective and beneficial technique for exploration and possible adoption in the future.
MATERIALS AND METHODS
Asamoah et al 2013, Adoptable Technique(S) for Managing Ghanaian Saline Soils
Oct. Jour. Env. Res. Vol 1(1): 48-51
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Saline Areas of Ghana: Majority of Ghana’s saline soils occurs within the Coastal Savanna Agro-Ecological Zone of the southeastern corner. In this zone lies the coastal scrub, savannah and mangrove swamp of the Lower Volta Basin in the Greater Accra and Volta Regions within Accra-Ho-Keta Plains. Soils in these areas are highly salty, intolerable to crops, hydromorphic, heavy textured and poor in nutrients. Impenetrable sodium-saturated pan occurs in some of these soils (Agawtaw series) on the uplands. With only 760 mm of unreliable annual rainfall and high potential evapo-transpiration, there is a high water-salt imbalance in the Plains (FAO, 2000).
Natural Sources of Salinity in Ghanaian Soils: Salinity of Ghanaian soils basically originates from the seas, native rocks or artesian waters. On the coasts of Ghana, the process of evaporation could bring saline ground water from shallow water tables to the surface by capillary movement, leading to strong soil salinization. High and constant temperatures, low relative humidity and constant high wind velocity of the Plains are important factors in promoting upward salt movement into the exploitable volume of soils. Soils have become saline mostly because of seawater intrusion and inundation on low-lying tidal flats and flood Plains or from soils sprays blown overland from lagoons. Weathering of native rocks containing sodium minerals such as feldspars and amphiboles produces soluble sodium salts of carbonates, bicarbonates, sulfates, silicates and chlorides (FAO, 2000 and Aubert, 1983).
Characteristics of Ghanaian Saline Soils: 200,000ha and 118,000ha of Ghana’s soils are Solonchaks and Alkaline respectively (Szabolcs, 1989) while 70, 000 ha and 600, 000 ha are Arenosols and Solonetzs respectively (FAO, 2000). Solonchaks (marine-originating) show decreasing salinity with depth; extend steadily outwards from sea and may show a weakly developed salt crust or a horizon of pseudo-sand (very fine aggregate of saline-alkali clay) five to six centimeters thick on the surface.
Solonchaks have cations of sodium or calcium-magnesium complex in combination with anions of chlorine or sulfur (Aubert, 1983).
Plate 1: A map of particularly saline areas of Ghana.
Techniques in Use for Managing Saline Soils in Ghana: To identify technique(s) that Ghana is using to manage its saline soils, questionnaires were administered to one hundred rain-fed co-operatives-belonging small-scale multiple-crop local farmers from Anloga, Keta, Adina and Adidome (plate 1) along the coast in June 2008.
RESULTS AND DISCUSSION
Other W manage crops; le grown fie 2004). Techniq Ghana, soils mu immense timber, p saline so at delive 1985; O 2004). CONCL Though not been readily a has bee would b effective site and adoption (aggress essentia REFERE AAdiku, S se G Aronson, U Aubert, G
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