Impact of Bush Burning on Chemical Properties of Some Soil in Igboora, Oyo State, Nigeria

M. Adejumobi
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Abstract

Soil is used in agriculture as an anchor and primary nutrient base for plants, and the types of soil and available moisture determine the species of plants that can be cultivated. Bush burning, whether as result of a wildfire or a controlled burning, affects not only the appearance of the landscape, but the quality of the soil. Bush burning method of land clearing is a traditional farming system used as a means of land clearing for crop production. This method of land clearing has both beneficial and detrimental effects on soil physical and chemical properties. Therefore, this study investigated the effects of bush burning on soil chemical properties at different soil depth of 0-30 cm and 30-60 cm respectively base on the rooting depth of crop planted. The experiment was carried out in six selected farms in Igboora, Ibarapa central Local Governmental, Oyo State. The soil sampled were collected from burnt and unburnt experimental soil and analyzed using USDA standard methods for soil analysis for the selected chemical characteristics (pH, Ca2+, Mg2+ Na+. TN and P). Two samples were taken from each burnt and un-burnt locations at depth of 0-30 and 30-60 cm. Paired t-test was used to compare means value of soil chemical properties determined from burnt and un-burnt soil. ANOVA was used for significance difference between soil from burnt and un-burnt soil. pH increased from moderately acidic to slightly acidic, phosphorus content of the soil increased greatly from un-burnt soil to burnt soil at 0-30 cm and 30-60 cm depths from 6.64 to 22.21 ppm and 3.53 to 24.95 ppm, respectively. Similarly, potassium increased from 0.27 to 0.40ppm at 0-30cm depth but decreased from 0.23 to 0.17 ppm at 30-60 cm depth. Nitrogen reduced at both depths from 0.80 to 0.76% and 0.72 to 0.68% respectively. Magnesium also increased from 1.3 cmol/kg to 2.00 cmol/kg and 1.65 to 1.75 cmol/kg at both 0-30 cm and 30-60 cm depth respectively. Whereas calcium showed a reduction from 3.17 to 2.85 cmol/kg and 1.65 to 1.45 cmol/kg at both depths. The variations observed between burnt and un-burnt soil for Ca, Mg, exchangeable acidity, pH, Nitrogen, potassium was significant at p<0.05 probability level. This indicates that bush burning has an impact on soil physical and chemical properties which may affect the suitability of the soil for crop production. Based on this, there is need for environmental education for farmers in the area in order to know the implications of bush burning on soil properties for soil sustainability which will boost food production.
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森林燃烧对尼日利亚奥约州伊博拉部分土壤化学性质的影响
土壤在农业中被用作植物的锚和主要营养基础,土壤的类型和有效水分决定了可以种植的植物的种类。灌木燃烧,无论是由于野火还是控制燃烧,不仅影响景观的外观,而且影响土壤的质量。灌木焚烧清理土地的方法是一种传统的农业系统,用于农作物生产的土地清理手段。这种土地清理方法对土壤的物理和化学性质既有有益的影响,也有有害的影响。因此,本研究以种植作物的生根深度为基础,研究了灌木焚烧对土壤化学性质的影响,土壤深度分别为0 ~ 30 cm和30 ~ 60 cm。试验在奥约州伊巴拉帕中央地方政府伊格博拉的六个选定农场进行。从燃烧和未燃烧的实验土壤中收集土壤样本,使用美国农业部土壤分析标准方法分析选定的化学特征(pH, Ca2+, Mg2+ Na+)。在0-30 cm和30-60 cm深度的烧伤和未烧伤部位各取2个样品。采用配对t检验比较烧焦土壤与未烧焦土壤化学性质平均值。用方差分析分析了燃烧土壤与未燃烧土壤的显著性差异。土壤pH值由中酸性向微酸性增加,0 ~ 30 cm和30 ~ 60 cm深度未燃土到燃土的磷含量分别从6.64 ~ 22.21 ppm和3.53 ~ 24.95 ppm显著增加。同样,钾在0-30cm深度从0.27 ppm增加到0.40ppm,但在30-60 cm深度从0.23 ppm下降到0.17 ppm。两个深度的氮含量分别从0.80降低到0.76%和0.72降低到0.68%。在0 ~ 30 cm和30 ~ 60 cm深度,镁含量分别从1.3 cmol/kg和1.65 cmol/kg增加到2.00 cmol/kg和1.75 cmol/kg。而钙则从3.17 cmol/kg降至2.85 cmol/kg,从1.65 cmol/kg降至1.45 cmol/kg。土壤中Ca、Mg、交换性酸度、pH、氮、钾在p<0.05概率水平上差异显著。这表明,丛林燃烧对土壤的物理和化学性质有影响,可能会影响土壤对作物生产的适宜性。基于此,有必要对该地区的农民进行环境教育,以了解丛林焚烧对土壤特性的影响,从而促进土壤的可持续性,从而促进粮食生产。
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