坦桑尼亚首都城区典型土壤的土壤学特征:土壤形态、理化性质、分类和土壤肥力趋势

B. Msanya, T. Mwasyika, N. Amuri, E. Semu, L. Mhoro
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引用次数: 7

摘要

在坦桑尼亚首都多马地区进行了土壤学表征。描述了花岗岩原位风化发育的3个土壤剖面,分别为HIS-P1、HISP2和HIS-P3。从遗传层取了15个样品,分析了物理和化学特征。土壤一般都很深,质地各异。HIS-P2剖面以壤土型为主,而HIS-P1和HIS-P3剖面均为粘土型,但后者为重粘土型。在HIS-P1剖面中,粘土淋溶-照亮作用是主要的成土过程,表现为在底土中存在粘土切口。HIS-P2剖面由于地下水位波动表现出氧合形态特征。在HIS-P3剖面上,缩小、肿胀和泥质-土扰动是典型的成土过程。HIS-P1剖面构造较发达(亚角块状),其次是HIS-P3剖面,最后是HIS-P2剖面,为无结构的块状断裂,呈弱亚角块状。虽然土壤的表土容重值在可接受范围内,但底土容重值可能导致根系渗透问题,特别是对于深根作物。HIS-P1和HIS-P3可能会限制作物生长,因为底土的pH值高(> 7.5),这可能会限制植物营养物质(如磷)的利用率。有机碳和氮在各剖面中普遍偏低和极低,多数值分别< 1.25%和< 0.10%。有效磷值在三个剖面中均较低至极低(< 7 mg/kg)。表层土壤饱和值在HIS-P1和HIS-P2剖面较高(约50%),而在HIS-P3剖面非常高(约83.118%)。锌和铁水平被认为不适合作物生产。根据美国农业部土壤分类,WRB土壤资源分为典型红砂(HISP1)、流质失溶(HIS-P2)和铬化钙砂(HIS-P3),分别对应于单聚性皮肤砂、单聚性Cambisols和钙质垂直砂。这三种土壤具有不同的物理化学性质,因此需要在施肥建议之前对土壤进行表征。
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Pedological Characterization of Typical Soils of Dodoma Capital City District, Tanzania: Soil Morphology, Physico-chemical Properties, Classification and Soil Fertility Trends
Pedolological characterization was done in Dodoma Capital City District, Tanzania. Three soil profiles developed from in-situ weathering of granic rocks and designated as HIS-P1, HISP2 and HIS-P3 were described. Fifteen samples were taken from genetic horizons and analyzed for physical and chemical characteristics. The soils were generally very deep, with varying textures. Whereas profile HIS-P2 was dominantly loamy, profiles HIS-P1 and HIS-P3 were both clayey but the latter had heavy clay type. In profile HIS-P1, clay eluviation-illuviation was a dominant pedogenic process manifested by presence of clay cutans in the subsoil. Profile HIS-P2 displayed redoximorphic features due to fluctuating water table. Shrinking and swelling, and argilli-pedoturbation were typical pedogenic processes in profile HIS-P3. Profile HIS-P1 had more developed structure (subangular blocky) followed by HIS-P3 and lastly profile HIS-P2 which was structureless massive breaking into weak subangular blocks. Whereas topsoil bulk density values of the soils were within acceptable range, subsoil BD values are likely to cause problems of root penetration particularly for deep rooted crops. Profiles HIS-P1 and HIS-P3 may present limitations to crop growth due to high pH values (> 7.5) in the subsoil which may limit availability of plant nutrients e.g. phosphorus. Organic carbon and nitrogen were generally low and very low in all profiles with most values being < 1.25% and < 0.10%, respectively. Availabe P values were low to very low (< 7 mg/kg) throughout the three profiles. Topsoil base saturation values were high (> 50%) in profiles HIS-P1 and HIS-P2 but very high throughout proflie HIS-P3 (83 118%). Zn and Fe levels were rated as inadequate for crop production. According to USDA Soil Taxonomy, the soils were classified as Typic Rhodustults (HISP1), Fluventic Dystrustepts (HIS-P2) and Chromic Calcitorrerts (HIS-P3) corresponding to Haplic Cutanic Acrisols, Haplic Cambisols and Calcic Mazic Vertisols in the WRB for Soil Resources. The three soils had different physico-chemical properties, hence the need to characterize soils before fertilizer recommendations is met.
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