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Distribution of Soil Iron Oxides along Catena at Two Different Locations, in Erbil Province, Northern Iraq

机译:伊尔比勒省伊拉克北部两国不同地区的土壤铁氧化物分布

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Two locations selected in Erbil province, Northern Iraq. Three pedons were dug in each location on catena and twenty-three soil samples were collected for determine physical and chemical propertie. Increasing iron oxide causes coating of clay particles and decreasing the specific surface area in turn decreasing the ability of soils for adsorbing cations on it surfaces that causes decrease of cations concentration and cation exchange capacity. Conversely, high percentage of iron oxides that is act as cementing agent of soil particles and changing their sizes expectedly, in this way increase sand particles more than silt and clay particles. Total free iron oxides irregularly distributed and vibrated between increasing and decreasing. Generally, total iron oxides percent was relatively increased towards down of catena and highly related with parent material, topography, climate and vegetation cover additionally, related with the following soil forming processes, leaching, weathering, erosion, eluviations and illuviation. Increase iron oxides in study soils indicated to, increase soil development. Results of active ratio indicated to, soil development was increased towards down slope of catena. The objectives of this paper are study the soil characteristics and development of the pedons on catena and study the pathway of iron oxides distribution in pedons on catena.
机译:在伊拉克北部埃尔比勒省选出的两个地点。在Catena的每个位置挖出三个佩托,并收集了23种土壤样品,用于确定物理和化学性质。增加氧化铁导致粘土颗粒的涂层,依次降低比表面积,降低土壤吸附在其表面上的阳离子的能力,从而降低阳离子浓度和阳离子交换能力。相反,高百分比的氧化铁作为土壤颗粒的硬质胶剂,并以这种方式增加了比淤泥和粘土颗粒更大的砂颗粒。在增加和降低之间,总自由氧化铁不规则地分布和振动。通常,氧化铁总氧化锆百分比朝向下降和与母体材料,地形,气候和植被覆盖的高度相关,与以下土壤成型过程,浸出,风化,侵蚀,灭菌和裂藻有关。增加研究土壤中的氧化铁,增加土壤发育。表明的活性比率,土壤开发增加到落下卡丁雅的坡度。本文的目的是研究CATEA上施用的土壤特征和开发,研究CATEA施用铁氧化铁分布的途径。

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