尼日利亚东南部湿润热带地区不同岩性土壤的性质

Afu, S. M.,, Adie, P. I.,, Olim, D. M.,, Isong, I. A.,, Akpama, A. I.,, Aaron, M. E.,
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摘要

本研究对五谷子地方行政区不同母质发育的土壤进行了性质评价。对5种不同母质上的5个剖面坑进行了挖掘、形态圈定和描述。5种母质分别为基底杂岩(BC)、泥岩(MS)、砂岩(SS)、页岩(SH)和灰岩(LS)。从形态上看,土壤较深,颜色、结构、质地和稠度各不相同。化学分析结果表明,BC、MS、SS、SH和LS土壤pH值分别为5.4、5.4、5.4、5.3和5.4。母材有机碳含量均较低(<15g/kg),而全氮含量均略高,分别为0.04 g kg-1、0.10 g kg-1、0.04 g kg-1、0.10 g kg-1、0.04 g kg-1、0.10 g kg-1和0.20 g kg-1。速效磷在各母材中均较低(<8mg/kg), SH的速效磷值略高于其他母材。在BC、MS、SS、SH和LS中,钙和钠的平均值分别为3.2 cmol/kg、3.93 cmol/kg、3.65 cmol/kg、3.3 cmol/kg、3.95 cmol/kg和0.25 cmol/kg、0.10 cmol/kg、0.08 cmol/kg、0.08 cmol/kg,分别为优势碱基和最小碱基。MS土壤的交换碱含量高于其他土壤。Al3+和H+对土壤酸度的贡献水平相同。相关分析表明,砂与粘土(-0.81)、OC(-0.41)、TN(-0.42)、Al++(-0.78)呈显著负相关,与pH(0.72)、Ca2+(0.7)、Mg2+(0.64)、K+(0.56)、ECEC(0.71)、BS(0.70)呈显著正相关。pH与交换碱、有效P值(0.83)、ECEC值(0.9)、碱饱和度(0.83)呈显著正相关。但大多数性状之间呈负相关且不显著相关。
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Properties of soils of different lithology in the humid tropics of southeastern nigeria
This study evaluated the properties of soils developed on diverse parent materials in Ogoja Local Government Area. Five profile pits on five different parent materials were dug, morphologically delineated and described. The five parent materials were basement complex (BC), mudstone (MS), sandstone (SS), shalestone (SH) and limestone (LS). Morphologically, the soils were deep with varying color, structure, texture and consistency. The results of chemical analyses revealed that the soils have acid pH with means of 5.4, 5.4, 5.4, 5.3 and 5.4 in BC, MS, SS, SH and LS. Organic carbon was low (<15g/kg) across the parent materials while total N was slightly higher in MS, SS and LS with means of 0.04 g kg-1, 0.10 g kg-1, 0.04 g kg-1, 0.10 g kg-1  and 0.20 g kg-1  in BC, MS, SS, SH and LS accordingly. Available P was low (<8mg/kg) across the parent materials with slightly higher value recorded in SH than in other parent materials. Calcium and sodium were the dominant and the least bases respectively with mean values of 3.2 cmol/kg, 3.93 cmol/kg, 3.65 cmol/kg, 3.3 cmol/kg and 3.95 cmol/kg and 0.25 cmol/kg, 0.10 cmol/kg, 0.08 cmol/kg, 0.08 cmol/kg, 0.08 cmol/kg in BC, MS, SS, SH and LS respectively. Exchangeable bases were higher in MS than other soils. Both Al3+ and H+ contributed at the same level to acidity of the soils. Correlation analysis showed that sand correlated negatively and significantly with clay (-0.81), OC (-0.41), TN (-0.42), and Al+++ (-0.78) and positively and significantly with pH (0.72), Ca2+ (0.7), Mg2+ (0.64), K+ (0.56), ECEC (0.71) and BS (0.70).  Correlation between pH and exchangeable bases, available P (0.83), ECEC (0.9) and base saturation (0.83) was significant and positive.  However, most properties had negative and non-significant correlation with each other.
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