Search results for: O. Faloye

Authors: Temitope Faloye

Abstract:

The absence of equity and transparency in Nigeria's economic system has resulted in unemployment. Women’s unemployment rate remains higher because women's range of jobs is often narrower due to discriminatory attitudes of employers and gender segregation in the labor market. Gender inequality is one of the strong factors of unemployment, especially in developing countries like Nigeria, where the female gender is marginalized in the labor force market. However, gender equality in terms of labor market access and employment condition has not yet been attained. Feminist theory is considered as an appropriate theory for this study. The study will use a mixed-method design, collecting qualitative and quantitative data to provide answers to the research questions. Therefore, the research study aims to investigate the present situation of gender inequality in the Nigerian labor market.

Keywords: unemployment, gender inequality, gender equality, labor market, female graduate

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Authors: Temitope Faloye

Abstract:

In today’s changing job market economy, most employers of labor want employees who are employable and possess relevant skills. Graduates need to possess generic skills due to the continually changing nature of the job market, which requires adaptive coping strategies. Most employers of labor complain that graduates are not employable, which is one of the major factors causing a high rate of graduate unemployment in Nigeria. However, the number of unemployed females is higher than that of unemployed males; hence gender difference is linked to the employability of graduates. The human capital theory is considered an appropriate theory for this study. A qualitative approach will be used to provide answers to the research questions. Therefore, the research study aims to investigate the employers’ perspective on female graduate employability in Nigeria.

Keywords: graduate employability, generic skills, graduate unemployment, gender

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Authors: S. O. Idakwo, A. T. Bolarinwa, D. L. Bish, S. I. Okonkwo, O. Faloye

Abstract:

The Cretaceous kaolinitic clay deposits of Ajali/Mamu and Enugu/Nkporo Formations from the Lower Benue Trough (LBT) of Nigeria were analyzed for their rare-earth elements and hydrogen and oxygen isotopic compositions to determine the formational history such as alteration type, origin, temperature of formation, fractionation factor as well as the precursor for the LBT clay deposits. The investigated samples are characterized by a negative Eu-anomalies, the chondrite-normalized La/Yb and Gd/Yb ratios varied in the Mamu/Ajali and Enugu Formations from 9.51 to 30.10 and 1.20 to 2.18 and 9.05 to 20.99 and 1.38 to 2.18 respectively, and LREE enriched with an almost flat HREE patterns. The δD value ranged from -66.1 to -50.80‰ for the clay samples of Mamu/Ajali Formation but -66.4 to -57.8‰ was obtained for the Enugu/Nkporo Formation The δO18 values varied between 15.8 and 21.2‰ in the clay samples of Mamu/Ajali Formation as against 15.4 to 16.7‰ in the Enugu/Nkporo samples with temperature of formation between 54 – 91°C for the two formations, suggesting that the clay samples are residual materials derived from chemical weathering (supergene origin) of felsic rock and have been deposited in a sedimentary basin (δO18 =+19 to +21.2‰), where the sediments have longer interaction with meteoric water enriched in δD and δ18O. The data also support equilibration of kaolinite with meteoric waters at surficial temperatures, evident from the values of ~1 obtained for all samples.The geochemical parameter (R~0.2) that approaches zero which proved an intensive weathering associated with the breakdown of feldspar and deposition to form kaolinite and the relationship between the concentration of LREE and Y in the clay samples revealed that they were significantly enriched during the weathering and kaolinization processes. Based on the rare earth elements and δD and δ18O values, the kaolinitic clay deposits of LBT are residual material of supergene origin derivative of felsic rock and were deposited in a sedimentary basin at a temperature < 100°C.

Keywords: LBT, kaolinitic clay, supergene, fractionation factors, origin

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