Humic substances in soils of diverse parent materials in humid tropical environment of south east nigeria.

S. M Afu, D. M Olim, L. O Nwamuo, A. I Akpama, M. E Aaron
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Abstract

The knowledge of humic substances of soil is essential for soil fertility management and productivity. The study evaluated the humic substances (HS) and physicochemical properties of soils of different lithologies. Twenty composite soil samples were collected at the depths of 0-15 and 15-30 cm in both upland and inland of sandstone (SS), limestone (LS), mudstone (MS), basement complex (BC) and shale (SH) and analyzed for HS and physicochemical properties. HS were higher in surface than subsurface soils and in SH, SS and MS than other parent materials. Humic acid had mean values of 0.649 and 0.683 g/kg, 0.327 and 0.055 g/kg, 0.736 and 1.167 g/kg, 0.976 and 0.839 g/kg and 0.449 and 0.411 g/kg in surface soils of upland and inland in BC, MS, SS, SH and LS. In subsurface soils, average values of humic acid were 0.322 and 0.426 g/kg, 0.055 and 0.012 g/kg, 0.499 and 0.713 g/kg, 0.656 and 0.908 g/kg and 0.276 and 0.047 g/kg in the upland and inland of BC, MS, SS, SH and LS correspondingly. Fulvic acid had averages of 0.237 and 0.3125 g/kg, 0.533 and 0.751 g/kg, 0.297 and 0.707 mg/kg, 0.6524 and 0.568 g/kg and 0.220 and 0.007 g/kg in the surface soils of upland and inland of BC, MS, SS, SH and LS. In subsurface, fulvic acid had means of 0.244 and 0.363 g/kg, 0.227 and 0.328 g/kg, 0.056 and 0.128 g/kg, 0.040 and 0.402 g/kg and 0.001 and 0.415 g/kg in upland and inland of BC, MS, SS, SH and LS respectively. BC was higher in clay content than other parent materials. ECEC correlated significantly and positively with BS, Ca, Na, pH, silt, K and Mg while fulvic and humic acids correlated positively with TN and OM. pH was strongly acidic in soils of upland and varied from medium acid to slightly acid in inland. OC was high in inland and varied from high in MS, SH and SS to low in BC and LS in upland. Available P, TN, exchangeable bases, ECEC varied from low to high while BS was high in soils of both upland and inland.    
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尼日利亚东南部潮湿热带环境中不同母质土壤中的腐殖质。
了解土壤中的腐殖质对土壤肥力管理和生产力至关重要。本研究评估了不同岩性土壤的腐殖质(HS)和理化性质。研究人员在砂岩(SS)、石灰岩(LS)、泥岩(MS)、基底复合岩(BC)和页岩(SH)的高地和内陆 0-15 厘米和 15-30 厘米深处采集了 20 个复合土壤样本,并对其进行了腐殖质和理化性质分析。地表土壤中的腐殖酸含量高于地下土壤,SH、SS 和 MS 中的腐殖酸含量高于其他母质。在 BC、MS、SS、SH 和 LS 的高地和内陆表层土壤中,腐殖酸的平均值分别为 0.649 和 0.683 克/千克、0.327 和 0.055 克/千克、0.736 和 1.167 克/千克、0.976 和 0.839 克/千克以及 0.449 和 0.411 克/千克。在亚表层土壤中,BC、MS、SS、SH 和 LS 的高地和内陆土壤中腐植酸的平均值分别为 0.322 和 0.426 克/千克、0.055 和 0.012 克/千克、0.499 和 0.713 克/千克、0.656 和 0.908 克/千克以及 0.276 和 0.047 克/千克。在 BC、MS、SS、SH 和 LS 的高地和内陆表层土壤中,富集酸的平均值分别为 0.237 和 0.3125 克/千克、0.533 和 0.751 克/千克、0.297 和 0.707 毫克/千克、0.6524 和 0.568 克/千克以及 0.220 和 0.007 克/千克。在亚表层土壤中,BC、MS、SS、SH 和 LS 的高地和内陆土壤中富里酸的平均值分别为 0.244 和 0.363 克/千克、0.227 和 0.328 克/千克、0.056 和 0.128 克/千克、0.040 和 0.402 克/千克以及 0.001 和 0.415 克/千克。BC 的粘土含量高于其他母本材料。ECEC与BS、Ca、Na、pH、淤泥、K和Mg呈显著正相关,而富集酸和腐殖酸与TN和OM呈正相关。内陆土壤的 OC 值较高,高地土壤的 OC 值从 MS、SH 和 SS 的高到 BC 和 LS 的低不等。可利用磷、氨、可交换碱、ECEC 从低到高不等,而 BS 在高地和内陆土壤中都很高。
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