尼日利亚热带稀树草原连续灌溉条件下土壤特性的变异

S. Yakubu, I. A. Jaiyeoba, M. Gasu, D. A. Yakubu
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摘要

本研究考察了尼日利亚热带稀树草原连续耕作条件下土壤性质的变异性。在旱季(DS)和雨季(WS)分别采集了8块灌溉农田和1块荒地的土壤样品。分析了沙土、粉土、粘土、容重、孔隙度、含水量、pH、有机质、全氮、速效磷、交换性阳离子(Ca、Mg、K、Na)、交换性酸度(H+Al)、交换性阳离子交换容量(ECEC)和碱饱和度等土壤肥力关键参数。土壤性质的百分比等值值是通过将WS中每种土壤性质的平均值表示为DS中相同性质的平均值的百分比来计算的。结果表明,两季土壤质地等级均为壤土。WS和DS期间表层土的平均值为:砂泥岩(51.38%和50.38),(38.63%和39.63),粘土(10%),体积密度(1.38和1.42),孔隙度(64.04%和47.75),水分含量(0.26 & 0.19立方厘米),pH值(5.7和6.03),有机物(0.62%和1.62),总N(0.08%和0.12),有效磷(58.36 & 48.25 mgkg-1)、阳离子(Ca (7.76 & 6.17 cmol /公斤),Mg (1.48 & 1.15 cmol /公斤)、K (0.36 & 0.21 cmol /公斤),和Na (0.61 & 0.25 cmol /公斤)],H +基地(0.59 & 0.50 cmol /公斤),ECEC (10.63 & 8.26 cmol /公斤)和基本饱和(92%和93)。这些结果表明,土地利用对土壤性质的变异既有直接影响,也有间接影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variability of Soil Properties under Continuous Irrigation Farming in Nigerian Savanna
This study examined variability of soil properties under continuous cultivation in the Nigerian Savanna. Bulked soil samples were collected from eight irrigated farm plots and one uncultivated field during both wet season (WS) and dry season (DS) respectively. The samples were analyzed for Sand, silt, clay, bulk density, porosity, moisture content, pH, organic matter, total nitrogen, available phosphorus, exchangeable cations (Ca, Mg, K, and Na), exchangeable acidity (H+Al), exchangeable cation exchange capacity (ECEC) and base saturation which are the key soil fertility parameters. Percentage equivalence value of soil property was computed by expressing the mean value of each soil property in WS as a percentage of the mean value of the same property over the DS. From the results, the soil textural grades remained loamy in both seasons. The mean values obtained at topsoil during WS and DS are: sand (50.38 & 51.38%), silt (39.63 & 38.63%), clay (10% each), bulk density (1.38 & 1.42), porosity (47.75 & 64.04%), moisture content (0.26 & 0.19cm3 ), pH (5.7 & 6.03), organic matter (1.62 & 0.62%), total N (0.12 & 0.08%), available phosphorus (58.36 & 48.25mgkg-1), cations [Ca (7.76 & 6.17cmol/ kg-1), Mg (1.48 & 1.15cmol/kg-1), K (0.36 & 0.21cmol/kg-1), and Na (0.61 & 0.25cmol/kg-1)], H+Al (0.59 & 0.50cmol/kg-1), ECEC (10.63 & 8.26cmol/kg-1) and base saturation (93 & 92%). These results suggest that land use has both direct and indirect effects on the variability of soil properties.
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