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首页> 外文期刊>International Journal of Agriculture and Forestry >Determination of Potassium Levels in Intensive Subsistence Agricultural Soils in Nyamira County, Kenya
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Determination of Potassium Levels in Intensive Subsistence Agricultural Soils in Nyamira County, Kenya

机译:肯尼亚尼亚米拉县集约化农业土壤中钾含量的测定

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Assessment of potassium levels in agricultural soils of Nyamira County, Kenya was necessitated by the observed progressive drops in maize acreage yields over the years despite use of phosphorus and nitrogenous fertilizers. In the study, concentration levels of potassium and other soil fertility indices such as, organic carbon, cation exchange capacity, exchangeable cations, soil pH, available nitrogen, total and available phosphorus were determined. Five composite soil samples were collected at depths of between 0-30 cm from five farms that have consistently been under intensive cultivation. Fractionation of potassium was achieved by sequential extraction of soil sampleswith distilled water, ammonium acetate and nitric acid in that order. Concentration levels of potassium in the extracts were determined using a flame photometer. Potassium concentration levels obtained from the water soluble soil extracts were used to calculate thermodynamic parameters such as free energy of replacement, potassium activity ratio and ionic strength of the soil solution. The relationship between the adsorbed and equilibrium potassium concentration, quantity/intensity was determined by plotting Freundlich adsorption isotherms. The isotherm was used to determine the buffering capacity ofpotassium and the concentration levels of potassium adsorbed on un-specific sites in the soil. The suitability of the adsorption equation was determined by applying the least square regression analysis. From the study available potassium in the soils ranged from 57 to 70 mg/kg and had amean value of 60.2 mg/kg (ammonium acetate method). The water soluble potassium ranged from 1.8 to 2.2 mg/kg with a mean of 2.02 mg/kg. Nitric acid extracted potassium had a mean of 149.6 mg/kg. The mean free energy of replacement, was found to be indicating that the soils have low supplying power of potassium. The potassium buffering capacity of the soils was found to have a mean of 1.189 mg/kg. The amount of potassium adsorbed on un-specific sites of the soilshad a mean value of 6.993 L/kg. These findingsreveal the extent of potassium depletionin the soils of this region and will form a baseline for working acreage potassium doses required for remediation.
机译:尽管使用了磷和氮肥,但多年来观察到的玉米种植面积逐年下降,因此有必要对肯尼亚尼亚米拉县的农业土壤中的钾含量进行评估。在研究中,测定了钾的浓度水平和其他土壤肥力指数,例如有机碳,阳离子交换能力,可交换阳离子,土壤pH,有效氮,总磷和有效磷。从五个一直精耕细作的农场中,在0-30厘米之间的深度收集了五个复合土壤样品。通过依次用蒸馏水,醋酸铵和硝酸依次萃取土壤样品来分离钾。使用火焰光度计测定提取物中钾的浓度水平。从水溶性土壤提取物中获得的钾浓度水平用于计算热力学参数,例如替代自由能,钾活度比和土壤溶液的离子强度。吸附和平衡钾浓度,数量/强度之间的关系通过绘制弗氏吸附等温线来确定。等温线用于确定钾的缓冲能力和吸附在土壤中非特异性部位的钾的浓度水平。通过应用最小二乘回归分析确定吸附方程的适用性。根据这项研究,土壤中的有效钾含量为57至70 mg / kg,安曼值为60.2 mg / kg(醋酸铵法)。水溶性钾的范围为1.8至2.2mg / kg,平均为2.02mg / kg。硝酸提取的钾的平均值为149.6 mg / kg。发现置换的平均自由能表明土壤的钾供应能力低。发现土壤的钾缓冲能力平均为1.189 mg / kg。土壤非特异性部位吸附的钾量平均值为6.993 L / kg。这些发现揭示了该地区土壤中钾耗竭的程度,并将为补救所需要的有效耕作钾剂量提供基准。

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