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首页> 外文期刊>Journal of the Indian Society of Soil Science >Potassium fixation capacity of surface soils under different land use systems.
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Potassium fixation capacity of surface soils under different land use systems.

机译:不同土地利用方式下地表土壤钾素固定能力

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This study was conducted in Navile, Shivamogga, Karnataka, India to examine the potassium fixation capacity of soils under different land use systems. Twenty-five surface soil samples (five soil samples in each land use system) at 0-20 cm depth were collected from different land use systems viz., agri-system (rice and tobacco), horti-system (arecanut), silvi-system (eucalyptus) and current fallow land use system (control). The water soluble potassium content in surface soils varied from 10.06 to 16.66 mg/kg. Among all the forms of potassium, water soluble potassium was the least dominant fraction. The exchangeable potassium content in surface soils varied from 50.1 to 152.6 mg/kg. The content of mineral potassium in surface soils of different land use systems varied from 0.77 to 1.59%. The contribution of this form to total potassium was maximum compared to other fractions as this fraction includes potassium from potassium- bearing minerals. The content of total potassium in surface soils varied between 0.82 to 1.62%. The results also revealed that the potassium fixation capacity of these soils varied widely. The agri-system (rice) recorded the lowest potassium fixing capacity (0.22 cmol(p)/kg), while the silvi-system (eucalyptus) recorded the highest potassium fixing capacity (0.76 cmol(p)/kg). It is evident that the wide variation in capacity of the land use systems to fix the added potassium is mainly due to the potassium saturation of exchange complex of the soils, nature and amount of clay minerals. Among the five different lands use systems studied, the soils under silvi-system and current fallow land use systems recorded higher potassium fixation capacity than the soils under cultivated land use systems.
机译:这项研究是在印度卡纳塔克邦Shivamogga Navile进行的,目的是研究不同土地利用系统下土壤的钾固定能力。从不同土地利用系统(农业系统(稻米和烟草),园艺系统(槟榔),银杏树)的0-20厘米深度收集了二十五个表面土壤样本(每个土地利用系统中的五个土壤样本)。系统(桉树)和当前休耕土地利用系统(控制)。表层土壤中水溶性钾的含量在10.06至16.66 mg / kg之间。在所有形式的钾中,水溶性钾是最不重要的部分。表层土壤中可交换的钾含量为50.1至152.6 mg / kg。不同土地利用方式的表层土壤中的矿质钾含量在0.77%至1.59%之间。与其他馏分相比,该形式对总钾的贡献最大,因为该馏分包括来自含钾矿物质的钾。表层土壤中钾的总含量在0.82至1.62%之间变化。结果还表明,这些土壤的固钾能力差异很大。农业系统(大米)的固钾能力最低(0.22 cmol(p)/ kg),而农用系统(桉树)的固钾能力最高(0.76 cmol(p)/ kg)。显然,土地利用系统固定增加的钾的能力的广泛变化主要是由于土壤交换复合体的钾饱和度,粘土矿物的性质和数量所致。在所研究的五种不同的土地利用系统中,与耕种土地利用系统相比,造林系统和现行休耕土地利用系统下的土壤固钾能力更高。

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