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首页> 外文期刊>Environment, development and sustainability >Fertility Status And Management Implications Of Wetland Soils For Sustainable Crop Production In Akwa Ibom State, Nigeria
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Fertility Status And Management Implications Of Wetland Soils For Sustainable Crop Production In Akwa Ibom State, Nigeria

机译:尼日利亚阿夸伊博姆州的湿地土壤肥力状况及其对可持续作物生产的影响

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摘要

Fertility status of soils of three wetland types in Akwa Ibom State, Nigeria, was investigated. The wetland types are Inland Valley (IV), Flood Plain (FP) and Mangrove (MG). The soils have silt-clay ratios above 0.15 and 0.25 indicating that they are of young parent materials with low degree of weathering and possible weatherable minerals for plant nutrition. The pH of the soils was near neutral (>6.4) when wet but extremely acid (>3.5) when dried indicating that the soils are potential acid sulphate soils. Organic matter content was high with mean values of 12.59, 6.03 and 3.20% for IV, FP and MG soils, respectively. Total N (nitrogen) was low except in IV soils where the value was above the 0.30% critical level. The C:N ratios were narrow with mean of 20.90, 12.17 and 12.12 for IV, FP and MG soils, respectively. The contents of basic cations [Calcium (Ca), Magnesium (Mg), Pota-sium (K) and Sodium (Na)] were low while acidic cations [Aluminium (Al) and Hydrogen (H)] were high. The Ca:Mg ratios were below the optimum range of 3:1 to 4:1 required for most crops. The Mg:K ratios were above 1.2, below which yields of crops like corn and soybean may be reduced. Effective cation exchange capacity (ECEC) was below the 20 cmol/kg. Percent base saturation was low (<38) indicating that the soils are potentially less fertile. Exchangeable Al and percent Al saturation were high, above 60% in IV and FP soils. Electrical conductivity was above the critical value of 2 dsm~(-1) while exchangeable sodium percentage was less than 15. Available Phosphorus (P) and low, <10 ppm and free Fe_2O_3/clay ratios were <0.15. Positive correlation existed between silt and ECEC, implying that silt contributed to nutrient status of the soils. Generally, fertility status of the soil is low and would require maintenance of adequate organic matter, application of lime and organic and inorganic fertilizers, drainage and irrigation if the land is to be used for intensive/sustainable crop production.
机译:调查了尼日利亚阿夸伊博姆州三种湿地类型土壤的肥力状况。湿地类型为内陆河谷(IV),洪泛平原(FP)和红树林(MG)。这些土壤的粉土-粘土比率高于0.15和0.25,表明它们是年轻的母体材料,风化程度低,并且可能存在耐候性矿物质以用于植物营养。湿润时土壤的pH值接近中性(> 6.4),而干燥时则是极酸性(> 3.5),表明该土壤是潜在的酸性硫酸盐土壤。 IV,FP和MG土壤有机质含量较高,平均值分别为12.59%,6.03和3.20%。总氮(氮)很低,但IV土壤的临界值高于0.30%。 IV,FP和MG土壤的C:N比很窄,分别为20.90、12.17和12.12。碱性阳离子[钙(Ca),镁(Mg),钾(K)和钠(Na)]的含量低,而酸性阳离子[铝(Al)和氢(H)]高。 Ca:Mg比值低于大多数农作物所需的3:1至4:1的最佳范围。 Mg:K比率高于1.2,低于该比率,玉米和大豆等农作物的单产可能会降低。有效阳离子交换容量(ECEC)低于20 cmol / kg。基本饱和度百分比很低(<38),表明土壤的肥沃程度可能较低。可交换的铝和铝的饱和百分比很高,在IV和FP土壤中高于60%。电导率高于2 dsm〜(-1)的临界值,而可交换的钠百分比小于15。有效磷(P)和低,<10 ppm和自由Fe_2O_3 /粘土比率<0.15。淤泥与ECEC之间存在正相关,表明淤泥有助于土壤养分状况。通常,土壤的肥力状况很低,如果要将土地用于集约/可持续的作物生产,则需要维持足够的有机质,施用石灰以及有机和无机肥料,排水和灌溉。

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