Suitability Evaluation of Pedons from Some Agricultural Communities on the Niger River Flood Plains in Bayelsa State, Nigeria

Achimota A. Dickson, B. Udom, P.T. Ogboin
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Abstract

Farmers under modern agriculture are expected to have direct or indirect knowledge of soil chemical and physical characteristics as well as their suitability for intended uses. This, however, is lacking in Bayelsa State, hence this study examined the potentials and limitations of some lower Niger River plain soils of southern Nigeria and their suitability for maize production. Based on landform differences, landscape segments were separated into three mapping units per location while profile pits were dug in each unit and morphologically described. Horizon differentiation guided soil sample collection followed by laboratory analysis. Silt loam dominated soil texture while Ca dominated the exchange complex but exchangeable bases concentration was generally low. Organic C, total N and available P concentrations were closely related and low which was attributed to land clearing and frequent bush burning. Excessive rainfall and inadequate length of day were the most limiting factors under climatic factors while temperature and relative humidity were highly suitable. The ELM3 and TFN3 pedons flooded each year by Nun and Forcados Rivers, respectively, were marginally suitable S3f. Texturally, ELM1, ELM2 and TFN1 were highly suitable (S1) while ELM3, TFN2 and TFN3 were moderately suitable (S2). Due to insufficient length of dry days and wetness challenges owing to excessive rainfall, all pedons were placed under actually not suitable but potentially suitable (N1) class. Improvement measures recommended included planting early in the dry spell to avoid excessive wetness and making available more dry days as well as organic matter conservation, avoiding frequent land clearing and bush burning. 
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尼日利亚巴耶尔萨州尼日尔河洪泛平原一些农业社区的基质适宜性评估
现代农业要求农民直接或间接地了解土壤的化学和物理特征及其对预期用途的适宜性。然而,巴耶尔萨州却缺乏这方面的知识,因此本研究考察了尼日利亚南部尼日尔河下游平原一些土壤的潜力和局限性及其对玉米生产的适宜性。根据地貌差异,每个地点的地貌片段被分为三个绘图单元,同时在每个单元中挖掘剖面坑并进行形态描述。地平线的划分为土壤样本的采集提供了指导,随后进行了实验室分析。壤土是主要的土壤质地,钙是主要的交换复合物,但可交换碱的浓度普遍较低。有机碳、全氮和可利用磷的浓度密切相关且较低,这归因于土地清理和频繁的灌木焚烧。在气候因素方面,降雨量过多和日照时间不足是最主要的限制因素,而温度和相对湿度则非常适宜。每年分别被努恩河和福卡多斯河淹没的 ELM3 和 TFN3 块地略微适合 S3f。从质地上看,ELM1、ELM2 和 TFN1 高度适宜 (S1),而 ELM3、TFN2 和 TFN3 中度适宜 (S2)。由于干旱日数不足以及降雨过多造成的湿度挑战,所有基质都被归入实际不适宜但潜在适宜(N1)等级。建议采取的改进措施包括在干旱期提早播种,以避免过度潮湿,增加干旱天数,以及保护有机质,避免频繁开荒和焚烧灌木。
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