克罗斯河州卡拉巴尔湿地和沿海平原土壤的比较评价

J. Akpan, E. Aki, I. A. Isong
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The mean organic carbon content in coastal plain soil was lower than wetland soil. Available phosphorus in the studied soils were high with Atimbo and Obufa Esuk coastal plain soil having a mean value of 32.10 and 32.42 mg/kg respectively, whereas those in Atimbo and Obufa Esuk wetland soils were 32.73 and 33.88 mg/kg respectively. The exchangeable calcium content obtained for both coastal and wetland soils were all below the critical limit of 5.0 cmolkg -1 . Although exchangeable magnesium content was low in both soils but wetland soils was only slightly below the critical value of 1.5cmol/kg when compared to coastal plain soil. Both wetland and coastal plain soils were below (>0.2 cmolkg -1 ) critical level of K in soils of the zone. Also, exchangeable Na in both soil were low and below 0.3 cmol/kg limit and are adequate for cultivation of arable and tree crops. ECEC in both soils were low whereas percent base saturation was high. 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引用次数: 8

摘要

对湿地土壤与滨海平原土壤的农业生产力进行了比较评价。调查在两个地区进行:克罗斯河州卡拉巴尔的Atimbo和Obufa Esuk。滨海和湿地土壤的主要粒径均为砂质。阿廷博和奥布法埃苏克滨海平原土壤的平均容重分别为1.35 g/cm 3和1.30 g/cm 3,阿廷博和奥布法埃苏克湿地土壤平均容重分别为1.33 g/cm 3和1.30 g/cm 3。湿地土壤的总孔隙度低于滨海平原土壤,而水分含量高于滨海平原土壤。除阿廷博滨海平原土壤的Ap水平外,其余土壤pH值均在5.0以下,为高酸性状态。滨海平原土壤平均有机碳含量低于湿地土壤。研究土壤速效磷含量较高,其中滨海平原土壤速效磷平均值分别为32.10和32.42 mg/kg,湿地土壤速效磷平均值分别为32.73和33.88 mg/kg。滨海和湿地土壤交换性钙含量均低于5.0 cmolkg -1的临界限值。虽然两种土壤的交换性镁含量均较低,但湿地土壤的交换性镁含量仅略低于1.5 5cmol/kg的临界值。湿地和滨海平原土壤钾含量均低于临界水平(>0.2 cmolkg -1)。两种土壤的交换性钠含量均低于0.3 cmol/kg,适宜种植耕地和林木作物。两种土壤的ECEC均较低,而碱基饱和度百分比较高。Atimbo和Obufa Esuk沿海平原土壤的平均C:N比值分别为11.45和15.48。相比之下,Atimbo和Obufa Esuk湿地土壤的C:N比值略高,平均值分别为16.39和18.14。这也反映了由于土壤的厌氧条件,分解率很低。两种土壤Mg:K比值均较低。湿地土壤Ca:Mg比值高于生产性土壤3:1 ~ 5:1的正常范围,滨海平原土壤Ca:Mg比值较低。湿地与滨海平原土壤样品的粉砂含量、水分含量、交换性钠含量差异显著(p<0.05)。研究结果表明,滨海平原土壤的肥力状态已经丧失,主要表现为低有机碳、低全氮、低交换阳离子、高酸度和低含水量;因此,有必要利用湿地土壤提高作物生产力。湿地土壤可用于水稻、油棕、椰子、车前草、菠萝和甘蔗的种植,合理施用石灰和氮肥、钾肥,因为这些作物在酸性条件下表现良好。关键词:湿地土壤,滨海平原土壤,土壤肥力,土壤性质
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparative assessment of wetland and coastal plain soils in Calabar, Cross River State
The comparative assessment of wetland and coastal plain soils for agricultural productivity were studied. The investigation was carried out in two areas: Atimbo and Obufa Esuk in Calabar, Cross River State. The dominant particle size in both coastal and wetland soil was sandy texture. The mean bulk density values of 1.35 g/cm 3 and 1.30 g/cm 3 were obtained for Atimbo and Obufa Esuk coastal plain soil while 1.33 g/cm 3 and 1.30 g/cm 3 were obtained for Atimbo and Obufa Esuk wetland soil respectively. Total porosity in wetland soils was lower than coastal plain soil whereas moisture content in wetland soil was higher than coastal plain soil. Except Ap horizon in Atimbo coastal plain soil, the pH observed for the studied soils were all below pH of 5.0 unit which signifies high acidic condition. The mean organic carbon content in coastal plain soil was lower than wetland soil. Available phosphorus in the studied soils were high with Atimbo and Obufa Esuk coastal plain soil having a mean value of 32.10 and 32.42 mg/kg respectively, whereas those in Atimbo and Obufa Esuk wetland soils were 32.73 and 33.88 mg/kg respectively. The exchangeable calcium content obtained for both coastal and wetland soils were all below the critical limit of 5.0 cmolkg -1 . Although exchangeable magnesium content was low in both soils but wetland soils was only slightly below the critical value of 1.5cmol/kg when compared to coastal plain soil. Both wetland and coastal plain soils were below (>0.2 cmolkg -1 ) critical level of K in soils of the zone. Also, exchangeable Na in both soil were low and below 0.3 cmol/kg limit and are adequate for cultivation of arable and tree crops. ECEC in both soils were low whereas percent base saturation was high. The mean C:N ratio in Atimbo and Obufa Esuk coastal plain soil were 11.45 and 15.48 respectively. Comparatively, the C:N ratio in Atimbo and Obufa Esuk wetland soils was slightly higher having a mean value of 16.39 and 18.14 respectively. This also reflect low rate of decomposition because of anaerobic condition of the soil. The Mg:K ratio were low in both soils. The Ca:Mg ratio values were high in wetland soil when compared with a normal range of 3:1-5:1 for productive soils and was low for coastal plain soil. Per cent silt content, moisture content, and exchangeable sodium of soil sample analyzed from wetland and coastal plain soil in Atimbo were significantly different (p<0.05). The result of the studied soils indicated that coastal plain soil is already losing its fertility status as typified by low values of organic carbon, total nitrogen, Exchangeable cations and high acidity couple with low moisture content; hence there is need to harnessed wetland soil for crop productivity. Wetland soils could be exploited for the cultivation of rice, oil palm, coconut, plantain, pineapple and sugar cane with judicious application of lime, and N and K fertilizers since these crops can perform well under acidic condition. Keywords: Wetland soil, coastal plain soil, soil fertility, soil properties
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