香蕉饼生产中的可持续增值作为减少香蕉废料的替代方法

Ajoagu G. M., Ukabiala M. E., Asadu C. LA., Umeugokwe P. C.
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摘要

本研究旨在对尼日利亚阿南布拉州 Njikoka 地区的土壤进行特征描述和分类。研究选取了三个不同社区的三个地形区(TA、TB 和 TC):利用数字高程模型(DEM)将其分为上坡(US)、中坡(MS)和下坡(LS)。根据联合国粮农组织的指导原则,对九个基质进行了描述,并采集了 64 个样本进行分析。土壤排水良好,主要为深红褐色和红褐色地层。土壤结构从弱细粒结构到中等角状和次角状块状结构不等,而质地则因沙子、淤泥和粘土成分的变化而不同。土壤酸度从极酸到微酸不等。有机质、总氮、可利用磷和可交换碱的含量一般较低至很低。钾含量从很低到中等不等,而可交换酸度、碱饱和度和阳离子交换容量(CEC)则从很低到很高不等。化学肥力的趋势是 TA 土壤 MS > US > LS,TB 土壤 US > MS > LS,TC 土壤 LS > MS > US。根据美国农业部的土壤分类,TA 土壤被确定为典型合生土(US)、典型坎地合生土(MS)和水生竞技合生土(LS)。TB 土壤被归类为 Grossarenic Kandiudualf(US)和 Typic Kandiudults(MS 和 LS),而 TC 土壤被归类为 Vertic Hapludults(US)、Grossarenic Hapludults(MS)和 Grossarenic Kandiudults(LS)。
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Sustainable Value Addition in Banana Cake Production as Alternative To Reduce Banana Waste
The study aimed to characterize and classify soils in the Njikoka Area of Anambra State, Nigeria. Three toposequences (TA, TB, and TC) from three different communities: Abagana, Nimo and Enugu-ukwu were selected and divided into upper (US), middle (MS), and lower (LS) slopes using a Digital Elevation Model (DEM). Nine pedons were described following FAO guidelines, and 64 samples were collected for analysis. The soils were well-drained, with predominant dark reddish brown and reddish brown horizons. Soil structure varied from weak fine granular to moderately medium angular and subangular blocky structures, while texture varied due to variations in sand, silt, and clay fractions. Soil acidity ranged from extremely acidic to slightly acidic. Organic matter, total nitrogen, available phosphorus, and exchangeable bases were generally low to very low. Potassium content ranged from very low to moderate, while exchangeable acidity, base saturation, and cation exchange capacity (CEC) varied from very low to high. The trend in chemical fertility was MS > US > LS for TA, US > MS > LS for TB, and LS > MS > US for TC soils. Based on the USDA soil classification, TA soils were identified as Typic Hapludults (US), Typic Kandiudults (MS), and Aquic Arenic Hapludults (LS). TB soils were classified as Grossarenic Kandiudualf (US) and Typic Kandiudults (MS and LS), while TC soils were categorized as Vertic Hapludults (US), Grossarenic Hapludults (MS), and Grossarenic Kandiudults (LS).
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