Nutrient Assessment of Rain-Fed Lowland and Upland Rice Production Systems in Okigwe, South-Eastern Nigeria

Ifeoma Monica Nwawuike
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Abstract

The study was carried out to assess the nutrient status of the two major rice production systems (rain-fed lowland and upland) and the relationship among the nutrient contents of the soil in Okigwe area of Imo State, Nigeria. Soil samples from 15 cm depth were collected from 10 farms in the area: 5 farms from rain-fed lowland and 5 from upland rice production system. The soil samples were prepared and analyzed for macro and micro nutrients together with the particle size distribution. The results from the nutrient concentration in both rain-fed lowland and upland soils showed that pH favoured conditions for more availability of nutrients as seen in upland soils. The t-test results indicates a significant variation in % Clay (0.01*), % TS (0.008**), pH (0.0005**), TN (0.038*), available P (0.01*), Exchangeable Ca (0.03*) and Extractable B (0.02*). Correlation results showed TN as the major determinant of the other soil nutrients in both rain-fed lowland and upland rice production systems. In rain-fed lowland production system, TN correlated negatively and strongly with % TS (-0.81) and Cu (-0.70) with a weak negative association with Na (-0.57), K (-0.55), Mg (-0.50), available P (-0.57) and Fe (-0.64). In the upland rice production system, TN also had a negative association with many soil nutrients though some were weakly correlated while some were of strong association. They include Ca (-0.93), Mg (-0.65), Cu (-0.86), Mn (-0.69) and Zn (-0.76) with a positive association with Na (0.83) and pH (0.69). Despite TN being perceived as the major determinant of nutrients, OM in upland soils had a more positive association with other nutrients compared to that in the lowland soils. Hence, any management practices which will enhance nutrient status should be encouraged to help boost and sustain rice yield in both rain-fed lowland and upland rice production systems.
尼日利亚东南部奥基圭雨水灌溉低地和高地水稻生产系统的养分评估
本研究旨在评估尼日利亚伊莫州奥基圭地区两种主要水稻生产系统(雨水灌溉低地和高地)的养分状况以及土壤养分含量之间的关系。从该地区的 10 个农场采集了 15 厘米深的土壤样本:其中 5 个来自雨水灌溉的低地农场,5 个来自高地水稻生产系统。土壤样本经制备后,进行了宏观和微观养分以及粒度分布分析。雨水灌溉的低地和高地土壤养分浓度结果显示,高地土壤的 pH 值有利于养分的更多利用。t 检验结果表明,粘土% (0.01*)、TS% (0.008**)、pH 值 (0.0005**)、TN 值 (0.038*)、可利用 P 值 (0.01*)、可交换 Ca 值 (0.03*) 和可提取 B 值 (0.02*) 均存在显著差异。相关结果表明,在雨水灌溉的低地和高地水稻生产系统中,TN 是决定其他土壤养分的主要因素。在雨养低洼地生产系统中,TN 与 TS%(-0.81)和 Cu(-0.70)呈强烈负相关,与 Na(-0.57)、K(-0.55)、Mg(-0.50)、可利用 P(-0.57)和 Fe(-0.64)呈微弱负相关。在高地水稻生产系统中,TN 也与许多土壤养分呈负相关,但有些呈弱相关,有些呈强相关。其中包括钙(-0.93)、镁(-0.65)、铜(-0.86)、锰(-0.69)和锌(-0.76),与钠(0.83)和 pH 值(0.69)呈正相关。尽管 TN 被认为是养分的主要决定因素,但与低地土壤相比,高地土壤中的 OM 与其他养分的正相关性更大。因此,在雨水灌溉的低地和高地水稻生产系统中,应鼓励任何能提高养分状况的管理措施,以帮助提高和维持水稻产量。
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