2009•West African Journal of Applied EcologyOpen access

Physico-chemical properties of three salt-affected soils in the Lower Volta Basin and management strategies for their sustainable utilization

D. F. K. Allotey, R. D. Asiamah, CD Dedzoe, AL Nyamekye

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Abstract

Differences in physical and chemical properties of three salt-affected soils, designated as pedons 1, 2 and 3, in the Lower Volta basin ofGhana were evaluated. Pedons 1 and 2 were located at Mokordzie in the South Tongu District while Pedon 3 was at Salo in the Ketu Districtof the Volta Region of Ghana. The soil properties determined included texture, pH, organic carbon, available P and K, exchangeable basesand acidity. The texture of the soils varied from clay to silty clay. The low pH of the soils, attributed to the presence of pyrite, ranged frommoderately acidic to extremely acidic and vary in the order Pedon 1 > Pedon 3 > Pedon 2. The electrical conductivity of all the three pedonswere more than 4 dS/m, thus, their rating as moderately saline. Organic C content in the A-horizon of pedons 1 and 2 were comparativelyhigher than Pedon 3. Total N contents of the three pedons was generally low. Available K, on the other hand, was very low within all thehorizons of Pedon 2; medium in Pedon 3 and ranged from very low to medium in Pedon 1. The CEC of the A-horizon of Pedon 1 is mediumbut the B-horizon is between low to high. Those of pedons 2 and 3 were between medium to very high in both horizons. The CEC is generallyin the decreasing order Pedon 1 > Pedon 2 > Pedon 3. Exchangeable sodium percentage (ESP) of all the three pedons were lower than 15,hence, the soils were rated saline. Based upon these data, pedons 1, 2, and 3 were classified as Gleyic Solonetz, Endogypsi-Gleyic Solonchakand Gleyic Solonchak, respectively. Suggested management practices to improve upon the productivity of these soils are ridges/mounds,application of lime (gypsum or oyster shells), organic manures and residues, planting of salt-tolerant crops, agroforestry, leaching anddrainage

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Differences in physical and chemical properties of three salt-affected soils, designated as pedons 1, 2 and 3, in the Lower Volta basin ofGhana were evaluated. Pedons 1 and 2 were located at Mokordzie in the South Tongu District while Pedon 3 was at Salo in the Ketu Districtof the Volta Region of Ghana. The soil properties determined included texture, pH, organic carbon, available P and K, exchangeable basesand acidity. The texture of the soils varied from clay to silty clay. The low pH of the soils, attributed to the presence of pyrite, ranged frommoderately acidic to extremely acidic and vary in the order Pedon 1 > Pedon 3 > Pedon 2. The electrical conductivity of all the three pedonswere more than 4 dS/m, thus, their rating as moderately saline. Organic C content in the A-horizon of pedons 1 and 2 were comparativelyhigher than Pedon 3. Total N contents of the three pedons was generally low. Available K, on the other hand, was very low within all thehorizons of Pedon 2; medium in Pedon 3 and ranged from very low to medium in Pedon 1. The CEC of the A-horizon of Pedon 1 is mediumbut the B-horizon is between low to high. Those of pedons 2 and 3 were between medium to very high in both horizons. The CEC is generallyin the decreasing order Pedon 1 > Pedon 2 > Pedon 3. Exchangeable sodium percentage (ESP) of all the three pedons were lower than 15,hence, the soils were rated saline. Based upon these data, pedons 1, 2, and 3 were classified as Gleyic Solonetz, Endogypsi-Gleyic Solonchakand Gleyic Solonchak, respectively. Suggested management practices to improve upon the productivity of these soils are ridges/mounds,application of lime (gypsum or oyster shells), organic manures and residues, planting of salt-tolerant crops, agroforestry, leaching anddrainage

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Available abstract

Differences in physical and chemical properties of three salt-affected soils, designated as pedons 1, 2 and 3, in the Lower Volta basin ofGhana were evaluated. Pedons 1 and 2 were located at Mokordzie in the South Tongu District while Pedon 3 was at Salo in the Ketu Districtof the Volta Region of Ghana. The soil properties determined included texture, pH, organic carbon, available P and K, exchangeable basesand acidity. The texture of the soils varied from clay to silty clay. The low pH of the soils, attributed to the presence of pyrite, ranged frommoderately acidic to extremely acidic and vary in the order Pedon 1 > Pedon 3 > Pedon 2. The electrical conductivity of all the three pedonswere more than 4 dS/m, thus, their rating as moderately saline. Organic C content in the A-horizon of pedons 1 and 2 were comparativelyhigher than Pedon 3. Total N contents of the three pedons was generally low. Available K, on the other hand, was very low within all thehorizons of Pedon 2; medium in Pedon 3 and ranged from very low to medium in Pedon 1. The CEC of the A-horizon of Pedon 1 is mediumbut the B-horizon is between low to high. Those of pedons 2 and 3 were between medium to very high in both horizons. The CEC is generallyin the decreasing order Pedon 1 > Pedon 2 > Pedon 3. Exchangeable sodium percentage (ESP) of all the three pedons were lower than 15,hence, the soils were rated saline. Based upon these data, pedons 1, 2, and 3 were classified as Gleyic Solonetz, Endogypsi-Gleyic Solonchakand Gleyic Solonchak, respectively. Suggested management practices to improve upon the productivity of these soils are ridges/mounds,application of lime (gypsum or oyster shells), organic manures and residues, planting of salt-tolerant crops, agroforestry, leaching anddrainage

Key concepts: Soil water, Soil horizon, Soil science, Total organic carbon, Horizon, Chemistry, Soil carbon, Geology

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Physico-chemical properties of three salt-affected soils in the Lower Volta Basin and management strategies for their sustainable utilization — Research Paper | ScholarLens